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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGEORGIADIS, Eleanor
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGIRAUDEAU, Jacques
hal.structure.identifierInstitute of Arctic Alpine Research [University of Colorado Boulder] [INSTAAR]
dc.contributor.authorJENNINGS, Anne
hal.structure.identifierUniversity of New Brunswick [UNB]
dc.contributor.authorLIMOGES, Audrey
hal.structure.identifierGeological Survey of Denmark and Greenland [GEUS]
dc.contributor.authorJACKSON, Rebecca
hal.structure.identifierGeological Survey of Denmark and Greenland [GEUS]
dc.contributor.authorRIBEIRO, Sofia
hal.structure.identifierTakuvik International Research Laboratory
dc.contributor.authorMASSÉ, Guillaume
dc.date.accessioned2024-01-23T13:08:31Z
dc.date.available2024-01-23T13:08:31Z
dc.date.issued2020
dc.identifier.issn0025-3227en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187426
dc.description.abstractEnNares Strait is one of three channels that connect the Arctic Ocean to Baffin Bay. Unique sea-ice conditions in the strait lead to the formation of landfast ice arches at its northern and southern ends. These ice arches regulate Arctic sea-ice and freshwater export through the strait and promote the opening of the North Water polynya. The present study addresses the paucity of pre-satellite records of environmental conditions in the Nares Strait area, and aims at reconstructing Holocene sea-ice conditions and ocean circulation in the strait. The investigation is based on a marine sediment core strategically retrieved from under the current ice arch in Kane Basin to the south of Nares Strait, and provides a continuous record spanning the past ca 9 kyrs. We use benthic foraminiferal assemblages and sea-ice biomarkers to infer changes in Holocene ocean circulation and sea-ice conditions in Kane Basin. The establishment of the modern ocean circulation in Kane Basin is related to ice sheet retreat and postglacial rebound, while changes in sea-ice cover concur with major shifts in the Arctic Oscillation (AO). Our results suggest that sea-ice cover in Kane Basin was highly variable between ca 9.0 and 8.3 cal. ka BP, before increasing, probably in link with the 8.2 cold event and the opening of Nares Strait. A short period of minimum sea-ice cover and maximum Atlantic bottom water influence occurred between ca 8.1 and 7.5 cal. ka BP, when Kane Basin was deeper than for the remaining of the Holocene. As atmospheric temperatures dropped, sea-ice cover intensified in Kane Basin between ca 7.5 and 5.5 cal. ka BP, but strong winds under prevailing positive-like AO conditions likely prevented the formation of ice arches in Nares Strait. During this time, our micro-paleontological data show that Atlantic water was progressively excluded from Kane Basin by the postglacial isostatic rebound. Increasingly cooler atmospheric temperatures and a shift towards more negative phases of the AO may have promoted the establishment of ice arches in Nares Strait between ca 5.5 and 3.0 cal. ka BP. Instabilities in the Kane Basin ice arch ca 3.0 cal. ka BP coincide with a shift towards prevailing positive phases of the AO, while a brief recovery of the ice arch occurred during more negative-like AO conditions between ca 1.2 and 0.2 cal. ka BP.
dc.language.isoENen_US
dc.subject.enArctic Ocean and adjacent high latitudes
dc.subject.enPaleoceanography
dc.subject.enMicropaleontology (forams)
dc.subject.enGlacial sediments
dc.subject.enSea-ice biomarkers
dc.title.enLocal and regional controls on Holocene sea ice dynamics and oceanography in Nares Strait, Northwest Greenland
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.margeo.2020.106115en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
dc.subject.halSciences de l'environnementen_US
dc.subject.halPlanète et Univers [physics]en_US
bordeaux.journalMarine Geologyen_US
bordeaux.page106115en_US
bordeaux.volume422en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02991666
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=Marine%20Geology&rft.date=2020&rft.volume=422&rft.spage=106115&rft.epage=106115&rft.eissn=0025-3227&rft.issn=0025-3227&rft.au=GEORGIADIS,%20Eleanor&GIRAUDEAU,%20Jacques&JENNINGS,%20Anne&LIMOGES,%20Audrey&JACKSON,%20Rebecca&rft.genre=article


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