georefid:2013-000394SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.4202/app.2008.0076<gco:CharacterString>Neogene radiolarian biostratigraphy and faunal evolution rates in the eastern Equatorial Pacific ODP Sites 845 and 1241</gco:CharacterString>2009-01-01publicationgeorefid:2013-000394doi:10.4202/app.2008.0076Kamikuri, Schin-IchiUniversity of Tsukuba, Department of Earth Evolution Sciences, Tsukuba, JapanauthorMotoyama, IsaoHokkaido University, JapanauthorNishi, HiroshiKochi University, JapanauthorIwai, MasaoauthorPanstwowe Wydawnictwo Naukowe, Warsaw, PolandpublisherdocumentDigitalActa Palaeontologica Polonica54 (4)713-742Radiolarians from Sites 845 and 1241 in the eastern equatorial Pacific were examined in order to evaluate the role of paleoceanographic perturbations upon the general faunal evolutionary pattern of tropical planktonic organisms during the last 17 Ma. Radiolarian appearance and extinction rates indicate no periods of mass extinctions during the past 17 Ma. However, a relatively rapid replacement of the species in the radiolarian assemblages occurs near the middle-late Miocene boundary. This replacement event represents the gradual extinction of a number of radiolarian species and their gradual replacement by evolving new species. The modern equatorial circulation system was formed near the middle-late Miocene boundary due to the closure of the Indonesian seaway. The minor faunal turnover appears to be associated with the formation of the modern equatorial circulation system near the middle-late Miocene boundary. Diatom assemblages in the equatorial Pacific became more provincial in character after about 9 Ma. The appearance and extinction rates of planktic foraminifers were relatively high near the middle-late Miocene boundary, and those of calcareous nannoplankton reached high values in the early late Miocene in the equatorial Pacific Ocean. Thus, faunal evolution from the middle Miocene type to late Miocene types occurred first, being followed by floral evolution. The middle-late Miocene boundary is not a sharp boundary for planktonic microfossils, but marks a time of transition critical for faunal and floral evolution in both siliceous and calcareous microfossil assemblages in the equatorial Pacific Ocean.completedInvertebrate paleontologyStratigraphybiologic evolutionbiostratigraphyCenozoicCocos RidgeEast PacificEquatorial PacificGuatemala BasinInvertebrataLeg 138Leg 202microfossilsmiddle MioceneMioceneNeogeneNorth PacificNortheast PacificOcean Drilling ProgramODP Site 1241ODP Site 845Pacific Oceanpaleo-oceanographypaleoenvironmentProtistaRadiolariaratesstratigraphic boundaryTertiarytropical environmentupper Mioceneurn:org.iodp:exp:138urnlargerWorkCitationcampaignurn:org.iodp:exp:202urnlargerWorkCitationcampaignurn:org.iodp:exp:202:site:1241urnlargerWorkCitationstudyurn:org.iodp:exp:202urnlargerWorkCitationcampaignurn:org.iodp:exp:138:site:845urnlargerWorkCitationstudyurn:org.iodp:exp:138urnlargerWorkCitationcampaignEnglishgeoscientificInformation-94.3527-86.27005.51009.3500application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www.app.pan.pl/archive/published/app54/app20080076.pdfdownload