Mostrar el registro sencillo del ítem

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMOJTAHID, Meryem
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorEYNAUD, Frederique
IDREF: 144113570
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
hal.structure.identifierSchool of Ocean Sciences, University of Wales (Bangor)
dc.contributor.authorSCOURSE, J.
hal.structure.identifierInstitut Français de Recherche pour l'Exploitation de la Mer [IFREMER]
dc.contributor.authorBOURILLET, J.-F.
hal.structure.identifierService Hydrographique et Océanographique de la Marine [SHOM]
dc.contributor.authorGARLAN, T.
dc.date.accessioned2024-11-15T12:39:46Z
dc.date.available2024-11-15T12:39:46Z
dc.date.issued2005-11
dc.identifier.issn0025-3227en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/203302
dc.description.abstractEnCore MD03-2692 was retrieved in a water-depth of 4064 m on the Celtic margin (Bay of Biscay) during the SEDICAR cruise onboard the RV Marion Dufresne II. It covers the last 360 ka in a total length of 39 m. Multidisciplinary analyses have been applied to this sequence with the aim of studying the palaeoclimatic and palaeoenvironmental signals of the last few climatic cycles. The analyses undertaken include: (1) non-destructive logging with: physical properties (magnetic susceptibility, sediment colour), X-ray radiography and measurement of the major elements by X-ray-fluorescence, (2) analyses of planktonic and benthic foraminifera, lithic grains and stable isotopic measurements (oxygen and carbon). We have focused on the longterm evolution of glacial stages (with special attention to terminations and Heinrich events). The results obtained confirm the close correlation between deep-sea sedimentation recorded on the Celtic margin and changes in the terrestrial environment of the adjacent continent. Heinrich layers have been identified in MIS 2, 3, 6 and 8. We note the occurrence of laminated facies within deglacial sequences deposited during Termination I and MIS 6. These facies are closely linked to disintegration phases of the British-Irish Ice Sheet (BIS). The laminations contain lower ice-rafted detritus (IRD) concentrations than the equivalent Heinrich layers and are linked to abrupt changes in sea-surface palaeotemperatures. We suggest that the laminations are formed by an annual cycle of meltwater and iceberg release from the disintegrating BIS generating cascading plumes of dense turbid meltwater coeval with IRD release.
dc.language.isoENen_US
dc.subject.enCeltic margin glacial terminations British-Irish Ice Sheet laminated sediments
dc.subject.enCeltic margin
dc.subject.englacial terminations
dc.subject.enBritish-Irish Ice Sheet
dc.subject.enlaminated sediments
dc.title.enPalaeoclimatology and palaeohydrography of the glacial stages on Celtic and Armorican margins over the last 360000 yrs
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.margeo.2005.07.007en_US
dc.subject.halPlanète et Univers [physics]en_US
bordeaux.journalMarine Geologyen_US
bordeaux.page57-82en_US
bordeaux.volume224en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue1-4en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03974620
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=2005-11&rft.volume=224&rft.issue=1-4&rft.spage=57-82&rft.epage=57-82&rft.eissn=0025-3227&rft.issn=0025-3227&rft.au=MOJTAHID,%20Meryem&EYNAUD,%20Frederique&ZARAGOSI,%20Sebastien&SCOURSE,%20J.&BOURILLET,%20J.-F.&rft.genre=article


Archivos en el ítem

ArchivosTamañoFormatoVer

No hay archivos asociados a este ítem.

Este ítem aparece en la(s) siguiente(s) colección(ones)

Mostrar el registro sencillo del ítem