BIG_X_Paleontology.pdf

BIBLIOGRAPHY OF THE GEOLOGY OF INDONESIAAND SURROUNDING AREAS Edition 6.0 September 2016 J.T. VAN GORSEL X. BIOSTRATIGRAPHY, PALEONTOLOGY (Comprehensive Edition) www.vangorselslist.com X. PALEONTOLOGY, BIOSTRATIGRAPHY This chapter of the bibliography contains 434 pages with ~3950 papers. It should be noted that: 1. This is an 'expanded version'. It does not just contain the references in Chapter X of the Bibliography master list, but also contains most of the paleontology/biostratigraphy papers that are under the regions chapters; 2. It includes not only papers from Indonesia, but also paleontological papers from surrounding areas. It is an updated version of the 'Annotated Bibliography of Biostratigraphy and Paleontology of Indonesia- SE Asia' of 337 pages that was published as a supplement to Berita Sedmentologi 29 (April 2014), and has been available online at: http://www.iagi.or.id/fosi/files/2014/04/BS29A_Bibliography_biostrat_hvg_final2.pdf. The present list is organized in nine chapters, arranged by increasing age (except Chapter 9): X.1. General Papers X.2. Quaternary-Recent faunas- microfloras and distribution X.3. Tertiary X.4. Cretaceous X.5. Jurassic X.6. Triassic X.7. Permian- Carboniferous X.8. Ordovician- Devonian X.9. Quaternary Hominids, Mammals X.1. General Papers Biostratigraphy is the main tool for age determinations of sedimentary rocks, and good age control is obviously critical for all geology interpretation. In addition, fossil assemblages provide information on depositional environments and paleoclimate. Paleobiogeographic patterns can be important constraints on the plate reconstructions of the SE Asia mosaic of tectonic blocks. Chapter X.1 contains a number of general papers on fossil faunas-floras of the region. X.2. Quaternary, General This section mainly contains papers on the taxonomy of modern or sub-recent microfaunas and microfloras, as well as their distribution in Recent environments of SE Asia. An understanding of modern biofacies distributions is obviously significant for the interpretation of depositional environments and paleoclimates in the geological rock record. These biofacies patterns, in turn, are invaluable for sequence stratigraphy interpretation Tables 1 and 2 list selected papers on present-day environmental distribution, sorted by environments. Chapters X.3- X8 deal with fossil faunas and floras of the region, organized by increasing age. Bibliography of Indonesia Geology , Ed. 5.1 2 www.vangorselslist.com March 2014 TABLE 1 MODERN FORAMINIFERA DISTRIBUTION FAUNA AREA REFERENCES Benthic foraminifera Challenger Exped.1873- Brady (1884), Barker (1960) , (Jones 1994) Monographs' 76 Durrand Collection Millett (1898-1904) Albatross Exped. 1891 Cushman (1921) Siboga Exped. 1899-1900 Hofker (1927, 1930, 1951) Snellius Exped. 1929-30 Hofker, 1978) Snellius II Exped. 1984- Van Marle, (1988-1991) 85 Recent Indonesia catalog Adisaputra, Hendrizan & Kholoq (2010) Brackish, estuarine SE Sulawesi Horton et al. (2005) N Borneo Dhillon (1968), Bronnimann & Keij (1986), Malay Peninsula Mahani et al. (2010, 2011), Culver et al. (2012, 2013) Delta front, prodelta, Mahakam Delta, Villain (1995), Lambert (2003) bay Java- north coast. Rositasari (2010) N Borneo Ho Kiam Fui (1971) Carbonate NW Java (incl. P. Seribu) LeRoy (1938), Wijono (1991), Renema (2008), Suhartati (2009) environments E Kalimantan Renema (2006) SW Sulawesi Troelstra et al. (1996), Renema & Troelstra (2001), Renema et al. (2001) Bali, Lombok Barbin et al. (1987), Adisaputra (1998, 2000), Renema (2003) PNG Haig (1979-1993) Langer & Lipps (2003) Great Barrier Reef Jell et al. (1965), Renema et al. (2013) NW Australia Parker (2009), Parker & Gischler (2011) Shelf seas Java Sea, Paternoster Myers (1945), Biswas (1976), Hofker (1978), Boichard et al. Platform (1985), Isnaniawardhani (2009) Sunda Shelf- S China Sea Waller (1960), Szarek (2001), Szarek et al. (2006), Suhartati & Muchslin (2012) Makassar Straits Adisaputra & Rostyati (2003) Arafura Sea Suhartati & Rubiman (2010) Deep marine East Indonesia Hofker (1927, 1930, 1951), Van Marle (1988, 1991) Makassar Straits Rositasari (2010), Suleiman et al. (2011) South China Sea-deep Miao & Thunell (1993, 1996), Jian & Wang (1997), Marquez (1999), Szarek et al. (2009) Sulu Sea Rathburn et al. (1994, 1995), Szarek et al. (2007) Andaman Sea Frerichs (1970, 1971) Timor Sea, Indian Ocean Loeblich & Tappan (1994), Basov & Krashenninnikov (1995), Murgese & De Deckker (2005) , De & Gupta (2010) Bibliography of Indonesia Geology , Ed. 5.1 3 www.vangorselslist.com March 2014 TABLE 2 OTHER MICROFAUNA/MICROFLORA - MODERN DISTRIBUTION FAUNA/ FLORA AREA REFERENCES Ostracodes Mahakam Delta Carbonel & Moyes (1987), Carbonel and Hoibian (1988) Sunda Shelf Mostafawi (1992) Java Sea, Bali Dewi (1997), Mostafawi et al. (2005) P. Seribu, Jakarta Bay Watson (1988), Whatley & Watson (1988), Fauzielly et al (2013) Malacca Straits Whatley & Zhao (1987, 1988) Other Indonesia Muller (1906), Keij (1953) Pollen, spores and SE Asia case studies Flenley 1973, Haseldonckx (1977), Gastaldo (op. div), Van kerogens der Kaars (1991), Chandra (2010), Sun et al. (1999) N Borneo Simmons et al. (1999) E Kalimantan-Mahakam Hardy & Wrenn (2009) Sulawesi Engelhardt et al. (2007) Diatoms (fresh-brackish Lake Toba, Sumatra Van der Marel (1947) waters) SE Sulawesi Horton et al. (2007) Malay Peninsula Zong & Kamaludin (2004) Indonesia Van Iperen et al. (1993), De Deckker & Gingele (2002) Diatoms (deep water) South China sea Wu et al. (2013) Calcareous nannofossils SE Asia Okada (1983), Varol (1985), Fernando et al. (2007) Radiolaria Banda Sea Harting (1863), Van de Paverd (1989) Dinoflagellate cysts Java Sea, etc. Lirdwitayaprasit (1997a,b), Matsuoka et al. (1999), Kawamura (2004), Furio et al. (2006, 2012), Hessler et al. (2013) X.3. Tertiary A vast amount of literature has been published on Indonesian Tertiary faunas. The principal tools for biostratigraphic subdivision of Tertiary sediments in Indonesia are planktonic foraminifera and calcareous nannofossils in open marine deposits, complex larger foraminifera in shallow marine carbonates and palynology in non-marine and marginal marine deposits. The basics of the Eocene- Recent larger foraminifera zonation, also called the 'East Indies Letter Classification', were developed in the 1920's. Ranges of the key genera on which this is based are shown in the figure below. More detailed and better calibrated charts like this can be found in the literature. Bibliography of Indonesia Geology , Ed. 5.1 4 www.vangorselslist.com March 2014 An early version of a distribution chart of Tertiary larger foraminifera, that defined the 'East Indies Letter zonation' (Van der Vlerk, 1948). Suggested reading Tables 3 and 4 list some of the key papers on Cenozoic biostratigraphy by topic. This listing is by no means complete. TABLE 3 CENOZOIC FORAMINIFERA BIOSTRATIGRAPHY FAUNA/FLORA AREA REFERENCES General Indonesia Billman & Scrutton (1976), Van Gorsel (1988), Lunt (2013a,b) , Van Gorsel, Lunt & Morley (2014) Neogene General Blow (1969, 1979), Kennett & Srinivasan (1983), Bolli & Saunders (1984) planktonic Java Bolli (1966), Blow & Banner (1966), Van der Vlerk & Postuma (1967), Hartono foraminifera (1960, 1969), Harsono P (1968, 1983), Blow (1969, 1979), Wibisono (1972), Kadar (1972- 2008), Saint-Marc & Suminta (1979), Van Gorsel & Troelstra (1981), Harsono et al. (1998) West Papua/ PNG Belford (1962, 1966, 1967, 1984, 1988) Sumatra LeRoy (1948, 1952), Blow & Banner (1966), Kadar et al. (2008) Andaman Sea Frerichs (1971) Paleogene Kalimantan Thalmann (1942), Baumann (1972) planktonic Java Hartono (1960, 1969), Purnamaningsih S & Harsono P. (1981), Novita (2014) foraminifera West Papua Belford (1966, 1974, 1989) Larger General Douville (1905-1924), Mohler (1946), Adams (1965-1992), Lunt (2003), Lunt foraminifera- & Allen (2004), Renema (2002) Letter zonation Van der Vlerk & Umbgrove (1927), Leupold & Van der Vlerk (1931), Gerth (1935), Tan Sin Hok (1939), Van der Vlerk (1959), Clarke and Blow (1969), Adams (1970), Haak and Postuma (1975), Boudagher-Fadel & Banner (1999), Govindan (2003), Lunt and Allan (2004), Renema (2007), Matsumaru (2011) Bibliography of Indonesia Geology , Ed. 5.1 5 www.vangorselslist.com March 2014 Cycloclypeus Tan Sin Hok (1932), MacGillavry (1962), Drooger (1955), Adams & Frame (1979) Lepidocyclina Van der Vlerk (1928, 1959-1973), Scheffen (1932), Tan Sin Hok (1936), Caudri (1939), Van der Vlerk & Postuma (1967), Ho Kiam Fui (1976), Van Vessem (1978), Adams (1987), Ghosh & Saraswati (2002) Miogypsina Tan Sin Hok (1936, 1937), Drooger (1953, 1963, 1993), Raju (1974), Schipper & Drooger (1974), De Bock (1976) Heterostegina.- Van der Vlerk (1925), Tan Sin Hok (1930, 1937), Krijnen (1931), Lunt & Spiroclypeus Renema (2014) Austrotrillina Adams (1968) Alveolinids Bakx (1932), Mohler (1949), Wonders & Adams (1991) Nummulitids Verbeek (1871, 1874, 1891), Doornink (1932), Renema et al. (2002) Larger Multiple areas Rutten (1911-1934), Van der Vlerk (1922-1973), Adams (1965, 1992), foraminifera- Boudagher Fadel (1997-2008) faunal studies Sumatra Verbeek (1871-1891), Brady (1878), Douville (1912), Tappenbeck (1936) Java Verbeek (1892), Martin (1881), Douville (1916), Hanzawa (1930, 1965), Caudri (1932, 1939), Doornink (1932), Mohler (1949), Cole (1975), Adisaputra et al. (1978), Adisaputra & Coleman (1983), Boudagher-Fadel (1997-2008), Renema (2002, 2007), Sharaf et al. (2006), Umiyatun et al. (2006), Irwansyah et al. (2011), Rahmawati et al. (2012), Lunt (2013) Kalimantan- Verbeek (1871), Von Fritsch (1877), Provale (1908), Rutten (1911-1926), Van North Borneo der Vlerk (1925, 1929), Tan Sin Hok (1930-1940), Adams (1965), Hashimoto et al. (1973), Hashimoto & Matsumaru (1981), Roohi (1998), Boudagher-Fadel et al. (2000), McMonagle et al. (2011), Cotton et al. (2014) Sulawesi Crotty & Engelhardt (1993), Boudagher-Fadel (2002), Sudijono (2005) West Papua- Schlumberger (1894), Rutten (1914, 1921, 1925, 1936), Crespin (1962), Papua New Guinea Binnekamp (1973), Bain & Binnekamp (1973), Beldord (1974), Brash et al. (1991), Sudijono (2000) Sumba, Kei islands Van der Vlerk (1922, 1966), Douville (1923), Caudri (1934), Bursch (1947) Timor Bakx (1932), Henrici (1934), Hayasaka & Ishizaki (1939, Ritsema (1951), Marks (1954) Smaller benthic Sumatra LeRoy (1939, 1941, 1944) foraminifera Java Koch (1923), Thalmann (1934, 1935), Yabe & Asano(1937), LeRoy (1941, 1944), Van der Sluis & Vletter (1942), Boomgaart (1949), Soeka et al. (1980), Sukandarrumidi (1990), Kadar (1992) Kalimantan, Koch (1926), LeRoy (1941), Mohler (1946), Billman and Witoelar (1974), Sabah Billman et al. (1980), Whittaker & Hodgkinson (1979) Seram, Timor Fischer (1921, 1927), Koch (1925), Rocha & Ubaldo (1964) New Guinea Belford (1962), Haig (1982) Bibliography of Indonesia Geology , Ed. 5.1 6 www.vangorselslist.com March 2014 TABLE 4 OTHER MICROFAUNA/MICROFLORA BIOSTRATIGRAPHY FAUNA/FLORA AREA REFERENCES Calcareous Indonesia Panuju (2010) nannofossils Kalimantan, N Borneo Keij (1964), Lambert & Laporte-Galaa (2005), Panuju et al. (2007) Java Okada (1981), A. Kadar (1990,1991), Kapid et al. (1991-2003), Siesser et al. (1984), Theodoridis (1984), Nur Hasjim (1988), Rubiyanto & Harsolumakso (1996), Choiriah & Kapid (1999), Panuju & Kapid (2007) Sulawesi Kadar & Sudijono (1993), Priyadi & Sudijono (1993) Roti Tan Sin Hok (1927), Kamptner (1955), Jafar (1975) Timor, Tanimbar Hadiwisastra (1987), Hadiwisastra (1993) Recent- Banda Sea Kleine (1990) Ostracodes multiple areas Brady (1880), LeRoy (1939, 1941), Kingma (1948), Van den Bold (1950), Keij (1953-1979), Hanai et al. (1980) C Java McKenzie & Sudijono (1981) Timor Fyan (1916) E Kalimantan Doeglas (1931) South China Sea Zhao (2005) Radiolaria Roti –Mio-Pliocene Tan Sin Hok (1927), Riedel (1953) Sumatra forearc Ling & Samuel (1998), Celebes, Sulu Seas Scherer (1991a,b) Waigeo Ling et al. (1991) Diatoms Java Grandjean & Reinhold (1933), Reinhold (1937), Ninkovich & Burckle (1979), P. Siregar (1981), Burckle (1982) Buton Reinhold (1952) Timor Sea Jouse & Kazarina (1974) Spores-Pollen Zonations Germeraad et al. (1968), Morley (1977, 1991), Yakzan et al. (1996), palynology Mao & Foong (2013) Dispersal, climate Morley (1998, 2000, 2003, 2007, 2011, 2012), Lelono (2007, 2012) E Kalimantan, Barre de Cruz (1982), Carter & Morley (1995), Polhaupessy (1998, Makassar Straits 2007), Morley et al. (2004, 2006), Morley & Morley (2010) East Java Sea Lelono & Morley (2011) Java Polhaupessy (1980, 2009), Takahashi (1982), Rahardjo et al. (1994), Van der Kaars & Dam (1995, 1997), Lelono (2000, 2001, 2007, 2012) Natuna Basin Morley et al. (2003, 2007) West Papua, PNG Lelono (2008), Playford (1982) Dinoflagellate cysts Java Matsuoka (1981, 1983, 1984), Morgenroth et al. (2000, 2008, 2011) NW Borneo Besems (1993) Sunda Shelf Kawamura (2002) Bibliography of Indonesia Geology , Ed. 5.1 7 www.vangorselslist.com March 2014 X.4. Cretaceous and X.5. Jurassic For a recent review of Cretaceous and Jurassic faunas and floras of Indonesia see Van Gorsel (2014). Relatively little has been published on Cretaceous and Jurassic faunas of Indonesia, and references to these are mainly found under the areas in which they occur. The Jurassic in East Indonesia (Misool, Sula, W Papua, etc.) appears to be dominated by open marine facies. Relatively many paleontological papers on ammonites, belemnites, brachiopods, bivalve mollusks, etc., were published, most of them in the early 1900's. Deep marine Late Jurassic pelagic limestone facies with abundant radiolarians and calcispheres are known from Buton, E Sulawesi, Timor, Seram and Misool (Wanner 1940). In these areas the Jurassic is overlain by relatively thin Cretaceous pelagic limestones, with common Globotruncana in the upper parts. In West Indonesia, Jurassic shallow marine carbonate facies are more common, exemplified by papers on corals, foraminifera, etc., from N and SW Sumatra (summarized in Fontaine and Gafoer 1989) and the Bau limestone of the W Sarawak- W Kalimantan border area (Wolfenden 1965, Beauvais and Fontaine 1990) Mid-Cretaceous shallow marine limestones with Orbitolina and rudists have been known from numerous localities across Kalimantan and W Sarawak since the late 1800's (Martin 1888, 1889), and also from S Sumatra (Lampung and Gumai Mts.; Zwierzycki 1931, Musper 1934, Yabe 1946) and the Lok Ulo accretionary complex of C Java (Verbeek 1891). These are generally interpreted as low-latitude Tethyan forms, and are not known from Australia- New Guinea. Today's most powerful biostratigraphic tool in this time interval is probably dinoflagellates. It is widely used in NW Australia and Papua New Guinea wells, but not much work has been done, or published, on this in Indonesia. Suggested reading See Tables 5 and 6 TABLE 5 CRETACEOUS FAUNA/FLORA AREA REFERENCES SE Asia Hashimoto et al. 1975 Faunas- General Sumatra Beauvais et al. 1989 Upper Cretaceous Birds Head Visser and Hermes 1962 Pseudorbitoides, Papua New Guinea Crespin and Belford 1957, Glaessner 1962 Omphalocyclus Borneo Van Gorsel 1978 Timor, Leti Schubert 1915, De Roever 1940, Sartono 1975 Sula islands Kholiq et al. 2011 Misool Vogler 1941 Upper Cretaceous Sabah Adams and Kirk 1962 planktonic Central Java Asikin et al. 1992 foraminifera (Globotruncana) W Kalimantan Tan Sin Hok 1936 SE Sulawesi, Buton Van der Vlerk 1925, Koolhoven 1932, Keijzer 1945 PNG Owen 1973, Haig 1981 Halmahera Brouwer 1923 Calc. Nannoplankton West Papua Panuju et al. 2010 Sumatra Baumberger 1923, 1925, Musper 1934 Molluscs Kalimantan Martin 1889, Vogel 1904 South Sulawesi Hasibuan and Limbong 2009 Bibliography of Indonesia Geology , Ed. 5.1 8 www.vangorselslist.com March 2014 De Beaufort 1932 Rudists NW Borneo Lau 1973. Buton. Harloff 1929 Zwierzycki 1931. Wolfenden 1965. Beauvais and Late Jurassic limestones Sarawak (Bau Lst) Fontaine 1990 with Cladocoropsis. Verbeek and Fennema 1896. Von Koenigswald 1939 PNG Matsumoto and Skwarko 1991. Vogler U Jurassic calcispheres Timor 1940. Pseudocyclammina Silvestri 1925. Yabe 1946. Jasin 1985-2000. S Sumatra 1989 Tan 1978. Clowes 1997.vangorselslist. Yabe 1946. Geinitz 1883. Martin 1888. Tan Sin Hok 1927. 1994 Buton Soeka 1991. 2000. Timor Wanner 1940 calpionellids NW Australia Brunnschweiler 1960 Sumatra Baumberger 1925 SW Sarawak Ishibasi 1982 Ammonites W Kalimantan Krause 1904. 1989. Bassoulet 1989 Bibliography of Indonesia Geology . Ling and Smith 1995 Roti Tan Sin Hok 1927. Munasri 1998 Ungar (Tanimbar) Jasin and Haile 1996 N Indian Ocean Renz 1974. Ed. Baumgartner 1993 Lower Cretaceous Buton. 2013. Bassi et al. Jasin and Tongkul 2013 C Kalimantan Hinde 1900. Beauvais 1983. 2009 West Sulawesi Brouwer 1934 Early Cretaceous W Sarawak Hashimoto and Matsumaru 1977 Orbitolina Sabah Leong 1972 Central Java Verbeek 1891. 1981. Bennett et Sumatra al. 2011 SE Kalimantan Martin 1888 Misool Boehm 1924 TABLE 6 JURASSIC FAUNA/FLORA AREA REFERENCES Sumatra Fontaine et al. Sato 1975. Riedel and Sanfilippo 1974. Riedel 1953 Timor Tan Sin Hok 1927. Skwarko 1967. Grunau 1965 SE Kalimantan Wakita et al. PNG Heinz 1928. Brouwer 1919. Djamal et al. 1932. 1983 Jurassic Stratigraphy Indonesia Wanner 1931. Aitchison 1994. Beauvais et al. 1983 Von Fritsch 1879. 1993 Lower Cretaceous West Papua Challinor 1989 belemnites NW Australia-SE Asia Mutterlose 1992 Fish (shark teeth) Timor Weiler 1932. Skwarko et al. Hofker Kalimantan 1966. Musper 1934. Sukamto and Westermann 1992 Seram. Hanzawa 1947.1 9 www. West Papua . 1995. Sabah 2012. Munasri 1995. Bolli 1974 (Pithonella) Buton Bothe 1927 Roti Tan Sin Hok 1927 NW Kalimantan/ Wilford and Kho 1965. Wanner 1940. Wakita et al. 1998 SW Sulawesi Wakita et al 1994. 2013 Radiolaria South Central Java Okamoto et al. 5. 1994. Misool. Fontaine and Ho 1989. Hashimoto and Matsumaru 1974. Asis and Jasin Sarawak. 1889.com March 2014 . Skelton et al. Helby et al. Mantle 2009. 1965. Stevens 1964 Middle. Hasibuan 2004 PNG Skwarko 1973. Stolley 1929. 1960. Bassoulet 1989. Schluter 1928. 1903. Mantle Dinoflagellate zonations and Riding 2010.vangorselslist.PNG and Getty 1970. Ed.b PNG Haig 1979 Cookson and Eisenack 1958. Wandel 1936 Timor. E Sulawesi Wanner and Jaworski 1931. Gerth 1927. 1983. Sarawak Tamura and Hon 1977. 1998 W Sarawak Jasin et al. Challinor Sula Islands and Skwarko 1982. Babar Rothpletz 1892. Martin 1899. Misool Stolley 1929. M-U Jurassic ammonites Westermann 1995 Timor. 1996. 1981 Sumatra McCarthy et al. Yabe 1946. Hirano et al. Wandel 1934. 2012 Papua New Guinea Davey 1988.com March 2014 . Vogel 1896. Westermann and Callomon 1988 Boehm 1913. Helby Morgan and Jurassic. Krumbeck 1923. Roti Sashida et al. Buru. Misool Krumbeck 1934 Inoceramus haasti) E Sulawesi Hasibuan and Kosworo 2008 ('anti-tropical') Papua New Guinea Glaessner 1945. 1991 Timor. 1991 Boehm 1907. Challinor 1989.E Cretaceous NW Australia margin Partridge 1987. 1935. 1912. 2001 SE Kalimantan Wakita et al. Westermann and Callomon 1988. Newton 1897. 1999. 1989 Late Jurassic shallow W Sarawak (Bau Lst) Bayliss 1966 marine foraminifera Sumatra Silvestri 1925. 2006 Sula. Riding. 1923 U Jurassic bivalves (Malayomaorica. Hayami 1984 E-M Jurassic bivalves Timor Krumbeck 1923 Misool Soergel 1913. Haig and Bandini 2013 Sula islands Panuju 2011 U Jurassic nannofossils Timor Kristan-Tollmann 1988a. 5.Late Jurassic Belemnites Yamdena Stolley 1929 W Papua/ PNG Challinor 1990 Central Sulawesi Stolley 1943 Indo-Pacific Stevens 1965 NW Kalimantan. Jaworski 1933 E Jurassic ammonites Roti. 1900. 1932. Timor Krumbeck 1922 W Kalimantan Krause 1911. Bassoulet 1983 Sarawak Beauvais and Fontaine 1990 U Jurassic corals Sumatra Beauvais 1983. Westermann W Papua. Roti Boehm 1908 Babar Callomon and Rose 2000 W Kalimantan Schairer and Zeiss 1992 Yamdena. Challinor 1989. Grant-Mackie et al. 1974. Stolley 1929. 1999. Roti. Welsh 1990 Bibliography of Indonesia Geology .1 10 www. NE Palawan Fontaine et al. 2004. Jasin and Said 1999 M-U Jurassic Radiolaria East Sulawesi Hojnos 1934 Sula Islands Pessagno and Meyerhoff Hull 2002 Timor. Kruizinga 1921. Edwards and Glaessner 1953 Australia NW Shelf Brunnschweiler 1960 Sula Islands Kruizinga 1926. Partridge 2006. Seram. Roti Krumbeck 1922. 1972 Late Trias Palynofloras Seram Martini et al. East Sulawesi. They represent depositional settings around two branches of the Tethys Ocean. Hayami 1984 X. S China Sea Kudrass et al. 1986 Krusin Flora SW Sarawak Kon'no 1968. Seram. General Wanner 1907. Triassic rocks and faunas are relatively widespread across Indonesia. Buton.. These Tethys ocean branches closed in Late Triassic and Early Cretaceous times respectively. Triassic For a recent review of Triassic faunas and floras of Indonesia see Van Gorsel (2014). etc. Jongmans 1951. Suggested reading See Table7 TABLE 7 TRIASSIC FAUNA/FLORA AREA REFERENCES Trias faunas. Hasibuan 2008 biostratigraphy Timor Charlton et al. 2009 Late Tr(?) Bintan Flora Riau Archipelago. Thailand Kon'no and Asama 1973 Late Trias Tonkin/ Reed Bank. 1992 Sula Islands Lelono and Nugrahaningsih 2012 Spores-Pollen NW Australia margin Burger 1996 Jurassic Coccoliths Timor Kristan-Tollmann 1988 E Jurassic brachiopods Seram Wanner and Knipscheer 1951 Lithiotis Limestone Timor Fatu Limestone Krumbeck 1923. 5. Wade-Murphy et al. 2004 Bibliography of Indonesia Geology . Misool Helby and Hasibuan 1988. separated by Cimmerian Blocks that stretch all the way from Turkey in the West to Sibumasu in the East. West Kalimantan. non-marine to deep marine clastics. Sarjeant et al. Paleo-Tethys and Mesotethys. 2008 N Vietnam. Ambon. and have been described from Timor- Roti. Ed. including volcanics.com March 2014 .1 11 www.vangorselslist. represent a wide variety of facies. shallow marine reefal to deep marine pelagic carbonates and oceanic radiolarian cherts. Geyer 1977. Buru. Triassic sediments. Misool.6. etc. Debates continue on the exact position of these Tethys sutures and possible Sibumasu -equivalent blocks in the Indonesian region East of the Malay Peninsula and Sumatra. Many of the papers dealing with Triassic faunas from East Indonesia remarked on the 'Tethyan' nature of faunas and the similarities with faunas and rock types in the eastern Alps. Sumatra. 1931. 1973 Malay Peninsula. Koike 1984. Diener 1923. 1989 Trias conodonts Nogami 1968.Dinoflagellates Seram Helby et al. Sarawak Vogel 1904. Tamura 1970. Hasibuan 1990. Von Kutassy 1934 Buton Hasibuan 2010 Timor Krumbeck 1922. 5. Kutassy Halobia. Krumbeck 1913 U Trias brachiopods Ambon Jaworski 1927 (incl. Wanner 1907. 1983 Buru. 2005 Seram Wilckens 1937 Heterastridium Timor. Rose 1994. Gheyselinck 1934 Wanner 1911. Musper 1930 Buru Krumbeck 1913 M-L Trias shallow Misool Jaworski 1915 marine bivalves (Myophoria assemblages) Papua New Guinea Skwarko 1963. 1915. Krumbeck 1921. Silberling 1985 M-L Trias pelagic Seram Krumbeck 1922 bivalves (Daonella.1981. Pia 1924 Lovcenipora Timor Vinassa de Regny 1915. Newton 1903. Krumbeck 1914. Rhaetian Misolia) East Sulawesi Von Loczy 1934. 1973. Gerth 1910. 1924.com March 2014 . Von Arthaber 1926. Wanner 1928 Welter 1915. Gruber in Kristan-Tollmann 1987 Sumatra Volz 1899. Krumbeck 1924. Krumbeck 1914 PNG Skwarko 1967. MacFarlan et al. Rothpletz 1892. 1922. Berry et al. Welter 1914. 1973 Gastropods Timor Tichy 1979 Seram. Roniewicz et al. Seram Gerth 1909. Nicoll and Timor Foster 1998 M-U Trias radiolarians Timor Hinde 1908. 1925.vangorselslist. Nakazawa and Bando E-M Trias ammonites Timor 1968. Seram Krumbeck 1913. Ichikawa 1958. Singapore Kobayashi and Tamura 1968. Misool 2011 Seram Deninger 1918. 1952. 2009 Sumatra Metcalfe et al. Cox 1936. 2004 Buru Gerth 1910 Late Trias corals Timor Vinassa de Regny 1915. Ed. 1927 (hydrozoan) Misool Krumbeck 1913 Von Seidlitz 1913. 1987. Kieslinger Timor U Trias ammonites 1924. Wanner 1923. 1999 U Trias dasyclad algae Seram. 1915. 2012. 1990 U Trias belemnites Timor Wanner 1911. Krumbeck 1922. 1984. 1924? Sumatra Vinassa de Regny 1915 Timor Kristan-Tollmann 1988 U Trias foraminifera Sumatra Vachard 1989 PNG Kristan-Tollmann 1986. Monotis) Timor. 1979. Buru Pia 1924 Bibliography of Indonesia Geology . Roti 1931. Sashida et al. Kummel 1968. Burur Wanner 1907. 1952 Buru Von Seidlitz 1913. Tatzreiter 1980. Tamura and Hon 1977. Tokuyama 1961. Von Bulow 1915. 1996. Grunau 1957 NW Australia margin Campbell 1994 Thailand Kobayashi and Tokuyama 1959 W Kalimantan.1 12 www. Skwarko and Kummel 1974 W Sumatra Boettger 1981. Martini et al. Brayard et al. Sugiaman and Andria 1999).X.com March 2014 . 5. Permian crinoids from Timor (Wanner 1921) Permian deposits are relatively widespread.vangorselslist. conodonts and graptolites from West Papua. The oldest fossils from Western Indonesia are a Devonian Heliolites coral and a stromatoporoid from a locality in C Kalimantan (Rutten 1940. etc. Vachard 1990) and Timor (numerous papers). Early Paleozoic For a recent review of Paleozoic faunas and floras of Indonesia see Van Gorsel (2014). The classic. including W Papua (Visser and Hermes 1962). Sumatra (Fontaine and Gafoer 1989). but also from West Sumatra and West Papua. 1947. The oldest fossils from Indonesia are Ordovician-Silurian nautiloids. but their localities were never confirmed. all indicating a 'Cathaysian' equatorial climate. Permian . rich marine Permian faunas from Timor have been the subject of numerous papers. and showing that these parts of Sumatra were not part of the much colder Gondwana continent at that time.8. W Kalimantan-Sarawak (Terbat Lst. A fairly extensive body of literature exists on Paleozoic faunas of Indonesia. The E-M Permian of W Sumatra contains reefal and fusulinid limestones and the famous 'Jambi Flora' of SW Sumatra.). They were believed to probably come from a local Chinese pharmacy by Von Koeningswald (1933). A larger volume of more modern studies of comparable faunas and floras is available from nearby SE Asia (Malaysia. Ed. Suggested reading See Tables 8- Bibliography of Indonesia Geology .1 13 www. The Indonesian region is host to some important localities of Paleozoic fossil faunas and floras. The Late Paleozoic faunas from Sumatra are generally comparable with those described from Thailand and Peninsular Malaysia.7. and not written in English or Indonesian. Most of these are from the Permian of Timor and adjacent islands. but much of it is in old and commonly hard to find papers.Carboniferous and X. Thailand. A Late Devonian brachiopod and a Permian ammonite were reported from the Kalosi region of C Sulawesi by Brouwer (1919). Fontaine 1990. Archbold 1981. Timor. Van Waveren et al. Ueno 2003. 1961 Bangka.TABLE 8 PERMIAN FAUNA/FLORA AREA REFERENCES Timor Wanner 1926. Haniel 1915a. 2008. Kato et al. Sakamoto and W Sarawak Ishibashi 2002 NE Kalimantan Tan Sin Hok 1930. 2013 Timor Wanner 1916. Fontaine and Gafoer 1989 Jongmans 1940. Wang 1947. 1940. 1983 Timor C. 1973 Ammonoids Bangka/Belitung Kruizinga 1950. 1916. Ed. Leti Gerth 1950. Van Overeem 1960 Permian Fusulinid Krekeler 1932. 1962. 2006 South Sumatra De Neve 1949. Sanderson 1966. West Papua Glenister et al. Glenister et al.b. Winkler Prins 2008 West Papua Visser and Hermes 1962. Rigby 1997. West Sumatra Tan Sin Hok 1933. 1998. 2009 'Cathaysian' flora Belitung Jongmans in Van Overeem 1960 NW Kalimantan Jongmans in Zeijlmans 1939 West Papua Playford and Rigby 2008 Palynoflora Australia Kemp et al. Charlton et al. Furnish and Glenister 1971. Shimizu 1966. Archbold and Bird 1989. Vachard 1989. Sumatra Crippa et al. 2008. 2005. Thompson 1936a. 2013 West Papua Visser and Hermes 1962 Sumatra Tien 1986 Tubiphytes Timor Riding and Barkham 1999 ( = Shamovella) Corals Timor Gerth 1921. Srivastava Cathaysian flora and Agnihotri 2010 Posthumus 1927. 2007. 2001. Webster 1998. Blastoids Timor Sprinkle and Waters 2013 Wanner 1915. 2002 Permian General Sumatra Fliegel 1901. Ozawa 1929. Jasin 1997 Radiolaria Thailand Kamato et al. Thompson 1949. Hamlet Brachiopods 1928. Leti. 1972. Krumbeck 1924. Roti Barkham 1989. 1929. Jongmans and Gothan 1935. 1940. Hasibuan 1994 Mollusks Sumatra Fliegel 1901 West Papua Dickins and Skwarko 1981 Fliegel 1901. Von Schouppe and Stacul 1955. 1993. Hopping and Wagner in Visser and Hermes Mixed Glossopteris- West Papua. 2000.b. Breimer and Macurda 1965. Meyer 1922. Smith 1927. Archbold et al. Leti Davydov et al. 2014 Rothpletz 1892. J.b. 1942. Playford and Rigby(2008. Li and Wu West Sumatra 1994. Spiller and Metcalfe 1994. Tan Sin Hok 1933. Hahn and Weber 1981. Charlton et al. Hasibuan et al. Timor.1 14 www. 5. De Maresz Oyens 1940 Crinoids Belitung Strimple and Yancey 1976 Wanner 1924. 1995.vangorselslist. 1941.1923. De Roever 1940. Lange 1925. Cummings NW Kalimantan/ foraminifera 1962. Wanner 1922. Broili 1915. Archbold and Timor. Nogami 1963.1951.E Triassic Malay Peninsula Sashida et al. Wanner and Sieverts 1935. Koker 1924. Vachard 1990.com March 2014 . Fontaine 1983. 1991. Roti. 1995. Asama 1976. 1922. Bibliography of Indonesia Geology . 1999. Wanner 1940. Tan Sin Hok (in Krekeler 1933). Fontaine 1990. Sugiaman and Andria 1999 (Upper Kutai) Schubert 1915a. Booi et al. 1977 Permian. 1982 Geinitz 1876. 1932. Belitung De Roever 1951. 1933. Volz 1904. Von Staff 1909. 2002. 2013 Timor Van den Boogaard 1987 Conodonts SE Asia Mei and Henderson 2001. Oliver et al. Sorauf 1984. 1999 Thailand Fontaine et al. and Burton 1971 Ordovian? orthoconic W Papua Central Range Crick and Quarles van Ufford 1995 nautiloids Birds Head Kruizinga 1957 E Ordovician conodonts W Papua. Minato and Kato 1965. Minato and Kato 1965. 2010 Silurian corals W Papua. 1989 Corals West Papua Kato et al. 1947. 1991 W Sumatra Metcalfe 1983. 1959. 5.b Thailand Fontaine et al. Sugiaman and Andria 1999 Devonian brachiopods West Papua Stehn 1927. Heluk River Fortey and Cocks 1986 (M Ordovician) W Papua Star Mountains Kobayashi. Birds Head Visser and Hermes 1962 (Silurian) graptolites W Papua. Teichert 1928. Wang et al. 1989. 1995 fish SE Asia Wang et al. 2002 Ostracodes Timor Grundel and Kozur 1975. Vachard 1989 Foraminifera NW Borneo Cummings 1962.S of C Range Van den Boogaard 1990. 2004 West Sumatra Volz 1904.vangorselslist. Musper 1938 Silurian conodonts W Papua. Sanderson 1966. Nguyen Duc Tien 1989a.DEVONIAN FAUNA/FLORA AREA REFERENCES West Papua Gerth 1927. 1986 Conodonts West Papua Nicoll and Bladon 1991 TABLE 10 ORDOVICIAN. 1994 Smaller Sumatra Nguyen Duc Tien 1989a. Ed. Keijzer 1941. Niermann 1975.1 15 www. 1995 Devonian corals NE Kalimantan Rutten 1940.b foraminifera Sibumasu Zhao and Zhou 1987. Bless 1987 TABLE 9 CARBONIFEROUS FAUNA/FLORA AREA REFERENCES W Sumatra Fontaine 1983.S of C Range Gerth 1927. Vachard 1990 Sumatra Metcalfe 1983. S Central Range Nicoll 2002 Bibliography of Indonesia Geology . Nicoll and Bladon 1991 Ordovician-Silurian W Papua. Feuilleteau de Bruyn 1921 Late Silurian-Devonian W Papua Turner et al.com March 2014 . Homo sapiens. East Java. Bibliography of Indonesia Geology .vangorselslist. common in Asia at that time. were reported from West Kalimantan and from Timor.1 16 www. have been interpreted as impoverished island faunas of Asian origin.0 Ma. Pleistocene vertebrate faunas were from SW Sulawesi. Eocene acanthocerids (Hippopotamus family). separating balanced ‘Asian’ Sundaland faunas from unbalanced island faunas on Sulawesi. followed by the arrivals of a more diverse Asian mammal population (including Homo erectus) in the Middle Pleistocene around 1 Ma. (1994) reported a radiometric age of 1. Similar forms from East Java and West Java suggest these parts of Java were also islands in the Early Pleistocene. but still primitive Upper Pleistocene hominid fossils were found in a Solo River terrace at Ngandong in East Java. not humans or other predators). Well-known biogeographic boundaries like the Wallace Line (1869).5 Ma. Only a selection of papers from this popular field of research is included in this bibliography. The first fossil evidence for human evolution and migration came with the discovery of ‘Java Man’ (Pithecanthropus erectus. Jacob et al. Land mammals started to appear on Java. Flores is also the site of the latest new discovery of cave-dwelling Homo erectus-like dwarf population of hominids of Late Pleistocene age (95-13 ka). The incomplete fossil record. Finding this rare material was a remarkable story of perseverance and luck. where there is a succession of faunas reflecting island conditions in the Late Pliocene. Quaternary Hominids. The most widely accepted interpretation of Homo erectus history has been an evolutionary transition from Homo habilis in E Africa around 1. and suggested it may have originated in Asia instead of Africa. Early island populations are typically composed of a limited number of migrant species of Asian origin that are relatively good swimmers (elephants. Ed. Flores and islands farther East. In the absence of carnivorous predators.6. separating the Australian faunas of Australia and New Guinea in the SE from the impoverished island faunas to its West. Additional Homo erectus fragments were reported in the 1930’s and later. Swisher et al.01 Ma. Present-day distributions of faunas and floras still reflect plate tectonic past history.com March 2014 .8-1. named Homo soloensis (‘Solo Man’) and represent another much-debated group of hominids transitional between H.Recent terrestrial vertebrate evolution and dispersal is best documented on Java. mammal species commonly developed into either dwarfed species (pygmy Stegodon elephants) or giants (giant tortoises. Komodo lizards. The history of Late Pliocene. as these areas emerged to form significant land areas during Plio.X. 5. It was named Homo floresiensis. erectus skull (De Vos and Sondaar 1994). the oldest date for any Homo erectus.1.9-1. now called Homo erectus) at Trinil by Dubois in 1891. and it overlaps in time with ‘Solo Man’ and with modern man. erectus and H. including hominids. Older mammal fossils are extremely rare in Indonesia.81 Ma for a Homo erectus skull from Mojokerto.6 Ma and a migration into SE Asia/ Java around 0. adults are only one meter tall.8 Ma. discovered relatively recently. mainly a reflection of the rarity of pre-Pleistocene terrestrial deposits in the archipelago.51. etc. Latest age dating of these skulls is in the 40-70 ka range.Pleistocene tectonic uplift processes and volcanism. at around 2.) in the Pleistocene of. hippos. as evidenced by well-dated stone tools. and Lydekkers Line. sapiens. Sulawesi and Flores relatively late in geologic history. Timor. (2006) and others have argued that these Flores hominids should be regarded as a dwarf population of Homo sapiens. and their evolution and dispersal from mainland Asia across the islands of Java and farther East. Younger. Mammals Indonesia has long been an area of great interest for the study of the Late Pliocene.Pleistocene vertebrate faunas. Recent Ar/Ar dating of pumice layers at Sangiran dome yielded an age range of the Homo erectus-bearing interval between 1. the often poorly documented origins of much of the fossil hominid material collected by local farmers and inaccuracies of various radiometric dating methods still leaves much room for debate on timing of arrivals and evolution of hominids in the region. The latter find is another indication that much of Timor Island was attached to Sundaland in Eocene time.Early Pleistocene. their dating is on tuff samples that may not be from the same horizon as the H. Homo erectus probably reached the island of Flores by 0. SW Sulawesi and Sumba. rats. deer. However. ... Leidsche Geologische Mededelingen. 5 ('Feestbundel Prof....... I... No illustrations of fossils) Fontaine...) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie..G........... (eds.... K......... p... (online at: http://library.............Devonian .M. a continuation of limestones in W Cambodia locally rich in fusulinids (Yabeina...........dmr........ etc. ('The paleontology and stratigraphy of Netherlands East Indies'... 17 X...H. 247 X........................ B...... No figures) Hashimoto....G...........G.......... 375 X.. 192 X..... p........... p..... Kobayashi & R...... Cretaceous . Martin).... Triassic (Timor... van der Vlerk. No figures) Escher........repository.F................... Widespread Jurassic. K.............. & S....... University of Tokyo Press... 552-566......... Carboniferous (Sumatra)...................... Kuenen (eds..... In: T....3...vangorselslist......Pliocene fossils assemblages from Philippines.. Triassic....Paleozoic In: B...... Rel.... Leidsche Geol.................. Mededelingen 5 (Feestbundel K..........) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie.................... also bivalve Trigonia mindoroensis..... Martin memorial volume).naturalis. Permian (Timor mostly endemic solitary species)... H. p................microfloras and environmental distribution ......Pisces...... Cretaceous with larger foram Orbitolina on Cebu.......... Phyllocera.......... (1931).. Reptilia and Aves....) Onze palaeontologische kennis van Nederlandsch Oost Indie. BIOSTRATIGRAPHY.... Carboniferous rare.... 20 X....Cretaceous (very rare.......PALEONTOLOGY X. 361 X................... In: B.......... H... Tertiary (rel............. Quaternary Hominids....................... reptiles and birds known from Indonesia as of 1931..... Toriyama (eds... 68 X................ M-L Triassic coral limestones...1 17 www................ In:B.. Leidsche Geol..) (1931)..pdf) (Listing of 71 fossiliferous localities in E Thailand. Timor.............. Martin')................ p....... Tertiary ..... Martin memorial volume).. Leidsche Geol........... (2) Jurassic with ammonoids Macrocephalites aff.7....... (1931).. Sumatra).... Permian mainly large bodies of limestone.Paleontology of the Philippines...Coelenterata......Carboniferous...... Voluminous book with 20 chapters summarizing ‘state of knowledge’ of paleontology and stratigraphy in Netherlands East Indies... 1-648....nl/document/549718) (Summary of fossil fish....... widespread)......... (eds.... 73-82.... 1. General Papers Brouwer. Inoceramus galoi. p........repository...... Perisphinctes taliabuticus.............th/library/Proceedings-Yearbooks/M_1/1997/7623........ Oldest rocks from Mansalay region on S Mindoro(1) Permian limestones with fusulinids and algae in Eocene conglomerate.......Cretaceous continental sediments) Gerth..1.........8...Biostratigraphy of East Thailand........ (also Andal 1968).. W Papua)) De Beaufort..... 283 X..... Martin. Escher et al...... Int............ Lepidolina)............... Mededelingen 5 (K.......... Ed....6.......... Escher et al.... Salyapongse (1997).........4....) Geology and Palaeontology of Southeast Asia. (online at: www...... L... Commerative volume at 80st birthday of Prof..naturalis..................... W....... J. Mededelingen 5 (K.....nl/document/549311) (Coelenterata chapter in 'Our paleontological knowledge of the Netherlands East Indies'.............. (Review of Carboniferous........... Dr....... Conf.... etc.... 217 X......Recent faunas.... Permian........... Jurassic ................................... Misool. Ceram......................X... 5...com March 2014 ..9.......... H......... Oppelia.... Mammals ....... Escher et al. (eds...... 461-470.... (1969).......5............ Overview of coral species and occurrences in Indonesia: Devonian (New Guinea).........................) Bibliography of Indonesia Geology ................ Sumatra only).................. Quaternary.........2... keeuwensis............ Bangkok 1997. Stratigraphy and tectonic evolution of Southeast Asia and the South Pacific...... Umbgrove & P... 6........go........................... (1931)... (online at: www........De palaeontologie en stratigraphie van Nederlandsch Oost-Indie............H.......... Ordovician...F.... Globotruncana marls overlain by Eocene limestones in Samaloc area.... Jurassic..... In: Proc...... 120-151...A...1....... (Brief review of distribution of Paleozoic rocks and fossils in Indonesia (Sumatra. General Papers ..................... 293-329............ With listings of species and fossil localities and stratigraphic tables.. complete Paleozoic section and possible Precambrian metamorphic rocks.......G..... Dr.. 509-551. Programs E and SE Asia (CCOP).1 18 www.Recent foram material) Metcalfe. B. (Extensive review of geology. Triassic.Ordovician cephalopod limestone. and correlations with other regions) Hasibuan. 34th Sess. Geological Agency. p. In: B. & Purnamaningsih (1998). Ingavat & P. Jurassic.Hasibuan. (online at: www. In: J.Permian (numerous localities with fusulinid limestones).F.go. 40-54. Spiller.. Mededelingen 5 (K. (Summary of state of knowledge of fossil brachiopods in Indonesia in 1931) Pitakpaivan. Martin Memorial Volume). Repts. Ed. p. Buru and Misool.com March 2014 . other rich faunas of Jurassic and Permian. Korea 1997. Bangkok. Co-ord. p.Pre-Tertiary biostratigraphy of Indonesia. Escher et al. F. p. Wu & K. 1-210.Annotations to the map of the more important fossil localities in the Netherlands East Indies. In: B.Pre-Tertiary biostratigraphy of Indonesia. constrains ages of Paleotethys Ocean opening (Devonian) and closing (Triassic)) Pannekoek. p. Geoscience resources and environments of Asian Terranes (GREAT 2008). 1. etc. Berita Sedimentologi 29.vangorselslist. Dept.dmr. p.G. vol. Comm.pdf) Bibliography of Indonesia Geology .nl/document/549269) (Map and chronological listing of 330 significant Paleozoic. p. (2008). etc. Rotterdam. Carboniferous. (Radiolarian biostratigraphy in Thailand. 2. (Mainly on Misool Archipelago M Triassic to Cretaceous macrofossil succession) Hasibuan.Cephalopoda. Bangkok. Thailand. biostratigraphy and stratigraphy of Misool Island. but relatively few species from Cretaceous) Lunt.nl/document/549628) (Summary of state of knowledge of ammonites and belemnites in Indonesia in 1931. Liu.Fossils of Thailand. Eastern Indonesia. F..) Proc. Most known species of Triassic age.pdf) (Listings of fossils known from Thailand: Cambrian trilobite-brachiopod shale off W Peninsular Thailand. Bandung. Pariwatvorn (1969). Mededelingen 5 (K. 396-435. paleontology (brachiopods. R..) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. Final Results IGCP Project 321. Escher et al. 1.).) Gondwana dispersion and Asian accretion. Mededelingen 5 (K.naturalis. I. (online at: www.. 123-132. 4th IGCP 516 and 5th APSEG. Pariwatvorn (1969). Thailand. 323-325. rare marine fossils).th/library/DMR_Technical_Reports/1969/4814. ammonoids. F. K. Symp. Leidsche Geol. (2012).id/fosi) (Description of technique of imaging foraminifera by combining series of digital photographs in automated software to produce single optical image with high resolution and superior depth of focus. Silurian Tentaculites and graptolite shale. p.The Paleo-Tethys in Mainland East and Southeast Asia: contributions from radiolarians studies. p. With examples of Indonesian Tertiry. Bangkok.Fossils of Thailand. H. (online at: http://library. Geol. S China. Sula Islands. Int. p. Martin memorial volume).Stacked digital imaging of foraminifera.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie.repository. Rau (ed.G. 5. Tertiary (in isolated intermontane basins only). Balkema.L. (1931). Other significant cephalopd faunas on Roti. F.Brachiopoda.iagi. bivalves. 1-65 + plates (online at: http://library.P. (online at: www. (eds.Cretaceous (rel. Taejon. Sashida (1999). Malaysia.Mesozoic marine macrofossil biostratigraphy of Indonesia. A.th/library/DMR_Technical_Reports/1969/4814. (Review of Paleozoic. In: I.Mesozoic geology and paleontology of Misool Archipelago. 1-67. Highest number of species known is from Timor. Coastal Offshore Geosc. particularly in Misool island) Krijnen.1_2.repository. no known Devonian fossils. In: Proc. (eds.go.Recent fossil localities in Indonesia) Kruizinga.1_1. (2014). R. W. P. Geol.C. Survey Memoir 3. Leidsche Geol. 259-281. Mineral Res. (1931). 2. Survey Memoir 3.dmr. (1931). Metcalfe (ed. P.naturalis. Dept Mineral Res. Techn. Sess. 297-389. Martin memorial volume). K. Ingavat & P. With descriptions and illustrations of Permian fusulinids and corals) Pitakpaivan.or.J. 2. Leidsche Geol. vol. go.) Posthumus. p. p.Die Perm. Ed. 567-609. (1931).com March 2014 . Permian- Triassic material from Ayer Mati area. 3. 2.. etc. includes Permian brachiopods (Spirifer spp.Mesozoikum In: B.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie.1 19 www. Dept Mineral Res. vol. (1931). and Stephanoceras (Coeloceras) and M Jurassic Belemnites gerardi) Skwarko. Ordovician-Silurian graptolites. A. Phillipsia. Pliocene. Spec. Triassic and Jurassic ages) Pitakpaivan. incl. 5.1_3. Mesozoic (11p. Also plant fossils: Permian 'Cathaysian' Pecopteris. Res. Proetus). Yusuf (1982). Mededelingen 5 (K. Dev.(Continuation 1 of fossils known from Thailand: descriptions and illustrations of brachiopods (incl. coral Zaphrentis.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. Also in mud volcano material 'Tethyan' Early Jurassic ammonites Arietites spp..pdf) (Continuation 2 of fossils known from Thailand: descriptions and illustrations of Cambrian trilobites(Pagodia.G. Martin memorial volume). Geol. ('The Permian. Survey Memoir 3. Palaeontographica 39. ammonoids of Permian (Agathiceras).Paleogene Sequoia.und Jura-Formation auf Timor und Rotti im Indischen Archipel. Thailand. ammonites Arcestes and Cyclolobus persulcatus and crinoids. (Listing of Permo-Carboniferous. Geol. Productus spp. From Roti some Permian fossils in mud volcano material.Fossils of Thailand. etc. Martin memorial volume). O. K. Leidsche Geol. 485-508. W Timor. (1892)... Taxodium. 3.th/library/DMR_Technical_Reports/1969/4814. Trias. (Three lists of literature references on invertebrate fossils of Indonesia: Paleozoic (11p). etc. bivalve Atomodesma. Thailandium). with cross-index tables) Wanner.G. Pariwatvorn (1969). (eds. (eds.).Pleistocene fossil plant species known from Indonesia and adjacent areas) Rothpletz. Borneo. 3. 436-460.Plantae. (Comprehensive review of distribution of Mesozoic rocks and fossils in E Indonesia. J. Lythonia (=Leptodus). Sumatra. Late Triassic-E Jurassic Clathropteris. p. Leidsche Geol. J. Descriptions of many new Permian.Echinodermata In: B. R. Mededelingen 5 (K. mainly collected by Wichmann 1888-1889. Centre. Ingavat & P.vangorselslist. Spirigera.) and Cenozoic fossils (10p. 57-106. S.). Carboniferous trilobites (Thaiaspis. & G. p. 1-66. U Cretaceous. Martin memorial volume). Alethopteris. Bandung. 1-41 + plates (online at: http://library. Permian Leptodus tenuis) and molluscs (Daonella sumatrensis. Cretaceous Araucaryoxylon from Khorat series. Escher et al.K. p. Triassic and Jurassic formation on Timor and Roti in the Indies Archipelago'. In: Onze palaeontologische kennis van Nederlandsch Oost Indie.Jurassic macrofossils from Indonesia. (1931). p. Halobia.Pleistocene vertebrates (Stegolophodon). Also white-red thin-bedded limestones with ‘alpine’ U Triassic Monotis salinaria and Halobia spp. Sphenophyllum. Bangkok. Escher et al. Mededelingen 5 (K. Publ. Rhynchonella). (Listings of fossil echinodermata described from Indonesia) Wanner. Cordaites and Taeniopteris spp. SE of Kupang.dmr.) Bibliography of Indonesia Geology .Bibliography of the invertebrate macrofossils of Indonesia (with cross references). Leidsche Geol. p. from top: (1) Globorotalia fimbriata-Bolliella adamsi. (1996). Conv. p. Ed. (3) Globorotalia crassaformis hessi and (4) Globigerinoides cyclostomus)) Adisaputra. Bali') Adisaputra. Geol. 15-21. Lombok and Savu Basins. 465-475. Miliolina.) Adisaputra. Indonesia 3. J. 10-17. (2) Globigerina calida. (1997). one SW of Timor (2313m). (1992).microfloras and environmental distribution Adisaputra.K. (1992)-Mikrofauna perairan Muria. Indonesia.K. Quaternary. ruber and Gr. incl. p. menardii. Four subzones in Quaternary Globorotalia truncatulinoides zone (N22-N23). Adisaputra.com March 2014 . Lombok and Savu Basins dominated by Gr. (1998). Geologi Sumberdaya Mineral 1. Neogloboquadrina dutertrei in S part) Adisaputra. Globigerinoides ruber dominant in North.K. Bull. HvG). A.25-36.10.Indonesian cores collected in 1990. tumida) Adisaputra.Schlumbergerella floresiana accumulation in coastal zone of Bali and Nusatenggara. Coord.K. (Abundant planktonic foraminifera in Makassar Straits bottom samples between 42. (IAGI). collected during Snellius II expedition. p. Inst. (Planktonic foraminiferal assemblages differ between Flores. Bull. W Lombok. M.Planktonic foraminifera in recent bottom sediments of the Flores.1 20 www.Belitung Straits') Adisaputra. Neogloboqudrina dutertrei is indicator of rel. Gs. 5. ('Microfauna in the waters of Muria'. 2-6. 33rd Sess. Baculogypsina. M. Sumberdaya Mineral 2. Shallow marine small benthic forams of Java Sea.Late Quaternary calcareous nannoplankton in the surface sediment of Makasar and Flores basin. Coastal and Offshore Programmes E and SE Asia (CCOP). 57.Mikrofauna dan potensi wisata perairan Benoa.Planktonic foraminifera and oxygen isotope records in two cores from the Banda Sea and Indian Ocean. Comm. Proc. J. etc. 1. Geol. Hastigerina siphonifera and Globigerina bulloides.K. Indon. (1985).Paleontological analyses of the Savu and Lombok basins and Argo abyssal plain. J. Inst. menardii. dutertrei is dominant followed by Gr. 2. M. 11-16. low salinity. M.K. ('White sands' along coasts of E Bali. Geologi Sumberdaya Mineral 6.vangorselslist. Marine Geol. 5. (Study of Quaternary planktonic foraminifera from two ~7-8m long French. beccarii. ('Foraminifera from seafloor sediments of the Bangka.Recent faunas. ('Microfauna and recreational potential of the water of Benoa. 70. p.K. (1988). 1. Proc. Pulleniatina obliquiloculata. M. p. eastern Indonesia. p. 205-221. Asterorotalia trispinosa. 4. Lombok and Savu Basins. J. N Sumbawa and S Flores composed mainly of rounded foraminifera Schlumbergerella floresiana (formerly also called Tinoporus.X.2.Foraminifera sedimen permukaa perairan Selat Bangka-Belitung. M. Netherlands J.K. p. Bali. 7. Shanghai 1996. Pseudorotalia schroeteriana. Indonesia: implementation for tourism. Sea Res. 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Sambipitu Fm shows 5 zones (NN2-NN6. Yogyakarta. (Localities on Jatirogo Quadrangle. Kano & W. Kamei & K. 1. Yogyakarta 2009. Suggesting younger ages than dated previously) Akmaluddin. Low δ18O values (warming of bottom water) of benthic foraminifera at ~18 Ma and ~12 Ma.Miogypsina cushmani and Miogypsina antillea from Jatirogo (East Java). daerah Bayat- Klaten. Ed. Consistently low planktonic δ18O values indicate sea surface temperature in this area was higher than other tropical areas during E-M Miocene.waset. Workshop on Earth Science and Technology. 71. NN9 (Discoaster hamatus) and NN10 (Discoaster calcaris). p. 6th Int. A. 5p.Sambipitu Fms. A. 97-102. Watanabe. In: Proc.Age correlation of Oyo Formation based on nannofossils and foraminifera biostratigraphy at Southern Mountains area. Indon. p. Int. In: Proc. Central Java.A. suggesting Oyo Fm is of Middle -Late Miocene age. K. 35th Ann. NN8 (Catinaster coalitus).com March 2014 .Paleoclimate reconstruction based on oxygen isotope composition of foraminifera in Southern Mountains area. Bull. Engin.org/journals/waset/v71/v71-11.Paleoceanography of Central Java and closing of Indonesian Seaway reconstruction based on oxygen isotope composition of foraminifera. E. Calcareous nannofossils Gn Lanang four zones: NN 7 (Zone Discoaster exilis). PIT IAGI 2014-247. demonstrate warm sea surface T during Miocene. Seminar on Geology of the Southern Mountains of Java.T. Res. Results suggest gap between Sambipitu and Oyo Fms. M. Rahardjo (2006). Rahardjo (2000). 103-108 Akmaluddin. 2 Ma. Conv.my/gsmpublic/NGC2013/…) Bibliography of Indonesia Geology . middle and upper Semilir Fm at Buyutan section yielded ages of 23.J. 2012-SS-09. (Fission track dating of 3 samples from lower. Muller (1975). Sed. Central Java.php?li=article_detail&id=645) ('Foraminifera distribution patterns within sequence stratigraphy. (Strontium isotopes used to calibrate ages of Oligocene.3 Ma of Oyo Fm tuff layers in agreement with biostratigraphic ages (tuff layers 10m above FO Discoaster hamatus (10.ac. good agreement with nannofossil biozones. p. 40Ar/39Ar dating & fission track dating in Southern Mountains. Proc. Proc.Oligocene-Early Miocene foraminifera. Assoc. inconsistent with nannofossils. Only one spore type. Bandung 30. Inst. Ledok and Ngliron River sections. 27th Ann. Floristic composition of mixed swamp forest stage in both bogs closely comparable.Strontium isotope stratigraphy and the Oligocene-Miocene T-Letter 'Stages' in Papua New Guinea. D. Conv. 4th PNG Petroleum Conv.) Papua New Guinea’s petroleum industry in the 21st century. (Palynology study of Holocene raised peat bog near Marudi (Sarawak) and Miocene coal near Berakas (Brunei) and compared with present-day swamp vegetation along NW Borneo coast. 155-168. Yogyakarta. p. Sambipitu Fm 5 zones (NN2-NN6. K. Bachtiar (1998). Foraminifera biostratigraphy of Sambipitu Fm 4 zones (N6- N8a). Geol.com March 2014 . Soc.Miocene calcareous nannofossils and foraminifera biostratigraphy. 3. Malaysia.. Watanabe & W.1 72 www. Tekn. Te/Tf1 boundary older (20.R. hamatus (9. Proc. Masters Thesis Inst. 66-68. Sabah: preliminary interpretation. p.2 Ma) younger than generally accepted age of 15. Nummulites possibly ranges in Late Oligocene) Anderson. (Calcareous nannofossil analysis on Miocene Sambipitu and Oyo Fms at Kali Ngalang section. paleobathymetry and sequences identification at Braholo. 76 pollen and spore types recognized.vangorselslist.A. near FO Globoquadrina dehiscens. p. but M Miocene (Oyo Fm) suggest hiatus of N10-N12. Geol..8±1..5 Ma. 41st Ann.3 Ma) than generally accepted age of 18. Ngrayong Sst Fm generally age N9-N10 ) Armein.. near Top Globigerina binaiensis) Akmaluddin.Miocene Optimum. Yogyakarta. T. Tawau.itb. Ed. (Extended Abstract only) (online at: http://geology. Rev.A. Assoc. J. Tekn.L. J. 19.Palynological study of a Holocene peat deposit and a Miocene coal deposit from NW Borneo. D. (IAGI). Palynol. Geol.7 Ma) and FO Globigerina nepenthes (11. Oyo Fm 3 zones (NN8-NN10. In: P. with absence of NN7. Woelandari & A. Khoiril (1998). M-L Miocene). tied to Late Miocene global cooling or due to closing of Indonesian Gateway) Akmaluddin. Paleobot. 291-351. Age of larger foram zonal boundary Tf1/Tf2 (12. 40Ar/39Ar date of 10. Pal. 2012-SS-08. 16-26.43Ma. Indon. Whitford & M. Conv. (Online at: http://journal. (1998).edu. Cooling at ~12 Ma.Pola penyebaran foraminifera dalam hubunganny dengan sikuen stratigrafi. a case study in Blora and surrounding areas'. p.early Late Miocene Darai Limestone.G.W. 19.7 Ma). Strat. 1-16. (IAGI).Miocene larger benthic foraminifera from the Kalumpang Formation. & Basir Jasin (2013). In: Proc.Pola sebaran foraminifera dalam hubungannya dengan stratigrafi sikuen (studi kasus: daerah Blora dan sekitarnyaldaerah lintang rendah. with calibrating the age using 40Ar/39Ar dating in Southern Mountains. & J. J. Guwo. p. 41st Ann. Indon. 20m below LO D. Age. Nat. Trotter. (IAGI).(eds. (On the use of foraminifera in sequence stratigraphy in NE Java) Anwar Maruyani. E-M Miocene).um. Port Moresby 2000. K. Central Java.0±1. Rahardjo (2012). Proc. K.4 Ma)) Allan. Ohira (2012). Buchanan et al. Geoscience Conf.0 Ma. Geol.Identifikasi fosil rombakan di lapisan Miosen cekungan Kutai dan implikasinya geologinya. Indon. Assoc. p. p.Korsch (2000). ('Identification of fossil debris in Miocene beds of the Kutai Basin and its geological implications') Asis. Proc.id/index. Stenochlaena areolaris became extinct in Borneo) Anwar Maruyani. Ipoh 2013. Warming of sea surface T related to development of W Pacific Warm Pool and flow of warn water through Indonesian seaway. 5.5 Ma and 19. Bandung. Watanabe & H. Results indicate gap between Sambipitu and Oyo Fms. Overlain by E Miocene (incl.E Oligocene/Tc limestone in Chimbu River gorge (Kubor Anticline?). Malaysia. Japan.dwc. Bur. & S. D. p. (1938). Ph. Flosculinella bontangensis. However. p.. 3. Papers. New Guinea. Nederl. Lepidocyclina (Nephrolepidina) spp.tulips. Chand (conv. Kon.) from Timor. of Tsukuba.The geology and planktic foraminiferal stratigraphy of the Northwest Borneo basin.ga. Int. mainly reflecting Early Cretaceous. sometimes separated by mudstones) Bakx. Mijnbouwk. 1-12.. 41. Akademie Wetenschappen.knaw. (1937). 1. H. (Lyell's survivorship percentages of Cenozoic mollusk assemblages s re-calculated for the Indonesian area) Bain.vangorselslist. with 14 species of larger foraminifera.The Lyellian coefficients checked for Tethyan and Indonesian Cenozoic benthic molluscs. Techn. SE Sabah. and probably also Pellatispira (fig.com March 2014 . L. Akademie Wetenschappen. Miogypsina. Symposium on Shallow Tethys 4. Lepidocyclina (Eulepidina).A. p.Tertiary rocks from the Misool Archipelago (Dutch East Indies). Conf.au/corporate_data/106/Bull_139. Sartori (1996). Gen. Mainly Eocene alveolinids (then called Fasciolites spp. not Miocene) Baggio. Geol. 333-356. Banda. Univ. Proc. Cycloclypeus (Katacycloclypeus) annulatus. 145p.pdf) (Larger forams from limestones from Weber collection from small islands S of Misool identified as Eocene (Alveolina on Jef Lili) and Miocene (Spiroclypeus.Eocene period of S- directed subduction. 9. 10 from Sabenibnoe island W). incl. 926-927) Baggelaar H. Tawau.G. Amsterdam. Ser. HvG) limestones with Miogypsinoides. 301. 205-266. Also critiqued by Musper in Neues Jahrbuch Geol.. & J. 6. Nederl. (1998).pdf) (Lepidocyclina and Spiroclypeus identified from seven islands S of Misool are Discocyclina and Asterocyclina. Sulawesi. (online at: www. Langhian.pdf) (~300m of M Eocene/Ta3. Mainly Cycloclypeus carpenteri) Baggelaar. a comparison with the Mesozoic.De genera Fasciolites en Neoalveolina in het Pacifische gebied. 5. (1994). Followed by study of planktonic foraminifera from overlying Late Oligocene-Pliocene basin) Bibliography of Indonesia Geology .H.M. (online at: http://www.Chronostratigraphic studies of Philippine Cycloclypeus. Verhandelingen Geol. Heterostegina borneensis and Eulepidina.(Miocene larger foraminifera from Spit Lst unit of Kalumpang Fm in Teck Guan Quarry. etc. (1980). Nummulites javanus. E.The foraminifera and stratigraphy of the Chimbu Limestone. R. p. p. (Cycloclypeus larger foram assemblages common in Miocene carbonates of Philippines.O. (online at: http://www. p.knaw. Kol.) Proc 25th Geol.gov. Austr. Proc. Philippines) 34. (most likely age E Middle Miocene. p.. Proc. In: F. All limestones therefore appear to be of Eocene age. Amsterdam.M.tsukuba.ac.1 73 www. all 'Miocene' identifications erroneous and should also be Eocene (Baggelaar 1938). 1937.dwc. Soc. Java. Discocyclina (no Pellatispira/ Biplanispira. etc. 285-292. (online at: http://www. ('The genera Fasciolites and Neoalveolina in the Pacific area'. Geol.D.Planktonic foraminiferal biostratigraphy of Miri-Tinjar road section. Nederl. HvG)) Ayala.J. Thesis.Some correcting notes on 'Tertiary rocks from the Misool-Archipelago (Dutch East Indies)'.jp/limedio/dlam/B14/B1451308/…. Lepidocyclina from 7 islands) genera. 77-116. North Sarawak. Malaysia. Miogypsina. 40.which ceased after Late Eocene Luconia Block collision.C. Eocene with Lacazinella. J. Ed. E Oligocene with Nummulites intermedius. Geological Papers 1970-71. The Philippine Geologist (J.) (Overview of NW Borneo/ West Sarawak geology. Binnekamp (1973). Kon. R. creating accretionary complexes. Fasciolites/ Alveolina. Palaont. as reported by Crespin (1938)).) Banda. 139. (1932). para- conformable on U Cretaceous.nl/DL/publications/PU00017168. Mineral Res. 3.nl/DL/publications/PU00017038. latest Oligocene Te4?. p. Sarawak. Bull. New Guinea. p.On Pseudotaberina malabarica (Carter) (Foraminiferida)..A. dutertrei in glacial times)) Bibliography of Indonesia Geology .J. Palaeoecology 101. Thesis University of Leiden. 1826. With meandrine. is similar to that recognized in other tropical areas of world. 147-167.com March 2014 . Drier climate and lower sea level resulted in expansion of Lower Montane oak forests on Halmahera. 1733-1745.Een monografie van het genus Operculina d'Orbigny. (Monograph on foram genus Operculina. indicating weakened NW winds. W. Micropal. Kuncoro & K. p. subsp. in Iloilo. banyakensis n. (New genus names Tansinhokella for Eocene members of Spiroclypeus group and Vlerkina for involute Heterostegina) Banner. deep basinal conditions until M Pliocene) Banner. 107-117. p. 138-143. Indonesia. including descriptions of Tertiary material from Borneo and Sumatra. Barmawidjaja. Yogyakarta.. (2000). J. early Mid Miocene) and Miri Fm (barren) sandy alternations) Bande. 1-159. Luzon. with reconstruction of Tertiary environments of region. (1950). & U. n. Southeast Asian Applied Geol. In Late Miocene when Central Valley paralic facies.gen. (On Archaias-type soritid species formerly assigned to Orbitolites. Watanabe (2010). (Compilation of information on Paleogene and Neogene floras of SE Asia.T. Rohling. sp.. involute chambers in large microspheric specimens. 