00352nas a2200121 4500008004100000245003500041210003500076260003500111300000800146490000800154100002500162856004300187 2014 eng d00aCenozoic bryozoans from Borneo0 aCenozoic bryozoans from Borneo bUniversity of Utrechtc02/2014 a5610 vPhD1 aDi Martino, Emanuela uhttps://ipaeg.myspecies.info/node/207400445nas a2200133 4500008004600000245005800046210005400104100001700158700002500175700002600200700002300226700001900249856004300268 Submitted eng d 00aIndirect paleo- seagrass indicators (IPSIs): a review0 aIndirect paleo seagrass indicators IPSIs a review1 aReich, Sonja1 aDi Martino, Emanuela1 aWesselingh, Frank, P.1 aTodd, Jonathan, A.1 aRenema, Willem uhttps://ipaeg.myspecies.info/node/205702165nas a2200181 4500008004600000245008500046210006900131520159300200653001401793653001701807653001701824653001301841653001501854100002501869700002101894700002501915856004301940 Submitted eng d 00aBryozoan diversity in the Miocene of the Kutai Basin, East Kalimantan, Indonesia0 aBryozoan diversity in the Miocene of the Kutai Basin East Kalima3 a
Miocene bryozoans from the Indonesian Archipelago have been poorly investigated in the past. Several factors combine to explain their poor fossil record, including difficulties in locating good exposures in areas characterized by lush vegetation, dominance of inconspicuous encrusting species, and the adverse effects of diagenesis on fossil preservation. A large collection of samples from the Kutai Basin (East Kalimantan) made during the Marie Curie Initial Training Network ‘Throughflow’ has allowed new insights into the diversity of Miocene bryozoans in this region. The bryozoan assemblage as a whole consists of 123 species, which represents a remarkable increase in diversity compared to previous knowledge. Substrate availability appears to be the main factor controlling bryozoan distribution, the majority of encrusting species being associated with plate-like scleractinian corals. Collecting curves allow sampled sites to be divided into three groups characterized by high, medium and low species richness. The site of highest diversity is a mesophotic reef slope, environment influenced by strong input of terrigenous sediment. Ordination plots show no clear patterns of distribution among sites, with putatively endemic species accounting for most of the discrimination. A similar level of endemism and habitat heterogeneity characterizes modern, tropical bryozoan faunas. However, many more intermediate sites need to be sampled to achieve a fuller understanding of the true pattern of bryozoan species distribution in the Miocene of the Kutai Basin.
10aabundance10agrowth-forms10apreservation10aRichness10asubstrates1 aDi Martino, Emanuela1 aTaylor, Paul, D.1 aJohnson, Kenneth, G. uhttps://ipaeg.myspecies.info/node/203801766nas a2200169 4500008004600000245009300046210006900139520122700208653001401435653002001449653001401469653001201483653001301495100002501508700002001533856004301553 Submitted eng d 00aMiocene Bryozoa from East Kalimantan, Indonesia. Part II: Cheilostomata ‘Ascophora’.0 aMiocene Bryozoa from East Kalimantan Indonesia Part II Cheilosto3 aWe describe 72 ascophoran-grade cheilostomes, ranging in age from Early to Late Miocene (late Burdigalian to Messinian), collected from 17 sections in the vicinities of Samarinda, Bontang and Sangkulirang in East Kalimantan, Indonesian Borneo. Two genera (Oviexechonella gen. nov. and Sendinopora gen. nov.) and twenty species (?Filaguria kalimantanensis sp. nov., Puellina bontangensis sp. nov., Caberoides gordoni sp. nov., Trypostega hasibuani sp. nov., Oviexechonella digeronimoi sp. nov., Reptadeonella curvabilis sp. nov., Reptadeonella toddi sp. nov., ?Hippomenella devatasae sp. nov., ?Hippomenella uniserialis sp. nov., Margaretta amitabhae sp. nov., Hippopodina indicata sp. nov., Saevitella renemai sp. nov., Gigantopora milenae sp. nov., Arthropoma renipora sp. nov, Bryopesanser bragai sp. nov., Bryopesanser sanfilippoae sp. nov., Tubiporella magnipora sp. nov., Buffonellaria sagittaria sp. nov., Lagenipora sciutoi sp. nov. and Sendinopora prima sp. nov.) are new. Ten species show affinities with Recent taxa from the Indo-Pacific; two species show similarities with Recent species recorded circumtropically; and three species were known previously from the Neogene of Europe, Australia or India.
