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dc.rights.licenseopenen_US
hal.structure.identifierDipartimento Scienze della Terra
dc.contributor.authorTOLOTTI, R.
hal.structure.identifierUniversidad de Salamanca [España] = University of Salamanca [Spain]
dc.contributor.authorBÁRCENA, M. A.
hal.structure.identifierIstituto Nazionale di Geofisica e Vulcanologia - Sezione di Roma [INGV]
dc.contributor.authorMACRÌ, Patrizia
dc.contributor.authorCABURLOTTO, A.
hal.structure.identifierDipartimento Scienze della Terra
dc.contributor.authorBONCI, M. C.
dc.contributor.authorDE SANTIS, Laura
dc.contributor.authorDONDA, F.
hal.structure.identifierDipartimento Scienze della Terra
dc.contributor.authorCORRADI, Nicola
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCROSTA, Xavier
dc.date.accessioned2024-05-17T11:49:14Z
dc.date.available2024-05-17T11:49:14Z
dc.date.issued2018
dc.identifier.issn0035-1598en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199922
dc.description.abstractEnA new method merges conventional and quantitative biostratigraphic approaches, supported by magnetic polarity data, to develop a chronological framework for sediment core MD03-2595 retrieved on the continental rise off Wilkes Land, East Antarctica before proceeding to paleoceanographic and paleoclimatic analysis. This combined method helped to identify climatic cycles, highlight stratigraphic discontinuities and reworking, and assess regional sedimentological and diatom biostratigraphic evolution. Core MD03-2595 spans the last 0.8 Ma, from the Mid Pleistocene Transition (MPT) to the Early Holocene. A hiatus including Marine Isotope Stages (MIS) 19, 18 and 17 was identified, and a decreasing trend in sediment accumulation rates from MIS 16 to the Holocene was observed. This quantitative diatom biostratigraphic dataset, placed in its own sedimentological and paleomagnetic context, provides new information regarding the paleobiogeographic distribution and ecological responses of biostratigraphically significant diatom species, such as Thalassiosira elliptipora and T. fasciculata, for the Matuyama-Brunhes (M-B) transition, and Actinocyclus ingens, Hemidiscus karstenii and Rouxia spp. for the middle and late Pleistocene diatom biozonation.
dc.language.isoENen_US
dc.subject.enMatuyama-Brunhes Transition
dc.subject.enMid Pleistocene Transition
dc.subject.enLate Pleistocene
dc.subject.enQuantitative Biostratigraphy
dc.subject.enDiatom Biomarkers
dc.subject.enPaleomagnetic dataset
dc.title.enWilkes Land Late Pleistocene diatom age model: From bio-events to quantitative biostratigraphy
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.revmic.2018.05.001en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Climatologieen_US
bordeaux.journalRevue de Micropaléontologieen_US
bordeaux.page81-96en_US
bordeaux.volume61en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02105533
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Revue%20de%20Micropal%C3%A9ontologie&rft.date=2018&rft.volume=61&rft.issue=2&rft.spage=81-96&rft.epage=81-96&rft.eissn=0035-1598&rft.issn=0035-1598&rft.au=TOLOTTI,%20R.&B%C3%81RCENA,%20M.%20A.&MACR%C3%8C,%20Patrizia&CABURLOTTO,%20A.&BONCI,%20M.%20C.&rft.genre=article


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