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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorFAUQUEMBERGUE, Kelly
IDREF: 233247483
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMULDER, Thierry
dc.contributor.authorREIJMER, J.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorHANQUIEZ, Vincent
dc.contributor.authorBETZLER, C.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorDUCASSOU, Emmanuelle
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorRECOUVREUR, Audrey
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorPRINCIPAUD, Melanie
dc.contributor.authorBORGOMANO, J.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorWILK, Stanislas
dc.contributor.authorPOLI, E.
dc.date.accessioned2024-11-14T13:02:02Z
dc.date.available2024-11-14T13:02:02Z
dc.date.issued2024-06-01
dc.identifier.issn1525-2027en_US
dc.identifier.urioai:crossref.org:10.1029/2023gc011077
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/203270
dc.description.abstractEnAbstractSlopes adjacent to the Bahamian carbonate platform revealed a large variety of depositional processes. In this study, we present a synthesis summarizing 109,000 km2 of bathymetric and reflectivity data with ∼7,900 km of seismic lines and 311 m of sediment cores that were obtained over the last 50 years. These data are used to develop a conceptual model of sedimentation patterns on Quaternary carbonate slope systems and their interaction with the adjacent shallow‐water carbonate platforms. Our data highlight that during the Quaternary, factors controlling large‐scale sedimentation on Bahamian slopes have numerous similarities as they have higher sedimentation rates during interglacials. At a small scale, every slope has its own characteristics that are contemporary controlled by two main characteristics: (a) facies on the adjacent shallow‐water platform, and (b) the impact of shallow‐ and deep‐water currents. Large‐scale tectonics influence sediment deposition as it determines the position of the islands and impacts platform facies distribution.
dc.language.isoENen_US
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/us/*
dc.sourcecrossref
dc.title.enSedimentology of Modern Bahamian Carbonate Slopes: Summary and Update
dc.typeArticle de revueen_US
dc.identifier.doi10.1029/2023gc011077en_US
dc.subject.halSciences de l'environnementen_US
bordeaux.journalGeochemistry, Geophysics, Geosystemsen_US
bordeaux.volume25en_US
bordeaux.hal.laboratoriesEPOCen_US
bordeaux.issue6en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcedissemin
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcedissemin
dc.rights.ccCC BY-NC-NDen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geochemistry,%20Geophysics,%20Geosystems&rft.date=2024-06-01&rft.volume=25&rft.issue=6&rft.eissn=1525-2027&rft.issn=1525-2027&rft.au=FAUQUEMBERGUE,%20Kelly&MULDER,%20Thierry&REIJMER,%20J.&HANQUIEZ,%20Vincent&BETZLER,%20C.&rft.genre=article


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