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Peaks of deepsea taxa like Krithe, Bradleya, Cytheropteron, Acantocythereis and Ambocythere related to changes in paleoproductivity. Other peak with mixed shallow-water Paracytheridea, Quadracythere, Loxocorniculum, Neonesidea and deep-sea taxa suggest downslope transport of sediments, possibly regressive events Dewi, K.

IAGI , Bandung , 1, p. Prabowo - Ostracoda perairan Utara P. Kangean: kaitannya dengan transpor sedimen. IAGI , 4, p. Bassinot, F. Guichard, Q.

Li, N. Fang, L. Labeyrie, R. Xin, M. Hardjawidjaksana - Distribution and ecology of planktonic foraminifera from the seas around the Indonesian Archipelago. Marine Micropal. Assemblages reflect sea-surface temperature, salinity, thermocline depth, and nutrient supply, related to circulation patterns. Strongest dissolution in Java upwelling region, with lysocline rising above m. Survey of Malaysia, Borneo Region, Bull. Frerichs, W. Cushman Found. Distribution of Recent planktonic foraminifera in sediments of Andaman Sea controlled by surface salinity, water depth, diagenesis and topography.

Large volumes of fresh water in N Andaman Sea result in lowering of surface salinity and exclusion of planktonic forams. Depth zonation: Sphaeroidinella and some Globorotalia species indicative of bathyal depths Fujita, K.

Osawa, H. Kayanne, Y. Yamano - Distribution and sediment production of large benthic foraminifers on reef flats of the Majuro Atoll, Marshall Islands. Coral Reefs 28, p. Estimates of sediment production by Large Benthic Forams, mainly Calcarina and Amphistegina, on reef flats of Pacific atolls. Calcarina density higher on windward sides Gastaldo, R. Palaios 11, 3, p. Three organic matter facies assemblages in Rajang River delta sediments Gastaldo, R. Staub - Water column and grab sample palynofacies assemblages from the Rajang River delta, Sarawak, East Malaysia.

Palynology 21, p. Glenn, E. Dissertation, University of Houston, p. Unpublished Glenn, E. McManus, L. Talaue, P. Glenn-Sullivan, E. Evans - The effects of time-averaging and taphonomy on the identification of reefal sub-environments using larger foraminifera: Apo Reef, Mindoro, Philippines.

Palaios 16, 4, p. Comparisons of live and dead assemblages show time-averaged assemblages, the product of taphonomic processes, more effective in delineating reefal subenvironments than do live assemblages. Robust calcarinids are in shallow seaward zones; free-living miliolids and small rotaliines in leeward zones. Planktonics and large thin rotaliines in fore reef Gremmen W. Gustiantini, L. Dewi, A. IAGI and 28th Ann. HAGI, Jakarta, 11p. Science in New Gunea 14, p. Haig, D. Royal Soc.

Australia 80, p. Recent foraminifera from m water depth at Exmouth Gulf: benthic and 6 planktonic species Haig, D. Hallock, P. Carbonate production rates by foram families Asterigerinidae, Calcarinidae, and Nummulitidae in Palau, W Caroline Islands: seaward reef flats up to 2.

Productivity on lagoonal reef slopes about one-fifth. In Hawaii, production rates much lower because of slower growth rates and absence of family Calcarinidae Hallock, P. Sen Gupta ed. Modern Foraminifera, Kluwer, Amsterdam , p. Glenn - Numerical analysis of foraminiferal assemblages: a tool for recognizing depositional facies in Lower Miocene reef complexes. Assigned to zone Te5, but more likely Lower Tf? Yajima - Checklist of Ostracoda from Southeast Asia.

University Museum, University of Tokyo, Bull. Short Pap. Tohoku Univ. Wrenn - Palynomorph distribution in modern tropical deltaic and shelf sedimentsMahakam Delta, Borneo, Indonesia. Palynology 34, p. Distribution of terrestrial palynomorphs in Mahakam Delta surface sediments from 12 depositional environments from head of delta to shelf edge can be explained by transport and depositional processes.

Amounts of marine palynomorphs foram linings, copepod eggs, dinocysts increases gradually offshore Harting, P. Contribution to the knowledge of the microscopic fauna and flora from the Banda Sea Early report on foraminifera, radiolaria, etc.

