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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorWARY, Melanie
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorROSSIGNOL, Linda
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSABINE, Marjolaine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCASTERA, Marie Helene
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorBILLY, Isabelle
dc.date.accessioned2024-10-07T11:47:01Z
dc.date.available2024-10-07T11:47:01Z
dc.date.issued2017-09-18
dc.identifier.issn0267-8179en_US
dc.identifier.uriorcid:0000-0001-5211-2168:10.1002/jqs.2965
dc.identifier.urioai:crossref.org:10.1002/jqs.2965
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202290
dc.description.abstractEnThe last glacial millennial Heinrich and Dansgaard–Oeschger events have been the subject of many studies in recent decades. However, significant uncertainties remain, notably regarding associated oceanic mechanisms. Here we investigate the evolution of hydrographical conditions in the 3–41 ka cal BP interval of core MD99-2285 located in the southern Norwegian Sea. Our results reveal an unusual scheme with: (i) warm Greenland interstadials marked by a relatively cold and homogeneous upper water column seasonally ice-covered and active deep water formation, (ii) cold Greenland and Heinrich stadials marked by a warm, low-salinity and nearly sea ice-free surface layer with iceberg calving, separated by a strong halocline from a colder and saltier subsurface layer, as well as strongly reduced deep convection, and (iii) close to modern Holocene oceanic conditions, but showing significant differences from interstadial conditions. Hence, our work strongly suggests different deep-water convection modes in the Nordic Seas, with, notably, interstadial deep water formation mainly forced by brine release. According to our results, the transition from the glacial mode of deep water formation to the modern open ocean convection mode might have occurred at the end of deglaciation/beginning of the Holocene, when both modes probably occurred.
dc.language.isoENen_US
dc.sourceorcid
dc.sourcecrossref
dc.title.enThe southern Norwegian Sea during the last 45 ka: hydrographical reorganizations under changing ice‐sheet dynamics
dc.typeArticle de revueen_US
dc.identifier.doi10.1002/jqs.2965en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalJournal of Quaternary Scienceen_US
bordeaux.page908-922en_US
bordeaux.volume32en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue7en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04723842
hal.version1
hal.date.transferred2024-10-07T11:47:03Z
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exporttrue
workflow.import.sourcedissemin
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Journal%20of%20Quaternary%20Science&rft.date=2017-09-18&rft.volume=32&rft.issue=7&rft.spage=908-922&rft.epage=908-922&rft.eissn=0267-8179&rft.issn=0267-8179&rft.au=WARY,%20Melanie&EYNAUD,%20Frederique&ROSSIGNOL,%20Linda&ZARAGOSI,%20Sebastien&SABINE,%20Marjolaine&rft.genre=article


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