14. changing upward into increasingly deeper-water bathyal facies. R.D.M.B...T.L. 1. Malaysia 1. (Neogene limestones of Nias and Tuangku. Palaeogeogr. (Core K12 N of Halmahera spans last 27. M. Glacial time climate drier than today.T.Cenozoic planktonic foraminiferal zonation and basinal development in Philippines. Ed.H. (Miri-Gunong Subis area four lithostratigraphic unit: Suai Fm metamorphosed shale (Ga binaiensis Zone. Late Oligocene-Early Miocene commenced with shelf-type conditions and orbitoidal facies.M. J.The Tertiary flora of Southeast Asia with remarks on its palaeoenvironment and phytogeography of the Indo-Malayan region. B. 47.J. 89-131. (also in J. p. & J. niasensis primitiva. C. AAPG Bull. (UGM) 2. Panay. Rev. Dept. Sibuti mudstone (Gs sicanus Zone. (1963).1 74 www. Rev.The planktic foraminiferal biostratigraphy of the Miri-Gunong Subis area.Geosc. and deeper marine and simpler A. Papers Min. Micropalaeontology 8. Techn.vangorselslist.D. p. and S Iloilo. Palaeobotany Palynology 49. F.sp. Soc. Lambir sandy alternations (Orbulina suturalis-Gr peripheronda Zone. P. May be same species as Archaias vandervlerki De Neve from E Kalimantan.The use of foraminifera fossils for reconstructing the Yogyakarta graben. 23. & M.A revision of the foraminiferal subfamily Heterostegininae.. p. Micropal. SE Asia flora compared with that of India and migration of various families and genera between these two areas is traced) Bandy. Philippines 16. (looks like Eocene Wilfordia)) Bannink.) Banner. Genus comprises nine species) Barianto.Alanlordia. with new acervulinid forma Alanlordia niasensis niasensis n. D. Malaysia. O. 2 (1962)) (Planktonic foraminifera zonation Late Oligocene-Pliocene of Central Valley.000 yrs. Esp. in Late Pliocene (looks like Maastrichtian Vanderbeekia of Middle East). 9 p. Samuel (1995). 113-129. Hodgkinson (1991). Geol. Ng.L.. D. Vergnaud Grazzini & W. J. F. Ph. Highton (1989). early Early Miocene). Also well-developed ‘Deep Chlorophyll Maximum layer’ (elevated Neogloboquadrina pachyderma. van der Kaars. Surface water salinities probably higher. Mid Early Miocene). 2. F. Palaeoclim. p. Serravallian limestones contain ancestral A. a new genus of acervuline foraminifera from the Neogene of Indonesia. 5. n. Zachariasse (1993)- Glacial conditions in the northern Molucca Sea region (Indonesia). p.Banda. 203-233. E. 101-140.A. Sarawak. W of Sumatra. Prakash (1986). In SE Asia characterizes carbonate platform facies of zone Tf1 (late E Miocene). & R. 2. (1943). 6. 349- 355.Revision of a Middle Eocene mollusc assemblage of Nanggulan (Java. M.Oligocene section of Pasir Basin.E.A. C. (1943). 817-829. C. (‘Contributions to the knowledge of the supposedly Oligocene-age mollusk fauna of Buton Island. Leidsche Geol. (1972). 16 also found in other Tethys basins. (1943). Sud de Kalimantan. E Kalimantan’.1935. p. (in Beets 1952 believed to be younger)) Beets.E. Celebes) und den Neogenfaunen des Ostindischen Archipels.com March 2014 . 218-254. 53. p. (‘A Late Miocene mollusk fauna from the Mangkalihat Peninsula. (1942). P. Moscow. 161p. ('Molluscs from the Tertiary of the East Indies Archipelago'.A. 61p. (On a new species of tube-shaped pelecypod of genus Brechites from Miocene of Sarawak) Beets. 160 well-preserved mollusc species from one locality 114 at N side of Mangkalihat Peninsula. (Listings of Middle Eocene mollusc assemblages from Nanggulan.Weitere Verwandtschaftsbeziehungen zwischen den Oberoligocaenen Mollusken von Buton (S. No illustrations of fossils) Bazzacco. Scienze Geol. Revue Inst. p. 1-110. C. (3) Observations on small Neogene mollusk fauna from E Kalimantan (collected by Rutten)) Beets.Les faunes de foraminiferes de l’Eocene superieur a la base du Miocene dans le basin de Pasir. 1. Leidsche Geol. but most similarities with Late Neogene of E Indonesia) Bibliography of Indonesia Geology . ein neuer Fund aus dem Miocan der Landschaft Serawak. Geol. Mer de Chine: Permis de Beibu). p. Mededelingen 13. Mededelingen 13. Brachiopods are generally very rare in Tertiary of Indonesia) Beets. C. 'Oligocene' Buton mollusk faunas mostly endemic in character. Baumann. Mem. ('The foraminifera of the Late Eocene to the base of the Miocene in the Pasir Basin. but possibly Late Oligocene as suggested by Martin. 1931. but endemic faunas (51 new species+ 11 species already described by Martin 1933. 329-333.Stratigraphy and foraminifera of Pliocene-Quarternary deposits of the Timor Trough. 2. (Description of new species of terebratulid brachiopod from asphalt rocks of Buton. Thesis Universite de Bordeaux III.. & V.Mollusken aus dem Tertiar des Ostindischen Archipels. p. Francais Petrole 27. die Leitfossilien-Frage). Leidsche Geol. (1943). Age of fauna uncertain. (2) Notes on some interesting molluscs from E Indies. (1941). S Kalimantan' Planktonic foraminifera faunas and zonation in open marine Eocene.. 341-347. Dutch East Indies. studied earlier by Boettger 1883 and Martin 1914. 256-328. while 35 others have affinities with European Eocene species) Beets.13. vol. Looks like diverse. ('Palynological study of the Tertiary of SE Asia (Kalimantan/Mahakam Delta and S China Sea/ Beibu Permit)) Basov. Mededelingen 13. p. 1-282. C. collected by Leupold)) Beets. C. Indonesia). Mededelingen 13. ('Additional relationships between the Upper Oligocene mollusks from Buton (SE Sulawesi) and the Neogene faunas of the East Indies archipelago'.Eine Jungmiocane Mollusken-Fauna von der Halbinsel Mangkalihat.Barre-De Cruz.On Waisiuthyrina. Leidsche Geol. Mededelingen 13. (1982). Description of mollusks from asphalt beds on Buton in collections in The Netherlands.Brechites venustulus.Beitrage zur Kenntnis der angeblich oberoligocanen Mollusken-Fauna der Insel Buton. Izdatelstvo "Nauchniy Mir".Etude palynologique du Tertiaire de Sud-Est Asiatique (Kalimantan: delta de la Mahakam.- Mijnbouwkundig Genootschap Nederland Kol. C. p.vangorselslist. Ost-Borneo (nebst Bermerkungen uber andere Faunen von Ost-Borneo. 1. p. Ed. W of Yogyakarta.W. 1937). 5. 29-35. Krashenninnikov (1995).1 75 www. Verhandelingen Geol. with discovery of a new species of Solen and proposal of a new name for a Ptychocerithium species. a new articulate brachiopod genus from the Upper Oligocene of Buton (S. Padova. Leidsche Geol. Three short papers on molluscs from collections in The Netherlands: (1) gastropod Buccinum in E Indies. Borneo. Niederlandsch-Ostindien. and vol. (2001). Ser. Netherlands East Indies’. N. Of 74 mollusc species. I. Celebes). p. SE Kalimantan. (1950). Beets. (1944). C. 237-258. of which Recent representatives are poorly known) Bibliography of Indonesia Geology . Beets.lowermost Miocene in age due but here re-interpreted as Mio-Pliocene. partly based on associated diatoms (Reinhold) and foraminifera (Keijzer). p.. Leidse Geol. 2.N. p.) Beets.Beets. Geologie en Mijnbouw.1 76 www.. 1. (1950). (Three species of Neogene fossil crabs from Java and Madura) Beets. (1949). p. Nederl.On Lower Tertiary Mollusca from SW and Central Celebes. Leidsche Geol. C. 200-203. Beets. E. (Incl. Geol. Geol. Geologie en Mijnbouw 5. p. 15. 6p. Geol. Mededelingen 15.Reconsideration of the so-called Oligocene fauna in the asphaltic deposits of Buton (Malay Archipelago). (1952). E. Geol. Leidsche Geol. Beets. Gen.sp. (1950). 5. Nederl. (1950). C. Geol. 15. 40-42. (1950). 9. 265-281.On fossil Mollusca from the island of Mandul. (1943). Mededelingen 15. Borneo. C. ('The species Buccinulum in the Early Miocene of the island Madura') Beets. Kol.Pliocene Mollusca from a coral limestone of a hill near Sekurau. 11. p. p.). Geologie en Mijnbouw.Die gattung Buccinulum im Altmiozän der Insel Madura (O. 241-264. Borneo.Revised determinations of East Indian and related fossil mollusca. Gen. C. Borneo. p. C. C. Mijnbouwk. p. 9. (Mollusks from asphaltic marls of Buton previously considered Oligocene... Mijnbouwk.vangorselslist. Beets. C Java) Beets.Note on fossil Echinoidea and Gastropoda from Sarawak and Kutei. 229-232. 13. p. East Borneo and from dessah Garoeng (Lamongan). Mijnbouwk.n. p. Ser. East-Borneo. Mijnbouwk. Ser. C. p. 15. (On Eocene gastropod species Puruninella permodesta from Upper Eocene of Nanggulan. ('The genus Galeodea (gastropod) in the Tertiary of Indonesia') Beets. (1950). Mededelingen 17. (1947).On fossil brachyuran crabs from the East Indies. Geologie en Mijnbouw. (1950).. Beets. Geologie en Mijnbouw. 2.. Trochocerithium gloriamaris n. Beets.. Ser.S. Mio-Pliocene mollusca. Leidsche Geol. 14-16. Nederl. Verhandelingen Kon. Verhandelingen Geol. Beets. Geol.Uber Puruninella permodesta (Martin) aus dem javanischen Obereozan von Nanggulan. 282-290.N. 2. 291-304. 329-341. C.s.-I.S.Die Gattung Galeodea Link im Tertiar von Insulinde. 435-443. p. (1947). Leidsche Geol..N. 7.S. Gen. Verhandelingen Kon.com March 2014 . Nederl. p. Geol. (1950). Gen. C (1943). C. Verhandelingen Kon.On probably Young Miocene fossils from the coal concession Batoe Panggal near Tenggarong (Samarinda). 342-348. Beets. C. C. C. Mededelingen 15. 92-93. 305-318.On Quaternary mollusca from the Islands of Boenjoe and Tarakan.On probably Pliocene fossils from the Mahakkam Delta region. Java. Mededelingen 15. p. Ed.. C.On the occurrence of Biplanispira in the uppermost Eocene (Kyet-U-Bok Band) of Burma. 349-354. Mededelingen 15. Eastern Borneo. Leidsche Geol.On an East-Indian representative of the rare gastropod genus Trochocerithium. The low % of Recent species is because this is deep water mollusk fauna. Preangerian (Miocene) Mollusca from the Lower Sangkulirang Marl Formation.Late Miocene Mollusca from Tapian Langsat and Gunung Batuta. Associated corals described by Felix 1921 and Gerth 1923) Beets. p.nl/document/148753) (Two small Late Miocene mollusc assemblages from NE Kutai Basin. Kari Orang. (online at: http://www. (online at: www. Scripta Geologica 82. Kalimantan (East Borneo). C. northern Kutai. northern Kutai. northern Kutai (East Borneo). C. Kalimantan Timur (East Borneo). in Late Miocene clays with limestones and sandstones. p.repository. Scripta Geologica 67. Tf3 (Late Miocene) age. suggesting mixed faunas and Miocene age) Beets.Note on Mollusca from the Lower Mentawir Beds. C. C. Scripta Geologica 82. (online at: www. New Guinea.naturalis. Tf3). 1-12.1 77 www. p.naturalis. Tarakan basin. 49-67.com March 2014 . 5.Miocene molluscs from Muara Kobun and Pulu Senumpah. Scripta Geologica 74.Preangerian (Late Miocene) Mollusca from a hill near Sekurau. 1-21. 35 species identified.repository. (1986). Scripta Geologica 67. (Mollusks from two localities around Sangkulirang Bay.Mollusca from Preangerian deposits of Mandul island. Northeastern Kalimantan (East Borneo). 49-80. Sungai Bangalun area. 23-47. Buccinidae).Miocene (Preangerian) molluscs from Kari Orang. (online at: http://www. E Kalimantan) Beets. Restudy identified 42 species. West Irian. Scripta Geologica 74. C. (1986). p. Some species belong to genera whose living species are restricted to Australian waters) Beets. Borneo). 1-37.Beets. but molluscs suggest probably Late Miocene/Tf3 age) Beets.naturalis. N Kutai. Leiden. and age 'uppermost Old Miocene' or 'Upper Miocene'.naturalis.repository. C. C.str.. Age determination difficult.nl/document/148740) (Compilation of investigations of molluscs collected Rutten from Late Miocene Gelingseh Beds.nl/document/148746) (Description of molluscs collected by BPM in Klasaman Fm of West Birds Head in 1930. (online at: http://www. Scripta Geologica.Notes on Buccinulum (Gastropoda. 83- 100. (1981). a reappraisal. Kalimantan Timur (East Borneo). (Molluscs collected by Rutten in Lower Sangkulirang Marls Preangerian. Scripta Geologica 67.Plio-Pleistocene' on basis of foraminifera by NNGPM. 1-82. Scripta Geologica 59. (1983).vangorselslist. p. (1986).repository.Molluscan fauna of the Lower Gelingseh Beds s. Kalimantan (East Borneo). 101-134. p. collected by Schmidt in 1902 and Rutten 1912 mainly gastropods of Preangerian age) Beets. East Borneo.repository. Bibliography of Indonesia Geology . 59.nl/document/148759) (Molluscs collected by Witkamp in 1908 on N flank Kari Orang anticline 27 species are of Preangerian age (Late Miocene.Neogene Mollusca from the Vogelkop (Bird's Head Peninsula). C. C. Sangkulirang Bay. 13-28. p. Sixty species suggesting Preangerian age (Tf3) and shallow marine conditions) Beets. Ed. Balikpapan Bay area. (online at: http://www. (1984). overlain by Pliocene coral limestones. (1983). not Early Miocene (Tf2) as originally interpreted) Beets. E Kalimantan) Beets.naturalis.. (1983). (Mentawir Beds NE of Balikpapan originally assigned to M Miocene Tf2 (Miogypsina. Lepidocyclina). Scripta Geologica 82. p. Subsequently dated as 'Late Miocene. (1981).repository. Sangulirang area.naturalis.nl/document/148808) (Molluscs collected in 1916 by BPM from Mandul Island. C. p. p. Kalimantan (E.nl/document/148710) (Molluscs fossils collected Schmidt in 1902 from hill near Sekurau. E Kalimantan. First examined by K Martin in 1916: 22 species. (1986). Permit 22. All contain mixed Permian. No locality maps)) Belford.vangorselslist.. (https://www.Belford. Mineral Res..gov. All material M Miocene. Bur. collected by Papuan Apinaipi Petroleum Ltd.. Mineral Res. Oldest rocks with Permian foraminifera and one sample with mollusc Atomodesma exarata. D. 1 well. 47 m NW of Port Moresby and 10 m NE of Cape Suckling.J.J. Radiolarian-rich sediments are probably of Triassic age (probable Halobia).Micropalaeontology of samples from Portuguese Timor.gov.1 78 www. Geoph. Records 1959/157. (online at: www.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10228) (Micropal analysis of 26 samples from Tubu area.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10530) (Tuffaceous limestones collected by J. Geoph. Records 1958/9. Papua.Miocene foraminifera from the Wira Anticline. Portuguese Timor. Bur. (1958).ga. p. Mineral Res. 1-6.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10402) (All rel.Micropalaeontology of samples from the Karema-Karova Creek and Malalaus-Saw Mountains areas. Papua. Jurassic-Cretceous and ?Miocene fauna) Belford. Mineral Res.. 1-6.ga.Micropalaeontology of samples from Portuguese Timor. Lepidocyclina (E.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10621) (Summary of analysis of cutting samples from well Ossulari 1 (2840'-3010') and Ossulari 1a (2960'-3100'). 1-4. Bur.ga.ga. Kaufana 1 well with diverse M Miocene and younger bathyal marine calcareous forams above 600' (incl.gov. Geol.com March 2014 . Records 1959/105. Miogypsina)) Belford. Mineral Res. D. Permit 22..). probably all still of Miocene age) Belford.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10733) (Biostrat of 56 outcrop samples collected by Timor Oil Co.Pliocene age) Belford. Rec. p. 1-2. p.. Papua.Pliocene deep marine faunas) Belford. (1960). Lower Miocene (Te with Spiroclypeus and reworked U Cretaceous Globotruncana limestone) and pelagic U Miocene (more likely Plio-Pleistocene. D. HvG).ga. p.Micropalaeontological examination of samples from the Tabu area. Rec. 1-2. (online at: www. Records 1957/029. Papua. Geoph..E. p.gov.ga.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10586) (Miocene. Thompson at Milne Bay (SE tipe of PNG mainland) probably all of Lower Miocene age (Upper Te with Spiroclypeus.. Canberra. Bur. 1-4. Ed. Records 1959/99. Bur. (1957).Micropalaeontology of samples from Ossulari No. 1960/98.ga. Bur.ga. Also several samples rich in radiolaria.J.Pliocene age) Belford. 1960/33. 1-3. p. p. 1961/6. 1 and No. Mineral Res.J. (online at: www. 1-5. (online at: www. Miocene Lepidocyclina at 350').Foraminifera from the Middle Purari River area. D.gov. deep marine sediments of M Miocene. Records 1958/94. Canberra. (online at: https://www. Tertiary samples M-U Eocene (with Nummulites and planktonics and reworked Upper Cretaceous plankton). Geoph. (https://www. Oldest samples are of Permian age (foraminifera). From 640-3348' (TD) poor deep arenaceous water foram faunas only. Mineral Res. p.Lower Miocene foraminifera from the Milne Bay area.ga. (1960).au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10588) (Samples from Wira anticline all Late Miocene. Mineral Res. D. (online at: https://www.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10686) (Biostrat of 76 outcrop samples collected by Timor Oil Co in Timor Leste. (1958). Geoph. D.gov. Bur. Bur.J. 1A bores.J. Bur. (1959).J. D. (online at: www. (1959). D.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10317) (Papuan Apinaipi Petroleum Co. Rec. (1959). Geol..J. Canberra.Micropalaeontology of samples from Kaufana No. Geol. Geol.J. Geol.gov.gov. Mineral Res. Geol.gov. p. Papua. proably Mesozoic. Also an Eocene limestone with Bibliography of Indonesia Geology . Puri-Purari River area. D.Pliocene sediments) Belford. Geoph. 5. 1-6. Papua. (1961). D. Geol. 1 bore. 1-3.ga.Foraminifera from Mutare No. Geol. 5. Mineral Res. G..Miocene and Pliocene smaller foraminifera from Papua and New Guinea. Mainly from Globorotalia pseudomenardii Subzone. (1967). Bur.1 79 www.au/ ) (43 outcrop samples.J..2000'). trinidadensis Zone) Belford.net/168/Bull_092. Austral. 1 bore. Bur. D. oldest beds may be Globigerina daubjergensis. Interval 370-760' regarded as 'block clay' of Upper Miocene age (but faunal lists include Pleistocene Gr.J.. Canberra.pdf) (Comprehensive taxonomy/ descriptions of 156 Mio-Pliocene marine benthic foram species. 92.Foraminifera from the Port Moresby area. Geoph. 1-33.J. Bull. Geoph. (1965). one sample with reworked Permian). ranging in age from M Miocene.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=10758) (Summary of biostratigraphy of Matai 1 cuttings (370'. (1965).J. (online at: www. Record 1965/102.Additional Miocene and Pliocene planktonic foraminifera from Papua and New Guinea. (1962).net/168/Bull_092. Bull. D. Rec. p. Geol. (online at: www. Ed. Globigerina. Austral. 1-3.cloudfront. Bur. (online at: www. D. Eocene limestone with Discocyclina and Alveolina rel. Bur.G.gov.au/ ) (Seven cores from Oil Search well Wuroi 1. p. Papua-New Guinea.pdf) (Three more species of Mio-Pliocene planktonic foraminifera recorded and figured from PNG: Globorotalia crassaformis. (https://d28rz98at9flks. Bur. Papua.J. Little or no stratigraphic info) Belford. Mineral Res. Geoph. D. Australia 79. and no microfossils observed between 1300-2000') Belford. D. D. Also limestone chips between 880-1000' with Late Eocene Discocylina and Pellatispira.. Eocene Pellatispira reworked in E Miocene (but Lower Te= Late Oligocene. Bull. archaeomenardii and Sphaeroidinellopsis kochi (mainly from Ramu Atitau area)) Bibliography of Indonesia Geology . 1-4. HvG.ga.Alveolina and planktonics-rich U Miocene sediments (more likely Pliocene?. D. common at 760-830'.ga. (1963). truncatulinoides and Hyalinea balthica. Mineral Res. p.J. Australia 62. (Thirty-four species of planktonic foraminifera described from Miocene-Pliocene beds of PNG) Belford. Sample gap between 1040-1300'.cloudfront. Bur.ga.Paleocene planktonic foraminifera from Papua and New Guinea. Globorotalia and Chiloguembelina. HvG) with reworked Upper Cretaceous and Eocene forams.ga. (1966). Record 1965/103. Bur. (online at: https://d28rz98at9flks.gov.pdf) (Paleocene planktonic forams described from PNG areas Wabag in W Highlands and Cape Vogel in SE.com March 2014 . (1967). p. Fourteen species assigned to Subbotina. but not sure if in situ. (online at: www.au/corporate_data/188/Bull_079. ranging in age from U Cretaceous to E Miocene/ Te. Mineral Res. 1961/31.gov. overlain(?) by zoneN8 planktonics from'Iwoer Fm') Belford. HvG)) Belford. 1 well.Mesozoic) Belford. p. 35-48.gov. Mineral Res.J.Micropalaeontology of samples from Matai No.gov. (1965)-Foraminifera from the Wuroi No. Geoph. D. p. p. Bureau Mineral Res.vangorselslist. Star Mountains. Mineral Res. p.ga. Bur. 1-223. Portuguese Timor. Bull..au/ ) (Basal Miocene carbonates on unidentified Mesozoic section) Belford.au/products/servlet/controller?event=GEOCAT_DETAILS&catno=11686) (Very brief report on outcrop samples from Star Mountains.gov. (online at: www. No locality maps) Belford. Mineral Res. Record 1965/233. 1-35. p.Foraminifera from outcrop samples. (1961). Mineral Res.J. 1-3. Papua.J. Geol. (online at: www. Mainly E-M Miocene limestones. Record 1963/170. 1-6.Miocene and Pliocene planktonic foraminifera from Papua New Guinea. 92. (1977). 216.indet.J. D. D. 35-42. p. D. (online at: www. Lacazinella. Ed. Palaeontological Papers 1981. Bur.Quasicyclammina gen. Age probably Letter zone Tf1. p. Geophysics 2. 192 (Crespin Volume). 165.au/corporate_data/80906/Jou1977_v2_n1_p035. Geophys. (online at: www.com March 2014 . Bull. Australian Geol. p. D. 4. Geoph. (1982).J. Geophys. Mineral Res. D. widespread in Early Miocene (Te5-Tf1) of PNG) Belford.1 80 www.gov. Bull. D. 1900) redescribed from Christmas Island type locality. It is referred to subgenus Lepidosemicyclina and is senior synonym of M. p.J. 329-343.au/corporate_data/81128/Jou1982_v7_n4_p321.au/corporate_data/116/Bull_150. droogeri Mohan & Tewari. PNG. Indian Ocean.ga.).pdf (New genus and species of cyclamminid agglutinated foraminifera from Upper Paleocene Lagaip Beds N of Central Range.pdf) (New species name for Linderina sp. (online at: https://d28rz98at9flks.Miocene larger foraminifera and Plio-Pleistocene planktonics and smaller benthics from SE PNG) Belford. Australian Geol. BMR J.Belford. NW of Mt. Geoph. p.ga. (online at: http://www. Bull. PNG.Tertiary foraminifera and age of sediments. PNG) Belford. Geol. nov. 5.gov. 315-320. D. Occurrence of Lacazinella near Telefomin) Belford. (online at: http://www. 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(online at: http://www. Mineral Res. Listings and illustrations of Upper Cretaceous planktonic foraminifera. New Ireland. as recorded from Cape Vogel area.pdf) (Foraminifera from rocks collected by Dow on way to Carstensz peak include Late Eocene (Discocyclina. 1-26. D. Late Oligocene and E-M Miocene larger forams from Carstensz limestone and Late Oligocene N3 planktonics from marly interbeds) Belford. p. Nummulites.ga.Foraminifera and age of samples from southeastern Papua. 321-325. BMR J. 1-21. M. Symp. Dev. Irian Jaya. W Papua) Belford. including Distal turbidite (often deformed 'Trochammina/ Recurvoides'). (1993). Sci. Schweiz. Discocyclina) and Late Oligocene. R. (online at: http://gf. in Naturalis Museum.J. H.Cape Ruge area. In: G. p. 4. Petrol. their canal system. Chaproniere (1993). etc. p. Kutei Basin. Leiden.. based on analysis of 56 wells off NW Borneo) Betzler. Paper 9. Ann. with normally magnetised interval) Belford. (eds. 13 p. Paleont. Challengerella brady. 22-49.M Eocene Lockhartia. Publ. (Leg 133 Queensland Plateau ODP site sites with Eocene (Nummulites. 41-58. SEAPEX Offshore South East Asia Conference Conf. (Overview of Cenozoic biostratigraphic zonations in Indonesia) Billman. Singapore 1976. Lagoon/ Distributary channel margin (mangrove swamps with Trematophragmoides. L.repository. (IPA). at least in part.D. Conv. (online at: www.G.D. 5. offshore East Kalimantan.G. Res.1 81 www.E.) Billman.vangorselslist. Haplophragmoides). 301-310. Proximal turbidite (fine-grained and thin-walled Trochammina. p. 101. Thomas (2000).Witoelar Kartaadipura (1974). Bibliography of Indonesia Geology .Recent dinoflagellate zonation. Ed. Zone N21-N22 age. P.Neogene fossil tonnoidean gastropods of Indonesia.H. 3rd. 5. 65-93. Hart et al. Nias.J.org/Documents/IWAF-5/Bidgood+Simmons+Thomas-IWAF5-1997. D. Asterorotalia gaimardii inermis. Davies et al.com March 2014 . p. D. Cyclammina. Plymouth 1997. (Paleogene.B. 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(Species and zonation of rotalid foraminifera successfully used for biozonation of E Kalimantan deltaic series. 51-66. SE of Misool) Besems. & G. Tidal flat/ tidal channel (coarse-grained Trochammina. Bandung.A. p. Tectonic framework and energy resources of the western margin of the Pacific Basin. Australian Geol.) Proc. Grzybowski Foundation Spec. but two age groups (1) general M Miocene age. 1-186.Stratigraphic correlation in Indonesia. youngest marine sediment recognised in New Britain.H. Scripta Geologica 130. Geol.au/corporate_data/81297/Jou1991_v12_n4_p297. Centre. Discocyclina and Distochoplax biserialis in ‘Daram Sandstone’ of Sabennibnu Island. Malaysia Bull. (1979). Mainly Late Oligocene. A. (1875). Parts of this work are based on Indonesian sections like Bojonegoro 1 well. (online at: www.Gr. (1922).gov. (1974)?.E-M Miocene (Te. Sammlungen Geol. Flosculinella) Binnekamp. Biplanispira. p. Record 1970/012.Foraminifera and age of samples from the Star Mountains. incl. Halkyardia).) Blow.gov. etc. 9-59.H. Bur. p. Geol.ga. Cl. 521-535. Record 1970/14..G. Aure Group deeper water facies of M Miocene age (zone N11-12. 5. taxonomy and biostratigraphy of Globorotalia barisanensis LeRoy. 1-8. Austrotrillina. Bur. p. 1-26. (online at: www. 3.(First Late Miocene. peripheroacuta. Darai Lst in S of area with E Miocene with Miogypsina near top. (Classic text on Eocene. Dictyoconus. Conf. C Sumatra) Boehm. Brill. 3. Brill. 1-32. Oligocene age rocks rel. Bibliography of Indonesia Geology . In: Die Fossilien von Java auf Grund einer Sammlung von Dr. kon. Cycloclypeus. with Gr. First Int. Micropaleontology 12. Territory of Papua New Guinea.au/corporate_data/107/Bull_140. p. Barisan mountain front. particularly the evolution of the Gr. Katacycloclypeus. taxonomy. (1970).Foraminifera and age of outcrop samples collected during the Kubor survey 1968. Nephrolepidina. J. etc. Most samples hard limestones with larger foraminifera. Bur.. 1939 from the Lower Palembang Fm of the Kassikan section. fohsi lineage. Mineral Res.D. J. W.ga. p. Bain et al. In: R. Reichs-Museum Leiden (N. New Guinea. Papua New Guinea.M. Pellatispira. Palaeontological Papers 1970-1971. Cycloclypeus. (1882). from Nanggulan. 45.. p.1 82 www.The Cainozoic Globigerinida. p. kais. Belford (1970). K. W.Die fossilen Mollusken der Eocanformation auf der Insel Borneo.F. Verbeek und von anderen bearbeitet durch Dr..Late Middle Eocene to Recent planktonic foraminiferal biostratigraphy. A study of the morphology.J. 3 vols. Incl. 22.com March 2014 .G.Recent biozonation based on rotaliid benthic foraminifera for use in deltaic sediments where planktonics and larger forams are usually absent) Binnekamp. Nyalindung. rare. Denkschr..G. 2. (Monumental study of Tertiary.Recent planktonic foraminifera zonations. Leiden.Recent planktonic foraminifera (expansion of Blow (1969) book)) Blow. Geol. Geoph. (Taxonomy of planktonic foraminifera around E-M Miocene boundary.D. Austr. 199-422. Upper Eocene Calianassa etc. Naturw. R. (1973). ('On some Tertiary fossils from Madura island. Geneva 1967. Bull. 1970)) Blow.. 26). J. 1-1413. Geoph. Reworking of Eocene larger forams into E Miocene in SE of area (in 'Movi Beds/ Omaura greywacke' which unconformably overlie Eocene- -E Oligocene Chimbu Lst.Gr. p. Late Oligocene Merai Volcanics (Lower Te with Eulepidina. For locality map see Bain et al. 140. & D. & Banner (1966). Die Eocanformation von Borneo und ihre Versteinerungen.html) (Foraminifera from 56 limestone outcrop samples from PNG Central Range. Bull. 3. 286-302. Asterocyclina and Lacazinella wichmanni. praefohsi. Martin. Geol. Math.lower Tf) ages. Palaeontographica Suppl. evolutionary relationships and the stratigraphical distribution of some Globigerinida. 1.H. North of Java') Boehm. J. 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Miocene-Pliocene of Indonesia. In: R. 9. etc. Jaarboek Mijnwezen Nederl. (M Eocene. collected by Buxtorf. 1. ('Ostracodes from NE Borneo'. Verbeek. 481 from Meratus Mts front between Rantau and Barabai) Douville. Pati District. M Eocene. Alcheringa 36. Oost-Indie 37 (1908). No locality maps. H. Reichs-Museums Leiden. & M.) rutteni and Lepidocyclina B form. Lombok.. Description of Spiroclypeus new genus and two species. G.M. p. 25-54.(S Mangkalihat. 6. Ser.J. W.U Miocene ostracodes from 43 localities in NE Kalimantan. Sammlungen Geol. Kol. (1911). D. 5. Geol. Renema & D.Les foraminiferes de l’Ile de Nias. one of Cythere. ('The foraminifera in the Tertiary of the Philippines'. PIT-IAGI-2010-248. Soc. p. (1912). Sci. stratigraphy) Douville. also small Oligocene Nummulites) Douville. Remarks on Cycloclypeus.Les foraminiferes des couches de Rembang.Sur quelques foraminiferes des Moluques orientales et de la Nouvelle Guinee.. (’The foraminifera from the Rembang Beds’. 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Palynological succession similar to Sunda Basin. p. (2002) of type specimens of Tertiary bivalves. Early Oligocene with common rain forest elements.W.B. suggesting everwet.esdm. p. suggesting absence of lake deposit. Oil Gas. 1-765. Contr. (online at: http://www. J. mainly from Martin. Nat. With listing of fossil localities and 289 color plates) LeRoy. 31. E. 333-345. Records of Dacrydium in Eocene of Ninety East Ridge and the Indian subcontinent may support alternative dispersal route into SE Asia via Indian plate) Lelono. Previously thought to haves migrated to Sunda region after collision of Australian and Asian plates.lemigas. Museum Techn.E. (online at: http://www. Geol. Early part of Late Oligocene much reduced rain forest elements with grass pollen.Some small foraminifera. & F.1 126 www. Gerth and Umbgrove collections) Leloux. (online at: http://www.. In: R. E. 5.Indie 99.com March 2014 . Lemigas.pdf) (Listings and illustrations of type material of 229 taxa of Tertiary and Permian corals in Leiden Natural History Museum.lemigas. Scient.The migration pathway of some selected Australian palynomorphs from their origin to SE Asia.esdm. Generally poor pollen assemblages.B. (online at: http://www. Unlike equivalent beds offshore NW Java. Renema (2007). (Descriptions of 95 species of Miocene small benthic foraminifera and six species of ostracoda from Telisa and Palembang formations along E front of Barisan mountains) Bibliography of Indonesia Geology . M. (2008).J.B. Contr. & W. E. Martin collection at Naturalis Museum. p. (2012). 10.B.Oligocene palynological succession from the East Java Sea.J. Oil Gas.A. Leiden.Oligocene palynology of onshore West Java. rainforest climate. 2. 34. In latest Late Oligocene rainforest elements return in abundance. lacustrine elements rare. Depositional environment transition non-marine. 2.id/ ) (Palynological studies of Oligocene in (unnamed) onshore wells in Ciputat sub-basin. Cottam & M. ostracoda and otoliths from the Neogene ("Miocene") of the Rokan-Tapanoeli area. 67- 82.Types and originals of fossil Porifera and Cnidaria of Indonesia in Naturalis.go. Lelono. Natuurhist. 49-56. 11. p.. 7-18. Common brackish pollen of Zonocostites ramonae and Spinizonocolpites echinatus indicate mangrove/ back-mangrove environment) Lelono. Museum Technical Bulletin. S Sulawesi and Natuna. p.P.B.Oligocene palynological succession from the East Java Sea. after collision of Australian plate and Sundaland in latest Oligocene. J.esdm. 1-305. Wilson (eds. 215-296. Lemigas. p. 2. expanded and illustrated version of Van den Hoek Ostende et al. LEMIGAS Scient.id/ ) (Proposes alternative dispersal route of Australian taxa Dacrydium and Casuarina to SE Asia. suggesting superwet climate. indicating more seasonal climate. Papua. Leiden. Soc. (online at: http://www. Ed. Wesselingh (2009). & R. 2. Oligocene defined by presence of Oligocene marker Meyeripollis naharkotensis.vangorselslist.go. p. Lemigas Scient. This may indicate earlier arrival of Gondwanan/ Australian fragment in East Java area than in other areas of Indonesia) Lelono.nl/sites/naturalis. 355.of other areas such as NW Java Sea.en/contents/i000884/the%20gerth%20catalogue. W Java Sea) Lelono. 35.J. 35. gastropods and scaphopods from Java in K. W Java. 95-104. Hall. Bull. Publ. Natuurhist. L. Netherlands East Indies. Netherlands East Indies. East Borneo. 576-584. (Fourteen new species of ostracode Cytherelloidea from Indonesia. W Java and 7 species from Miocene of C Sumatra) LeRoy. 3. With discussion of stratigraphy and faunas of Kassikan section near Aliantan. L. 612-621. p. Colorado School Mines 39.com March 2014 . Natuurkundig Tijdschrift Nederl.Smaller foraminifera from the Late Tertiary of Southern Okinawa. Paleontology 22. L. (1948). 70-113. 2. a suggested middle Tertiary time indicator. 1-69. Bantam Residency. W Java) LeRoy. L. 107-132. (online at: http://pubs. Netherlands East Indies. incl.W. E of Pelabuhan Ratu. p.W.The foraminifer Orbulina universa d'Orbigny.Miocene foraminifera from Sumatra and Java. Quart. (Includes discussion and illustrations of growth stages of Cythereis holmani from Telisa Fm of C Sumatra) LeRoy. (Descriptions of 107 species of small benthic foraminifera from Miocene marls at Tjijarian bridge.The ostracode genus Cytherelloidea from the Tertiary of the Netherlands East Indies. p. 1. (1941). LeRoy. J.Small foraminifera from the Late Tertiary of the Netherlands East Indies. Survey (USGS) Prof. Colorado School Mines 36. (Descriptions of 183 species of Miocene small benthic foraminifera from Telisa and L-M Palembang formations along E front of Barisan mountains. L. Small foraminifera from the Miocene of West Java.W.W. 1. p. 1. L. Small foraminifera from the Late Tertiary of Siberoet Island. p. 81-86.pdf) (Good descriptions of typical Indo-Pacific shallow and shelfal marine smaller benthic foraminifera)) Bibliography of Indonesia Geology . 4. (1945).1 127 www. Colorado School Mines 39.usgs.W. (1944).W. Quart. (1941).. p. 5. Paper 454-F.W. (1952). J. 1-62. 4. (Lowest stratigraphic occurrence of pelagic foraminifer Orbulina universa proposed to bea good mid-Miocene markerhorizon. (1941). 2. Quart.Small foraminifera from the Late Tertiary of the Netherlands East Indies.gov/pp/0454f/report. 63-105. U.The ostracode genus Cytherelloidea from the Late Tertiary of the Netherlands East Indies. (1964). p. J. (Lowest occurrence of planktonic foram Orbulina within Telisa Fm of C Sumatra good base of Middle Miocene marker horizon. Bodjong beds. Barisan mountain front) LeRoy. 6. L. Paleontology 19. (Same paper as above: 14 new species of ostracode Cytherelloidea from Indonesia.Miocene foraminifera from Sumatra and Java.A contribution to ostracodal ontogeny. Miocene foraminifera of Central Sumatra. Small foraminifera from the Late Tertiary of the Sangkulirang Bay area.M Palembang formations in Kasikan section. Quart. off the West coast of Sumatra. incl. Geol. 1. Little or no stratigraphic or locations information) LeRoy. where this event occurs near top of Telisa Fm) LeRoy. (1940). p. W Java and 7 species from Miocene of C Sumatra) LeRoy. p. 179-196. J. 3. 1.vangorselslist. Colorado School Mines 36. L. 3 from Late Miocene of NE Kalimantan. Netherlands East Indies. Paleontology 26. 500-508. L.W. p. West Java. Quart. Colorado School Mines 36.Indie 100.Orbulina universa d’Orbigny in Central Sumatra. C Sumatra.LeRoy.W. LeRoy. LeRoy. Sultanate of Siak. With chart of foraminifera distribution in Telisa.Small foraminifera from the Late Tertiary of the Netherlands East Indies. L. p.W. Ed. 4 from Mio-Pliocene from Bantam.S.W. (1941). 4 from Mio-Pliocene from Bantam. L. 3 from Late Miocene of NE Kalimantan. 3. Some small foraminifera from the type locality of the Bantamien substage. (1944). Paleontology 15. 1-58. their taxonomy and stratigraphic significance. Geol. Southeast Asian Earth Sci.. Overlies ?Late Jurassic-Early Cretaceous ophiolite complex and thin volcaniclastic Kapadiri Fm with Early Cretaceous calpionnelids) Ling. Geophys.in/vol38/v1.B. p.Y. Martin memorial volume. (Similar to M Eocene radiolarians on ophiolite of S Andaman (Ling and Srinivasan 1993)) Ling. Bur. H. (eds.) Proc. Lituolacea and Miliolacea. Part 2.R. p.G. Miner.J. No location/ stratigraphy info) Ling.Neogene foraminifera from H. (1943). 1991)) Lloyd. Wreck Island No. Palaeont. Karkare (2006). Samuel (1998). Res. R. H. p. p. (eds. Nichols (1991). 16. Ed. & R. India 38.R.A.Siliceous microfossils from Nias Island: their significance for the Tertiary paleoceanography of the northeast Indian Ocean. (Basal sedimentary unit on Waigeo is Tanjung Bomas Fm and contains late M Eocene radiolarian assemblage. J. Chandra & S. Palaeontological papers.1 128 www. Lloyd. 13. p. 92.R. A. L. 53-57. Ser. & I. Southeast Asian Earth Sci. 166-179. Nodosariacea and Buliminacea.) Stratigraphie van Nederlandsch Oost-Indie. G. Geophys. In: A.Less. Miner. & E.Neogene foraminifera from HBR Wreck Island No. With distribution chart of larger foraminifera and 'Letter Classification' zonation) Lignac-Grutterink. Leidsche Geol.ga. Jones & R. In: B. 11. 407-417. (Well-preserved Early Eocene radiolarian assemblages confirms presence of Eocene marine sediments on Waigeo Island. 1967. Verhandelingen Geol. Geol. Leupold. J. p.The Late Eocene evolution of nummulitid foraminifer Spiroclypeus in the Western Tethys. 145-225. (1967). Java. Bibliography of Indonesia Geology . 303-316. Endean (eds. 299-305. Hall (1995). (Brief descriptions of Tertiary calcareous algae from Borneo. (online at: http://www. p. 1 bore and Heron Island bore. Feestbundel Martin.Note on an age of the basal sedimentary sequence of Waigeo Island.. Ozcan (2008).. J.H. & M. p. 2.E Eocene sedimentological hiatus) Ling. 4.au/…) (Mainly Miocene open marine shelf foraminifera from below Great Barrier Reef.. In: O.S. their taxonomy and stratigraphic significance. Mijnb. H. 5. 108. p.. A. (M Eocene radiolarians in red chert from SW Nias constrains oldest age of emplacement of ophiolitic basement. W.Y.G. overlying Late Cretaceous or Early Eocene ultramafic 'basement' on S Andaman. J. Northeast Indian Ocean.Y.The Tertiary. Bur.Foraminifera of the Great Barrier Reef bores. in Leiden collection. etc. Similar to M Eocene radiolarians of Nias (Ling et al.Some Tertiary Corallinaceae of the Malaysian Archipelago.) Biology and geology of coral reefs. Srinivasan (1993).gov. A.pdf) (M Eocene radiolaria in chert in Port Blair Fm. Mededelingen 5. p. 1 bore and Heron Island bore.M. Bull. 69 species nodosarids and buliminids) Lloyd.Significance of Eocene radiolaria from Port Blair Group of South Andaman Island. (Overview of Tertiary stratigraphy across ‘Netherlands East Indies’ in K. van der Vlerk (1931). Academic Press.Tectonic significance of Eocene and Cretaceous radiolaria from South Andaman Island. Escher et al. Queensland.Early Eocene radiolaria from Waigeo Island. INTERRAD VII Conf. 1-5. (M Eocene) and Campanian radiolarian faunas from basement rocks of SE South Andaman Island affirm Paleocene.Y. Eastern Indonesia.R.com March 2014 . Polonica 53. Yao et al. & M. 1. New York. eastern Indonesia.vangorselslist. India. H. Res. R. p. Hall & G.Y. 611-648. 347-366. Soc. Geol. Asian Earth Sci. NW of Birds Head) Ling. Gen. Acta Palaeont.A. 283-297. (1973). Bull. Island arc 5. Queensland. Part 1. (1970). (online at: http://palaeontologicalsociety. 6. H. Lloyd, A.R. (1974)- Time measurement of geological time and precision in correlation. Proc. SEAPEX Conv. 1, Singapore, p. 31-43. (On stratigraphic correlations, with examples from SE Asia) Lloyd, A.R. (1975)- Paleontology and its role on oil exploration. Proc. SEAPEX Conv. 2, Singapore, p. 152- 159. Lloyd, A.R. (1975)- An outline of the Tertiary palaeontology and stratigraphy of the Gulf of Papua, Papua New Guinea. In: Wiryosujono & A. Sudrajat (eds.) Proc. Reg. Conf. Geology and Mineral Resources of Southeast Asia (GEOSEA), Jakarta 1975, p. 43-54. Ludbrook, N.H. (1965)- Tertiary fossils from Christmas Island (Indian Ocean). J. Geol. Soc. Australia, 12, p. 285-294. (Algal imestones of Christmas Island in Indian Ocean of Late Eocene (Tb) and Early Miocene (Te-Tf) age. Upper Eocene limestone with Discocyclina, Nummulites, Heterostegina. Lower Miocene limestone lower part with Lepidocyclina (Eulepidina), followed by Miogypsinoides dehaarti, then Flosculinella bontangensis. No rocks younger than Burdigalian identified other than young fringing reef) Lunt, P. (2003)- Biogeography of some Eocene larger foraminifera, and their application in distinguishing geological plates. Palaeontologia Electronica 6, 1, p. 1-22. (Online at http://palaeo-electronica.org/2003_2/geo/geo.pdf) (Eocene larger foram assemblages can distinguish between Asian-Pacific-Mediterranean (Pellatispira- Assilina) or Australian- New Guinea (Lacazinella) realms) Lunt, P. (2013)- The sedimentary geology of Java. Indon. Petrol. Assoc. (IPA), Jakarta, Spec. Publ., p. 1-340. (Comprehensive book on Java sedimentary geology with introductory chapters on biostratigraphy/ micropaleontology) Lunt, P. (2013)- Foraminiferal micropalaeontology in SE Asia In: A.J. Bowden et al. (eds.) Landmarks in foraminiferal micropalaeontology: history and development, The Micropalaeontological Society, Spec. Publ. 6, Geol. Soc. London, p. 193-206. (History of foraminiferal micropaleontology in SE Asia (mainly Indonesia) since late 1800's) Lunt, P. (2014)- A review of the foraminiferal biostratigraphy of the Melinau Limestone, Sarawak. Berita Sedimentologi 29, p. 41-50. (online at: www.iagi.or.id/fosi) (Study of Melinau limestone, Sarawak show age range from M Eocene (Letter Stage Ta) to E Miocene (Te5, about 20.3 Ma). Strontium dating and biostratigraphy shows significant change in sedimentary rates or preserved thickness during mid-Oligocene (latest Tc or intra-Td times). Termination of Melinau limestone with initial event near the Oligo-Miocene boundary (Te4-Te5 boundary) and youngest limestones dated as Te5) Lunt, P. & T. Allan (2004)- A history and application of larger foraminifera in Indonesian biostratigraphy, calibrated to isotopic dating. Geol. Res. Dev. Centre Museum, Bandung, 2004 Workshop on Micropaleontology, 109p. (Modern overview of Indonesian Tertiary larger foraminifera and zonations) Lunt, P. & W. Renema (2014)- On the Heterostegina- Tansinhokella- Spiroclypeus lineage(s) in SE Asia. Berita Sedimentologi 30, p. 6-31. (online at: www.iagi.or.id/fosi) (Detailed discussion of larger foraminifera evolutionary series from Heterostegina (Vlerkina) through Tansinhokella to Spiroclypeus, which can be observed twice in fossil record: (1) in Late Eocene and in mid- Oligocene- E Miocene. Morphologically no reliable way to distinguish Late Eocene and later Oligocene tests. Bibliography of Indonesia Geology , Ed. 5.1 129 www.vangorselslist.com March 2014 Second evolutionary development of Tansinhokella and Spiroclypeus was at same time in three geographically separate areas. Tansinhokella important for biostratigraphic subdivision of Letter Stage Te) MacGillavry, H.J. (1962)- Lineages in the genus Cycloclypeus Carpenter. Proc. Kon. Nederl. Akademie Wetenschappen B65, 5, p. 429-458. (Eight Eocene- Recent Cycloclypeus lineages distinguished) MacGillavry, H.J. (1978)- Foraminifera and parallel evolution- how or why? Geologie en Mijnbouw 57, 3, p. 385-394. (On evolutionary trends in larger foraminifera, by former Stanvac micropaleontologist. With appendix B and C summarizing larger foraminifera and stratigraphy in S Sumatra Basin) Madon, M.B., R.B.A. Karim & R.W.H. Fatt (1999)- Tertiary stratigraphy and correlation schemes. In: Petronas (ed.) The Petroleum Geology and Resources of Malaysia. Petronas, Kuala Lumpur, p. 113-137. (Review of biozonations and stratigraphic nomenclature of Malay Basin, Penyu Basin, NW Borneo, Sabah), Maha, M. & S. Sanyoto (2000)- Biodatum dan zonasi foraminifera bentik kecil serta hubungannya dengan foraminifera planktonik Sumur-95 daerah Cepu, Kab. Blora, Jawa Tengah. Proc. 29th Ann. Conv. Indon. Assoc. Geol. (IAGI), 4, p. 247-258. ('Datum levels and zonation of smaller benthic forams and their relations with planktonic foraminifera in well 95, Cepu area, C, Java'. Shallow well W of Cepu, TD 340m, penetrating Late Pliocene- Pleistocene Mundu, Selorejo and Lidah Fms. Calcarina calcar restricted to Pleistocene, planktonic foram zones N22-N23, Pseudorotalia indopacifica basal occurrence near base zone N20) Mandang, Y.I. & N. Kagemori (2004)- A fossil wood of Dipterocarpaceae from Pliocene deposit in the West Region of Java Island, Indonesia. Biodiversita 5, 1, p. 28-35. (Online at http://www.unsjournals.com/D/D0501/D0501pdf/D050106.pdf) (Giant silicified dipterocarp tree trunk 28 m long from Lower Pliocene near Leuwidalang, Banten, W Java, described as Dryobalanoxylon lunaris) Mandang, Y.I. & D. Martono (1996)- Keanekaragaman fosil kayu di bagian barat pulau Jawa. Bul. Penelitian Hasil Hutan 14, 5, p. 192-203. ('Fossil wood diversity in the western part of Java Island'. Of 199 wood fossils, 81% belong to family Dipterocarpaceae (Dryobalanops,Alstonia, Calophyllum, Dillenia, etc.)) Mao, L. & S.Y. Foong (2013)- Tracing ancestral biogeography of Sonneratia based on fossil pollen and their probable modern analogues. Palaeoworld 22, p. 133-143. (Review of biogeography of tropical mangrove pollen Florschuetzia, which is ancestral to modern Sonneratia. Florschuetzia documented from Late Eocene- M Miocene in palaeotropics around Tethyan region. Migrated from center of origin in SE Asia probably during E Eocene, and radiated and expanded China, Japan, Australia and E Africa. Until warm early M Miocene (Langhian) Sonneratia had largest geographical range) Marks, P. (1954)- Contributions to the geology of Timor. III. An occurrence of Miogypsina (Miogypsinella) complanata Schlumberger in the Lalan Asu area, Timor. Indonesian J. Natural Science 110, p. 78-80. (Lalan Asu area polymict basal conglomerate above amphibolite, originally described by Tappenbeck 1939, contains latest Oligocene larger forams Miogypsinoides complanata (with >21 spiral chambers) and Spiroclypeus. Probably equivalent of Base Cablac Limestone in E Timor (Called Aquitanian by Marks, but age should be Late Chattian, Latest Oligocene; HvG) Marks, P. (1956)- Smaller foraminifera from well No. 1 (sumur 1) at Kebajoran, Djakarta. Djawatan Geologi, Publ. Keilmuan 30, Ser. Paleont., Bandung, p. 25-47. (Study of foraminifera in water well drilled to 255m in 1950 at S side of Jakarta. Mainly barren, non-marine section with 3-4 thin intervals with shallow marine microfauna (Asterorotalia, Pseudorotalia, Elphidium, etc.). Uppermost samples rich in reworked planktonic forams. Age of section latest Pliocene- Pleistocene) Bibliography of Indonesia Geology , Ed. 5.1 130 www.vangorselslist.com March 2014 Marpaung, L.P., K.A. Maryunani, I.N. Suta & C. Irawan (2007)- Quantitative biostratigraphy of Jabung Block, South Sumatra Basin: a probablilistic approach for biozonation and correlation. Proc. 31st Ann. Conv. Indon. Petrol. Assoc. 1, p. 317-331. (Probabilistic analysis of Oligocene- lower Middle Miocene in ten S Sumatra wells enabled higher precision of correlation and biozonation. Palynology, foram and nannofossil micropaleontology gave 52 biostrat events, 11 of which proved reliable. An eight-biozone scheme is proposed) Martin, K. (1879-1880)- Die Tertiarschichten auf Java, nach den Entdeckungen von Fr. Junghuhn, Palaeontologischer Teil. E.J. Brill, Leiden, p. 3-164. (‘The Tertiary beds of Java, after the discoveries of Fr. Junghuhn; paleontological part’. One of earliest descriptions of Tertiary macrofossils from Java, with many new species, incl. Cycloclypeus annulatus from Citarum valley, W Java. Chapter on corals p. 132-146, mainly from Miocene of Nyalindung area, W Java) Martin, K. (1880)- Untersuchungen uber die Organisation von Cycloclypeus Carp. und Orbitoides D'Orb. Niederl. Arch. Zoologie 5, 2, p. 185-206. ('Investigations on the organization of Cycloclypeus and Orbitoides'. Early descriptions of Java larger foraminifera Cycloclypeus (C. annulatus, C. communis, C. neglectus) and Lepidocyclina (here still called Orbitoides; including new species radiata, carteri, gigantea)) Martin, K. (1881)- Eine Tertiaerformation von Neu-Guinea und benachbarten Inseln nach Sammlungen von Macklot und v. Rosenberg’s. Sammlungen Geol. Reichsmuseum Leiden, ser. 1, 1, p. 65-83. (also in Jaarboek Mijnwezen 11 (1882), Wetensch. Ged., p. 137-156) (‘A Tertiary formation from New Guinea and adjacent islands, from collections of Macklot and Von Rosenberg’. Descriptions of Tertiary fossils from W Papua (incl. Eocene Alveolina limestone), Kur, Kai Besar and Aru islands (post-Tertiary mollusk breccia)) Martin, K. (1881)- Jungtertiare Ablagerungen im Padangschen Hochlande auf Sumatra, nach der Sammlung Horner’s. Sammlungen Geol. Reichsmus. Leiden, E.J. Brill, Ser. 1, 1 (2), p. 84-101. (‘Young Tertairy deposits in the Padang Highlands on Sumatra, from the collection of Horner’. Probably Miocene-age 19 mollusc species, mainly bivalves, from Tanjung Ampalo, Padang Highlands, W Sumatra) Martin, K. (1881)- Tertiaerversteinerungen vom ostlichen Java, nach Sammlungen Junghuhn's und der Indischen Bergbeambten. Samml. Geol. Reichsmus. Leiden, Ser. 1, 1, E.J. Brill, p. 105-130. ('Tertiary fossils from East Java, from collections of Junghuhn and Indies mining engineers'. Incl. descriptions of Eocene Nummulites djokjakartae n.sp. and Discocyclina (Orbitoides dispansa) from Yogyakarta area, echinoids, bivalves, gastropods, etc.) Martin, K. (1882)- Tertiaerversteinerungen vom ostlichen Java, nach Sammlungen Junghuhn's und der Indischen Bergbeambten. Jaarboek Mijnwezen Nederl. Oost-Indie 1882, Wet. Ged. p. 253-280. ('Tertiary fossils from East Java, etc'. Same as Martin (1881) paper above) Martin, K. (1883)- Nachtrage zu den 'Tertiarschichten auf Java', 1er Nachtrag: Mollusken, nach Sammlungen der Indischen Bergbeambten, Junghuhn's und Reinwardt's. Samml. Geol. Reichsmus. Leiden, Ser. 1, 1, E.J. Brill, p. 194-270. (also in Jaarboek Mijnwezen Ned. Oost-Indie 1883, Wetensch. Ged. p. 285-358) (Continuation of ‘The Tertiary beds of Java', part 1, molluscs. Descriptions of 71 species) Martin, K. (1883)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln. Samml. Geol. Reichsmus. Leiden, Ser. 1, 3, p. 1-380. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Descriptions of Tertiary fossils from outcrops and from water wells on Java (Grissee (=Gresik?) NE Java, Batavia, Ngembak- W of Purwodadi), mainly collected by Van Dijk of Geological Survey) Bibliography of Indonesia Geology , Ed. 5.1 131 www.vangorselslist.com March 2014 Martin, K. (1883)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln- 1. Jaarboek Mijnwezen Nederl. Oost-Indie 12 (1883), Wet. Ged., p. 371-412. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 1 of Martin (1883) paper above) Martin, K. (1884)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln- 2. Jaarboek Mijnwezen Nederl. Oost-Indie 13 (1884), Wet. Ged., p. 77-216. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 2 of Martin (1883) paper above) Martin, K. (1885)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln-3. Jaarboek Mijnwezen Nederl. Oost-Indie (1885), Wet. Ged., p. 5-108. ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 3 of Martin (1883) paper above) Martin, K. (1887)- Palaontologische Ergebnisse von Tiefbohrungen auf Java, nebst allgemeineren Studien uber das Tertiar von Java, Timor und einiger anderer Inseln-4. Jaarboek Mijnwezen Nederl. Oost-Indie (1887), Wet. Ged. 2, p. 253-342). ('Paleontological results of deep wells on Java, and more general studies on the Tertiary of Java, Timor and some other islands'. Part 4 of Martin (1883) paper above) Martin, K. (1891)- Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek. Samml. Geol. Reichsmuseums Leiden, N.F., 1, 1-2, E.J. Brill, Leiden, p. 1-538. (also partly reprinted in Jaarboek Mijnwezen Nederl. Oost-Indie 1896, Wetensch. Ged., p. 43-328) ('The fossils of Java, based on a collection of R.D.M. Verbeek'. Collection of papers by Martin and collaborators, published between 1891-1922. Mainly extensive descriptions of Tertiary molluscs) Martin, K. (1891)- Die Foraminiferen fuhrenden Gesteine, Studien uber Cycloclypeus und Orbitoides. Appendix in Die Fossilien von Java, auf Grund einer Sammlung von R.D.M. Verbeek, Sammlungen Geol. Reichsmuseums Leiden, N.F., 1, p. 1-12. ('The foraminifera-bearing rocks- Studies on Cycloclypeus and Orbitoides'. Early summary paper on W, C and E Java larger foraminifera (mainly species of Cycloclypeus)) Martin, K. (1895)- Neues uber das Tertiar von Java und die mesozoischen Schichten von West-Borneo. Sammlungen Geol. Reichsmuseums Leiden, E.J. Brill, ser. 1, 5, 2, p. 23-51. ('News on the Tertiary of Java and the Mesozoic beds of West Borneo'. Mainly listings of Tertiary gastropods from various localities of Java. No maps, no illustrations) Martin, K. (1898)- Die Fauna der Melawi-Gruppe, einer Tertiaren (Eocanen?) Brackwasser-ablagerung aus dem innern von Borneo. Jaarboek Mijnwezen Nederl. Oost-Indie 1898, Wet. Ged. 2, p. 37-96. (also in Samml. Geol. Reichsmuseums Leiden 1899, ser. 1, 5, p. 257- 316) ('The fauna of the Melawi Group, a Tertiary (Eocene?) brackish-water deposit in Central Borneo'. Descriptions of brackish-fresh water molluscs from Melawi and Kajan Rivers area, collected by Wing Easton. Mainly species of Corbula, Cyrena and Paludomus, less common Arca melaviensis n.sp. Age indeterminate) Martin, K. (1899)- On brackish water-deposits of the Melawi in the interior of Borneo. Proc. Kon. Akademie Wetenschappen, Amsterdam, 1, p. 245-248. (online at www.digitallibrary.nl) (Molluscs collected by Wing Easton and Molengraaff in sediments of Melawi River area, Upper Kapuas, C Kalimantan, mainly fresh (Melania, Paludomus) or brackish water (Cyrena, Corbula), but also some shallow marine species. Age Tertiary, possibly Eocene) Bibliography of Indonesia Geology , Ed. 5.1 132 www.vangorselslist.com March 2014 Martin, K. (1900)- Die Eintheilung der Versteinerungs-fuhrenden Sedimente von Java. Jaarboek Mijnwezen Nederl. Oost-Indie (1900), 108 p. ('The classification of the fossiliferous rocks of Java' Overview of fossils and discussion of probable ages of formations from various parts of Java and Madura. Very 'wordy'; no maps or other illustrations) Martin, K. (1900)- Die Eintheilung der Versteinerungs-fuhrenden Sedimente von Java. Samml. Geol. Reichs- Museum Leiden, Ser. 1, 6, p. 135-244. ('The classification of the fossiliferous rocks of Java'. Same paper as above) Martin, K. (1904)- Jungtertiare Kalksteine von Batjan und Obi. Sammlungen Geol. Reichs-Mus. Leiden, ser. 1, VII, p. 225-230. (Young Tertiary limestones from Bacan and Obi'. Occurrence of probably Early Miocene age limestone with Lepidocyclina and Heterostegina in SW Bacan and N-Central Obi) Martin, K. (1907)- Eine Altmiocane Gastropodenfauna von Rembang, nebst Bemerkungen uber den stratigraphischen Wert der Nummuliden. Samml. Geol. Reichs-Museums in Leiden, Ser. 1, 8, p. 145-152. (‘An Early Miocene gastropod fauna from Rembang, with comments on stratigraphic value of nummulitids’. Listing of 40 gastropod species from Sedan and Gunung Butak, Rembang District, NE Java, only 6 species still known from recent faunas. Fauna held for Early Miocene (but associated with Cycloclypeus annulatus, so more likely Middle Miocene age, probably Bulu Limestone; HvG)) Martin, K. (1907)- Systematische Ubersicht uber die Gastropoden aus Tertiaren und jungeren Ablagerungen von Java. Neues Jahrb. Min. Geol. Pal. 1907, 2, p. 151-162. ('Systematic overview of Tertiary and younger gastropods from Java'. Listing of 648 gastropod species names. No illustrations, ranges, descriptions, etc.) Martin, K. (1911)- Palaeozoische, Mesozoische und Kaenozoische Sedimente aus dem sud-westlichen Neu- Guinea. Sammlungen Geol. Reichsmus. Leiden, ser. 1, 9, 1, E.J. Brill, p. 84-107. (Paleozoic, Mesozoic and Cenozoic fossils from foothills from SW New Guinea expeditions 1907-1909. Brief review of fossils collected in foothills South of Central Range by Heldring. Flanks of Wilhelmina (=Trikora) peak composed of Eocene Nummulites and Alveolina limestones. Float in Setakwa (Otakwa) river with Mesozoic limestone with ammonite (Coeloceras?) and Eocene Lacazina limestone. In Noordwest River hard quartz sandstone with brachiopods Rhynconella and Spiriferina (Permian?). In Noord/ Lorentz River Paleozoic grey limestone with trilobite fragments, also blue gray rock with orthoceratid, probably Actinoceras. In B-River (upper tributary of Eilanden R.) Jurassic ammonites (Macrocephalites?), belemnites, also Eocene Nummulites and Alveolina limestones, E Miocene Lepidocylina limestone, etc. No plates) Martin, K. (1914)- Miocane Gastropoden von Ost-Borneo. Sammlungen Geol. Reichs-Museums Leiden, ser. 1, 9, p. 326-336. ('Miocene gastropods from E Kalimantan') Martin, K. (1914)- Die Fauna des Obereocaens von Nanggulan auf Java, A. Gastropoda. Samml. Geol. Reichs- Museums Leiden, ser. 2, 4, p. 107-178. (online at: http://bhl.ala.org.au/bibliography/50429/summary) (‘The fauna of the Upper Eocene of Nanggulan, C Java, A. Gastropoda’. Descriptions of very well-preserved gastropods from U Eocene marls of Nanggulan, W of Yogyakarta) Martin, K. (1915)- Die Fauna des Obereocaens von Nanggulan auf Java, B. Scaphopoda, Lamellibranchiata, Rhizopoda u. Allgemeiner Teil. Samml. Geol. Reichs-Museums Leiden, N.F. 2, 5, p. 179-222. (online at: http://bhl.ala.org.au/bibliography/50429/summary) (‘The fauna of the Upper Eocene of Nanggulan, Central Java, B. Scaphopoda, Lamellibranchiata, Rhizopoda and general part’. Part 2 of Martin (1914) paper. Descriptions of well- preserved molluscss from Eocene marls of Nanggulan, W of Yogyakarta) Bibliography of Indonesia Geology , Ed. 5.1 133 www.vangorselslist.com March 2014 Martin, K. (1916)- Die Altmiocane Fauna des West-Progogebirges auf Java. A. Gastropoda. Samml. Geol. Reichs-Museums Leiden, N.F., 2, 6, p. 223-261. (‘The Early Miocene fauna of the West Progo Mountains on Java, A. Gastropods’, SW of Yogyakarta) Martin, K. (1917)- Die Altmiocane Fauna des West-Progogebirges auf Java. B. Scaphopoda, C. Lamellibranchiata, D. Rhizopoda. Samml. Geol. Reichs-Museums Leiden, N.F., 2, 7, p. 261-296. (‘The Early Miocene fauna of the West Progo Mountains on Java- Scaphopoda, Lamellibranchiata, etc.) Martin, K. (1918)- On some fossils from Celebes believed to belong to the Oligocene. Proc. Kon. Nederl. Akad. Wetenschappen, Amsterdam, 20, p. 793-799. (online at www.digitallibrary.nl) (Fish fossils found by Abendanon near Enrekang along lower Saadang River, believed to be of Oligocene age by Dollfus, based on presence of Vicarya. However, this is misidentified and mollusk fauna more likely of Neogene age) Martin, K. (1918)- On the Miocene fauna of the West Progo Mountains in Java. Proc. Kon. Akademie Wetenschappen, Amsterdam, 20, 6, p. 800-804. (online at www.digitallibrary.nl) (Rich Miocene macrofossils from right bank of Progo River, W of Yogyakarta, Main localities: marls at Gunung Spolong and clay Kembang Sokkoh (well preserved, still some shine and color). Shallow marine Indo-Pacific mollusc assemblage, 103 species, only 7% still alive today. Associated with Miogypsina thecidaeformis. Most likely age Early Miocene) Martin, K. (1919)- Unsere palaeozoologische Kenntnis von Java mit einleitenden Bemerkungen uber die Geologie der Insel. Brill, Leiden, 158 p. ('Our paleozoological knowledge of Java, with introductory remarks on the geogy of the island'. Early overview of Cretaceous- Recent Java fossils) Martin, K. (1921)- Die Mollusken der Njalindungschichten erster Teil, Gasteropoda. In: Die Fossilien von Java auf Grund einer Sammlung von Dr. R.D.M. Verbeek und von anderen bearbeitet durch Dr. K. Martin. Sammlungen Geol. Reichs-Museums Leiden (N.F.) 1, 2, 3, E.J. Brill, Leiden, p. 446-496. (‘The molluscs of the Nyalindung Beds, part 1, Gastropods'. Molluscs from M Miocene, SW Java) Martin, K. (1922)- Die Mollusken der Njalindungschichten, Gasteropoda (Fortsetzung), Scaphopoda, Lamellibranchiata, Allgemeiner Theil. Sammlungen Geologischen Reichs-Museums Leiden. (N.F.) 1, 2, 4, E.J. Brill, Leiden, p. 471-496. (‘The molluscs of the Nyalindung Beds, continuation, Scaphopoda, Lamellibranchiata, General Part') Martin, K. (1926)- Plioceene versteeningen van Cheribon in Java. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl.-Indie 4, p. 1-24. ('Pliocene fossils from Cirebon in Java'. Shallow marine and brackish water molluscs from Pliocene of Tji Doerei, SW of Karang Suwung) Martin, K. (1928)- Eine Nachlese zu den neogenen Mollusken von Java. Leidse Geol. Mededelingen 3, p. 105- 129. ('Supplement to the Neogene molluscs from Java'. Additions to Martin (1919) paper, based on new Miocene- Pliocene mollusc material collected by Geological Survey in W Progo Mts (C Java), Nyalindung Beds (W Java) and Tjilanang Beds. No maps or stratigraphy info) Martin, K. (1928)- Mollusken aus dem Neogen von Atjeh in Sumatra. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl-Indie 10, p. 1-36. (Descriptions of Neogene mollusks from Aceh, N Sumatra, collected by 'Dienst Mijnwezen'. Indo-Pacific fauna) Martin, K. (1928)- Concerning the Tertiary of Atcheen. Proc. Kon. Nederl. Akademie Wetenschappen, Amsterdam, 31, 3, p. 300. (online at http://www.dwc.knaw.nl/DL/publications/PU00015579.pdf) Bibliography of Indonesia Geology , Ed. 5.1 134 www.vangorselslist.com March 2014 (One-page communication summarizing work on molluscs from ~3000m thick Pliocene deposits of N Aceh. Department of Mines collected >6000 molluscs, belonging to 347 different species. Typical Indo-Pacific fauna) Martin, K. (1929)- Ein neues Argonautiden Geschlecht von Sumatra. Leidsche Geol. Mededelingen 3, p. 221- 226. ('A new Argonautid genus from Sumatra'. New octopod nautiloid shell, described as Kapal batavus, from clay nodule in M-L Miocene Lower Palembang Beds of Pangadang, 25 km W of Sekayu, S Sumatra) Martin, K. (1931)- Mollusken aus dem Obereocaen von Nanggulan. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Indie 18, p. 1-56. ('Molluscs from the Upper Eocene of Nanggulan'. Follow-up of Martin 1915 paper. Taxonomic descriptions of molluscs (mainly gastropods) from the shallow marine Upper Eocene of Nanggulan, C Java, collected by Zwierzycki, Van der Vlerk and Gerth. 72 new species. No stratigraphy, locality descriptions) Martin, K. (1932)- Ein eocaner Nautilus von Java. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Indie 20, 4 p. ('An Eocene nautilus from Java'. New Nautilus species from Eocene of Kali Puru, Nanggulan, C Java) Martin, K. (1932)- Bericht over fossielen van Kedoengwaroe in Soerabaja. Jaarboek Mijnwezen Nederl.-Indie 59 (1930), Verhandelingen 3, p. 113-121. ('Report on fossils from Kedung Waru in Surabaya'. Shallow marine Pliocene molluscs from Kedung Waru anticline along road Jetis-Sidoteko) Martin, K. (1933)- Eine neue Tertiare Molluskenfauna aus dem Indischen Archipel. Leidsche Geol. Mededelingen 6, 1, p. 7-32. ('A new Tertiary mollusc fauna from the Indies Archipelago'. Mollusc assemblage of 26 new species from Buton asphalt-bearing marls/ limestones, which are unconformable over folded Mesozoic sediments. Assigned Late Oligocene or E Miocene age. Later interpretations generally favor Late Miocene-Pliocene age (e.g. Beets 1952, Keyzer 1953)) Martin, K. (1935)- Oligocaene Gastropoden von Buton. Leidsche Geol. Mededelingen 7, 2, p. 111-118. (‘Oligocene gastropods from Buton’) Martin, K. (1937)- Die oligocaenen Mollusken von Buton als Auswurflinge eines Schlammsprudels betrachtet. Leidsche Geol. Mededelingen 8, p. 311-314. ('The Oligocene mollusks from Buton, interpreted as clasts in mud volcano'. Molluscs from Buton originally dated as Oligocene, here regarded as mud volcano ejecta. Subsequently found to be Mio-Pliocene age; Beets 1952) Martin-Icke, H. (1911)- Die fossilen Gastropoden. In: L. Selenka & M. Blanckenhorn (eds.) Die Pithecantropus-Schichten auf Java. Geologische und palaontologische Ergebnisse der Trinil-Expedition (1907 und 1908). Engelmann, Leipzig, p. 46-51. ('The fossil gastropods'. Late Pliocene - E Pleistocene gastropods from Trinil, collected by Selenka expedition) Martini, E. (1971)- Standard Tertiary and Quaternary calcareous nannoplankton zonation. In: A. Farinacci (ed.) Proc. Second Planktonic Conference, Rome, 1970, p. 737-785. Martino, E., P.D. Taylor, A. Kudryavtsev & J.W. Schopf (2016)- Calcitization of aragonitic bryozoans in Cenozoic tropical carbonates from East Kalimantan, Indonesia. Facies 62, 11, p. 1-15. (Calcification of originally aragonitic skeletons of cheilostome bryozoans Reussirella and Reptadeonella in muddy reefs from Miocene of E Kalimantan) Matsumaru, K. (1974)- The transition of the larger foraminiferal assemblages in the Western Pacific Ocean- especially from the Tertiary period. J. of Geography (Chigaku Zasshi), Tokyo, 83, 5, p. 281-301. Bibliography of Indonesia Geology , Ed. 5.1 135 www.vangorselslist.com March 2014 (In Japanese. Review of stratigraphic distribution of larger foraminifera in localities across SE Asia- W Pacific, the Letter zonation and its calibration to planktonic foram zones) Matsumaru, K. (1974)- Larger foraminifera from East Mindanao, the Philippines. In: Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 14, p. 101-115. (E Mindanao Cretaceous andesites and sediments, unconformably overlain by Tertiary clastics and carbonates. Larger foram assemblages Early Oligocene (Tcd/ with Nummulites fichteli and Borelis pygmaeus) and Miocene (Te1-4, Te5 and Tf1-2)) Matsumaru, K. (1980)- Cenozoic larger foraminiferal assemblages of Japan, Part 1. A comparison with Southeast Asia. In: T. Kobayashi et al. (eds.) Geology and Paleontology of Southeast Asia, University of Tokyo Press, 21, p. 211-224. (Review of Eocene- Recent larger foram occurrences and zonation in Japan and correlation with Indonesian letter zonation. Three abundance peaks: (1) M-L Eocene, (2) Late Oligocene; (3) latest E Miocene-M Miocene) Matsumaru, K. (2011)- A new definition of the Letter Stages in the Philippine Archipelago.Stratigraphy 8, 4, p. 237-252. (M Paleocene- Recent Letter Stages for Philippines re-defined in terms of 17 larger foram assemblage zones) Matsumaru, K. (2012)- Miogypsinid foraminiferal biostratigraphy from the Oligocene to Miocene sedimentary rocks in the Tethys Region. In: I.A. Dar (ed.) Earth Sciences, InTech Open Science, 25, p. 619-648. (online at: http://cdn.intechopen.com/pdfs/27609/.. ) (Good review of late Oligocene- M Miocene miogypsinid larger foram evolution and biostratigraphy Matsumaru, K. & K. Kimura (2012)- Larger foraminifera from the Eocene Shimizu and Miocene Misaki Formations in Tosa Shimizu City, Kochi Prefecture, Japan. Trans. Proc. Palaeont. Soc Japan 156, p. 255-269. (online at: www.palaeo-soc-japan.jp/download/TPPSJ/TPPSJ_NS156.pdf) (Larger foraminifers from Eocene Shimizu Fm (Asterocyclina, Orbitoclypeus. Discocyclina) and Miocene Misaki Fm (Nephrolepidina) in Tosa Shimizu City, Kochi Prefecture, Shikoku, Japan) Matsuoka, K. (1981)- Dinoflagellate cysts and pollen in pelagic sediments of the northern part of the Philippine Sea. Bull. Fac. Liberal Arts, Nagasaki Univ. Natural Science 21, 2, p. 59-70. Matsuoka, K. (1981)-Dinoflagellate cyts and Pediastrum from the Nanggulan and Sentolo Formations in the middle Java Island, Indonesia. In: T. Saito (ed.) Micropaleontology, petrology and lithostratigraphy of Cenozoic rocks of the Yogjakarta Region, Central Java,. Spec. Publ. Yamagata University, p. 48-52. Matsuoka, K. (1983)- A new dinoflagellate cyst (Danea heterospinosa) from the Eocene of Central Java, Indonesia. Review Palaeobot. Palynology 40, 1-2, p. 115-126. (New gonyaulacacean dinoflagellate species Danea heterospinosa from Nanggulan Fm of Kali Puri, 20km W of Yogyakarta. Associated with M Eocene calcareous nannoplankton assemblage of zones CP 13-CP14) Matsuoka, K. (1984)- Some dinoflagellate cysts from the Nanggulan Formation in Central Java, Indonesia. Trans. Proc. Palaeont. Soc. Japan, N.S., 134, p. 374-387. (online at: http://www.palaeo-soc-japan.jp/download/TPPSJ/TPPSJ_NS134.pdf) (13 species of Paleogene dinoflagellate cysts belonging to nine genera of Gonyaulacales group. Four new species; Glaphyrocysta circularis and G. dentata of Ceratioid Lineage and Exochosphaeridium reticulatum and E. brevispinosum of Gonyaulacoid Lineage) McGowran, B. (1978)- Australian Neogene sequences and events. Proc. 2nd Working Group Mtg. Biostratigraphic datum planes of the Pacific Neogene, IGCP Project 114, Bandung 1977, p. 165-167. McGowran, B. (1979)- The Tertiary of Australia: foraminiferal overview. Marine Micropal. 4, 3, p. 235-264. Bibliography of Indonesia Geology , Ed. 5.1 136 www.vangorselslist.com March 2014 Widespread oceanic hiatuses appear to correlate with episodes of global warming and transgression) McGowran. Centre. eine Leitform aus dem Eocan von Sudost Borneo und Java. M. Thalmannia.G. McGowran. K.sp. p. 3-27. W... Larger foraminifera in Australia limited to 5 Eocene and 4 Oligo-Miocene excursions of tropical larger benthic forams. 302-309. (eds.E. L. 29-51. B.1 137 www. P. etc.Handleiding voor het determineeren van de groot foraminiferen-genera van Nederlandsch Oost Indie. p.A. Sr age 1. p.(Four major Tertiary sequences. Li (2000). Publ. W. Late Oligocene N3-N4. 1-46. (1946). Southern Australia. Eclogae Geologicae Helvetiae 39. Johnson. Berau area. including Cenozoic larger foraminifera of Papua New Guinea and biostratigraphic correlations in the Indo-Pacific region) McGowran. an index species for Upper Eocene in SE Kalimantan (Asem Asem and many other E Kalimantan localities) and C Java (Nanggulan)) Mohler.sp. 459 p. Burdigalian) Bibliography of Indonesia Geology . HvG)) McGowran. B. (Descriptions of 25 ostracode species in Late Pliocene Upper Kalibeng Fm and Pleistocene Pucangan Fm at Sangiran Dome.Biostratigraphy: microfossils and geological time. 298-300. Palaeoecology 55.M Miocene N8-N11 and N14 (similar to distribution in Japan. B. Palaeoclim. Publ.Plio-Pleistocene ostracoda from Sangiran. (1946). (1986). Palaeoclim.6 Ma).J. (‘Manual for the identification of larger foram genera of Indonesia’. Pal. (1946).Martin Glaessner's foraminiferal micropaleontology..0 Ma). Lacustrine Upper Pucangan Fm with Physocypria and Indocythere) McMonagle. in area underlain by oceanic crust and dominated by deep marine sedimentation. p. London. (2005). Lower Pucangan Fm with brackish water assemblage of Ishizakiella.J. Jawa. The Micropaleontological Society. & Q.. larger foram zone Te1.B. & Sudijono (1981).) Landmarks in foraminiferal micropaleontology: history and development. K. Palaeogeogr.8-27.. Dev.. aus dem Burdigalien von Ost-Borneo. 5. 28-42.A. p. Spec. Geol. Res. 2. Sr isotope ages 28. Small atlas of key larger foraminifera genera of Eocene. Eclogae Geologicae Helvetiae 39. Lunt... Re-dating of limestones in E Sabah: (1) Lower Kinabatangan Lst mid-Oligocene (coral-rich. Bowden et al. Palaeoecology 305. Stenocypris and Cyprinotus.Evolutionary palaeoecology of Cainozoic Foraminifera: Tethys. 1. W. Description of new small miliolid Sigmoilina personata. Stellate and advanced nephrolepidine Lepidocyclina with four rays from Sungai Mandai. (Review of M. Cambridge University Press. (Overall Cenozoic climatic deterioration reversed in Eocene and in Miocene by short-lived. (2) Gomantong Lst Early Miocene (LBF zone Te5/earliest Tf1. extratropical excursions by tropical-type foraminifera. 15. B. (‘Sigmoilina personata n. Hemicytheridea. Ser. Wilson. an index species from the Eocene of SE Borneo and Java’. In: A. Associated larger foram assemblage includes Miogypsina and Miogypsinoides and suggests zone Tf1. Hemicytheridea. C Java. (2013). (Tertiary larger foram extinctions and migrations into higher latitudes tied to major cooling/warming events) McKenzie.72 Ma) Mohler. Palaeogeogr. ('Lepidocyclina crucifera new species from the Burdigalian of E Kalimantan'. Unknown publisher.A. Soc. late E. warm climate periods: late M-L Eocene.vangorselslist. (Shallow marine limestones rel. Young (2011). p.sp. nannofossil zone NP24. p. rare onshore N Borneo and show punctuated development.Sigmoilina personata n. far-reaching. 227-250.Lepidocyclina crucifera n. Shallow marine Kalibeng Fm fauna with Neonesidea.A re-assessment of age dating of fossiliferous limestones in eastern Sabah.Recent of Indonesia) Mohler. reflecting rel. (3) Togopi Limestone with Alveolinella quoyi and abraded Calcarina (Pliocene-Pleistocene..G..Cainozoic oceanic and climatic events: the Indo-Pacific foraminiferal biostratigraphic record. Ilyocypris. Historical Biol. Glaessner contributions to foraminiferal micropaleontology. p. C. Geol.247-265. Sr age 21. Indo-Pacific.com March 2014 . Ed. Borneo: implications for understanding the origins of the Indo-Pacific marine biodiversity hotspot. Cytherelloidea. Manning & J. A.125-157. Proc. 99- 108. Eclogae Geologicae Helvetiae 41. ('On the occurrence of Alveolina and Neoalveolina in Kalimantan'. Lejeunecysta. W.vangorselslist. (1949). Java’. Indonesia. Eocene Alveolina rel. E Kalimantan) Morgenroth. A. 1968 work) Morley. but not in Priabonian. both marine claystones overlain by Rajamandala Fm limestones. (Flosculinella reicheli. from genera Achomosphaera. 111-137. p. Javadinium. Anwar Maruyani (2011). N Barito basin. 329-332. Suggests Aquitanian age for Spiroclypeus limestone and Burdigalian age for Flosculinella-bearing limestones) Mohler. in Hajup rubber plantation N of Tanjung. p. Neoalveolina (N. 29th Ann. Proc. 321-329. Geol. 521-527. (1977). Rahardjo & K.A. 2. Petrol. p. Conv. Morgenroth. commonly associated with Nummulites fichteli) Mohler. Palaeontographica. 4-6.1 138 www. common in NE Kalimantan. p. Bibliography of Indonesia Geology . 15 new. P. 4.T.Palynology of Tertiary and Quaternary sediments in Southeast Asia. R. M Eocene (Ta). HvG) first occurs at base of Tc/ Oligocene.Dinoflagellate cysts from two Oligocene surface sections on Java island. P.Dinoflagellate cysts from Miocene outcrops on Java island.Dinoflagellate cysts. Twenty-six dinoflagellate species found. p.T. A. R. aus dem Tertiar e5 von Borneo. Indonesia. (1949).A. 6th Ann. Also common in Lutetian. p. (Two Oligocene surface sections studied in W Java. W. Rahardjo & K.T.J.J.Development and vegetation dynamics of a lowland ombrogenous peat swamp in Kalimantan Tengah.A. Dinoflagellate cysts in phosphatic nodules heavily affected by thermal metamorphism. building on Germeraad et al. W. Hystrichosphaeropsis. Eclogae Geologicae Helvetiae 42.sp. (Up to eight palynozones in Oligocene.Late Oligocene boundary. (1949). Southern Mountains. Edwardsiella. Anwar Maruyani (2008). also around Early. (IAGI). Assoc.) Morgenroth. J. 519-521. B 278. 383-404. p. mainly based on evolution of Florschuetzia species of mangrove pollen. 5. Most samples common dinoflagellate cysts. Indonesia. Palaeontographica.Pelabuhan Ratu road (M Miocene Cimandiri Fm). W.Quaternary. 29 species. Assoc. rather than Lower Eocene and represents reef deposit formed at same time as Nanggulan limestones farther W (already identified as Late Eocene Pellatispira limestone by Gerth 1930. Dilabidinium. Indon. p. Hulu-Sungei area. HvG)) Mohler. Batuasih Fm near Cibadak and equivalent section near Padalarang. A.A. Biogeography 8. 1.Spiroclypeus und Flosculinella in Kalken aus dem Kustengebirge zwischen Patjitan und Blitar (Java). (1949). p. a new species of globular flosculinellid from foram-rich marl of Te5/Burdigalian age. P. Spiniferites. etc. Foraminifera and nannoplankton date Batuasih section around Early-Late Oligocene boundary. ('Spiroclypeus and Flosculinella in limestones of the coastal ranges between Pacitan and Blitar. 255-276. (Dinoflagellate cysts in three Miocene surface sections in West and C Java: Cipimangkis River near Jatiluhur (Late Miocene Cisubuh Fm). including three new species) Morley. Rahardjo & K. 2. 2. Ed. Maryunani (2000).. Padalarang section planktonic foraminifera indicative of zones P20-P21. Limestone of Gamping outcrop W of Yogya is Upper. Kali Jaya NNE of Kebumen (around E-M Miocene boundary) and Cijarian River along Bogor..Das Alter des Eozan-Kalkes von Gunung Gamping westlich Djokjakarta. Indon. SE Java'. Dinoflagellate cysts may indicate slightly younger age than Batuasih. Bandung. but not S of Sangkulirang Bay. (‘The age of the Eocene limestone of Gunung Gamping W of Yogyakarta. Java. 4-6.Uber das Vorkommen von Alveolina und Neoalveolina in Borneo.com March 2014 .an alternative stratigraphic tool in marine Tertiary strata in Indonesia. Eclogae Geologicae Helvetiae 41. B 284. Conv. Operculodinium.Flosculinella reicheli n. pygmaeus group= Borelis.Mohler. Eclogae Geologicae Helvetiae 42. (1981).. 9. In: M. Much of Sunda region moisture deficient in Oligocene. (2003). Nine dispersal routes. R.J. Phyllocladus subsequently dispersed into SE Asia) Morley. (1982). R. leading to more pine forests and savannah. p.E Tertiary Gondwana break-up and routes formed since M Eocene phases of plate collision) Morley. Sunda Eocene flora stretched as far East as S arm of Sulawesi. Chapter 1. (1982). 211-234.Interplate dispersal paths for megathermal angiosperms. Int.pdf) (Tertiary plant dispersals reflect tectonic and climatic evolution of SE Asia.com March 2014 .000 year pollen record from Danau Padang. (1998). Flenley (eds. 151-190. New Guinea mountains formed in M Miocene allowing dispersal of Gondwana taxa from S. 28. Jakarta 1995. Morley.J. (On palynomorph distribution patterns in sequences/ systems tracts) Morley.J. In: C. Symposium on sequence stratigraphy in SE Asia. p. Ed. In: R.J. Central Sumatra. Greatest extent of rainforest at beginning of M Miocene. Some.A. Indon. p. so in Tertiary application of palynology is mainly in correlation rather than dating.Cretaceous and Tertiary climate change and the past distribution of megathermal rainforests. 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Includes reports of Lacazina larger foram in Eocene of Dramai Island SE of Triton Bay. Reichsmus. Sammlungen Geol. Vier Eozanvorkommen aus Ost-Borneo. Coralline nummulitid limestones described by Hirschi from Batu Putih rich in large Lepidocyclina formosa (= Eulepidina). Discocyclina dispansa. Sammlungen Geol.coal beds on Pulau Laut. N.repository. Rutten footnote: “it is remarkable that the Eocene fauna of Celebes is more similar to samples from New Guinea than Java and Borneo”) Rutten. Leiden (1). javanus. but called Calcarina. Sample from Sungai Apat also rich in Pellatispira.nl/document/552375) ('Studies on foraminifera from East Asia. Alveolina. 9. Discocyclina. previously described as Calcarina) Bibliography of Indonesia Geology . etc. With Nummulites bagelensis. Four Eocene localities in East Kalimantan'. fichteli= E Oligocene ?) and black Nummulites limestone from Sebuku River) Rutten. Lepidocyclinea limestones of Bau Putih near Puruk Cahu. (online at: http://www. Balambangan and Banguey (= Banggi)) Rutten.repository. L. HvG) characterized by large Lepidocyclina. 6.com March 2014 . (1915).Foraminiferen-fuhrende Gesteine von Niederlandisch Neu-Guinea.. NE Kalimantan’. ('Some foraminifera from the east arm of Sulawesi'. South Kalimantan'..-Indie 43 (1914). L. p. Ed. 8. Oligocene with Nummulies fichteli. Jaarboek Mijnwezen Nederl. 9. Eocene at Sg Bungalun (with Pellatispira. Lepidocyclinenkalke von Batoe Poetih bei Poeroek Tjahoe.vangorselslist. L. 2. but Oligocene or early Miocene age) Rutten.322. 11-18. M Miocene marls with Lepidocyclina angulosa. (online at: http://www. Sud. Cycloclypeus annulatus. Verhandelingen 2. Eocene with Orthophragmina (= Discocyclina).Eocene orbitoiden en nummulieten van Paloe Laoet. 9. W Java limestone belt between Cibadak.Studien uber Foraminiferen aus Ost-Asien. 10. Indie 44.1 157 www.R. L.Studien uber Foraminiferen aus Ost-Asien. L. (1914). Zwei Fundstellen von Lepidocyclina aus Java. L.Tagogapu (=Rajamandala Limestone. 7. 29-32. Tertiare Foraminiferen von den Inseln Balambangan und Banguey.Foraminiferen-kalksteenen uit de Tidoengsche landen (Noord-Oost Borneo). Sammlungen Geol. p. p. p. (1914). Includes an Eocene sample with Alveolina wichmanni n. L. Leiden (1). 74-77. Leiden (1). collected by Hotz from two islands N of Sabah. Follow-up of Rutten (1915) description of Eocene limestones collected by Munniks de Jongh (1913) in upper Tarakan basin. 322-324. 9. Sammlungen Geol. etc. ('Studies on foraminifera from East Asia.Sukabumi. (1915). SE Borneo) Rutten. Nova Guinea 6. Leiden (1). Tanjung Seilor (Kayan River.Studien uber Foraminiferen aus Ost-Asien.) Rutten.Rutten. Rutten not sure if earliest Miocene or Oligocene) Rutten. 307-320. Reichsmus. 10. Einige Foraminiferen aus dem Ostarm von Celebes. 5. Nummulites). Miocene and Eocene larger forams from Balambangan and Banguey islands. (1914). Miocene Lepidocyclina associated with arc volcanics on Arimoa Islands off N New Guinea.Studien uber Foraminiferen aus Ost-Asien. (Orthophragmina (=Discocyclina) omphalus and Nummulites bagelensis demonstrate Eocene age of marl formation above the sandstone. p. Mangkalihat Peninsula (Discocyclina. nordlich von Borneo.naturalis. 6. L. Reichsmus. Geol.nl/document/552375) ('Studies on foraminifera from East Asia. sp. Leiden (1). 320. p.naturalis. North of British Borneo'. 9. 21-51. (1916). 7. Sammlungen Geol. (Description of foraminifera-bearing rocks from the 1903 Netherlands New Guinea Expedition collected by Wichmann. 3-10. ('Studies on foraminifera from East Asia. (1914).Borneo.Studien uber Foraminiferen aus Ost-Asien. p. here called Orthophragmina). 5. Reichsmus. therefore not Eocene. also with N. Jaarboek Mijnwezen Nederl. (‘Foraminiferal limestones from the Tidung Lands. p. 8. (1915). Reichsmus. Two localities with Lepidocyclina on Java'. sp. Jaarboek Mijnwezen Nederl. Akademie Wetenschappen. 23. L. Proc. (online at: http://www. Amsterdam. Proc. p. Nederl. (online at: http://www.) brouweri n.Over de foraminiferenfauna en den ouderdom van kalksteenen uit Zuid-Celebes afkomstig uit de groep der vischresten-bevattende gesteenten.vangorselslist. 27.pdf) (Tertiary limestones collected by BPM from N New Guinea between Tami and Biri rivers. (2) Embryonal chambers of Lepidocyclina acuta from Balikpapan area.Kleine mededeelingen over foraminiferen uit Nederlandsch-Indie. ('On the occurrence of Halimeda in Old-Miocene coast reefs of East Borneo'. Gen. (1925). (1924). Proc.pdf) (English version of Dutch paper above)) Rutten. Also two samples of black-grey Eocene reefal limestone with Alveolina.dwc.dwc. Jaarboek Mijnwezen Nederl. 415-428. epigona in Globigerina-chert of Skru Island (W New Guinea) (confirmation of small. L. 5. p.dwc.and the Biri- River basins. (1924). 2.Quaternary and Tertiary limestones of North New Guinea between the Tami.knaw. Kon. Kon. p. (online at: www. Kon. Akademie Wetenschappen Amsterdam 28. Amsterdam. no fragments of volcanic rocks observed in limestones and sandstones) Rutten. in nearby samples suggest E Miocene age) Rutten. Amsterdam. Akademie Wetenschappen. 8. Verhandelingen. Linderina limestone on Bacan (probably Late Miocene or Pliocene calcareous sandstone rich in Planorbulinella). Verhandelingen Geol.. (1921). L.nl/DL/publications/PU00012007. Brief descriptions of foram- bearing samples. Kon. Includes: 1. L.dwc. Akademie Wetenschappen. L. (1921). L. p. 7-8. Indie 52 (1923). No detailed locality information. Ed. but rel. Kon. Proc.On Foraminifera-bearing rocks from the basin of the Lorentz River (Southwest Dutch New Guinea). 173-183. (3) Age of limestone on island Kamara(ng) in Pare Pare Bay. Kon.On the occurrence of Halimeda in Old-Miocene coast reefs of East Borneo.R. Mijnbouwk. 8 (Verbeek Memorial Volume). Geol. L. (Larger forams from limestone from series with fish fossils in S Sulawesi (Brouwer 1924). (1925). 1.. (1924). Ser. Unlike N New Guinea. (1920). Proc. 506-508.com March 2014 . Nederl. L. Eocene Alveolina-Lacazina limestone from top of Wilhelmina (Trikora) peak. 539-544. 1137-1141.Rutten. Nederl. (online at: http://www. Nederl. 6.Over fossielhoudende Tertiaire kalksteenen uit Britsch Noord Borneo. L.knaw. 606-614. but true Lepidocyclina)) Rutten.pdf) (Eocene Alveolina-Lacazina and Nummulites and Miocene Lepidocyclina foraminiferal limestone pebbles from Lorentz River (S foreland of Central Range). p.Over het voorkomen van Halimeda in Oudmiocene kustriffen van Oost Borneo. etc. p.1124-1126.pdf) (English version of Rutten (1924). Nummulites. Akademie Wetenschappen. Spiroclypeus and Lepidocyclina (N. Bibliography of Indonesia Geology .nl/DL/publications/PU00014672. (Short notes on foraminifera from the Dutch Indies'. Eocene Nummulites-Alveolina-Lacazina in Horna region and many E-M Miocene limestone localities) Rutten.knaw. 1. Amsterdam. (1920). Majority of limestones of Oligo-Miocene age with Lepidocyclina. 529-534.M. Calcareous algae Halimeda rel.1 158 www. common in modern coastal reefs in E Indonesia. Orthophragmina (=Discocyclina) in Nanggoi River. Several E Miocene limestones from E Kalimantan have Halimeda. including globigerinid limestone near SE coast (= Imskin Fm of subsequent authors). opuntia) Rutten. 28. 23. S Nimboran Mts) Rutten.nl/DL/publications/PU00015069. Amsterdam. S Sulawesi (Late Neogene.knaw.Foraminiferen-houdende gesteenten uit het gebied van de ‘Vogelkop’ op Nieuw Guinea. p. Verslag. Nederl. Indie 53 (1924). common Operculina without Lepidocyclina.nl/DL/publications/PU00014766. Kolon. Nederl. probably same as recent species H. See English version below) Rutten. Akademie Wetenschappen. (4) Lepicocyclina cf. p. ('Foraminifera-bearing rocks from the area of the 'Birds Head' on New Guinea'. uncommon in Miocene limestones. 22.Some notes on Foraminifera from the Dutch Indies. Fish-bearing limestones with non-diagnostic Heterostegina only. p. E Kalimantan. 147-167. Geologie en Mijnbouw 10. p. M. Geol. 27th Ann. W Sulawesi'. 297-328. Geol. Ser. A.G. Kon. p. Pisang Island.Over Tertiaire. 5. Nederl. Kudat Peninsula N of Kinabalu Eocene limestones with Discocyclina. Kabupaten Mamuju Utaru. 170-172.dwc. Sulawesi Barat. Assoc. Mijnbouwk. Proc.H. Sempor and Rawakele Formations of the Kebumen Area. (‘Tertiary foraminifera from E Sulawesi’. First and only occurrence is Lepidocyclina zeijlmansi Tan Sin Hok 1936 from northern Central Borneo. Congr. Geol.E Pliocene. (1936). Correlation with Bodjonegoro sequence relatively easy) Saito.. Indon. 10. (1926). Geol. Tokyo 1976.Tertiaire foraminiferen van Oost Celebes. Part of Von Loczy (1934) E Sulawesi mapping report) Rutten. In: Late Neogene Epoch boundaries. Kendeng zone. 4. p. 8. etc. Arifin ( (2012). ENE of Ngawi. Verhandelingen Geol. L. etc. Spiroclypeus and Pellatispira. ('On Tertiary foraminifera-bearing rocks from Berau. Mus.pdf) (Planktonic foram biostratigraphic study of Late Miocene. ('Rocks and fossils from Pisang Island and from New Guinea'. P. from widespread limestones in Berau region. Ser. 179. no Pellatispira) Rutten. Rutten. Burckle & J. (1950). p. Nederl. Miogypsina. Most Tertiary clastic sediments contain rounded fragments of Mesozoic radiolarite. samples.Late Miocene to Pleistocene biostratigraphy of equatorial Pacific sediments. 106-117.Pliocene Globigerina Marls Fm of Ngepung section. p.F. 2012-SS-28.. Nederl. ('Planktonic foraminifera biostratigraphy of the sand member of the Pasangkayu Formation. Saito. M. NE Kalimantan. p. 640m thick.G. J. 2. Akademie Wetenschappen 53.('On fossiliferous Tertiary limestones from British North Borneo'. foraminiferenhoudende gesteenten uit Beraoe (Oost Borneo).geoscienceworld. Foraminiferal Research 9.Biostratigrafi foraminifera planktonik satuan batupasir Formasi Pasangkayu. Verhandelingen Kon.knaw.R.M. Hist. (IAGI). & Suminta (1979). 286-289. Roy. Indon.Planktic foraminifera biostratigraphy of the Penosogan. L. but closely related species. T. L. p. (1934).Late Cenozoic planktonic forminiferal datum levels: the present state of knowledge toward accomplishing Pan-Pacific stratigraphic correlation.pdf) (Larger foram genus Lepidocyclina very rare in Eocene of SE Asia. Indonesia. Both belong in subgenus Polylepidina) Safitri. Kecamatan Pasangkayu.org/content/9/2/106. Hays (1975).D. Oligocene and Miocene larger forams Lepidocyclina. Conv.. E Java. L. Mijnbouwk.On the contemporaneous occurrence of Lepidocyclina and Discocyclina in Northern Borneo. T. 41st Ann. E of Misool. First Int. p.Comparison of Lepidocyclina zeijlmansi Tan from Borneo with Lepidocyclina birmanica Rao from Burmah.M. (1977). collected by Weber (NKPM) and Beucker Andreae. 2. (IAGI). include Eocene limestone with Lacazinella. Ed. (online at: http://www. but some samples with younger Lepidocyclina) Rutten. 10. Pasangkayu. Proc. Study of N Lariang basin upper M Miocene.full. Conv.vangorselslist.Roches et fossiles de l’Ile Pisang et de la Nouvelle Guinee. Gen. Nummulites. Geol. p.Biostratigraphy of Late Miocene and Pliocene deep water sediments of eastern Java. E Kalimantan'. & F.. Nat. 1-13. consisting of three zones) Saint-Marc. Central Java Indonesia. Gen. Proc. 226-244.nl/DL/publications/PU00018769. birmanica Rao 1942 from Eocene of Burma is distinct. Bibliography of Indonesia Geology . 196-198. Belgique 12. Yogyakarta. Pacific Neogene stratigraphy. Proc. Assoc. L. Marls with sandy and tuffaceous intercalations.com March 2014 . Discocyclina. Hendrasto (1998). p. (1948). (online at: http://jfr. 7. 61-80. Micropaleontology Press. Kol. with abundant planktonic foraminifera. suggesting significant Pre-Tertiary uplift) Rutten. D. Imran & M.1 159 www. Bull. (Abstract only) Sahabuddin. Sarasin (1898). (1932). Tonga. Current Science India 31. mainly extant species. Zoologischer Anzeiger 20 (536)-. p. B. P. Bolli. (Standard work on Cenozoic radiolaria and zonations) Santoso.Materialien zur Naturgeschichte der Insel Celebes. In: H.M.The occurrence of Globorotalia velascoensis in the Philippines. Magazine 121. Geol. Ombilin basin. Saunders & K. (1934). A. Philippine Geologist (J. Indonesia. (Brief communication reporting first find of M Miocene foraminifera association of Miogypsina and Orbulina in calcareous sandstones of Strait and Nicholson Islands. C Java') Sanders. & T.V.M. (IAGI). 5. hoffmeisteri (Whipple) and in Andaman Islands by B.K. Geol. Kapid (2014). Ed. vol. Teil I. C.R.Pleistocene in the North Rast Java Basin. 97-99. p. Jurnal RISET Geol. Geol.D.) Scheffen. R.Paleosalinity conditions on Late Miocene. ('On the identification of Lepidocyclina's.geological travels in Sulawesi by cousins P. 20-21. V. (Biplanispira closely related to Pellatispira.vangorselslist. p. and F. Pertambangan (LIPI) 24. First discovered by Verbeek in 1874.com March 2014 . Orbulina in the Miocene of the Andaman islands. In Upper Eocene of Garo Hills. Biplanispira is confined to region between E India and Eua. mirabilis) Sampurno.B. 3. 1. Kreidel's Verlag.M.Ueber die Molluskenfauna der grossen SusswasserSeen von Central-Celebes. (Peaks in abundance of nannofossil species Calcidiscus leptoporus and Helicosphaera carteri used to infer rel. p. Sarasin) Sastri. p. Proc.On the occurrence of Miogypsina. ('On the mollusk fauna of the large freshwater lakes of Central Sulawesi') Sarasin. Includes 7 species of cyprinid fish. 11. and restricted to middle and upper parts of Upper Eocene. W. 4-76. Nederl. p. 25th Ann. from which it probably arose. Associated with plant fossils described by Heer 1874 and a water bird described by Lambrecht 1931) Sanfilippo. 1. 631-712. 1-102. Soc. M.Die fossilen Fische der Alttertiaren Susswasser Ablagerungen aus Mittel-Sumatra.Ostindische Lepidocyclinen. Gen. Indon.1 160 www. J. Bibliography of Indonesia Geology . Mijnbouwk.Zur Lepidocyclinen-Bestimmung. p. 4. R. Conv. Padang Highlands. Perch-Nielsen (eds. Cycloclypeus. (online at: http://www. G.. Barmawidjaja (1996).. Kapid & D.) Plankton Stratigraphy. Assoc. Insani & R.The genus Biplanispira Umbgrove (Foraminiferida) and its occurrence in India. & F. (1932). Cambridge University Press. Sarasin (1897). W. 1-11. Wiesbaden. De Mijningenieur 13.. (1984). 65-74. 241-245. (also Thesis University of Amsterdam. p.J. 16-30. W.. Ser. 1. Description of well- preserved Eocene fresh-water fish fossils from bituminous marly shales from S. hyposaline conditions in Late Miocene Ledok and Late Pliocene-E Pleistocene Selorejo Fms) Sarasin. & F.Cenozoic Radiolaria. 1-144.org/details/materialienzurna01sara) ('Materials for the natural history of the island of Sulawesi. Volume 1 of 5 of the classic work on the late 1800's geographic. Die Susswasser-Mollusken von Celebes. H. 142p. Geol.Analisis foraminifera kuantitatif pada kala Pliosen di daerah Ledok Kabupaten Blora. Sipang. it is represented by B. Jawa Tengah.S. (1964). Westberg-Smith & W. M. P. Riedel (1985). 1. 2. Chapter 14. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl-Indie 21. with further collections by Musper in 1927.archive. The fresh-water molluscs of Celebes island'. (First record of Paleocene planktonic foraminifera in S Palawan) Samanta. ('Quantitative analysis of Pliocene foraminifera of the Ledok area.Samaniego. en Kol. p. Philippines) 18. E India. Bedi (1962).W. Middle and S Andaman Islands) Scheffen. p.) ('The fossil fishes from Early Tertiary fresh water deposits from Central Sumatra'. based on nannoplanktonon population changes. Verhandelingen Geol. p. 311-318. M. Pal. C. No Late Eocene radiolarians due to probable hiatus or condensed section. Rangin et al. Earth-Science Rev. Scheiber. Part 3 (Families Eratoidae. Little or nothing on localities. Onset of larger foraminifera-dominated platform correlates with Paleocene/Eocene Thermal Maximum. Pliocene of Solo River and E Pleistocene of Mojokerto region. Geol.edu/publications/124_SR/VOLUME/CHAPTERS/sr124_26. in Nederl.a response to long.-Indie (IV).tamu.com March 2014 .A. Results 124. 659-661. R.E Eocene Tethys carbonate platforms: (1) late Paleocene: coralgal-dominated at low-mid paleolatitudes.P.A. 171-194. Leg 124. E. 233-256.P. Sites 767 and 770. (1907). Nummulites) platforms at low-middle paleolatitudes. In: E. 345-357. 153-203. Leg 124. Orbitolites.A. p. Descriptions of molluscs from Kajoe ragi area. 494-500. (3) E Eocene larger foraminifera-dominated (Alveolina.Late Paleocene.The marine mollusca of the Kendeng beds (East Java). ('The Buton asphalt with its foraminifera'.) Scheibner. 90. 11.Miocene radiolarians of the Sulu Sea. In: E.and short-term paleoclimatic change. Sammlungen Geol. (1932). p. F. Pelagic sedimentation until E Miocene. 195-210. with sea-surface temperatures in tropics beyond maximum temperature range of corals) Schepmann. 3. 81. when sedimentation became strongly influenced by continentally derived material) Scherer. (Part of series of papers on Kendeng Beds marine molluscs by Van Regteren Altena 1938-1950 and Schilder) Bibliography of Indonesia Geology . 4.(‘East Indies Lepidocyclinids’. etc. F.Radiolarians of the Celebes Sea. p. Mededelingen 12. (eds. (eds.Early Eocene Tethyan carbonate platform evolution. Sci. stratigraphic significance. not Oligocene as originally suggested by Martin (1934). & R. p. (1991).pdf) (Radiolarians generally rare in ODP Leg 124 sediments from Sulu Sea) Schilder. p. and Amphiperaidae).Zur Morphologie und Morphogenese der 'Lepidocyclinen'. ('Neogene Cypraeacea from East Java'. Paleontological paper describing dozen new 'species' and varieties of Lepidocyclina. collected by Fennema) Scherer. Results 124. 1. C. Speijer (2008). Descriptions of cowrie shells from Miocene of Lodan anticline.P. Rangin et al. Decline of coralgal reefs in low latitudes related to warming. 8. Leiden. Leidsche Geol. Gastropoda). R. Ranikothalia. W. collected during mapping by Bandung Geological survey) Schilder. F.J.(2) latest Paleocene: coralgal reefs dominant at middle paleolatitudes and larger foraminifera-dominated (Miscellanea. (1991). Reichsmus. (Celebes Sea ODP Sites 767 and 770 brown clays over basalt at both sites contain radiolarians of late M Eocene Podocyrtis chalara Zone.vangorselslist.1 161 www. p. p. (online at: http://www-odp. ('Molluscs from the post-Tertiary beds of Sulawesi'. Assilina) at low paleolatitudes. Obscure reference reporting presence of planktonic foraminifera Pulvinulina (=Globorotalia) menardii and Orbulina universa in asphalt-bearing rocks of Buton. Brill.Uber einige fossile Cypraea aus dem Sunda-Archipel. 1. p.) Proc. De Ingen.A. p. Sci.Neogene Cypraeacea aus Ost. Oligocene represented by Theocyrtis tuberosa and Dorcadospyris ateuchus zones. Gastropoda. (1941).) Scheffen. (1939). (Three stages in Late Paleocene. 4. 359-368. Silver. Ocean Drilling Program (ODP). R. (1932). Silver. ('On some fossil Cypraea from the Sunda Archipelago') Schilder. Zeitschrift 14. Neues Jahrbuch Min. Ocean Drilling Program (ODP). 71-102. Ser.A.M.Mollusken aus posttertiaren Schichten von Celebes.Java (Mollusca. Strassenbautechnik 32. Ed. 5. Cypraeidae. This clearly suggests M Miocene or younger age. C. Palaont.Der Boetonasphalt mit seine Foraminiferen. Asphalt und Teer.) Proc. etc. (1937). N9)) Schlumberger. 6.Note sur un Lepidocyclina nouveau de Borneo.pdf) (‘On the occurrence of Miogypsina and Lepidocyclina in Pliocene marls from the Bismarck Archipelago'. peripheroronda zone. epigona and M. Zool. p. France (3). and comparison with Baculogypsina sphaerulata.seals. kais. cushmani (~N8?) and M.1 162 www. Reichsanst. p. (1910). 1. 45-134. (1934). 9.at/pdf_frei_remote/AbhGeolBA_20_0001-0130. Verhandl. 1910. Verhandl. HvG)) Schubert. Reichsanstalt. 6.J.Note sur les genres Trillina et Linderina. p. 3. 22. Proc. Nederl. 250-253. globulina (N5-N7?). Lengguru foldbelt. (online at: http://www.W. 128-134. Lepidocyclina insulae natalis (probably E Miocene Euleidina. 318-328. Most of samples collected by Weber.-Indien). but are associated with younger deep water fauna. 295-298. kon. from S coast of Flores. a new species from Teweh. p. Geol. Soc. (1893). Akademie Wetenschappen B77. Vienna. New species of Miogypsina M. (online at: http://retro.J. 87-90. Sammlungen Geol.. (Three E-M Miocene miogypsinid species assemblages from same samples studied for lepidocyclinids and planktonics by Van der Vlerk and Postuma (1967): rel. (online at: http://www. (1900). Reichsanstalt. 20. SE Kalimantan) Schmid. 5.Miogypsinidae from East Java and Madura. (1902). C. Soc. 14.Note sur Lacazina wichmanni Schlumb. S Australia) Schlumberger.at/pdf_frei_remote/VerhGeolBundesanstalt_1910_0318-0328. ('Note on a new Lepidocyclina from Borneo'. Species also known from New Caledonia?.vangorselslist. R. E Java and stellate Lepidocyclina martini from Miocene of Madura. France 1896. Incl. p.at/pdf_frei_remote/VerhGeolBundesanstalt_1910_0395-0398.pdf) Bibliography of Indonesia Geology . Sammlungen Geol. Not very useful. common in Indian and Pacific Oceans) Schlumberger. R.) Schubert. Kon. France (3).Note sur le genre Tinoporus. 130p. Victoria. p. HvG).Truncatulina margaritifera granulosa Fischer) aus dem Pliocaen von Ceram (Niederl. p. upper Barito area. Kais. Reichs-Mus.Schipper.landesmuseum.ch/cntmng?type=pdf&rid=egh-001:1934:27::574&subp=hires) ('Biometric investigations on foraminifera (…) from the Pliocene of Seram'. Geol.Die fossilen Foraminiferen des Bismarckarchipels und einiger angrenzender Inseln. Ed. Kais. M. (First description of (Austro)Trillina howchini from Muddy Creek. Geol. Geol.com March 2014 .) Globorotalia tumida (Brady) und Truncatulina margaritifera Brady. (Description of Recent species Baculogypsina floresiana n. long-lived M. Kon. C. Bull. 395- 398. 4. antillea (Gr. (1910). 4.Biometrische Untersuchungen an Foraminiferen (Globorotalia menardii (d'Orb. Kon. laganiensis (These shallow marine larger forams look like M Miocene age.sp. ('Note on two species of Lepidocyclina from the Netherlands Indies'. & C. Listing of Pliocene deep marine smaller foraminifera from blueish marls of Torricelli Mountains.landesmuseum. (1911). C. Leiden (1). (1894). Bull. Vienna. (1896). collected by Verbeek) Schlumberger. 1910. 1. Vienna. R. C. p. C.J. (online at: http://www. Eclogae Geologicae Helvetiae 27. Geol. J. Drooger (1974). 22. Reichs-Mus.. Leiden (1).Uber das Vorkommen von Miogypsina und Lepidocyclina in pliocanenen Globigerinengesteinen des Bismarckarchipels. 118. K. Abhand. Mem. Soc. HvG) from Ngembak well.landesmuseum. new species Globigerina fistulosa (= Globigerinoides fistulosus)) Schubert. Lepidocyclina formosa (= Eulepidina.Uber Foraminiferen und einen Fischotolithen aus dem fossilen Globigerinenschlamm von Neu-Guinea.Note sur deux especes de Lepidocyclina des Indes Neerlandaises. (Lacazina wichmanni new species described from (Eocene) limestone from Triton Bay area.pdf) ('On foraminifera and a fish otolith from a fossil Globigerina marl of New Guinea'. Extensive measurements on selected planktonic and smaller benthic forams from ?Pliocene Fufa Beds foram marls from Wai Wahai hinterland of N Central Seram. collected by Wichmann. p. 1-14. Koolhoven 1929) Schlumberger. Andaman Sea. R. Kais.H.Nannofossil and planktic foraminiferal biostratigraphy around the Oligocene-Miocene boundary in parts of the Indo-Pacific region.J. Taxonomy updated by Srinivasan & Sharma (1980)) Schweitzer.1 163 www. Rieb (eds. 187-268. 1-66. C. Novara Expedition. Eight new Bibliography of Indonesia Geology . Two Tethyan molluscs species recorded for first time from Nanggulan.. p. (BMR) J.K. C. Drobne. (online at: www.vangorselslist. Jauhri. E Kalimantan (Dryobalanoxylon musperi. Ratanasthien & S. Indonesia.M Miocene limestones with larger foraminifera (incl. L. C. Less.pdf) (Based on study of Ashmore Reef 1 (Australia NW shelf). Foraminifera from North Arm and N part of East arm of Sulawesi. Geol. Feldmann & C. Bureau Mineral Res. Looks like typical Tethyan fauna) Scolari. a discussion on shared taxa. Hottinger. nummulitids and orthophragminids. Flosculinella n. etc.J. Nanggulan. Lepidocyclina) Schwager. C Java. Palaeontographica B 105. Banten). bangkoense. Goneplacoidea) from the Eocene of Java. 1-54. Java (Bogor. Stratigraphy 9.Pliocene Globigerina-rich pelagic sediments) Schubert.Hole 762C with ~240m of Eocene pelagic chalk off NW Australia: ~250 Eocene species. 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Geol. 30.g. collected by Brouwer) Tan Sin Hok (1927). Eucyrtidium (now Archaeodictyomitra) brouweri. A. 126.nl/DL/publications/PU00015375. Akademie Wetenschappen. calci and manganese peroxide spherulites.J.Coccolith biostratigraphy in Southeast Asia. p. drilled to 2630m. Sukiman. 5-165. Thesis University of Wales. 3. In: T.1 169 www. S (1977). 29-36. & F. Lelono (1994). (online at: http://www.Sur deux bois fossiles du gisement de la region Pachitan a Java. Bull.Zonasi polen Tersier Pulau Jawa. ('On two fossil woods from the deposits at Pacitan in Java'. 5. 1. Rahardjo. M Miocene (Lepidocyclina verbeeki. p. Nederl. Bioevents and Australasian microtektite impact event calibrated to oxygen isotope stratigraphy. Jurnal Tekn. (online at: http://naosite. Polhaupessy. p. 1. N. Comptes Rendus 102nd Congres Nat. Jasin & Haile 1996. (Seven calcareous nannofossil bioevents identified over past 2. S. K. (eds. T. Amsterdam. W Philippine Sea. Kobayashi et al. p. 17 of which are new) Takayama. Ed. Proc. Indon. South Sulawesi.A. E of Luzon. Akademie Wetenschappen. Tang (2011). Chinese Sci.36 Ma in two sediment cores from Benham Rise. With Shoreoxylon pachitanensis) Sun. Bibliography of Indonesia Geology . 197-209.) Geology and Palaeontology of Southeast Asia.nagasaki-u. p.Palynological study of the Burecing member. Roti.Biostratigrafi sumur pemboran CLS-X. Proc.On a young Tertiary limestone on the isle of Rotti with coccoliths. All radiolarian species described from marls on Roti believed to be of Late Tertiary age by TSH. Delft University.pdf) (Early description of Late Teriary calcareous nannofossils and radiolaria in pelagic limestone with radiolaria and small manganese nodules from S part of Roti island. Munasri 2013)) Tan Sin Hok (1927). Palaeont. . A.T. Ph. Trans. 29.vangorselslist.knaw. etc.87. Wiyono. Jatibarang'.com March 2014 . ('Biostratigraphy of well CLS-X.pdf) (Palynology study of 48 palynomorph types in M Eocene lignite at Nanggulan.dwc.D. H. Pioneering study of radiolarians and calcareous nannoplankton from deep water sediments of Timor. Yu.D. R. Media Teknik 12. (2001). X. 23rd Ann. ('Tertiary pollen zonation of Java') Takahashi. Coccolithinae and Radiolaria. 180-184.On the genus Cycloclypeus Carpenter. Mijnbouw en Geologie). 1-194. 12. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. including new Late Pliocene species of Discoaster: D. boetonensis from Eocene(?) of Buton) Bibliography of Indonesia Geology . Java.1 170 www. ('Two new microspheric Lepidocyclinas from Java'. Vlerk.Recent Cycloclypeus in West Java) Tan Sin Hok (1934)..nl/DL/publications/PU00015461. a new Polylepidina from Central Borneo. De Ingen. (B) omphalus. De Mijningenieur 11. 144-146. (eds. Larger foram Spiroclypeus evolved from Heterostegina in middle part of Tertiary e= Late Oligocene) Tan Sin Hok (1930). Possibly close to Lep. pentaradiatus. D. Tegal (Mittel-Java) und Benkoelen (Sud-Sumatra).Uber Lepidocyclina gigantea Martin von Sud-Priangan (West-Java). 19. De Ingen.Lepidocyclina zeylmansi n. 92-114.-lndie (IV). p. assigned to Lepidocyclina papulifera Douville) Tan Sin Hok (1935).knaw.Recent. 2. Reported in more detail in 1932)) Tan Sin Hok (1931). S. p. De Ingen.Over Spiroclypeus met opmerkingen over zijn stratigraphische verspreiding.sp. a stellate form from W Java) Tan Sin Hok (1935). De Mijningenieur 11.-Indie (IV). 1. Large microspheric Lepidocyclina from Lusi River near Ngampel. De Ingen. ('On microspheric Lepidocyclinas from Ngampel (Rembang. in Nederl. De Ingen. C Java)'. Mededelingen 5.- Indie (IV. p. etc. Larger foram genus known from Early Oligocene. Escher et al. brouweri. Bantam.Discoasteridae.pdf) (First publication on 'aragonite stars' (calcareous nannofossils/coccoliths) from E Indonesia.d. Tan Sin Hok (1930).Die peri-embryonalen Aquatorialkammern bei einigen Orbitoiden. Part 1 and an appendix on the Heterostegines of Tjimanggoe.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. Lep. D. nebst Bemerkungen uber die verschiedenen Entstehungsweisen der Lepidocyclinen.collected by Ter Haar.). 5.-Indie (IV).. 3. ('On Spiroclypeus and its stratigraphic distribution'. C. in Nederl. (Listings of calcareous nannoplanton and radiolaria species reported by 1931 from Indonesia) Tan Sin Hok (1932). 2. Java. (General discussion of initial chamber morphologies in Cretaceous and Tertiary orbitoidal foraminifera) Tan Sin Hok (1936). p. collected by Bothe and Lep. 233-242. 7-14. 1.G. 12. p. Martin. molengraaffi. 2-3-211. Leidsche Geol.Over Cycloclypeus: voorlopige resultaten eener biostratigraphische studie. ('On Cycloclypeus: preliminary results of a biostratigraphic study'.sp. Two M-L Miocene new species described. 113-126. 12. In: B.(online at: http://www. in Nederl. Large microspheric Lepidocyclinids) Tan Sin Hok (1935).com March 2014 . p. Tegal (C Java) and Bengkulu (S Sumatra)'. This most evolved Lepidocyclina subgenus regarded by Van der Vlerk as limited to upper Tertiary f. Feestbundel K. Ed. in Nederl. p. Indie. but questioned by TSH) Tan Sin Hok (1930).vangorselslist. 2. p. tributary of Mahakam River. New. p.Enkele opmerkingen over de stratigraphische verspreiding van Trybliolepidina v. ('Some remarks on the stratigraphic distibution of Trybliolepidina'. ('On Leidocyclina gigantea Martin from S Priangan (W Java). in Nederl.with remarks on the various origins of the Lepidocyclinids'. 2. 9. eine neue Polylepidina von Zentral Borneo. primitive species of Lepidocyclina from Eocene in Tjihan River. (Classic paper on evolution and species of Early Oligocene. ('Lepidocyclina zeylmansi n. 1. 1-8. De Mijningenieur 11. (B) stratifera from Pasean village. Mitteljava).Uber mikrosphare Lepidocyclinen von Ngampel (Rembang.-Indie (IV). 9-18. C Kalimantan.dwc.Zwei neue mikrosphare Lepidocyclinen von Java. p. ecuadorensis. (‘Remarks on Cycloclypeus from Sipura.On the genus Spiroclypeus Douville with a description of the Eocene Spiroclypeus vermicularis nov. 6. 3. p. bifida) Tan Sin Hok (1936). Natuurk. De Ingen. sp. with remarks on various classifications of the lepidocyclinids’.Zur Kenntnis der Lepidocycliniden. p. 5. M. 3.-lndie (IV). 35-45. E Borneo) Tan Sin Hok (1936). Akademie Wetenschappen 39. 7-15. 235-280.Second continuation and end'.II'. here reclassified as subspecies of M.vangorselslist. p. complanata.Beitrag zur Kenntnis der Lepidocycliniden. 9. p. a polylepinid orbitoid from Central Borneo. p. p. De Ingen. Miolepidocyclina excentrica n. 3. 4. in Nederl.-lndie (IV). ('Further investigations on the Miogypsinids.Lepidocyclina zeijlmansi nov. Proc.. Geologie en Mijnbouw 15. Discussion of more 'obscure' Miogypsian species and details of chamber patterns and stolons) Tan Sin Hok (1936). p.-lndie (IV). De Ingen. 4. ('On the knowledge of the Miogypsinids. 3. 4.-lndie (IV). 109-123. II Fortzetsung und Schlusz.Weitere Untersuchungen uber die Miogypsiniden I. 45-61. 7. in Nederl. Nederl.com March 2014 . (First Polylepidina-type Lepidocyclina from the Indo-Pacific.Zur Kenntnis der Miogypsiniden. De Ingen.-Indie (IV). I Fortzetsung. 3. ('Further investigations on the Miogypsinids.1 171 www. 3. De Ingen.Tan Sin Hok (1936).Bemerkungen uber die Cycloclypeen von Sipoera (Mentawai-Inseln).Zur Kenntnis der Miogypsiniden. 57-58. p. Five types/ stages: M. De Ingen. in Nederl. Tan Sin Hok (1937). p. First (and only?) record of Eocene lepidocyclinid from Indonesia) Tan Sin Hok (1936). 87-111. (Mainly a critical review of Barker & Grimsdale 1936 paper on American lepidocyclinids. in Nederl. p. sp. 5. ('On the different paleontological criteria for the subdivision of the Tertiary') Tan Sin Hok (1937). M.Over verschillende paleontologische criteria voor de geleding van het Tertiair.Weitere Untersuchungen uber die Miogypsiniden II. No illustrations) Tan Sin Hok (1936).-Indie (IV). 4. from Madura) Tan Sin Hok (1937). Mentawai Islands’) Tan Sin Hok (1936). Ed. in Nederl.First continuation'. from Koetai in East Borneo. 177-193.-lndie ( IV) 3. No figures or data) Tan Sin Hok (1936). indonesiensis and M. cushmani) Tan Sin Hok (1937). De Ingen. Discussion of growth patterns of miogypsinid and other larger forams and remarks on stratigraphic distribution and interregional correlations. in Nederl. De Ingen. in Nederl. eine polylepidine Orbitoide von Zentral Borneo.Zur Kenntnis der Miogypsiniden. Mainly on Miogypsina indonesiensis group.-lndie (IV). Bibliography of Indonesia Geology . in Nederl. 84-98. Tijdschr. from tributary of Mahakam River.sp. Nederl. Miogypsinids probably evolved from Rotalia. ('Lepidocyclina zeylmansi. 8. p. First of series of five papers on miogypsinid evolution and species in Indonesia. De Ingen. (‘On the knowledge of Miogypsinids’. (online at website Koninklijk Instituut voor de Tropen ) ('On the knowledge of the Miogypsinids.Note on Miogypsina kotoi Hanzawa.-Indie 96. 1. (Discussion of value of various larger foram genera for biostratigraphic subdivision of the Tertiary) Tan Sin Hok (1936).I'. M. 2. p. nebst Bemerkungen uber die verschiedenen Einteilungsweisen der Lepidocyclinen.Over verschillende paleontologische criteria voor de geleding van het Tertiair. 3. 173-179.-lndie (IV). Kon. borneensis. 10. 3-32. 3. in Nederl. in Nederl. lndie (IV). 173-179. 990-999. p. De Ingen. 585-586.E. 1-70.nl/DL/publications/PU00016907. 93-97. Acad. 428-440.com March 2014 .sponge symbiosis from the Lower Miocene of Indonesia') Tesch. 294. 5.Note on the occurrence of Miogypsinoides Yabe and Hanzawa in Oligocene deposits.ch/cntmng?type=pdf&rid=egh-001:1934:27::628&subp=hires) Bibliography of Indonesia Geology .F. Continuation of above monograph.. 2. Kon. 7. J.I.vangorselslist. Faunas dominated by gastropods.knaw. Molengraaf 1909. Ed. nov. p.Tertiary foraminifera from Borneo.go. In: J. off W Sumatra. Poignant (1982).Jungtertiare und quartare Mollusken von Timor. in Nederl.part 2’. P. Nephrolepidina spp.dwc. (Brief paper with comments on larger foram 'letter zonation'. In: J.(Review of larger foram genus Spiroclypeus. Nummulites). (1933).. 1911 expeditions. (online at: http://retro. species 114- 233. 113 species.jp/article/pjab1912/19/9/19_9_585/_pdf) (During exploration in 1942 of Cimandiri coalfield. 5. On p.-lndie (IV). 6. (1899). p. New name Rotalia trispinosa for Rotalia pulchella. 661-670. 179: mention of Biplanispira in Wani series of Buton) Tan Sin Hok (1939). Eclogae Geologicae Helvetiae 27. a sample was collected N of mouth of Tjibeuleungbeung that contains both Camerina fichteli. Imp. Nat. (online at: http://www. p.Uber Tertiare Foraminiferengesteine von Sipoera (Mentawei-Inseln). Miogypsinoides appears in Late Oligocene.) Palaeontologie von Timor 8. H. nov. Late Pliocene. trispinosa nom. Ann. described by Brady (1884) from Bangka Straits) Thalmann. 349-353.. accompanied by isolepidine- nephrolepidine and eulepidine Lepidocyclines.E. Larger foraminifera in M Eocene black limestone (zone Ta with Assilina. 41-121. etc. Hist. no map) Tesch. (Brief general review) Tan Sin Hok (1939).) Palaeontologie von Timor 5.E. p. Termier G. in Nederl. Proc.Jungtertiare und quartare Mollusken von Timor-II. 14. Miogypsina. and a Miogypsinoides sp. D. With table listing localities. 248-251. W Java. p. This demonstrates that Miogypsinoides made its appearance in Oligocene time (Td)) Tappenbeck.- lndie (IV). Mag. Proc.Remarks on the “Letter classification” of the East Indian Tertiary. und R. Schweizerbart. 9.Early Pleistocene and Pleistocene) Thalmann. 98-101. D. & A. 2. Amsterdam 39.) Tan Sin Hok (1943). (1920). (online at: http://retro. De Ingen. Acad. Mainly taxonomic descriptions of mollusks collected by Wanner.part 1'. p. Early Miocene (zone Te with Spiroclypeus. p. Eclogae Geologicae Helvetiae 26. ('Late Tertiary and Quaternary molluscs from Timor.The results of phylomorphogenetic studies of some larger foraminifera (a review). 7.Une symbiose algue rouge-spongiare dans le Miocene inferieur de l'Indonesie. 7. (‘Late Tertiary and Quaternary molluscs from Timor.jst.Mitteilungen uber Foraminiferen I. In stratigraphic conclusions samples grouped in 3 categories: Late Miocene?-Early Pliocene. ser. guembelianus) marl and limestones) Tenison Woods. Akad Wetensch.1 172 www. 6. 245-264.Zwei neue Vertreter der Foraminiferen-Gattung Rotalia Lamarck 1804: R. Paris. trispinosa'.ch/cntmng?type=pdf&rid=egh-001:1933:26::270&subp=hires) ('Two new representatives of the genus Rotalia Lamarck: R. Abh. p.seals. (1934). p. 2. (online at: www. (1916). Wanner (ed.seals. Stuttgart. 9. p. Stratigraphic range Late Oligocene. Nederl. Wanner (ed. 17 new.jstage. cubana new name and R. Tokyo 19. (1936). cubana nom. H. Sci.). De Ingen. 3. Short paper. and Late Miocene (Tf with Pliolepidina and Cycloclypeus cf.pdf) ('On Tertiary foraminifera rocks from Sipura (Mentawai Islands)'. ('A red algae.E Miocene (zone Te) and also in Late Eocene (Tb). Compte Rendu Hebd. ser. P. . H.ch/cntmng?type=pdf&rid=egh-001:1937:30::563&subp=hires) ('Communications on foraminifera.. 5. H. p. p. Soc. Known only from E half of East Indies Archipelago: E Sulawesi (Boealemo peninsula). from Late Tertiary and E Quaternary of N Java) Thalmann. Geol. p. 1927 ex Tan Sin Hok.uu.('Communications on foraminifera. 5. Discocyclina and Alveolina. 3. 2. 57. 333-337. S. 57. Utrecht Micropal. Soc.E. (INA) Newsl. H. and Seram island) Thalmann. Helvetiae 31. Brief. Includes chapter 8. (Incl.nl/handle/1874/205891) (Miocene nannofossil zonation. Mainly a brief review in the importance of work by Tan Sin Hok (1932-1937) on the 'morphogenetic' evolution of Cenozoic larger foraminifera Lepidocyclina.) ('Communications on foraminifera. 12. p. Miogypsina. E Java. Geol. (1942). Spiroclypeus. p. (Occurrence of Late Eocene planktonic foram marker genus Hantkenina in Sangkulirang and Tanjung Selor regions.Occurrence of the genus Lacazina Munier-Chalmas in the East Indies. Nannoplankton Assoc.E. W Papua (Pisang Island E of Misool.org/JNR/NINA/INANewsl5(1).seals. H. Kai Besar Island (between Riamroe and Yamtimur) Thalmann.III'. and 4 on two new species from the Plio-Pleistocene of Java. 1-271. Birds Head between Rumberpon and Horna.library. description of Pseudorotalia indopacifica n. assigned to 'subgenera' Eu-Discoaster and Helio-Discoaster) Theodoridis.pdf) (Commonly used genus name Discoaster is technically invalid because at the time of first description no type species was designated (instead spp. America Bull. 15-21.seals. 1838-1839. 1931.E.Wert und Bedeutung morphogenetischer Untersuchungen an Gross-Foraminiferen fur die Stratigraphie. S and E of Paniai Lake).On the legitimacy of the generic name Discoaster Tan Sin Hok.Mitteilungen uber Foraminiferen III. (online at: http://ina. etc. (1946). p. Onin Island. early review of Miocene. 2. Includes chapters 1 on Rotalia gaimardi. (Abstract only) (Eocene limestones with larger foram Lacazina (= Lacazinella) often associated with Nummulites. 12. 53. 2. 5-24. 12.ch/digbib/. (1942). Stanford Univ. Rotalia catilliformis and Rotalia alveiformis) Thalmann. 592-606. Nothing on SE Asia) Thalmann. Long Iram area). (1946). 1946)) Theodoridis. 2 on Rotalia conoides from Cepu area.E. E Kalimantan) Thalmann. on Wilhelmina Peak of Central Range. Dramai Island. (1984). p. Eclogae Geologicae Helvetiae 28.New occurrences of the foraminiferal genus Hantkenina in Europe and Asia. 337-356. (online at: http://retro.ch/digbib/view?pid=egh-001:1938:31::352) ('Value and meaning of morphogenetic investigations on larger foraminifera for stratigraphy'. H. S and E of Triton Bay. PNG (Chimu aerodrome). (1935).Hantkenina in the Eocene of East Borneo.New occurrences of the foraminiferal genus Hantkenina in Europe and Asia. Cape Pasanea. p. Ed. presence of Eocene planktonic foram genus Hantkenina in E Kalimantan (many localities along upper reaches and tributaries of Mahakam River. partly based on Miocene material of Solo River section.II'.vangorselslist. H.I'.seals.tmsoc. (online at: http://dspace. Int. (1937). (1938). Sci. (1983). Geol. America (GSA) Bull. S. Cycloclypeus. p. Geol. Setawka River in SW New Guinea.E. America (GSA) Bull.Calcareous nannofossil biozonation of the Miocene and revision of the Helicoliths and Discoasters. (Meeting abstract only) (Incl. and C Seram (Wai Tali. Returns to emended definitions of Helio-discoaster Tan and Eu-discoaster Tan for Discoaster species) Bibliography of Indonesia Geology . Germeraad. Eclogae Geologicae Helvetiae 30. E Java. 1.E. Kendeng zone. 2. presence of Eocene planktonic foram genus Hantkenina in E Borneo. 32. 1236-1237. (online at: http://retro.Pleistocene Pseudorotalia species from Indonesia.Mitteilungen uber Foraminiferen II. and Sungei Ingsiim. Bull.sp. Abstract. (online at: http://retro. H.1 173 www. 2.E. Eclogae Geol. from Indonesia) Thalmann. 1236-1237. Publ. Soc.com March 2014 . Eclogae Geologicae Helvetiae 20. Recent foram faunas dominated by Indo-Pacific reef genera Calcarina. Ammonia.Recent smaller foraminifera from Guam. collected by Buxtorf. 9. 87-102. A. H.S.pdf) (Descriptions of planktonic and smaller benthic foraminifera from Late Eocene (172 species).usgs. Ujie. first description of Schlumbergerella neotetraeda in Quaternary? limestones) Tobler. Nat. 323-330.Restudy of Japanese Miogypsinids. U. (below 179'). A. 99-114. (online at: http://retro. Incl. Survey Prof. ('Calcification of the lateral chambers in Miogypsina'. Part 2. Austrotrillina striata n. Brief paper on occurrence of Miogypsina with Spiroclypeus in Tabalong section. H. 547-568. Paleontology. R. (Descriptions of marine benthic forams from Middle Miocene Sandakan Fm.gov/pp/0260m/report. A. No stratigraphy or biozonations) Bibliography of Indonesia Geology . ('Notes on some foraminifera-bearing rocks from the Sanggar Peninsula (Sumbawa)'. Larger foram Meandropsina from marly limestone of Samui near Balikpapan. p.Miocene foraminiferal faunas from the Sandakan Formation.pdf) (Eocene. 113-141. p. 2. Geol. HvG)) Tobler. >4500m thick clastic series.Tobler. 16. abunensis) Todd. Survey Prof. E Kalimantan. Bull. Nat. (1970). 413-430. 5.Recent smaller foram faunas from Bikini Atoll dominated by miliolids and peneroplids. Geol. 115-136'.com March 2014 . Gyroidina. p.ch/digbib/view?pid=egh-001:1925-1926:19::729) (’Miogypsina in the basal Neogene of Trinidad and East Borneo’. p. sp. mostly barren. 3 samples with middle Miocene planktonic forams (Gr.“Evolutionary line” of Miocene Miogypsinid populations. p. (Sandakan Fm on Sandakan Peninsula.Verkalkung der Lateralkammern bei Miogypsina. Upper 95' of wells dominated by Calcarina spengleri (reef deposition). Late Oligocene (61 species) E-M Miocene (161 species) sediments. etc. Mus. (1927). from donated collection in Basel. Survey Prof.Geology of Saipan. 3. Paper.S. 280-H. 260-N.New species and subspecies of benthonic foraminifera from the Miocene Sandakan Formation. p. Sci. (1927). Pseudorotalia borneensis. new species Miogypsina tuberosa. (online at: http://pubs. (1926). New species of Bolivina. (1977). NE Sabah. In: Geology and Palaeontology. & R. Paper 403-I. 2. Appendix in Pannekoek van Rheden (1918)-paper. University of Tokyo Press. Bull. H. Baculogypsina and also Marginopora) Todd. Post (1954). (1966). Rotalia calcar and Calcarina delicata n. 3. 265-320.1 174 www.gov/pp/0403i/report.Miogypsina im untersten Neogen von Trinitad und Ost Borneo. U. M. (’Meandropsina in the Tertiary of East Borneo’.sp. Papers.seals.vangorselslist. 165-185. 189-192. (1957). (1973).pdf) (Miocene. p.S. U. p.Distribution of the Japanese Miogypsina with description of new species. Geol. Mus.usgs. Sci. (1918). May be Pseudotaberina (Meandropsina is Upper Cretaceous genus. R.Smaller foraminifera from Bikini drill holes.Maeandropsina im Tertiar von Ostborneo. Eclogae Geologicae Helvetiae 20. hispida. 321-323.Smaller foraminifera from Guam. Part 3. Deeper also C. Assigned to Zone Tertiary 3y of Van der Vlerk. Ujie. North Borneo. p. Baculogypsina sphaerulata (reef. Mariana Islands. Tokyo. see also Cole 1966) Todd. E Kalimantan.Notiz uber einige foraminiferenfuhrende gesteine von der Halbinsel Sanggar (Soembawa).usgs. University of Tokyo Press. 1. Smaller foraminifera. Southeast Asia 18. (online at: http://pubs. Incl. Not much new) Tobler. p. p. 719-721. Ed. In: Geology and Palaeontology of Southeast Asia 8. A. Eclogae Geologicae Helvetiae 19. (1966). (online at: http://pubs. Zeitschrift Vulkanologie 4. fohsi zone)) Ujie.gov/pp/0280e-j/report. H. North Borneo. R.) Ujie. Hotz (eds. Wetenschappelijke Mededeelingen 10. 82-89. Tokyo Press. vol. Philippines. SE Kalimantan. (1928).H. S Sumatra. SE Borneo) Umbgrove. J.vangorselslist. In: Geology and Paleontology of Southeast Asia. (Planktonic foraminifera spanning zones upper N17-lower N21 in Opol Fm of N Mindanao) Umbgrove. p. Martin. (1930). H. Leidsche Geol. p.F. Pasir.nl/document/549462) (Biplanispira absurda n. (New species of Lepidocyclina from marly limestone in Ayer Laje. In: B.Pliocene Menkrawit. Embryon advanced nephrolepidine to trybliolepidine.Heterospira: a new foraminiferal genus from the Tertiary of Borneo.Tertiary sea connections between Europe and the Indo-Pacific area. 5. (1931). Dienst Mijnbouw Nederl.1 175 www. p. (Describing difficulties in Indonesia. 45-76.repository.H. Indie. J.H.A second species of Biplanispira from the Eocene of Borneo. Wetenschappelijke Mededeelingen. 