Sains Malaysiana 3, 2, p. Haseldonckx, P. Shallow Holocene peat near Pekan Nanas, Johore, with 47 pollen and spore types. Pollen profile shows succession from open swamp vegetation with mangrove influence to marginal peat swamp facies with river bank vegetation. Brief, general overview of pollen and spores, processing and application in determination of paleoenvironments. Australian Geogr. Studies 39, p. In: G. Paramananthan eds. Malaysia Bull. Families Tinoporidae, Rotaliidae, Nummulitidae, Amphisteginidae.

Siboga Expedition , Mon. Brill, Leiden, p. IV, p. Part III. Hofker, J. Bijdragen tot de Dierkunde 37, p. Highest diversity in NW part of bay. The foraminifera collected in and in the eastern part of the Indonesian Archipelago: Zool.

Hohenegger, J. Marine Ecol. Living larger foraminifer restricted to photic zone. Peneroplids in shallow-water from intertidal common Peneroplis to 40 m Dendritina, sandy substrates. Soritids subtidal, from reef moat down to 60 m. Amphisorus and Marginopora common down to 30 m, Parasorites in deeper parts of reef slope. Alveolinella in upper 40 m of reef slope. Amphisteginids in entire photic zone, with test flattening with increasing depth.

Calcarinids cling to firm substrates. Baculogypsina restricted to high energy reef flat regions. Calcarina similar facies, extending to fore reefs down to 80 m. Baculogypsinoides dominant calcarinid genus from 30 m depth. Heterostegina prefers hard substrates on reef slope.

Operculina frequent in deeper part, independent of substrates. Sandy bottoms from 60 m are inhabited by Nummulites Operculina venosus. Cycloclypeus restricted to fore reef areas below 50 m down to base of photic zone Hohenegger, J. Papers, Kagoshima Univ.

Pacific Isl. Good overview of depth distribution modern larger benthic forams in W Pacific Hohenegger J. Hohenegger J. Paleobiology 32, 1, p. Yordanova - Depth-transport functions and erosion-deposition diagrams as indicators of slope inclination and time-averaged traction forces: applications in tropical reef environments.

Sedimentology 48, p. Yordanova - Displacement of larger foraminifera at the western slope of Motobu Peninsula Okinawa, Japan. Palaios 16, p. Heterostegina depressa broad range in light intensities and is protected against irradiation by thick tests and cryptic life mode near surface. Test construction enables life under strong hydrodynamic regimes. Lives firmly attached to hard substrates, thus counteracting transportation by water movement.

Nummulites venosus lives exclusively on coarse sand and avoids high sediment movement, starting distribution beneath fair weather wave base. Cycloclypeus carpenteri easily transported due to thin, plate-like form. Upper distribution limit correlates with storm wave base, below 50 m. Lower distribution limit depends on light intensity and is near base photic zone Hohenegger J. Yordanova, Y. Tatzreiter - Habitats of larger foraminifera on the upper reef slope of Sesoko Island, Okinawa, Japan. Peneroplis common on reef flat, hardgrounds down to 30 m.

Dendritina on sandy bottoms avoids uppermost slope, found down to 50 m. Alveolinella similar distribution, common on hard bottom. Parasorites restricted to sandy substrates, m. Sorites and Amphisorus firm substrates between reef edge and 50 m. Amphistegina species prefer hardgrounds, A. Calcarinids withstand high energy, abundant on firm substrates close to reef edge.

Baculogypsinoides deeper slope, sandy bottom, avoids shallowest parts. Hard substrates settled by Heterostegina down to 80 m, occasionally on sandy bottoms. Nummulites on sands between 70 m. Operculina, starting at 20 m, sandy substrates, rare individuals on rubble Ho Kiam Fui - Distribution of recent benthonic foraminifera in the inner Brunei Bay. The Brunei Mus.

