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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorDE DECKKER, P.
dc.date.accessioned2024-06-07T12:19:55Z
dc.date.available2024-06-07T12:19:55Z
dc.date.issued2015-02-17
dc.identifier.issn0812-0099en_US
dc.identifier.urioai:crossref.org:10.1080/08120099.2015.1014846
dc.identifier.uriorcid:0000-0002-5985-9747:10.1080/08120099.2015.1014846
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/200339
dc.description.abstractEnThe Australian continental margin presents highly contrasted settings depending on (1) the presence or absence of a fluvial sediment supply, (2) the distance from the Australian mainland, and (3) the local hydrological setting. Despite the importance in surface area of the continental margin around the Australian mainland, so far only a few studies have dealt with sedimentation, most of them focusing on the northeastern Australian Shelf. This work presents the first large-scale investigation of modern sedimentation along the southern margin of Australia in the SE Indian Ocean, and the western margin of the Tasman Sea. Sedimentation intensity was assessed on a century timescale using a multi-tracer approach (234Th, 210Pb, 232Th) on interface cores around the 1000 m water depth contour. 234Th (half-life: 24.1 days) in excess was detected in all surface samples, testifying to the occurrence of freshly deposited particles. Sedimentation and mass accumulation rates based on sedimentary 210Pb excess profiles (CF:CS model) range between 0.027 and 0.280 cm y–1 and between 14 and 222 mg cm–2 y–1, respectively. Whereas sedimentation rates are low and associated with carbonates on the western margin, sediments are more influenced by the detrital fraction and organic carbon on the eastern side of the continent. In comparison with northern continental margins (e.g. Timor Sea, Gulf of Papua), the southern Australian margin receives little sediment today, as it is rarely linked to a river system that would otherwise deliver large amounts of sediment, and also because of the presence of the extended shelf south of Australia.
dc.language.isoENen_US
dc.sourcecrossref
dc.sourceorcid
dc.subject.enAustralian continental margin
dc.subject.ensedimentation rate
dc.subject.enmass accumulation rate
dc.subject.enthorium-234
dc.subject.enthorium-232
dc.subject.enlead-210
dc.subject.enparticulate organic carbon
dc.subject.encarbonate
dc.subject.engrain size
dc.title.enPresent-day sedimentation rates on the southern and southeastern Australian continental margins
dc.typeArticle de revueen_US
dc.identifier.doi10.1080/08120099.2015.1014846en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalAustralian Journal of Earth Sciencesen_US
bordeaux.page143-150en_US
bordeaux.volume62en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.identifierhal-04604854
hal.version1
hal.date.transferred2024-06-07T12:19:56Z
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=Australian%20Journal%20of%20Earth%20Sciences&rft.date=2015-02-17&rft.volume=62&rft.issue=2&rft.spage=143-150&rft.epage=143-150&rft.eissn=0812-0099&rft.issn=0812-0099&rft.au=SCHMIDT,%20Sabine&DE%20DECKKER,%20P.&rft.genre=article


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