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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDENIS, Delphine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCROSTA, Xavier
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.contributor.authorROMERO, O.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTIN, B.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierUnité Géosciences Marines [GM]
dc.contributor.authorMAS, V.
dc.date.accessioned2024-10-14T15:27:32Z
dc.date.available2024-10-14T15:27:32Z
dc.date.issued2016
dc.identifier.issn0959-6836en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202484
dc.description.abstractEnA 40 m long sediment core covering the 1000-9600 years BP period was retrieved from the Dumont d'Urville Trough off Adélie Land, East Antarctica, during the MD 130-Images X-CADO cruise. This sedimentary sequence allows the documentation of changes in climate seasonality during the Holocene. Here we show preliminary results of diatom communities, lithic grain distribution and titanium content measured on two 30 cm long sequences of thin sections. The two sequences originate from two different climate regimes, the colder Neoglacial and the warmer Hypsithermal. Proxies were measured at microscale resolution on 25 laminations for the Neoglacial and 14 laminations for the Hypsithermal. The two sequences reveal alternating light-green and dark-green laminae. Light laminae result from low terrigenous input and high sea-ice edge diatom fluxes and are interpreted to represent the spring season. Dark laminae result from high terrigenous input mixed with a diversified open ocean diatom flora and are interpreted to represent the summer-autumn season. The two sequences therefore resolve annual couplets composed of one light plus one dark lamina. Variations in the relative thickness of laminations and annual couplets, associated with diatom assemblage changes, are observed in each sequence and between the two sequences giving information on interannual to millennial changes in environmental conditions.
dc.language.isoENen_US
dc.subject.enAdélie Land
dc.subject.enHolocene
dc.subject.enlaminated sediments
dc.subject.endiatom ooze
dc.subject.enseasonality
dc.subject.ensea ice
dc.subject.enEast Antarctica
dc.title.enSeasonal and subseasonal climate changes recorded in laminated diatom ooze sediments, Adélie Land, East Antarctica
dc.typeArticle de revueen_US
dc.identifier.doi10.1177/0959683606069414en_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.journalThe Holoceneen_US
bordeaux.page1137-1147en_US
bordeaux.volume16en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue8en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02105681
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=The%20Holocene&rft.date=2016&rft.volume=16&rft.issue=8&rft.spage=1137-1147&rft.epage=1137-1147&rft.eissn=0959-6836&rft.issn=0959-6836&rft.au=DENIS,%20Delphine&CROSTA,%20Xavier&ZARAGOSI,%20Sebastien&ROMERO,%20O.&MARTIN,%20B.&rft.genre=article


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