Three foraminifera assemblage in nearly landlocked Brunei Bay: 1 Trochammina cf. Culver, M. Hardbattle, P. Larcombe, G. Milne et al. Samples behind barrier reef with water depths from 4. Two foraminiferal zones: inner shelf with Elphidium hispidulum, Pararotalia venusta, Planispirinella exigua, Quinqueloculina venusta and Triloculina oblonga; and middle shelf dominated by Amphistegina lessonii, Dendritina striata and Operculina complanata Horton, B.

Larcombe, S. Woodroffe, J. Whittaker, M. Wynn - Contemporary foraminiferal distributions of a mangrove environment, Great Barrier Reef coastline, Australia: implications for sea-level reconstructions.

Modern foraminifera and associated environmental information from Cocoa Creek, a mesotidal fringing mangrove environment on Great Barrier Reef. Three elevational zones.

Zones I highest and II dominated by agglutinated species Trochammina inflata and Miliammina fusca, respectively; and Zone III lowest dominated by calcareous species, notably Ammonia tepida and Elphidium discoidale multiloculum. These assemblage zones similar to those found in both tropical and temperate intertidal environments Horton, B. Whittaker, K. Thomson, M. Hardbattle, S. Wright - The development of a modern foraminiferal data set for sea-level recontructions, Wakatobi Marine National Park, Southeast Sulawesi, Indonesia.

Foraminiferal Res. Intertidal foraminifera from Tukang-Besi islands. Agglutinated species like Arenoparella mexicana, Miliammina fusca and Trochammina inflata most common at landward margin, and small calcareous species Ammonia tepida, Elphidium advanum and Quinqueloculina dominant at seaward margin of mangrove belt Horton, B.

Zong, C. Engelhart - Diatoms from Indonesian mangroves and their suitability as sea-level indicators for tropical environments. Modern diatoms from mangrove swamps of Tukang Besi islands collected for environment reconstructions in tropical environments. Mixed mesohalobous, oligohalobous-halophilous and oligohalobous-indifferent diatoms in mangrove vegetation, mesohalobous assemblages in fringing Rhizophora and tidal flat environments Howe, H. Northern Territory Mus.

Arts Sciences, Mon. Hughes, G. Amphistegina lessoni and Heterostegina depressa two most common species in all samples Hughes, G. Increase in abundance and diversity between ,m associated with regional oxygen-maximum zone between m and m and a salinity-minimum zone below m Hustedt, F. Band 15, p. Distribution of nannoplankton and foraminifera in 26 shallow marine surface sediment samples from Madura Strait and 24 samples from open marine water N of Madura Isnaniawardhani, V. Suparka, R.

Latief - Nannoplankton and foraminifera assemblages and their relations to bathymetry in Madura waters. In: Eighth Int. Pacific Neogene Stratigraphy, Chiang Mai , p.

Jell, J. McKellar - The significance of the larger foraminifera in the Heron Island reef sediments. Jian Z. Wang, M. Kienast, M. Sarnthein, W. Kuhnt, H. Wang - Benthic foraminiferal paleoceanography of the South China Sea over the last 40, years.

Jones, R. Oxford University Press, p. Updated taxonomy and reproductions of foraminifera from H. Foram distributions in 96 samples of coastal sediments down to 3m depth along E coast India. Kawamura, H. Doctor Diss. Christian-Albrechts-University, Kiel, p. Keij, A. Malaysia Geological Survey , p. Distinct increases in relative abundance of Orbulina, Pulleniatina, Globorotalia menardii below m. Globorotalia truncatulinides, Gr.

Micropaleontology 12, 3, p. Discussion of distribution of 4 species of Miocene- Recent ostracode genus Paijenborchella in Brunei, CebuPhilippines, etc. B 78, p. B 82, p. Thesis Univ. Leiden, Brill, 79 p. Measuremments on selected modern foraminifera species from coasts of Java, Bali, Madura. Khare, N.

Mazumder - An overview of foraminiferal studies in nearshore regions off eastern coast of India, and Andaman and Nicobar Islands. Indian J. Marine Sci. Science Repts. Tohuku University, ser. Common on outer reef slopes, and confined by the m isobath.

Not present in pelagic environments, reef banks, lagoons or bays. In Recent samples found between m depth, but clear abundance peak around 90m Lambert, B. Micropalaeontology 11, 1, p. Langer, M. General trend in Recent benthic foraminifera from Madang Lagoon of depletion in heavier C and O isotopes, with depth appears to be depth- and light-dependant Langer, M.