1-22.sp. J. p. J.F. p.F. J.Neogene en Pleistoceene koralen van Sumatra. Fourth Pacific Science Congress. 91-104.) Geological. n. 2nd ser.H. J. 155-157. p. p.naturalis.F.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. 13. Antjang and Domaring beds.Europe biostratigraphic correlations due to faunal provincialism) Umbgrove. Proc. Mededelingen 8. gen.Het genus Pellatispira in het Indo-Pacifische gebied. Java 1929. Indie 5. van Sumatra. a few km S of Bataraja. J. Tanah Bumbu. spec. 28-41.sp. (1938). 129-144. (online at: http://www. p. Middle-Late Miocene age) Umbgrove.H. p. p. 25 species identified.H.Tertiary foraminifera. Wetenschappelijke Mededeelingen. Escher et al. nov. from Eocene of Sungei Sangajam. Palaeontology. 25. Mededelingen 10. petrographical and palaeontological results of explorations.repository. (?Middle Miocene ‘Upper Tf’ larger foraminifera from Bebulu River.F. Leidsche Geol. (1936). (online at: http://www.F.H. Pasir (Zuid Oost Borneo). Univ.. Mededelingen 5. Low diversity coral assemblages from Late Miocene. Dienst Mijnbouw Nederl. (1926).F. Dienst Mijnbouw Nederl. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. about 80 Recent species. S Palembang.55. J. (1924). probably all Late Pliocene or younger age) Umbgrove.H. 109-113. 32.Ujie. Probabbly Upper Tf. Rutten & W.Upper Miocene planktonic foraminiferal faunas Northern Mindanao.F. collected by Leupold in NE Kalimantan) Umbgrove. five of which new) Umbgrove. (Corals collected by Rutten from 13 localities in C and E Seram.H. Genus later renamed Biplanispira) Umbgrove. 36-91.com March 2014 .naturalis.Anthozoa van Noord-Oost Borneo. Seven species.. Descriptions of Miocene-Pleistocene corals from N Aceh.F. p. from several localities in E Kalimantan. IIA. J. Leidsche Geol. (eds.Report on Pleistocene and Pliocene corals from Ceram. (1927). Indie 9. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl.G. (Review of Late Eocene (Ta-Tb) larger foram genus Pellatispira in Indo-Pacific area. collected by 'Mijnbouw' and from other N Sumatra localities collected by Tobler) Umbgrove.-Indie 4.Pliocene. listing foraminifera species reported from Tertiary of Indonesia) Umbgrove.43-71. In: L. carried out from September 1917 till June 1919 in the island of Ceram. & T. (‘Neogene and Pleistocene corals from Sumatra’.Lepidocyclina transiens. (1929). Ed.Neogene foraminiferen van de Soengei Beboeloe.nl/document/549681) (Description of Late Eocene larger foram Heterospira mirabilis n. J. (Chapter in Martin memorial volume. Samata (1973). Feestbundel K.F. Considered to be are aberrant specimens of Pellatispira madaraszi or Pellatispira mirabilis by Cole (1970)) Bibliography of Indonesia Geology . with double arrangement of chambers on both sides of a median plane. ('Anthozoans from NE Borneo'.H. (1929).-Indie 9. Miocene corals from Flores (East-Indies). Stephanotrochus. 729-778. Amsterdam. Soc. (online at: http://www. (Small hill of Gunung Linggapadang near Prupuk. p. Kon.H. incl. Akademie Wetenschappen. (online at: http://www.nl/document/549525) (Pliocene corals from Buton asphalt deposits at Waisiu.H. 20.repository.F. collected by members of Geological Survey) Umbgrove.com March 2014 .F. 8. Meded. Geol.H. 47% still living. as demonstrated by their steep Bibliography of Indonesia Geology . p. Amer. Verhandelingen Geol. 14-16. Reef comparable to patch reefs in Bay of Jakarta.Corals from asphalt deposits of the Island Buton (East-Indies). 62- 67.H. Ed. p. collected by Kuenen.nl/DL/publications/PU00018197. (1947). J. 521-542. (1945). (Review of investigations on coral reefs in E Indies in last 15 years before WWII. Leiden.naturalis.Corals from the Upper Kalibeng beds (Upper Pliocene) of Java. 340-344.repository.1 176 www. 9 species. p.Umbgrove.Corals from an elevated marl of Talaud (East Indies). Ser..) 5.F.repository. (1946). Extreme thickness of some reefs. Progyrosmilia vacua. Platygyra and Porites Also illustration of fossil coconut) Umbgrove. (Geol. (online at: http://www..Coral reefs of the East Indies.nl/document/150648) (Corals collected by Kuenen during Snellius expedition from marine marl near Mahammale. p. Hydnophyllia.Holocene age) Umbgrove. 263-274. Proc. Leidsche Geol.15 could be identified. America Bull.naturalis. incl. J. J.knaw.F. Mijnbouwk. J.nl/document/549421) (Corals from limestone at N coast of Flores near Papang. p.F. 393-398. 49. so young. 29-37. 15 species. p. Goniopora planulata) Umbgrove. Paleontology 20. 48. C Java. (1946). (1939). J. 23-31. E Java. p.H. Kon.F. Amsterdam. Cyphastrea. (1946). Well preserved.F. Favia. (1938). Phyllangia. (online at: http://www. Every atoll and barrier reef studied shows evidence of subsidence. J. 87-93. Percentage suggests Cisande limestone older than coral-bearing localities in Pliocene Sonde beds (Th). 8 of which still living species. Geol. Leidsche Geol.dwc. Akademie Wetenschappen. Gen. Mededelingen 11. 58.dwc. J. Geologie en Mijnbouw (N.F.H.Corals from a Lower Pliocene patch reef in Central Java.H.) 13. J. Caryophyllia.H. Leptoseris. Well. Proc. 6. (Percentage-of-living-species figures useful for stratigraphic dating and correlation) Umbgrove.Evolution of reef corals in the East Indies since Miocene time. (1946). p. Nederl. probably Miocene age. Zoolog.H.S. Goniastrea. 5. 1.naturalis. (1943). Talaud Island.H. (online at: http://www. p.F. Java. 1. C Java. 30. Coeloria. maybe around Mio-Pliocene boundary) Umbgrove. Assoc. J. N of Lurahgung. Fungophyllia spp. (Miocene and Eocene corals (mainly solitary species.Tertiary corals from Sumba (East Indies).preserved coral fauna of 70 species) Umbgrove.vangorselslist. Cyphastrea monticulifera. 9 species. Goniastrea.knaw. Mededelingen 13. Associated with Aceratherium boschi rhinoceros tooth (oldest land mammal fossil known from Java). Umbgrove. Nederl. Diploastaea) from Witkamp collection from W Sumba) Umbgrove. J. 1. J. is Lower Pliocene patch reef in marly Tapak Beds.pdf) (35 coral species from Late Pliocene Upper Kalibeng Beds at Sonde in W part Kendeng zone. Petrol. probably Pleistocene.F.Corals from the Upper Miocene of Tjisande. Twnenty-one coral species.pdf) (Reefal limestone lenses in U Halang Beds along Cisande River.nl/DL/publications/PU00017948. all still living. (1942).A revision of fossil corals from Celebes described by Dollfus. sp. Schreurs (1996). Van Andel. J. J. Indon.1 177 www. Klaten. 503-504. SE of Rembang. with only 50% living species. Bayat.Corals from the Putjangan beds (Lower Pleistocene) of Java. p. S.sp.). Proc. collected by Wanner. 760-765. and Nummulites perforatus de Montf. Geol.Wungkal. 51. This abnormally low percentage probably due to special character of fauna which consists mainly of solitary 'deep water' corals) Umbgrove.pdf) (Lepidocyclinids from Early Miocene 'orbitoidal limestone (OK)' of Rembang Beds near Sumberan. B. Assoc. Geol. 20. N. offshore Sabah. Bandar Seri Begawan. 5.naturalis.. and Spiroclypeus vermicularis) Umiyatun Choiria. In: S. R.) The geology and hydrocarbon resources of Negara Brunei Darussalam (2nd ed. Pellatispira orbitoidea. 1-11. Amsterdam. wanneri n. 5- 14. (Umbgrove objects to use of 'East Indies Letter Classification' without proper referencing. p. Elbert and Selenka and Bandung Geological Survey. Assilina spp. Bayat Klaten.Notes on freshwater Mollusca from the Malay Archipelago. Java'.dwc. pengaronensis. Kon. cannot be explained by glacial control only. M-U Eocene (zone Ta3) larger forams from classic Jiwo Hills locality include Nummulites javanus. Nummulites javanus (Verbeek) considered to be younger synonym of N. Nederl. Akademie Wetenschappen. p. H.nl/document/149951) (Monograph of fresh water molluscs from collections of Dubois. Proc. (1948). C.The claystone age of Wungkal Formation based on calcareous nannofossils in Gunung Pendul area.. Proc.E.knaw. Koopman & A. p. T. Proc. T. Muzium Brunei and Brunei Shell Petroleum Company Berhad. 1013-1023. (1931). Setiawan (2001).nl/DL/publications/PU00018695. Prastistho. Ed.. 8. Publ.T. E Java. p. Spec. mainly subgenus Nephrolepidina. Sekarbolo. (Forty species of corals from lower Pleistocene Pucangan beds of Kendeng zone. (IAGI).Some remarks on Nummulites javanus Verb. W Timor. (online at : http://www.Sandal (ed. (Includes review of biostratigraphy in Brunei region (p.Foraminifera besar pada satuan batugamping Formasi Gamping.K. p.dwc. perforatus) Van Benthem Jutting. Conv. Assoc. Paleontology 24. Indon..repository.J. N. L. No data) Umiyatun Choiria. American Assoc. introduced for specimens with multilepidine embryon) Van den Brink. 637-651.H. 34th Ann. Yogyakarta. Prevailing wind and wave action are important influence on upper structure of reefs. 81-128.H. Additional examples of currents as factors of morphological importance) Umbgrove. Pekanbaru. Zool. Syabas.knaw. Molluscs from same samples described by Wanner & Hahn (1935). Bayat. Akademie Wetenschappen 52.Neogene dinoflagellate cysts from a deep water well. & J. Mtg.Stratigraphy.Tertiary stratigraphy of the Far East. (1937). 81-96)) Van den Abeele. (IAGI) and 10th GEOSEA Conv. (1949). American J. (online at: http://www. a protest. (1954). 6. Discocyclina spp. Bringin and Gegunung oilfield. Palynologists. p.Non marine mollusca from fossil horizons in Java with special reference to the Trinil Fauna. Kon. (Abstract only) Bibliography of Indonesia Geology . collected by Tappenbeck. some Multilepidina.nl/DL/publications/PU00018566. Ann.Conv. Lepidocyclina wanneri n. 83-180. Nederl. Jawa Tengah. p. Van Benthem Jutting. mainly from Latest Pliocene-Pleistocene of Kendeng zone/ Trinil area) Van Borren. northern Borneo. (online at http://www. Proc. Meded.Lepidocyclininae from Rembang (Java) with a description of L. djokdjakartae. Science 252. J.pdf) (Study of Nummulites perforatus from Mollo.vangorselslist. Treubia 13. 30th Ann. (2002). Seven Lepidocyclina species. Jiwo Barat. Central Java.F. W Jiwo. T. 278-279.Wungkal Fm. (1950). A.com March 2014 . ('Larger foraminifera from limestones of the Gamping. p.F. Jati Kurniawan & Surono (2006). 7. S. Strat. D. p.submarine slopes. PIT IAGI2006-072. 5. J.Recent in deep-water wells off Sabah and Brunei. No location map.W.nl/DL/publications/PU00017817. ('A new Cycloclypeus species from East Borneo'. W. incl. de Vletter (1942). Little stratigraphic info..ch/cntmng?type=pdf&rid=egh-001:1923-1924:18::764&subp=hires) (New miogypsinid larger foram species from Larat. C Java.nl/document/45042) (Listing and re-descriptions of Tertiary mollusk type specimens in K. Geol. Contains 5700 type specimens of 912 species) Van der Kaars. C.pdf) (Palynological study of ODP Site 767 in Celebes Sea indicates presence of extensive wetlands in area in Middle and Late Miocene. Nederl. (Looks like mainly M Miocene. so should be assigned to genus Miogypsinoides) Bibliography of Indonesia Geology . Akademie Wetenschappen 45. Lepidocyclina spp. HvG)) Van der Vlerk. & D. Alveolinella. etc. I. Sample from Gunung Mlendong near Kari Orang. Dinoflagellate cyst assemblages similar to open oceanic assemblages from E Indian Ocean and NE Australian margin) Van den Hoek Ostende. which looks like and is associated with C. I. (eds.Een nieuwe Cycloclypeus soort van Oost-Borneo. Leloux. With locality map.Miogypsina Dehaartii nov. Natuurhist.seals. 429-431. 5. Martin collection at Naturalis Museum. Ser. acritarchs. Nat.dwc. Silver et al. At start of Late Pleistocene montane vegetation expanded.-Mijnbouwkundig Genootschap Nederland Kol.M. Samples collected by Rutten in SW corner of 109-Lamongan map sheet.knaw. Winkler Prins (2002).A. Description of new genus and species Orthocyclina soeroeanensis from Kali Soeroean. collected by BPM geologist De Haart. Looks like an advanced M-L Miocene radiate Lepidocyclina (Trybliolepidina). Palynological assemblages dominated by land plant material. 3.) Van der Vlerk. Geol. (Online at http://www. I.1 178 www.P.. 137-140. Bagelen area. Proc. Cycloclypeus (incl. No lateral chambers. mainly from Java. Ed.repository.) Proc. (1923). 5. p.com March 2014 . spec. etc.Young Tertiary smaller foraminifera from the neighbourhood of Ngimbang. Kon. With discussions on Indonesia larger foram species and distribution.. Sammlungen Geol. Ocean Drilling Program (ODP). National Museum of Natural History. p. Mus. Bull. No locality info. Results 124. (online at: http://www-odp. equivalent of Wonosari Lst of South Java. annulatus with concentric rings. In: E.F.Een overgangsvorm tusschen Orthophragmina en Lepidocyclina uit het Tertair van Java.sp. F. Their occurrence on Sumbawa and significance for the geology of East Asia and Australia'. an island off SW coast of New Guinea.. p. (1991). Associated with Cycloclypeus annulatus. Miogypsina.Cenozoic Molluscan types from Java (Indonesia) in the Martin Collection (Division of Cenozoic Mollusca). de Larat (Moluques). but is smaller and supposedly has somewhat different embryon. ('Studies on Nummulinidae and Alveolinidae. marine elements (dinoflagellate cysts. 2. Limestone samples from Sumbawa with Miocene larger foraminifera. Flosculinella bontangensis.Studien over Nummulinidae en Alveolinidae. ('A transitional form between Orthophragmina and Lepidocyclina from the Tertiary of Java'. Verhandelingen Geol. (1923). Contains Cycloclypeus martini n. 329-464. (1924). East Java. Lepidocyclina spp. Names never used by other workers. I.M. 369-374. p.Palynological aspects of Site 767 in the Celebes Sea.R. p. Eclogae Geologicae Helvetiae 18. algae) only 2-5% of microflora.. probably due to tectonic upheaval) Van der Sluis. Wesselingh & C. Tech. annulatus).A. p. Verhandelingen Geol. no stratigraphic context) Van der Vlerk.vangorselslist. Sci. (online at: http://retro.pdf) (129 species of mainly deeper marine foraminifera in Pliocene marls.. Kutai basin (no map or stratigraphy info) rich in ?M Miocene larger forams. p. J. Leiden. (1922).(Attempt to establish dinoflagellate cyst biozonation for Late Miocene.. Reichs- Museums in Leiden 10.M.-Mijnbouwkundig Genootschap Nederland Kol.M.tamu. L.P.naturalis. Leiden. 10. 1-130. 1010-1015. Haar voorkomen op Soembawa en haar betekenis voor de geologie van Oost-Azie en Australie. 91-98.edu/publications/124_SR/VOLUME/CHAPTERS/sr124_27. Ser 7. HvG) Van der Vlerk. (online at: http://www. Reinhard & E. Great Britain 1948. Nephrolepidina. 15. Isolepidina and Pliolepidina) Van der Vlerk. Pasir. I.Het genus Lepidocyclina in het Indo-Pacifische gebied. Indisch Natuurwet.M. (online at: http://retro. 3e Nederl.Tabulation of determinations of larger foraminifera. 16-35.Groote foraminiferen van N.Cenozoic Amphineura. (1925).Stratigraphy of the Caenozoic of the East Indies based on foraminifera. I. (Listing of all Cenozoic mollusc species described from Indonesia before 1931) Van der Vlerk. Leidsche Geol. (1928). p. NE Borneo Eocene-Miocene larger forams collected by Leupold from Tidungsche Landen. 13-32.Foraminiferen uit het Tertiair van Java. p.com March 2014 . spec. Wetenschappelijke Mededeelingen Dienst Mijnb. Bull. no maps) Van der Vlerk. 267-269.M. Verhandelingen Geol. I.sp. I. (1928). Congress. Mededelingen 5 (K. (1951). from Nyalindung beds near Sukabumi) Van der Vlerk. Geol. 137- 145. p. (1925). from Tji Lalang beds and Lepidocyclina/ Miogypsina/ Cycloclypeus and Rotalia beccarii atjehensis n. Wetenschappelijke Mededeelingen 1. Associated with Lepidocyclina (Eulepidina) formosa and Spiroclypeus. Three new species of Spiroclypeus. p. 8 (Verbeek volume).-Mijnbouwkundig Genootschap Nederland Kolon. p. Dienst Mijnbouw Nederl.vangorselslist.G. 371-380. 61-63. Eclogae Geologicae Helvetiae 21. I. 18th Int. Martin memorial volume). Borneo.M.seals. 7-86. Little or no stratigraphy) Van der Vlerk. ('Larger foraminifera from NE Borneo'. (New species of Lepidocyclina (Eulepidina) from Sungei Telakai. I. Escher et al.Early Miocene larger forams from Naintoepo and Tempilan beds. Bibliography of Indonesia Geology . (Late Oligocene. (1929). p. Buitenzorg. With species determination table) Van der Vlerk. British Territories Borneo 1. Ed. Java: Lepidocyclina rutteni n.E Miocene age) Van der Vlerk. NE Kalimantan.De verspreiding van het foraminiferengeslacht Lepidocyclina en haar beteekenis voor de palaeogeographie. (eds. 8. Trybliolepidina. suggesting Late Oligocene.M.. Oost-Indie. With stratigraphic table. Gastropoda. p. primarily based on characteristics of embryon: Eulepidina.) Geology of the Colony of North Borneo.1 179 www. p. SE Kalimantan. Survey Dept. 561-568. p. Congr. ('The distribution of the foraminiferal genus Lepidocyclina and its significance for paleogeography') Van der Vlerk. (1950). ('The larger foram genus Spiroclypeus and its significance for the stratigraphy of the Tertiary of the Indo- Australian Archipelago') Van der Vlerk. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl.) De palaeontologie en stratigraphie van Nederlandsch Oost-Indie. (1924). In: B.Het foraminiferen genus Spiroclypeus en zijn beteekenis voor de stratigraphie van het Tertiair van den Indo-Australischen Archipel. 3-44.Van der Vlerk. 206-296.-Indie 3. collected by Leupold. 1. Rept.The genus Lepidocyclina in the Far East. Wetenschappelijke Mededeelingen Dienst Mijnb. Scaphopoda. I.M. In: M.-Indie. I.A study of Tertiary Foraminifera from the "Tidoengsche Landen" (E. Eclogae Geologicae Helvetiae 19. 182-211. (Classification of Indo-Pacific Lepidocyclina. Geol. Nederl. 5. var.Lepidocyclina mediocolumnata nov. (1931).O. Wenk (eds. 9. p.-Indie. p. de Pasir (SE-Borneo). Nederl. (Miocene larger forams from W. I.M.M.ch/cntmng?type=pdf&rid=egh-001:1928:21::604&subp=hires) (Early review of Oligo-Miocene larger foram genus Lepidocyclina. I. Borneo). (1924).M. I. Handel. (Summary of Tertiary larger foram Ta-Tg 'Letter zonation' used in shallow marine carbonates of Indonesia) Van der Vlerk.M.M.M. (1925). lamellibranchiata. Bulungan and Mangkalihat Peninsula. Dickerson (1927).E.J. No locality map or local stratigraphy. M. Quart. p. p. p. Ser.M. 45-50% at Te-Tf boundary and 50- 55% in E Miocene/ Burdigalian) Van der Vlerk. (On evolutionary tendency in iso-. 5.M. D. maximum values increase from 25-30% in Late Eocene. (1961). & D. Kon. (1966). I. (1955). (1963).1929. Akademie Wetenschappen B76.M. ('Stratigraphy of the Tertiary of the Indo-Pacific and Mesogean domains (attemp of correlation)'. 334-338. Geol. Geol. (“Degree of curvature” preferred method over “grade of enclosure” to characterize evolutionary stage of Lepidocyclina) Van der Vlerk. Kon. Kon. 3. (Three limestone samples from central part of Larat Island (=Kai Besar?). Strat-graphic correlations between Far East and Europe using evolutionary stages of Lepidocyclina) Van der Vlerk. Verh. 1880. Geol. I. 245-255. Martin). 183-218.Lepidocyclina radiata (K. Proc. I. Nederl. 1934) Bibliography of Indonesia Geology . 115. Kon. p. p. Ges. Bull. p. p. 40-45% in Late Oligocene. with miogypsinids already described by Drooger (1953). 169-174.. I. (1973). Mijnbouwk. Ed. B69. Micropaleontology 14. 620-626.Correlation of the Tertiary of the Far East and Europe.. B 72. Nederl. 425-426. I. 1.Van der Vlerk. Dozy (1934). 185-192.M. 3. Van der Vlerk.M.Miogypsinoides. (appendix in Brouwer.Recent) Van der Vlerk. 1 (Kugler memorial Volume). Eclogae Geologicae Helvetiae 59. Type locality of Miogypsinoides dehaartii Van der Vlerk 1924. B64. p.Modification de l’ontogenese pendant l’evolution des Lepidocyclines (Foraminiferes). Amsterdam.Nomenclature and numerical taxonomy (name and number). Micropaleontology 1.Two methods of worldwide correlation.. 421-429. p.com March 2014 . Basel 84. Wet. (Brief paper on how larger foraminifera genera can be used by field geologists to determine broad ages of Tertiary limestones) Van der Vlerk. (On the different ways of classifying Lepidocyclina) Van der Vlerk. No locality descriptions or local stratigraphy) Van der Vlerk. & J.vangorselslist. p. 336-344. 72- 75. nephro. 669-673. Proc. Van der Vlerk.Stratigraphie du Tertiare des domaines Indo-Pacifiques et Mesogeen (essai de correlation).M.M. Proc. Soc.The Tertiary rocks of the Celebes-expedition. 49-63. London. p. I. (Includes measurements on Operculina foram material from SE Asia. France (7).and trybliolepidine embryons in Lepidocyclina embryon of deuteroconch to enclose protoconch to an increasing degree.Biometric research on Lepidocyclina. (1968). (Description of type specimen of M-L Miocene Lepidocyclina radiata from south coast of W Java) Van der Vlerk. Gen.M. I. 245-259. Miogypsinoides dehaartii and Miogypsina borneensis suggest Aquitanian age. (1973). & R.M. (1966). (1959).Biometrical investigations on Operculina. 5. Measured as 'grade of enclosure. Akademie Wetenschappen. Naturf. J. Nederl.1 180 www. Van der Vlerk. 3. p. 3. J. Miogypsina. I.M. Observed gradual decrease in grade of enclosure of second chamber by third in specimens from Eocene.Distinctions among certain genera of larger foraminifera for the field geologist of the East Indies. p. Bannink (1969). Micropaleontology 9.Problems and principles of Tertiary and Quaternary stratigraphy. Lepidocyclina et Cycloclypeus de Larat (Moluques). Amsterdam. I. I. Akad. Akademie Wetenschappen. Geol. Soc. I. Nederl. 4. I.M. 10. Proc. Van der Vlerk. Verhandelingen Kon. collected by Weber (BPM). (1959). I.M. Nederl.An improved method of biometric research. Paleontology 1. (eds.Oligocene planktonic foram biostratigraphy of Indian Ocean ODP sites along Ninety-East Ridge. A. Proc. Miogypsina borneensis) and B (with Miogypsina indonesiensis. I. Wennekers (1929). ('Some foraminifera-bearing limestones from South Palembang (Suamatra)'.M.1 181 www. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Rate of evolution changes from very slow to very fast to slow again and to fast again.basal Miocene (Zones P19-P22/N4) O and C isotope stratigraphy of benthic and plankonic forams from E Indian Ocean ODP Hole 758A. Lepidocyclina (T.com March 2014 . (Oligocene. (Composite section of Oligo-Miocene sediments of E Java and Madura with Lepidocyclinas and planktonic foraminifera.M. p. Smit (1991). 1-45. J.Tf2) assemblages A (with Lepidocyclina (N) besaiensis n. Assoc. Ganssen (1995).Tertiaire gidsforaminiferen van Nederlandsch Oost Indie.Paleoenvironmental distribution of Mid-Cretaceous to Recent larger foraminifera.Australia. Little or no stratigraphic info) Van Eijden. (1988). Akademie Wetenschappen. Telisa Fm E-M Miocene (Te5. Gloor (1968). Lower Palembang Fm localities C and D M Miocene zone Tf3(?) with Miogypsina indonesiensis and Lepidocyclina pilifera. Ocean Drilling Program.M. Genetica 39. Jakarta. Larger foraminifera from Early Miocene (lower Tf) Baturaja limestones between Batu Raja and Muara Dua) Van Eek.pdf) (Upper Cretaceous.An Oligocene multi-species foraminiferal oxygen and carbon isotope record from ODP Hole 758A (Indian Ocean): paleoceanographic and paleo-ecologic implications. Bordeaux.tamu.M.sp. De. Petrol. Oost-Indie 6. (online at: http://www-odp.J. (Overview of methods.Einige foraminiferenfuhrende Kalksteine aus Sud-Palembang (Sumatra). 17th Ann. (1981). p. 392-399. I. One of earliest papers to define the Eocene-Recent larger foram zonation known as the 'East Indies Letter Classification') Van der Vlerk. 121. I. p..) martini). & J. (IPA). Sci. not of glacio-eustatic origin) Van Gorsel. 4. 2. 5. Res.1EX. Exploration Memo EPR-E. Esso Production Res. Indonesia. & J. etc.H. p. J. 47-55.Biostratigraphy in Indonesia: methods. Most intervals reflect temperate. B. p. p.Eastern Indian Ocean Cretaceous and Paleogene quantitative biostratigraphy.subtropical climate) Van Eijden. W and SW of Sumatra. (Small guidebook describing principal larger foram genera from the Tertiary of Indonesia. (Measurements on embryonic shambers of Lepidocyclina from Java and Madura. (E-M Miocene Lepidocyclinids and Miogypsina from 4 localities on Gedongratoe map. Indon.A.M.F. Eclogae Geologicae Helvetiae 22.(Documentation of Eocene limestones with Pellatispira and Miocene limestones in different parts of Sulawesi) Van der Vlerk. p. pitfalls and new directions. facies interpretations. in Indonesian Tertiary biostratigraphy) Bibliography of Indonesia Geology .) Proc. in Nederl. D. & G.Oligo-Miocene Lepidocyclinas and planktonic foraminifera from East Java and Madura. including major fall at 30 Ma.Evolution of an embryo. (Unpublished) Van Gorsel. A. 47-65.M. Extent to which deuteroconch encloses protoconch or extent to which dividing-wall between them is curved (“degree of curvature”) increases from 10% in M Oligocene to 67% in M Miocene. Oligo- Miocene boundary placed above Globigerina ciperoensis ciperoensis zone) Van der Vlerk. & J. p. M borneensis. Weissel et al. Postuma (1967). (1937). Kon. Marine Micropal. Ed. 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Nederl.id/fosi) (Brief overview of principal groups and literature of Cenozoic macrofossils known from outcrops in Indonesia. p. C. Also brief reviews of work done on ostracodes.The marine Mollusca of the Kendeng Beds (East Java). p. Berita Sediment. In: Proc. p. (2014). Molluscs mainly from Pucangan Fm. 6. C.) and by Cosijn. Edwards (1986). L.iagi.H. 1-421. Bull. Lunt & R. Leidsche Geol. Cenozoic marine macrofossil assemblages from Indonesia all represent tropical faunas of Indo-Pacific province affinity) Van Gorsel. Carbonate buildup with ferro- manganese cement. personnel during Kendeng zone mapping survey (Duyfjes et al. Tijdschr. (First of series of paleontological papers on molluscs from Plio-Pleistocene Kendeng Beds W of Surabaya.T. (Listing of proposed nomenclatural changes for mollusc names described from Indonesia by K. (Overview of Cenozoic biostratigraphy and biofacies interpretation of SE Asia. 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J. which drowned in latest Oligocene time. p.1100m (probably 600-900m) and >2 km of post E Pleistocene uplift) Van Morkhoven. Centre Rech. Sea Res. (1989). Snellius II Symposium. 116-122.M. Bull. 5. were principal objects of paleontological and biostratigraphic studies in Indonesia. Helsing (2014). p.T. 217-320. Leiden. Natuurk. directly on Paleozoic metamorphics.com March 2014 . Wetenschappelijke Mededeelingen 27. based on presence of Miogypsinoides cf. (1938). 63-76. Prior to 1930's macrofossils. Bandung. F.-Prod. 27 p. 7. Principal microfossil groups used in region are foraminifera. (Two M Pliocene. 29. J.T.. Mem. (online at: www..Cenozoic cosmopolitan deep-water benthic foraminifera.or.Late Neogene planktonic foraminiferal biostratigraphy and climatostratigraphy of the Solo River section (Java. Morley (2014). bantamensis near crest and Spiroclypeus and Neorotalia mecatepecensis deeper in section. Part. in ‘Martin Collection’) Van Marle. Jonkers (2004). I.O. 183-209. NNM Techn. Van Regteren Altena. 2. Ed.Catalogue of the Mesozoic and Cenozoic holotypes in the collection of plant fossils in the Nationaal Natuurhistorisch Museum. (online at: www.iagi. Elf-Aquitaine. p.Renamed Mollusca from the Dutch East Indian Tertiary. in particular molluscs. I (Families Fissurellidae-Vermetidae inclusive). Troelstra (1981).Pleistocene (N19-N22) outcrop sections in SW Seram.. (1938). P. J. suggest paleobathymetries between 400.Gastropoda. some Upper Kalibeng Fm) Van Regteren Altena.P.S. Bibliography of Indonesia Geology . Material collected by Geological Survey. (1938).Recent and fossil benthic foraminifera and late Cenozoic palaeobathymetry of Seram. 24.Introduction to Cenozoic biostratigraphy of Indonesia. Expl. W. & S. Indonesia). C.C. 6-40. Paleoclimate signal inferred from fluctuations in cooler-climate planktonic forams used to correlate with Mediterranean Miocene-Pliocene boundary stratotype) Van Konijnenburg-van Cittert.O. Java. ). Bandung. Portunien nouveau du Tertiaire de l'Ile Celebes. 169-170. Madura (Calappa madoerensis n. V. Ser. p. 1-86.Arthropoda.sp.naturalis. Dev. a new portunid from the Tertiary of Sulawesi'. Ixoides. Nederl. described as Ranina (Hela) molengraaffi. Martin).The marine Mollusca of the Kendeng beds. p. (1923).V. 5-6.O. Amsterdam.A reappraisal of Protoplotus beauforti from the Early Tertiary of Sumatera on the basis of a new Pelecaniform family. Gastropoda. Proc. Centre. 89-120. Leidsche Geol. C. P. In:B. Kon. sp. (online at: http://www. Leidse Geol. V. etc. Amsterdam. East Java. p. Mededelingen 13.. (online at: http://www. as known in 1931.) Van Tets.Crustaces decapodes Cenozoiques des Indes Orientales neerlandaises. W. Decapod crab fossils collected by Lohr in Tuhup River valley.) Onze palaeontologische kennis van Nederlandsch Oost Indie.O. S Sulawesi (see also Brouwer 1924)) Van Straelen. (online at: http://www.Eocene of Sumba (Ranina (Lophoranina) soembaensis n. Bandung) Van Regteren Altena.etc. Res. (1923). Cenozoic crab fossils) Van Straelen. 421-428. p. (also in: Wetenschappelijke Mededeelingen 28. part IV (Families Cassididae-Ficidae inclusive). Gastropoda. 37-67.vangorselslist. SW of Bandung. (1977). G. Protoplotidae) Van Vessem. No maps or stratigraphic context info) Van Straelen. 90-103. Review of Neogene crab fossils from Neogene of Java (Calappa sangiranensis n. Akademie Wetenschappen. (1943).777-782.Portunus brouweri. Mijnbouwk. Akademie Wetenschappen B80.com March 2014 . V.dwc. Incl.repository. p. 156-163. Nederl.). Geol. 26. (1931). 5.J. & C. 57-75. Mededelingen 15.nl/document/549700) ('Cenozoic decapod crustaceans from the Netherlands East Indies'. Verhandelingen Kon.The internal structure of Miogypsina polymorpha and Miogypsina bifida. 26. Oost-Indie (1923). Leidsche Geol. p. 14 (Gedenkboek Tesch).O.G. 9-10. (Listings of arthropod fossils from Indonesia. Decapod crab fossils collected by Kemmerling in Barito Basin described as Ranina (Lophoranina) kemmerlingi (probably from Oligocene) and Calappilia borneoensis (from Eocene marls W of Lemoe village)) Van Straelen. Van Regteren Altena. Ed.nl/DL/publications/PU00014998.dwc. Mededelingen 5 (Feestbundel K. Ranina toehoepae. ('Portunus brouweri. Nederl. Proc. Jaarboek Mijnwezen Nederl.sp . Verhandelingen p.pdf) (‘Description of new raninian crabs from the Tertiary of Borneo’. (1941).V. Escher et al. Van Regteren Altena. Marino (1989).Description des Crustaces decapodes nouveaux des terrains tertiares de Borneo.knaw.The marine Mollusca of the Kendeng beds. Leidsche Geol. Part II (Families Planaxidae-Naticidae inclusive).nl/DL/publications/PU00014967.Description de Raniniens nouveaux des terrains tertiaires de Borneo. part V (Families Muricidae-Volemidae inclusive). E. Barito Basin. Kon. (1950). 1. Gen. Geol. p. (1924).1 183 www. East Java.). (Suggest Eocene water bird fossil initially described by Lambrecht 1931 from lacustrine shales of Ombilin basin should be placed in new pelicaniform family. p.(Reprint of Van Regteren Altena (1938) above) Van Regteren Altena.)) Van Straelen. Leidsche Geol. Permian trilobites.sp. (eds.O. Dienst Mijnbouw. New species of crab fossil from probably Miocene-age lithographic limestones with fish fossils at Patunuang Asu. C. Rich & H. 1. 5. p. Mededelingen 12. Neogene ostracodes. Proc. Akademie Wetenschappen. Philyra. (1938). 5.knaw. etc. V. 489-492. Beets (1944). Kon.R.pdf) (‘Description of new crabs from the Tertiary of Borneo’. 205-240. Nederl. Cancer javanicus n.Eine Neogene Molluskenfauna vom Tji Gugur (Priangan). p. Bibliography of Indonesia Geology . Paleont. Mededelingen 10.. (Rich Neogene mollusk faunas from Priangan. V. C. C.The marine Mollusca of the Kendeng Beds (East Java) Gastropoda. De Nummulieten uit den Eoceenen kalksteen van Borneo. Malaysia Bull.c=ctz) (On characteristics of large Melongena-type gastropods from Miocene-Recent of Sarawak.L. Geol. sumatrensis. Also found in Cebu and Bicol) Bibliography of Indonesia Geology . 103-113.uva. (L) polymorpha may be ancestor of M (L. (online at: http://dpc. Boegoel wells) and Madura.library. 5 of which have Eocene sediments unconformably overlying Pretertiary metamorphics. Utrecht Micropal.Brunei) Villavicencio.D. 2.. 1-163.nl/cgi/t/text/get-pdf?idno=m7803a03. Only 6 areas of Java with Early Tertiary in outcrop. Jaarboek Mijnwezen Nederl. Geol. Kinabatangan River). 101-138.Voorloopig bericht over nummulieten. (1983). Palaont. (Latest Cretaceous. Indie 51.12. C and E Java (Lodan. 37-46. Solomon Islands and Bougainville. isolepidinoides.M. modified from schemes of Martini (1971) and Okada & Bukry (1980)) Varol. Papua New Guinea regions. Discocyclina.pdf) (Quantitative study of lepidocyclinids of Nephrolepidina group from 42 samples from N Borneo (Klias Peninsula. 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(1989). (http://books. L. (First report of Paleocene. Neues Jahrbuch Min. Zoology 78. Geol. orbitoiden en alveolinen in Java en over den ouderdom der gesteenten waarin zij optreden. 5. M. M. p. R. 18 new species) Verbeek.uba. particularly from Java and Borneo. First descriptions of Eocene Nummulites from SE Borneo (and Indonesia). originally described by Rutten (1911. Res.J.Calcareous nannofossil study of the central and western Solomon Islands.sp. R. E Kalimantan (Kutei. based on material from E Kalimantan and E Java.html?id=uFoYAAAAYAAJ) ('Preliminary note on Nummulites. 1-14. (1871). Contrib. Dutch version of 1871 paper on Eocene Nummulites from SE Borneo. 113-127. B9. G.com/books/about/Natuurkundig_tijdschrift_voor_Nederlands. called species: L. N. ('The Nummulites from the Eocene limestone of Borneo'. O. 4. orbitoids and alveolinids in Java and on the age of the rocks in which they occur'.1 184 www. (1874).Proposed calcareous nannofossil zonation scheme for the Miocene to Holocene of Southeast Asia. Raven (2009). 133-161. martini and L. angulosa.com/2014/09/bgsm1983004.M.Die Nummuliten des Borneo-Kalksteines. Soc. p. Includes first descriptions of Eocene Nummulites (Nummulites javanus.files.google.vangorselslist. Tremboel. Miscellanea and small Paleocene foraminifera. Assemblages subdivided into five successive biometric units. L. L. (1978).Southeast Asia as the birthplace of unusual traits: the Melongenidae (Gastropoda) of northwest Borneo. & H. p. incl. (online at: https://gsmpubl.) bifida)) Van Vessem.Lower(?) Eocene (Ta) index algal genus Distichoplax biserialis from Philippines. E. Philippines) 18. p. R. Earth Science Ser. Bull.(Study of two Miogypina (Lepidosemicyclina) species.nl/dissertations/2011-0624- 200310/Utrecht%20Micropaleontological%20Bulletins-19-van%20Vessem.D. 1912) from E Kalimantan. Suppl. HvG) Von der Marck. (1877). 2. First paper on fresh water fish fossils from bituminous shale in Ombilin Basin.Die Echiniden der Nummuliten-Bildungen von Borneo. (1967). K. Suppl.Einige Crustaceenreste der Eocanbildungen von Borneo.) Indian Ocean geology and biostratigraphy. Palaeontographica.R. 236-251. p. 1. 1. W. Sardinioides amblyostoma.An Upper Eocene mammal of the family Anthracotheriidae from the island of Timor. Heirtzler (ed. 5. SE Kalimantan. Palaeontographica. Protosyngnathus sumatrensis. omphalus) from Pengaron area. ('Fossil fish from Sumatra'. 139- 143. 1. decipiens and O.Indian Ocean Neogene planktonic foraminiferal biostratigraphy and its paleoceanographic implications. 529-533. p. Oost-Indie 8 (1879).Einige Eocane Foraminiferen von Borneo. (‘Some Eocene foraminifera from Borneo’. Ducrocq 1996) Bibliography of Indonesia Geology . 3.1 185 www. p. Union (AGU) Mem. K. Descriptions of Nummulites and Discocyclina ('Orbitoides papyracea. Brachyspondylus indicus. Mainly new species) Von Fritsch. Nederl. Also descriptions of mid-Cretaceous orbitolinids 'Patellina scutum' and 'Patellina trochus' from Seberuang River.Fossile Korallen der Nummulitenschichten von Borneo. Description of rel. Palaeontographica. 138-155. p. (1877). O. Jaarboek Mijnwezen Nederl. 85-92. named Anthracothema verhoeveni n. In: J. and may be used to support proximity of much of Timor island to SE Asia/Sundaland in Eocene. p. E. epihippum. etc.Fossile Fische von Sumatra. 405-414. 3. K.vangorselslist. 3. Oost-Indie 7 (1878). 1. (online at: http://archive. all new. 136-138. p. 143-230) (‘Fossil corals from the Nummulites beds of Borneo’ Description of well-preserved coral assemblage from Eocene limestone collected by Verbeek in Pengaron area. American Geophys. W Borneo (both assigned to Orbitolina concava by Martin 1889)) (Same material already described by Verbeek (1871). Reprint of paper above) Von Koenigswald. Oost-Indie 8 (1879). dispansa. (also in Jaarboek Mijnwezen Nederl. Suppl. (1878). W Timor. 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(Description of Eocene Hippopotamus-like skull fragment and upper molar from W of Laharus. Oost-Indie 8 (1879). W Sumatra. p.Einige Eocane Foraminiferen von Borneo. (1877). Reprint of paper above) Von der Marck. Palaeontographica 22.org/details/palaeontographic22cass) ('Fossil fish from Sumatra'. S China and W Borneo and is first indication of Eocene mammalian fauna in E Indonesia. Oost-Indie 7 (1878). 93-135. p. 1. collected by Verbeek. 1. 469-584. 127-142). SE Kalimantan. Four new species. poor echinoid assemblage of 6 species. 3. Ed. Jaarboek Mijnwezen Nederl.Fossile Fische von Sumatra. p. N. W of Rengat. Butak. Symposium on Biostratigraphy of Mainland Southeast Asia. Distributed among various academic institutions) Wanner. p. 111-142. C Sumatra) Wade.. In: T.Sur sune nouvelle Dipterocarpacee du Tertiaire de Sumatra: Shoreoxylon rangatense n. . In: M.W. Wanner notes N to S facies changes. Molluscs mainly gastropods. Thanasuthipitak (ed.Von Kutassy. Watanasak. 68 species. Gen. Selenka & M. Ngandong and Lodan).Palynological zonation of Mid-Tertiary intermontane basins in northern Thailand. 104.Mid-Tertiary palynostratigraphy of Thailand. Ph. p.Einige neogene Seeeigel von Java. p.Mid-Tertiary palynology of onshore and offshore Thailand. Thesis University of Adelaide. Earth-Science Rev. Associated with Miogypsina thecidaeformis. Basis for zonations is first or last appearances of key species incl. A. Berggren & H. (1980). (Unpublished) Watanasak. 79 B. Pearson. estelae. kotoi. (’Miocene molluscs from the Rembang area (Java)’. Ser.. Geol. Min. p. p. p. p.D. Sea urchins in Pliocene? marls in Trinil area.com March 2014 . The Hague. Correlation between terrestrial and dated marine sequences) Bibliography of Indonesia Geology . J. Kol. ('On a new dipterocarp from the Tertiary of Sumatra: Shoreoxylon rangatense n. Zeitschrift Deutsch. 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Joint 36th HAGI and 40th IAGI Ann.sp. p. Bullen (1903).. PNG and probably New Zealand and Nepal) Oosting. Pacific. (online at: http://dspace. 2.). Westermann (1998). (Jurassic rocks with molluscs known only from West of Borneo island: Sultanate of Sambas and W Sarawak.) Panuju (2011). p.('Global distribution of ammonite faunas in the Middle Jurassic (Upper Aalenian to Middle Bathonian): relations between biodiversity and paleogeography'.The evolution and geography of Jurassic ammonoids. Geol. L. Baumgartner & A. (Jurassic ammonites 7 suborders. & G. E Pacific. 35-57.vangorselslist.G. (2004). with distinct European affinity. K.) Newton. Buya and Tanamu Formations. Malacological Soc. including a new species of Trigonia. (2008). 3-4.Palaeoenvironmental and climatic changes in Australia during the Early Cretaceous. described from Sula Islands.O. Thesis University Utrecht. 5.nl/handle/1874/1578) (Biochronostratigraphy for Tethyan and Boreal M Cretaceous traditionally based on ammonites. Tethyan. 6. Subkossmatia) and Perisphinctidae (Indosphinctes. Makassar. Geol. P.The perisphinctid ammonite Sulaites n. R. Virgatosphinctes. 231-240. probably from Sarawak River. with approximate ages. gen. (Useful listing of 6296 Mesozoic radiolarian species names. Part 2: Jurassic-Cretaceous. (Illustrated catalogue of type species of 581 genera of Jurassic. Bandini. Initially described as Cretaceous by Martin (1890). R.On a Jurassic Lamellibranch and some other associated fossils from the Sarawak River Limestones of Borneo.g.Albian stage boundaries in Australia) Page. Banggai- Sula basin. Indo- Malgach Province recognizable first in Callovian. helpful in confirming correctness of Hojnos (1934) Late Jurassic. Geodiversitas 31. 407- 415.Pre-Tertiary nannoplankton biostratigraphy of Bobong. S Pan- Tethyan Realm includes Mediterran-Caucasian. M Jurassic (Trigonia molengraafi considered to be species of Myophorella (Haidaia) by Kobayashi 1957) O'Dogherty. Aulacosphinctoides. subsequently determined to be Liassic. Alcheringa 22. Carter. in combinations as originally described. P. E. 271-356. By Tithonian.. in ~20 distinguishable biogeographical provinces and subprovinces.Early Cretaceous age assignments of E Sulawesi radiolarian rocks) O’Dogherty L.Catalogue of Mesozoic radiolarian genera. correlations between different realms is not straightforward. Magazine IV. with endemic Sphaeroceratidae (Macrocephalites. p. etc. several restricted Indo- Pacific/Austral genera and endemic species: Pachysphinctes.Notes on some Jurassic shells from Borneo. and Late Oxfordian-?E Kimmeridgian 'Pseudoparaboliceras aramaraii' group described from W Papua. Boreal domains and associated epicratonic platforms divided into 16 paleobiogeographical provinces. 5. Protocardia. Dumitrica. 403-409. Dinoflagellate cyst events combined with changes in carbon- isotope stratigraphy used here to assess Barremian.library. Himalayitidae. P. Exelissa.com March 2014 . etc. Kinkeliniceras. E. W Kalimantan.1 235 www. p. Most likely age 'Lower Oolitic'= ~Bajocian. Indo-Pacific and Austral realms/ subrealms. 2. Assoc. p. Bibliography of Indonesia Geology .E.S. and faunal and floral latitudinal contrasts. with place of Macrocephalitinae taken by endemic Mayatinae. Corbula. collected by McCarthy. Choffatia.N. S.. Matsuoka (2009). Gorican. (2009).. Uhligites. Pseudomonotis. 1-203.Inventory of Mesozoic radiolarian species (1867-2008).uu. with a sketch of the Mesozoic fauna of that island. De Wever. A. Conv. Geodiversitas 31. London. Provinces that show strong endemism are isolated (Boreal and SE Tethyan margin)) Newton. 371-481. Bullen (1897). etc. (New genus Sulaites comprises Oxfordian group of 'Perisphinctes' sularus and moluccanus. Proc. Proc. No range charts) Oloriz. endemic Blanfordiceras). Persisted into Oxfordian times.Cretaceous macrofossils known from Borneo. F. from the Upper Jurassic of the Indo-Southwest Pacific. A. Description of new Jurassic fossils from Boedak (Buduk). au/image_cache/GA14151. Late Cretaceous.Campanian. J.Early Cretaceous for Australia. Helby (2001). Jurassic and earliest Cretaceous dinoflagellate cysts: supplement 1. p. Shallow marine deposition. but not illustrated. Area subsided ~4000 m since deposition) Remane. 349-367. Wallaby Plateau. Riding.nerc. A. (online: /www. p.G. Foraminiferal Research 41. J. J. 2. (1985). Riding.A selective reappraisal of Wanaea Cookson & Eisenack 1958 (Dinophyceae). First record of marine rocks of this age from Australia) Quilty. (Foraminifera from RV Sonne sample dredged from 4438–4049 m water depth on Wallaby Plateau SW margin.) Australian Mesozoic palynology zonations.ga. and paleobiogeographic significance. 5. Cambridge University Press. (2012). p. www. M Jurassic.B. Australia. each through different formations. biostratigraphic. with Marthasterites furcatus at bottom. Micropaleontology 48. 24. presence of calpionellids in PNG by Rickwood (1955)) Riding.pdf. 182-195. Quilty. 1-32.gov. 985-995. p. 1-119. J. Palynology 37. p.B. Assoc. Western Australia. (2006). p. P. Jurassic.au/image_cache/GA14153. (1981). Assoc. dominated by Conicospirillina. Tanamu Fm zones CC13-CC17 (Coniacian. E.uk/19423/1/Jurassic_dinocyst_reference_list_- _revised_manuscript_March_2012_word_2003.updated to the 2004 Geologic Time Scale.Calpionellids. with Zeugrhabdotus embergeri at bottom. In: H.Early Jurassic Foraminifera from the Exmouth Plateau.B. 3.D. Paleontology 55. (Review of Late Tithonian. 345-354. J. (1990). & R.The literature on Triassic. Eastern Indian Ocean. Late Jurassic. J. chronostratigraphic.Triassic and Jurassic foraminiferid faunas. J. & R. Oxfordian/Kimmeridgean foram fauna. (online at: http://nora. Buya Fm zone NJ17 (Tithonian. 4. Strat.(Nannoplankton from three M Jurassic. 229-256.ac. (Samples dredged from Exmouth Plateau by RV Sonne yielded Late Sinemurian forams Ichthyolaria and Geinitzina. Bolli. Offshore Western Australia. 33-58. northern Exmouth Plateau. p. Monteil (coord. and earliest Cretaceous dinoflagellate cysts.B.ga. Conorboides and Lenticulina. Late Cretaceous- Cenozoic Gippsland Basin) Pessagno. Dallas. 46. & D. 24. Low diversity fauna.pdf) (Spore-pollen and dinocyst zonations charts: Jurassic.Upper Jurassic (Oxfordian) radiolaria from the Sula Islands (East Indies): their taxonomic.Australian Mesozoic and Cenozoic palynology zonations (Charts1-4). P. with Watznaueria brittanica. in keeping with Gondwana origin of Sula) Quilty. Babong Fm contains zone NJ9 (Bajocian. Quadrum gartneri at top)) Partridge.G.gov. older than previously known ages in region and predates initiation of seafloor spreading along W Australian margin.B. J. (2013). American Assoc. 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Athol Fm indicates E Bajocian marine transgression onto Australian block) Roggeveen.P. Described as Protocupressinoxylon malayense n. (online at: http://journals.Jurassic dinoflagellate cyst zones of NW Shelf (relatively minor modifications of Helby.. Nederl.Phallocysta granosa sp. S. Inoceramus molluscs and fragment of an aegoceratid ammonite from S coast of W Sumba in rocks collected by Witkamp. Assoc. Mantle & J. J.B. 24. Ed. Riding. Philippe et al. J. P. (1932). J.pdf) (English version of paper above. Kon.Epidiceras (Bivalvia. Proc.A review of the chronostratigraphical ages of Middle Triassic to Late Jurassic dinoflagellate cyst biozones of the North West Shelf of Australia. p. (1983).dwc. Assoc. Riding.. & R. 177-220. Riding. S coast of Sugi island. Palaeobot.B. Australia. Earth Sci. (Co-occurrence of ammonites (Pseudotoites robiginosus) with palynomorphs in Athol Fm of Tusk-1 and 2 wells. D.vangorselslist. confirms E Bajocian age of Dissiliodinium caddaense dinoflagellate zone. In opinion of Kruizinga this could be Hammatoceras molukkanum.dwc. offshore Carnarvon Basin. Mem. Palynology 162. Rev.59–63.Dinoflagellate cysts from the Late Jurassic (Kimmeridgian) Dingodinium swanense Zone in the North-West Shelf and Timor Sea. 24. 4. & R. p. S of Singapore.M. (Reassessment of ages of 20 M Triassic. Akademie Wetenschappen. Helby (2001).s. HvG)) Sano. Nederl. Akademie Wetenschappen 35.pdf) Bibliography of Indonesia Geology . Helby (2001).Jurassic in the island of Sumba. Australasian Palaeont.W. p.tubitak.sp. Hippuritoidea) from the Tithonian-Berriasian Torinosu-type Limestones of the Sakawa Area. Turkish J. S Andes.Microplankton from the Mid Jurassic (late Callovian) Rigaudella aemula Zone in the Timor Sea. Thought to be probably Triassic-age but could be Jurassic-Cretaceous (Age of beds poorly constrained and classification uncertain. north-western Australia. Folded Mesozoic intruded by igneous rocks and unconformably overlain by Eocene (Caudri. p. nov. Australia. J. Silicified conifer wood in sandstone-shale- conglomerate series at cliff of Tanjung Riau. (online at: http://www.B. humphriesianum forma indica). (online at: http://www.Marine microplankton from the Late Jurassic (Tithonian) of the north-west Australian region. 19. Helby (2001).B. (1929). & R. p. Helby (2001). W New Guinea (where identified previously as Stephanoceras cf. Western Australia. Tentatively placed in U Liassic by Wanner (1931). Assoc. Riding. G. Alcheringa 34.B. Bajocian) in the Tusk-1 and Tusk-2 wells. P. 733-743. 65-110. Proc.knaw. Assoc. p. 111-140. 24..knaw. as known from Jurassic of Sula islands. Riau Archipelago’. Australasian Palaeont.Dinoflagellate cysts from the Late Jurassic (Oxfordian) Wanaea spectabilis Zone in the Timor Sea region. Mem. p. 1934)) Roggeveen. & R. Mem. Helby (2001). Australasian Palaeont. Amsterdam 32. 2004. Westermann & D. p. More likely age of beds is Cretaceous according to Von der Borch et al. 24.nl/DL/publications/PU00016260. Riding. Niederlandisch Ost-Indien. 5.Mesozoisches Koniferenholz (Protocupressinoxylon malayense n. & R. 1. Mem.B. Ammonite Pseudotoites prominent in E Bajocian of Indo-Pacific Realm (onshore W Australia. 2004 zonations)) Riding.) von der Insel Soegi im Riouw Archipel. Skelton (2010).E.1 237 www. 512-514. J. J.com March 2014 . p. Morgan and Partridge 1987.pdf) (‘Mesozoic conifer wood from Sugi Island. Other specialists deem the ammonite fragment indeterminate and the Inoceramus more likely a Cretaceous species (HvG). Kon.B. 21-35. Southwest Japan.I. Australasian Palaeont. & P.Riding. 24. Backhouse (2010).M. a Mid Jurassic (Bathonian) dinoflagellate cyst from the Timor Sea. Assoc.G. 543-575.. 141-176.New evidence for the age of the Athol Formation (Middle Jurassic. J. 580- 584. off Carnarvon Basin.J. Protocupressinoxylon in China is Jurassic genus.F. Australasian Palaeont.tr/earth/issues/yer-10-19-6/yer-19-6-5-0905-2. Darbyshire (2010). 81- 108. 32. NNE of Saigon. 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(online at: www. with araucarias and ginkgos also present.Sur quelques empreintes Mesozoiques de Malaisie. 40 km NW of Sanggau. Affinities with Europe. Perispinctes spp.G. Laos and Vietnam'. Mesozoic forests dominated by podocarps. Zeiss (1992). Jurassic-Cretaceous fossil wood from 4 localities in S Vietnam and Cambodia. p. T. some conglomerate and sandstone. C. & A. with Hectioceras spp..Sur des bois fossiles de l’Archipel de Tho Chau (Golfe de Thailande). Philippe et al. 1-28. C. G. Borneo. Geol. Vietnam 8. p.com March 2014 . M-U Jurassic macrofossils from geodes in float of Upper Sepik River near 4d 15’S. (1928).. Pahang. 2004)) Serra. from Kazanian (Permian) of Sisophon (Cambodia). 1-15. London) Skelton. Also canaliculate belemnites and Incoceramus galoi. J. Philippe et al. Dadoxylon khmerinum n.. 17-40. (1968). 105-112. probably of Triassic age described from N of Mentakab.Rudist bivalves and the Pacific in the Late Jurassic and Early Cretaceous. Australian Geol. Soc. 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E. etc.Oberer Jura in West-Sumatra. Noda & K. This suggests an eastern limit for gas-productive Middle Jurassic sandstone reservoirs of Bintuni Bay and thus have significant negative implications for the potential of Mesozoic hydrocarbon plays in Cenderawasih Bay) Van Gorsel. Geol. ser. Uhlig. 5. Corbula borneensis n. Samml. (2012). K. Protocardia..Neue Mollusken aus dem Jura von Borneo..Middle Jurassic turtles from southern Thailand. Bibliography of Indonesia Geology . Oost-Indie 1899. 753-758. (1896). p. Oost-Indie 25. Corbula.No Jurassic rocks on Sumba? Berita Sedimentologi 25.. p. Samml. (2012).iagi. tenuicostata n. sp.id/fosi/. 243-293. (1896). Berita Sedimentologi 23. Magazine 139. ('Molluscs from the Jurassic of Borneo'. IV. Dogger with Stephanoceras and Macrocephalites) Van Gorsel. (online at: http://www.687-697. 2) (‘New molluscs from the Jurassic of Borneo’.. Leiden. Occ. p. Ged.sp. Geol. Closely resembles species M. J. Pal. Protocardia crassicostata n.. 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(4) Shoal facies rich in ooids and near-monospecific Pilammina sulawesiana association (as known from Sulawesi). Mag. Samodra & L.and fore-reef: mainly Duostomina and Variostoma. A.. Geol. cool. Paris 318.. Asian Earth Sci.S. with a fourth. Vrielynck.sp. J.lowermost Jurassic palynology and palynostratigraphy: a review. mainly based on bivalve molluscs. p. Twelve faunal zones. also Grammotodon malayensis. Palaeoecology 100.R. (Overview of Triassic successions of Timor.. southern Tethys margin) vs. Three formal lithostratigraphic units defined previously (Niof. & J. Limestones can be correlated with U Triassic limestones of Tokala Mts of Sulawesi East Arm) Cox. Chiang Mai University. Nat.Geographic differentiation of Triassic brachiopods.Upper Triassic.echinoderms and benthic foraminifera (Aulotortus spp. Barber. coral clusters. Gunawan. Comptes Rendus Acad. Aitutu and Babulu Fms). Age interpreted to be pre-Rhaetian Triassic.or. J. Int. (1993).iagi. with some ooids and intraclasts. mainly Myophoria spp. S. Bibliography of Indonesia Geology . H. 341-363. ser. R. Foraminifera Tethyan tropical affinity. C. 809-814. Bird (2009).R. (Relatively complete marine Triassic section in Thailand >3000m thick. Roniewicz. primarily Jurassic in age but extending down into Triassic. Triassic extension not associated with major volcanism. Carnian-Norian age matches Tethyan carbonate platform/ reefs in Alps and Asinepe Limestone in Seram.green algae (including dasycladaceans). & J. p.. Barkham & P. Wai Luli Fm. Grant-Mackie (1993). Zaninetti... Distance in accordance with velocity and direction of plates related to Neo-Tethyan ridge opening) Charlton. Special Publ. Ser. W..A. Limestones range from boundstone to grainstone. (2) Back. T.Une plate-forme carbonatee d’age rhetien au centre-est de Sulawesi (region de Kolonodale. Federated Malay States. E. A. (online at: www. S. Symp. (1936). A.J. N of Raub gold mine. 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SE of Klabat Bay.Seram. based on cephalopods. from Thailand (Norian.A. Band 10. Upper Cretaceous Sawai Fm only planktonics: Globotruncana. 2.Triassic floras of Eurasia. S. Other areas Triassic starts with Carnian transgression. unicava. 1-422. Hedbergella. First documentation of poorly preserved Norian corals (Montlivaltia molukkana). Brief reviews of Triassic on Timor.) Dobruskina. (online at: http://www. etc. Diplotremina. p. Review of global Triassic macrofaunas as known in 1916. 475-492 (online at: http://opac. (The flora of the Upper Triassic of Vietnam. folded with phyllites and fine-crystalline quartzites. Amsterdam.at/wwwopacx/…) ('Additions to the Dibranchiate fauna of the Halstatter Limestone'. peri-Gondwanian. Wien. C. (1918). Akad. Vietnamese U Triassic flora belongs to coastal floristic assemblage of SW Pacific. venezuelana.Foraminifera Pra-Tersier dan Paleogen di daerah Saleman.Rhaetian near base of Khorat Group). Seram Utara. Timorhynchia) De Franceschi. Vienna. 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(1997). Springer Verlag. Ser. Buru. (1916). Sumatra. Komm. Akad.. Kon. de Roever (1947). Osterrr.La flore du Trias superieur vietnamien. and Meadrospira.nl/DL/publications/PU00018447.A. etc. 3. Akademie Wetenschappen. Verhandelingen 4. Indonesian area groups in Himalayan Domain. Savu. Encrinus).Ammonoidea trachyostraca aus der mittleren und oberen Trias von Timor.Die marinen Reiche der Triasperiode. Jaarboek Mijnwezen Nederl. D. Nederl. Mainly comparison of Late Triassic belemnoid faunas from Timor and from North Calcareous Alps.vangorselslist. 333-340. See also Vozenin-Serra & De Francesci (1999)) De Neve. C. (1994). Prefers to maintain Aulacoceras timorense Wanner as separate species) Diener. Upper Norian- Rhaetian faunas not demonstrated. 10. resembling ‘Halstatt Limestones’ in Alps. Erdwissensch. Dominated by Haloritids. Assemblages from blocks very rich in well preserved ammonites. 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G. & E. Probably mainly of Late Triassic-Jurassic age. 4. in reality an Early Jurassic Analytoceras hermanni Gumbel. Malaya.) Geology and Palaeontology of Southeast Asia. Savu. Dictyomitra. Gondwana Res. Toriyama (eds.. which is same as Monotis subcircularis Gabb (Westermann 1962)) Ichikawa.). Fewer. Jaarboek Mijnwezen Nederl. 101-106. Includes description of new species Monotis (Entomonotis) timorica from Timor. Molukkenverslag. University of Tokyo Press. Buru and Mangoli in Verbeek's Moluccas report.Triassic conodonts from Kelantan. 157-171. J. Ged. p. Warta Geol. K. Conv. 694-736. ('On the taxonomy and phylogeny of the Triassic 'Pteridae (Lamellibranchiata). Keupp (2010). Ishida. T.1 258 www.E Jurassic (Hettangian). Pseudofurnishius murcianus confers S Tethyan low-latitude character to Kodiang Lst.D. (Radiolaria from Timor. Kobayashi & R. Geosc. 9. 41st Ann. p.Some Triassic ammonites from Indonesia and Malaysia.Hinde. 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Polonica 60.Zur Taxonomie und Phylogenie der triadischen „Pteriidae" (Lamellibranchiata) mit besonder Berucksichtigung der Gattungen Claraia. 93-95. & H. Wetensch. 1927. K. p. Verbeek.) Irwansyah & Panuju (2012). Maluku. p. Geosc. central part of Malay Peninsula include white-grey Permian limestone with common fusulinids and grey M Triassic limestones rich in ammonoids and conodonts (dominated by Hindeodella spp and Hibbardella sp. K. Sulawesi.Radiolaria from Triassic and other rocks of the Dutch East Indian Archipelago.The Triassic conodonts of the NW Malayan Kodiang Limestone revisited: taxonomy and paleogeographic significance. p. Osaka City University 9. In: T. (1975). (A) 111. Basir (1994). Geologische verkenningstochten in het oostelijke gedeelte van den Nederlandsch Oostindische Archipel. 131-212. forming Sundaland platform. 19. Jurassic and Cretaceous ages) Ishibashi.H. 5. 2. Ed.H. part of Cimmerian terranes that in Triassic formed diagonal partition between gradually closing Paleo-Tethys and widening Neo-Tethys. Toriyama (eds.. Geol. 22-36. Oxytoma und Monotis. Malaya. Tanimbar. Malaya. with particular emphasis of the genera Claraia.) Geology and Palaeontology of Southeast Asia University of Tokyo Press. p. Igo. In: R. 45-56. 74 new.J. Krystyn 1978) that age of original boulder is E Jurassic (Hettangian). 1861)) Ichikawa. 1861.Integrated microfossil analysis of Pre-Tertiary sediments in the Bubuan Island. Oxytoma und Monotis'. In: T. p. Eumorphotis. Assoc. Proc. Yin (1966). (1958). K. J. Yin (1966). but similar species in loose chert pebbles collected at Seram and E Sulawesi) Hoffmann. Ceram. p. Kobayashi & R. (1908). Biostratigraphy analysis of outcrop samples of Pre-Tertiary sediments from mud volcano deposits on Bubuan island. shows Triassic.M. Tanimbar group.vangorselslist. 'Hallstatt facies' limestones ranges in age from Triassic. stretching E to Malaya (Shan Thai Terrane). northwest Peninsular Malaysia. & Y. p. Verhandelingen III. Basir. W. Anadontophora. J. but still considered to be Rhaetian-Liassic by Wade-Murphy and Van Konijnenburg(2008). (Cherty packstone-wackestone in Bukit Kodiang quarry. A. Kedah.sp. p.. northern Thailand and their paleogeographic significance. Similar fauna and rocks to E continental margin of Sibumasu Block. and Protocupressinoxylon malayense Roggeveen.com/2014/09/bgsm2005005. K. Basir. P. E. 31-39. Leptophyllia praecursor n.Fossil plants of the Island of Bintan. Charoentitirat.-Indie 55 (1926).. S Kedah. Ueno. 5.sp.sp.wordpress. SE Peninsular Thailand with two kinds of radiolarian-bearing fine-grained sediments: Middle- early Late Permian lower shale unit and E-M Triassic upper chert unit.Die Fauna der obertriadischen Nuculamergel von Misol. T. K. With Late Triassic (Late Carnian. northwest Peninsular Malaysia. 18 species) Jasin. Sashida. K. 51.. E.files. Nederl. 20. 110. Charusiri (2002). HvG) Kamata.) Jaworski. Interpreted as part of Late Triassic Dictophyllum. Asian Earth Sci.. include Ptilophyllum bintαnense n.. etc. southern peninsular Thailand: implications for the tectonic setting of the eastern margin of the Sibumasu Continental Block and closure timing of the Paleo-Tethys. rather than abyssal plain pelagic deep-water sediments) Kamata. Nucula marls in SE part of Lios island SE of Misool underlies the 'Athyridenkalk' (Misolia limestone). Four assemblage zones. solitary corals (Molukkia triasica n. W. Ali & K. Hisada (2014)- Late Permian and Early to Middle Triassic radiolarians from the Hat Yai area. more comparable to Neocomian Gagau flora of W Malaysia by Kon’no (1972). Marine Micropal. Brachiopods from dark limestones intercalated in several 100m thick sandy shales package including Rhynchonella. n. Saengsrichan..sp. (1915). nathorsti. Proc. J. p. Hisada. Mainly bivalves (Pecten misolensis and other spp. Cycadolepis sp. Charoentitirat.1 259 www. Jaarboek Mijnwezen Nederl. (Early to Late Triassic (Spathian-Carnian) radiolaria from bedded cherts of Mae Sariang Gp in NW Thailand.com March 2014 . Y. Spiriferina spp. Sardsud. Y.J. P. Harun & U. NW Peninsular Malaysia. 201-229. Charusiri. Koike & K. Myophoria. 183-190. rosenkrantzi. P. (online at: http://gsmpubl. 5. C. Nakornsri & P. 2. K. p. 12. Nucula misolensis n.M Norian) radiolarian assemblage. Y. Southeast Asian Earth Sci. Entactinosphaera chiakensis (late Spathian). Southern Bibliography of Indonesia Geology . not well preserved. Ed. Z. gastropods. Charusiri & K. K.. Said (2005). p.Triassic radiolarian faunas from the Mae Sariang area. Peninsular Malaysia. Paleocardita).pdf) (27 taxa of E-M Triassic radiolaria from outcrop of chert units in Semanggol Fm (and Kodiang Limestone?). Hisada (2008)- Stratigraphy and geological ages of siliceous sedimentary rocks distributed in the Hat Yai Area. Akademie Wetenschappen. T. 491-506. Triassocampe deweveri (late Anisian) and Oertlispongus inaequispinosus (E Ladinian)) Jaworski.. (First description of latest Triassic 'Bintan flora'. (1927). 73-174.Triassic radiolarian biostratigraphy of the Semanggol Formation.Clathropteris flora (But thought to be younger. Pterophyllum muensteri. Soc.5 km E of Kuala Ketil.Obertriadische Brachiopoden von Ambon (Molukken). 5. Malaysia Bull. A. 8-24 (Hat Yai area.Jasin. (‘The fauna of the Upper Triassic Nucula marls of Misool’. Ueno. (1951). T. Shirouzu. B54. Roslan Mohamed (1995). Ueno. 4.vangorselslist. South Kedah. NW Malay Peninsula. 