03199nas a2200157 4500008004100000245010100041210006900142260003200211520265700243100002402900700002002924700001702944700001802961700001902979856004302998 2013 eng d00aMicrobial carbonates in Miocene reefs in the Mahakam Delta in East Kalimantan, Borneo, Indonesia0 aMicrobial carbonates in Miocene reefs in the Mahakam Delta in Ea aBerlin, Germanyc11/03/20133 a

Microbial carbonates are deposits that form by the activity of bentic microbial communities. Microbialites usually form domical, columnar or conical structures and can have laminated, clotted, dendritic or homogenous macrofabric. They have a broad distribution and can grow in a variety of different environments such as hot springs, freshwater lakes, hypersaline lakes, reefs and other marine environments. This research focuses on microbialites associated to coral reefs. Coral patch reefs in the Miocene Mahakam Delta in East Kalimantan (Borneo, Indonesia) grew in shallow marine turbid waters. These patch reefs developed from delta front to deeper (prodelta) settings in areas with temporary reduced siliciclastic input. Langhian reef deposits are well exposed in limestone quarries in the Samarinda area and locally include microbial carbonates. Two different types of microbial carbonates have been found around Samarinda in two localities 2 km apart. These sections were logged in detail and 208 samples were collected. Meso and macrostructure of microbialites were identified at the outcrops. Thin sections from carbonate samples were examined under optical microscope and microfacies were classified using the Dunham (1962) and Embry and Klovan (1971) terms. The carbonate content was analyzed using Total Inorganic Carbon analysis, with 12% carbon as a standard for carbon calibration. In the northern section, microbialites occur as low-relief domes, up to 2 m wide and 0.5 m high, with internal lamination, developed around large coral fragments at the transition from reef deposits to fine-grained siliciclastics.
The second type of microbialites has been found in the southern locality as decimeter-scale nodules ("megaoncoids") formed around nuclei of large coral fragments. Small nodules were bound together into bigger nodules. Microbial micrite with laminated to digitated fabrics intergrew with coralline algae to form the thick covers of these "megaoncoids", which laterally change into coral boundstones. In both sections microbialites are not components of the reef framework. They grew around large coral fragments on the flanks of the patch reefs. The microbialites that form low relief domes developed on a nearly flat, stable seafloor seawards of the patch reef. The "megaoncoids" in the southern section formed as a result of downslope movement of coral fragments coated by microbialite/coralline algal crust. The steep slope at the flank of the patch reef favoured falling and overturning of encrusted corals and continued growth of microbial crusts on other sides of nodules.

1 aPretković, Vedrana1 aBraga, Juan, C.1 aNovak, Vibor1 aRösler, Anja1 aRenema, Willem uhttps://ipaeg.myspecies.info/node/206900528nas a2200109 4500008004100000245014400041210006900185260007300254100002300327700002500350856004300375 2014 eng d00aEstimating species durations and turnover in a hyperdiverse Neogene gastropod radiation - An insight into patterns of Cenozoic biodiversity0 aEstimating species durations and turnover in a hyperdiverse Neog a Gainesville, FloridabThe Paleontological Society Special Paper, 221 aTodd, Jonathan, A.1 aJohnson, Kenneth, G. uhttps://ipaeg.myspecies.info/node/206800563nas a2200145 4500008004100000245008900041210006900130260007300199100002500272700001700297700002300314700001900337700001800356856004300374 2014 eng d00aThirty years of field-based 'Big Paleontology' on Cenozoic shallow marine ecosystems0 aThirty years of fieldbased Big Paleontology on Cenozoic shallow  a Gainesville, FloridabThe Paleontological Society Special Paper, 221 aJohnson, Kenneth, G.1 aKlaus, James1 aTodd, Jonathan, A.1 aRenema, Willem1 aBudd, Ann, F. uhttps://ipaeg.myspecies.info/node/206700552nas a2200121 4500008004100000245013200041210006900173260007300242100002500315700001900340700002800359856004300387 2014 eng d00aOligocene and Miocene history of reef corals and coral reefs in eastern Borneo (East Kalimantan, Indonesia and Sabah, Malaysia)0 aOligocene and Miocene history of reef corals and coral reefs in  a Gainesville, FloridabThe Paleontological Society Special Paper, 221 aJohnson, Kenneth, G.1 aRenema, Willem1 aSantodomingo, Nadiezhda uhttps://ipaeg.myspecies.info/node/206602197nas a2200109 4500008004100000245011900041210006900160260003200229520176600261100001702027856004302044 2012 eng d00aGastropod associations as a proxy for seagrass vegetation in a tropical carbonate setting (San Salvador, Bahamas) 0 aGastropod associations as a proxy for seagrass vegetation in a t aCharlotte, North Carolina. 3 a