Hottinger - Biogeography of selected 'larger' foraminifera. Micropaleontology 46, Suppl. Coral Reefs 22, p. LeRoy, L. De Ingen. Indie IV 5, 8, p. Lipps, J. Science in New Guinea 11, p. Lobegeier, M. Calcarina mayori smaller and dominates in deeper water off reef flat.

Baculogypsina sphaerulata is shallow water high-energy species. Cushman Foundation Spec. Lloyd, A. In: O. Endean eds. Biology and geology of coral reefs, 1, Academic Press, New York, p. Loeblich, A. Recent foraminifera from Timor Trough and Sahul Shelf, collected in Mainly species descriptions Maloney, B.

World Archaeology 24, 1, p. Kelman, R. Laurie - Australian biozonation chart Geoscience Australia, Canberra. Anwar - Calibration of tropical Pacific marine sediment indices d18O to sea surface temperature. McCloskey, B. Thesis University of South Florida, p. Violanti - Foraminiferal biodiversity and Holocene evolution of the Phetchaburi coastal area Thailand Gulf.

Area characterized by inflow of Mae Khlong river. Typical low diversity brackish-water faunas. Four assemblages, with salinity fluctuation controlling factor Miao, Q. Miao, Q. Thunell - Late Pleistocene-Holocene distribution of deep-sea benthic foraminifera in the South China Sea and Sulu Sea- palaeoceanographic implications. Millett, F. Royal Microscopical Society,. Reprinted by Antiquariaat Junk, Lochem 17 papers on foraminifera from sample collected by A.

Venec-Peyre - Shallow-water foraminiferal taphocoenoses at Site implications for the Pleistocene evolution of the central Great Barrier Reef shelf, Northeastern Australia. In: J. McKenzie et al. Ocean Driling Program, Sci. Morley, A. In: R. Noble et al.

Mostafawi, N. Senckenbergiana Lethaea 72, p. Babinot - An account on the taxonomy of ostracodes from recent reefal flat deposits in Bali, Indonesia. Muller, J. In: Symposium on ecological research in humid tropics vegetations, Kuching, Sarawak. Murphy, S. MS thesis, Southern Illinois Univ. Newsome, J. Palaeopalynology and vegetational history. Biogeography 15, p. O'Neill, M. Oostingh, C.

Landbouwhoogeschool Wageningen 26, 3, Verhand. Archiv Molluskenkunde 63, , p. Listings of recent molluscs from southernmost Sumatra, along Sunda straits Palmieri, V. Panchang, R. Recent benthic foraminiferal distribution on Ayeyarwaddy Delta Shelf off Myanmar shows Asterorotalia trispinosa has preference for low salinity.

Variations in abundance used as proxy for delineation of past wet and dry periods: dry climate prior to AD and warm and wet climate since to present Parker, J. Australasian Palaeont. Parker, J. Gischler - Modern foraminiferal distribution and diversity in two atolls from the Maldives, Indian Ocean. Two coral-reef lagoons comprise eight foraminifera assemblages with species. Three assemblages reefal and dominated by Amphistegina and Calcarina. One lagoon assemblage with abundant Ammonia and smaller miliolids.

Jian - Modern distribution patterns of planktic foraminifera in the South China Sea and Western Pacific: a new transfer technique to estimate regional sea-surface temperatures.

Polhaupessy, A. Centre, Bandung, Bull. Post, A. Sbaffi, V. Greene eds. Mapping the seafloor for habitat characterization, Geol. Canada, Spec. Three areas different benthic foram assemblages. High relict content in surface samples. Pudjoarinto, A. Palynology of 18m core from small lake in Dieng Plateau, C Java. Montane forest assemblages record climate changes Rasheed, D. Madras Univ. B, p. Rasheed, D. Rasheed D. B , p. Madras University B, p. Rathburn, A.

Corliss - The ecology of living stained deep-sea benthic foraminifera from the Sulu Sea. Paleoceanography 9, p. Corliss, K. Lohmann - Comparisons of the ecology and stable isotopic compositions of living stained benthic foraminifera from the Sulu and South China Seas.