31-39.. Geol. E (?) Carnian radiolarian assemblage from bedded chert shows closure of Paleotethys Ocean between Sibumasu-Indochina blocks after E Carnian) Kamata.Late Triassic radiolaria from the Kodiang Limestone. Sardsud. A.) Jongmans. p. Triassic chert interpreted as continental slope sediments overlying Permian clastic-calcareous facies. N.) Palaontologie von Timor II.gen. P. Species identified Tanjung Batu Itam. Wanner (ed. Bintan island. Otozamites gagauensis. In: J. ('Upper Triassic brachiopods from Ambon (Moluccas)'. Triassocampe coronata (M Anisian). Kon. Riau islands. p. Spirigera.A. Shamovella and Mizzia velebitana and colonial coral Waagenophyllum. H. T. Verhandelingen.. Kyushu Unversity.th/Geology/English/News/Technique/GREAT_2008/PDF/104.1 260 www. In: III Congr. 39-78. generally reddish color Permian. Simp. Flugel (2000). (Corals from U Triassic Pacific seamount limestones in Japan. (1985). Eptingium. 325-350.ac. Facies 43. separated from Indochina Block in M Permian and collided with S China Block in Late Cretaceous (then separated again with S China Sea opening)) Kimura. 51-145. with a short note on the Cenozoic floras of Southeast Asia and China. M Triassic radiolarians in bedded chert (Triassocampe coronata. Permian.com March 2014 . 15. 135-200. etc. (1924). Symp. Includes mention of species previously known only from Timor) Keupp. Terra Science Publ. Also found 1-5 cm big globular hydrozoans Heterastridium conglobatum. Colania douvillei. (Well-illustrated report on 2008 fossil collecting trip to Baun area. deweveri. University of Tokyo Press. Fossilien.Chlathropteris floristic province) Kimura.Die Nautiloideen der mittleren und oberen Trias von Timor. p.sc.Geographical distribution of Paleozoic and Mesozoic plants in East and Southeast Asia. In: T. D Geology. etc. ('The nautiloids from the Middle and Upper Triassic of Timor'. Bangkok. Int.) Geology and Palaeontology of Southeast Asia 25.Lower Jurassic limestone blocks in olistostrome in Late Tertiary marl-radiolarite-tuff succession. p. Tokyo. Bibliography of Indonesia Geology . 3. With Golonka Permian-Triassic plate recontructructions. 214-220. Large erratic. Geoscience Resources and Environments of Asian Terranes (GREAT 2008).geo. Oost Indie 51 (1922). Ser.Triassic coral faunas from the Konose Group in Kyushu. (Review of Triassic. sobre Floras Trias. W. N Palawan probably part of Indochina in Carboniferous-Permian.). Triassic. p. 5-9. Latino America Paleontology. Malay Peninsula. 117-147. suggesting closure of Paleo-Tethys after M Triassic in Peninsular Thailand) Kanmera. Mainly from isolated blocks of ‘Halstatter facies’ condensed Triassic section (other classic works on Triassic ammonites are by Welter 1914.Early Jurassic limestones open ocean facies. Malay Basin. (1964). Parafusulina. Permian Minilog Fm Guadalupian fusulinids (Verbeekina verbeeki. T. Incl. Neoschwagerina) and dasycladacean wacke-packstones with Permocalculus.. probably continental margin sequence at E side of Sibumasu Plate. Science. (1984). commonly coated by manganese layer.) Historical biogeography and plate tectonic evolution of Japan and Eastern Asia. 4/2009. (online at: www.Notes on the present status of Late Triassic floras in East and Southeast Asia. (Permian.Timor: Bonanza nicht nur fur Triasfossilien. Mexico City. 1915 and Diener 1922)) Kiessling. A. Tashiro (eds. Busuanga Island Late Triassic (Rhaetian) limestones in reef and platform facies with Triasina hantkeni.chula.Triassic Kaeng Krachan and Yaha Fms deep marine clastics of Peninsular Thailand. Paglugaban Fm with M Carboniferous fusulinids (Pseudofusulinella). of Norian age and possibly a pelagic hydrozoan colony) Kieslinger.E Jurassic Krusin flora is part of Indochina/ South China Dictyophyllum. Mainly taxonomic descriptions of nautiloid ammonites collected by 1916 Jonker expedition.Cretaceous floras in SE Asia and China. 349-352.vangorselslist. locally rich in ammonites and aulocerate belemnites. (1987). SW Timor. Jaarboek Mijnwezen Nederl. 20km W of Hat Yai. p. In: A. Carbonates formed on seamounts surrounded by deep water radiolarian cherts. p. K.Peninsular Thailand. p. Taira & M. Proc. p. etc.pdf) (Permian. 5. Kimura. 4th IGCP 516 and 5th APSEG. dark shale with Late Permian radiolaria (Follicucullus scholasticus). Mem.Carboniferous limestones in El Nido area. T. T. Banda Basin.. NW Borneo Late Triassic.Late Paleozoic and Late Triassic limestones from North Palawan Block (Philippines): microfacies and paleogeographical implications. (eds.Triassic carbonates contradict close paleogeographic connection between N Palawan Block and S China. Mem. similar to E Sulawesi. Ed.Mesozoic floras of East and Southeast Asia. Kobayashi et al. p. Pseudostylosphaera japonica. (2009). & E. Fac. 4.). p. T. sec. R. mainly of Ladinian age. Cherts in Tuhul Fm of S Sumatra are M-L Triassic or Permo-Triassic in age) Bibliography of Indonesia Geology . Nakaya (2006)..Diplotremina astrofimbriata (Ladinian) and (4) Aulotortus sinuosus (Carnian). (Includes review of Paleozoic. Tokuyama & E. p.On the Triassic Daonella beds in central Pahang. Kimura (1944). Japan). (Four Triassic foraminiferal limestone localities in Lampang Group of Sukhothai foldbelt. 6. 34. based on occurrence of Pilammina densa and Meandrospira dinarica. NW Khorat Plateau) Kobayashi. In: T. N Thailand. from Temerloh area. 2. Triassic shales of Temerloh associated with Pahang Volcanics tuffs.jstage.A study on the radiolarian rocks. also Europe (unlike M. p. Fac.H.K. & T.) Geology and palaeontology of Southeast Asia. D. 751-763. University of Tokyo Press.Kobayashi.Triassic foraminifers of the Lampang Group (Northern Thailand). Kobayashi (ed. T. D. 3.38. 312-325. 7. lommeli. Ratanasthien. B. (Daonella faunas with 5 species incl. C. Geobios. Daonella Beds mainly Ladinian. p.jp/article/pjab1945/49/10/49_10_825/_pdf) (Non-marine conchostracan (bivalve crustacean) Euestheria mansuyi from Late Triassic Nam Pha Fm. 101-112. Geogr. T. 10. Daonella and Halobia widespread in deep-water W zone. University of Tokyo Press.A Norian conchostracan from the basal part of the Khorat Group in Central Thailand. (3) endothyroid foraminifers.Halobia and some other fossils from Kedah. Proc. basal Khorat Group. Kobayashi & R. 57-90. therefore possibly more likely of Triassic age. Imperial University Tokyo.Upper Triassic estheriids in Thailand and the conchostracan development in Asia in the Mesozoic era. 27. L. Kobayashi.Typical Tethyan fauna. Central Malay Peninsula. (1975). Zaninetti.. Terrane was part of N Gondwana margin.vangorselslist. Important taxa of these associations common to S China and SE Asia. J. Contributions to the geology and palaeontology of SE Asia.com March 2014 . Pahang. H. p. Characterized by: (1) Glomospirella lampangensis n.Mesozoic radiolaria data from Sumatra. northwest Malaya. 34. Saegusa & H. Zaninetti (2005). (online at: https://www. 5. T. In: T. Martini. then isolated eastwards before E Cretaceous amalgamation with S China) Kobayashi. etc. E zone on E side of Main Range. (1963).3. 825-828. West Kyushu.sp. from Kelantan via Pahang and Johore to Singapore.On the Triassic Daonella Beds in Central Pahang. Ed. A. between Sibumasu (Shan-Thai) Terrane in W and Indochina in E..The Daonella and Halobia facies of the Thai- Malay Peninsula compared with those of Japan.E Norian. (Occurrence of Ladinian-Norian hemipelagic bivalves Posidonia kedahensis Kobayashi. Malaya. T. sp. Geology and Palaeontology of Malaya 1. 3-67. associated with Triadodiscus.. Halobia beds mainly Carnian. Aulotortus. indica. T. (35 species of M Triassic foraminifera in allochthonous oolitic limestone blocks in Carnian Tanoura Fm in Kurosegawa Terrane of W Kyushu. etc. D. Geol. Blocks are of Anisian in age. Same paper as Kobayasi 1963) Kobayashi. (M-L Triassic mollusc-bearing beds in Malay Peninsula E and W zones. Contributions to the geology and palaeontology of SE Asia. from S Thailand through Kedah to N Perak ('Semanggol Fm'). Geol. Malaya. F. Japan Academy 49. Asian Earth Sci. In: Geology and Palaeontology of Southeast Asia 16. (2) Pilammina densa (Anisian). Martini & L. (1973). characterized mainly by nearshore Myophoria sandstones) Kobayashi. F. T. Yin (1967). p.go. (1963). NW Malay Peninsula) Kobayashi. Burton. Toriyama (eds. (1964). Japanese J. Halobia talauana Wanner. R. Kalimantan Danau Fmradiolaria transitional between Jurassic and Carboniferous faunas.Anisian foraminifers from allochthonous limestones of the Tanoura formation (Kurosegawa Terrane.. 98-122. Kalimantan. pahangensis n. R. 113-128. Geogr. Rettori. Similar distribution to Myophoria sandstones across Malay Peninsula) Kobayashi. Japanese J.Late Permian foraminiferal assemblages which have many provincial and endemic characters) Kobayashi.jst. (E Triassic ?). Halobia parallella Kobayashi and Halobia comata Bittner in Semanggol Fm. (Five species of Daonella (one new species Daonella pahangensis ) from M Triassic shales NW of Temerloh. J. Nam Phrom Dam.1 261 www. p. p. 75-187. p.. 2. Sci. jp/DKoseibu/pdf/Ref_0211_.E Carnian) and 3 km NW of Kampong Awah (C Pahang. (Review of Triassic bivalves Claraia. Pecten (Entolium?). Kobayashi et al. Tamura (1983). Thailand and Sumatra) Kobayashi. University of Tokyo Press. Temerloh. SW Singapore. Tokuyama (1959). distributed from Europe-Himalaya to Borneo. Bibliography of Indonesia Geology . Japan Academy 59. chegarpahangensis n. New faunas with Daonella sumatrensis Volz (originally described from N Sumatra) from Na Thawi at Thai-Malay border area. Geol. Kobayashi & R.1 262 www. University of Tokyo Press. Paragondolella polygnathiformis. Borneo is junction of three Monotis seas: (1) salinaria group. incl. T.. In: T. with Epigondiella mungoensis. Also samples from chert of Semanggol Fm at Tawar (S Kedah. p. Japan.u-tokyo.vangorselslist.l. 12. 12. & K.The Halobiidae from Thailand. J. T. T. In: T. West Malaysia.Myophoria (s. (Triassic conodonts from N Kedah. J. verbeeki. (online at: http://umdb. megalodontids in Malay Peninsula. Daonella-Halobia. kwaluana. fauna described by Newton (1923)) Kobayashi. p. poorly preserved Late Triassic neritic bivalves from Jurong Industrial Estate.Triassic conodont biostratigraphy in Kedah. 2-4. etc.). 88-137. (Family Trigoniidae evolved from Myophoriidae polyphyletically in M and Late Triassic. Myophorids from Padang Beds of Sumatra limited to 3 Norian species of Costatoria)) Kobayashi. 201-227. Costatoria). pahangensis. Fac. 5. Halobia cf. Sci. & M. Thailand and adjacent areas. (1982). 2. styriaca Krumbeck (originally described from Timor) and H.sp. myophoria and other spp. late Ladinian. & M.pdf) (Late Triassic bivalves previously reported from Chiang Rai and Lampang areas. Tamura (1984). p. Malaysia. p. sp. pichleri.) Geology and Palaeontology of Southeast Asia. T. Tamura (1968). mainly P. (Lake Toba area 'Kualu Fm' open marine mudstone with Carnian deeper marine bivalves Halobia tobaensis n. 113-123. Fauna similar to Katialo Fauna of Sumatra described by Krumbeck 1914 (?) and also to Mount Faber. Trigoniaceae (incl. sect. Geogr.. (1973). C. & M. p. 5.com March 2014 . Toriyama (eds. Kobayashi et al. Carnian-Norian subdivided into four zones based on Halobia species) Kobayashi. Tokyo. myophoria. 91-113.Upper Triassic Halobia (Pelecypoda) from North Sumatra with a note on the Halobia facies in Indonesia. (eds. Cassianella cf. In: T. Toriyama (eds. 138-150. 5.) Geology and Palaeontology of Southeast Asia 25. viewed as M-U Triassic foreland or fore-arc basin along W side of E Malaya Terrane (Ismail 2007). etc. University of Tokyo Press. Bukit Kechil (probably Ladinian.ac. Monotis. (eds. 27-30. In: T. Ed. In: T. With 17 species. Also Daonella cf.) 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Geology and Palaeontology of Southeast Asia 23. Jurong-Singapore. T. University of Tokyo Press. probably of Early Norian age. Kobayshi & R. 1. Cardium scrivenori n. (2) ochotica group from Siberia to Borneo through Japan and (3) subcircularis group from Canada to New Zealand and Borneo through E Pacific coast) Kobayashi. Univ. p. incl. E Carnian)) Koike.Upper Triassic pelecypods from Singapore.) and Bukit Kodiang (E Carnian?.The Arcto-Pacific Realm and the Trigoniidae in the Triassic Period. Presence of Neoschizodus.Triassic conodonts from Kedah and Pahang. All species related to Carnian of Alpine-Himalayan region) Koike. & A. Myophoria. Towapteria. New Mexico Mus. Palaont. Cladophlebis spp. 22. (1968). D. H. and 'East Asian floristic zone' . (On thin-walled molluscs Claraia spp. Norian of Timor Leste)) Komatsu. Float collected by Boehm in Wai Sifu River at Bara Bay. and similar to Norian Tonkin Flora of N Vietnam.. In: T. Todites goeppertianus. Kobayashi & R. (Description of Late Triassic (E Norian?) flora dominated by Equisetites arenaceus. University of Tokyo Press.go. etc. (Brief review of Triassic conodont faunas in Malay Peninsula. now called‘Krusin flora’. (‘Remarks on the ammonites from the asphalt shales of Bara Bay.) The Global Triassic. Hist. E.Summary of Triassic conodonts of Southeast Asia. p. (online at: www.T. Paleobiogeography based on conodonts: Triassic of SE Asia.. p. Nat. Anisian-Ladinian and Carnian and W Timor. Neues Jahrb. p. 5. T. 8. Toriyama (eds. etc.T.jstage. Dictyophyllum cf. 125-178. Belongs to Dictyophyllum-Clathropteris floral province of E Asia/ SW Pacific. F. Thailand and Indonesia (Carnian of Lake Toba. Science Bull. Geol. J. In: S. p. which lies unconformably over Permian limestone in Khorat Plateau. Ed. Chen (2007).Koike. p. Innsbruck 3.G. similar to 'Yamaguti Flora' of Japan. 470- 483.Faunenprovinzen in der Trias und ihre Bedeutung fur die Klarung der Paleogeographie. & K. Kobayashi et al. ('Faunal provinces in the Triassic and their significance for paleogeography'. (eds. Thailand.) Geology and palaeontology of Southeast Asia 10. Todites.. 25. Eumorphotis. nilssoni. Huyen & J. contains Jurassic 'Buru Limestone' with inoceramids and belemnites. NW coast of Buru. Buru’. 15 plant species from Sadong Fm. T. Huyen & J. southernmost occurrence of Dipteridaceae flora of SE Asia in Borneo in U Triassic) Kon’no. Botany. (1973). (1972). open marine bivalves) Komatsu. in basal Triassic calcareous mudstones of Yangtze Block of S China and N Vietnam) Kon'no. (eds.1 263 www.com March 2014 . In: T. 295-302. Flora similar to 'Tonkin flora' of N Vietnam and belongs to Dictyophyllum.) Geology and Palaeontology of Southeast Asia. is in Tethyan faunal province.Mesozoic plants from Khorat. J. p. D. p. Clathropteris miniscoides... Kobayashi et al. by Dobruskina 1994)) Kon'no.jp/article/jgeography1889/115/4/115_4_470/_pdf) (Similar to paper below: E Triassic Claraia.Bemerkungen uber die Ammoniten aus den Asphaltschiefern der Bara-Bai (Buru). 41. No stratigraphy details (Hutchison 2005: associated in same formation Carnian-Norian bivalves Halobia and Monotis salinaria and sands derived from Serian Volcanics) (Krusin flora classified as Carnian age. Probably of Late Carnian age. p. Bd. but was subsequently re-identified as Neotibetites of Late Triassic (Norian) age by Krumbeck 1909.Some Late Triassic plants from the Southwestern border of Sarawak. T. Miner. Beil. Asama (1975). (1906).Clathropteris flora of SW Pacific floral province) Kossmat. without any European or North Asian floral elements. in Huai Hin Lat Fm. generally crushed Tissotia weteringi.Depositional environments and fossil bivalves in the lowermost parts of the Triassic systems in North Vietnam and South China. In:T. 149-171. 1913) Kozur. Mitt. etc.Bivalve assemblages in North Vietnam and South China following the end-Permian crisis. Geography (Chigaku Zasshi) 115. 93-105. London. 686-691. Also common flat pieces of dark bituminous shales with numerous ammonites. Geol. Lucas & J. (Description of Cuxthropteris (=Clathropteris) meniscoides from near SW border of Sarawak. 384. Chen (2006). Linnean Soc. 1-41. (Plants from beds near basal conglomerates of Halobia-bearing coaly series near Krusin. 61. This ammonite was interpreted by Kossmat to signify Upper Cretaceous age. etc. 134-136.) Geology and Palaeontology of Southeast Asia. (1984). 12. East Malaysia. also with Chlathropteris meniscoides. With Neocalamites. NE Thailand. incl. Timor. E. 4. No maps) Bibliography of Indonesia Geology . Spielmann (eds. Palaont. Sumatra.vangorselslist. incl.Some Upper Triassic species of Dipteridaceae from Japan and Borneo. E.jst. SW Sarawak.H. University of Tokyo Press.A. pdf) ('Microcrinoids from the Upper Triassic of the Tethys'. Upper Triassic Tethyan faunas remarkably similar all the way East to New Zealand. E. 82 (1989). with other Tethyan species Nodobairdia mammilata and Tethyscythere austriaca. Geol. p.-Palaont. 245-253. W Timor. (online at: http://www2.A comparison of Late Triassic agglutinated foraminifera of Western and Eastern Tethys. E. PNG Kuta Limestone and Timor). (1988). With descriptions of new taxa from Alpine Late Triassic of Eastern Alps (Austria). 245-253. Thecosmilia chlathrata) and diverse forams. p.. showing uniformity of Late Triassic Tethyan reef faunas. p. Palaont. Most common species Cytherella acuta.G. Australien. Abhand. PNG. Soc. Timor fauna includes Verneulinoides mauritii and Variostoma helictum) Kristan-Tollmann. (‘Observations on the Triassic of the SE margin of the Tethys. 37. Bundesanstalt. Ges. Ges. incl.) Ostrocoda and global events.Rhaet-Foraminiferen aus dem Kuta-Kalk des Gurumugl-Riffes in Zentral- Papua/Neuguinea. PNG Kuta Limestone and Timor).Foraminiferen aus dem Rhatischen Kuta-Kalk von Papua. Mitteil. 41. similar to same age faunas from Mediterranean/ Alps area. Mitt.Pandemic ostracod communities in the Tethyan Triassic. Coronipora. Hagen area. E. 541-544. Involutina liassica. Publ.. All species also known from West Tethys. Bundesanstalt. Galeanella tollmanni. Taurus Mts (Turkey) and Norian 'Hallstatt Limestone' at Bihati near Baun.at/pdf_frei_remote/AbhGeolBA_41_0245-0253. Similar Triassic ostracode faunas on N and S sides of Tethys (Timor. Abhand. Mt.landesmuseum. Geol. E. etc. 4. (1988). 291-317. etc. (online at: http://www. 5. Publ.Papua New Guinea. (First description of Rhaetian foraminifers from Kuta limestone. Maybury (eds.pdf) (Examples of common species of Triassic arenaceous and calcareous agglutinated foraminifera across Tethys realm (mainly from Austrian Calcareous Alps. PNG Highlands. etc. Mitteilungen Osterreich. p. British Micropal. p.vangorselslist. Innsbruck 17. Incl. Fauna of Tethyan affinity.at/pdf_frei_remote/AbhGeolBA_41_0245-0253.). Leiocrinus krystini. Includes discussion of Kubor terrane Rhaetian Gurumugl reefal limestones ESE of Mount Hagen. 78 (1985). 51-100. (1988). Vienna. E. No stratigraphic info) Kristan-Tollmann. Whatley & C. Glomospira/ Glomospirella) Kristan-Tollmann. NW Australia)) Kristan-Tollmann. 201-222. fore-reef (crinoid detrital limestones with Variostoma cochlea. Vienna.com March 2014 . (1990). Semiinvoluta. Osterr. (1988). Geol. 1880-1890m. L. (1986). 41.).at/downloads/c715/gpm_17/051_100_17.Neuguinea. E. Australia and New Zealand.Beobachtungen zur Trias am Sudost-Ende der Tethys. which contains latest Triassic corals (Montlivaltia norica. (1986). (Remarkable uniformity in Triassic faunas throughout Tethyan region. In: M. p. Monatsh. Involutina liassica.ac. Geol. (Tethyan Late Triassic ostracodes in Sahul Shoals 1 well. incl.landesmuseum. In: R. W Kundiawa. More detailed account of Latest Triassic foram assemblage of 85 species from W part of Gurumugl Reef. suggesting Rhaetian age) Kristan-Tollman. Timor fauna includes Verneulinoides mauritii and Variostoma helictum) Kristan-Tollman.uibk. Audley-Charles & A. p. E. gracilis. E.Unexpected microfaunal communities within the Triassic Tethys.pdf) (Examples of common species of Triassic arenaceous and calcareous agglutinated foraminifera across Tethys realm (mainly from Austrian Calcareous Alps.) Bibliography of Indonesia Geology . Australia NW Shelf.A comparison of Late Triassic agglutinated foraminifera of Western and Eastern Tethys. (online at: http://www.1 264 www. Both planktonic and benthic organisms. Neuseeland. p.) Gondwana and Tethys. Tetrataxis. Geol.Mikrocrinoiden aus der Obertrias der Tethys. Geol. Very little on SE Asia) Kristan-Tollmann. London. etc. (1991). ('Rhaetian foraminifera from the Kuta Limestone of the Gurumugl Reef in central PNG'. Hallam (eds.Papua/ Neuguinea. NW Australia.Kristan-Tollman. Spec.) and lagoonal (low diversity with Angulodiscus. Bihaticrinus manipalus. 213-223. Soc. 211-289. Three biofacies types: near-reef (with Trocholina.. Ed. Neues Jahrbuch Geol. Haq et al. J. Saito Hoon Kai Spec. including Timor and PNG.J. Trocholina spp. 82. Centralblatt. 2008) Kristan-Tollmann. Geol. Part of Alpine Late Triassic. nebst ihren Faunenelementen. Hasibuan (1990). Shallow Tethys 3. Geol.ac. fascigera. Nearly all genera known from W Tethys. Neues Jahrbuch Geol. I. 467-492. & J. liassica usually signifies lowermost Liassic). similar to other Tethyan/ 'Alpine' foram faunas.U. 1909.Ostracoden aus der Obertrias von Misol (Indonesien).vangorselslist.Kristan-Tollmann. Lower Liassic yellow echinoid-mollusc limestone samples dredged from submarine Exmouth Plateau from >2000 m water depth. p. E. turgida. Innsbruck 20.at/downloads/oegg/Band_84_301_308. Dickins et al. Himalaya') Kristan-Tollmann. Geol. Oesterr. 80.uibk.(although these may be found in latest Triassic. Mitteil. 84. but found here for first time in E-most Tethys. In: U. Sample 96 DR 30 with distinct foram fauna with Involutina liassica. see also Chablais et al. B. p. 561-562. SW of Soe. confirming Tethys-wide distribution) Kristan-Tollman. suggesting close similarity of faunal communities throughout Tethys realm) Kristan-Tollmann. & V. Eoconusphaera zlambachensis and Prinsiosphaera triassica are most common species in uppermost Triassic of calcareous Alps. E. 1-11. E.pdf) ('Alpine Enzesfelder Limestone (Lower Liassic) from the Exmouth plateau. salinaria) by Gruber) Kristan-Tollmann.are Upper Triassic in age) Bibliography of Indonesia Geology . Monatshefte 1987. (online at: http://www2. 463-474. 301-308. With descriptions of U Triassic and Liassic ostracod assemblages and Liassic calcarous nannofossils by Kristan-Tollman. echinoderms. Geol. Small ostracod fauna from marine Early Carnian?.Anmerkungen zur Mikrofauna der rhaetischen Kiotomergel von Kumaun. & F. p. Results 122. Scient.Kurze vorlaufige Mitteilung uber eine neue obertriadische Fauna aus den Molukken. (Upper Triassic (Norian. One new form (Hasibuana asiatica)) Krumbeck.com March 2014 .) and Monotis (M. NW Australia.Weitere Beobachtungen an Rhatischen nannofossilien der Tethys. and revision of U Triassic mollusc genera Halobia (H. Ed. Similar to Enzesfeld Fm in Northern Limestone Alps in Austria and also from Timor. Osterr. Mitteil. (1909). ('Remarks on the microfauna of the Rhaetian Kioto-Marls from Kumaun. and ostracodes).) Proc. 3. E. Ammonites from Buru interpreted as Cretaceous by Kossmat (1909). Kotaka. (1995).Rhaetian fauna. E. p. 5. abundant I. with no Pacific faunal elements. rugosa. H. Ocean Drilling Program (ODP)..Rhaetian) E Jurassic thin-bedded marls-limestones and faunas from deep marine 'Aitutu Fm'. Palaont. p. etc.Jurassic facies belt that stretches for >15. radiata. Pal. ('Ostracods from the Upper Triassic of Misool'. L.1 265 www.uibk. & F. von Rad. (Limestone samples from ODP site 764 and Sonne cruise 1979 dredge samples from N side Wombat Plateau have Norian. In: T. Ges. S.ac. Gramann (1992). Close faunal and lithological similarities with members of age-equivalent 'Hallstatt facies' rocks in Eastern Alps (W Tethys).Potschenschichten.M. Gruber (1987). Himalaya. Ges. (eds. (First description of U Triassic foraminifera from Panthalassan seamount reefal limestone in Sambosan accretionary complex in Japan. (online at: http://www2. p.at/downloads/c715/gpm_20/20_001-011. 8. p. 35-49. E. mainly along Meto River. SW part of W Timor.) Proc. also present off Wombat Plateau. Mitteil. (eds. 173-181.. Osterreich. Palaont. Publ. Miner. NW of Australia'. Obertrias) und Liasfleckenmergel in Zentraltimor. Zlambachmergel (Hallstatter. Colwell (1991). Sendai 1990.Paleontological evidence for the Triassic age of rocks dredged from the Northern Exmouth Plateau (Tethyan foraminifers. Gupta (1987). etc. (1991). Barkham & B. Symp.Triassic Tethyan microfauna in Dachstein limestone blocks in Japan. Ges. Geol..Int.000km from Alps to Australia-PNG) Kristan-Tollmann.Alpiner Enzesfelder Kalk (Unter-Lias) vom Exmouth-Plateau NW von Australien. p. E. H. Mitteil. ('Brief preliminary communication on a new Upper Triassic fauna from the Moluccas'.pdf) ('Additional observations on Rhaetian nannofossils of the Tethys'.. 229-285. bituminous platy limestones. Placunopsis.). 142 p. L. etc. Pecten. etc. and overlain by Eocene sandstones of Ombilin Basin). IV. Halobia sumatrana n. Bituminous platy limestone and marls. ?Megalodon. fish scales. 1-38. (1911). Der Athyridenkalk des Misol-Archipels. Anadontophora. Nucula.-Buru). (Also similar to Jurong Fauna of Singapore. 5. ('Upper Triassic of Sumatra (The Padang Beds of West Sumatra…'.1 266 www. Lima.sp. 3. despite same age as Fogi Beds of Buru?)) Krumbeck. marly fossiliferous. 5. condensed 'Halsttter facies'. Palaeontographica Suppl.. Ed. Savu. Geologie Niederlandisch-Indien II. p. Brachiopod Limestone (rel. Geologie Niederlandisch-Indien II.part 1. (1921). rare).. The asphalt beds at Sifu (NW Buru)'. Cardita. Dissert. A. L. Schweizerbart. Pecten (Aequipecten) verbeeki.Uber die Fauna des Norischen Athyridenkalkes von Misol. Pinna.sp. Klippen/ Fatu coral reefal limestone. L. Burmesia. etc. with distribution of ages and facies and comparisons to Triassic in other regions. Pinna blanfordi. (1913b) Obere Trias von Buru und Misol. Rich in fossils: mainly bivalves (Pseudomonotis. Palaeontographica Suppl. 1-119. Beitr. 1. Extensive overview of Triassic occurrences on Timor. Macrofaunas collected by Boehm and Wanner from the lower Norian? Fogi-Beds of W Buru. crinoids (Pentacrinus). Protocardia. 3. A. Halobia limestone and shales) Bibliography of Indonesia Geology . pectenids. Geologie Niederlandisch-Indien II. Cephalopod Limestone. Alectryonia. Macrofaunas collected by Boehm and Wanner from the ~50m thick Athyrid Limestone of the Misool islands. shallow marine dark grey limestone with grey and yellowish marls with corals (Thecosmilia cf. Includes some corals (Thecosmilia). Geologie Niederlandisch-Indien II.Die Brachiopoden. p. Sagenites. Roti. Krumbeck. In: J. Cardita globiformis. etc. Aulacothyris). Five main facies: 1. ammonites (Neotibetites weteringi). C. Neotibetites weteringi) and brachiopods (Misolia).Obere Trias von Sumatra (Die Padang-Schichten von West-Sumatra nebst Anhang). clathrata). Schweizerbart.Krumbeck. ('Upper Triassic of Buru and Misool.. Cardita.. L. I. (1913c) Obere Trias von Buru und Misol. but not very deep marine dark marls and limestones with bituminous limestone interbeds (up to 19% bitumen). p. Lamellibranchiaten und Gastropoden der Trias von Timor. No illustrations) Krumbeck. The Fogi Beds of West Buru'. Stratigraphic part’. IV. Stratigraphy. (1914). 120-127.vangorselslist. The Athyrid limestone of the Misool Archipelago'.paleontology of >210m thick Upper Triassic Padang beds from two main localities Lurah Tambang and Bukit Kandung/Katialo. C. hydrozoans (Heterastridium). ('Upper Triassic of Buru and Misool. bivalves and gastropods from Timor. 17. 128-161. Die Fogi-Schichten West Burus. (‘On the fauna of the Norian athyrid limestone of Misool’. N India Himalayas) Krumbeck. Poorly fossiliferous clastics with four layers of dark. IV. Tibetites. Rel. B. bivalves (Pecten. incl. L. Myophoria myophoria. brachiopods (Spirigera. Macrofaunas collected by Boehm and Wanner from Triassic (Lower Norian?) asphalt beds of NW Buru: bivalves (Pecten). Gervilleia bouei. Myophoria. Palaeontographica Suppl. HvG) (Absence of Misolia. described by Volz 1904. (‘The Triassic brachiopods. 2.com March 2014 . 1.W. p. Faunas similar to Juvavites Beds of Spiti. Beitr. also ammonites (Sibirites. stromatoporoids. Distal. hydrozoa (Heterastridium). Most similar to fauna from Napeng Beds.) Palaeontologie von Timor 10. Wanner (ed. off S Misool. Stratigraphischer Teil. Beitr. often oolitic. p. L.. Die Asphaltschiefer am Sifu (N. Upper Birma as described by Healy 1908). 2. Palaeontographica Suppl. Based on collections from 1911 Wanner and Molengraaff Timor expeditions. With review of geologic setting by Verbeek of Triassic beds E of Lake Singkarak in Padang Highlands (Triassic overlies Permocarboniferous granites. Kobayashi & Tamura 1968) (Some species described earlier by Boettger 1881. 195-266. B. clastics and fusulinid limestones. rich in thick-walled bivalves that look related to Carnian North-Alpine Cardita facies (38 species. Age similar to Fogi Beds) Krumbeck. Stuttgart. 4. (1913a) Obere Trias von Buru und Misol. etc. Cassianella verbeeki n. but erroneously assigned E Eocene age. Brief description of macrofauna of ~50m thick limestone rich in Misolia brachiopods from S coast and ilands Jillu. ('Upper Triassic of Buru and Misool. 1. Friedrich-Alexanders- Universitat zu Erlangen. 2. Beitr. IV. 2. (1931). Lett... B. p. Schweizerbart. Akad. Bull. (Triassic brachiopods.Scythian ammonoids from Timor. Neues Jahrb. central Malay Peninsula (= E Malaya/ Indochina terrane?: HvG). p. Ed. L. etc. 1. Beitr.. p. Beyrichites. Ser. (Brachiopoda) from the Upper Carnian Hallstatt limestones of Timor (Indonesia). Komm.Anisian ammonoids from Malaya. Brachiopoden. p. B.Integrated Upper Carnian to Lower Norian biochronology and implications for the Upper Triassic magnetic polarity time scale. and Monotis bed at Wai Ehana (typical Monotis limestone rich in Monotis salinaria). p. 22. Incl. Geologie Niederlandisch-Indien III. Norian Kanikeh Beds with Myophoria.) Kutassy. Wanner (ed. p. 349-351). & M. (online at: http://www. Trigonia. Ptychites.org/page/4294222page/308/mode/1up) (Description of Lower Triassic ammonites from Wanner. (1968). Verhandelingen Geol.org/details/bulletinofmuseum13719681969harv) (Treatise on Early Triassic/ Scythian ammonoids. 1-275.-Mijnb.org/details/breviora121178harv) (M Triassic ammonites from folded dark grey shales 10. mainly from 'Block E near Nifoekoko'.Triadische Fossilien vom Portugiesischen Timor. Owenites. 343-351.Austriellula robusta n. Trachyceras (Paratrachyceras).Ein Choristoceras Vorlaeufer (Ceratitina. Himalayas and Timor) Krystyn.5 miles SSW of Kuala Lipis. & J. III. Zoology.vangorselslist.185-246. 4.) Palaeontologie von Timor 13. Timor. Palaeontologischer Teil. L.. Wiedmann (1986). ('Geological results of Deniger’s 1912 trip in the Moluccas.biodiversitylibrary. (Summary of Upper Carnian. Lamellibranchiaten und Gastropoden aus der oberen Trias der Insel Seram (Mittel-Seram). bivalves and gastropods from Timor.archive. Stuttgart. based on data from Alps. Many specimens manganese-coated. IV. 5. (Online at: http://www. On Carnian Halobia shales of Wai Isana near Manusela with Halobia spp. Deninger's in den Molukken. Breviora. (New rhynchonellid brachiopod species from Carnian (U Triassic) of Baun. described previously by Welter (1922). Contains Hungarites spp. Pronorites spp. 1-8. (1923). 137. Breviora 124. (1960). (‘A Choristoceras ancestor (Ceratitina. L. p. Sicily. (1969).Ammonoids of the Late Scythian (Lower Triassic). Y. Also Misolia Limestone) Krumbeck. III. Acrochordiceras and Ptychites) Kummel. bivalves and gastropods from the Upper Triassic of Seram island (Central Seram)'.. Ammonoidea). Mae Moh River). Siblik (1983). 49-56.Lower Norian ammonoid. Besse & J. collections. Bibliography of Indonesia Geology . Brachiopods. L. Cladiscites beyrichi. Palaeont. Geol. 1986. 259-266. etc.1 267 www.Geologische Ergebnisse der Reisen K. p. Marcoux (2002). including material from Timor (p. 1-21. Pahang. J. p. (1960). (online at: http://www. 203. B. 5. Osterreich. Jonker. aus dem Nor von Timor. Sturia sansovinii. Earth Planet. Lobites). Paleontology 34. A.Die Brachiopoden. 27-37. all from isolated blocks from extremely condensed sections. IX. In: J. Comparative Zoology. 682-694. p. Prosphingites) Kummel. Ammonoidea) from the Norian of Timor’) Kummel. Contains Tethyan species Paraceratites trinodosus. Geol. Monatshefte. Turkey. Gallet. (1924). 5. etc. Sturia) and Carnian (Joannites. Lamellibranchiaten und Gastropoden der Trias von Timor II. J. Cardita. From ‘Halstatt facies’ ammonite-rich limestone blocks in Tertiary olistostrome in SW Timor) Krystyn. Balkans.Triassic ammonoids from Thailand. Sci. Harvard.part 2. None of Triassic localities and faunas known to date from mainland SE Asia anywhere comparable to abundance and diversity of faunas known from Himalayas and Timor) Kummel.archive. Schriftenreihe Erdwissensch. Mainly addendum to Welter (1922) monograph. L. sp. B. Wissenschaften. conodont and halobiid biochronology. showing presence of Anisian (Balatonites. Mus.com March 2014 . Paleontological part) Krystyn. 311-701. Gen. Museum Comp. (First Triassic ammonoids from N Thailand (Doi Chang.Krumbeck. 1. Palaeontographica Suppl. Tropigymnites. 283. In: G. Comptes Rendus Acad.. Assoc. Cyprus.Mesozoic brachiopods of Misool Archipelago. a new foraminifer from Upper Triassic reefal facies in E. Ta (1998). Association with Triasina hantkeni and conodont Miskella posthernsteini suggests U Rhaetian age (species subsequently also found in Asinepe Lst of Seram. deposited on wide. 326. Palaeogeogr. 1-2.(Triassic fossils from Von Loczy 1922 expedition in S part of Portuguese Timor near Suai. (2008). three varieties of Von Seidlitz (1913) are synonyms).vangorselslist. typical of Late Triassic reefal carbonates. 41. p. S. Ninh Binh area (Song Da Terrane. (2) oncolitic grainstones. Ed. Cornee & M. R. L. Indonesia).) Martini. Mem. (Ammodiscidae. 149-177. 3. C. 75-102.. Wombat Plateau and Sinta Ridge all part of same N Australian margin marine bioprovince) McRoberts. p. E Sulawesi. Shi (ed. p. subfam.J. (New genus name Claviatractites proposed for belemnite originally described as Atractites claviger by Von Bulow (1915) from Late Triassic of Timor. N Vietnam).T. R.A. Aucklandirhynchia yefbiensis. (Species of marine bivalves of pectinoid genus Monotis provide useful biochronologic indices for Late Triassic (M Norian–earliest Rhaetian). p.Upper Triassic carbonate deposits of Seram (Indonesia): palaeogeographic and geodynamic implications. and Prochlidonophora spinulifera of Austral affinity and Ptilorhynchia pugnaciformis belongs to Circum-Pacific or bipolar genus) Mariotti.. Palaeoclim.sp. 113-119. Turkey. Pignatti (1995). Surviving Monotis dwarfed compared to Norian predecessors) Bibliography of Indonesia Geology . (online at: http://archive-ouverte. 2. incl. L. Sulawesi (Kolonodale area. Vachard & L. Grant-Mackie (2011). Mostly from folded deep-water marly limestones with ammonites. belemnites (Aulacoceras striatus) and pelagic molluscs Daonella indica. Zaninetti. E Sulawesi. Lathuilliere. N. shallow water carbonate platform. Halobia styriaca) MacFarlan. Sambosan accretionary complex in Japan.S. South China Block.. With Glomospirella. Arenovidalina. Hasibuan & J. Karakorum. Tran & T. Zaninetti. Australasian Palaeont.A. 45-52. B. Palynology suggests Seram-Buru Block more tropical than Sulawesi/ Kolonodale Block. 5. Villeneuve (2004). Affinities to coeval faunas from N Malaysia and S China Block suggest connections during Triassic between continental blocks of Indochina Peninsula) Martini.) Brachiopods: extant and extinct. J. Geochemical and geodynamic interpretations placed Seram-Buru Block as derived from New Guinea. Four new Late Triassic species. J. Aucklandirhynchia yefbiensis) and three Cretaceous. Proc.ch/unige:35376) (New small.Decouverte de foraminiferes du Trias dans les calcaires de la region de Ninh Binh (Nord-Vietnam). Lower Triassic(?) to Anisian benthic foraminifera in Dong Giao Fm limestones.). etc. Villeneuve. Four reefal facies: (1) boundstone forming buildup cores with calcisponges and calcareous algae.J. Ser.com March 2014 . a new xiphoteuthidid cephalopod from the Upper Triassic of Timor. <20% coral.)) Martini.B. Biogeographically fauna is Perigondwanan (or S Tethyan). p.A. Revue Paleobiologie 14. Cornee. IIA. Sci. only one previously described (Rhaetian Misolia misolica.1 268 www. Palaeopelagos 5. complex agglutinated ammodiscid foraminifera species Pilammina sulawesiana from Norian- Rhaetian limestones of Kolonodale area. Profound extinction event in pelagic realm at Norian-Rhaetian boundary where c.Pilammina sulawesiana n. Brachiopod Congress.. & J.. etc. Palaeoecology 206. n.721-735. N. two Jurassic (incl. p. 6th Int. D. eastern Indonesia. Meandrospira. (3) foraminiferal packstone-grainstones. waist is narrower. Palaeontology 51. Cirilli. because Atractites has ventral furrows. F.Rhaetian (Late Triassic) Monotis (Bivalvia: Pectinoida) from the eastern Northern Calcareous Alps (Austria) and the end-Norian crisis in pelagic faunas. Zugmayerella bogalica. Foraminifera suggest Seram. etc.unige. 455-460. Carnian-Norian to Rhaetian Asinepe Lst (=Manusela Fm) part of allochthonous series. (Seram Upper Triassic limestones of Gondwanian-Australian type in ‘Parautochthonous’ and of Laurussian- Asian type in ‘Allochthonous’.R. Melbourne 2010.Claviatractites. R. 15 monotids became extinct. D. but cooler than Timor/ NW Shelf. (Mesozoic brachiopod fauna of Misool ten species. M. ('Discovery of Triassic foraminifera in limestones from the Ninh Binh Area (North Vietnam)'. Zaninetti (1995). Pilammininae. (4) foraminiferal-megalodont mudstones. N Italy. Koike. incl. and Metapolygnathus spp. p.S. 3. overlying Halobia- Daonella shale.vangorselslist. Faunas correlate with similar faunas from Chuping Lst of Perlis.Lower and Middle Triassic conodonts from the Jerus Limestone.Lower Norian and conodonts. Peninsular Malaysia. Peninsular Malaysia.wordpress. Also Bibliography of Indonesia Geology . N Sumatra) Metcalfe.f Southeast Asian Earth Sci.pdf) (Conodonts representative for all Triassic stages. Halobia (Carnian-M Norian). 201-219. NW corner of Peninsular Malaysia (= Sibumasu Terrane). p. Magazine 127. Kedah. found in Malay Peninsula. I. Daonella (M Triassic).. I. Southeast Asian Earth Sci. Haile (1979). 191-194. London.) The Pre-Tertiary fossils of Sumatra and their environments. Triassic of Malay Peninsula three regions: (1) Elongate carbonate platform complex on Sibumasu block (Chuping Lst. Metcalfe. p.McRoberts. (1989).Lower Triassic (Smithian) conodonts from northwest Pahang Peninsular Malaysia. J. supporting pre-E Triassic rifting of W Malay Peninsula (Sibumasu) from Gondwana) Metcalfe. 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(Five biogeogeographic areas in Circum-Pacific region. A.Conodonts of Dienerian age (Early Triassic) from northern Thailand. Heterastridium conglobatum.Famennian conodonts in W Thailand mostly cosmopolitan species. (2) Kana Fm detritus from acid volcanics (with Triassic Costatoria. (5) Maril Shale (U Jurassic Buchia malayomaorica. (https://www. Territory of New Guinea. Mineral Res. HvG). Wellington 2006. probably Lower Jurassic Balimbu greywacke. New Caledonia.. 126..M. Associated with volcanics. S. Yuat Fm black shale with Late Anisian ammonites. Bur. Grant Mackie (1998). In: V. etc. Bismarck Mts and Central Highlands five sedimentary units.Carnian sandstones-shales with halobiid bivalves.000 Sheet area.G. Parapopanoceras. Bur. Geoph. Japan. (4) Jurassic Mangum volcanics.. Howell (ed. Orchard (2006). Timor.gov. Mineral Res. Inoceramus cf. T. N America. S. Bull. 2. China.K. Spiriferina). Kobayashi (ed. Ed. Timor. originally described from Timor). haasti)) Skwarko. etc. Geol. 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('The genus Stromatoporidium Vinassa de Regny from the Upper Triassic of Timor island (Hydrozoa)') Tamura. Bur. Kl.Claraia from North Malaya. (1973). Bull. Miner. bivalves and conodonts (Misikella) E of Mt Hagen. Yuat River gorge in W Highlands with Anisian cephalopods (Beyrichites. M. Papua New Guinea.com March 2014 .K. 150. Geol. Bull. intermedia multistriata and C. S.-Naturw. Wissensch. Bull.) and two corals (Pamiroseris rectilamellosa. Branching spongiomorph (Spongiomorpha sp. Bibliography of Indonesia Geology .. 5.S. 217.Spia. a new Triassic bakevellid bivalve from Papua New Guinea. conodonts and brachiopods of the Kuta Formation.) Skwarko.K.Upper Triassic spongiomorph and coral association dredged off the northwestern Australian shelf.K. Palaeontological papers 1969.K. Toriyama (eds. Kummel (1974). Rowley Terrace occurrences may be E-ward extension of Wombat reefs.. p. C Malay Peninsula: C. 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(‘Gastropods from Triassic Halstatt limestone blocks of W Timor’. Most common genera Arcestes. C. 1973). Kobayashi. East Malaysia. Hashimoto.landesmuseum. & C.Monotis subcircularis Gabb from Sarawak. Palaeonucula. Palaeoworld 20. 4. Can be correlated with E zone of Changning-Menglian Belt in SW Yunnan. p.. 119-133. (M Triassic (Anisian) radiolarians from bedded chert in Chiang Dao.Lower Triassic conodonts from North Vietnam. Ed. Grant-Mackie. 15. Trias) der Tethys aufgrund neuer Untersuchungen in Timor. Nuculana. subcircularis.1 277 www.H. Acta Palaeontologica. J. G. SE of Kupang. ) Tamura. Q. Bundesanst. (online at: http://hw. Kl. (1979). University of Tokyo Press. Hon (1977). H. Wiss. Toriyama (eds. 103-149. SW Timor Bihati River limestones with abundant ammonites and rare gastropods.M Triassic sequence. F. Verhandelingen Geol.The Triassic system of Malaysia and adjacent areas. Revision of abundant Norian ammonoids from blocks of condensed. p. 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(’Orthocerids and belemnites from the Triassic of Timor’.Ammonoidea leiostraca aus der oberen Trias von Timor. In: J. 2: Trias in Borneo. D. 75-118. Atractites spp. Indie 55 (1926). D. 217-220. (1915). (1982). etc. (1926).) from Molengraaff. 5. E. Palaontologie von Timor. CCOP Techn. Montlivaltia). (1915). pachyporidae (Lovcenipora). East Timor (Nine coral species in common with alpine Zlambachschichten. 1-173. 4.Tozer. Bull. Vietnam) Vinassa de Regny. Savu and Roti. etc. Resembles microfauna from Kodiang Lst of NW Malay Peninsula and Namyua Gp in E Burma. and resembles Kodiang Lst of NW Malaysia and various outcops of Sumatra) Vachard. Philippines (Malajon Island). Dictyoconites spp. E. species of Thecosmilia. oncoliths. (Illustrations of U Ladinian. (Late Triassic algae (Solenopora). 135-141.Biostratigraphic importance of Triassic foraminifera and algae from South- East Asia. Mainly on taxonomy of straight nautiloids (Orthoceras spp. stromatoporidae and bryozoa. 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('Leiostraca ammonites from the Upper Triassic of Timor'. Verhandelingen 2. Palaont. Duotaxis. Revue Paleobiologie 7. (Carnian-Norian Aulotortus assemblage of Thailand characteristic of Tethyan province. 8.Marine Triassic faunas of North America: their significance for assessing plate and terrane movements. Ed. p. Schweizerbart. ser. Stuttgart. 87-98. 7. p. (1988). p.Norian ammonites described from Timor (66% endemic. (1989). Spongien. Gafoer (eds. Carnian-Norian belemnites in bright limestones. CCOP Techn. p. 5. 211-214. (1907). C. Soc. Review of Triassic-Cretaceous floras.. B. First author to recognize Alpine/ Tethyan affinities of the Late Triassic bivalves and ammonites of Seram and Timor) Wanner. Beilageband 24. E Seram. Neues Jahrbuch Min. Y.Notes sur des bois Mesozoiques et Cenozoique du Viet-nam et du Cambodge. p. but also ‘Pacific’ mollusc Pseudomonotis ochotica). (’Triassic fossils from the Moluccas and Timor Archipelago’. Ed. Absence of fern and sphenophytes and dominance of diminutive Pterophyllum and Ptilophyllum leaves.Triaspetrefakten der Molukken und des Timorarchipels. ('Notes on the Mesozoic and Cenozoic woods from Vietnam and Cambodia') Vozenin-Serra. Timor/Roti/ Savu Triassic reminiscent of N Sumatra Upper Triassic described by Volz. Neues Jahrbuch Min. C. Geol. 73-105.Savu (generally deeper water facies.Etat de nos connaissances sur les flores du Paleozoique superieur et du Mesozoique du Sud-Est Asiatique. W. ammonites faunas from Misool (Carnian dark shales with Daonella). Also Triassic fossils from Timor-Roti..Triassic radiolarians from the Yarlung Zangbo suture zone in the Jinlu area. Bibliography of Indonesia Geology . Additional taxa determined.Clathropteris floral province' of SW Pacific at end-Triassic (also known from Vietnam.nl/08/nr136/a04) (Flora from SW Bintan Island. clathrata and Montlivaltia molukkana and Pachypora intabulata (= Lovcenipora). Wanner. p. IV. Grenoble 1983. 169-181. For Indonesian region only mentions W Sarawak Krusin flora of Kon'no 1972. Band 32. T. Description of ichthyosaur remains from E-M Triassic of Noil Bunu. (1971).uva. Soc.Etat de nos connaissances sur les flores mesozoiques du sud-est Asiatique. 19.H. O. 1-47. p. mainly from Vietnam. Pal. Thailand. which is part of Late Triassic 'Dictyophyllum. Neues Jahrbuch Min. also known from NW Australian margin) Vozenin-Serra. Palaont. eine neue Brachiopoden-Gattung aus den Athyridenkalken von Buru und Misol. (1984). W Timor) Von Huene. (1931). Kobayashi. & J. Genus characteristic of ‘Gondwanan Tethys’. 1. 215-227. ('Status of our knowledge of the Mesozoic floras of SE Asia' .('Ichthyosaur remains from Timor'.uba.vangorselslist.A revision of the Late Triassic Bintan flora from the Riau Archipelago (Indonesia).J. Geol. (New genus Misolia for Upper Triassic (Norian) shallow marine costate athyrid brachiopod from Athyrides limestone in Misool and Fogi Beds of Buru.W Japan)) Vozenin-Serra. Nagahashi & Q. Vietnam 14. Zetang County. Interpretations paleogeographiques. but unlikely to be Early Cretaceous as suggested by Kon’no 1972) Wang. Scripta Geologica 136.1 279 www.A. Stronger similarities between Bintan and SW Asian than with SE Asian floras. van Konijnenburg-van Cittert (2008). Geologie Niederlandisch-Indien II.. southern Tibet. Mem. Riau Archipelago. 2. Archives Geol. 159-220. Zeng (2002). Sciences de la Terre.. Palaeontographica Suppl. Sinica. Differences may point to slightly younger age (E-M Jurassic). Geol. Acta Micropal. Comptes Rendus 108e Congres Nat. Amonotis and brachiopod Halorella).G. Daonella. 177-196. Beil. F. p. J. 3. corals. Late Triassic molluscs. p. France 147. Beitr. C.Ichthyosaurier von Seran und Timor. J.. etc. A.Triascephalopoden von Timor und Rotti. p. Seram (typical Tethys-Mediteranean Norian molluscs Monotis salinaria.163-194..Misolia. (1911). From Seram limestone come corals Thecosmilia aff. and Basleo. Palaont. p. partly described by Jongmans in 1951. p. 101-116. J..com March 2014 . Thailand. Savantes.. (1983). Geol. Matsuoka. 2. 1899. Yang. (online at: http://dpc. but potentially similar ‘alpine’ character with mainly Halobia. K. Beilageband 66. (1913). W Timor) Von Seidlitz. ('Status of our knowledge of the Upper Paleozoic and Mesozoic floras of SE Asia and paleogeographic interpretations') Wade-Murphy. (Triassic or Jurassic Ichthyosaurus vertebrae from Bula. Associated with white tuffs and ammonites commonly with black iron-manganese coating.A.1 280 www. Incl. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. (online at: http://retro. Chondrites gonidioides n. Eclogae Geologicae Helvetiae 42. Pal. Stuttgart. collected by Wanner and Molengraaf 1909-1911 expeditions. (‘The ammonites and nautiloids from the Ladinian and Anisian Triassic of Timor’.sp.sp.. ('Anisian Monophyllites from Timor'. timorensis n. 83-154. Band 67. Schweizerbart.(‘Triassic cephalopods from Timor and Roti’.A. HvG)) Welter. Some ammonites with black manganese staining. from S half of W Timor. (online at: http://retro. Cladiscites) and belemnites (Aulacoceras timorense)) Wanner. p. Bandung. J.. continuus) Wanner.Anisische Monophylliten von Timor.ch/cntmng?type=pdf&rid=egh-001:1952:45::440&subp=hires) (‘On the knowledge of the Triassic of Seram’. Palaeontologie des ostindischen Archipels IV. J. 19. marls. (‘The Upper Triasic ammonites and nautiloids from Timor’. New species of M Triassic ammonite Monophyllites from Oe Masih. Similar Upper Triassic limestones in C Seram. and J. p. bathyal Triassic cephalopod limestones called ‘Halstatt Facies’ from various Timor localities. In: J. Description of ‘Tethyan’ ceratitid ammonites collected by Weber from Late Triassic flysch of Wai Sabora in SE Seram.ch/cntmng?type=pdf&rid=egh-001:1949:42::702&subp=hires) ('Trace fossils from the Upper Triassic of Seram (Moluccas) and the Alps'. 183-195. (1922). limestones and macrofossils.. Upper Norian with lenses of massive Lovcenipora. Good documentation of NE Seram Late Triassic (Carnian- Norian) ‘flysch’. (1949). Flemingites timorensis n.) Palaeontologie von Timor 11. Remarkable similarities to Mediterranean and Himalayan ammonites. Triassic macrofaunas dominated by Tethyan elements like Monotis salinaria. Incl. marly limestones and calcareous sandstones. Schenk (1952). Sirenites malayicus n.Lebensspuren aus der Obertrias von Seran (Molukken) und der Alpen. p. In N of Timor age- equivalent Norian ‘Fatu’ coral limestones (Both these U Triassic carbonate facies considered part of 'allochtonous' nappe complex by Wanner 1956 and others. p. Rich assemblage of Middle Triasic ammonites (>27 genera) from blocks of thin. Eclogae Geologicae Helvetiae 45. Probably of Norian age. J. S Buru and Timor. Early paper on Triassic ammonites (Meekoceras indoaustralicum n. .Halorella limestone. J.sp.Ueber einige Juvaviten von Ceram (Molukken). 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Norian more platy limestones. 5.C. Ammonite assemblages more 'Alpine' than 'Asian' in character) Welter. reddish. (1932).Die Ammoniten und Nautiliden der Ladinischen und Anisischen Trias von Timor.sp. from Ehrat collection) Wanner. Schweizerbart. O. Knipscheer & E. Wanner (ed. ~2 m thick fossil accumulation without terrigenous sediment. 1. p. In: J. 1-258. Bibliography of Indonesia Geology . Rare loose fossil material suggests limited presence of E-M Jurassic.G. On deep-water Palaeodictyon seranense n.Zur Kenntnis der Trias der Insel Seran (Indonesien). Indie 10. O. 1. Carnian dominated by clays. Halobia spp and Juvavites. Neues Jahrbuch Miner. aff.) Palaeontologie von Timor. O. p. (1915).Cretaceous deep water marls and limestones. H. Triassic overlain by Jurassic. Taiwan..Korallen und Kalkschwamme aus dem obertriadischen Pharetronenkalk von Seran (Molukken). 4. Seranella. Yeh. III. (‘Remarks on the ammonite and nautilid fossils collected by Deninger from Seram’. 12. p.com March 2014 . Timor 'Bihati C' fauna has more Mediterranean than Asian elements) Welter. 196- 197. Vinassaspongus subsphaericus. Mus.. Nat. Geol.) Palaeontologie von Timor 11. (1963). Stuttgart. etc). Sect. Includes new coral species Thecosmilia alfurica. Band B77. Congr. (Abstract only) (Rich Triassic radiolaria in ~100m thick section of bedded siliceous rocks N of Mae La Noi. Radiolaria Newsletter 28. 4. Wanner (ed. 155-159. Many similarities with Himalayan- Mediterranean Triassic faunas.. I). Believed to be part of Permian-Jurassic Liminangcong. Nat.. p. 5. Juvavites) and nautilids (Phoioceras) from C Seram resemble species known from Timor and of 'alpine' affinity) Westermann. etc. (1937). 171-211. Geol. Branch. Chert in uppermost part of section with significant siliciclastics and carbonate minerals. N Palawan Block.nmns. In: J.edu. Nat.E. etc.Carnian age. In: Proc. Schweizerbart. Sci. p. indicating U Ladinian. Suppl. Nat. 1-63. Monograph on high-diversity (26 genera.G.('The ammonites from the Lower Triassic of Timor'. 374-389. NW Thailand. Anasiberites multiformis from Noil Saban and Ophiceras crassecostatum Fatu Toekoenenu. 2.Rhaetian radiolaria from Uson island. Northern Thailand.vangorselslist.. 245. Triassic corals and sponges of Seram and Timor have ‘alpine’ character. Neues Jahrbuch Min. Other blocks are limestones with Owenites egrediens from Bihati. Cadiz 2012. Palaeont. Mem. (1922). Mae Hong Son province. Descriptions of 4 additional Early Triassic ammonoid species. All blocks of condensed 'Hallstatt facies' with tuffs and black manganese coating. and new calcareous sponge genera Deningeria. Top of section of E-M Norian age (Capnuchosphaera crassa. (online at: bull3. Sci.Some Triassic corals from Portuguese Timor (Palaeontological study of Portuguese Timor.Species distribution of the world-wide Triassic pelecypod Monotis Bronn. O. p. Cryptocoelia. (2012). 83-87. Bull. indicating gradual change from deep oceanic environment to continental marginal realm.1 281 www.A.A. Flugel (2002. (1990). (Short paper on U Triassic corals collected in 1961 from Fatu Laculequi near Pualaca in C Timor Leste) Yeh. Bull.. Flugel also suggests close similarities with Timor Fatu Limestone) Wonganan. Wilckens. (1992).Y.Bemerkungen uber die von Deninger gesammelten Ammoniten und Nautilidenreste von Seran. Mus. No locality maps) Welter. (1973). Taiwan. Osaka Univ. 51-91. 71 species) Lower Triassic ammonites from various Timor localities. K. p. ('Corals and calcareous sponges from the Upper Triassic Pharetronen-limestone of Seram'. 8. Genus Amarassites first described from Timor now also found in Alps. (1923). Beil. Arts Educ. cherts) Bibliography of Indonesia Geology . 55 species. Isastrea seranica. Palaeontographica. India 1964. Appendix in Krumbeck (1923) Seram brachiopod/mollusc paper. 22nd Int. 19. (2004) found no endemic fauna.) (Ladinian. implication for the tectonic of Southeast Asia. Philippines. Paleo-Tethys almost closed in middle Late Triassic) Yamagiwa.Y. p. N. G. p. Beitrage zur Palaontologie des Ostindischen Archipels 14.Nachtrag zu den obertriadischen Ammoniten von Timor. Proc. Philippines. Nat. representing Paleo-Tethys Ocean deposits. only species of Tethyan affinity. Therefore. K. Lib..Triassic radiolaria from Uson Island. Oldest horizon is yellow Meekoceras limestone from Kapan and Nifoekoko near Niki-Niki (overlying dark red Permian limestone).. Mem.tw/….Taxonomic studies of Triassic radiolaria from Busuanga Island. but Martini et al. Multimonilis. p. 420) suggested W Seram Late Triassic corals and sponges mostly endemic taxa or taxa known from Timor.. etc. O. p. N. 13th Interrad Conf. Capnuchosphaera crassa. including Palaeosaturnalis triassicus. Fragments of Upper Triassic ammonites (Choristoceras. 3. collected by Wanner and Molengraaf 1909-1911 expeditions. ('Supplement to the Upper Triassic ammonites from Timor'. Anatomites. O. Ed..The youngest radiolarians from Mae Hong Son region. Sci. Yeh, K.Y. & Y.N. Cheng (1996)- An Upper Triassic (Rhaetian) radiolarian assemblage from Busuanga Island, Philippines. Bull. Natl. Mus. Nat. Sci., Taiwan, 7, p. 1-43. Yin, Hongfu (1997)- Triassic biostratigraphy and palaeobiogeography of East Asia. In: J.M. Dickins (ed.) Late Palaeozoic and Early Mesozoic Circum-Pacific events and their global correlation, Cambridge University Press, p. 168-185. (Timor Triassic classified as ‘Gondwanan Tethys’ facies, similar to Lhasa- W. Birma?; different from ‘India- Gondwana’ and ‘Cathaysian-Tethys’. Misolia is element of subtropical ‘Gondwanan Tethys’. Gondwanan Tethys and Tropical Tethys merged in Late Triassic due to S-ward expansion of tropical-subtropical biota) Zammit, M. (2010)- A review of Australasian ichthyosaurs. Alcheringa 34, 3, p. 281-292. (Ichthyosaur fossils recorded from M Triassic of Timor (Mixosaurus sp.), from U Triassic of New Caledonia (Shonisauru) and Lower Cretaceous of Australia and New Zealand (Platypterygius)) Zaninetti, L. (1976)- Les foraminiferes du Trias, essai de synthese et correlation entre les domaines mesogeens europeen et asiatique. Rivista Ital. Paleontol. Strat. 82, p. 1-258. (Synthesis of Triassic foraminifera and correlation between European and Asian domains) Zaninetti, L., R. Martini & T. Dumont (1992)- Triassic foraminifers from sites 761 and 764, Wombat Plateau, Northwest Australia. In: U. von Rad, B.U. Haq et al. (eds.) Proc. Ocean Drilling Program (ODP) Sci. Results 122, p. 427-436. (online at: www-odp.tamu.edu/publications/122_SR/VOLUME/CHAPTERS/sr122_24.pdf) (Late Norian (Triasina oberhauseri) and Rhaetian (Triasina hantkeni) forams from ~250m thick Late Triassic reefal-platform carbonate section in ODP cores from Wombat Plateau at edge of Argo Abussal Plain, NW Australia. Reefal carbonate platform with inner shelf (intertidal to lagoon), patch reef, and outer shelf facies. Close affinity to microfauna of Seram. First record of Galeanella? laticarinata outside Seram) Zaw Win (1991)- Triassic ammonites from the Plateau Limestone, East of Lungyaw and Baukkewzu, Myit-tha and Ywa-ngan Township, Myanmar. Georeports 1, 1, p. 75-87. Zwierzycki, J. (1925)- Overzicht der Triasformatie in Nederlandsch Indie. Verhandelingen Geol. Mijnbouwk. Gen. Nederl. Kol., Geol. Serie, 8 (Verbeek volume), p. 633-648. (‘Overview of the Triassic formations in Indonesia’. Lower- Middle Triassic found only on Timor. Everywhere in Indies Upper Triassic is developed in ‘Alpine facies’. Upper Triassic present on Savu/ Roti, Timor, Leti/Babar, Ceram, Ambon, Misool, Buru, Buton, Borneo, Lingga, Sumatra and Malay Peninsula. With one overview map) Bibliography of Indonesia Geology , Ed. 5.1 282 www.vangorselslist.com March 2014 X.7. Permian- Carboniferous Andal, P.P. (1966)- A report on the discovery of fusulinids in The Philippines. The Philippine Geol. 20, 1, p. 14-22. (First report of M Permian fusulinid foraminifera (Schwagerina, Verbeekina) in limestone pebbles in Eocene conglomerate from Carabao Island, SW Mindoro (see also Koike et al, 1968)) Archbold, N.W. (1981)- Permian brachiopods from western Irian Jaya, Indonesia. Geol. Res. Dev. Centre, Bandung, Paleont. Ser. 2, p. 1-25. (Early Permian (Latest Artinskian- early Kungurian) brachiopods in Aifat Fm in Taminabuam area, Birds Head. Assemblage similar to age-equivalent faunas in Thailand) Archbold, N.W. (1981)- Quinquenella magnifica sp. nov. (Chonetidina, Brachiopoda) from the Permian of Irian Jaya, Indonesia: a study of the ontogeny of a chonetid brachiopod. Geol. Res. Dev. Centre, Bandung, Paleont. Ser. 2, p. 2, 27-34. Archbold, N.W. (1981)- New Permian trilobite from Irian Jaya, Indonesia. Geol. Res. Dev. Centre, Bandung, Paleont. Ser. 2, p. 35-41. (New species of Early Permian trilobite) Archbold, N.W. (1983)- A Permian nautiloid from Belitung, Indonesia. Publ. Geol. Res. Dev. Center, Bandung, Paleont. Ser. 4, p. 32-36. (Fragment of straight nautiloid Neorthoceras at Kelapa Kampit, NE Belitung, suggests E-M Permian age for part of NE Belitung Island 'basement' complex. Only other occurrence of Neorthoceras in Indonesia is Bitauni, Timor With summary of other Permian macrofossil occurrences on Belitung.) Archbold, N.W. (1983)- Permian marine invertebrate provinces of the Gondwanan realm. Alcheringa 7, p. 59- 73. (Permian chonetidine brachiopods allow distinction of five Permian Gondwanan faunal provinces: Andean, Paratinan, Austrazean (E Australia- New Zealand), Westralian (W Australia) and Cimmerian (Cimmerian terranes, from Tunisia, Himalayas, Thailand, Sumatra, Leti to W Papua). With description of Waterhouseiella n.gen. for Waagenites speciosus))) Archbold, N.W. (1983)- West Australian Permian brachiopoda: their taxonomy, biostratigraphy and provincialism; with an appendix of published articles including a description of Permian brachiopoda from Irian Jaya, Indonesia. Ph.D. Dissertation, University of Melbourne, 2 vols. Archbold, N.W. (1983)- Studies on Western Australian Permian brachiopods 3. The Family Linoproductidae Stehli 1954. Proc. Royal Soc. Victoria 95, 4: p. 237-254. (Incl. Productus spp., Globiella foordi, Globiella flexuosa, etc.) Archbold, N.W. (1987)- South-western Pacific Permian and Triassic marine faunas: their distribution and implications for terrane identification. In: E.C. Leith & E. Scheibner (eds.) Terrane accretion and orogenic belts, Am. Geophys. Union (AGU), Geodyn. Ser. 19, p. 119-127. (Three provinces of SW Pacific Permian faunas: (1) Cimmerian (Arabia to Irian Jaya, Timor: cold earliest Permian with bivalve Eurydesma, etc., warm-tropical later in E Permian), (2) Westralian (cold earliest Permian followed by temperate faunas, with tropical elements only in Late Permian) and (3) Austrazean (E Australia- New Zealand, New Caledonia) cold and cool temperate conditions throughout Permian). Marine Triassic faunas two provinces: (1) Tethyan- cosmopolitan, (2) cool Maori Province in New Zealand (not including Torlesse)) Archbold, N.W. (1988)- Permian brachiopoda and bivalvia from Sahul Shoals No. 1, Ashmore Block, Northwestern Australia. Proc. Royal Soc. Victoria 100, p. 33-38. Bibliography of Indonesia Geology , Ed. 5.1 283 www.vangorselslist.com March 2014 (Brachiopod- bivalve fauna of Late Permian fine, light-grey, biomicrite limestone in Sahul Shoals 1 well, off NW Australia: Streptorhynchid fragments, Waagenoconcha, Neospirifer, Elival sp., Gjelispinifera sp., Etheripecten and Cyrtorostra. Fauna interpreted to indicate paleogeographic proximity of Late Permian Sahul Shoals limestone and Maubisse Fm of Timor (but Permian brachiopod provinciality rel. poorly defined?; HvG)) Archbold, N.W. (1991)- Late Paleozoic brachiopod faunas from Irian Jaya, Indonesia. In: D.I. McKinnon, D.E. Lee & J.D. Campbell (eds.) Brachiopods through time. Proc. 2nd Int. Brachiopod Congress, Dunedin 1990, Balkema, Rotterdam, p. 347-353. (M Carboniferous- Permian brachiopods from Aifam- Aifat Formations of Birds Head) Archbold, N.W. (1991)- Early Permian brachiopoda from Irian Jaya. BMR J. Australian Geol. Geophysics 12, p. 287-296. (online at: https://d28rz98at9flks.cloudfront.net/81296/Jou1991_v12_n4_p287.pdf) (New E Permian (E Artinskian) brachiopod fauna from Aiduna Fm, from float boulder in upper Mapia River, S flank of Charles Louis Mountains, SW West Papua. New species of Neochonetes, Chonetinella, Aulostege, etc.. Significant links with E Permian faunas of W Australia and Peninsular Thailand) Archbold, N.W. (1999)- Additional records of Permian brachiopods from near Rat Buri, Thailand. Proc. Royal Soc. Victoria 111, p. 71-86. (Permian brachiopods from Ratburi Lst of NE Peninsular Thailand, which overlies Phuket Gp 'pebbly mudstones'. Referred to Ufimian (=Roadian) stage) Archbold, N.W. (2000)- Palaeobiogeography of the Australasian Permian. In: A.J. Wright et al. (eds.) Palaeobiogeography of Australasian faunas and floras, Mem. Assoc. Australasian Palaeont. 