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dc.rights.licenseopenen_US
hal.structure.identifierInstitut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
dc.contributor.authorTOUCANNE, Samuel
dc.contributor.authorRODRIGUES, Teresa
hal.structure.identifierLaboratoire de Géologie de Lyon - Terre, Planètes, Environnement [LGL-TPE]
dc.contributor.authorMENOT, Guillemette
hal.structure.identifierDurham University
hal.structure.identifierInstitut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
dc.contributor.authorSOULET, Guillaume
hal.structure.identifierLaboratoire Géosciences Océan [LGO]
dc.contributor.authorCHERON, Sandrine
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierLaboratoire d'Ecophysiologie et Ecotoxicologie des Systèmes Aquatiques [LEESA]
dc.contributor.authorBILLY, Isabelle
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
hal.structure.identifierLaboratoire de géographie physique : Environnements Quaternaires et Actuels [LGP]
dc.contributor.authorANTOINE, Pierre
dc.contributor.authorSINNINGHE DAMSTE, Jaap
hal.structure.identifierCentre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement [CEREGE]
dc.contributor.authorBARD, Edouard
dc.contributor.authorSANCHEZ GOÑI, Maria-Fernanda
dc.date.accessioned2024-02-06T15:25:24Z
dc.date.available2024-02-06T15:25:24Z
dc.date.issued2023-10
dc.identifier.issn0921-8181en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187931
dc.description.abstractEnMarine Isotope Stage (MIS) 4 (ca. 71-57 ka; within the Middle Weichselian Substage) is considered a significant Pleistocene glaciation, but it remains poorly constrained in comparison to that of the Late Weichselian Last Glacial Maximum (LGM; ca. 29-19 ka, during MIS 2), or even the Late Saalian MIS 6 (ca. 190-130 ka). Most MIS 4 glacial landforms in Europe were erased by the more extensive LGM ice advance, precluding a robust reconstruction of its extent and dynamic through time. Marine sedimentary archives, in preserving the source-to-sink sediment transfer signals of ice-sheet and glacier processes, help to bridge this gap. Here, the signals west of the European Ice Sheet (EIS) are tracked for MIS 4 from the deep Bay of Biscay (NE Atlantic), which was the outlet for Fennoscandian Ice Sheet (FIS) sediment-laden meltwater during extensive glaciations, specifically when the British-Irish Ice Sheet (BIIS) and the FIS coalesced into the North Sea (as during MIS 6 and the LGM). Sedimentological, geochemical, and mineralogical proxies reveal the absence of FIS-derived material in Bay of Biscay sediment throughout MIS 4, which indicates that FIS meltwater and huge river systems from the North European Plain never drained into the Bay of Biscay at that time. This suggests that contrary to MIS 6 and the LGM, the BIIS and FIS were not likely large enough to coalesce and form a (grounded) ice bridge onto the North Sea, thus confirming geomorphic evidence for a significant, but relatively limited, glaciation in Europe during MIS 4. Closer to the Bay of Biscay, ice-marginal fluctuations of the BIIS are identified in the Celtic-Irish Sea region from the deep-sea record. More specifically, our findings suggest an early retreat of the Irish Sea Ice Stream as soon as ca. 68-65 ka, a few millennia before the demise of the EIS, and the Northern Hemisphere ice sheets as a whole, during Heinrich Stadial (HS) 6. This pattern is similar to that already recorded during MIS 2. Finally, this study reveals that the MIS 4 period in Western Europe corresponds, as for MIS 2, to a complex combination of general ice advance interspersed by preliminary-to-final EIS demises highlighted by HS conditions.
dc.language.isoENen_US
dc.title.enMarine Isotope Stage 4 (71–57 ka) on the Western European margin: Insights to the drainage and dynamics of the Western European Ice Sheet
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.gloplacha.2023.104221en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
bordeaux.journalGlobal and Planetary Changeen_US
bordeaux.page104221en_US
bordeaux.volume229en_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-04202407
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=Global%20and%20Planetary%20Change&rft.date=2023-10&rft.volume=229&rft.spage=104221&rft.epage=104221&rft.eissn=0921-8181&rft.issn=0921-8181&rft.au=TOUCANNE,%20Samuel&RODRIGUES,%20Teresa&MENOT,%20Guillemette&SOULET,%20Guillaume&CHERON,%20Sandrine&rft.genre=article


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