10aAscophora10aEast Kalimantan10aINDONESIA10aMiocene10aTAXONOMY1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/node/203701704nas a2200193 4500008004100000245010600041210006900147300001100216490000800227520111600235653001201351653002001363653001401383653001201397653001301409100002501422700002001447856004301467 2014 eng d00aMiocene Bryozoa from East Kalimantan, Indonesia. Part I: Cyclostomata and Cheilostomata ‘Anasca’.0 aMiocene Bryozoa from East Kalimantan Indonesia Part I Cyclostoma a17-1440 v1463 aThe Cenozoic bryozoan fauna of Indonesia has been severely neglected in the past. In this pioneering study, based on new material collected during the two field seasons of the Throughflow project, we describe a total of 51 bryozoan species, comprising 15 cyclostomes and 36 anascan-grade cheilostomes, ranging in age from Early to Late Miocene (Late Burdigalian to Messinian), collected from 17 sections located in the vicinities of Samarinda, Bontang and Sangkulirang in East Kalimantan, Indonesian Borneo. Eleven of these species (Microeciella nadiae sp. nov., Pseudidmonea johnsoni sp. nov., Cranosina rubeni sp. nov., Parellisina mirellae sp. nov., Vincularia berningi sp. nov., Vincularia semarai sp. nov., Vincularia tjaki sp. nov., Vincularia manchanui sp. nov., ?Gontarella sendinoae sp. nov., Canda giorgioi sp. nov. and Canda federicae sp. nov.) are new. Ten species show affinities with Recent taxa from the Indo-Pacific. Bryozoans are found mainly encrusting the undersides of platy corals from low- and high-relief build-ups and coral carpets in mixed carbonate-siliciclastic environments.
10aBRYOZOA10aEast Kalimantan10aINDONESIA10aMiocene10aTAXONOMY1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/node/203602493nas a2200193 4500008004100000245007000041210006900111260006700180490000600247520188400253653001402137653001302151653001702164653001502181653001502196100002002211700002502231856004302256 2013 eng d00aWhy is the tropical Cenozoic fossil record so poor for bryozoans?0 aWhy is the tropical Cenozoic fossil record so poor for bryozoans aCatania, ItalybMuseo Tridentino di Scienze Naturalicin press0 v13 aDiverse bryozoan assemblages have been recorded from widely across the Cenozoic palaeotropics, including the West Indies and Central America (Miocene-Pleistocene), Arabia (Oligocene), East Africa (Miocene), India (Eocene-Miocene) and the East Indies (Eocene-Miocene). However, records of Cenozoic tropical bryofaunas are relatively few compared with higher latitudes, and bryozoan limestones seem to be lacking. Insights into the reasons for this poor fossil record can be gleaned from comparisons with modern tropical bryozoan faunas, and consideration of the effects of diagenesis on fossil preservation and other factors that bias against the tropical Cenozoic fossil record. At least for the North Atlantic, bryozoan assemblage diversity in the modern tropics is not significantly less than in higher latitudes. However, a survey of colony-forms shows that encrusting species of small biomass are more dominant in tropical assemblages (mean 78% of species) than they are outside the tropics (mean 60% of species). These encrusting colonies may be difficult to observe and study when, as is often the case in tropical carbonate settings, diagenetic cement binds sediment firmly to the colony surfaces. Most erect bryozoan species living today in the tropics have weakly mineralized skeletons with a poor potential for fossilization; robust species capable of generating large quantities of carbonate sediment are uncommon. In addition, a higher proportion of cheilostomes in the tropics have metastable skeletons of aragonite: a Raman spectroscopic survey of 23 bryozoan species encrusting the undersides of platy corals from Puerto Rico and Malaysia showed 30% to be aragonitic and 27% bimineralic. Along with the typically higher Mg levels in the calcite of tropical cheilostomes, this further biases against preservation of bryozoans in the Cenozoic fossil record.