23, p. 287-310. Archbold, N.W. (2001)- Permian Productida of Australasia: palaeobiogeographical and palaeoclimatological implications. In: S.L. Long et al. (eds.) Brachiopods, chapter 37, CRC Press, p. 363-371. (Permian Productid brachiopods few genera in common between Westralian (rel. warm, S Tethys margin) and Austrazean (colder water, mainly endemics, strong links with New Zealand) provinces) Archbold, N.W. & S.T. Barkham (1989)- Permian brachiopoda from near Bisnain village, West Timor. Alcheringa 13, p. 125-140. (Permian brachiopoda from outcrops of calcarenites-shales attributed to Maubisse Fm near Bisnain, W Timor. Assemblage correlative to late Sakmarian (E Permian), temperate climate, Callytharra Fm of W Australia) Archbold, N.W. & P.R. Bird (1989)- Permian brachiopoda from near Kasliu Village, West Timor. Alcheringa 13, p. 103-123. (Permian brachiopoda from outcrops of Maubisse Fm volcanoclastics near Kasliu, W Timor. Assemblage probably Chidruan age and correlative of classic Late Permian ‘Tethyan’ Basleo and Amarassi faunas) Archbold, N.W., C.J. Pigram, N. Ratman & S. Hakim (1982)- Indonesian Permian brachiopod fauna and Gondwana-South-East Asia relationships. Nature 296, p. 556-558. (First description of late E Permian articulate brachiopods in Birds Head. Assemblage similar to Thailand Rat Buri Limestone, suggesting geographical proximity of Thailand and Irian Jaya in E Permian) Archbold, N.W. & G.R. Shi (1995)- Permian brachiopod faunas of Western Australia: Gondwanan-Asian relationships and Permian climate. J. Southeast Asian Earth Sci. 11, 3, p. 207-215. (W Australian Permian brachiopod faunas mixture of Gondwanan, endemic Westralian and Asian (Tethyan) genera. Presence of Tethyan genera largely temperature dependent; no apparent geographical barriers to migration of such genera into intracratonic basins of W Australia. Paleotemperature curve indicates peak warm conditions in Sterlitamakian and Late Baigendzhinian and subtropical conditions in Dzhulfian) Bibliography of Indonesia Geology , Ed. 5.1 284 www.vangorselslist.com March 2014 Asama, K. (1966)- Permian plants from Phetchabun, Thailand and problems of floral migration from Gondwanaland. In: T. Kobayashi & R. Toriyama (eds.) Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 2, p. 197-244. (Re-evalution of Permian floras of Phetchabun, described by Kon'no (1964) as Cathaysian with Gondwanan elements Glossopteris and Paleovittaria. Asama interpreted only Cathaysian flora. Similarities to Jambi flora of SW Sumatra (6 genera (but no species?) in common, incl. Sphenophyllum, Alethopteris, Pecopteris, Taeniopteris, Cordaites. With discussion on Permo-Carboniferous floral provinces) Asama, K. (1973)- Lower Carboniferous Kuantan Flora, Pahang, West Malaysia. In: Geology and Paleontology of Southeast Asia, University of Tokyo Press, 11, p. 109-118. (Lower Carboniferous (Visean) flora from Raub series near Kuantan, East coast Malay Peninsula. This warm- humid 'Kuantan flora' is on East Malaya/ Indochina Block and contains Lepidodendron spp., Stigmaria, etc.)) Asama, K. (1976)- Gigantopteris flora in Southeast Asia and its phytopalaeogeographic significance. In: T. Kobayashi & R. Toriyama (eds.) Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 17, p. 191-207. (Sumatra Permian Jambi flora typical Asian, not Gondwanan) Asama, K. (1984)- Gigantopteris flora in China and Southeast Asia. In: T. Kobayashi et al. (eds.) Geology and Palaeontology of Southeast Asia 25, University of Tokyo Press, p. 311-323. (Mainly on classification and evolution of Permian Gigantopteris flora. C Sumatra Permian Jambi flora typical Asian Gigantopteris flora, not Gondwanan Glossopteris flora) Asama, K., A. Hongnusonthi, J. Iwai, E. Kon’no, S.S. Rajah & M. Veeraburas (1975)- Summary of the Carboniferous and Permian plants from Thailand, Malaysia and adjacent areas. In: T. Kobayashi & R. Toriyama (eds.) Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 15, p. 77-101. (online at: http://library.dmr.go.th/library/DMR_Technical_Reports/1975/324.pdf) (Oldest plants in SE Asia are from Lower Carboniferous, known from Malaysia only (Kuantan flora, with Lepidodendron, on E Malaya Block). Five known Permian floras. Permian Jambi flora of Sumatra greatest similarities with Artinskian-Kungarian Shansi Fm of N China. Four other U Permian Cathaysian floras with Gigantopteris: Linggiu and Jengka floras from E Malay Peninsula; Phetchabun and Loei floras of N Thailand. Permian plants from W New Guinea are Gondwana-type flora, but some apparent Cathaysian elements) Asama, K, J. Iwai, M. Veeraburus & A. Hongnusonthi (1968)- Permian plants from Loei, Thailand. In: T. Kobayashi & R. Toriyama (eds.) Geology and palaeontology of Southeast Asia, University of Tokyo Press, 4, p. 82-99. (Typical Gigantopteris flora in continental facies U Permian of Loei area, NNE ofPhetchabun, NE Thailand (= W margin Indochina terrane). 16 species of Sphenophyllum, Pecopteris, Bicoemplectopteris, Gigantonuclea, Taeniopteris, etc. (but no Gigantopteris) (more locality information in Iwai et al. 1966)) Aung, A.K. & M.K. Shuib (2013)- Similarities in Middle-Late Permian fossils from Myanmar and Malaysia and its paleogeographic implications. In: Proc. Nat. Geoscience Conf., Ipoh 2013, Geol. Soc. Malaysia, B14, p. 87-88. (Abstract) (online at: http://geology.um.edu.my/gsmpublic/NGC2013/…) (M-L Permian rugose corals from 'Plateau Limestone' of Myanmar (Sibumasu Block) include Thomasiphyllum (Cimmerian province) and Wentzellophyllum, suggesting mixed Cimmerian (Sibumasu) and Cathaysian provinciality in M Permian and imply that M Permian Paleo-Tethys is only narrow seaway that probably closed by collision in Late Permian) Aung, A.K. & J. Azmi (2014)- Yatsengia jengkaensis- a new yatsengiid rugose coral from the “Jenga Pass Limestone”, Pahang, central Peninsular Malaysia. Warta Geol. (online at: http://www.gsm.org.my/products/702001-100339-PDF.pdf) (Yatsengia jengkaensis n.sp. rugose coral from early M Permian (Wordian) Jengka Pass Limestone outcrop, ~24 km E of Temerloh and 8 km E of Bukit Kepayang, Pahang, C Peninsular Malaysia (= W margin of Bibliography of Indonesia Geology , Ed. 5.1 285 www.vangorselslist.com March 2014 Indochina Plate). Jengka Fm steeply folded, Associated with fusulinds Neoschwagerina katoi, Verbeekina verbeeki, Sumatrina annae, Pseudofusulina, indicating Middle Permian age. Also with coral Michelina indica and algae Mizzia sp)) Aw, P.C., K. Ishii & Y. Okimura (1977)- On Palaeofusulina- Colaniella fauna from the Upper Permian of Kelantan, Malaysia. Trans. Proc. Palaeont. Soc. Japan, N.S, 104, p. 407-417. (online at: https://www.jstage.jst.go.jp/article/prpsj1951/1977/104/1977_104_407/_pdf) (First record of uppermost Permian fusulinids (Palaeofusulina cf. bella, Reichelina, also Colaniella media and C. parva) in Malay Peninsula. In folded, WSW-dipping argillo-tuffaceous limestone interbedded with tuffs of Sungei Paloh, Lebir River area of S Kelantan, S of Kotabaru (= W margin of E Malaya Block?). Overlain by E Triassic with bivalve Claraia) Baird, A., O. Dawson & D. Vachard (1993)- New data on biostratigraphy of the Permian Ratburi limestone from north peninsular Thailand. In: T. Thanasuthipitak (ed.) Proc. Int. Symp. Biostratigraphy of mainland southeast Asia: facies & paleontology, Chiang Mai 1993, Chiang Mai University, p. 243-260. (online at: http://library.dmr.go.th/library/Proceedings-Yearbooks/M_1/1993/6790.pdf) (Ratburi Lst of Peninsular Thailand deposited on broad carbonate platform that covered Shan-Tai (Sibumasu) Terrane. With rel. low diversity fusulinid forams (Nankinella, Staffella, Eopolydiexodina afghanensis and rare Parafusulina, Pseudofusulina, Chusenella), typical hemigordiopsid small forams (Hemigordius reicheli, Hemigordiopsis renzi, Baisalina, Shanita amosi) and Sphairionia sikuoides, suggesting age range of late Murgabian- Midian (late M- early Late Permian)) Bassler, R. (1929)- The Permian bryozoa of Timor. In: Palaontologie von Timor, Schweizerbart, Stuttgart, 16, Abh. 28, p. 37-90. (Principal (and only?) work on Permian bryzoa of Timor. Ross (1978): Artinskian Bitauni Beds sparse bryozoan fauna, early Late Permian Basleo beds more abundant, overlying Amarassi beds sparse bryozoan. Some species, like Fistulipora timorensis Bassler rel. widespread in M-U Permian of Tethys region) Battail, B. (2009)- Late Permian dicynodont fauna from Laos. In: E. Buffetaut, G. Cuny et al. (eds.) Late Palaeozoic and Mesozoic ecosystems in SE Asia. Geol. Soc. London, Spec. Publ. 315, p. 33-40. (New collection of Late Permian Dicynodon spp.tetrapods from purple beds of Luang Prabang area) Batten, R.L. (1972)- Permian gastropods and chitons from Perak, Malaysia. Part 1. Chitons, bellerophontids, euomphalids and pleurotomarians. Bull. Amer. Mus. Nat. Hist., 147, 2, p. 1-44. (online at: http://digitallibrary.amnh.org/dspace/handle/2246/1103) (One of richest Permian gastropod faunas of Asia 92 species) in H.S. Lee No. 8 opencast tin mine near Kampar, Perak. Associated with fusulinids, all with Tethyan affinities (but on Sibumasu Terrane; HvG)) Batten, R.L. (1979)- Permian gastropods from Perak, Malaysia. Part 2. The trochids, patellids, and neritids. Amer. Mus. (Nat. Hist.) Novitates, 2685, p. 1-26. (online at: http://digitallibrary.amnh.org/dspace/handle/2246/5386) (Continuation of Batten (1972). Rich Permian gastropod fauna from white limestone in H.S. Lee Mine 8 near Kampar, Perak, associated with corals, scaphopods, bivalves, brachiopods, cephalopods and fusulinids. Fusulinids suggest Late Artinskian- E Guadalupian age, Misellina claudiae zone (Jones et al. 1966). Neritacean species similar to those found in Sicily, Timor and Sumatra and identified as typical Tethyan) Batten, R.L. (1985)- Permian gastropods from Perak, Malaysia. Part 3. The murchisoniids, cerithiids, loxonematids, and subulitids. Amer. Mus. (Nat. Hist.) Novitates 2829, p. 1-26. (online at: http://digitallibrary.amnh.org/dspace/handle/2246/3583) ((Final part of 3-part study of rich Permian gastropod fauna from H.S. Lee Mine 8 near Kampar, Perak) Belasky, P. (1994)- Biogeography of Permian corals and the determination of longitude in tectonic reconstructions of the Paleopacific region. Canadian Soc. Petrol. Geol. Spec. Publ., p. 621-646. Bibliography of Indonesia Geology , Ed. 5.1 286 www.vangorselslist.com March 2014 (Mainly focused on American terranes. South China was center of diversity of Permian Tethyan coral province and was located near Permian equator and W margin of Paleopacific Ocean) Beyrich, E. (1865)- Uber eine Kohlenkalk-Fauna von Timor. Abhandl. Konigl. Akad. Wissensch. Berlin, 1864, p. 59-98. ('On a Carboniferous fauna from Timor'. First description of ‘Carboniferous’ (now accepted as Late Permian) limestone fauna from Timor, collected in Kupang area by Dr. Schneider. Includes mollusc genus Atomodesma, solitary rugose coral Zaphrentis, new brachiopod species Spirifer kupangensis (= Arcullina; Waterhouse 2004), Rhynchonella timorensis (assigned to Uncinunellina timorensis by later authors; HvG), etc.) Bless, M.J.M. (1987)- Lower Permian ostracodes from Timor (Indonesia). Proc. Kon. Nederl. Akademie Wetenschappen B, 90, 1, p. 1-13. (Lower Permian (Sakmarian- Artinskian) ostracodes from Bitauni, Mutis, Nono Ofien and Noil Toensieh in W Timor. Diverse 'Thuringian-type' assemblages with 40 species, usually interpreted as deep marine, as also suggested by Grundel & Kozur 1975) Boehm, G. & F.A. Bather (1908)- Jungeres Palaozoikum von Timor. In: G. Boehm (ed.) Geol. Mitteil. Indo- Australischen Archipel VIb, Neues Jahrbuch Min., Geol., Palaeont., Beilage Band 25, p. 303-323. ('Young Paleozoic of Timor'. First description of two Permian blastoids from Timor, collected by Verbeek in 1899 from Bisano Hill S of Baung (Schizoblastus (now called Deltablastus), Schizoblastus timorensis and S. delta). Associated with Spirifer lineatus, Nautilus, ammonoid Agathiceras timorense n.sp., trilobite Phillipsia) Booi, M., I.M. van Waveren, J.H.A. van Konijnenburg-van Cittert & P.L. de Boer (2008)- New material of Macralethopteris from the Early Permian Jambi flora (Middle Sumatra, Indonesia) and its palaeoecological implications. Rev. Palaeobotany Palynology 152, 3-4, p. 101-112. (New material of E Permian Jambi flora. Comparison with related Cathaysian and Euramerican species show the isolated occurrence of alethopterid genus Macralethopteris in Cathaysian region) Booi, M., I.M. van Waveren & J.H.A. van Konijnenburg-van Cittert (2009)- Comia and Rhachiphyllum from the Early Permian of Sumatra, Indonesia. Rev. Palaeobot. Palynology 156, p. 418-435. (Early Permian flora from Mengkarang Fm of Jambi with Comia, Rhachiphyllum, Supaia-like material and an Autunia fructification, corroborating peltasperm affinity. Material shows strong relationships with N China and even Angaran region, but no Gondwanan elements, suggesting migration zone running from N China Block to W Sumatra- W Myanmar terrane) Booi, M., I.M. van Waveren & J.H.A. van Konijnenburg-van Cittert (2009)- The Jambi gigantopterids and their place in gigantopterid classification. Botanical J. Linnean Soc. 161, 3, p. 302-328. (Two gigantopterid species/genera from E Permian Mengkarang Fm of Jambi, originally described by Jongmans & Gothan 1935 as Gigantopteris bosschana (reclassified to new genus Gothanopteris by Koidzumi 1936) and G. mengkarangensis (reclassified to Palaeogoniopteris by Koidzumi 1936). Similar to other gigantopterids, but not related directly. Possible scenario for evolution of gigantopterid leaf morphology) BouDagher-Fadel, M.K. (2008)- The Palaeozoic larger benthic foraminifera: the Carboniferous and Permian. In: Evolution and geological significance of larger benthic foraminifera, Chapter 2, Developments in Palaeontology and Stratigraphy, Elsevier, 21, p. 39-118. (General review of Paleozoic larger foraminifera, mainly Carboniferous-Permian fusulinids. End of Permian is major extinction event) Boureau, E. & W.J. Jongmans (1955)- Novoguineoxylon lacunosum n.gen., n.sp., bois fossile de la Nouvelle- Guinee hollandaise. Rev. Gen. Botanique 62, p. 720-734. (' Novoguineoxylon lacunosum n.gen., n.sp., fossil wood from Netherlands New Guinea'. New wood species of supposedly Jurasssic age from Birds Head (but very similar to Australoxylon mondii described from U Permian of East Antarctica, and Permian age more likely according to Bamford & Philippe 2001) Bibliography of Indonesia Geology , Ed. 5.1 287 www.vangorselslist.com March 2014 Breimer, A. & D.B. Macurda (1965)- On the systematic position of some blastoid genera from the Permian of Timor. Proc. Kon. Nederl. Akademie Wetenschappen, Amsterdam, B68, p. 209-217. Breimer, A. & D.B. Macurda (1972)- The phylogeny of the fissiculate blastoids. Verhandelingen Kon. Ned. Akademie Wetenschappen, Amsterdam, ser. 1, 26, 3, p. 1-390. (online at: http://www.dwc.knaw.nl/DL/publications/PU00011028.pdf) (Monograph on Paleozoic fissiculate blastoids (echinoderms). Mainly taxonomy, anatomy and phylogeny, also discussions of geographic distribution (worldwide), stratigraphic distribution (Silurian- Permian) and paleoecology (open marine, attached to limy-muddy seafloors). Most extensive development of Permian fissiculates is on Timor, associated with tuffs (12 genera; all in allochtonous blocks). Main collecting area is Basleo; many endemic species, some also in other areas, e.g. Pterotoblastus gracilis in Thailand) Briggs, D.J.C. (1998)- Permian Productidina and Strophalosiidina from the Sydney-Bowen Basin and New England Orogen: systematics and biostratigraphic significance. Mem. Assoc. Australasian Palaeont. 19, p. 1-258. Broili, F. (1915)- Permische Brachiopoden der Insel Letti. Jaarboek Mijnwezen Nederl. Oost-Indie 43 (1914) Verhandelingen 1, p. 187-207. (‘Permian brachiopods from Leti Island’ (E of Timor). Small brachiopod fauna collected by Molengraaff. With Productus spp., Chonetes strophomenoides, Spirifer spp., Martinia nucula, Retzia, Dielasma and Notothyris) Broili, F. (1916)- Die Permischen Brachiopoden von Timor. In: J. Wanner (ed.) Palaontologie von Timor, Schweizerbart, Stuttgart, VII, 12, p. 1-104. (‘The Permian brachiopods of Timor’. Descriptions of 46 species in material from numerous localities in W and some from E Timor, collected by Wanner and Molengraaff. Many are long-ranging and widely distributed Tethys forms, incl. Productus, Spirifer, Spirigera, Retzia, Camarophoria, Dielasma, etc. Rare Lyttonia (Leptodus) cf. tenuis from Basleo and Niki-Niki areas.) Broili, F. (1922)- Permische Brachiopoden von Rotti. Jaarboek Mijnwezen Nederl. Oost-Indie 49 (1920), Verhandelingen 3, p. 223-227. (Nederlandsche Timor expeditie 1910-1912). (Brief description of Permian brachiopods from Roti island, W of Timor, sampled by Brouwer in 1912. Species rel. long-ranging, incl. Derbya beyrichii, Productus waageni, Productus cf. semireticulatus, Spirifer fasciger, Spirigera timorensis, Retzia radialis, Camarophoria pardoni, Notothyris, etc.) Broili, F. (1931)- Mixosauridae von Timor. Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Indie 17, p. 3-10. (Vertebrae collected from clays with manganese nodules and ammonites by Jonker in 1873 in NE part of W Timor near E Timor border ('Wai Loelik/ Ramea, Beloe district'). Looks like primitive Ichtyosaurus group and described as Mixosaurus timorensis n.sp.. Age probably Triassic (Manganese nodules known in Timor-Roti from Upper Triassic, Jurassic and Upper Cretaceous; HvG; see also Zammit, 2010)) Bronnimann, P., J.E. Whittaker & L. Zaninetti (1978)- Shanita, a new pillared Miliocean foraminifera from the Late Permian of Burma and Thailand. Riv. Ital. Paleont. 84, p. 63-92. (New late M- Late Permian pillared miliolid Shanita amosi from W margin of Shan Plateau, E Myanmar. Species mainly characteristic of M Permian of Sibumasu terranes?) Brouwer, H.A. (1919)- Fossielhoudende Palaeozoische afzettingen op Celebes. De Ingenieur, 8 Nov. 1919, p. 832-833. ('Fossiliferous Paleozoic beds on Sulawesi'. Permian ammonite Popanoceras timorense in collection of Colonel G.J. Verstege, reportedly from 'the Sadang and Mato Allo river basins and the mountains in-between, partly found by myself, partly presented by chiefs of Enrekang, Doeri and Maiwa in 1907 and 1910' (Kalosi region). This suggests presence of Paleozoic marine sediments in S-C Sulawesi, but localities never independently verified, and questioned by Abendanon (1920) and Von Koenigswald (1933), who believed they probably came from Timor, via a Chinese pharmacy (But cannot be dismissed completely?: Permian brachiopods also reported from E Sulawesi by Von Loczy (1934) and Von Kutassy (1934); HvG) Bibliography of Indonesia Geology , Ed. 5.1 288 www.vangorselslist.com March 2014 Bunopas, S., H. Fontaine,S. Salyapongse & D. Vachard (1983)- Permian paleogeography in Southeast Thailand evidenced by new discoveries. J. Geol. Soc. Thailand 6, p. 17-21. (online at: http://library.dmr.go.th/library/J-Index/1983/85.pdf) (Complete sequence of Permian fossils now known from region. New Permian limestone localities described from E Thailand near Cambodia border (incl. M Permian Ipciphyllum timoricum). In E Thailand limestones dominant, in W dominantly shale with rare limestones) Burke, J.J. (1966)- On the occurrence of Oklahomacrinus in Ohio and Timor. Ohio J. Science 66, 5, p. 464-468. (Delocrinus expansus Wanner from M Permian of Basleo, W Timor, re-assigned to Oklahomacrinus) Campi, M.J., G.R. Shi & M.S. Leman (2002)- The Leptodus shales of central Peninsular Malaysia: distribution, age and palaeobiogeographical affinities. J. Asian Earth Sci. 20, 6, p. 703-717. (‘Leptodus Shales’ is M Permian argillaceous facies rich in brachiopods in C Belt of Peninsular Malaysia. Sediments often highly tuffaceous and in N Pahang associated with pyroclastic volcanics of probable island-arc origin. Probably represent deposits on W continental shelf of Eastern Belt/ Indochina Block. Faunas of Paleo- Equatorial affinity and closest to faunas in Indochina (S China, Cambodia, Japan)) Caridroit, M. (1993)- Permian radiolaria from NW Thailand. In: T. Thanasuthipitak (ed.) Proc. Int. Symp. Biostratigraphy of Mainland Southeast Asia, facies and paleontology 1, Chiang Mai University, p. 83-96. (online at: http://library.dmr.go.th/library/Proceedings-Yearbooks/M_1/1993/7485.pdf) (Permian and Triassic radiolaria from Chiang Dao region, NW Thailand, an area SW of Nan from which U Silurian- Triassic deep water radiolarian-bearing rocks are known, and where nappe sheets are indicated. With descriptions of Permian radiolaria (Folliculus, Albailella, etc.) Caridroit, M., D. Bohlke. & A. Lamchuan (1993)- A mixed radiolarian fauna (Permian/Triassic) from clastics of the Mae Sariang area, northwestern Thailand. In T. Thanasuthipitak (ed.) Proc. Int. Symposium on Biostratigraphy of Mainland Southeast Asia: facies and paleontology (BIOSEA), Chiang Mai, 2, p. 401-413. (online at: http://www.mnhn.fr/mnhn/geo/PDW/Caridroit%20et%20al%201993.pdf) (Folded sequence of red conglomerates/ sandstones/shales W of Amphoe Mae Sariang not of M Triassic age but Late Triassic or younger. Pebbles include metamorphic quartz and reworked chert clasts with two distinct radiolarian assemblages, M-L Permian and M Triassic) Caridroit, M., H. Fontaine,V. Suteethorn & D. Vachard (1990)- New paleontological data on the Carboniferous and Permian of NW Thailand. In: Ten years of CCOP research on the Pre-Tertiary of East Asia, CCOP, Spec. Vol., p. 337-351. (Microfaunas from 40 new localities of Visean- Late Permian limestones in NW Thailand) Caridroit, M., D. Vachard & H. Fontaine (1992)- Datations par radiolaires (Carbonifere, Permien et Trias) en Thailande nord-occidentale. Mise en evidence de nappes de charriage et d'olistostromes. Compte Rendu Acad. Sci. Paris, ser. II, 315, 4, p. 515-520. ('Radiolarian age datings (Carboniferous, Permian and, Triassic) in NW Thailand, evidence of nappes and olisthostromes'. Paleozoic stratigraphic column in NW Thailand described as single Ordovician- Permian marine succession, tectonized in Triassic time, but ages from radiolarite dating (Carboniferous- Triassic) demonstrate existence of separate sedimentary basin far from detritic sources and of Carboniferous- Triassic limestones. Present structural imbrication of radiolarites with limestones and detritic series interpreted in terms of tectonic nappes with considerable shortening, and olistostrome deposits) Chapman, F. & W.J. Parr (1937)- On the discovery of fusulinid foraminifera in the Upper Palaeozoic of Northwest Australia. Victorian Naturalist 53, p. 175-179. (Described presence of fusulinid genera Verbeekina and Neoschwagerina in NW Australia (but were shown to be fish remains by Crespin (1958), Quilty (1975). No fusulinid forams recorded yet from Australia, but present on Timor and probably also in Birds Head of New Guinea; HvG) Bibliography of Indonesia Geology , Ed. 5.1 289 www.vangorselslist.com March 2014 Shallow marine.Middle Permian ostracods from Tak Fa Limestone. T. C. mainly anti-tropical taxa (but herer grouped with warm water taxa rather than with cold water taxa from Gondwanan-Perigondwanan region). Archbold.J. 5. J. (Extensive compilation of Timor Permian stratigraphy and paleontology. Bur. Bull. I. 1954)) Crippa. Pseudoschwagerina cf.pdf) (106 species/46 genera of Permian foraminifera. Eight new species) Chitnarin. Nat.ga. R. Ed. (online at: https://www. (online at: http://www. Whittaker (2002). Bull. Crasquin.R.Ostracods (Crustacea) of the Early-Middle Permian from Central Thailand (Indochina block). A. 719-774. Mineral Res. S. Tasmania. W Australia. mainly arenaceous.J. Brachiopods 6 genera (mainly Stereochia aff. Geobios 41. families Aparchitidae. 1-207. part of the W Sumatra Block Volcanic Arc deposits. and Coelonellidae. Owens. cephalopods. Samples from 12 limestone localities in Loei.T. afghanensis. Mineral Res. Eoparafusulina ?haydeni).The Permian of Timor: stratigraphy. Florinites florini and Convolutispora sp. Amphissitidae.G. (Brachiopods. poor assemblage of widespread genera but-tropical Tethyan affinity due to common occurrence large schwagerinids.J. p. also Eostaffella. Harris. which shows paleobiogeographic links between C Thailand and S China) Crespin. . Sumatra) and their palaeobiogeographical significance. p. S. palaeontology and palaeogeography. Youngiellidae. Geol.. 3. N.vangorselslist.au/webtemp/1225667/Bull_048. different from coeval assemblages of Gondwanan region. p.au/products/servlet/controller?event=FILE_SELECTION&catno=206) (On smaller benthic forams from Queensland.. Grote & N. 129-175. Morris. J. from M Permian Tak Fa Lst in Phetchabun province. etc. P. (1958). C Thailand. conodonts. Taiwan. T (2002). N.). foraminifera. Bird.. Jambi. irianensis. Phetchabun and Nakhon Sawan-Lopburi contain 39 species of Palaeocopida. Crow. Canberra. T. S. Central Thailand.. Bull. except one. Crasquin. M. New South Wales. 15. J. G. 4. mainly Pseudofusulina rutschi. 20. S.Upper Paleozoic and Lower Mesozoic radiolarian assemblages from the Busuanga Islands. P. R. HvG)) Crespin. Thanee (2012). meranginensis.E. Y. P. Ueno (2014)- Brachiopods. L. I.. and fusulinids are probably fish remains (Brunnschweiler. Knoxitidae.R.Charlton. also Marginifera.H.W. corals.com March 2014 . Publ. p. Kirkbyidae. The only record of two genera of Fusulinid forams is Neoschwagerina and Verbeekina from W Kimberley area in W Australia by Chapman and Parr (1937) (but identifications now believed to be erroneous. R.) Charoentitirat. Geoph... Asian Earth Sci. Science. 48. bryozoans. (1989).Permian fusulinodean biostratigraphy and carbonate development in the Indochina Block of Thailand with their paleogeographic implication. Hasibuan. Fusulinids at one level at Teluk Gedang (rel. F. Webster & J. fusulines and palynomorphs of the Mengkarang Formation (Early Permian.D. A. Van Waveren. p. Owen. North Palawan Block.. Nicoll. fusulines and palynomorphs from Lower Permian Mengkarang Fm. C Thailand. poor assemblage of 6 species. molluscs. Paraparchitidae. Stephenson & K. rel.Foraminifera in the Permian rocks of Australia.gov. p.gov.M. etc. Beds in W Australia from which Chapman and Parr (1937) described fusulinids are not Permian but Triassic. Hollinellidae. Barkham. 15 species mainly endemic. Bur. Palynomorphs dominated by Laevigatosporites spp. with specialist reviews of brachiopods. P.Permian foraminifera of Australia. 341-353. Charoentitirat. Asian Earth Sci. and Neochonetes carboniferus. Doctoral Thesis. Museum Nat. Podocopida will be described in second paper. P. echinoderms. but affinity with Cathaysian phytogeographic province as represented in N China. University of Tsukuba. Taylor.) Bibliography of Indonesia Geology . Barber. Order Palaeocopida.ga. (First Permian ostracod fauna described from Thailand. Most likely age Sakmarian. Spec. Chitnarin.A. p. Broutin. Phetchabun Province.E. (1947). Sorauf. etc. Kloedenellidae. etc. Reticulatia.S. 801-835. Geodiversitas 34. M. p. A.D. Thanee (2008). G. Philippines. Schubertella. Angiolini. 206-223. 79. but E Artinskian age cannot be excluded. J. (Unpublished) Cheng. Tepnarong & N. all small benthics. 1. Chonglakmani.1 290 www. nearshore assemblages. trilobites.J. (E-M Permian shallow marine ostracods from W margin of Indochina block. Part I. H. I. Bangkok 1991. Southeast Asian Earth Sci. 49-65. McCartain (2013). and can be correlated with S Pamirs. Iran. I.Crow. Johore and W Sumatra Associated dasycladacean floras assignable to E Circum-Pacific Realm. Mineral and Energy Resources of SE Asia (GEOSEA VII). Subdivided with abundant fusuline and calcareous algal biota.K.calcareous algal paleoecology of the Permian Ratburi Limestone. p. D. Geological Journal 44. Symp. central Thailand. Afghanistan.go. HvG)) Bibliography of Indonesia Geology . Also suggest subtropical environment at paleolatitude of ~40° S. HvG)) Davydov. Paraschwagerina. Central Thailand. Ed. 9-33. (1962). 5. 8. Geol. Ratburi Lst transgressive-regressive carbonate platform sequence. O.Tobler's oyster and the age of the Tabir Formation.1 291 www.. 36-48. (Tabir Fm of Jambi long considered to be Upper Jurassic. & A. Palaeoclim. J. British Territories Borneo. Fusulinid foraminifera including Schwagerina spp. Van Waveren & S.A latest Carboniferous warming spike recorded by a fusulinid-rich bioherm in Timor Leste: implications for East Gondwana deglaciation. at S end of Phetchabun foldbelt in C Thailand. Kulau bioherm is oldest unit recognized in Maubisse Fm of Timor. with 6 main assemblages. West Sarawak. Biostratigraphy of mainland Southeast Asia: facies and paleontology (BIOSEA). Survey Dept. (For Davydov et al. Palaeoecology 376. and Eostaffella suggest latest Carboniferous (-earliest Permian) age.The palaeoecological and palaeobiogeographical significance of Shanita (foraminifera) and associated foraminifera/ algae from the Permian of peninsular Thailand. West Sarawak. Cummings. p. (Permian carbonates N of Saraburi. p. See also Fontaine 1990. Racey & J.I.E Midian supratidal to outer platform biofacies.Limestones of the Terbat Formation. E Burma. R. uber. (E-M Permian Ratburi Lst of C Thailand (= W margin of Indochina terrane) folded sequence of Sakmarian. S China. (Lensoidal limestone body of Maubisse Fm near Kulau village in central highlands of Timor Leste is bioherm with massive lower unit. Schwagerina). 117-121. 2013 these forms signify a broad latest Carboniferous to Early Permian age. (1993). A.K.early Late Permian (Midian) age.A preliminary account of foraminifera from the Carbo-Permian.. Racey (1993). Geol. HvG)) Dawson. similar to M Permian reefs of Austria and W Texas. p. Chiang Mai University. Central Sumatra.W.vangorselslist. and bedded grainstone upper unit. Report for 1955. Survey Dept. Palaeogeogr. Tan et al. British Territories Borneo. In: B. Saraburi.J. based on small molluscs collected by Tobler and assigned to Ostrea. J. Saraburi. O.M.th/library/Proceedings-Yearbooks/M_1/1993/6791.. Turkey. In: T.E.) 7th Reg. Appears to be restricted to W Tethys and Shan-Tai Block. With fusulinid facies distribution model) Dawson. including reef framework at base.H. (online at: http://library. Haig & E.H.. Jambi Province. Whittaker (1993). at N margin of Gondwana (where E Permian is glacial-dominated) (Authors do not consider alternative interpretation that Maubisse Fm may be 'allochthonous' and not part of Australian margin. R. 22-38. 1. 283-295. O. Fusulinid distribution depth-controlled. 1. Tethyan Verbeekinoidea dominate late M Permian fusuline assemblages together with some cosmopolitan species of Parufusulina and Schwagerina. Chiang Mai 1993. Fusulinid faunas of Arctic-Tethyan affinities in E Permian and Tethyan affinities in M Permian. p. P.Fusiline foraminiferal biostratigraphy and carbonate facies of the Permian Ratburi Limestone. Geology. These are not oysters and other fauna/flora show Tabir Fm is Late Permian) Cummings. (Terbat Fm with fusulid foraminifera of Early Permian (Asselian) Pseudoschwagerina zone (Pseudoschwagerina heritschi. (eds. Micropalaeontology 12. (Good marker for(early) Late Permian) of Sibumasu/ Cimmerian terranes. p.dmr.Fusuline.. p. Associated with poor fusulinid assemblages (unlike high-diversity fusulinids in E Thailand. Eight fusuline assemblage zones) Dawson. Ann. M. N-S trending carbonate platform with diverse fusulinid-algal assemblage of E Permian (Sakmarian). Archaeolithoporella and Tubiphytes form reef frameworks. Donovan (2008). Congr. (1955).pdf) (late Middle Permian (Midian) pillared miliolid foram Shanita amosi known from Ratburi Lst of peninsular Thailand and from platform carbonates in Tunisia. Ann. Thanasuthipitak (ed.com March 2014 .) Int. Report 1961. 79. Bioherm developed on basalt substrate in warm shallow water. V. Royal. Dept. F. Soc. Proc. Natuur.Geneesk..pdf) (Permian fusulinid foraminifera from limestone blocks associated with spilitic pillow lavas from Whangaroa Harbour.pdf) (Six species of Permian ammonite Paralegoceras proposed by Smith (1927) from Jonker collection from Timor are all variations of P.W. O. Nederl.W.Mizzia in Palaeozoische gesteenten uit de omgeving van Palembang.Neue Permische Krinoiden von Timor.Preliminary note on the occurrence of a new ammonoid fauna of Permian age on the island of Timor. 240-242.Permian foraminifera from northeast and peninsular Thailand. Geol. Padang Highlands (Pia 1935. Magazine 77. (1933). etc. 323-332. Nederl. New Zealand 79. 9.A. Akademie Wetenschappen. F. Neoschwagerina. where fusulinid assemblage of low diversity.E. (M Permian dasyclad calcareous algae Mizzia velebitana Pia in grey-black limestone at Bukit Pendopo. 1. Thought to be stratigraphically transitional between known Basleo and Bitauni faunas) De Marez Oyens.) Proc. Kon. from Basleo. F.nl/DL/publications/PU00017273. F. diverse foraminifera and algal assemblages mainly of M Permian (late Murgabian-Midian) age. associated with marls and common diabase with tuffs. Proc. Neoschwagerina margaritae. Verbeekina verbeeki.Over het voorkomen van Fusulina-kalken in het Basleo gebied. (‘New Permian crinoids from Timor. tuberculatus.vangorselslist. p. In: P. 88-98.A. etc. 2.pdf) (Listing of Permian ammonites from new locality Tae Wei.dwc. Amsterdam. (online at: http://www. (online at: http://www.W.natlib. p. a correction. G. NE Thailand (Indochina terrane) age-equivalent fusulinids are abundant and diverse Tethyan assemblages with Colania douvilei.. F.H. locally ranging down into Sakmarian. p.A. collected by Keil in 1931. Handelingen 28th Nederl. (1938). Fontaine 1983).Dawson. N. New Zealand. A. with remarks on their occurrence in the Basleo area’. 1. 41. Associated with fusulinids Fusulina and Neoschwagerina) Bibliography of Indonesia Geology . Amsterdam.th/library/Proceedings-Yearbooks/M_1/1994/6958.W. In Noil Toeke in series of Permian rocks enclosed in Mesozoic rocks. Loose blocks of fusulinid limestones in Noil Boenoe river deposits. (1949). 319-321. 1122-1126. p.nz/volume/rsnz_79/rsnz_79_02_004230.. Utrecht. Angsuwathana et al. Lepidolina.Permian fusulinid foraminifera from the North Auckland Peninsula. ('On the occurrence of Fusulina limestones in the Basleo area’. 36. (1940).nl/DL/publications/PU00016378. Yabeina multiseptata probably of M Permian (Wordian. North Island. (eds. Amsterdam. Symp.. p 253- 254. Racey & J. (1951).A.govt.Capitanian) age) De Marez Oyens. Mineral Resources. With mod. Hornibrook. Stratigraphic correlation of Southeast Asia. sundaicum Haniel) De Marez Oyens. 3.H.On Paralegoceras sundaicum Haniel and related forms.A. Marls locally rich in crinoids.go. mit Bemerkungen über deren Vorkommen im Basleogebiet.pdf) (Permian carbonates of Peninsular Thailand originally deposited on Shan-Tai (Sibumasu) terrane. Bangkok 1994. p. Brouwer (ed. p. Chronica Naturae. 285-348.dwc. NW of Basleo Permian limestones generally thin lenses. 224-225. In some areas this Permian adjacent to deep marine Cretaceous with manganese nodules and fish teeth) De Marez Oyens. (online at: http://library. probably remnants of thrust sheet) De Neve. S Sumatra. 5. (1940). Congr.A. Timor) De Marez Oyens. 10. 106.A. Int.dmr. Whittaker (1994).H. Kon. In: H. coarse conglomerates with brachiopods.com March 2014 . Also known from Guguk Bulat.knaw.knaw.W.H. p.Platycrinus tuberculatus Oyens. (1941). Noord Hollandsche Publ. Ed. 1937. Verbeekina.) Geological Expedition of the University of Amsterdam to the Lesser Sunda Islands. 5 km NE of Basleo. Localities with Shanita amosi and common Hemigordius and Hemigordiopsis restricted to peninsular Thailand. Akademie Wetenschappen.1 292 www. (Suggests Permian crinoid Platycrinus wrighti to replace P. Trans. are first record of fusulines New Zealand. (online at: http://rsnz.)) De D. Batavia.H. IGCP 306. p. 2.Problems of a Late Palaeozoic glaciation in Australia and subsequent climate in the Permian. 339-342. etc. (1940). p.Correlation of fusulinid rocks from southern Sumatra.. Also white silicified limestone interbedded in phyllite-sandstone series with Permian fusulinid foraminifera in old tin mine 17 at at Airduren. Faunas associated with glacial deposits low diversitywith Deltopecten. Geologie en Mijnbouw 13. jasperoids and combustible clay shales from W Borneo found by Krekeler (1932. all separated probably by colder periods. 185-197.Upper Palaeozoic pelecypods and gastropods from Irian Jaya. J. p. J.vangorselslist. J. in Sekaju area pebbles with fusulinids in Old Neogene conglomerate by Van Tuyn (1931) and (4) silicified limestones and fine crystalline quartzites with fusulinids of Sungailiat area near Aerduren. in H. Bibliography of Indonesia Geology . Dev.M. Bull. 23. Bangka island collected by de Roever) De Roever. Eurydesma. in Palembang area. Palaeoclim. (online at: https://s3-ap-southeast-2. Carnarvon. 1933). End of glaciation asssociated with worldwide eustatic rise in sea-level in Early Sakmarian.. Palaeontological Appendix to Simons (1940). p.Some additional data on the stratigraphy of Bangka. 29. Marine Levipustula fauna may represent less cold sea water than Eurydesma fauna) Dickins. (1963). Ed.P. from Perth. with similar rocks from Malaya. Bureau Mineral Res. E Kalimantan (Tan Sin Hok 1930). p.P. (3) Two localities of limestone with Neoschwagerina and Fusulina spp. Palaeoclim. (1996). p. marbles. & S. Indonesia. Ends with eustatic rise in sea level. Kungurian. p. 63. Centre. with entry of Tethyan forms (Spriferella. (1957). W.M. Palaeogeogr. Bull. NE Bangka) Dickins. Proc. Western Australia. Palaeogeogr.E Artinskian) cool.cloudfront. (Two main periods of glaciation: (1) Namurian (E Carboniferous) possibly extending into beginning of Late Carboniferous. Lidak. and Borneo. J.D (Artinskian-Kungurian) slow warming in W Australia. 1-203. Western Australia.Description of some Permian ammonoids from F. (1956). indicating tropical temperatures) Dickins. 206-210. 9th Pacific Science Congress. Geol.De Neve. 10. Ser. Leptodus in N. (online at: https://d28rz98at9flks. discovered by Keil and (3b) 18 km W of Palembang. S Sumatra.net/173/Bull_063.) (1940) Geological Expedition of the University of Amsterdam to the Lesser Sunda Islands 1937. (3a) E of Bukit Pendopo. Geophysics. Dickins.M. G. Geophysics. (2) Asselian (earliest Permian).amazonaws. p.Lower Permian pelecypods and gastropods from the Carnarvon Basin. J. Geol. Keeneia and Trigonotreta. 33-46. Bureau Mineral Res. J. C. 43-52. Skwarko (1981). Geol.M. 1-42. (1978). Bangka.K.. B (Sakmarian. (New species of cyclolobid ammonite Waagenoceras lidacense from Lower Permian of NE West Timor) De Roever.1 293 www.pdf) (150 species of pelecypods and 60 gastropods from Lower and Upper Permian of W Australia.Permian pelecypods and gastropods from Western Australia.M. 1. W.com March 2014 . 41. Bangkok 1957. 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(Abstract only) (Four occurrences of U. Thailand and Burma. in Lower Tertiary conglomerate in Kutai. Canning and Fitzroy Basins) Dickins. Koekatoe. Kazanian and Dzhulfian. 113-122.) Permian stratigraphy. E of Timor) Edwards. Malayan Branch Royal Asiatic Soc. Macroporella. 308- 324. (First record of Permo-Carboniferous plant fossils from 'Raub series' shale with thin ash beds at Sungei Chiku. In: T. M. Solenopora. p. (Algae from conglomeratic beds near Mansalay Fm (probably Jurassic) at Agbahag Point.) Ehiro. (2) Equatorial American. Fusulinids described earlier by Toriyama and Kanmera 1968. Proc. 171-172. Mindoro Oriental. Mizzia velebitana. M. Early Permian (Sakmarian). In: Jin et al. Macroporella. New South Wales. verbeeki Gothan & Jongmans from Sumatra) and Cordaites sp.com March 2014 . 56.S. with E Permian perrinitids. 575-587. (Incl. HvG).) Geology and Paleontology of Southeast Asia. p. Kelantan.Les calcaires a fusulines de l’Indo-Chine. Soc. 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Australia.Foraminifera and their habitats within a cool-water carbonate succession following glaciation. (1968).Permian ammonoid fauna of the Kitakami Massif. Geol. 30th Int. Himalayas. VSP. 211-219. 18-28. 5.Fossil algae from Mindoro Oriental Province. & E. SE Asia. Haig (2004). environments and resources 2. C. W. Beijing 1996. 2. Douville. Congress. Archaeolithporella hidensis. 491-497. W. Most species known from Permian of Japan. Epimastopora malaysiana n.N. Bull. M Permian Timorites. 4. 4. was in equatorial realm near S China/ Khanka Terranes. Palaeontology and historical geology.F. Vermiporella nipponica (=Vermiporella sumatrana Pia 1937?. 33-85.Carboniferous plants from the Malay States. Foraminiferal Research 34. R. (1926). Mainly systematic descriptions of 64 species of 33 genera.Three new Tethyan Dasycladaceae (calcareous algae). Australia. (3) Equatorial Tethyan (incl. Res. Spirifer. Notes 21. Bandung. p.1 295 www. Similar to those from mainland SE Asia. Canning. 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(33 species of latest Permian radiolaria from bedded cherts in S China) Feng. Oklahoma Geol.Carboniferous. which was not single block. (1961). 4. geochemical and biochemical data') Fay. Permocalculus) Bibliography of Indonesia Geology . Wonganan. p. Pavastehphyllum. I.).Latest Permian Spumellaria and Entactinaria (Radiolaria) from South China. subelegans Minato & Kato. and initially described by Roemer (1880). Collie.Permian palynostratigraphy of West Australian rift basins: resolving tectonic and eustatic controls during Gondwanan glaciations. p. collected by Verbeek and donated to Breslau University. corals. (1901). trilobites (Phillipsia). 84. (1961). brachiopods (Dalmanella. Geol. Y. He.. gracilis from Basleo beds) Fay. K. Ph. (M Permian reefal limestone from Guguk Bulat and Silungkang areas E of Singkarak lake. 2-3. Sumatra.D. Dev. Ser.J. Indonesia. Oklahoma Geol. J. with type species. 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Q. 305-319. a new Permian blastoid genus from Timor. p. Jin & Y. (2000). Backhouse (2002). but composed of Paleotethyan Ocean and two continental terranes affiliated with Gondwana and Cathaysian domains. Coral faunas include Sinophyllum. 21.. W. Ed.Mae Sariang area. Associated with rich fusulinid fauna.Uber Oberkarbonische Faunen aus Ost und Sudasien. (1986). D. H. (online at: http://archive. 237-255. Thesis Universite Libre Bruxelles. Q.O. Re- description of 59 Permian fossil species from dark limestones in Padang Highlands. Incl. S. Thomasiphyllum. Productus. Tripartite successions of glacial- deglaciation cycles (diamictite/ shale/ sandstone) of different ages and marked variations in thickness. respectively) Fliegel. Revue Micropal. Main oceanic basin was in 'Shan-Thai Block'.. represent Paleotethyan pelagic basin in Late Paleozoic-Triassic. late Ladinian and M Carnian radiolarians (51 species) from Mae Hong Son. small foram Hemigordius sp. p. 5.com March 2014 . Feng. Palaeoclim. I. Ipciphyllum fliegeli (Lange). I. 1. Palaeoecology 184. 36- 40. Mory & J. Micropal. R. Locally up to 600m thick. CCOP Techn. In: G. 20. p. H. Teh & S. Laos.. HvG)) Fontaine. Include Tabulata (mainly Sinopora.Discovery of Lower Permian corals in Sumatra. p. Unlike earlier papers here believed to be mainly of M-U Carboniferous age.Lower Carboniferous corals. (1986). Bull.) The Pre-Tertiary fossils of Sumatra and their environments.vangorselslist. (Extensive review of geology and paleontology of Permian of Thailand. (First record of E Permian corals from Sumatra. Waagenophyllum?)) Fontaine. p. Fontaine (ed. Pavastehphyllum) and rare compound rugosa (Paraipciphyllum. a very famous Permian limestone locality of Sumatra. H. Fontaine & S. No massive Rugosa found) Fontaine. H. Vietnam.Fontaine. tubular sponges. (1989). Bull.183-191. Paper 19. ranging up into earliest Permian (Moscovian. 112-127. (M Permian corals from three localities: some Tabulata (Sinopora asiatica) and abundant Tetracoralliia. E Thailand and Vietnam.) The Pre-Tertiary fossils of Sumatra and their environments. Paper 19. but some local recrystallization near ?Triassic granite intrusions) Fontaine. Mainly solitary Rugosa (Zaphrentites) and compound Rugosa (Siphodendron). 1. Muara Liso. Bangkok. CCOP Techn. In: H. and Wentzelloides (called Lonsdaleia by Volz 1904 and Lange 1925)). Geol. p. H.. Fontaine & S.com March 2014 . p. 81-89. (1989). Followed by 7 appendices on Permian fauna-flora by Fontaine. In: H.5 km NE of Singkarak Lake in Padang Highlands of ~150m thick grey. Paper 19. algae and occasional fusulinids (type locality of Sumatrina. Vachard and Vozenin-Serra)) Fontaine. p. Kuala Lumpur 1984.. Jurassic (Kedadom Fm) and Cretaceous (Pedawan Fm) ages (also reworked inn Paleogene of NW Kutai Basin. 5. Associated with M-L Asselian Pseudoschwagerina zone fusulinids.Permian corals of West Thailand. Kepingophyllum.Guguk Bulat. and is reefal facies) Fontaine. (1990).H. CCOP Techn. 41-44. (1986). Bangkok. bedded M Permian limestone rich in corals (including massive tetracorallia of Waagenophyllidae family). Indonesia. (1989). Fontaine (ed. Publ. 149-165. Jambi Province) Fontaine.1 296 www. Batu Impi): Protomichelinia.Lower Permian corals of Sumatra. Cummings (1961) and Sanderson (1966). Geol. (W Sarawak Terbat Fm dark grey limestone with fusulid foraminifera and little or no corals. 18. Michelinia). (1990). Gafoer (eds. (1990). Ed. Sumatra. Faunas many similarities with M Permian rocks on SE Asia mainland. Limestone not metamorphosed. Pebbles of possibly related fusulinid limestone found in conglomerates of Triassic (Sadong Fm). but very different from age-equivalent rocks of W Malay Peninsula. GEOSEA V Conf. p. Publ. Gafoer (eds.) Proc.173-181. solitary rugosa (Lophophyllidium. Paramananthan (eds. Malaysia Bull.) Ten years of CCOP Research on the Pre-Tertiary of East Asia. 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(Corals present but not prolific in Lower Carboniferous limestones of N and C Sumatra.The Terbat Formation of Sarawak (Malaysia): a very peculiar limestone. In: H. CCOP Techn. H. described earlier by Krekeler (1932). Nguyen Tien. CCOP Techn. Batu Gajah. Jahrbuch B73. In: H. H. (1988).) Ten years of CCOP research on the Pre-Tertiary of East Asia. H. H. Guguk Bulat rich and massive tetracorallia colonies (mainly Ipciphyllum spp. p. also Verbeekina). (Corals from W Thailand (Sibumasu Terrane) not abundant and mainly simple forms.Middle Permian corals of Sumatra. Amplexocarinia. CCOP Techn. Classic locality 3. H. Jambi Province (Sungei Luati. Rel. environments of deposition and to define crustal blocks and Permian paleogeography) Fontaine. poor coral assemblages of mainly solitary Rugosa. Publ. V. These characterize well-defined biogeographic unit (= Shan-Tai/ Sibumasu terrane. CCOP Newsl.S. 6. Chaetetes) Fontaine. Salyapongse. Bibliography of Indonesia Geology . Sumatra. Pseudohuangia. Bangkok. some associated with volcanics: Padang Highlands (Guguk Bulat. Local occurrences of thick-bedded cherts indicate deep marine environments. nothing similar in Australia. 9. near Lubuksikaping (Muara Sipongi) and N Sumatra near Takengon (Situtup Lst)) Fontaine. Suteethorn & D. Batang Tabir. Limestones with fusulinids. p. & S. Publ.12-17. (online at: http://library. 19.org/files/20121027151807120. Techn. Jambi Province. H. Guangzhou 1985. 17. p. (online at: http://permian. incl. Co-ord. I.. T. Asian Earth Sci. Ed. Peninsular Thailand.(NE of Loei in NE Thailand small outcrops of M Carboniferous(Visean. extending into NW Malay Peninsula with low diversity corals. HvG). 20. M. low diversity corals and fusulinids (Pseudofusulina.Pre-Tertiary limestones found at the bottom of wells drilled in Malacca Straits. E Malay Peninsula and Timor. p. 567-588. 129-151. Palepat). found to be Triassic. Gafoer (1989). CCOP Techn. 5. Kibul. Chonglakmani. H. H. Fossils rel. In: H. (Review of M Permian fossil localities of Sumatra. (M-U Permian-Triassic Ratburi Lst of Peninsular Thailand and Chuping Lst of NW Peninsular Malaysia with rel. H. Geinitzina.com March 2014 . Amnan & S. 4. p. Joint Prosp.A well-defined Permian biogeographic unit: peninsular Thailand and northwest Peninsula Malaysia. This E Permian flora and fauna similarities with C Europe. Widespread massive limestones represent extensive carbonate platforms. Sg. Gafoer (1989).pdf) (Limestone is widespread in Surat Thani Province and forms spectacular karst topography. including foram genus Shanita at depth 2630’. S. Some localities rich in Hemigordiopsis renzi. Tanjung Alai). etc. Volcanic rocks absent in NW Peninsular Malaysia and Thailand. 19. with high diversity assemblages similar to Cambodia. Staffella.The Middle Permian.. & S. Silungkang. known from >100 localities. Gafoer (eds. Pebbly mudstones in Myanmar.go. Fontaine & S. Bangkok. many with fusulinids. (1999). 99-112.Permian of Southeast Asia: an overview. Permophiles 33. Asian Offshore Areas (CCOP).H. Vietnam and S China. with smaller foraminifers Sphairionia sikuoides. on Geology of Thailand: towards sustainable development and sufficiency economy. J. p. Asiah & S. H. CCOP. Many limestones with fusulinaceans recognized as Permian. Hemigordiopsis and Shanita. (2002). Sanatul (1992). 36-38. from Lower to Upper Permian.vangorselslist. Multithecopora. Pachyphloia. (Four wells: Singa Besar-1 basal carbonate ('Tampur Fm'?) contain Middle Permian age fossils. but widespread in N Vietnam. J.1 297 www. Fontaine & S. In: GEOTHAI’07 Int. 47-51. Sg.Diverse Permian coral faunas are widely distributed in Thailand. NW Malaysia and Sumatra formed in glacial environment. Southeast Asian Earth Sci. Bukit Pendopo (Palembang). Laos. C. Monodiexodina). 221-228. Gafoer (eds. Conf. Endothyra. and with forams incl. but ones without fusulinaceans and previously assigned to Permian.) The pre-Tertiary fossils of Sumatra and their environments. Papers 22nd Sess. Two distinct provinces (1) E and C Thailand. rare due to dolomitization or recrystallization. p.th/library/Proceedings-Yearbooks/M_1/2007/12726.dmr. Piyasin (1994).pdf) (Summary of Permian coral distribution in Thailand.2740’ (generally associated with 'Sibumasu'/ Cimmerian terranes: HvG)) Fontaine. H. Vachard (2007). Thailand. Hoang.Permian limestone of Surat Thani Province. Faunal and floral assemblages used to establish climatic conditions.The Lower Permian..Bashkirian) limestones in two facies belts. Mainly limestones. and (2) Peninsular Thailand. (Lower Permian of Merangin River area W of Bangko. U Permian declining coral faunas) Fontaine. p. Noted similarities of several fossil groups with Timor Permian faunas) Fontaine. absence of corals in Lower Permian and no Ipciphyllum. In: H.T. (Permian rocks widespread in SE Asia. Ages probably mainly M Permian. Comm. Mineral Res.). well known since 1930's for its Cathaysian 'Jambi Flora' in Mengkarang Fm.stratigraphy. incl Monodiexodina wanneri in Padang Higlands (Hahn & Weber 1981)) Fontaine.) The Pre-Tertiary fossils of Sumatra and their environments. Peninsular Malaysia.) Proc. Fusulinella. Geol. Verbeekina. (2) Jengka Pass black shale with limestone lenses with Michelinia and fusulinids a. Kavinate. V.. p. Kavinate. Geol. Bull. Papers 2. primitive Verbeekinoids (Pamirina leveni. H.).. palaeogeographic significance. etc. W Thailand. Malaysia. Pseudostaffella. H. fusulinids (Schellwienia.Important discovery of late Early Permian limestone in Southern Terengganu. Nguyen & D. In: G. 39-47. Suteethorn & D. T. algae (Mizzia. rare Fusulinidae and solitary corals.The Neoschwagerina -zone and the Lepidolina-Yabeina -zones in Malaysia and the Dzhulfian-Dorashamian in Malaysia: the transition to the Triassic. Vachard (2013).) and corals (mainly solitary Rugosa). Amnan & D. 1-65. in Seri Bandi area in E part of Malay Peninsula. Malaysia Bull.com March 2014 .or.H.T. 69-99. Sumatrina. Kuala Lumpur. p.1 298 www. indicate three Late Cisuralian (=Artinskian-Kungurian) biozones. & Ibrahim B. near Myanmar border.). Energy Res.P.a. Ibrahim B. Geol. Cha-am and Thong Pha Phum areas. also Mizzia. In: B.L. fasciculate and massive Rugosa) (= Ratburi Lst of Shan-Tai/ Sibumasu terrane. etc. Ibrahim B. 9th Congr. Chiang Mai. Levenella. Soc. calcispherids.Carboniferous corals from the Kuantan area. Fontaine. Papers 4. 453-460.A. Misellina). (Small exposures of grey-black . etc. Tubiphytes). Profusulinella. Soc. S. 38. Leeina. Khao Yoi localities rich in fusulines (Eopolydiexodina a megasphaerica) indicating U Murgabian/ M Permian age. Permocalculus). Khoo D. Geological Survey of Malaysia. H. (3) Bukit Biwah M Permian Bibliography of Indonesia Geology .pdf) (Carboniferous limestones in NW Thailand.).Carboniferous of Malaysia: biostratigraphy and paleogeography. Soc. Chalaroschwagerina. (Description of M and Late Permian corals from three localities on E Malay Peninsula: (1) Bukit Kepayang quarry (Kampong Awah) andesite with dark limestone blocks with Waagenophyllum and Ipciphyllum. Hoang & D. etc. Thailand. Very different from Carboniferous of Peninsular Thailand) Fontaine. (1999). Palaeofusulina. Vachard (1994). M.org/nhbsspdf/vol051-060/NHBSS_058_1k_Fontaine_PermianLimestone. GEOSEA ’98. (Karsted limestones of Kinta valley probably of Permian age) Fontaine. 159-172. Hemigordiopsis. p. Endothyra. Ed. etc. algae (incl. Brevaxina. Rocks of area previously considered Early Carboniferous age) Fontaine. Ibrahim B. fossils similar to above . Nat.. more widespread than previously thought (usually assigned to Permian). Other samples rich in low-diversity Fusulinidae (Parafusulina spp. Permocalculus. Issue. Cha-am. 500 m from granite.. H. solitary.T. Malaysia Bull. Fontaine. Ratanasthien & S.Wide extension of Carboniferous Limestone in Northwest Thailand with an interesting stratigraphy. etc. Descriptions of localities and diverse assemblages of smaller foraminifera . 65-78.T. Ipoh. 58. J. In Cha-am District M Permian corals (Paraipciphyllum. 26-44. p. Vachard (2003). Perak. N of Chiang Dao. Vachard (2012). Int. Techn. and associated microfauna: peculiar faunas for Southest Asia and puzzling faunas for stratigraphy. Spec. Peninsular Malaysia. Soc. Amnan & D. 1-74.. H.Permian limestone of Peninsular and Western Thailand in Khao Yoi.) Proc. H. H.Biostratigraphy of the Kinta Valley. Toriyamaya. Amnan. Hoang. abundant fusulinids (incl.Some Permian corals from East Peninsular Malaysia: associated microfossils. Southeast Asian Earth Sci. Symposium on Shallow Tethys 5. S. (online at: www. Minerals and Geoscience Dept. In Thong Pha Phum. p.gst. p. 43. p. Estimated thickness 90-300m. also suggesting M Permian Shan-Thai fauna (=Sibumasu) Block) Fontaine. Yangchienia.vangorselslist. & Ibrahim Bin Amnan (1995). smaller foraminifers (Tetrataxis..th/sites/default/files/GST-Limestone-E-book. Min.Globivalvulina and Agathammina. Chusenella) with few. late E Permian massive shallow marine limestone.. HvG)) Fontaine. common Tubiphytes. p. Lys & Nguyen Duc Tien (1988). 2. Kanchanaburi Province. Hist. With stromatolites. fusulinid forams Neoschwagerina. Vachard (1999). T. H. J. Rieb (eds. Fontaine.. Geol. Geol. SE Asia. Siam.. Petchaburi Province) and W Thailand.. Sinopora asiatica) and fusulinids (Yangchienia iniqua).pdf) (Paleontological study of limestones in N Peninsular Thailand (Khao Yoi. 5.siamese-heritage. with Sinopora asiatica and Paraipciphyllum. H. low diversity corals (Tabulata. Teh (ed. (online at: http://www. ~360km NNE of Bangkok. Chusenella. 1-107.th/library/Proceedings-Yearbooks/M_1/2002/6375. Profusulinella. Bangkok. 51.thaiscience.Permian fossils recently collected from limestones of Nan area.. CCOP Techn. energy and water resources of Thailand: towards the year 2000. 250km NE of Bangkok. S.com March 2014 . p.info/journals/Article/Glimpses…) (Review paper of fossil corals of Thailand. Nguyen D.The Permian of Khao Tham Yai area in Northeast Thailand. E Malay Peninsula and Sumatra (Indochina. Peninsular Thailand (= Shan-Thai/ Sibumasu terrane. Bangkok 1999.massive limestone with Parawentzelella and algae.Permian corals of Southeast Asia and the nearing of a recent discovery of Lower Permian corals in Northeast Thailand.E Malaya terrane'. p. S. Verbeekina verbeeki. H. p. p. with rugose corals. (online at: http://library.th/library/Proceedings-Yearbooks/M_1/1999/6617.pdf) Bibliography of Indonesia Geology .dmr.. Conf. & V. CCOP Techn. Tien & D. Parafusulina gigantea. Central and NE Thailand.go.1 299 www.dmr.pdf) (M Permian limestone around Nan. H. N Thailand. Staffella. Of Cathaysian affinity. incl. 45° E-dipping M Permian limestone of Tham Yai hill cave in Nam Nao district. Vachard (2002). Central Thailand. Also Latest Permian with Colaniella and ?Paleofusulina in area. 1. Carboniferous volcanic section overlain by E-M Permian limestones (=W margin Indochina Block?. In: Symp.) and mainly massive rugose corals (Ipciphyllum.dmr. with strong affinities to S China. HvG). more abundant and and more diverse than NW of Malay Peninsula) Fontaine. 24. Suteethorn (1992). (Permian corals common and diverse assemblages in SE.Glimpses into fossil assemblages of Thailand: coral perspectives.Jurassic faunas) Fontaine. Salyapongse & V. thick-bedded. p. In: N.pdf) (M-U Carboniferous fossils from black limestone lenses intercalated in basic-intermediate volcanoclastics E of Lam Narai.pdf) (>700m thick. & V. H.) Proc. Lepidolina.. smaller foraminifera and fusulinids (Pseudodoliolina cf. Rare fusulinds. In: N. Suteethorn (1988).Permian corals of Thailand. Assemblages of E Malay Peninsula corals and fusulinids different. Nat.th/library/Proceedings-Yearbooks/M_1/2002/6376. incl.) Proc. Symposium on Geology of Thailand. Mineral.go. H. Nankinella. affinities with Vietnam and S China) with rich coral faunas.. Bull. Hist. Siam Soc. Salyapongse. p. HvG)) Fontaine. Bangkok 2002. Piencharoen (ed. 37-67. Suteethorn (1994). (W Thailand part of Shan-Thai/ Sibumasu Block. Parawedekindellina(?). Vachard (2002). (online at: http://library. Bangkok 2002. 20. Carboniferous. Multimurinus) (Lower Midian Horizon 3 comparable to Guguk Bulat fauna of Sumatra?)(see also Fontaine & Salyapongse 2001)) Fontaine. Descriptions of Devonian. Mantajit (ed. Devonian and Jurassic corals locally common. Resources. Suteethorn (2003). Typical Tethyan/ Indochina Block assemblages of fusulinids (incl.go. Nguyen D. pseudolepida.E Frasnian. Lower Permian (Asselian-Sakmarian) unknown in area. etc.th/library/Proceedings-Yearbooks/M_1/1992/6234. Dept Min. H. 58-76. C Thailand. Salyapongse & D. Bull.Late Paleozoic and Mesozoic fossils of West Thailand and their environments.) Proc. Permian and Triassic corals widespread. p. (online at: http://library. 45-57. Vietnam. N.. 1- 108. etc.dmr.vangorselslist.. stromatoporoid Chlathrodictyon and tabulate coral Heliolites porosus (= same taxa as reported by Rutten 1940 from NE Kalimantan)) Fontaine. although Nan area is separated from Indochina block by Nan- Uttaradit suture) Fontaine. Symposium on Geology of Thailand.Protriticites. schwagerinids. Salyapongse. Bull. Sattayarak & V. Vachard (2000). 5. Tien & D. Geologic resources of Thailand: potential for future development. (online at: http://library. Cambodia. Includes Devonian limestone in NE Thailand area near Laos border (possibly Givetian. H.go. Ordovician and Silurian corals rare and poorly known. S. Colania douvillei. 201-211. In: C. (online at: http://www. HvG) only rare corals belonging to Tabulata and solitary Rugosa and with low diversity fusulinids) Fontaine. 346-354. but unknown in Australia. Sumatrina.New Carboniferous fossils found in Ban Bo Nam area. Nat. North Thailand. S. Mantajit (ed. Ed. H. Suteethorn & D.Carboniferous corals of Thailand.(Brief review of Permian corals of SE Asia. Afghanella. Absent or only rare tiny corals without dissipiments in Peninsular Thailand (=Sibumasu terrane. H. W Europe. Tabulata (Syringopora. (online at: http://library. No corals found in Carboniferous of Peninsular Thailand or NW Peninsular Malaysia (Sibumasu)) Fontaine. 1-17. p. near Burma border. all of which are richer and more prolific than those from Australia.Moscovian to Gshelian coral assemblages in northeastern Thailand: field- relationship between Carboniferous and Permian strata. Bangkok 2002. In parts of area overlain by Permian (mainly limestone). etc. Schubertella). p. CCOP Techn. Carboniferous of N Thailand affinities with S China. 