Nile floods recorded in deep Mediterranean sediments
| dc.rights.license | open | en_US |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | DUCASSOU, Emmanuelle | |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | MULDER, Thierry | |
| dc.contributor.author | MIGEON, Sébastien | |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | GONTHIER, Eliane | |
| dc.contributor.author | MURAT, Anne | |
| dc.contributor.author | REVEL, Marie | |
| dc.contributor.author | CAPOTONDI, Lucilla | |
| dc.contributor.author | BERNASCONI, Stefano M. | |
| dc.contributor.author | MASCLE, Jean | |
| hal.structure.identifier | Environnements et Paléoenvironnements OCéaniques [EPOC] | |
| dc.contributor.author | ZARAGOSI, Sebastien
IDREF: 189039159 | |
| dc.date.accessioned | 2024-10-25T12:07:07Z | |
| dc.date.available | 2024-10-25T12:07:07Z | |
| dc.date.issued | 2008-01-01 | |
| dc.identifier.issn | 0033-5894 | en_US |
| dc.identifier.uri | https://hal.archives-ouvertes.fr/hal-00407867 | |
| dc.identifier.uri | oai:crossref.org:10.1016/j.yqres.2008.02.011 | |
| dc.identifier.uri | ftunivnice:oai:HAL:hal-00407867v1 | |
| dc.identifier.uri | oai:researchgate.net:222814165 | |
| dc.identifier.uri | orcid:0000-0001-7672-8856:10.1016/j.yqres.2008.02.011 | |
| dc.identifier.uri | https://oskar-bordeaux.fr/handle/20.500.12278/202820 | |
| dc.description.abstractEn | AbstractClastic 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.iso | EN | en_US |
| dc.source | crossref | |
| dc.source | base | |
| dc.source | researchgate | |
| dc.source | orcid | |
| dc.title.en | Nile floods recorded in deep Mediterranean sediments | |
| dc.type | Article de revue | en_US |
| dc.identifier.doi | 10.1016/j.yqres.2008.02.011 | en_US |
| dc.subject.hal | Sciences de l'environnement | en_US |
| bordeaux.journal | Quaternary Research | en_US |
| bordeaux.page | 382-391 | en_US |
| bordeaux.volume | 70 | en_US |
| bordeaux.hal.laboratories | EPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805 | en_US |
| bordeaux.issue | 3 | en_US |
| bordeaux.institution | Université de Bordeaux | en_US |
| bordeaux.institution | CNRS | en_US |
| bordeaux.team | GEOLSED | en_US |
| bordeaux.peerReviewed | oui | en_US |
| bordeaux.inpress | non | en_US |
| bordeaux.import.source | dissemin | |
| hal.popular | non | en_US |
| hal.audience | Internationale | en_US |
| hal.export | false | |
| workflow.import.source | dissemin | |
| dc.rights.cc | Pas de Licence CC | en_US |
| bordeaux.COinS | ctx_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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