10aBryozoans10aCenozoic10acolony-forms10adiagenesis10amineralogy1 aTaylor, Paul, D1 aDi Martino, Emanuela uhttps://ipaeg.myspecies.info/node/203502143nas a2200193 4500008004100000245007200041210006700113260006800180490000600248520154200254653001401796653001401810653001101824653001101835653001501846100002501861700002001886856004301906 2013 eng d00aA brief review of seagrass-associated bryozoans, Recent and fossil.0 abrief review of seagrassassociated bryozoans Recent and fossil aCatania, ItalybMuseo Tridentino di Scienze Naturali cin press0 v13 aInformation concerning fossil and modern bryozoan assemblages reported from seagrass habitats is scattered through a large number of papers. The current paper groups taxonomically data from the literature on both modern and fossil bryozoans associated with seagrasses. Most of the modern data comes from studies focused on Posidonia oceanica meadows inhabiting the Mediterranean Sea, where a total of 152 bryozoan species have been recorded. Forty-one species have been reported on seagrasses from other geographical areas, such as Saudi Arabia, tropical America, Japan and Australia. Differences are outlined between the well-delineated communities of the leaves and the rhizomes, and some generalizations are made about morphological strategies for living as seagrass epiphytes. Seagrasses are seldom fossilized but examples of ancient communities can be inferred from the presence of bioimmurations of seagrass surfaces and from associated biota. They include a single Cretaceous community from the Maastrichtian of The Netherlands (43 bryozoan species), and a few Cenozoic communities described from several geographical regions (e.g. Europe, tropical America, Indo-Pacific; 72 species). New data is reported from a dark grey, silty clay in the Miocene of East Kalimantan (Indonesia) where the presence of the seagrass-indicative gastropod Smaragdia allows interpretation of the palaeoenvironment as a seagrass meadow with associated corals. The bryozoan assemblage here is monogeneric, comprising two species of Vincularia.
10aBryozoans10aepiphytes10afossil10aRECENT10aseagrasses1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/node/203400700nas a2200205 4500008004600000245009700046210006900143100002800212700001700240700002400257700002100281700001800302700002500320700002100345700001700366700002400383700001900407700002500426856004300451 Submitted eng d 00aA diverse patch reef from turbid habitats in the Middle Miocene (East Kalimantan, Indonesia)0 adiverse patch reef from turbid habitats in the Middle Miocene Ea1 aSantodomingo, Nadiezhda1 aNovak, Vibor1 aPretković, Vedrana1 aMarshall, Nathan1 aRösler, Anja1 aDi Martino, Emanuela1 aLoGiudice, Elena1 aReich, Sonja1 aBraga, Juan, Carlos1 aRenema, Willem1 aJohnson, Kenneth, G. uhttps://ipaeg.myspecies.info/node/203302842nas a2200205 4500008004100000245012500041210006900166300001200235490000800247520207100255100001702326700002802343700001802371700002502389700002402414700002002438700002502458700001902483856013402502 2013 eng d00aEnvironmental reconstruction of a late Burdigalian (Miocene) patch reef in deltaic deposits (East Kalimantan, Indonesia)0 aEnvironmental reconstruction of a late Burdigalian Miocene patch a110-1220 v3743 aMost studies of Cenozoic shallow-water, mixed carbonate-siliciclastic depositional systems have focused on their sedimentology. To date, however, comprehensive analyses of biotas and biofacies of Indo-West Pacific reefs that developed in mixed carbonate-siliciclastic systems are lacking. This study describes the palaeoenvironment and biodiversity of a late Burdigalian patch reef that developed in a mixed carbonate-siliciclastic depositional system. The studied exposure is located at the