35-37. In SE and NW only rare solitary Rugosa. Rugosa most common. V. Chiang Mai. more affinities to Indochina than Sibumasu. 3.go. Bull. limestone is rare and fusulinids and compound corals are absent) Fontaine.The Carboniferous corals of Southeast Asia with new discoveries in Laos and Thailand. p. 5. Kepingophyllidae) Fontaine. Verbeekina. Bibliography of Indonesia Geology . Most diverse coral faunas in 'mid-Carboniferous' (Upper Visean. Bangkok 1994. 25-42. (Carboniferous corals abundant in C and NE Thailand. Sphairionia.The coral Koninckophyllum in the Early Carboniferous of Thailand.. (All stages of Carboniferous represented in NE Thailand (Indochina Block).Khao Yoi. shale and chert occur occasionally in C and N parts of area. E Permian (Sphaeroschwagerina. incl. Overlain by Permian (Asselian) sandstones-limestones and M Permian fusulinid limestone) Fontaine. mainly solitary Rugosa.Carboniferous and Permian limestones in Sop Pong area: unexpected lithology and fossils. Jongkanjanasoontorn (1991).The Carboniferous of northeast Thailand: a review with new data. E of Loei.Lower Serpukhovian.vangorselslist.dmr. 34-41.. Rugofusulina). Suteethorn & Y. Japan. H. Symp. Loei Province. Stratigraphic correlation of Southeast Asia. Sumatrina. low diversity. Vachard (1995). Tansthein (1987). Vachard (1998). M-U Devonian limestone. (online at: http://library. a Permian limestone hill of the Ratburi area. where. J. Sumatra corals of Padang and W Jambi regionshigh diversity reefal limestone. as in NW Australia. Ed. H. algae (Permocalculus).go. V. Thailand 2000. very rare corals. V. H. foraminifera (Dagmarita. Suteethorn & D.th/library/Proceedings-Yearbooks/M_1/1994/6937. & V.pdf) (New M-U Carboniferous (mainly Moscovian) coral limestone localities in Ban Na Duang area. p..th/library/Proceedings-Yearbooks/M_1/1993/7487. Geol. Biostratigraphy of mainland Southeast Asia: facies and paleontology. Terbat Lst of W Borneo common fusulinids. Suteethorn (2000). In: Proc.dmr. transitional form between Hemigordiopsis and Shanita). V. and Alas River in N Sumatra. Chaetetes) rel. NW Peninsular Malaysia and Timor. Peninsular Thailand. corals (Sinopora. H. Int. p. p. With diverse fusulinid foraminifera in Late Carboniferous (Triticites. but differs from Peninsular Thailand/ NW Malaysia. & W.th/library/J-Index/2000/148. Soc.dmr. H. 22. Suteethorn & D. Mizzia. Vachard (1993).go. U Tournaisian-Visean and U Carboniferous limestones rich in corals. Timor corals rel.com March 2014 . V.pdf) (On thick reefal E Carboniferous (Visean) Late Permian Doi Chiang Dao Limestone in Inthanon Zone of NW Thailand. H. Southeast Asian Earth Sci. Sumatra only place in Indonesia with Carboniferous corals: Visean at Muara Gorge in C Sumatra. Hemigordiopsis.1 300 www. CCOP Newslett. In: Proc. primitive Colaniella). HvG)) Fontaine. 23. Also Hemigordius. 12. 12-14. NE Thailand.. HvG). etc. Permian corals of Thailand more diverse than Peninsular Thailand.pdf) (Review of geographic and stratigraphic distribution of Carboniferous corals in SE Asia (generally rare). algae. rare))) Fontaine. Int. 1-73. Vachard (1994).. fasciculate Waagenophyllidae) (= late M Permian 'Sibumasu Fauna'. but few or no corals. Now considered to be Paleotethyan seamount carbonate) Fontaine.. p. 319-336. Permocalculus. J. Symposium on Geology of Thailand. M Permian (Neoschwagerina. Suteethorn & D. (online at: http://library. Symp. 1. In: Proc. (Midian-age Ratburi Lst at Khao Yoi with Pseudoalgae (Tubiphytes). New Lower Permian fossil localities in NE Thailand (Loei) with solitary and compound rugose corals. W Sarawak lower Terbat Lst is of M-U Carboniferous age. M.Early Permian ammonoids from the Kaeng Krachan Group of the Phatthalung-Hat Yai area. = youngest coal seams and with last known Glossopteris).. 739-752 (Late E Permian (Kungurian/ Bolorian) small ammonoid fauna with Neocrimites. Bisatoceras. samoilovichii). changxingensis. 5. & T. commonly associated with Glossopteris). Diaboloceras involutum. Vachard (1981). Pseudogastrioceras. Saengsrichan. (Ammonoids from N Thailand in latest Permian of Lampang (Prototoceras. Sardsud. W. 14-18. Ed.1 301 www. Geol. Publ. Nakornsri (1999). Pseudoparalegoceras sp.B.M. 153-175. W Timor) Bibliography of Indonesia Geology . Ruasnain. Gzheloceras.go. southern peninsular Thailand. T.Spore-pollen assemblages of the Bowen Basin. Agathiceras suessi.th/library/Proceedings-Yearbooks/M_1/2002/6374. West Pakistan. occurrences from Basleo. indicative of Namurian.A note on the discovery of Lower Carboniferous (Middle Visean) in Central Sumatra. Geol.F. Malaysia Bull. Xenodiscus) and Carboniferous from Loei and Sop Pong (Lower Pennsylvanian. 372. Mem. Ishibashi & N. E of Bukit Tinggi along road to Payakumbuh. Temnocheilus and Epistroboceras. from old to young:“Upper Stage 5” (= Dulhuntyipora zone of authors. No range charts (Morante 1996 suggests Base P..my/products/702001-100793-PDF. 30. N Thailand.gsm. Protohaploxypinus microcorpus Zone (also with P. Pronorites.pdf) (E Carboniferous rugose coral genus Koninckophyllum not common in Thailand. A. (1982).. incl. clastic-dominant shelf to temperate. p. Neogastrioceras.dmr. Asian Earth Sci. Queensland (Australia): their relationship to the Permian/Triassic boundary.vangorselslist. No regional metamorphism. Pseudotirolites. (On M Permian ammonite Cyclolobus. Lower Carboniferous limestones rel. Palaeobotany Palynology 36.subtropical. carbonate platform. Soc. 165-183. NE Australia) Foster. Gastrioceras. Paralegoceras. & D. Tapashanites floriformis.Permian ammonoid Cyclolobus from the Salt Range. T. W. (online at: http://www. Ueno. (Permian palynology of Bowen Basin. Environment of Sibumasu Block changed around this time from cool. Catastroboceras subsulcatifomae. Epidomatoceras doohylense. (1979). Ishibashi (1999). latest Permian or E Triassic?) and Protohaploxypinus samoilovichii Zone (= E Triassic). northern Thailand. Paratirolites. C. ~15m below Ratburi Lst (with Monodiexidina in basal transition beds )on S Peninsular Thailand (= Sibumasu block) suggests these beds are of Kungurian/Bolorian age. Second locality in C Thailand. girtyi and Miklukhoceras from uppermost Kaeng Krachan Gp. CCOP Newslett.Permian plant microfossils of the Blair Athol coal measures. Congress Geology. J. p. M. 1. Science. Playfordiaspora crenulata Zone (M Permian.Carboniferous and Permian ammonoids from North Thailand. Rev. slightly younger than previously considered. etc. 43.Moscovian age. Kuala Lumpur. M. poor in fossils and darker than associated Permian fusulinid limestone.Middle Carboniferous cephalopods from Loei area. C. 467-475. microcorpus is ~Base E Triassic = base of Mt Goodwin shale in Bonaparte basin) Fujikawa.pdf) (Abundant M Carboniferous cephalopods at 'Barite Mine'. In: Ninth Reg. p. 6. Kamata & K. K. Survey Queensland. D. Fac. & B. just local contact metamorphism around igneous intrusions) Foster. Lunatisporites pellucidus Zone (also contains Falcisporites= Alisporites?. 8. p. H. In: Stratigraphic boundary problems: Permian and Triassic of West Pakistan. Mineral and Energy Resources of SE Asia (GEOSEA '98). p. and basal Rewan formation of Queensland. Syngastrioceras.org. With brief overview of known Late Paleozoic ammonoid localities in Thailand) Fujikawa. Ammonoid fauna much less diverse than probably coeval faunas of Timor) Furnish.E Triassic of Bowen Basin.) Fujikawa. 1-244.(online at: http://library. Kyushu University.com March 2014 . p. 24. Five genera of ammonoids and 5 nautiloids: Branneroceras branneri. (Five palynofloral zones in M Permian. 91-110.B. in M Visean limestone 40 km SW of Phetchabun) Fontaine. Baralaba coal measures. Y. (Lower Carboniferous limestones with M Visean foraminifera in Agam River. N Loei city. p. A. Hisada (2005). Glenister (1970). collected by Verbeek) Gerth. Geol.B. Coloquios de Paleontología. Mutis region. Metalegoceras involutum. Colaniella) Gaillot. crinoids. (1876).Roadian of Bitauni. Potonieisporites spp. NW slope of Mount Somohole ~3 km SW of village at Fatu Bena. The Somoholitidae: Mississippian to Permian Ammonoidea. W. p.Die Anthozoen der Dyas von Timor. 100-118. Interradispora.. T. 'Lysites'. Nederl. etc). ('The paleontological character of the Permian coral fauna of Timor'. & B.sp. Jaarboek Mijnwezen Ned.West Yunnan and its geologic significance.Der palaeontologische Character der Anthozoenfauna des Perms von Timor. p. E Thailand) characterized by presence of Lepidolina. Timor Expeditie 1910-1912. J. new species. p. ('The corals from the Permian of Timor'. With Neopronorites timorensis. (1921). New sponge species from Permian limestone. J. 55 species. Waagenina dieneri. Ed. Asselian-Sakmarian in age) Geinitz. (Middle. Schweizerbart. (2007). p. ranging from S Turkey to S China and up to Japan) Gao Lianda (1998). Indie 7 (1878). (1909).. (First record of palynomorphs from E Permian Dingjiazhai Fm in Baoshan.S China plates (e.Zur Geologie von Sumatra's Westkuste. 65-147. W Sumatra. Palaontologie von Timor. Eopolydiexodina ex. Hemigordiopsis renzi.) and 3 species of 'waagenophyllid' colonial rugose corals (Lonsdaleia. Reprint of Geinitz. Vachard. new foraminiferal taxa. ('On the geology of Sumatra'. J.B.g.sp. H. 1. Descriptions of grey limestone with globular fusulinids (incl. 399-414. Brakarites rotatus. Carcinophyllum. Martini (2009). In: W. Paleogeographic distribution interpreted to be Neo-Tethyan regions. Paleobiogeographically significant M-L Permian foraminifera for Cimmerian/ Sibumasu blocks incl. 405-414) Geinitz.F. ('Timorella permica.1 302 www. p. W Thailand. Oost-Indie 49 (1920). 1. 16. Fusulina verbeeki n. (Somohole Horizon of Kekneno series.New latest Permian foraminifers from Laren (Guangxi Province. p. Miospore assemblages assigned to Parasaccites distinctus-Microbaculispora fentula zone.) Gaillot. Jaarboek Mijnwezen Nederl.The Lower Permian Somohole fauna of Timor.sp. and Vachard. n. S China) with rich small foram fauna. Verh. persica. p. probably of Sakmarian age. H.W Yunnan. Properrinites. Verbeekiella. Stutgart. South China): palaeobiogeographic implications.On the discovery of a Gondwana affinity microflora from Baoshan. 695-700.Furnish.. Carcinophyllum from Artinskian. Somoholites beluensis. New Bibliography of Indonesia Geology . First and still principal monograph on Permian corals from Timor. 5. Dominated by solitary corals (Timorphyllum wanneri. etc. (1878). Paleofusulina.g. Microbaculispora. HvG). incl. Geobios 42. Glenister (1971). brachiopods. a new lithistid from the Permian of Timor'. ('On the geology of Sumatra's West Coast'.Zur Geologie von Sumatra. and palaeogeographical implications. Horriditriletes. Michelinia)) Gerth. D. (Latest Permian limestones at Laren (Guangxi. p.. H.Timorella permica n.).Late Permian foraminiferal biostratigraphy for 'Cimmerian Plates' of Middle East (can be applied to to Sibumasu plates in SE Asia. Basleo).com March 2014 . p. N West Timor is one of oldest Permian horizons. Acta Geoscientica Sinica 1998. Indochina. 1909. gr. D. 1-30. Saunders. 37-223. 15 species of solitary rugose corals (Timorphyllum. Also 50m thick Eocene coral limestone Companion paper by Von der Marck (1876) on Tertiary fossil fish from region.vangorselslist.. 9. Agathiceras. Min. 45. 57. New species Somoholites deroeveri n. The Khuff Formation (Middle East) and time-equivalents in Turkey and South China: biostratigraphy from Capitanian to Changhsingian times (Permian). Juresanites somoholensis. III. Parasaccites distinctus.B. 127-137. etc. H.M. Baoshan) include Shanita. Centralbl. Brief description of rocks collected by Verbeek from Ombilin area. Palaeont. Galfetti & R. (1921). 1. etc. 1876) Gerth. Verbeekiella. p. new genus. dominated by Gondwana microfloral elements (up to 80%. 141-168. Palaeontographica 22. Propopanoceras boesei. eine neue Lithistide aus dem Perm von Timor. H. Palaont. Amsterdam.-Indie 55 (1926). C. Key paper on Timor Permian ammonite zonation and correlations with Sumatra. Jaarboek Mijnwezen Nederl. 5. ('The sponges from the Permian of Timor'. Waagenoceras (Sosio satge).A.vangorselslist. but whole sponges mainly known from Permian and Triassic of Timor. B. Mortieria permica from Tai Wei near Basleo) Gerth. 1952). (Single specimen of Cyclolobus persulcatus Rothpletz (1892) from Hardman Fm. Alps. B. Ser. Furnish & G. J.naturalis. & W. Doct. Geol. 399-402. (1944). Baker. from old to young: Properrinites (Sakmarian). p. Gen. Furnish & J. (‘The ammonoids from the Permian of Timor and significance for zonation of Permian formations’. 233-320.) 2e Nederlandsche Timor- Expeditie VI. 3. mainly siliceous sponges. Paleontology 35.. H. suggesting these areas were farther apart in Permian time. Isolated sponge needles known from various formations in Indonesia.M. 7-14. Canning Basin. Perrinites (Artinskian). At least 25 species of siliceous sponges in Permian.F. Paleontology 64. Geol. B. Five ammonoid zones in Permian. W.G.The Permian ammonoids of Australia.R. etc.C. crinoids and fusulinids and is typical warm water fauna. Leidsche Geol. 4. 91. W.repository. H. p.Die Spongien aus dem Perm von Timor. (1929). 392-399. 25 species. ('A new species of the sponge genus Mortieria from the Belgian Carboniferous from the Permian of Timor'.Porifera. Youngest Permian ammonoid known from Australia. (1931). No figures) Gerth.. p. H.F.Die Korallenfauna des Perm von Timor und die Permische Vereisung.M. Abhandl. R. Ed. Thesis University of Amsterdam. In:B. (‘The coral fauna of the Permian of Timor and the Permian glaciation’. H. About 100 specimens.M. (1950). etc.Eine neue Art der Spongiengattung Mortieria des belgischen Kohlenkalkes aus dem Perm von Timor. 93-132. Verhandelingen Geol. 14 (Tesch volume). Most common species is Neoproetus indicus Tesch. Palaont. Escher et al. Timorites (Basleo stage) and Cyclolobus (Chidru stage)) Gheyselinck. H. Mijnbouwk.M.Late Permian ammonoid cephalopod Cyclolobus from Western Australia. Originally described from W Timor Late Permian 'Amarassi fauna') Glenister. 673- 736. Paleontology 64.com March 2014 . (eds.nl/document/549435) (Porifera (sponges)chapter in 'Our paleontological knowledge of the Netherlands East Indies'. J. p. C. B. (Svetlanoceras irwinense (Teichert and Glenister. Martin). mainly from Basleo. 1-108.F.Die Ammonoiden des Perm von Timor und ihre Bedeutung fur die stratigraphische Gliederung der Perm-Formationen. Dickins (1990). from basal Callytharra Fm oldest ammonoids from Permian of Carnarvon Basin) Glenister. p. 7 species. 1. It is contemporaneous with glaciations in nearby Australia. Japan.. No locality maps or stratigraphic info) Glenister. 115-119.1 303 www.sp. China. Mededelingen 5 (Feestbundel K. Neues Jahrb. (online at: www.F. Scheltema & Holkema. p.Additional Early Permian ammonoid cephalopods from Western Australia. collected by 1916 Jonker Timor expedition. p.A. Furnish (1961). Thomas (1990). Permian of Timor 25 species. Timor Permian marine fauna rich in corals.. most of them new. Brouwer (ed. In: H. (1926).Permian trilobites from Timor and Sicily. Baker.. (= Ipciphyllum timoricum) from Fatu Oinino on road to Nenas and Favosites permica from Basleo) Gerth. (Comprehensive study of rare trilobites from Permian of Timor. 199-203.colonial corals Lonsdaleia timorica n. p. p. 2. Verhandelingen 1. Rather endemic assemblage of lithistids) Gerth. With world map showing distribution of Permian floras and faunas) Gerth. J. 3. Mededelingen 2. Triassic of Timor mainly calcareous sponges. Bibliography of Indonesia Geology . (1937).) Onze palaeontologische kennis van Nederlandsch Oost Indie. Leidsche Geol. Furnish (1988).M. associated with rich brachiopod fauna described by Archbold (1982).F.M.Ammonoid cephalopods from the Lower Permian of Thailand. Four species identified: Miklukhoceras cf.go. Timor) Glenister. Advanced perrinitid suggestive of Late Artinskian (Baigendzhinian).Patterns in stratigraphic distribution of Popanocerataceae. Prostacheoceras cf. Birds Head. Tamiabuan sheet. Pseudoschistoceras irianense n. p. Baun area.S. 1940. (Late Early Permian (Artinskian) cephalopods from Aifam B (Aifat) Fm mudstones in Aifam River. J. Paleontology 47. 74-85. Zhou (2004). from Amarassian beds at Kuafeu.. Furnish & Z.G. Furnish (1987). Propinacoceras. P. No figures) Glenister. (eds. Res. 6. Skwarko (1983). 43-71. Ser. diverse.F. Geol. Basleo) and D.vangorselslist. Metalegoceratidae are distinctive element of Lower Permian 'Boreal' ammonoid realm) Goodall. (With descriptions of Propopanoceras boesei (Smith) from Somohole and Epitauroceras soewarnoi n. clarkei Miller conspecific with senior Indonesian synonym. Dominant species Punctatisporites/ Retusotriletes spp. Zhou &M. australe (Smith). W. ancestral to Waagenoceras-Cyclolobus lineage. p.K. redescribed from Roadian of Timor) Glenister. 982-998. Indonesia. Int. 3. a new Upper Permian (Wuchiapingian) ammonoid from Indonesia (Timor). A. 4.L.com March 2014 . lidacensis (de Roever. oshense.Metalegoceras. Glenister & S. B. & W. Perrinites cf. 479-780. Paleontology 61. B. Baun area. pamiricum. Dev. from Aifat Fm) Glenister. etc. Senckenbergiana Lethaea 69. Ed.. Incl. Agathiceras.sp. Ecologically. Thai ammonoids close to assemblages of SW China and Pamir. 1-2. Associated with cyclolobid genera Timorites and Cyclolobus. based on collections from W Australia.~150 km NE of Bangkok. p.) Proc. Dheeradilok et al. B. Polahan (1990). 1031-1043.F.M. Spore color 4-5 (heavily carbonised. hilli. Bangkok. 56-61. (New species Eohyattoceras gerthi and Cardiella martodjojoi from late Early Permian (Roadian) of Basleo and Bitauni. Hightom (1997).M. Bandung.F. P. In: P. J. (online at: http://library.F.New Permian representatives of ammonoid superfamilies Marathonitaceae and Cyclolobaceae. (Taxonomy of Lower Permian Juresanites.pdf) (Clastic basement in wells 7-152-1X and 8-320-1X at W flank of N Pattani Trough in Gulf of Thailand with mod. J. formerly assigned to Waagenoceras. mainly from sedimentary basins of W Australia. Centre. cosmopolitan mid-Tournaisian miospore assemblage..Paedopronorites. Racey & P. p. J.F. Timor and Oman.M. No strat info) Glenister. Amarassi Province. 1014-1015. p. M.th/library/Proceedings-Yearbooks/M_1/1997/7622. Palaeont. Speleotriletes balteatus and Vallatisporites vallatus. Windle & W. from Lidak district). in dry gas or barren maturity window)) Bibliography of Indonesia Geology . W. Stratigraphy and tectonic evolution of Southeast Asia and the South Pacific. B.1 304 www. Conf... L. B. 5.sp. D. Paleontology 64. 1950 from Tae Wei. simile Teichert) Glenister.. B. Timor. Furnish.. Names Paralegoceras sundaicum form.dmr. hanieli (Smith) (both formerly Gastrioceras).M. M. Paleontology 78. Pseudoschistoceras gigas (Smith) from Bitauni beds of Timor figured and compared with P. Furnish (1973)-Australasian Metalegoceratidae (Lower Permian Ammonoids). Permian Ammonoids. 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(32 species of radiolaria from 20 chert samples of folded/faulted Semanggol Fm in N and S Kedah. Northwest Peninsular Malaysia. Aljinovic (2009). Y.A. sutschanica and M. Thailand. 171-181. Y. Halobia comata. Basir (1991). (online at: http://geology. This 'tropical trio' became extinct near Guadalupian-Lopingian boundary.1 311 www.M Triassic) Jasin. p. Verhandelingen Kon.Die Variationsstatistische Methode angewandt auf ein groszes Material von Schizoblastus aus dem Perm von Timor und einige neue Anomalien dieser Gattung. I.Discovery of Early Permian radiolaria from the Semanggol Formation. Iskandar E. M Triassic cherts interfingers with Ladinian-Norian mudstone with Posidonia kedahensis. van Waveren & J. Asian Earth Sci.Some Permian radiolarians from Bukit Yoi. 11-21.. Interbedded with siliceous and tuffaceous mudstone. Associated terrigenous detritus suggest deep continental margin setting. 5. Tokyo.) 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Fauna represents upper Pseudoalbaillella lomentaria Zone. Pseudoalbaillella fusiformis and Follicucullus monacanthus..H. Basir (2013). Located near E margin of Bentong suture and above andesitic volcanics and sheared olistostrome unit. incl. (eds. Tuffaceous sediments became widespread in Late Permian and Triassic) Jasin. Harun (2001). Basir & C. with 34 radiolarian taxa . p. (22 radiolaria species from 30m folded chert sequence in roadcut near Pos Blau.Middle Permian radiolarians from the siliceous mudstone block near Pos Blau. Steeply dipping to SE. lower part ribbon chert.Lower Permian Radiolaria from the Pos Blau area. Geol. Geol.my/products/702001-100333-PDF. Geol.wordpress.gsm.and early Late Triassic conodonts (Metcalfe 1984. p. Geol.Chert blocks in Bentong-Raub Suture Zone: a heritage of Palaeo-Tethys. Ali (1997). incl. Soc. Ali (1997). Teh et al.edu.Jasin. Soc. Southeast Asian Earth Sci.com/2014/09/bgsm1997028. 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(eds. B05.A. Assemblage similar to W Europe and suggests deposition in equatorial regions of Tethys.1 312 www. Pangkor. Ulu Kelantan. 1992). Most of Posidonia in area very closely related to Posidonia becheri) Jasin. 69-71. Teh et al. Harun (2001). Basir (2013). J. 85-91. divided into two zones. (online at: https://gsmpubl. New samples from clastic-chert sequence at base of Bukit Kechil with 11 taxa of radiolarians. Ipoh 2013. northwest Peninsular Malaysia. Tuffaceous material related to volcanic activity on E Malaya terrane. E. Probably Lower Carboniferous age. Overlying limestone at Bukit Kechil with M Triassic conodonts (Koike 1973) and foraminifera (Gazdzicki & Smit 1977)) Jasin. Basir.) Proc. 105- 109. Geol. Ulu Kelantan and their significance. deflandrei and A. p. (2) Tournaisian. Basir & Z. Negeri Sembilan. Soc.Some Triassic radiolarians from the Kodiang Limestone. (online at: www. Geol. Nat. Geol.H. In: G. M Permian/ Wordian Follicucullus monacanthus Zone) Jasin. 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Dyscritella and Streblascopora exilis indicate Artinskian age. U. porrectus Neoalbaillella ornithoformis and N.edu. p. (online at: http://geology.edu. 1. Geol.. 47-54. Abdul Rahman (1995). Warta Geologi 18. Bibliography of Indonesia Geology . Bryozoa genera Fenestella. Polypora. Geol. Five radiolarian zones recognized (Pseudoalbaillella scalprata. Malaysia 57.um. J. U. 2. optima). 14km N of Kuah. from Frasnian (Late Devonian) Triassic. (online at: http://geology.Permian radiolarian biostratigraphy of the Semanggol Formation. Sains Malaysiana 19. Said & R.files. Soc.Jasin. Malaysia. Tournaisian radiolarian cherts widespread in Paleo-Tethys ocean) Jasin. older than Sakmarian.Lower Carboniferous (Tournaisian) radiolarians from Peninsular Malaysia and their significance. W. Thailand) Jasin. 53. Ed. 79-83. Geol.my/gsmpublic/BGSM/bgsm57/bgsm2011007. Bukit DurianPerangin. at E side of Central basin of Malay Peninsula.Late Permian) Jasin. 12. Saad (2005). (online at: http://geology. Z. 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Assemblage with Entactinia spp.my/gsmpublic/BGSM/bgsm57/bgsm2011005. clastics and overlying Ratburi Lst-equivalent in NW Malay Peninsula (= 'anti-tropical' genus from Kungurian or Artinskian of Sibumasu Terrane. Malaysia Bull. Peninsular Malaysia. Soc. S Kedah. south Kedah.wordpress.com/2014/09/bgsm2005004. 27-38. (Nine species of radiolarians from tin. 2004. Conf. Soc. p. Most of Permo- Triassic biozones identified from Semanggol Fm) Jasin. Deep marine clastics with cherts with 5 Permian and 4 E-M Triassic radiolarian biozones.Radiolarian biostratigraphy of Peninsular Malaysia. Basir. 103-109. Hassan & M. (online at: https://gsmpubl. Harun (2004). p. Geol. Bull.pdf) (Deep marine radiolarian cherts common in Late Paleozoic.com March 2014 .pdf) (Semanggol Fm outcrops in NW Malay Peninsula.. 49. Harun (2007). Thickness of formation hard to determine due to intense folding-thrusting) Jasin. 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Kajiwara, N. Nakornsri & A. Sardsud (2000)- Late Permian to Middle Triassic radiolarian faunas from Northern Thailand. J. Paleontology 74, 5, p. 789-811. (Late Permian- M Triassic radiolarians from Shan-Thai Block in almost continuous chert- shale sequences exposed N of Chiang Mai, N Thailand. 50 species, 35 genera. Radiolarians identical to faunas of Late Permian Neoalbaillella ornithoformis and N. optima zones and E Triassic Parentactinia nakatsugawaensis and Triassocampe coronata Assemblage Zones in chert sequences of Japan) Sashida, K., H. Igo, S. Adachi, K. Ueno, N. Nakornsri & A. Sardsud (1998)- Late Paleozoic radiolarian faunas from northern and northeastern Thailand. Sci. Repts. Inst. Geoscience, University of Tsukuba, B, 19, p. 1-27. Sashida, K., H. Igo, K. Hisada, N. Nakornsri & A. Ampornmaha (1993)- Occurrence of Paleozoic and Early Mesozoic radiolaria in Thailand (preliminary report). In: B.K. Tan et al. (eds.) 7th Reg. Congr. Geology Mineral and Energy Resources of SE Asia (GEOSEA VII), Bangkok 1991, J. Southeast Asian Earth Sci. 8, p. 97-108. (Devonian. E Carboniferous and Permian radiolaria found in 'Fang Chert' near Chiang Mai, NW Thailand (= Paleotethys ocean floor sediment). Late Devonian- E Carboniferous radiolaria also in tuffaceous shale/ chert in Loei area near Pak Chom (NE Thailand, Indochina Block). Well-preserved late E Triassic radiolarians in limestone near Patthalung, S Peninsular Thailand) Sashida, K., H. Igo, K. Ueno, N. Nakornsri & A. Sardsud (1998)- Late Paleozoic radiolarian faunas from northern and northeastern Thailand. Science Repts. Inst. Geoscience, University of Tsukuba, B 19, p. 1-27. Sashida, K., N. Nakornsri, K. Ueno & A. Sardsud (2000)- Carboniferous and Triassic radiolarian faunas from the Saba Yoi area, southernmost part of Peninsular Thailand and their paleogeographic significance. Science Reports Inst. Geoscience, University of Tsukuba, B, 21, p. 71-99. (see also Sashida et al. 2002) Sashida, K. & S. Salyapongse (2002)- Permian radiolarian faunas from Thailand and their paleogeographic significance. J. Asian Earth Sci. 20, p. 691-701. (Eight Permian radiolarian zones in chert and fine-grained pelagic-hemipelagic rocks in Permian of Thailand, Deposited in deep pelagic environment of Paleotethys Ocean that existed between Late Devonian- M Triassic. N Thailand uppermost Permian- M Triassic deposited in pelagic basin, in E Thailand change in depositional environment from deep pelagic in Permian to shallow seas in Triassic) Sashida, K., S. Salyapongse & P. Charusiri (2002)- Lower Carboniferous radiolarian fauna from the Saba Yoi- Kabang area, southernmost part of Peninsular Thailand. Micropaleontology 48, Suppl. 1, Proc. INTERRAD 9, p. 129-143. Bibliography of Indonesia Geology , Ed. 5.1 334 www.vangorselslist.com March 2014 (U Tournasian radiolaria from black chert in thick-bedded sandstone at Saba Yoi-Kabang, S Peninsular Thailand, near Malausia border. 23 species of Albaillella indensis assemblage, also known from Pyrenees, SW China, peninsular Malaysia and E Australia. Deposited in pelagic- hemipelagic environment in Paleotethys Ocean) Sashida, K., S. Salyapongse & N. Nakornsri (2000)- Latest Permian radiolarian fauna from Klaeng, Eastern Thailand. Micropaleontology 46, 3, p. 245-263. (Latest Permian radiolarian fauna from chert-clastic sequence at Khao Wang Chik, Klaeng, E Thailand (Shan- Tai Block). composed of Neoalbaillella, Albaillella, Entactinia, etc. and represent latest Permian Neoalbaillella optima Assemblage, also known from Japan, Russian Far East, Philippines, S and SW China, and N Thailand. Probably deposited in deep, pelagic environment of Paleotethys Ocean) Saurin, E. (1960)- Foraminiferes Viseens de Bhan Phit. Ann. Fac. Sci. Saigon, p. 345-376. ('Visean foraminifera of Bhan Phit', Vietnam) Schubert, R. (1915)- Die Foraminiferen des jungeren Palaozoikums von Timor. Palaontologie von Timor, Schweizerbart, Stuttgart, 2, 3, p. 47-60. ('The foraminifera of the younger Paleozoic of Timor'. First paper on Timor Permian fusulinids and smaller foraminifera from many localities, collected by Wanner, Molengraaff and Weber expeditions (no maps). (Thought to be Late Carboniferous age, but placed in Early Permian by later workers. Four species described. Parafusulina wanneri is type species of Monodiexodina wanneri; HvG) Schubert, R. (1915)- Uber Foraminiferengesteine der Insel Letti. Jaarboek Mijnwezen Nederl. Oost-Indie 43 (1914), Verhandelingen 1, p. 169-187. ('On the foraminifera-bearing rocks of the island of Leti'. Abundant, rel. large elongate Permian fusulinids in loose limestone blocks, described as Doliolina lepida var. lettensis (Thompson 1948: small fauna of verbeekinids described here from Leti is different from Timor faunas). Also Upper Cretaceous Globotruncana linneana and E Miocene Lepidocyclina and Heterostegina (= Spiroclypeus; HvG)) Segroves, K.L. (1969)- Saccate plant microfossils from the Permian of Western Australia. Grana Palynologica 9, p. 174-227. (online at: http://www.tandfonline.com/doi/pdf/10.1080/00173136909436435) (29 species of saccate spores from Permian of N Perth Basin) Senowbari-Daryan, B. & R. Ingavat-Helmcke (1993)- Upper Permian sponges from Phrae province (northern Thailand). In: Int. Symposium on Biostratigraphy of mainland Southeast Asia: facies and paleontology, Chiang Mai, p. 439-451. (online at: http://library.dmr.go.th/library/Proceedings-Yearbooks/M_1/1993/7494.pdf) (Uppermost Permian in Phrae Province, ESE of Chiang Mai, N Thailand, is shale- sandstone- limestone sequence W of Nan-Uttaradit suture. Limestones in area contain Paleofusulina and Colaniella parva and locally rich sponge faunas) Senowbari-Daryan, B. & R. Ingavat-Helmcke (1994)- Sponge assemblage of some Upper Permian reef limestones from Phrae province (Northern Thailand). Geologija 36, p. 5-59. (Fauna of uppermost Permian reefal limestones of Phrae province, N Thailand dominated by sponges incl. hexactinellida, sclerospongea, 'sphinctozoans', and 'inozoans'. Associated with Tubiphytes and Hemigordius, but no corals and fusulinid foraminifers found. Locality is just W of 'Nan-Uttaradit' suture, which was probably not trace of Paleotethys, but closure of minor oceanic basin) Shen, S.Z. & G.R. Shi (1996)- Diversity and extinction patterns of Permian Brachiopoda of South China. Historical Biology 12, p. 93-110. Shen, S.Z. & G.R. Shi (2000)- Wuchiapingian (early Lopingian, Permian) global brachiopod palaeobiogeography: a quantitative approach. Palaeogeogr., Palaeoclim., Palaeoecology 162, 3-4, p. 299-318. Bibliography of Indonesia Geology , Ed. 5.1 335 www.vangorselslist.com March 2014 (Late Permian brachiopods five marine biotic province: Cathaysian (tropical ), W Tethyan (tropical), Himalayan (warm temperate), Austrazean (cold temperate) and Greenland-Svalbard (cold temperate). Also Cimmerian biogeographical region from Middle East through Afghanistan and Himalayas SE to Shan-Thai terrane and Timor, typified by mix of genera of both Cathaysian and Gondwanan affinities) Shen, S.Z. & G.R. Shi (2002)- Paleobiogeographical extinction patterns of Permian brachiopods in the Asian- western Pacific region. Paleobiology 28, p. 449-463. (End-Permian extinction eliminated ~90% of genera and 95% of species of Brachiopoda. End-Guadalupian extinction less profound ) Shen, S.Z. & G.R. Shi (2004)- Capitanian (Late Guadalupian, Permian) global brachiopod palaeobiogeography and latitudinal diversity pattern. Palaeogeogr., Palaeoclim., Palaeoecology 208, p. 235-262. (Six paleogeographic provinces based on M Permian brachiopods: (A) Greenland-Svalbard (Arctic region), (B) Grandian (W North America), (D) Cathaysian (Paleotethys and Mesotethys), (F) Austrazean (E Australia- New Zealand), and two transitional zones (C) Sino-Mongolian-Japanese (N temperate zone) and (E) Himalayan (S temperate zone) Province. West Timor Aileu-Maubisse assemblages grouped with Lhasa, Chitichun and Zhongba assemblages of S Tibet and Salt Range (Pakistan) in 'Himalayan Province') Shen, S.Z., G.R. Shi & N.W. Archbold (2003)- A Wuchiapingian (Late Permian) brachiopod fauna from an exotic block in the Indus-Tsangpo suture zone, southern Tibet, and its palaeobiogeographical and tectonic implications. Palaeontology 56, 2, p. 225-256. (online at: http://onlinelibrary.wiley.com/doi/10.1111/1475-4983.00296/pdf) (Late Permian (Wuchiapingian) brachiopod fauna from exotic limestone block in Indus-Tsangpo suture zone in S Tibet. Comparable with faunas in Salt Range of Pakistan, Chitichun Lst in S Tibet and Basleo area of W Timor (incl. 'antitropical' peri-Gondwanan species Stenoscisma purdoni and S timorense, etc.). Fauna mixed peri-Gondwanan and Cathaysian character, possibly seamount biota originally from S margin of Neotethys in Late Permian, displaced and sandwiched into younger marine deposits in Cenozoic India- Eurasia collision) Shen, S.Z., G.R. Shi & Z.J. Fang (2002)- Permian brachiopods from the Baoshan and Simao Blocks in Western Yunnan, China. J. Asian Earth Sci. 20, 6, p. 665-682. (Four Permian brachiopod assemblages from W Yunnan, SW China. Faunas from Baoshan Block dominated by species characteristic of Cathaysian Province with some links with Peri-Gondwanan faunas. Simao Block characterised exclusively by taxa of Cathaysian Province) Shen, S.Z., H. Zhang, W.Z. Li, L. Mu & J.F. Xie (2006)- Brachiopod diversity patterns from Carboniferous to Triassic in South China. Geol. J. 41, p. 345-361. (Carboniferous to Triassic includes (1) 100 My-long stable biodiversity stage from Late Carboniferous- late Middle Permian,with highly diverse brachiopod faunas;(2) end-Permian most severe mass extinction in Phanerozoic; (3) bleak stage in E Triassic and (4) rapid recovery stage in M Triassic) Shi, G.R. & N.W. Archbold (1995)- Permian brachiopod faunal sequences of the Shan-Thai terrane: biostratigraphy, palaeobiogeographical affinities and plate tectonic/palaeoclimatic implications. J. Southeast Asian Earth Sci. 11, p. 177-187. Shi, G.R. & N.W. Archbold (1995)- A quantitative analysis on the distribution of Baigendzhinian- Early Kungurian (Early Permian) brachiopod faunas in the western Pacific region. J. Southeast Asian Earth Sci. 11, 3, p. 189-205. (Cluster analysis of distribution of 222 species of Early Permian brachiopods from 25 localities across E Asia- Australia suggest 6 bioprovinces. In SE Asia two provinces, both sub-provinces of Cimmerian terranes: (1) Group B, Shan-Tai/ Sumatra/ W Papua Birds Head (warm temperate to S-subtropical; with Stereochia- Stictozoster) and (2) Group C, Himalayan/ Lhasa/ Timor (S-temperate; with Reedoconcha, Callytharella; also fusulinid Monodiexodina). Notable conclusions: Timor (Maubisse) was southern extension of Lhasa terrane, W Thailand most similar to Birds Head, Sumatra Jambi and Padang faunas similar and grouped with Shan Tai) Bibliography of Indonesia Geology , Ed. 5.1 336 www.vangorselslist.com March 2014 Shi, G.R., N.W. Archbold & L.P. Zhan (1995)- Distribution and characteristics of mixed (transitional) mid- Permian (Late Artinskian-Ufimian) marine faunas in Asia and their palaeogeographical implications. Palaeogeogr., Palaeoclimat., Palaeoecol. 114, p. 241-271. (Asia Permian marine biogeography 3 realms: Boreal, Tethyan and Gondwanan. In early E Permian sharp biogeographical boundaries, due to Gondwanan glaciation. In M Permian two transition zones with mixed faunas: (1) North (N China, Japan, etc.), with warm Cathaysian and temperate Boreal genera, (2) South (Arabia, Iran, Shan-Tai, Timor, W Irian Jaya, etc.) with both Gondwanan and Cathaysian elements. Both transition zones have antitropically distributed genera like Monodiexodina, Lytvolasma and Spiriferella and are succeeded by Late Permian tropical Tethyan faunas) Shi, G.R., Z.J. Fang, N.W. Archbold (1996)- An Early Permian brachiopod fauna of Gondwana affinity from the Baoshan block, westernYunnan, China. Alcheringa 20, 81-101. (E Permian brachiopod fauna from U Dingjiazhai Fm, 30 km S of Baoshan, W Yunnan, dominated by Stenoscisma sp. and Elivina yunnanensis sp. nov. Strong links with faunas from Bisnain assemblage of Timor and Callytharra Fm of W Australia. Late Sakmarian age suggested) Shi, G.R. & T.A. Grunt (2000)- Permian Gondwana-Boreal antitropicality with special reference to brachiopod faunas. Palaeogeogr., Palaeoclim., Palaeoecology 155, p. 239-263. (Permian marine antitropicality (genera from Boreal and Gondwanan Realms but absent in Paleoequatorial Realm) reported from most marine pelagic or benthic invertebrate groups, suggesting biotic interchanges between Gondwanan and Boreal Realms. Possible migration pathways and mechanisms reviewed: ‘stepping- stone' migration via islands in E Paleotethys, migration along W coast of Paleotethys, etc.) Shi, G.R., M.S. Leman, K. Tan et al. (1997)- Early Permian brachiopods of Gondwanan affinity from the upper Singa Formation, Lankawi Island, NW Peninsular Malaysia: biostratigraphical and biogeographical implications.. In: P. Dheeradilok et al. (eds.) Proc. Int. Conf. Stratigraphy and tectonic evolution of Southeast Asia and the South Pacific, Dept. Mineral Res., Bangkok, p. 62-72. Shi, G.R., L. Raksaskulwong & H.J. Campbell (2002)- Early Permian brachiopods from northern and central peninsular Thailand. In: L.V. Hills et al. (eds.) Carboniferous and Permian of the World, Canadian Soc. Petrol. Geol., Mem. 19, p. 596-608. Shi, G.R. & S.Z. Shen (2001)- A biogeographically mixed, middle Permian brachiopod fauna from the Baoshan Block, Western Yunnan, China. Palaeontology 44, p. 237-258. (Baoshan Block (= part of Sibumasu complex; HvG) M Permian brachiopod assemblage with Cryptospirifer in from lower Shazipo Fm. Associated with fusulinids Nankinella, Polydiexodina spp. and Schwagerina. Overlying U Shazipo Fm 500-700m carbonate contains Shanita- Hemigordiopsis foram assemblage. Paleogeographical distribution of Cryptospirifer overlaps with that of slightly younger (Capitanian-Wuchiapingian) Shanita- Hemigordius (Hemigordiopsis) foram fauna, also endemic or largely confined to M Permian transitional faunas of Cimmerian region (Baoshan Block)) Shi, G.R., S. Shen, S., H.J. Campbell & L. Raksaskulwong (2001)- A Meekella-dominated Early Permian brachiopod assemblage from central Peninsular Thailand. In: Contributions to Geology and Paleontology of Gondwana in honour of Helmut Wopfner, Cologne, p. 441-451. Shi, G.R. & J.B. Waterhouse (1991)- Early Permian brachiopods from Perak, West Malaysia. J. Southeast Asian Earth Sci. 6, p. 25-39. (New Permian brachiopod fauna of probable Sakmarian (E Permian) age from Nam Loong 1 Mine of Kinta Valley, W of Kampar, Perak, on Sibumasu Terrane. Material collected by Gobbett below fossiliferous H.S. Lee Beds (Pseudofosulina kraffti and Misellina claudiae fusulinid zones; Ishii 1966). Nam Loong beds ~150m thick, with crinoid limestone of at base, overlain by brachiopod limestone) Bibliography of Indonesia Geology , Ed. 5.1 337 www.vangorselslist.com March 2014 Shi, Y. (2010)- Early Permian fusulinids from West Yunnan and their chronological puzzle. In: C.P. Lee et al. (eds.) 6th Symp. Int. Geol. Correl. Progr. Project 516 (IGCP516), Geological anatomy of East and South Asia, Kuala Lumpur 2010, p. 42-43. (Abstract only) (E Permian (Artinskian) fusulinids described recently from W Yunnan Sibumasu/ Cimmerian terranes: Eoparafusulina-Pseudofusulina faunas from Baoshan Block, Eoparafusulina-Monodiexodina fauna from Tengchong Block) Shi, Y., H. Huang, X. Jin & X. Yang (2011)- Early Permian fusulinids from the Baoshan Block, Western Yunnan, China and their paleobiogeographic significance. J. Paleontology 85, 3, p. 489-501. (Sakmarian-Artinskian fusulinids from N and S Baoshan and W Yunnan, dominated by Pseudofusulina and Eoparafusulina spp. and similar to those from C Pamir, S Afghanistan, E-C Iran, C Oman, E Hindu Kush and N Karakorum) Shi, Y., X. Jin, H. Huang & X. Yang (2008)- Permian fusulinids from the Tengchong Block, Western Yunnan, China. J. Paleontology 82, p. 118-127. (Permian fusulinid faunas from N Tengchong Block, SW China. Lower Dadongchang Fm dominated by Eoparafusulina, possibly Sakmarian age. Dadongchang Fm mainly Chusenella and Monodiexodina, indicating Wordian-Capitanian age. Similar to fusulinid assemblages from Baoshan and Sibumasu Blocks (both low diversity without Cathaysian- Tethyan Pseudoschwagerinidae, Verbeekinidae, Neoschwagerinidae)) Shimizu, D. (1966)- Permian brachiopod fossils of Timor (Palaeontological study of Portuguese Timor 3). Mem. Coll. Science, Kyoto University, Ser. B, Geol. Min., 32, 4, p. 401-427. (17 brachiopods from E Timor localities suggest Early Permian age. At some localities in part of autochthonous complex of reddish or purplish brown tuffaceous shale; in others associated with purplish tuffaceous, occasionally argillaceous limestones and shales) Smith, J.P. (1927)- Permian ammonoids of Timor. In: H.A. Brouwer (ed.) 2e Nederlandsche Timor-Expeditie 1916, IV, Jaarboek Mijnwezen Nederl.-Indie 55 (1926), Verhandelingen 1, p. 1-58. (Ammonoid material from 1916 Jonker expedition to Timor. Richest Permian ammonoid fauna in world, in both species and abundance. Especially rich in Cyclolobidae and Medlicottiidae and rel. poor in Ceratitoidea. Successive Permian age faunas: (1) E Permian Somohole (common Marathonites, Gastrioceras, Paralegoceras, Pronorites), Bitauni (Perrinites, Agathiceras sundaicum, Paralegoceras spp.) and Basleo (with Waagenoceras, increase in Haloritidae); (2) Late Permian? Amarassi/ Ajer Mati fauna (still with Cyclolobus). Latest Permian faunas not seen in Timor) Smith, S. (1941)- Some Permian corals from the Plateau Limestone of the Southern Shan States, Burma. Palaeontologia Indica. N.S., 30, 2, p. 1-21. (Permian corals from Plateau Limestone of E Myanmar (= Sibumasu Block?). With rel. common solitary rugose ncl. Lophophyllidium orientale, Pavastehphyllum), also Protomichelinia, Wentzelella cf timorica Gerth(= Paraipciphyllum?; Fontaine1988). (= part of Cyathaxonia faunas from Sibumasu Terrane of Wang et al. 2013) Sone, M. (2010)- A new species of the rare neritopsid gastropod Magnicapitatus from theGuadalupian (Middle Permian) of East Thailand (the Indochina Terrane). Alcheringa 34, 1, p. 1-6. (Neritopsid gastropod genus Magnicapitatus from a fusulinoid-rich limestone of Khao Taa Ngog Fm (Capitanian, M Permian) at Khao Makha in E Thailand near Cambodia border, in Indochina Terrane) Sone, M., C. Chonglakmani & A. Chitnarin (2009)- Middle Permian productidine brachiopods from Central Thailand (the Indochina Terrane) with paleobiogeographic implications. J. Paleontology 83, 5, p. 804-810. (Assemblage of productid brachiopods Haydenella, Paraplicatifera and Compressoproductus from Wordian of U Saraburi Limestone Gp of C Thailand (W margin Indochina Terrane) suggests endemism for M Permian marine faunule of Indochina Terrane) Sone, M. & M.S. Leman (2000)- Some mid-Permian fossils from Felda Mayam, Central Peninsular Malaysia. Proc. Geol. Soc. Malaysia Ann. Conf, p. 143-150. Bibliography of Indonesia Geology , Ed. 5.1 338 www.vangorselslist.com March 2014 Sone, M. & M.S. Leman & M. Ehiro (2001)- Middle Permian cephalopods from central Peninsular Malaysia: implications for faunal migration through the southern Tethys. J. Asian Earth Sci. 19, 6, p. 805-814. (Wordian (early M Permian) cephalopod fauna in steeply dipping shales- tuffaceous sandstones at Bera South, S Pahang, dominated by Agathiceras. Also ammonoids Tauroceras, Bamyaniceras and Pronoritidae and nautiloids Tainoceras and Orthocerida. Presence of Tauroceras. aff. scrobiculatum suggests correlation with S Tethys strata of NE Iraq, N Oman and Sicily) Sone, M., M.S. Leman & I. Metcalfe (2004)- Triassic nautiloid Sibyllonautilus from Gua Bama, Peninsular Malaysia and its regional stratigraphic implications. Alcheringa 28, p. 477-483. (Coiled nautiloid suggesting Late Permian- earliest Triassic (Lopingian- Anisian) age for Gua Bama sponge- algal reefal limestone, just E of Bentong-Raub suture, NW Pahang, Peninsular Malaysia. Overlies Permian tuffaceous Leptodus brachiopod shales) Sone, M., M.S. Leman & G.R. Shi (2001)- Middle Permian brachiopods from central Peninsular Malaysia- faunal affinities between Malaysia and west Cambodia. J. Asian Earth Sci. 19, p. 177-194. (Moderately diverse Permian brachiopod fauna from Bera District, C Pahang, Central Belt of Peninsular Malaysia (on E Malaya- Indochina Plate). 19 species, typically warm-water Tethyan. Strong linkage to Yabeina beds of Sisophon Lst, W Cambodia. Possible E Capitanian (M Permian) age) Sone, M., I. Metcalfe & M.S. Leman (2003)- Palaeobiogeographic implications of Middle Permian brachiopods from Johore (Peninsular Malaysia). Geol. Magazine 140, p. 523-538. (New M Permian brachiopods fauna from folded tuffaceous sandstone at Sermin, N Johore, with Pseudoleptodus, Neochonetes, etc., associated with ammonoid Agathiceras sp.. Fauna lacks diagnostic Cathaysian taxa, but has minor Sibumasu elements. Locality just E of Bentong-Raub suture on East Malaya terrane of Cathaysian province, suggesting species interchange between shallow waters of E Malaya and Sibumasu across Paleo-Tethys. Sibumasu, Timor (Bitauni) and W Irian Jaya dominantly Gondwanan affinity and cooler, higher latitude than E Malaya) Sorauf, J.E. (1978)- Original structure and composition of Permian rugose and Triassic scleractinian corals. Palaeontology 21, 2, p. 321-339. (Study of Permian solitary coral structure based on exceptionally well-preserved material in Wanner collection from Guadalupian of Basleo 23 locality, SW Timor (Polycoelia angusta, Timorophyllum wanneri, Lophophyllidium spinosum)) Sorauf, J.E. (1983)- Primary biogenic structures and diagenetic history of Timorophyllum wanneri, Rugosa, Permian, Timor, Indonesia. Assoc. Australasian Pal. Mem. 1, p. 275-288. Sorauf, J.E. (1984)- Upper Permian corals from Timor and diagenesis. Palaeontogr. Americana 54, p. 294-302. (Description of phraetic cements in well-preserved Permian rugosan fauna from Basleo, supposedly from blocks in ‘Tertiary deep water wildflysch’ (= ‘Bobanaro melange’)). Sorauf, J.E. (2004)- Permian corals of Timor (Rugosa and Tabulate): history of collection and study. Alcheringa 28, 1, p. 157-183. (History of collection and study of corals in Permian of Timor began in 1911 with Wanner, Molengraaff and Weber. Biostratigraphy of faunas uncertain, partly because of collection from tectonic melange sequence in Baun to Basleo region, and purchase of fossils from indigenous people. Permian corals from Timor need restudy from stratigraphic sequences in northern 'Fatu' belt of outcrops) Spiller, F.C.P. (1996)- Late Paleozoic radiolarians from the Bentong-Raub suture zone, Peninsular Malaysia. The Island Arc 5, 2, p. 91-103. (Radiolarians from deep marine siliceous sediments from melange from Bentong-Raub suture zone contain 7 radiolarian zones from 10 localities: Late Devonian (Famennian), E Carboniferous (Tournaisian and Visean) Bibliography of Indonesia Geology , Ed. 5.1 339 www.vangorselslist.com March 2014 and E Permian. Suggests ocean existed between Sibumasu and East Malaya terranes from at least Late Devonian- late E Permian time) Spiller, F.C.P. (2002)- Radiolarian biostratigraphy of Peninsular Malaysia and implications for regional palaeotectonics and palaeogeography. Palaeontographica Abt. A, 266, p. 1-91. Spiller, F.C.P. & I. Metcalfe (1995)- Late Paleozoic radiolarians from the Bentong-Raub suture and the Semanggol Formation of Peninsular Malaysia- initial results. J. Southeast Asian Earth Sci. 11, 3, p. 217-224. (Cherts and tuffaceous siltstones from Bentong-Raub suture zone, Peninsular Malaysia, with Late Devonian and E Carboniferous radiolarians. Cherts deposited in Paleo-Tethys ocean between Sibumasu and East Malaya. Radiolarians from siliceous Semanggol Fm of NW Peninsular Malaysia Early and Late Permian ages, extending age of Semanggol Fm down to E Permian and confirms presence of deep-marine basin in NW Peninsular Malaysia during Permian) Spiller, F.C.P. & I. Metcalfe (1995)- Paleozoic and Mesozoic radiolarian biostratigraphy of Peninsular Malaysia. Proc. IGCP Symposium on Geology of SE Asia, J. Geology, Hanoi, ser. B., 5-6, p. 75-93. Sprinkle, J. & J.A. Waters (2013)- New ridged, conical, fissiculate blastoid from the Permian of Timor. J. Paleontology 87, 6, p. 1071-1076. (Recent collections in Permian of N slope of Sonmahole (Somohole) Mountain, 3.5 km NE of Manufui, NE part of W Timor, produced first new genus of blastoid described from Timor in 70 years Corrugatoblastus savilli, n. gen. n. sp, is ridged and furrowed, conical, fissiculate blastoid with unusual thecal morphology mimicking a small, solitary, rugose coral. Placed in Family Codasteridae) Srivastava, A.K. & D. Agnihotri (2010)- Dilemma of Late Palaeozoic mixed floras in Gondwana. Palaeogeogr., Palaeoclim., Palaeoecology 298, p. 54-69. (Carboniferous and Permian plant assemblages of N and S hemispheres distributed in four floral provinces. Mixed M and U Permian Cathaysian- Gondwanan floras from margins of Paleo-Tethys, i.e. New Guinea, Tibet, Oman, etc. No clear explanation) Stehli, F.G. (1961)- New genera of Upper Paleozoic Terebratuloids. J. Paleontology 35, 3, p. 457-466. (New genus and species name Timorina broili for small terebratulid brachiopod, originally described as Notothyris minuta by Broili (1916)- from M Permian of Basleo, Timor) Stephenson, M.H. (2008)- A review of the palynostratigraphy of Gondwanan Late Carboniferous to Early Permian glacigene successions. In: C.R. Fielding et al. (eds.) Resolving the Late Paleozoic Ice Age in time and space, Geol. Soc. America Spec. Paper 441, p. 317-330. (E Permian W Australian, Arabian and S African sequences can be correlated using taxa like Converrucosisporites confluens and Pseudoreticulatispora pseudoreticulata. C. confluens and P. pseudoreticulata zones considered to be Sakmarian, and Striatopodocarpites fusus zone is Artinskian. Difficult to correlate Gondwana palynological assemblages precisely to Russian type areas because of scarcity of marine fauna in Gondwana and different paleolatitudes, so Carboniferous-Permian boundary cannot be precisely correlated in Gondwana by palynology) Stokes, R.B., P. Lovatt Smith, A. Racey, C.H.C. Brunton, O. Dawson, A.R.H. Swan & M.F. Whitaker (2012)- Some Upper Palaeozoic fossil localities in the Vientiane Contract Area, Lao PDR, and their geological Importance. J. Sci. Technol. MSU, p. 63-73. (online at: http://journal.msu.ac.th/2012_/index.php/SCI/article/view/286/294) (New Upper Paleozoic (Carboniferous- Permian) localities from C and W Laos. Includes latest Permian limestone with Palaeofusulina- Colaniella fauna N of Vientiane) Strimple, H.L. & T.E. Yancey (1976)- Moscovicrinus preserved in magnetite from Selumar, Belitung Island, Indonesia. J. Paleontology 50, 6, p. 1195-1202. Bibliography of Indonesia Geology , Ed. 5.1 340 www.vangorselslist.com March 2014 (Rare, probably Early Permian age crinoid from folded, E-W trending sandstones-shales in Selumar open pit mine on E side of Billiton Island, near margin of magnetite-cassiterite vein. Moscovicrinus hoskingi n.sp.. Also mention Van Overeem (1960) record of fusulinid limestone in wells just off N coast of Beliting. See also Hosking et al. 1977) Sugiyama, T. (1982)- Middle Permian corals from the Ratburi Limestone in the Khao Khao area, Sara Buri, Central Thailand. In: T. Kobayshi, R. Toriyama & W. Hashimoto (eds.) Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 24, p. 15-29. (M Permian corals from 360m thick Ratburi Lst in Khao Khao section (with Afganella spp.- Neoschwagerina haydeni zones fusulinids described by Toriyama and Kanmera 1979). Five coral localities with waagenophyllids Ipciphyllum saraburiense n.sp., Paraipciphyllum, Pseudohuangia Chihsiaphyllum kanmerai n.sp. and tabulate Tetraporinus) Sugiyama, T. & R. Toriyama (1981)- Coral and fusuline faunas from the Kabin Buri Area, East Central Thailand. In: T. Kobayshi & R. Toriyama (eds.) Geology and Palaeontology of Southeast Asia, University of Tokyo Press, 22, p. 1-22. Sun, K. (1999)- Origin, evolution and extinction of Cathaysia flora. Chinese Science Bull. 44, 2, p. 100-108. (Carboniferous- Permian Cathaysia flora mainly distributed in China, Korea, Japan, Laos, Thailand, Sumatra and Malaysia. Mixed Cathaysian and Gondwanan flora known in S Tibet, Kashmir, Turkey and New Guinea. Cathaysian flora developed from global uniform E Carboniferous Lepidodendropsis flora) Swart, R.H. (1998)- Revision of Permian pleurotomarian gastropods from the Carnarvon and Bonaparte basins. In: G.R. Shi, N.W. Archbold & M. Grover (eds.) Strzelecki international symposium on Permian of eastern Tethys; biostratigraphy, palaeogeography and resources. Proc. Royal Soc. Victoria 110, 1-2, p. 163-172. Tan Sin Hok (1933)- Notiz uber das Basalskelett von "Verbeekina". Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Indie 25, p. 57-65. (Permian fusulinids from Padang Highlands, thought by Verbeek 1876, to lack 'parachomata', distinguishing it from Doliolina, so new genus Verbeekina was created. New material from Guguk Bulat type locality near Lake Singkarak shows this feature in later stages, so species belong in Doliolina) Tan Sin Hok (1933)- Uber Leptodus (Lyttonia auctorum) cf. tenuis (Waagen) vom Padanger Oberland (Mittel Sumatra). Wetenschappelijke Mededeelingen Dienst Mijnbouw Nederl. Indie 25, p. 66-70. (Permian brachiopod Leptodus collected by Musper from Padang Highlands, C Sumatra, confirms presence of rocks of younger Permian in Sumatra. Other Leptodus in Indonesia only known from Timor) Teichert, C. (1951)- The marine Permian faunas of Western Australia (an interim review). Palaeont. Zeitschrift 24, p. 76-90. (Marine Permian faunas (~350 species) compared with Tethyan, E Australian and Gondwana faunas. W Australian faunal province affinities with E Tethys (Salt Range, Timor) but dissimilar to E Australian province, although some W Australian elements migrated into N (Queensland) and S (Tasmania) parts of E province) Tesch, P. (1916)- Permische trilobieten van Atjeh. Tijdschr. Kon. Ned. Aardrijksk. Gen. Ser. 2, 33, p. 610-611. ('Permian trilobites from Aceh'. Two species of trilobite casts in dark red, tuffaceous marly rock, associated with corals, crinoids, brachiopods and gastropods, previously reported by Klein 1916 as presumably Devonian. Species very similar those described form Permian in Timor) Tesch, P. (1923)- Trilobiten aus der Dyas von Timor und Letti. Palaeontologie von Timor 12, 21, p. 123-132. (Trilobites from the Permian of Timor and Leti’. Phillipsia sp. and Neoproetus indicus n.sp., collected by Wanner, Molengraaff, Jonker et al. Trilobites relatively rare and poorly preserved in Timor Permian) Tharalson, D.B. (1984)- Revision of the Early Permian ammonoid family Perrinitidae. J. Paleontology. 58, 3, p. 804-833. Bibliography of Indonesia Geology , Ed. 5.1 341 www.vangorselslist.com March 2014 Fusulinids of Timor not similar to widespread complex fusulinid faunas in other parts of E Hemisphere) Tien.L. studied by Jongmans & Gothan.Foraminifera and algae from the Permian of Kampuchea. Nguyen D.gen. Silungkang locality with common Tubiphytes) Tien. Hemigordius) and algae (incl. Sumatra) Thompson. (Well-illustrated summary of foraminifera from Permian limestones from W and S Cambodia. J. known from Cambodia.The fusulinid genus Verbeekina. Nguyen D. See also Ueno et al (2006) and Ueno in Crippa et al 2014)) Thompson. p. 109-111. Species described by De Roever from Timor as Perrinites waageni was renamed Properrinites deroeveri by Gerth (1950) is here called Properrinites cumminsi.Suteethorn (eds.. 138-147. Verbeekina). etc. HvG)) Bibliography of Indonesia Geology . 182-192. incl. meranginensis looks like fusulinids of the Schwagerina princeps group. Nguyen D. p. 1-166. P. Malay Peninsula (= also 'Sibumasu fossil' subsequently reported from Oman.) The Permian of Southeast Asia.Etude micropaleontologique (foraminiferes) de materiaux du Permien du Cambodge. S Vietnam) Tien. United Nations CCOP Techn. W. Paleontology 10. square in section. Fauna from this locality first described by Lange (1925). 18. Thailand. Pseudodoliolina. M. Jambi). Sumatrina. (1988). United Nations CCOP Techn. a small tube.sp. In: H. high diversity 'Tethyan' M Permian fusulinid assemblage with Neoschwagerina from Nui Com. (Two organisms of uncertain affinity relatively common in Permian of W Thailand: (1) Rectostipulina quatrata.Note on two "Incertae sedis" from the Permian of West Thailand. (U Sakmarian). Nguyen D. Leonardian or older age. Description of Verbeekina verbeeki (Geinitz) from Padang Highlands. Iran.) The Permian of Southeast Asia. Ed. Nguyen D.L. In: H.Quelques fusulinides de Nui Com. Appendix 3.vangorselslist. (1970). Fontaine (ed.The Permian fusulinids of Timor.. Thesis 3me Cycle. Sumatra. C Sumatra (Merangin.1 342 www. (1936). Schwagerina brouweri n. In: 11th Congress Carboniferous Stratigraphy Geol. Orsay. Bull. sp.com March 2014 . Also description of Artinskian Paraperrinites subcumminsi (Haniel) (originally Cyclolobus subcumminsi) from Bitauni) Thompson. Nguyen D. J. (1987). 18. (1979). a small bubble that may be foraminifer or fossil of algal affinity. p. Schwagerina.. etc. also known from Turkey.Foraminifera and algae from the Permian of Guguk Bulat and Silungkang. Fontaine & V. (Unpublished) ('Micropaleontological study (foraminifera) of material from the Permian of Cambodia') Tien. Mizzia. (Illustrations of foraminifera from two Permian limestone localities from Padang Highlands. Bangkok. etc. 5. Guguk Bulat reefal limestone with corals and diverse fusulinids (Colania. Sud Viet-Nam (Zone a). p. In: H. Cyprus. J.(Includes descriptions of Timor Permian perrinitid ammonoids. Bull. 193-201. Bull. 20. 1. Paleontology 23. n. All appear to indicate Early Permian. 2. (1986). Interpreted age Lower Permian. p. Tien. Fontaine (ed. using thin sections originally used by Gubler (1935)for study on fusulinids of Indochina) Tien. 1-70.Overlain by Soengi Garing plant beds with famous 'Jambi Flora'. Universite Paris Sud. 116-137. (Rel. (1936). C Sumatra. p.Description of a new microfossil from the Permian of Southeast Asia: Sphaerionia. (Genus Verbeekina includes 5 species and two varieties. 587-592. (2) Sphairionia sikoides n. (1986). 3.?. Permocalculus). Beijing 1978.Lower Permian fusulinids from Sumatra. Afghanistan. Paleontology 10. Archives Geol. CCOP Techn. M. small benthic foram assemblages (incl. (Fusulinid limestones collected by Brouwer expedition in 1937 in W Timor contain five species of fusulinids.L. Viet-Nam 13. Appendix 2. p. (1949).) Late Paleozoic and Mesozoic fossils of West Thailand and their environments. p. M.. p. (Two new species of Early Permian fusulinids Schwagerina rutschi and Pseudoschwagerina meranginensis from dark grey. ~100’ thick "Productus limestone" of Telok Gedang. 7. p. Also already described in 1988 'Note on two 'Incertae Sedis' from the Permian of West Thailand'. Bangkok. Fac. (eds. 19. (online at: http://retro.Middle Permian foraminifera. p. (1989). Kobayashi & W. 5. etc. Geogr. Pseudoschwagerina cf. et sp.Kungurian age. (Review of M Permian foraminifera from four areas on Sumatra. p. Gafoer (eds. Beijing 1987. No locality maps) Toriyama. Central Thailand. R. p. Pronina 1996)) Tobler. 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The Pre-Tertiary fossils of Sumatra and their environments. (Description of 'small bubble'. (1976).) Geology and palaeontology of Southeast Asia. simplex Cancellina. At Guguk Bulat fusulinids Verbeekina verbeeki. Mem.Permian fusulinid forams in Thailand and Malaysia) Bibliography of Indonesia Geology . 2006 who restudied Batu Impi locality and prefers Artinskian. A. D-XVII-1.. Fusulinella cf. Permian fusulines from the Rat Buri Limestone in the Khao Phlong Phrab area. D. rich Lower Permian foram assemblages of fusulinids. Fontaine & S. p. 23. p. Sci. etc. a Permian incertae sedis organism: Sphairionia.Sphairionia sikuoides gen. Mem.Fusuline fossils from Thailand.. Overall assemblage 'of Tethyan aspect' (but is on Sibumasu Plate. p. Fusulines of the Rat Buri Limestone of Thailand.) Permian-Triassic evolution of Tethys and Western Circum-Pacific. Kyushu Univ. In: T. (Paper mainly on stratigraphic distribution of foram genera. 73-78. 2. Toriyama. chei.1 343 www.. R. R. either lagenid foraminifer or charophyte algae from M Permian of W Thailand and Cambodia. p. In: H. 3. J.) Geology and Palaeontology of Southeast Asia 25. Yin.Evolution of Permian and Triassic foraminifera in South China. 137-146.On some fusulinids from Northern Tai.M.R. Fac. Fac. (Systematic descriptions and vertical distribution of 91 species/26 genera of fusulinid forams from 225m thick late Early. suggesting Late Asselian age (near locality of famous 'Jambi flora. Mesumai River localities with fusulinids Boultonia willsi. 243-247. neoschwagerinids. Geol. Sara Buri. Sci. 17. Fontaine & S. 313-342. meranginensis. Part I. R.com March 2014 .) Tien. incl. Gafoer (eds. Kyushu Univ. (eds.Summary of the fusuline faunas in Thailand and Malaysia. Nguyen D. R. Part IX. Schwagerina sp. smaller benthic forams (incl. Sara Buri. Schubertella kingi. Kobayashi et al. (1944).Tien. University of Tokyo Press. Nguyen D. Permocalculus) from W Jambi province. HvG). 