Seagrass ecosystems play an important role in sedimentation processes and nutrient cycling and support local biodiversity by providing food and shelter for numerous associated organisms. These ecosystems have been around since the Late Cretaceous. In order to understand their emergence in geological time and their response to past perturbations we have to be able to recognize seagrass communities in the fossil record. However, seagrass itself hardly fossilizes and therefore we are searching for indirect indicators to recognize ancient seagrass vegetation. In this contribution we review molluscan evidence for palaeo-seagrass settings. Indicator species are rare since the majority of seagrass associated molluscs occurs in other marine habitats as well. Furthermore, those habitats appear to be patchy, both spatial and temporal, resulting in mixed occurrences of seagrass and non-seagrass faunas. Often only the high abundance of certain mollusc groups and the general taxonomic composition of a fauna points to seagrass environments. However, the distribution of gastropod trophic guilds in species richness versus abundance data appears to yield patterns that may be very characteristic for the identification of fossil seagrass associated faunas. We are currently applying Indirect PaleoSeagrass Indicators (IPSI’s) to a number of fossil and modern shelly samples, both from seagrass and non-seagrass environments. We also briefly review potential sedimentary and geochemical IPSI’s as well as fossil groups different than molluscs. Identifying seagrass environments enables us to assess diversity trends in such ecosystems through time and to study their response over time intervals with major environmental and climate change.

1 aReich, Sonja uhttps://ipaeg.myspecies.info/node/206102246nas a2200121 4500008004100000245014000041210006900181260003200250520176600282100001602048700001702064856004302081 2012 eng d00aDiversity, abundance and taphonomic patterns across bivalve dead assemblages associated with sea grass beds, San Salvador, the Bahamas0 aDiversity abundance and taphonomic patterns across bivalve dead  aCharlotte, North Carolina. 3 a

Seagrass ecosystems play an important role in sedimentation processes and nutrient cycling and support local biodiversity by providing food and shelter for numerous associated organisms. These ecosystems have been around since the Late Cretaceous. In order to understand their emergence in geological time and their response to past perturbations we have to be able to recognize seagrass communities in the fossil record. However, seagrass itself hardly fossilizes and therefore we are searching for indirect indicators to recognize ancient seagrass vegetation. In this contribution we review molluscan evidence for palaeo-seagrass settings. Indicator species are rare since the majority of seagrass associated molluscs occurs in other marine habitats as well. Furthermore, those habitats appear to be patchy, both spatial and temporal, resulting in mixed occurrences of seagrass and non-seagrass faunas. Often only the high abundance of certain mollusc groups and the general taxonomic composition of a fauna points to seagrass environments. However, the distribution of gastropod trophic guilds in species richness versus abundance data appears to yield patterns that may be very characteristic for the identification of fossil seagrass associated faunas. We are currently applying Indirect PaleoSeagrass Indicators (IPSI’s) to a number of fossil and modern shelly samples, both from seagrass and non-seagrass environments. We also briefly review potential sedimentary and geochemical IPSI’s as well as fossil groups different than molluscs. Identifying seagrass environments enables us to assess diversity trends in such ecosystems through time and to study their response over time intervals with major environmental and climate change.

