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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMILZER, Gesa
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGIRAUDEAU, Jacques
hal.structure.identifierBundesanstalt für Geowissenschaften und Rohstoffe [BGR]
dc.contributor.authorRÜHLEMANN, C.
dc.contributor.authorFAUST, J.
hal.structure.identifierThe Arctic University of Norway [Tromsø, Norway] [UiT]
dc.contributor.authorKNIES, J.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.date.accessioned2024-10-01T11:59:28Z
dc.date.available2024-10-01T11:59:28Z
dc.date.issued2016
dc.identifier.issn0272-7714en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202091
dc.description.abstractEnBenthic stable isotopes (d 18 O c and d 13 C c) in the Trondheimsfjord reliably reflect the prevailing hydrological conditions with regard to the distance to the fjord entrance and the local topography. At the fjord entrance the d 18 O c and d 13 C c variabilities record changes in the temperature of the North Atlantic Current (NAC), and in the delivery of terrigenous organic matter by the Norwegian Coastal Current (NCC) and the fjord estuarine circulation, respectively. In the inner fjord basins, the benthic stable isotope compositions are predominantly controlled by hydrological characteristics linked to internal mixing and the prevailing wind pattern. The fjord deep basins are relatively sheltered from erosion and both land and marine-derived sediments accumulate at very high rates indicating past regional climate and associated driving parameters. In the present study we discuss the recent variability (last 55 years) of the stable isotope compositions (oxygen and carbon) measured in calcite shells of the benthic foraminiferan Mel-onis barleeanus with regard to the changing influence of marine versus fresh water inputs and of the prevailing wind patterns. The relative influence of marine versus continental waters were analysed as well as the complex topography and the related hydrology of the Trondheimsfjord using sediment cores collected in three different settings along the fjord axis. The variability the of stable isotope compositions obtained from the sedimentary archives is compared with in situ instrumental measurements over the investigated time interval.
dc.language.isoENen_US
dc.subject.enTrondheimsfjord
dc.subject.enBenthic foraminiferal stable isotopes
dc.subject.enCentral Norway
dc.subject.enFjord hydrology
dc.title.enBenthic stable isotope variability in the Trondheimsfjord during the last 50 years: Proxy records of mixing dynamics related to NAO
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.ecss.2016.01.034en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Géochimieen_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
bordeaux.journalEstuarine, Coastal and Shelf Scienceen_US
bordeaux.page34-46en_US
bordeaux.volume172en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-02128892
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=Estuarine,%20Coastal%20and%20Shelf%20Science&rft.date=2016&rft.volume=172&rft.spage=34-46&rft.epage=34-46&rft.eissn=0272-7714&rft.issn=0272-7714&rft.au=MILZER,%20Gesa&GIRAUDEAU,%20Jacques&R%C3%9CHLEMANN,%20C.&FAUST,%20J.&KNIES,%20J.&rft.genre=article


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