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Nile floods recorded in deep Mediterranean sediments

dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDUCASSOU, Emmanuelle
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMULDER, Thierry
dc.contributor.authorMIGEON, Sébastien
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorGONTHIER, Eliane
dc.contributor.authorMURAT, Anne
dc.contributor.authorREVEL, Marie
dc.contributor.authorCAPOTONDI, Lucilla
dc.contributor.authorBERNASCONI, Stefano M.
dc.contributor.authorMASCLE, Jean
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorZARAGOSI, Sebastien
IDREF: 189039159
dc.date.accessioned2024-10-25T12:07:07Z
dc.date.available2024-10-25T12:07:07Z
dc.date.issued2008-01-01
dc.identifier.issn0033-5894en_US
dc.identifier.urihttps://hal.archives-ouvertes.fr/hal-00407867
dc.identifier.urioai:crossref.org:10.1016/j.yqres.2008.02.011
dc.identifier.uriftunivnice:oai:HAL:hal-00407867v1
dc.identifier.urioai:researchgate.net:222814165
dc.identifier.uriorcid:0000-0001-7672-8856:10.1016/j.yqres.2008.02.011
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202820
dc.description.abstractEnAbstractClastic mud beds rich in continental organic matter are observed recurrently in the Nile deep-sea turbidite system. They formed during flooding periods of the river similar to those that induce sapropel formation and occurred during periods of increased density stratification of the eastern Mediterranean. The very fine-grained flood deposits are intercalated within pelagic sediments, sapropels and Bouma-type turbidites. These flood deposits form by the successive reconcentrations of surface (hypopycnal) plumes by convective sedimentation, which in turn generate a fine-grained low-energy hyperpycnal flow. Sea-level high stands seem also to favor hypopycnal plume formation and increase clastic mud bed formation. Consequently, these muddy clastic beds provide a direct link between deep-marine sedimentary records and continental climatic change through flood frequency and magnitude.
dc.language.isoENen_US
dc.sourcecrossref
dc.sourcebase
dc.sourceresearchgate
dc.sourceorcid
dc.title.enNile floods recorded in deep Mediterranean sediments
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.yqres.2008.02.011en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalQuaternary Researchen_US
bordeaux.page382-391en_US
bordeaux.volume70en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue3en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamGEOLSEDen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
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=Quaternary%20Research&rft.date=2008-01-01&rft.volume=70&rft.issue=3&rft.spage=382-391&rft.epage=382-391&rft.eissn=0033-5894&rft.issn=0033-5894&rft.au=DUCASSOU,%20Emmanuelle&MULDER,%20Thierry&MIGEON,%20S%C3%A9bastien&GONTHIER,%20Eliane&MURAT,%20Anne&rft.genre=article


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