1 aCecares, B.1 aReich, Sonja uhttps://ipaeg.myspecies.info/node/206002508nas a2200133 4500008004100000245009600041210006900137260002200206520204200228100001802270700002202288700001902310856004502329 2013 eng d00aSub - annually resolved Miocene/Pliocene tropical palaeo - climate records from giant clams0 aSub annually resolved MiocenePliocene tropical palaeo climate re aBarcelonabSitges3 a

Changes in seasonality play an important role in regards to climate changes (e.g. Eldrett
et al.,
2009). To better characterize Miocene/Pliocene tropical climate and environmental change, it is
therefore crucial to reconstruct their variability on a seasonal scale. However, highly time resolve
d
palaeoenvironmental records which allow assessing
tropical intra
-
annual SST variability (like
ENSO or monsoon events) are rare, especially in 'deep
-
time'.
Here, we present high resolution
trace element and stable isotope proxy records from well
-
preserved aragonitic Late Miocene and
Pliocene
Tridacna
spp.
shells, sampled along the coast of East Kalimantan (Indonesia) and Sabah
(Malaysia), respectively. Our multi
-
proxy approach utilizes LA
-
ICPMS El/Ca ratios (e.g. Mg/Ca,
Sr/Ca, Ba/Ca) and micromilled stable isotope profiles (
δ
18
O,
δ
13
C).
Records obtained fr
om our
Miocene specimens show a remarkable agreement in Mg/Ca, Sr/Ca and
δ
18
O and can be aligned
with the shell banding pattern.
δ
18
O intra
-
annual variability indicates a palaeoseasonality of 3
-
4°C
(if interpreted as being temperature
-
controlled only). Ba/
Ca profiles from Pliocene tridacnin shells
are characterized by pronounced, episodically occurring peaks with a high intrashell
reproducibility. Very similar Ba/Ca signals found in modern
Tridacnagigas
have been interpreted
as palaeoproductivity indicators
(Elliot et al., 2009). Records of a modern
Tridacna
spp. from
Sabah are utilized for comparison and calibration purposes
.

1 aWarter, Viola1 aMüller, Wolfgang1 aRenema, Willem uhttp://www.icp2013.cat/USB/PDF/P-183.PDF00610nas a2200121 4500008004100000245013000041210006900171260004700240100002600287700002100313700002000334856013400354 2013 eng d00aSimulation of the Indonesian Throughflow response to Antarctic ice-sheet changes during the Middle-Miocene Climate Transition0 aSimulation of the Indonesian Throughflow response to Antarctic i aMuseum fuer Naturkunde, Berlinc11/03/20131 aBoix, Amanda, Frigola1 aPrange, Matthias1 aSchulz, Michael uhttps://ipaeg.myspecies.info/content/simulation-indonesian-throughflow-response-antarctic-ice-sheet-changes-during-middle-miocene00485nas a2200097 4500008004100000245009500041210006900136260004700205100001700252856011800269 2013 eng d00aInventorying hyperdiverse marine molluscs: is there an alternative to focusing on species?0 aInventorying hyperdiverse marine molluscs is there an alternativ aMuseum fuer Naturkunde, Berlinc11/03/20131 aTodd, J., A. uhttps://ipaeg.myspecies.info/content/inventorying-hyperdiverse-marine-molluscs-there-alternative-focusing-species00547nas a2200109 4500008004100000245010500041210006900146260004700215100001800262700002200280856013500302 2013 eng d00aSeasonally-resolved records from giant clams – Snapshots of the Miocene climate of East Kalimantan0 aSeasonallyresolved records from giant clams Snapshots of the Mio aMuseum fuer Naturkunde, Berlinc11/03/20131 aWarter, Viola1 aMüller, Wolfgang uhttps://ipaeg.myspecies.info/content/seasonally-resolved-records-giant-clams-%E2%80%93-snapshots-miocene-climate-east-kalimantan-000598nas a2200145 4500008004100000245009300041210006900134260003000203100002600233700001700259700001400276700001800290700002500308856011900333 2012 eng