1-116. rich basal Murghabian fusulinid assemblage with Neoschwagerina cf. (1975). Colania douvillei. Part IX. Dickins et al. University of Tokyo Press.ch/cntmng?type=pdf&rid=egh-001:1923-1924:18::756&subp=hires) (‘Our paleontological knowledge of Sumatra’. and algae Mizzia velebitana. above) Toriyama. Rugosofusulina rutschi and Parafusulina n. rare Monodiexodina. Pseudofusilina padangensis. Sci. utahensis. Papers 19. HvG)) Tien. (also reported from Thailand and other areas of Tethys. p.. Sumatrina annae. In: T. Permian fusulines from the Rat Buri Limestone in the Khao Phlong Phrab area. no fossil illustrations) Toriyama. CCOP Tech. Eclogae Geologicae Helvetiae 18. Papers 19..Neogene macrofossils across Sumatra) Tong. Hashimoto (eds. CCOP Techn. B. 71-93. Neofusulinella.Unsere palaeontologische Kenntniss von Sumatra. (Four M Permian fusulinid zones with Afganella. Kanmera & R. Toriyama (eds. C and E. 5. lantenoisi from lower part of 'Ratburi Lst' in Khao Phlong Khrab section. Kobayashi & R. In Permian stronger affinity to E Tethys. 17-22. 14. 43-61. Genus ranges from Misellina zone to Neoschwagerina simplex zone and is good indicator of upper Lower. Thailand. Central Thailand. Hongnushonthi (1974). p. p. Sci. 25-48. Kanmera. N.lower Middle Permian) Toriyama. praecursor and N. Hashimoto (eds.th/library/Proceedings-Yearbooks/M_3/2521-2530/9492. (online at: http://library. 9. Sumatrina annae.) Geology and palaeontology of Southeast Asia.Permian Fusulinids from Central Thailand. Madrid 1983. 15-32. Kobayshi & R. Kobayshi & R. W and E zones similar paleobiogeographic characteristics. R. p. (Two new fusulinid genera Thailandina and Neothailandina described from rich fusulinid assemblages in 275m thick Rat Buri Limestone section at Phao Phlong Phrab. Changwat Lop Buri. (lower M Permian fusulinids from Ratburi Lst near Kirinakratanaram Temple. Verbeekina verbeeki. C Thailand. Fusuline faunas of Thailand and Malaysia close relationship to W Tethys in M-U Carboniferous.com March 2014 . (E-M Permian fusulinids Neofusulinella sarburiensis n. 128-132. Geology Mineral Resources of SE Asia (GEOSEA III). Kaewbaidhoam & A. 7. Pitakpaivan (1973). with Neofusulinella lantenoisi. Fac. Permian fusulines from the Rat Buri Limestone in the Khao Khao area. S. Toriyama (eds. & K.th/library/DMR_Technical_Reports/1974/10.dmr.go. (online at: http://library. C Thailand) Toriyama.Fusulinacean fossils from Thailand.Biostratigraphic zonation of the Rat Buri Limestone in the Khao Phlong Phrab area. University of Tokyo Press. appears to extend into Malay Peninsula and N Kalimantan. Neofusulinella from Thailand. p. p. 29-44. Subdivided in 3 zones. Sara Buri. R. & G. University of Tokyo Press.l. R. ~250m thick and very rich in fusulinids (81 species. High affinity of fauna with SE Pamir. Stratigraphie et de Geologie du Carbonifere. R.. In: T.1 344 www. Pitakpavan & R. C. 295-306. NE Thailand.) of Thailand with 238 species of fusulinids. Neoschwagerina in Ratburi Lst in Khao Khao section. Sugi (1959). NE Thailand (names deemed invalid by Kobayashi et al.) Geology and Palaeontology of Southeast Asia 4. p. Conf. Ingavat (1969).dmr. In: T. Ingavat (1978).Neoschwagerina- Presumatrina zones).pdf) (Permian 'Ratburi Lst' (s. p.) Geology and palaeontology of Southeast Asia. University of Tokyo Press. Bibliography of Indonesia Geology . Kobayashi & R..vangorselslist.Fusuline fossils from Thailand.Fusulinacean fossils from Thailand. 3rd Reg.lower M Permian)) Toriyama. U Permian fusulinds (Paleofusulina. In: T. Kobayashi & R. R. Tripathi. Mem. Kanmera (1979).Maklaya. In: T. Part II: Two new Permian genera from Thailand. Toriyama (eds.) Geology and palaeontology of Southeast Asia. Kyushu University. & T. 26 genera). No maps) Toriyama. S China and Japan) Toriyama. 2010). Singh (1985). 20. In: T. Toriyama & W. Part V. Subdivided into 7 zones (Misellina. Central Thailand. K. Bangkok 1978. C. Part VII: Middle Permian fusulines from Wat Kirinakratanaram.) Toriyama... K. & K. Colaniella) only found in W zone. W.Carboniferous flora of India and its contemporaneity in the world.pdf) (late Early-Middle Permian 'Ratburi Lst' at Khao Phlong Phrab Hill section. Comptes Rendus Dixieme Congres Int. Section ranges from Misellina zone to lower part of Neoschwagerina zone (upper Lower. Central Thailand.Toriyama. Pseudodoliolina pseudolepida. p. Changwat Sara Buri. R. & K. Nutalaya (ed. Parafusulina gigantea. In: P. Series D. Part XII. Western zone with 41 species/ 28 genera. 12.Fusulinacean fossils from Thailand. etc. Sara Buri. R. Kanmera (1968).go. Ed. 23-93.sp.) Proc. University of Tokyo Press.) Geology and palaeontology of Southeast Asia. Toriyama (eds.The paleogeographic characteristics of fusuline faunas of the Rat Buri Group in Thailand and its equivalent in Malysia.. K. University of Tokyo Press. P. Lobatanularia.vangorselslist. and Neoalbaillella ornithoformis (late Late Permian)) Udchachon. 1. 1-24.270. F. tropical bivalves in M Permian Khao Khwang platform Permian limestones. Soc. p. Nine main microfacies types. Palaeogeogr. Glossopteris flora and Eurydesma fauna: (1) (S) Lesser Himalaya belt with Permian Volcanics directly on Precambrian/ Cambrian basement and with typical India Glossopteris flora. 4 (Spec. (Permian fusulinids in four levels in Baoshan and Sibumasu Blocks. Burrett. Philippines 46. Monogr. In: G. Amer. C. H. Palaeoclim. p. East Cimmerian continent poor Tethyan neoschwagerinid and verbeekinid genera in M Permian. (Permian radiolarians in chert from five sections in C Busuanga lsland suggest four Permian interval zones: Follicucullus monacanthus (late Early Permian). Mizzia velebitana) Ueno. 169-176.) Gondwana Six: Stratigraphy. incl. p. (1994). Tetrataxis) and algae incl. Chonglakmani. 160-163.go. & G.P. K. 6th Int. Philippines 49. Palawan. J. Thanee (2007).. M. 119-193. Geosciences J. C.th/library/Proceedings-Yearbooks/M_1/2007/12718.. Geophys. (Permian-Jurassic radiolarian biostratigraphy (see also Marquez et al. 5. McKenzie (ed. Campbell & Q. (2003). In Kashmir Basin Artinskian? Mamal Fm above Panjal Volcanics with rich E Permian flora. Columbus. Chonglakmani. C. F. 49-104. both with widespread diamictite. University of Tsukuba.. Conf. J. p.Permian to Jurassic radiolarian biostratigraphy of Busuanga Island. C Thailand (W side of Indochina Block). Philippines. Series 41.P. H. Ohio.com March 2014 .1 345 www. Singh (1987). Hemigordius sp. Union (AGU).) Proc. Gingkophyllum and Parasphenophyllum.Lingshi) with more complete Cambrian. Sedimentology. With common large alatoconchid bivalves. Doc.Permian section and more marine influence (limestones) and mixed Gondwana-Cathaysia flora.Gondwana and associated rocks of the Himalaya and their significance. (M Permian carbonate sequence in S of Khao Khwang Platform. Geophys. Palaeoecology 193. In: W.Tripathi. and Paleontology. Sci. 195-205.87. Thassanapak.. (Along N margin of India Plate (Permian rift margin) two Permian Gondwanan domains. In Karakorum Basin (= Lhasa or Qiantang Block?) Fenestella Shale.). 2006)) Tumanda. C. Philippines. Geol. Tumanda. Follicucullus scholasticus (early Late Permian) Latentifistula similicutis (middle Late Permian). Philippines. Midian-age limestone with fusulinids and smaller forams.Depositional setting and paleoenvironment of an alatoconchid-bearing Middle Permian carbonate ramp sequence in the Indochina Terrane. Palawan. p. (1991).Permian radiolarian from Busuanga Island.. p. (1991). Also endemic vertebrate fauna. incl. Ed.The Permian fusulinoidean faunas of the Sibumasu and Baoshan blocks: their implications for the paleogeographic and paleoclimatologic reconstruction of the Cimmerian Continent. K. p. p. Asian Earth Sci. 37-55. C Thailand (tropical Tethyan shelf of Indochina Terrane).dmr. Tantiwanit (ed.Permian fusulinacean faunas of the Sibumasu and Baoshan Blocks: implications for the paleogeographic reconstruction of the Cimmerian continent. Increase in diversity from E to late M Permian (N- Bibliography of Indonesia Geology . Agathammina. F. Rajahia. (2) (N) Tethyan Himalaya belt (Salt Range-Ladakh. Feng (2014). probably contemporaneous with Kamura event and related to global cooling and sea-level lowstand) Udchachon. Platform evolved from rimmed platform in E Permian to ramp in M Permian. Geol. central Thailand. (online at: http://library. Gondwana Symposium. Ed.Thakkola.Radiolarian biostratigraphy in central Busuanga Island. Gondwanan Glossopteris spp. Dissertation. endemic Gangamopteris kashmirensis.. Palawan. overlain by diamictite. Gangamopteris plant bed and fusulinid lst) Tumanda. Campbell & N. J.. Soc. 1985. (Expanded version see below) Ueno. Geology of Thailand: towards sustainable development and sufficiency economy. H. also common 'Cathaysian' elements like Taeniopteris. M.Late Middle Permian alatoconchid- bearing limestones from the south of the Khao Khwang platform.D.pdf) (Thick-shelled. Int. (2000). Bangkok.Abrupt negative shift in d 13C in late Wordian and late Capitanian indicate significant changes in paleoenvironment. exposed extensively along Phetchabun fold-thrust belt along W edge of Khorat Plateau. non-tropical. K. p. E. Monodiexodina-bearing areas can be restored to either N or S middle latitudes. Rare Tethyan fusulinids in Baoshan and Sibumasu blocks suggests E Cimmerian continent still far from Cathaysian domain and in warm temperate. Geosci. J. Igo (1997). J. etc. Geol. K.M. Inst. Asian Earth Sci. Artinskian. E Cimmerian migrated into tropical zone by Late Triassic with Carnian sponge-coral buildups in Sibumasu Block) Ueno.Artinskian conodonts from the Dingjiazhai Formation of the Baoshan Block. & H. Northeast Thailand. Sugiyama (1996). N.. K. Inst.Upper Carboniferous forminifers from Phu Tham Maholan.B (Geol. Arita. Saesaengseerung (2014). Generally found in monotypic. Sugiyama (1995).. Type species of Monodiexodina is Schwagerina wanneri Schubert 1915 first described from Timor. and paleobiogeographic implications. Sugiyama (1994). late E Permian fusulinid genus Monodiexodina from 33 areas. Changwat Loei. Asian Earth Sci. (2006). (2007). similar to Indochina Block) Ueno. Nakornsri & T.E Midian (=Capitanian)) Ueno.1 346 www. Sardsud & D.subtropical zone until end-Permian. Northeastern Thailand. 1. In: 13th Int. Iskandar et al. Wang & S. J. p.Early Permian fusuline faunas from Jambi. Southeast Asian Earth Sci. Meno. Inst. p. Northern Thailand: geologic age.) 16. p. I. faunal affinity.van Waveren. east of Wang Saphung. Repts. Congress on the Carboniferous and Permian. crowded manner in sandy sediments with uni-directionally aligned shells. 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Yakhtashian-Bolorian (=late Artinskian.. Nagai. M.Late Paleozoic foraminifers from the Chiang Dao area. 339-354. Northeast Thailand. Nishikawa. Mei (2003).. S. M.. Sci.com March 2014 . Interpreted as warming spikes during late Yakhtashian-Bolorian transgression) Ueno.. 79-89... Southwest China. Nakornsri & T. 157.A. Fauna consists of Pseudofusulina and Praeskinnerella? spp. (E Permian conodonts from Dingjiazhai Fm diamictite-bearing unit in Gondwana-derived Baoshan Block. K. Univ. 741-750. Mizuno. 5. Krakow 1995. K. A. West Yunnan. F.. Sci. 26. K. J. (Small foraminiferal fauna with two species of Fusulinella) Ueno.) 15. Congr. K. Nanjing. p. Sumatra. Geosci.vangorselslist. southeast of Wang Saphung. p. Yala fauna almost coeval with Monodiexodina fauna known elsewhere on Sibumasu Block. Nagai. Similar Tethyan affinity shallow marine fauna in Sibumasu in E Permian of Kinta Valley area in W Peninsular Malaysia. kraffti. B (Geol. Geological anatomy of E and S Asia. 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Major monograph on crinoids of Timor. from various localities (genus often regarded as cold- water 'Gondwanan'. collected in 1909 and 1911. 1937. Verhandelingen Geol. 5. gen. Detailed description of anatomy of Permian blastoids Timorechinus spp.) Palaontologie von Timor 6. Noord Hollandsche Publ. Yang. scholasticus. published over 15 year period. 1-329.vangorselslist. Stuttgart. 4. Palaeoworld 15.F. Ed. Nederl.E Lopingian F. Li (2006). 2. ('On a remarkable echinoderm from the Permian of Timor'. one of richest in world. (ed. incl.. Pal. Amsterdam. Wanner (ed.) Geological Expedition of the University of Amsterdam to the Lesser Sunda Islands. Q. Schweizerbart.X.Timorocrinus nov. 18. ventricosus- F. based on new material collected by Ehrat in 1927 and Brouwer/ De Roever 1937 expedition. (1940). (Permian gastropods from Timor 70 species.1 352 www. p. Bibliography of Indonesia Geology .Die permischen Echinodermen von Timor I. In: H..P.A. 1-82. 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(1914-1929).Lopingian (Upper Permian) radiolarian biostratigraphy of South China. J. J.com March 2014 .. Cheng & J. mainly from Basleo area. Y. (1920). (1915).J. Flexibilia.Neue Beitrage zur Kenntnis der Permischen Echinodermen von Timor. Proc. Wetenschappelijke Mededeelingen 16. (1931). p. J. J. 1-31. J. (‘New contributions to the knowledge of Permian echinoderms of Timor 5. Hypocrinites. (1931).('On arm-less crinoids from the Late Paleozoic') Wanner. (1924). V. p. Wetenschappelijke Mededeelingen 11. First of long series. (1926). II. probably representing different stages of Permian. 1-81. IV. und Bolboporites Pander). Paracatillocrinus und Allagecrinus. Character of faunas more European (Tethys) than American (NB: taxonomy of blastoids revised by Breimer & Macurda (1972). p.Neue Beitrage zur Kenntnis der Permischen Echinodermen von Timor. (‘New contributions to the knowledge of Permian echinoderms from Timor. 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(‘The Permian crinoids of Timor’) Wanner. The anomalies of the Schizoblasts') Bibliography of Indonesia Geology . 23. New crinoid species. Pt. Brouwer (ed. 42 p. nov.VII. 20-48. III. 696-712.dwc. Sonderband (Steinmann Festschrift). (1930). Wetenschappelijke Mededeelingen 14.Ueber einige palaeozoische Seeigelstacheln (Timorocidaris gen.A. Amsterdam. Geol. in German) Wanner. Indie. Wetenschappelijke Mededeelingen 20.-Indie. In German) Wanner. (1920). Dienst Mijnbouw Nederl. Paracatillocrinus and Allagecrinus’. p. p. Hypocrininae. (‘The Permian echinoderms of Timor.Die permischen Krinoiden von Timor. 22. In German.1 353 www.Neue Beitrage zur Kenntnis der Permischen Echinodermen Von Timor.com March 2014 . Dienst Mijnbouw Nederl. Kon. p. 1. Dienst Mijnbouw Nederl. Timor) Wanner. Allagecrinus and II. HvG)) Wanner. Die Crinoidengattung Paradoxocrinus aus dem Perm von Timor. 297-314. 370-395. Pal. 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Orbitremites) also occur outside Timor (But: Timoroblastus and Deltoblastus also in North Oman. 201-281.) Geological Expedition of the University of Amsterdam to the Lesser Sunda Islands. (‘New contributions to the knowledge of Permian echinoderms of Timor 14’..echinoids') Wanner. Neues Jahrbuch Miner. Geol. with a contribution to the systematics of the blastoids'.Poteriocrinidae part 4') Wanner. Geologie Niederl. 12. mit einem Beitrag zur Systematik der Blastoiden. Amsterdam. 4. B. J. Echinoidea. Monatschafte 1950.com March 2014 . Beitr. p. Beitr. No stratigraphy. 295-314. already known from earlier Timor papers) Wanner. J. Geologie Niederl.. 1. 201-214. Beitr. Zentralblatt Min. Descriptions of Permian ammonites from Basleo.. 7. mainly from De Marez Oyens and Brouwer 1937 collections from Basleo. 5. (‘New blastoids from the Permian of Timor. collected by Ehrat. J. (‘Contributions to the paleontology of the East Indies Archipelago 19. In: H. 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In German) Wanner.-Indien IV. (1941). ('On the knowledge of the Permian brachiopods of Timor: 1. Of the 13 Permian blastoid genera known from Timor only two or three (Schizoblastus. Palaeontologie des Ostindischen Archipels III.A. p. J. (‘New contributions to the knowledge of Permian echinoderms of Timor 8-13’. Suppl. (1941). Sieverts (1935). 215. etc.277.Zur Kenntnis der permischen Brachiopoden von Timor. (1951). Palaeontographica. p. (Permian bivalves collected by Ehrat in 1927 and Brouwer1937 expedition.-Indien IV. Palaeontologie des ostindischen Archipels 12. Molengraaff. Amsterdam. Band 74. Pal. ('On the knowledge of the Permian ammonoid fauna from Timor. Band 67. 3 Teil. p. p. (1932). Geol.. Brouwer (ed. Geol.Neue Beitrage zur Kenntnis der permischen Echinodermen von Timor XIV. Co. B. (1940). J. Pal. 1. (1940). W Timor. p. (Common late E Permian (Baigendzhinian) bryozoa in outcrops of Aifat Fm (= M Aifam) of upper Aifar River.The evolution. 83-197.K. few families. Reg. Harland (eds.B. etc. 337-354. P. (online at: https://gsmpubl. southern Thailand. (1981).Origin and evolution of Permian brachiopods of Australia. J. R. n. especially Himalayas. Indonesia. East Australia. 11-25. Vietnam. Palaeontographica. (Permian brachiopods of Australia two main associations: (1) E Australia. (Cyclolobidae of M Permian age. (1972).. suggesting pebbly mudstones are cool water deposits. Rhabdomeson.B.E. Most genera are found in temperate. Paralyttonia transiens n. Magazine 119. Cambridge University Press. Conference on the Geology of SE Asia. With Lyttonia catenata n.sp. (1981).files. J.B. Bangkok. 251-270. (1989). Malaysia 6. (E Permian (Asselian) small brachiopod fauna from E Permian pebbly mudstones. In: B. Palaeont. 187-210. Assoc. (2011). In: M.com March 2014 .B. Thailand. 43-213. affected by cool- glacial conditions. Piyasin (1970). probably of mid- Sakmarian age suggested by Brachythyrina rectangulus and Neospirifer sterlitamakensis.gen.) 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SW part of Birds Head. 4. Waterhouse et al. Ser. interpreted Late Artinskian age by Sakagami 1976) and NW Australia Canning Basin (with Stenodiscus variablis)) Waterhouse.B. Centre. HvG)) Waterhouse. Assemblages affinities with Ko Muk region of Peninsular Thailand (with Sulcoretepora. (1973). Mineral Res.. 41.B. No mention of any Indonesian faunas) Waterhouse. Lethaia 5. Res. (eds. Waagenoceras.wordpress. A. Dept.sandstones of Phuket Gp at Ko Muk and Ko Phi Phi islands. Rhynchopora. Kuala Lumpur 1972. p. p. A.B.) Bibliography of Indonesia Geology . and paleogeographic significance of the Permian ammonoid family Cyclolobidae. (Incl. 1-56. Paralyttonia girtyi)) Wass. with limestone beds with diverse crinoid assemblage of 40 species. G. In: G. D. 1-2. & P. 64-68. (1998). 12. G. Alcheringa 11. p. Timor faunas Sakmarian-Asselian and Kazanian.Permian crinoids from the type-section of the Callytharra Formation. Halimeda limestone (deep fore-reef slope ~20-60m. In: G. G.) Strzelecki Int. Mem. 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Shi. 339-352. 51 from East Australia. (New canted-cup crinoid from W Timor described as Exotikocrinus dochmos gen. J. 45-72. 5. palaeogeography and resources. Australian faunas generally considered as cooler water faunas. Proc.D. 49-74.S.Revision of two species of ?Ulocrinus and a new pelecocrinid crinoid from West Timor. Paleoecology and stratigraphy poorly understood. (1987). and most diverse and abundant. p. Ed.Permian echinoderms from Western Australia. G. 1-2. Symposium on Permian of Eastern Tethys: biostratigraphy.D.) Webster. Heterostegina. (Rich Permian Timor fossils poorly constrained stratigraphically. n.. Palaeoworld 21. Reasons for local endemism unclear.Waters. J. p. Soc. Callytharra Springs. n. N. Potts. Wallace. Some common species between Timor and Australia. In Artinskian greater similarity beween W Australia and Timor than between W and E Australia) Webster. Gallup (2004)- Coralgal composition of drowned carbonate platforms in the Huon Gulf.. p. 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B57.A.Pleistocene vertebrates from Celebes. Early Pleistocene) Hooijer. p. Quaternaria 3. (1954). 11. Leiden. should be assigned to Lower Pleistocene) Hooijer. D. (online at: www. p.com March 2014 . 5-10. 15. Elasmobranchii. X. (1954). 6-9. Lower molars of Archidiskodon celebensis Hooijer. (1956). Flores. Dentition and skeleton of Celebochoerus heekereni Hooijer. p. p. Proc.A. Ed. 91-102. Zoologische Mededelingen. (1957). 31. Zoologische Mededelingen. p. Zoologische Verhandelingen. Kon. p. 125-128. originally considered to be of Middle-Late Pliocene age by Von Koenigswald. 486-489. 4. (1954). Amsterdam. Stegodon spec. Central Ngada.1 394 www.naturalis. D. S Sulawesi) Hooijer.(Tjidjulang and Kali Glagah mammal assemblages of Java.The correlations of fossil mammalian faunas and the Plio-Pleistocene boundary in Java. 60. Zoologische Mededelingen. Kon. trigonocephalus Martin from Pleistocene of Java) Bibliography of Indonesia Geology .Pleistocene vertebrates from Celebes. 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Techn. 131-149. with emphasis on human origins.('A prehistoric culture center along the Solo River'.40.The place of Homo soloensis among fossil men.37.A. (2007). (Review of chronostratigraphy of hominid-bearing formations of C and E Java. etc. Modern Quaternary Research in Southeast Asia 7.Evidence on the age of the Asian Hominidae. Comm. perhaps suggesting slightly drier climate than today) Polhaupessy.La sedimentation du lac de Guyang Warak (Punung-Java Est. LIPI Press.25 Ma and 0. Proc. (eds. (Two pollen zones distinguished in Pleistocene of Trinil (site of first Homo erectus in C Java) Pucangan Fm rel. A. p. & J. Asian fossil record suggests gradual change over ~1 million years) Pope. East Java. Most radiometric dates without well documented stratigraphic position or analytical uncertainty. Seri Paleontologi 9.Palynological evidence for a Pleistocene environment in Trinil.W.0 Ma old. Orchiston.E.The influence of climate and geography on the biocultural evolution of the Far Eastern hominids. suggest temperatures several degrees cooler than today) Pope. In: E. (eds. East Jawa. New Haven. Most reliable date is 0. Histoire Naturelle.Environmental setting of human migrations in the circum-Pacific region. Dev. Bandung. 377-396. D.P.O. Soejono's Festschrift. Ed.F. 5.S. Trinil. J. On mammal and hominid remains in Pleistocene fluvial terraces near Ngandung. 1-21. 1-7. Sess. p. All can be incorporated in Homo erectus or Homo sapiens. Centre (GRDC). 16. Exposures at 1. R. C.65-0. G. p. Siesser (1982).Chronostratigraphy of the Plio-Pleistocene fossil hominids of Java. Master Thesis. 348-360. Jakarta.) Archaeology: Indonesian perspective. Early Man.Environment of early man in Java. p. A.E. (2006). Rotterdam. Biogeography 35. (Review of palynological analyses at Quaternay deposits of Java. National Academy Sciences USA 80. Geol. Programs E and SE Asia (CCOP). Absence of large carnivores and primates suggest more insular affinity than Borneo. show Late Miocene transition from stegolophodons to stegodons. 1-13. East Java. (2013). Mojokerto.The ages of the Solo Terraces at the Ngancar and Ngandong Region. 448-451 and p. (Humans first colonized Palawan at ~40. 455-459. Palaeoclim. Y.R. Re-described by Martin 1886) Rahardjo. Palaeogeogr. Garong (2001). G. Buletin Geologi (ITB) 37. Epileptobos groeneveldtii). ('On fossil bones from the Pandan'. Palombo (2013).. Philippines. Rizal. (online at: http://eprints. Palaeoecol.und Ost-Java.1 411 www. 73-85. Middle Jawa. etc.E. R. Schulz.fr/doc/2005QP11abstracts.vangorselslist. Yunnan. K. 5. flourished in eogene and Quaternary of Asia. ('Climate change and Pliocene-Pleistocene age boundary based on foraminifera and palynology analysis in the Mojoroto area.65 + 1. 1-251. C Java. Cambridge University Press. 433-437. & A.pdf) (Best estimates of ages of Pleistocene terraces along Solo River: High-terraces ~47 ka.Stratigraphie et sedimentation au Sud Est de Dome de Sangiran: l’environnement des Homo erectus au debut de Pleistocene moyen. H. p. De Vos. 1.5 ka) Rizal. Javanese bovid Duboisia santeng from Sangiran regarded as typical insular endemic species due to small size. Iriani (2005). Y. but higher diversity than truly ocenaic islands in Late Quaternary) Rightmire. 409-412. Palaeoecology. East Java') Reis.. Thesis Universita degli Studi di Ferrare. p..R. but is present in late M Pleistocene of what is now Peninsular Malaysia) Saegusa. E. Y..unife.mnhn. (2005). p.Jawa Timur. A. Winkler.. 1891) from the Early-Middle Pleistocene of Java: a multiproxy approach to its palaeoecology.Kabuh Formations. M. (1998). 31-48. South Sukabumi. p. Bibos palaesondaicus. 377. p.D. p.com March 2014 . llike fossil bovids. Palaeogeogr. Y.Die Terrassen entlang des Solo-Flusses in Mittel.(online at: http://hopsea. 29-34. Zaim & Y.mnhn. (online at: http://hopsea. D.Over fossiele beenderen van den Pandan. identification of soil horizons with human occupation. (Unpublished) (’The terraces along the Solo River in Central and East Java’) Rizal. Ph. Plalaeoclim. 1- 189.it/831/1/Purnomo_tesi.T. Natuurkundig Tijdschrift Nederlandsch-Indie 29. (1993). Ed.. Depositional environments of Upper Pucangan. frequent volcanic eruptions. Middle-terraces ~20 ka and Lower-terraces 1.P.fr/pc/thesis/Purnomo_Andri_2007.Notes on Asian stegodontids. Thesis Universitat Koln. 1. (Stegodontids (elephant-like proboscideans). Ratanasthien (2005). (1999). Y.. 422-423.Late Quaternary terrestrial vertebrates from Palawan Island.Late Tertiary fossil whale from Surade. p. Indonesia. Rozzi. A. (During Pleistocene. Buletin Geologi (ITB) 3. 171. Thailand and Yuanmou Basin.pdf) ('Sedimentation of Guyang Warak lake (Punung. Italy.000 yr BP. Thasod & B. Indonesia'.The evolution of Homo erectus: comparative anatomical studies of an extinct species. 126-128. J.The enigmatic bovid Duboisia santeng (Dubois. p. Significant recent finding of new stegodontid fossils at Nakhon Ratchasima.)) Raden Saleh (1867). 276p. South Central Java ) Purnomo.M. common in E-M Pleistocene 'Stegodon- Homo erectus fauna' (Bubalus palaeokerabau. Cambridge. suggesting stegodons originated in Asia) Bibliography of Indonesia Geology . Mojokerto. faunal elements of Indo-Chinese origin entered Java and most Javanese mammalian taxa are close or identical to their mainland relatives. West Java. 426-429.Perubahan iklim dan batas umur Pliosen-Plistosen berdasarkan analisis foraminifera dan palinologi di daerah Mojoroto.pdf) (Stratigraphy and sedimentation at the SE Sangiran Dome: the environment of Homo erectus at the start of the Middle Pleistocene'. Quaternary Int.Grenzbank. wordpress. (1972). C Java.K. 3. Paleontol. Survey Indonesia. (1973). Nederl. HvG) (see also Siesser & Orchiston 1978)) Sartono. Modern Quaternary Research in Southeast Asia 2.pdf&id=887&up=13) (Pithecantropus C mandible is from surface of Lower Pleistocene Putjangan beds from Sangiran area. S. Reg. Proc. Kon. Migration followed two routes. 124-126.Sartono. Sartono.Observations on a newly discovered jaw of Pithecanthropus modjokertensis from the lower Pleistocene of Sangiran. (First description of Pleistocene dwarf elephant from Timor. Sartono. 26-31. Publ. (1969). p. presumably suggesting Lower Pleistocene age (NB: most forams in Sangiran fluvial Pleistocene deposits are reworked from underlying Kalibeng Fm marine beds. Nederl. Bandung (ITB) 4. Current Anthropol. S. Central Java.. Malaysia 6. crassa. Gr. Sartono. Sartono. Akademie Wetenschappen. (1961)-Notes on a new find of a Pithecanthropus mandible. and an eastern route via Taiwan and Philippines toward Sunda Land area and Sulawesi) Sartono. p.com March 2014 . S. Teknik. Publ. (1975). Proc Inst. Proc. at base of low bluff on S side of Putjung creek) Sartono. 5. Akademie Wetenschappen B 74.On the stratigraphic position of Pithecanthropus mandible-C. p. p. (1970). S. Kon. S. Geol. S. a male specimen of Pithecanthropus erectus.Discovery of another hominid skull at Sangiran. 185-194. 273-286.id/download. S. Nat. Conf. 192-202.com/2014/09/bgsm1973018. (online at: https://gsmpubl. (1974). 5 km E of Atambua) Sartono. Akademie Wetenschappen B 71. Rotterdam. Akademie Wetenschappen.Observations on a new skull of Pithecanthropus erectus (Pithecanthropus VIII) from Sangiran. Geol. 1. (1969). In: B. 5. Bull. p. Bull.files. Proc. Geology and Mining (NIGM).vangorselslist. p. p.) Palaeoanthropology. 4. Globigerinoides obliquus. Tan (ed. S. Tuttle (ed.Genesis of the Solo terraces. Kon. Geology of Southeast Asia. 396-422. p. 1-19. Pulleniatina) and deeper marine smaller benthic foraminifera. Seri Paleontologi 2. 1-21. p.Implications arising from Pithecanthropus VIII. S. In: R. Globorotalia tumida. 327-360.itb. S. 1-51. collected by Verhoeven from sandy conglomerate overlying marine claystones near Umaklaren (Atambua). Kon. a western route across Sunda Land area. (In Sangiran area of C Java Plio-Pleistocene boundary should be placed between Corbicula beds and Lower Volcanic Breccia bed.On the Plio-Pleistocene boundary of Java. Ed. (1973). Inst. (New fossil Homo erectus skull discovered in 1969 at S flank Sangiran dome.1 412 www. (1971). Balkema. 91-102. B72. 2. W Timor) Sartono.) Proc.On Pleistocene migration routes of vertebrate fauna in Southeast Asia. (1976).Early man in Java: Pithecanthropus skull VII. (Description of additional Stegodon tooth. (online at: http://journal. Proc. B 77. central Java. Bandung 2.php?file=A70002. 1-13. Teknik Direkt.Stegodon timorensis: a pygmy species from Timor (Indonesia).H. Based on mammalian fauna it should be placed between 'Unterer Wirbeltierhorizont' and 'Oberer Wirbeltierhorizont' of Von Koeningswald) Sartono. Bibliography of Indonesia Geology . Soc. p. Central Java. (1968). Nederl. 13. p. S.On an additional Stegodon timorensis Sartono. Sartono. p. Geol. Ser. collected by Verhoeven in 1964. Nederl. Encrusting matrix of mandible with planktonic (incl. S. Kuala Lumpur 1972. 1.ac.pdf) (Pleistocene vertebrates in SE Asia originated on Asian continent and migrated during Pleistocene into the island archipelago of Indonesia. 2. Teknol. N of Ngawi. De Lumley (eds. 121-131. S.Migrasi manusia Plistocen Indonesia: kaitannya dengan tektonik lempeng. (1986). Modern Quaternary Research in Southeast Asia 4. p. complete Homo erectus trinilensis lower jaw from black claystones of Pucangan Fm in central part of Sangiran dome) Sartono. Rotterdam. Soc.com March 2014 . p. Kuala Lumpur 1984. Spec. p. hampering movement of early humans from Asia) Sartono.1 413 www. less well-known terraces identified. 2. de Paleontologie Humaine. p.Pleistocene peopling of the Southeast Asian Archipelago. In: G. C-E Java: Upper Pleistocene High terrace (Ngandong. Penablanca-Cagayan. 7. Rotterdam.and M. S. Indonesia. 7-20. (1982). coincided with onset of Gunz glacial.8 Ma. (Fossiliferous terrace deposits of Walanae River most likely Pleistocene. 1-12. Indonesia. (1980). Balkema.H. Geol. (1978).The age of the vertebrate fossils and artifacts from Cabenge in South Sulawesi. 5. S. p. Sartono.New lights on human evolution in Southeast Asia. Appear to be associated with more advanced Homo erectus ngandongensis) Sartono.The stratigraphy of the Sambungmacan site in Central Java. S. 57-63. 83-88. mainly from aerial photos. p.pdf) (Until 1980 the subdivision of Pleistocene human fossils as proposed by Von Koenigswald (1968) was used. Mineral and Energy Resources of SE Asia (GEOSEA V). Highest terraces oldest (Early Pleistocene?) and 97m above Solo River. p. (see also Bartstra 1977)) Sartono. off Solo River. Publ. In: Geologi Kuarter dan lingkungan hidup. Res. Rotterdam. (Rel. p. Sartono. S. Development Center. Bandung. 12th Indo-Pacific Prehistory Association Congress. Modern Quaternary Research in Southeast Asia 5.my/products/702001-101423-PDF. S.) Congres Int. Phillipines. possibly coinciding with Riss glaciation). Rotterdam. Modern Quaternary Research in Southeast Asia 9.org. possibly Holocene) Sartono.equivalent) Sartono. S. Geol. (First report of Pleistocene Stegodon mandible from Sumba (Watu Mbaka). 2. Rotterdam. Anthropologie 18. Balkema. p. p. New discoveries in last 5 years necessitate re-assessment. 129-135.Notes on the Pleistocene stratigraphy of Java. (Primitive stone artefacts named 'Sangiran flakes' limited to Top Kabuh/ Base Notopuro Formations at Sangiran. (online at: www. Teh & S. ('Pleistocene human migration in Indonesia: relation to plate tectonics') Bibliography of Indonesia Geology .vangorselslist. (1985). S. CNRS. Sartono. (1979). Nice (France). Proc. S. Rotterdam. 115-125. (1979).gsm. Described as Stegodon sumbaensis) Sartono.Datings of Pleistocene man of Java. Ed. 65-82. S. East Indonesia: an announcement. In: H. (1985). Earliest wave of human migration into SE Asia (Java) at ~1. Modern Quaternary Research in Southeast Asia 8. 495-541.Homo erectus ngandongensis: the possible maker of the 'Sangiran flakes'. Balkema. Paramananthan (eds. not E-M Pleistocene 'Grenzbank'/ Kabuh Fm. 269-288. (1984). (1987).The site of Homo erectus mandible F. p. C Java. Before this period most of SE Asian region still inundated by sea. Congress Geology. Balkema. Low Terrace and Flood Terrace.The discovery of a pygmy Stegodon from Sumba. Balkema. Modern Quaternary Research in Southeast Asia 5. Malaysia 20. 5th Reg. 19-24. Sartono. snads and silts at small Sambungmacan site. S. Modern Quaternary Research in Southeast Asia 5.) Proc. (Gravels. in which Homo erectus cranium was found in 1973.Characteristics and chronology of early man in Java.(Three well-known river terrace levels along transverse valley of Solo River. Also three older. (1979). Bull. now regarded as of part of Ngandong Fm of Late Pleistocene age. Balkema. none found in lower levels with hominid remains. Sartono, S. (1991)- A new Homo erectus skull from Ngawi, East Java. Bull. Indo-Pacific Prehistory Assoc. 11, p. 23-35. (online at: http://ejournal.anu.edu.au/index.php/bippa/article/view/596/585) Sartono, S. (1991)- Meganthropus paleojavanicus v.K.: its place in human evolution. Fourth Int. Senckenberg Conf., Frankfurt 1991, p. Sartono, S. (1996)- Java: diversity of Upper Pliocene- Pleistocene hominids. Buletin Geologi (ITB) 26, 1, p. 1- 12. (Final paper by Sartono; overview of hominids distribution, evolution, migration on Java) Sartono, S. (1991)- Homo (Pithecanthropus) erectus: le debat sans fin. L'Anthropologie 95, 1, p. 123-136. ('Homo erectus: the debate without end'. On taxonomic status of Homo (Pithecanthropus) erectus. Two groups of early men are found in Java: Homo (H. robustus and H. erectus) and Australopithecus (A. (Meganthropus) palaeojavanicus). Pleistocene hominids from SEt Asia probably subjected to evolution while they migrated from Asia toward Australia. Two migration routes, a western (Sunda Shelf) and a northern one (Philippines), both arriving in Wallacea, possibly also in Sahul (Australia-New Guinea) Sartono, S. & S. Hadiwisastra (1983)- Fosil vertebrata Plistosen di Busur Banda: implikasi struktural. Proc. 12th Ann. Conv. Indon. Assoc. Geol. (IAGI), p. 153-161. ('Pliocene fossil vertebrates in the Banda Arc: structural implications') Sartono, S. & R. Marino (1978)- A mandibula and a maxilla of Stegodon timorensis. Modern Quaternary Research in Southeast Asia 4, Balkema, Rotterdam, p. 41-50. (Additional Pleistocene elephant teeth from Weaiwe region, Atambua, NE part of West Timor) Sartono, S., D.W. Orchiston, W.G. Siesser & T. Djubiantono (1981)- Upper Pliocene sediments in Sangiran, Central Java (Indonesia). Buletin Geologi (ITB) 5, p. 1-25. (Base Sangiran Fm between nannofossil zones NN16 and NN18 (1.65- 3.25 Ma); Bettis et al. 2004) Sartono, S., F. Semah, K.A.S. Astadiredja & T. Djubiantono (1981)- The age of Homo modjokertensis. Modern Quaternary Research in Southeast Asia 6, Balkema, Rotterdam, p. 91-102. (On age of fossil child skull cap originally described by Von Koenigswald in 1936, from locality near Perning, 14 km ENE of Mojokerto. Supposedly from Lower Pleistocene Upper Pucangan Fm/ volcanic facies,but rocks more likely equivalent of M Pleistocene Kabuh Fm of Sangiran. Underlying clay facies of Lower Pucangan/ Lidah Fm with zone N21 planktonic foraminifera (Globorotalia tosaensis, Globigerinoides obliquus extremus; also Asterorotalia trispinosa. New finds of associated Hippopotamus, Sus, Buffelus bubalus, etc., suggest M-U Pleistocene Trinil or Ngandong fauna) Satyana, A.H. (2007)- Geological disaster in the demise of Jenggala and Majapahit empires: a hypothesis of historical mud volcanoes eruptions based on historical chronicles of Kitab Pararaton, etc. folklore of Timun Mas; analogue to present LUSI eruption, and geologic analysis of the Kendeng depression- Brantas Delta. Proc. Joint Conv. 36th IAGI, 32nd HAGI, Bali 2007, 38 p. (Jenggala and Majapahit are two empires of 11th to early 16th centuries at Brantas delta, E Java. Rise and fall related to geological processes in Brantas delta. Large mud volcano eruptions may have caused or contributed to demise) Satyana, A.H. (2008)- Roles of mud volcanoes eruptions in the decline of the Jenggala and Majapahit Empires, East Java, Indonesia: constraints from the historical chronicles, folklore, and geological analysis of the Brantas Delta-Kendeng Depression. Majalah Geologi Indonesia 23, 1-2, p. 1-10. (Mud volcanoes in Kendeng zone may have lead to demise of 11th- 16th century Jenggala and Majapahit empires) Bibliography of Indonesia Geology , Ed. 5.1 414 www.vangorselslist.com March 2014 Satyana, A.H. (2009)- Sangiran dome, Central Java: mud volcanoes eruption, demise of Homo erectus erectus and migration of later hominid. Proc. 37th Ann. Conf. Indon. Assoc. Geol. (IAGI), Bandung 2008, 12 p. Schutt, G. (1972)- Fossil mammals of Java IV. Zur Kenntnis der pleistozanen Hyanen Javas. Proc. Kon. Nederl. Akademie Wetenschappen, Amsterdam B 75, p. 261-287. ('On the knowledge of Pleistocene hyenas from Java') Schutt, G. (1973)- Fossil mammals of Java V. Pleistozane Caniden (Carnivora, mammalia) aus Java. Proc. Kon. Nederl. Akademie Wetenschappen, Amsterdam, B 76, 5, p. 446-471. ('Pleistocene canids from Java') Selenka, M.L. & M. Blanckenhorn (eds.) (1911)- Die Pithecanthropus-Schichten auf Java. Geologische und palaontologische Ergebnisse der Trinil-Expedition (1907-1908). W. Engelmann, Leipzig, p. 1-342. (Extensive report of 1907-1908 excavations of Pleistocene beds near Trinil, C Java, by Selenka Trinil Expedition No new hominid fossils found, but extensive documention of localities and good descriptions of Pleistocene vertebrate and invertebrate faunas and flora) Semah, A.M. (1982)- Etude palynologique de sites a hominides de l'ile de Java. These 3me cycle, Universite de Provence, Marseille, p. 1-127. ('Palynological study of hominid sites of Java island') Semah, A.M. (1982)- A preliminary report on a Sangiran pollen diagram. Modern Quaternary Research in Southeast Asia 7, Balkema, Rotterdam, p. 165-170. (Summary of palynology work on U Pliocene- Pliocene of Sangiran Dome, C Java. Rel. common mangrove pollen (Rhizophora, Sonneratia, Nypa)in Upper Kalibeng Fm Blue Clays (absent in Pucangan Black Clay and in younger section). In Pucangan/ Kabuh interval mainly Graminae (grasses)) Semah, A.M. (1984)- Remarks on the pollen analysis of the Sambungmacan section (Central Java). Modern Quaternary Research in Southeast Asia 8, Balkema, Rotterdam, p. 29-34. (Pollen diagram of Pleistocene deposits of Sambungmacan, E of Solo, site of 1973 discovery of Homo erectus skull. <10m thick poorly-dated fluvial, sandy-tuffaceous section, unconformable over Pliocene limestone) Semah, A.M. (1984)- Palynology and Javanese Pithecanthropus environment. In: P. Andrews and J.L. Franzen (eds.) The early evolution of man with special emphasis on Southeast Asia and Africa. Courier Forsch. Inst. Senckenberg. 69, p. 237-243. Semah, A.M. (1984)- Le milieu naturel lors du premier peuplement de Java, Resultats de l’analyse pollinique. Doct. Thesis, Universite de Provence, Marseille, p. 1-152. ('The natural environment of the first human seetlement of Java; results of pollen analysis') Semah, A.M. & F. Semah (2001)- La signification paleoecologique des couches a hominides de l’ile de Java. In: F. Semah et al. (eds.) Origine des peuplements et chronologie des cultures paleolithiques dans le sud-est asiatique, Semenanjung/Artcom, Paris, p. 251-277. Semah, A.M. & F. Semah (2012)- The rain forest in Java through the Quaternary and its relationships with humans (adaptation, exploitation and impact on the forest). Quaternary Int. 249, p. 120-128. (Landscape change in Java over last 2.5 million years highly complex, with repeated expansion and fragmentation of rain forest. Evidence of intensive human impact on rain forest observed late, ~1500 years ago) Semah, A.M., F. Semah, T. Djubiantono & B. Brasseur (2010)- Landscapes and hominids' environments: changes between the Lower and the Early Middle Pleistocene in Java (Indonesia). Quaternary Int. 223, p. 451- 455. Bibliography of Indonesia Geology , Ed. 5.1 415 www.vangorselslist.com March 2014 (Change in paleoenvironments in Lower and early M Pleistocene, based on sediment and pollen records in C Java. 'Grenzbank' layer at ~0.9 Ma at Sangiran marks major tectonic (folding of Kendeng zone) and climatic change (fragmentation of rainforest cover)) Semah, F. (1982)- Pliocene and Pleistocene geomagnetic reversals recorded in the Gemolong and Sangiran Domes (Central Java). Modern Quaternary Research in Southeast Asia 7, Balkema, Rotterdam, p. 151-164. (Notopuro and Kabuh Fms of Sangiran and Gemolong all with normal geomagnetic polarity and tied to Brunhes Epoch. Reversal events in underlying Pucangan Fm, tied to Matuyama Event. Top of U Kalibeng Fm normal polarity, probably Olduvai Event (1.67-1.87Ma)) Semah, F. (1984)- The Sangiran Dome in the Javanese Plio-Pleistocene chronology. In: P. Andrews and J.L. Franzen (eds.) The early evolution of man with special emphasis on Southeast Asia and Africa. Courier Forschungen Inst. Senckenberg. 69, p. 245-252. (Review of Late Pliocene- M Pleistocene stratigraphy of Sangiran, C Java (~2.0- 0.5 Ma)) Semah, F. (1986)- Le peuplement ancien de Java: ebauche d’un cadre chronologique. L’Anthropologie 90, p. 359-400. (Chronology of human population of Java) Semah, F. (1997)- Plio-Pleistocene reference sections in Indonesia. In: J.A. van Couvering (ed.) The Pleistocene boundary and the beginning of the Quaternary, World and Regional Geology 9, Cambridge University Press, p. 264-272. (Brief review of Plio-Pleistocene stratigraphy in C Java areas known for vertebrate fossils (Bumiayu, Sangiran)) Semah, F., C. Falgueres, Y. Yokoyama, G. Feraud, H. Saleki & T. Djubiantono (1997)- Arrivee et disparation des Homo erectus a Java, les donnees actuelles. Abstracts 3rd Mtg European Assoc. Archaeol., p. 11-12. ('Arrival and migration of Homo erectius on Java, the actual data'. Critique of Swisher et al. (1994), suggesting their 1·66 Ma age assigned to H. erectus skulls from Sangiran is based on radiometric age of volcanic tuff that underlies these skulls and therefore too old) Semah, F., G. Feraud, H. Saleki, C. Falgueres & T. Djubiantono (2000)- Did early man reach Java during the late Pliocene? J. Archaeol. Sci. 27, p. 763-769 Semah, F., H. Saleki, C. Falgueres, G. Feraud & T. Djubiantono (2000)- Did early man reach Java during the Late Pliocene? J. Archaeol. Sci. 27, 9, p. 763-769. (Homo erectus (Pithecanthropus) reached Java from Asian continent and became one of oldest islanders in world. Combined 40Ar/39Ar and paleomagnetic data of 'Lower lahar' at base of fossil-bearing series of Sangiran dome show that emergence of first dry land at Sangiran, took place at end and just after Olduvai subchron. Therefore ~1.7 Ma is max. age for arrival of first hominids at Sangiran) Semah, F., A.M Semah & T. Djubiantono (1998)- From the shoreline to the slopes of the volcanoes: the long Pithecanthropus trek. In: H.T. Simanjuntak et al. (eds.) Sangiran: man, culture and environment in Pleistocene times, Yayasan Obor Indonesia, Nat. Research Centre of Archaeology and Ecole Francaise d’Extreme Orient, p. 195-218. Semah, F., A.M. Semah, T. Djubiantono & H.T. Simanjuntak (1992)- Did they also make stone tools? J. Human Evolution 23, p. 439-446. (Recent excavations at excavation in Ngebung, NW part of Sangiran dome, C Java, found archeological layers in M Pleistocene Kabuh beds with several stone tools (flake artefacts, bolas made of andesite and quartz; older than other stone implements known from Java)) Bibliography of Indonesia Geology , Ed. 5.1 416 www.vangorselslist.com March 2014 Semah, F., A.M. Semah, C. Falgueres, F. Detroit, X. Gallet, S. Hameau, A.M. Moine & T. Simanjuntak (2004)- The significance of the Punung karstic area (eastern Java) for the chronology of the Javanese Palaeolithic, with special reference to the Song Terus cave. Modern Quaternary Research in Southeast Asia 18, p. 45-62. (Caves in S Mountains (Punung- Wonosari) existed at least since middle M Pleistocene. Human remains, including numerous stone artifacts, date back to ~230 ka) Semah, F., A.M. Semah, R. Moukridah, F. Frohlich & T. Djubiantono (2004)- A Late Pleistocene and Holocene sedimentary record in Central Java and it palaeoclimatic significance. Modern Quaternary Research in Southeast Asia 18, p. 63-88. (Study of 40m cores from Ambarawa Basin, C Java, representing Late Pleistocene- Holocene, ~21 ka- Recent. Pollen from ~21-15 ka reflect open, herbaceous landscape of rel. cool-dry climatic conditions. From ~15-10.5 ka more humid. From 10.5 ka onward more forest vegetation. First evidence of human activity at ~1500 yrs BP) Semah, F., A.M. Semah & T. Simanjuntak (2002)- More than a million years of human occupation in insular Southeast Asia. In: J. Mercader (ed.) Under the canopy- The archaeology of tropical rain forests, Rutgers University Press, New Brunswick, NJ, p. 161-190. Setiyabudi, E. (2016)- Pleistocene reptiles of the Soa Basin (Flores, Indonesia): adaptation and implication for environment. J. Geologi Sumberdaya Mineral 17, 2, p. 107-124. (Presence of fossil reptiles from mainland Asia, like giant tortoise (Megalochelys sp.), fresh water turtle (Geoemydidae), crocodiles and komodo dragon (Varanus komodoensis) in Pleistocene of Soa Basin, Flores. After crossing 'Wallace Line' at ~1 Ma lived in isolated conditions and adapted to savannah environment. Vertebrate faunas of Soe basin dominated by extinct proboscideans (Stegodon)) Setiyabudi, E., I. Kurniawan & G.D. van den Bergh ( (2012)- Fossils of Stegodon and Varanus komodoensis Sumba and Flores: a Pleistocene landbridge? Proc. 41st Ann. Conv. Indon. Assoc. Geol. (IAGI), Yogyakarta, 2012-SS-31, 4p. (Recent field survey in Sumba relocated original locality of Stegodon sumbaensis mandible described by Sartono (1979). At Lewapaku dwarf Stegodon found, with tooth of Varanus komodoensis and giant murine rodent. Lewapaku fauna similar to 900 ka old Tangi Talo fauna from Flores) Setyanta, B., H.P. Siagian & H. Wahyono (2014)- Penentuan umur fosil manusia purba di Jawa berdasarkan magnetostratigrafi. J. Geologi Sumberdaya Mineral 15, 1, p. 11-24. ('Determination of the ages of the ancient hominid fossils in Java based on magnetostratigraphy'. Review of previous magnetostratigraphic studies of hominid sites of C Java: Sangiran (hominids between base Jamarillo subchron and Brunhes-Matuyama chron boundary (0.78- 1.07 Ma)), Trinil (near top Jaramillo (0.99 Ma)), Kedungbrubus, Mojokerto (near lower limit Jaramillo (1.07 Ma)) and Patiayam (hominids in Brunhes or younger (<0.78 Ma)) Shutler, R., J.M. Head, D.J. Donahue, A.J.T. Jull, M.F. Barbetti, S. Matsu’ura, J. de Vos & P.Storm (2004)- AMS radiocarbon dates on bone from cave sites in Southeast Java, Indonesia, including Wajak. Modern Quaternary Research in SE Asia 18, p. 89-93. (14C apatite dates for bones from Wajak Cave, SE Java. Wajak fauna calibrated age ~12,1-12,9ka, Wajak femu ~7.5 ka (older ages obtained by Storm et al. 2013)) Siesser, W.G. & D.W. Orchiston (1978)- Micropalaeontological re-assessment of the age of Pithecanthropus mandible C from Sangiran, Indonesia. Modern Quaternary Research in Southeast Asia 4, p. 25-30. (Pithecanthropus mandible C discovered in 1960 in Pucangan Fm near Mandingan, Sangiran Dome. Sartono (1970) reported 11 planktonic and 15 benthic species of foraminifera in claystone adhered to mandible. Co- occurrence of Globorotalia crassaformis and Globigerinoides obliquus suggests Late Pliocene age, between 4.2-1.6Ma. (N.B.: Sangiran Pleistocene fluvial-lacustrine Pucangan Fm contains locally abundant Pliocene planktonic foraminifera, all reworked from underlying Kalibeng Fm; Van Gorsel and Troelstra 1981)) Bibliography of Indonesia Geology , Ed. 5.1 417 www.vangorselslist.com March 2014 Sighinolfi, G.P., S. Sartono & G. Artioli (1993)- Chemical and mineralogical studies on hominid remains from Sangiran, Central Java (Indonesia). J. Human Evolution 24, p. 57-68. Simanjuntak, T. (2001)- New light on the prehistory of the Southern Mountains of Java. Bull. Indo-Pacific Prehistory Assoc. (IPPA) 21, p. 152-156. (online at: http://ejournal.anu.edu.au/index.php/bippa/article/view/272/262) (Many limestone caves in Gunung Sewu, S Java, were inhabited in Prehistoric times. Excavations revealed chronology from Early Holocene (possibly Late Pleistocene) to 4500 BP. by ‘Australomelanesian’ people) Simanjuntak, T. (2002)- Gunung Sewu in prehistoric times. Gadjah Mada University Press, Yogyakarta p. Simanjuntak, T. (2004)- New insight on the prehistoric chronology of Gunung Sewu, Java, Indonesia. Modern Quaternary Research in Southeast Asia, Balkema, Leiden, 18, p. 9-30. (C Java Southern Mountains numerous Late Pleistocene- Holocene, Paleolithic- Neolithic prehistoric sites) Simanjuntak, T. (2006)- Indonesia-Southeast Asia: climates, settlements, and cultures in Late Pleistocene. Comptes Rendus Palevol 5, p. 371-379. (Late Pleistocene period between Paleolithic culture and E Holocene Preneolithic culture, marked by climate and sea level fluctuations and appearance of modern human (oldest Homo sapiens), replacing H. erectus) Simanjuntak, T., B. Prasetyo & R. Handini (eds.) (2001)- Sangiran: man, culture and environment in prehistoric times. Yayasan Obor Indonesia, Jakarta, p. 1-443. (Collection of papers on Sangiran hominid site, C Java, presented at 1st Int. Colloquium on Sangiran, Solo 1998) Simanjuntak, T. & F. Semah (1996)- A new insight into the Sangiran flake industry. In: The Chiang Mai papers, 1, Indo-Pacific Prehistory Assoc. Bull. 14, p. 22-26. (online at: http://journals.lib.washington.edu/index.php/BIPPA/article/view/11584/10215) (Flake tools made of chalcedony, jasper, etc., and supposedly made by Homo erectus, first discovered by Von Koenigswald in 1936. Flakes can be found throughout Kabuh Fm at Negung, NW Sangiran Dome, C. Java) Simanjuntak, T., F. Semah & C. Gaillard (2010)- The Palaeolithic in Indonesia: nature and chronology. Quaternary Int. 223-224, p. 418-421. (Brief review of Indonesian ‘older’ Paleolithic stone tool assemblages. Human presence on Java dates back to ~1.5 Ma, but no stone tools known older than ~1.0 Ma) Soares, P., J.A. Trejaut, J.H. Loo, C. Hill, M. Mormina et al. (2008)- Climate change and postglacial human dispersals in Southeast Asia. Molecular Biol. Evol. 25, 6, p. 1209-1218. (Modern humans in Island SE Asia since at least 50,000 years, commonly thought to be from Neolithic dispersal from China. Genome sequencing of modern humans suggest migration of humans from Sundaland across region since start of Holocene, at time of Sundaland breaking up into archipelago by rising sea levels) Soerastopo Hadisoemarno (1972)- Geomorphology of the Sangiran dome, Java, Indonesia. Ilmu Alam, 1, p. 57- 65. (in Indonesian) Soergel, W. (1914)- Stegodonten aus den Kendengschichten auf Java. Palaeontographica Suppl. 4, 3, 1, p. 1-24. ('Stegodont elephants from the Kendeng beds on Java'. On Pleistocene Stegodont elephant teeth collected by Elbert) Sondaar, P.Y. (1981)- The Geochelone faunas of the Indonesian Archipelago and their paleogeographical and biostratigraphical significance. Modern Quaternary Research in Southeast Asia 6, Balkema, Rotterdam, p. 111- 120. Bibliography of Indonesia Geology , Ed. 5.1 418 www.vangorselslist.com March 2014 (E Pleistocene giant tortoise Geochelone atlas known from Java (Sangiran, Kali Klagah), Sulawesi and Timor. Probably part of island faunas, which became extinct with arrival of Asiatic mamals via land bridge in E Pleistocene. (see also critical discussion by Hooijer 1982)) Sondaar, P.Y. (1984)- Faunal evolution and the mammalian biostratigraphy of Java. In: P. Andrews & J.L. Franzen (eds.) The early evolution of man with special emphasis on Southeast Asia and Africa. Courier Forsch. Inst. Senckenberg 69, p. 219-235. (Re-interpretation of Java fossil mammal successions, linked to changes in paleobiogeography. Seven Late Pliocene- Pleistocene vertebrate faunas, from old to young: Satir (early island fauna), Ci Saat, Trinil HK (with arrival of Homo erectus), Kedung Brubus, Ngandong, Punung and Wajak faunas) Sondaar, P.Y. (1987)- Pleistocene man and extinctions of islands endemics. Mem. Soc. Geologique France, N.S., 150, p. 159-165. Sondaar, P.Y. (1989)- Did man reach Australia via the giant rat and Dingo route? Geol. Res. Dev. Centre (GRDC), Bandung, Seri Paleontologi 5, p. 76-83. (Discussion of possible routes followed by Pleistocene man from China to Australia) Sondaar, P. (1994)- De Homo erectus fauna’s van Java. Cranium 11, 2, p. 92-96. Sondaar, P.Y., F. Aziz, G.D. van den Bergh & J. de Vos (1996)- Faunal change and hominid evolution during Quaternary of Jawa. Geol. Res. Dev. Centre (GRDC), Bandung, Seri Paleontologi 8, p. 1-10. (Quaternary vertebrate assemblages, from old to young: Satir (unbalanced island fauna), Cisaat, Trinil, Kedung Brubus, Ngandong, Punung and Wajak. Homo erectus in several different stratigraphic levels) Sondaar, P.Y., J. de Vos & J.J.M. Leinders (1983)- Reply. Facts and fiction around the fossil mammals of Java. Geologie en Mijnbouw 62, p. 339-343. (Discussion of Bartstra (1983) critique of De Vos, Sartono et al. (1982) reinterpretation of relative ages of mammalian faunas of Trinil and Kedungbrubus of Java. See also Hooijer and Kurten 1984) Sondaar, P.Y., G.D. van den Bergh, J. de Vos & F. Aziz (1995)- Homo erectus in S.E. Asia: time space and migration routes, IV. Overseas traveling of Homo erectus and faunal turnovers. In: J. Gibert et al. (eds.) Proc. Int. Conf. The hominids and their environment during the Lower and Middle Pleistocene of Eurasia, Orce 1995, p. 383-388. (Homo sapiens generally believed to be first to cross water barriers. Stone tools of 0.7 Ma age on Flores suggest Homo erectus probably also had this capability) Sondaar, P.Y., G.D. van den Bergh, J. de Vos & F. Aziz (2001)- The Flores case: the earliest island colonizers. Geol. Res. Dev. Centre (GRDC), Bandung, Spec. Publ. 27, p. 15-19. Sondaar, P.Y., G.D. van den Bergh, B. Mubroto, F. Aziz, J. de Vos & U.L. Batu (1994)- Middle Pleistocene faunal turnover and colonization of Flores (Indonesia) by Homo erectus. Comptes Rendus Academie Sciences, Paris, II, 319, p. 1255-1262. (Artifacts associated with fossil Stegodon tigonocephalus florensis Hooijer and fresh water molluscs in fluvial sands of Ola Bula Fm near Mata Menge, W Central Flores dated as slightly older than 0,73 Ma, were probably made by Homo erectus) Spriggs, M., C. Reepmeyer, Anggraeni, P. Lape, L. Neri, W.P. Ronquillo, T. Simanjuntak et al. (2011)- Obsidian sources and distribution systems in Island Southeast Asia: a review of previous research. J. Archaeol. Sci. 38, p. 2873-2881. (Review of distribution and origin of stone age obsidian artifacts in Philippines, Sulawesi, Flores, W and E Java, S Sumatra, Borneo and E Timor. Many were probably sourced from islands on which they were found) Bibliography of Indonesia Geology , Ed. 5.1 419 www.vangorselslist.com March 2014 Stehlin, H.G (1925)- Fossile Saugetiere aus der Gegend von Limbangan (Java). Dienst Mijnbouw Nederlandsch-Indie, Wetenschappelijke Mededeelingen 3, p. 1-12. (‘Fossil mammals from the Limbangan area, Java’. Diverse Pleistocene mammal assemblage in conglomeratic sandstone near Limbangan, Brebes District, Pekalongan Residency, C Java) Storm, P. (1995)- The evolutionary significance of the Wajak skulls. Scripta Geologica 110, p. 1-247. (online at: www.repository.naturalis.nl/document/148692) (Two Late Pleistocene- Holocene robust hominid skulls from Gua Wajak, SE Java, first described by Dubois (1922). Most likely interpretation as Mesolithic robust representatives of present Homo sapiens of Java.) Storm, P. (2001)- The evolution of humans in Australasia from an environmental perspective. In: R.A.C.Dam & S. van der Kaars (eds.) Quaternary environmental change in the Indonesian Region. Palaeogeogr., Palaeoclim., Palaeoecology 171, p. 363-383. (Incl. climatic sequence for Java: before and around 135 ka climate considerably drier and hot; between 126- 81 ka mainly humid-warm (with Punung fauna), becoming drier and cooler (with Wajak fauna) before returning to more interglacial conditions in Holocene) Storm, P. (2012)- A carnivorous niche for Java Man? A preliminary consideration of the abundance of fossils in Middle Pleistocene Java. Comptes rendus Palevol 11, p. 191-202. (Anatomical and archaeological aspects of Homo erectus suggest vertebrates meat was important part of diet) Storm, P., F. Aziz, J. de Vos, D. Kosasih, S. Baskoro, Ngaliman & L.W. van den Hoek Ostende (2005)- Late Pleistocene Homo sapiens in a tropical rainforest fauna in East Java. J. Human Evolution 49, 4, p. 536-545. (Redescription of two original sites of 'Punung fauna', as first described by Von Koenigswald (1939) and Badoux (1959) from karst hills of S Mountains, E Java. Punung and new nearby mammal site Gunung Dawung reflect tropical rainforest environment with common Pongo (orangutan) fossils. Punung fauna younger than Ngandong, possibly around 100 ka) Storm, P. & J. de Vos (2006)- Rediscovery of the Late Pleistocene Punung hominin sites and the rediscovery of a new site Gunung Dawung in East Java. Senckenbergiana Lethaea 86, 2, p. 121-131. (On re-location of Von Koenigswalds's Punung sites where in 1930s he collected hominin remains and mammals indicating presence of tropical rainforest like orang-utans (Pongo) and gibbons (Hylobates)) Storm, P. & A.J. Nelson (1992) - The many faces of Wajak Man. Archaeology in Oceania 27, p. 37-46. Storm, P., R. Wood, C. Stringer, A. Bartsiokas, J. de Vos, M. Aubert, L. Kinsley & R. Grun (2013)- U-series and radiocarbon analyses of human and faunal remainsfrom Wajak, Indonesia. J. Human Evolution 64, p. 356- 365. (Radiometric dating of human and faunal bone fragments from Wajak, Java, indicate minimum age of 37.4- 28.5 ka, significantly older than previously published radiocarbon estimates, probably due to secondary carbonatisation. Requires reassessment of evolutionary relationships of human remains in SE Asia- Oceania) Stremme, H. (1911)- Die Saugetiere mit Ausnahme der Proboscidier. In: M.L. Selenka & M. Blanckenhorn (eds.) Die Pithecanthropus-Schichten auf Java, geologische und palontologische Ergebnisse der Trinil Expedition (1907 und 1908), W. Engelmann, Leipzig, p. 82-150. (Description of mammals, not including elephants, from Pleistocene of Trinil area, from material collected by Selenka expedition, 1907-1908) Sudijono, K. Mano & R. Wikarno (eds.) (1995)- Geology of the Quaternary environment of the Solo-Madiun area, Central-East Java. Geol. Res. Dev. Centre (GRDC), Bandung, Spec. Publ. 17, p. 1-128. Suminto, J. Kimura & T. 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Quaternary geology of the hominid fossil bearing formations in Java, Geol. Res. Dev. Centre, Spec. Publ. 4, p. 309-357. (Eight radiometric ages obtained from 21 pumice tuff layers and 2 javites of Pleistocene of Sangiran. Tuffs from Pucangan Fm 1.16 Ma and Kabuh Fm 0.71- 0.78 Ma). Javites 0.71 Ma) Swisher, C.C., G.H. Curtis, T. Jacob, A.G. Getty, A. Suprijo & Widiasmoro (1994)- Age of the earliest known hominids in Java, Indonesia. Science 263, p. 1118-1121. (40Ar/39Ar ages from pumice from Mojokerto hominid sites 1.81 and 1.66 Ma, 0.6 million years older than Homo erectus fossils from Olduvai Gorge, and comparable to age of H cf. erectus (H. ergaster) in Kenya. Ages would suggest Homo erectus may have evolved in Asia instead of Africa (NB: these Java age dating results widely disputed in subsequent literature due to erroneous locality information (Huffman et al. 2006, etc.)) Swisher, C.C., G.H. Curtis & R. Lewin (2000)- Java Man- how two geologists’ dramatic discoveries changed our understanding of the evolutionary path to modern humans. Scribner, New York, p. 1-244. (Popular account of events leading to new conclusions on human evolution. (This ‘dramatic' but highly controversial relatively old age dating of Mojokerto hominids probably based on erroneous location information) Swisher, C.C., W.J. Rink, S.C. Anton, H.P. Schwartz, G.H. Curtis & A. Suprijo (1996)- Latest Homo erectus of Java; potential contemporaneity with Homo sapiens in Southeast Asia. Science 274, p. 1870-1874. (Hominid fossils from Ngandong and Sambungmacan considered the most morphologically advanced Homo erectus. Dating of fossil bovid teeth collected from hominid-bearing levels gave mean ages of 27 to 53 ka, much younger than previous age estimates for these hominids) Tassy, P., P. Anupandhanant, L. Ginsburg, P. Mein, B. Ratanasthien & V. 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