northeast margin of the Kutai Basin near Bontang (Indonesia), and is approximately 80 m wide and 25 m thick. Multi-taxon analysis of the most abundant fossil groups, including larger benthic foraminifera, corals, coralline algae, and bryozoans, aims to provide a model for environmental interpretation that will allow comparison with similar deposits of Indo-West Pacific region. Based on fossil content and lithology, five different facies types have been distinguished: foraminiferal packstone (FP), bioclastic packstone with foralgal communities (BP), thin-platy coral sheetstone (CS), platy-tabular coral platestone (CP), and shales (S). Among larger benthic foraminifera, smaller and more robust forms dominate in the FP and BP facies, while larger and flatter forms are the most abundant in the CS and CP facies. Thin-platy corals are dominant in the CS facies and gradually change into thicker platy-tabular forms in the CP facies. Assemblages and growth forms of coralline algae show no major differences between the facies types and are dominated by melobesioids and Sporolithon. The majority of bryozoan species are encrusting and were found only in the CS facies. Light-dependent organisms occurring in the reef indicate low light conditions typical for mesophotic reefs. The relatively small size of this reef complex and quite distinct vertical changes in the facies types, combined with the high siliciclastic content in most of the units, points to strong terrigenous input affecting water transparency as the main factor controlling the reef growth.
1 aNovak, Vibor1 aSantodomingo, Nadiezhda1 aRösler, Anja1 aDi Martino, Emanuela1 aBraga, Juan, Carlos1 aTaylor, Paul, D1 aJohnson, Kenneth, G.1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/environmental-reconstruction-late-burdigalian-miocene-patch-reef-deltaic-deposits-east-kalim00475nas 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-000588nas a2200205 4500008004100000022001400041245006600055210006500121260001200186300000900198490000900207653001200216653001800228653001100246653001300257653001100270100002500281700002000306856005600326 2012 eng d a1175-532600aPyrisinellidae, a new family of anascan cheilostome bryozoans0 aPyrisinellidae a new family of anascan cheilostome bryozoans c11/2012 a1-200 v353410aBRYOZOA10aCheilostomata10afossil10anew taxa10aRECENT1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttp://www.mapress.com/zootaxa/list/2012/3534.html 00836nas a2200217 4500008004100000022001400041024002900055245015400084210006900238260001200307300001100319490000700330653004100337653001200378653002000390653001700410653001200427100002500439700002000464856013400484 2012 eng d a0375-7633 adoi:10.4435/BSPI.2012.1100aSystematics and life history of Antoniettella exigua, a new genus and species of cribrimorph bryozoan from the Miocene of East Kalimantan (Indonesia)0 aSystematics and life history of Antoniettella exigua a new genus c09/2012 a99-1080 v5110aAntoniettella exigua gen. et sp. nov10aBRYOZOA10aEast Kalimantan10alife history10aMiocene1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/content/systematics-and-life-history-antoniettella-exigua-new-genus-and-species-cribrimorph-bryozoan00923nas a2200289 4500008004100000245008400041210006900125260003500194300000800229490000700237653001400244653002400258653001200282653003800294653001600332100002800348700001700376700002100393700002500414700002100439700002100460700002400481700001800505700001900523700002500542856006600567 2012 eng d00aDevelopment of a turbid reef in the Middle Miocene (East Kalimantan, Indonesia)0 aDevelopment of a turbid reef in the Middle Miocene East Kalimant aCharlotte, North Carolina, USA a6230 v7710aINDONESIA10amarginal ecosystems10aMiocene10apalaeonvironmental