d00aThermocline temperature variability in the Timor Strait over the last two glacial cycles0 aThermocline temperature variability in the Timor Strait over the aSan Franciscoc03/12/20121 aCappelli, Lo, Giudice1 aHolbourn, A.1 aKuhnt, W.1 aRegenberg, M.1 aGarbe-Schoenberg, D. uhttps://ipaeg.myspecies.info/content/thermocline-temperature-variability-timor-strait-over-last-two-glacial-cycles00597nas a2200145 4500008004100000245009000041210006900131260003500200100002600235700001700261700001400278700001800292700002500310856011600335 2013 eng d00aThermocline temperature variability in the Timor Strait during the last glacial cycle0 aThermocline temperature variability in the Timor Strait during t aMuseum fuer Naturkunde, Berlin1 aCappelli, Lo, Giudice1 aHolbourn, A.1 aKuhnt, W.1 aRegenberg, M.1 aGarbe-Schoenberg, D. uhttps://ipaeg.myspecies.info/content/thermocline-temperature-variability-timor-strait-during-last-glacial-cycle00571nas a2200145 4500008004100000245008000041210006900121260004700190100001700237700001400254700001700268700001800285700001700303856010500320 2013 eng d00aVariations in monsoon driven runoff from Sulawesi over the last Termination0 aVariations in monsoon driven runoff from Sulawesi over the last  aMuseum Fuer Naturkunde, Berlinc11/03/20131 aKüssner, K.1 aKuhnt, W.1 aHolbourn, A.1 aRegenberg, M.1 aAndersen, N. uhttps://ipaeg.myspecies.info/content/variations-monsoon-driven-runoff-sulawesi-over-last-termination00496nas a2200121 4500008004100000245006300041210006200104260004700166100002300213700002500236700002100261856009200282 2013 eng d00aOligocene to Pliocene palaeovegetation maps for Sundaland.0 aOligocene to Pliocene palaeovegetation maps for Sundaland aMuseum fuer Naturkunde, Berlinc11/03/20131 aMorley, Robert, J.1 aMorley, Harsanti, P.1 aJais, Jaizan, md uhttps://ipaeg.myspecies.info/content/oligocene-pliocene-palaeovegetation-maps-sundaland00433nas a2200109 4500008004100000245007700041210006900118260005400187100002800241700002500269856002900294 2013 eng d00aUnderstanding the murky origins of coral diversity in the Coral Triangle0 aUnderstanding the murky origins of coral diversity in the Coral  aMuseum für Naturkunde, Berlin, Germanyc11/03/131 aSantodomingo, Nadiezhda1 aJohnson, Kenneth, G. uhttp://www.sage2013.org/01792nas a2200133 4500008004100000245010100041210006900142260003200211520123000243100002401473700002001497700001801517856012301535 2013 eng d00aMicrobial carbonates in Miocene reefs in the Mahakam Delta in East Kalimantan, Borneo, Indonesia0 aMicrobial carbonates in Miocene reefs in the Mahakam Delta in Ea aBerlin, Germanyc11/03/20133 aCoral patch reefs grew in shallow marine turbid waters in the Miocene Mahakam Delta in East Kalimantan (Borneo, Indonesia). These patch reefs developed from delta front to deeper (prodelta) settings in areas with temporary reduced siliciclastic input. These coral reef deposits are well exposed in limestone quarries in the Batu Putih area in Samarinda and locally include microbial carbonates. Two different types of microbial carbonates have been found in two localities around Samarinda, 2 km apart from each other. In the northern section, microbialites occur as low-relief domes, up to 2 m wide and 0.5 m high, with internal lamination, developed around large coral fragments. They appear at the transition from bioclastic sediments with coralline algae and corals to fine-grained siliciclastic deposits in a deepening succession. The second type of microbialites can be found in the southern locality as decimetre-scale nodules formed around nuclei of large coral fragments. Microbial micrite with laminated to digitated fabrics intergrew