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dc.rights.licenseopenen_US
hal.structure.identifierInstitut des Sciences de la MER de Rimouski [ISMER]
dc.contributor.authorCARON, Myriam
hal.structure.identifierInstitut des Sciences de la MER de Rimouski [ISMER]
dc.contributor.authorST-ONGE, Guillaume
hal.structure.identifierInstitut des Sciences de la MER de Rimouski [ISMER]
dc.contributor.authorMONTERO-SERRANO, Jean-Carlos
hal.structure.identifierInstitut des Sciences de la MER de Rimouski [ISMER]
dc.contributor.authorROCHON, André
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGEORGIADIS, Eleanor
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGIRAUDEAU, Jacques
hal.structure.identifierPetroleum and Environmental Geochemistry Group
dc.contributor.authorMASSÉ, Guillaume
dc.date.accessioned2024-02-29T12:56:52Z
dc.date.available2024-02-29T12:56:52Z
dc.date.issued2019-01
dc.identifier.issn0300-9483en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188508
dc.description.abstractEnThe northeastern Baffin Bay continental margin, which experiences high sediment accumulation rates, is an excellent location to study Holocene sedimentary variations. However, it is often difficult to obtain reliable chronologies of the sediment archives using traditional methods (d 18 O and radiocarbon) due to specific oceanographic conditions (e.g. corrosive bottom waters). Here we propose a chronostratigraphy of three cores collected on the northwestern Greenland margin (AMD14-204, AMD14-210 and AMD14-Kane2B) based on a combination of radiocarbon dating and palaeomagnetic records. Geophysical properties of discrete samples were used to verify the reliability of the palaeomagnetic records. Palaeomagnetic analyses indicate a strong and stable natural remanent magnetization carried by low coercivity ferrimagnetic minerals (magnetite) in the pseudo-single domain grain size range. Correlation of the full palaeomagnetic vector (inclination, declination, and relative palaeointensity) was used to establish a reliable chronostratigraphical framework for two of the cores (AMD14-204 and AMD14-210) and to propose an original palaeomagnetic record for the previously 14 C-dated core AMD14-Kane2B that covers most of the Holocene. Overall, this new chronostratigraphy allowed improvement of the timing of the main palaeoenvi-ronmental changes that occurred in this area during the Holocene.
dc.language.isoENen_US
dc.title.enHolocene chronostratigraphy of northeastern Baffin Bay based on radiocarbon and palaeomagnetic data
dc.typeArticle de revueen_US
dc.identifier.doi10.1111/bor.12346en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalBoreasen_US
bordeaux.page147-165en_US
bordeaux.volume48en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02411243
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=Boreas&rft.date=2019-01&rft.volume=48&rft.issue=1&rft.spage=147-165&rft.epage=147-165&rft.eissn=0300-9483&rft.issn=0300-9483&rft.au=CARON,%20Myriam&ST-ONGE,%20Guillaume&MONTERO-SERRANO,%20Jean-Carlos&ROCHON,%20Andr%C3%A9&GEORGIADIS,%20Eleanor&rft.genre=article


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