Deep Sea Res 1, 43, 10, p. Differences result from large differences of bottom-water temperatures Renault-Miskovsky, J. Semah - Palynology of the Quaternary in temperate and ropical areas: chronostratigraphy, palaeoclimatology and vegetal environment of fossil man.

In: N. Dutta et al. Current concepts in pollen-spore and biopollution research S. Chandra volume , Research Period. House, Houston, p. Renema, W. Recent larger foraminifera from Bali total 19 species. Species richness similar to SW Sulawesi and Cebu, but different composition. Schlumbergerella locally abundant and geographically restricted to Lesser Sunda Islands and Java.

Very low abundance of imperforate species probably due to climatic or oceanographic parameters, most likely periodic upwelling, which causes seasonal seawater temperature drops Renema, W. Lethaia 38, p. Increased turbulence thickens the test, whilst decreased light intensity causes flatter test. Modern large benthic forams on Berau shelf two- three depth-controlled assemblages: shallow m; dominated by Operculina ammonoides and deeper m; dominated by Operculina complanata and Planostegina operculinoides.

Deepest living LBF at m. Cycloclypeus carpenteri between m Renema, W. Coral Reefs 25, 3, p. Composition of Larger foram assemblages on Berau carbonate shelf with a barrier reef system and some reefs outside barrier.

Four clusters corresponding to substrate type Renema, W. Coral Reefs 29, p. Reefal habitats dominated by algae are inhabited by specific group of larger foraminifera, Calcarinidae Renema, W, B. Distribution patterns of 20 species of larger benthic foraminifera in Spermonde Archipelago, off SW Sulawesi.

Substrate type, hydrodynamic energy, light intensity, nutrient availability and environmental stabiltity determine distribution Renema W. Hohenegger - On the identity of Calcarina spengleri Gmelin Commonly confused with Calcarina mayori Cushman , C. Troelstra - Larger foraminifera distribution on a mesotrophic carbonate shelf in SW Sulawesi Indonesia.

Modern larger foram distribution on Spermonde Shelf Robles, E. Masters Thesis Mus. Paris, p. IAGI , Jakarta , p. On Calcarina larger foram in Recent reefal limestone deposits Rositasari, R. Susana - Tipe estuari sebagai faktor pembatas pada komunitas foraminifera; hasil penelitian di Muara Sungai Ciawi dan Muara Sungai Bekasi. Schubert, R. Anzeiger 23, p. Recent shallow marine foraminifera from calcareous sand from Singapore. Fauna dominated by miliolids Severin, K.

Science in New Guinea 10, p. Shafik, S. Stuijts, I. Modern Quat. Southeast Asia 8, p. Thesis Universiteit Groningen, Balkema, Rotterdam. Southeast Asia 12, p.

Suhartati M. Toyama Univ. Most abundant species Ammonia beccarii, Calcarina calcar and Elphidium advenum. In: S. Sudara et al. Living Coastal Resources, Bangkok, 2, p. Dominant species in reef-flat seagrass areas are miliolids Quinqueloculina spp. Also common Ammonia beccarii, Calcarina calcar, Elphidium spp.

Reopical Biodiversity 5, 1, p. Lingkungan Tropis 3, 2, p. Distribution and abundance of Recent benthic foraminifera in Opak Besar, Seribu islands'. Indonesia 36, 2, p. Dominant symbiont bearing foraminifera are Amphistegina, Calcarina and Tinoporus.

Natsir - Kelimpahan foraminifera Resen pada sedimen permukaan di Teluk Ambon. EJurnal Ilmu Tekn. Kelautan Tropis 2, 1, p. Ilmu Tekn. Kelautan Tropis 2, 2, p. Arafura Sea shallow waters S of Papua. Shallow-water ecosytems such as mangrove, seagrass bed, and coral reefs. Samples mainly beteen m, deepest is station 13 at m. Benthic foraminifera in.. Media Teknik UGM 13, 2, p. Bachtiar - Quaternary benthic foraminifera from bathyal zone seabed of mamuju offshore, North Makassar Basin, West Sulawesi.