with coralline algae to form the thick covers of these "megaoncoids". The large nodules are the main components of carbonate breccias deposited on the flanks of a patch reef. 1 aPretković, Vedrana1 aBraga, Juan, C.1 aRösler, Anja uhttps://ipaeg.myspecies.info/content/microbial-carbonates-miocene-reefs-mahakam-delta-east-kalimantan-borneo-indonesia01679nas a2200157 4500008004100000245009000041210006900131260003500200520105800235100001901293700001701312700002601329700002801355700001901383856011901402 2013 eng d00aDiversity and palaeoecology of Miocene coral-associated molluscs from East Kalimantan0 aDiversity and palaeoecology of Miocene coralassociated molluscs  aMuseum fuer Naturkunde, Berlin3 a

Currently, SE Asia is the global marine centre of diversity. High diversity is concentrated in and around reefs. A large variety of organisms, including corals and fish, but also molluscs, crustaceans and echinoderms contribute to this high diversity. In order to understand the timing and the context of the origin of the modern biodiversity hotspot, the fossil record needs to be documented. However, reef facies often suffer strong diagenesis, compromising the fossil record of reef and reef-associated organisms. Here we present an assessment of a well-preserved Late Miocene mollusc fauna from Bontang (East Kalimantan, Indonesia). The fauna is found in association with branching corals, dominated by Dictyaraea. The mollusc fauna is dominated by predatory and browsing carnivorous snails and includes reefal indicators such as the gastropod Coralliophyla and the bivalve Tridacna. The new Bontang fauna gives a glimpse of the diversity and ecological composition of a Late Miocene mollusc fauna from a so-called coral-carpet environment.

1 aKusworo, Aires1 aReich, Sonja1 aWesselingh, Frank, P.1 aSantodomingo, Nadiezhda1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/diversity-and-palaeoecology-miocene-coral-associated-molluscs-east-kalimantan01918nas a2200145 4500008004100000245006400041210006400105260003500169520140000204100001701604700002601621700001901647700001801666856008801684 2013 eng d00aMollusks as seagrass indicators in the Miocene of Indonesia0 aMollusks as seagrass indicators in the Miocene of Indonesia aMuseum fuer Naturkunde, Berlin3 a

Today’s centre of maximum marine biodiversity is located in the Indo-Malayan region. Understanding the development of this biodiversity hotspot through the Cenozoic could answer numerous questions about the responses of highly diverse faunal associations to small and large scale environmental changes. When assessing marine biodiversity through time comparisons of taxon diversity are only meaningful when comparing faunas from similar habitats. To evaluate diversity through time within the same ecological setting, it is indispensable to reliably discriminate different habitats. A good example for the difficulties which may occur when identifying marine paleo-habitats is the challenge of recognizing seagrass vegetation in the fossil record. Due to the low preservation potential of marine angiosperms, indirect indicators, e.g. associated organisms with a higher potential for preservation, are commonly used to infer the presence of seagrass meadows in the geological past. Because of their high fossilization potential and their abundance in marine habitats mollusks yield the possibility to be useful paleo seagrass indicators. Here we assess the potential use of indicator species, species and feeding guild composition of whole assemblages, as well as stable isotope signals in shells for their suitability to determine seagrass vegetation in the Miocene of Indonesia.