reconstruction10apatch reefs1 aSantodomingo, Nadiezhda1 aNovak, Vibor1 aMarshall, Nathan1 aDi Martino, Emanuela1 aFraser, Nicholas1 aLoGiudice, Elena1 aPretković, Vedrana1 aRösler, Anja1 aRenema, Willem1 aJohnson, Kenneth, G. uhttps://gsa.confex.com/gsa/2012AM/webprogram/Paper209284.html00599nas a2200193 4500008004100000245006900041210006700110260003100177300000800208490000700216653001200223653001400235653002000249653001200269653001300281100002500294700002000319856006600339 2012 eng d00aBryozoan diversity in the Miocene of East Kalimantan (Indonesia)0 aBryozoan diversity in the Miocene of East Kalimantan Indonesia aCharlotte, North Carolina a6240 v4410aBRYOZOA10aDiversity10aEast Kalimantan10aMiocene10aTAXONOMY1 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://gsa.confex.com/gsa/2012AM/webprogram/Paper205773.html00573nas 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-tropics00771nas a2200181 4500008004100000245013200041210006900173260003600242100002500278700002100303700001700324700002800341700001800369700002400387700002500411700001900436856013400455 2012 eng d00aPalaeoenvironmental reconstruction of a Miocene patch reef in East Kalimantan (Indonesia): a close-up on the bryozoan component0 aPalaeoenvironmental reconstruction of a Miocene patch reef in Ea aBrno Czech Republicc31/05/20121 aDi Martino, Emanuela1 aTaylor, Paul, D.1 aNovak, Vibor1 aSantodomingo, Nadiezhda1 aRösler, Anja1 aBraga, Juan, Carlos1 aJohnson, Kenneth, G.1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/palaeoenvironmental-reconstruction-miocene-patch-reef-east-kalimantan-indonesia-close-bryozo00682nas a2200181 4500008004100000245008700041210006900128260001500197100001700212700002800229700001800257700002500275700002000300700002000320700002500340700001900365856011600384 2012 eng d00aEnvironmental reconstruction of a Langhian patch reef (East Kalimantan, Indonesia)0 aEnvironmental reconstruction of a Langhian patch reef East Kalim c29/03/20121 aNovak, Vibor1 aSantodomingo, Nadiezhda1 aRösler, Anja1 aDi Martino, Emanuela1 aBraga, Juan, C.1 aTaylor, Paul, D1 aJohnson, Kenneth, G.1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/environmental-reconstruction-langhian-patch-reef-east-kalimantan-indonesia00669nas a2200181 4500008004100000245007200041210006900113260003100182100002500213700002100238700001700259700002800276700001800304700002400322700002500346700001900371856009700390 2012 eng d00aBryozoans from a Langhian patch reef in East Kalimantan (Indonesia)0 aBryozoans from a Langhian patch reef in East Kalimantan Indonesi aCatania, Italyc24/05/20121 aDi Martino, Emanuela1 aTaylor, Paul, D.1 aNovak, Vibor1 aSantodomingo, Nadiezhda1 aRösler, Anja1 aBraga, Juan, Carlos1 aJohnson, Kenneth, G.1 aRenema, Willem uhttps://ipaeg.myspecies.info/content/bryozoans-langhian-patch-reef-east-kalimantan-indonesia00401nas a2200109 4500008004100000245004200041210004100083260005100124100002500175700002000200856007100220 2012 eng d00aLiving fossils: a view from bryozoans0 aLiving fossils a view from bryozoans aThe Natural History Museum, Londonc27/03/20121 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/content/living-fossils-view-bryozoans00569nas a2200133 4500008004100000245011500041210006900156260001700225300000600242490000800248100002500256700002000281856013400301 2012 eng d00aMorphology and palaeobiogeography of Retelepralia, a distinctive cheilostome bryozoan new to the fossil record0 aMorphology and palaeobiogeography of Retelepralia a distinctive cJanuary 2012 a80 v2631 aDi Martino, Emanuela1 aTaylor, Paul, D uhttps://ipaeg.myspecies.info/content/morphology-and-palaeobiogeography-retelepralia-distinctive-cheilostome-bryozoan-new-fossil-000521nas 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