Benthic foraminifera from m depth, sampled during geohazard survey, offshore, Lariang Basin. Mainly calcareous benthics usually found in outer shelf- upper bathyal instead of arenaceous tests that are common in bathyal zone. This suggests deposition is allochtonous sediment debris from upslope Sumawinata, B. Southeast Asian Studies, Kyoto 36, 3, p. Luo, F. Huang, J. Szarek, R. Thesis, Christian Albrechts Univ. Recent benthic foraminifera distribution around Natuna Island between m. Taylor, A. Magister Dissertation, University of Wales, Aberystwyth, p.

Unpublished Titterton, R. Titterton, R. Whatley - Recent marine Ostracoda from the Solomon Islands. Part 2. Cytheracea Xestoleberidae. Micropaleontologa, 37 2 , Part 1: Cypridoidea, Platycopina and Cladocopina. Both first appeared late in Tertiary. Troelstra, S. Scripta Geol. Near-reef facies dominated by few species Calcarina, Elphidium. Mid-shelf reefs mainly with Heterostegina depressa and Amphistegina radiata.

Outer platform reefs more open ocean influence with Amphisorus hemprichii and Amphistegina lessonii Van de Paverd, P. Bjorklund - Frequency distribution of polycystine radiolarians in surface sediments of the Banda Sea, Eastern Indonesia.

Numbers of radiolarians in sea-floor sediments of Banda Sea vary widely: low from 0- m, high between m, and low again below m water depth. Distribution pattern result of sediment influx and occurrence of highly productive areas in surface water Van der Kaars, W. Van der Kaars, S. Palaeoclimates 3, p. Bassinot, P.

Guichard - Monsoon and ocean circulation and the vegetation cover of southwest Sumatra throughout the last 83, years: the record from marine core BAR Palynological record from deep-sea core off SW Sumatra used to reconstruct monsoon circulation and vegetation of SW Sumatra over the last 83 ky.

Dam - A ,year record of vegetational and climatic change from the Bandung area, West-Java, Indonesia. Dam - Vegetation and climate change in West-Java, Indonesia during the last , years.

Penny, J. Tibby, J. Fluin, R. Suparan - Late Quaternary palaeoecology, palynology and paleoclimatology of a tropical lowland swamp: Rawa Danau, West-Java, Indonesia.

Open vegetation and drier climate suggested for Late Glacial, but no evidence for cooler conditions. Onset of Holocene coincides with change to more humid conditions Van der Kaars, S. Williams, F. Moreno - The influence of the 73 ka Toba super-eruption on the ecosystems of northern Sumatra as recorded in marine core BAR Evidence for impact on regional climatic conditions remains inconclusive Van Iperen, J.

Marine diatoms from 53 seafloor samples between m water depth in Indonesian Archipelago. Three significant assemblages, related to parameters of overlying water mass: 1 related to warm saline surface waters of Pacific and Indian Ocean origin; 2 low-salinity lobe in Makassar Strait; 3 seasonal upwelling areas in Arafura Sea and S of Java.

Also three groups of allochthonous species, indicators of productivity in littoral environment, bottom currents and river outflow Van Marle, L. Study of distribution of species of benthic foraminifera in 35 seafloor samples from Australia- Irian Jaya continental margin between m water depth, along three transects across Banda Arc. Four fauna1 depth-zones and four subzones distinguished Van Marle, L.

Collection of 11 papers also published elsewhere on modern foraminifera distribution and Neogene stratigraphy of E Indonesian islands Van Marle, L. Nederbragt - Plankton percentage of the foraminiferal fauna in seafloor samples from the Australian-Irian Jaya continental margin, Eastern Indonesia. Marine Geol, 77, p. Plankton percentage of foram fauna in 36 seafloor samples between m depth from Australian-Irian Jaya continental margin increases with water depth.

Percentage- Depth Transform derived from data set. Van Waveren, I. Mix of open marine foraminifera, dinoflagellates and land-derived material spores-pollen, etc. Thesis University of Utrecht, Geol. Ultraiectina , p. Collection of seven publications, six of which deal with Recent Banda Sea palynomorphs, organic matter, tintinnomorphs and dinoflgellate cysts Van Waveren, I. Visscher - Analysis of the composition and selective preservation of organic matter in surficial deep-sea sediments from a high-productivity area Banda Sea, Indonesia.