1 aReich, Sonja1 aWesselingh, Frank, P.1 aRenema, Willem1 aWarter, Viola uhttps://ipaeg.myspecies.info/content/mollusks-seagrass-indicators-miocene-indonesia00565nas a2200133 4500008004100000245009700041210006900138100001900207700002000226700001800246700002200264700001900286856012600305 2013 eng d00aIndonesian Throughflow variability through the Makassar Strait during the last glacial cycle0 aIndonesian Throughflow variability through the Makassar Strait d1 aSchroeder, Jan1 aKuhnt, Wolfgang1 aHolbourn, Ann1 aRegenberg, Marcus1 aAndersen, Nils uhttps://ipaeg.myspecies.info/content/indonesian-throughflow-variability-through-makassar-strait-during-last-glacial-cycle00526nas a2200121 4500008004100000245009700041210006900138100002100207700002100228700001800249700002000267856011700287 2013 eng d00aTropical convection variability in the West Pacific Warm Pool since the Last Glacial Maximum0 aTropical convection variability in the West Pacific Warm Pool si1 aFraser, Nicholas1 aBolliet, Timothe1 aHolbourn, Ann1 aKuhnt, Wolfgang uhttps://ipaeg.myspecies.info/content/tropical-convection-variability-west-pacific-warm-pool-last-glacial-maximum01998nas a2200121 4500008004100000245006500041210006500106260004700171520152600218100001701744700001901761856009601780 2013 eng d00aForaminiferal assemblages in Miocene carbonates of Indonesia0 aForaminiferal assemblages in Miocene carbonates of Indonesia aMuseum fuer Naturkunde, Berlinc11/03/20133 aNeogene carbonates in Indonesia are characterised by different depositional environments. We studied localities outcropping on Mangkalihat Peninsula, Kutai Basin, and Java, that were deposited in a time interval from Early (Te5) to Middle Miocene (Tf2). In order to reconstruct depositional environments and obtain biostratigraphic information, larger benthic foraminifera (LBF) assemblages were analysed from these three locations. The northernmost, and stratigraphically oldest, from the studied carbonates are exposed on Mangkalihat Peninsula. They were formed in shallow-water environment on carbonate platform. Stratigraphically important LBF indicate Early to Middle Miocene age (Te5-Tf1). Towards the south, in the Kutai Basin, isolated patch reefs occur within siliciclastic sediments, developed in mixed carbonate-siliciclastic depositional systems. In general, LBF assemblage is indicative of low-light conditions typical for mesophotic reefs. Based on LBF late Early to Middle Miocene age (Tf1-Tf2) can be suggested. The southernmost carbonate exposures are located on Central Java, in the Bulu Limestone member. The LBF assemblage composition indicate environmental conditions typical for continental shelf edge. Middle Miocene (Tf2) can be inferred for these limestones based on LBF. Here we present an overview of Indonesian Early to Middle Miocene LBF assemblages in a range of depositional environments. We will assess the interplay between stratigraphical and environmental control on LBF assemblages. 1 aNovak, Vibor1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/foraminiferal-assemblages-miocene-carbonates-indonesia00475nas a2200109 4500008004100000245006800041210006700109260004700176100002500223700002100248856009600269 2013 eng d00aBryozoan diversity in the Miocene of East Kalimantan, Indonesia0 aBryozoan diversity in the Miocene of East Kalimantan Indonesia aMuseum fuer Naturkunde, Berlinc11/03/20131 aDi Martino, Emanuela1 aTaylor, Paul, D. uhttps://ipaeg.myspecies.info/content/bryozoan-diversity-miocene-east-kalimantan-indonesia-002264nas a2200121 4500008004100000245007800041210006900119260002900188520178000217100001801997700002402015856010302039 2012 eng d00aCoralline algae from the Miocene Mahakam Delta (East Kalimantan, SE Asia)0 aCoralline algae from the Miocene Mahakam Delta East Kalimantan S aCharlotte, USAc04/11/123 aAlthough the Miocene is the epoch of the onset of the biodiversity hotspot in South East Asia, crustose coralline algae (CCA) of this age are poorly known in region. To fill this knowledge gap, crucial to understand the evolutionary history of reef building coralline algae, we studied CCA in Miocene reefs in the