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dc.rights.licenseopenen_US
dc.contributor.authorEKBLOM JOHANSSON, Fanny
hal.structure.identifierGeological Survey of Denmark and Greenland [GEUS]
dc.contributor.authorWANGNER, David
hal.structure.identifierGeological Survey of Denmark and Greenland [GEUS]
dc.contributor.authorANDRESEN, Camilla
dc.contributor.authorBAKKE, Jostein
dc.contributor.authorSTØREN, Eivind Nagel
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorVIELI, Andreas
dc.date.accessioned2024-04-03T08:52:32Z
dc.date.available2024-04-03T08:52:32Z
dc.date.issued2020
dc.identifier.issn0959-6836en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/189150
dc.description.abstractEnTo improve knowledge of marine-terminating glaciers in western Greenland, marine sediment cores from the Ata Sund fjord system, hosting two outlet glaciers, Eqip Sermia and Kangilerngata Sermia, were investigated. The main objective was to reconstruct glacial activity and paleoceanographic conditions during the past 600 years. Ice-rafted debris (IRD) was quantified by wet-sieving sediment samples and by using a computed tomography scan. Variability in relative bottom water temperatures in the fjord was reconstructed using foraminiferal analysis. On the basis of this, three periods of distinct glacial regimes were identified: Period 1 (1380–1810 CE), which covers the culmination of the Little Ice Age (LIA) and is interpreted as having advanced glaciers with high IRD content. Period 2 (1810–1920 CE), the end of the LIA, which was characterised by a lowering of the glaciers’ calving flux in response to climate cooling. During Period 3 (1920–2014 CE), both glaciers retreated substantially to their present-day extent. The bottom water temperature started to decrease just before Period 2 and remained relatively low until just before the end of Period 3. This is interpreted as a local response to increased glacial meltwater input. Our study was compared with a study in Disko Bay, nearby Jakobshavn Glacier and the result shows that both of these Greenlandic marine-terminating glaciers are responding to large-scale climate change. However, the specific imprint on the glaciers and the different fjord waters in front of them result in contrasting glacial responses and sediment archives in their respective fjords.
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subject.enCT scanning
dc.subject.enEqip Sermia
dc.subject.enforaminiferal analysis
dc.subject.enGreenland
dc.subject.enice-rafted debris
dc.subject.enKangilerngata Sermia
dc.subject.enLate Holocene
dc.subject.enLittle Ice Age
dc.title.enGlacier and ocean variability in Ata Sund, west Greenland, since 1400 CE
dc.typeArticle de revueen_US
dc.identifier.doi10.1177/0959683620950431en_US
dc.subject.halSciences de l'environnement/Milieux et Changements globauxen_US
bordeaux.journalThe Holoceneen_US
bordeaux.page095968362095043en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02917820
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccCC BYen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=The%20Holocene&rft.date=2020&rft.spage=095968362095043&rft.epage=095968362095043&rft.eissn=0959-6836&rft.issn=0959-6836&rft.au=EKBLOM%20JOHANSSON,%20Fanny&WANGNER,%20David&ANDRESEN,%20Camilla&BAKKE,%20Jostein&ST%C3%98REN,%20Eivind%20Nagel&rft.genre=article


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