Palynological analysis of box-core samples from deep-sea sediments along three transects in Banda Sea Van Zeist, W. Villain, J. In: M. Gayet et al. Foraminifera distribution on shelf between Mahakam delta and Makassar Strait. Deltaic assemblages arranged according to salinity. Inner shelf with larger Rotaliidae towards euryhaline conditions.

Operculina typical of shallow marine low-oxygen organic-rich clays, coarser seafloor rich in oxygen with Amphisteginids. Nodosariidae and planktonics bathymetric markers on slope.

Bathyal areas mostly agglutinants. Model above valid only for highstand situations, comparable to present day. Sediments deposited during last lowstand period cored and correlated. Shelf microfaunas thin-walled, due to low oxygen and low carbonate concentrations; Rotaliidae indicate low salinities at shelf edge, where they coexist with Operculina and Amphistegina, close to deeper facies with planktonics, Buliminidae and Nodosariidae Watson, K.

Unpublished Wells, P. Wells, J. Whatley, R. Whittaker, J. Hodgkinson - The foraminifera of the Pitcairn Islands. Linnean Soc. Recent foraminifera from Pitcairn Islands, Pacific Ocean. Living forams almost exclusively from phytal attached or clinging habitats. Foraminifera in sediment samples mainly thanatocoenoses. Fauna all calcareous, low diversity, dominated by large soritids [Marginopora, Amphisorus, Sorites and Amphistegina, with small miliolids and small attached genera discorbids, etc.

Apparent absence of Calcarina, small rotaliids, elphidiids and agglutinating species, common in W Pacific islands Wijono, S. Papateo, Kepulauan Seribu, Laut Jawa. Forams from 18 samples from m depth Woodroffe, S. Horton, P. Whittaker - Intertidal mangrove foraminifera from the central Great Barrier Reef shelf, Australia: implications for sea-level reconstruction.

Foraminifera distribution in intertidal zone tied to elevation. Joint Prosp. Mineral Res. Rahardjo, Dardji Noeradi, D. Hirakawa - A Holocene pollen record of vegetation and coastal environmental changes in the coastal swamp forest at Batulicin, South Kalimantan, Indonesia.

Asian Earth Sci. Sukapti, A. Siregar, P. Hirakawa Mangrove shoreline responses to Holocene environmental change, Makassar Strait, Indonesia.

Mangroves developed at Batulicin in mid-Holocene, persisting to present at Batulicin. Micropaleontology 35, p. Zong, Y. Kamaludin - Diatom assemblages from two mangrove tidal flats in Peninsular Malaysia. Diatom Research 19, p. Tertiary Adams, C. London , p. One new genus, Wilfordia, three new species: Dictyoconus melinauensis, Neoalveolina inflata, and Wilfordia sarawakensis. Dictyoconus recorded for first time from strata of Oligocene age Adams, C.

In: C. Ager eds. British Mus. In: A. Hallam ed. Atlas of Palaeobiogeography. Elsevier, Amsterdam, p. Larger foram faunas similar between Mediterranean and Indo-West Pacific, but different from Americas. From M Miocene onward diverged rapidly Adams, C. Mediterranean Neogene, Athens , Ann. Pays Hellen. No major changes in larger foram faunas distribution at Oligo-Miocene boundary.

Sims et al. The emergence of the biosphere, Syst. Adams, C. Tsuchi eds. Pacific Neogene datum planes, Contributions to biostratigraphy and chronology. Micropaleontology 33, p. Three subgenera, Lepidocyclina Lepidocyclina , L.

Eulepidina , and L. Nephrolepidina , discriminated on nature and arrangement of peri-embryonic chambers. Two groups of species recognized within L. Lepidocyclina on basis of equatorial chamber shape Adams C. Ingle eds. Pacific Neogene. University of Tokyo Press, Tokyo, p. Palaeontology 17, p. Once the program is installed, you can go to any working torrent site and start downloading. Magnet links are the easier of the two to use.

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