Kutai Basin, the largest sedimentary basin in Borneo that was dominated by siliciclastic sediments of the Proto-Mahakam delta. Local carbonate buildups comprising low relief patch reefs occur within the deltaic succession in shallow and turbid water, influenced by high siliciclastic input (Wilson, 2002). CCA in the Kutai basin are mostly found in association with coral reefs, encrusting corals or fragments of them. In beds with very high siliciclastic content no coralline algae were observed in the outcrops, but corals were still present. Two main CCA assemblages have been recognized in the studied Middle Miocene reefs: 1) a shallow-water assemblage, with two species of Neogoniolithon, thick crusts of Spongites, various Hydrolithon and also Sporolithon and Lithoporella. 2) In darker waters preferentilaly grew melobesioid assemblages, dominated by rhodoliths mainly consisting of Lithothamnion or by thin crusts of Mesophyllum and Sporolithon. This last one is the only assemblage found in mesophotic reefs. CCA of East Kalimantan show occurrences of some extant species earlier than expected. These new first-occurrence dates are being used to produce a detailed time tree of the main reef building CCA species with the help of a new molecular phylogeny based on five genetic markers. Wilson Moyra E.J. (2002) Cenozoic carbonates in Southeast Asia: implications for equatorial carbonate development. Sedimentary Geology 147, 295– 4281 aRösler, Anja1 aBraga, Juan, Carlos uhttps://ipaeg.myspecies.info/content/coralline-algae-miocene-mahakam-delta-east-kalimantan-se-asia00573nas a2200157 4500008004100000245007400041210006900115260004200184653001200226653001300238653001400251653001400265100002000279700002500299856009100324 2012 eng d00aAn overview of the Cenozoic fossil record of bryozoans in the tropics0 aoverview of the Cenozoic fossil record of bryozoans in the tropi aCharlotte, North Carolinac04/11/201210aBRYOZOA10aCenozoic10aEvolution10aTaphonomy1 aTaylor, Paul, D1 aDi Martino, Emanuela uhttps://ipaeg.myspecies.info/content/overview-cenozoic-fossil-record-bryozoans-tropics00560nas a2200121 4500008004100000245010500041210006900146260002500215100002500240700001900265710002400284856013000308 2011 eng d00aLate Cenozoic history of the Southeast Asian marine biodiversity maximum: new data for old questions0 aLate Cenozoic history of the Southeast Asian marine biodiversity aPlymouthc19/12/20111 aJohnson, Kenneth, G.1 aRenema, Willem1 aThroughflow Network uhttps://ipaeg.myspecies.info/content/late-cenozoic-history-southeast-asian-marine-biodiversity-maximum-new-data-old-questions00551nas a2200121 4500008004100000245010400041210006900145260002200214100001800236700002200254710002400276856012900300 2012 eng d00aHigh-resolution palaeoenvironmental records from Miocene patch reefs from SE-Kalimantan (Indonesia)0 aHighresolution palaeoenvironmental records from Miocene patch re aCairns, Australia1 aWarter, Viola1 aMüller, Wolfgang1 aThroughflow Network uhttps://ipaeg.myspecies.info/content/high-resolution-palaeoenvironmental-records-miocene-patch-reefs-se-kalimantan-indonesia00615nas a2200121 4500008004100000245007200041210006900113260013300182100002800315700002500343710002400368856010100392 2011 eng d00aHow diverse were reef corals of South East Asia during the Miocene?0 aHow diverse were reef corals of South East Asia during the Mioce aLiège, BelgiumbM. ARETZ, S. DELCULÉE, J. DENAYER & E. POTY (Eds.). Kölner Forum Geol. Paläont., 19: 155-156.c19-29/08/20111 aSantodomingo, Nadiezhda1 aJohnson, Kenneth, G.1 aThroughflow Network uhttps://ipaeg.myspecies.info/content/how-diverse-were-reef-corals-south-east-asia-during-miocene00521nas a2200109 4500008004100000245010300041210006900144260002700213100002500240710002400265856012200289 2011 eng d00aCenozoic bryozoans from southeast Asia: a contribution to the origin of high tropical biodiversity0 aCenozoic bryozoans from southeast Asia a contribution to the ori aSantiago de Compostela1 aDi Martino, Emanuela1 aThroughflow Network uhttps://ipaeg.myspecies.info/content/cenozoic-bryozoans-southeast-asia-contribution-origin-high-tropical-biodiversity