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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
IDREF: 131836129
dc.contributor.authorPASTOR, L.
dc.contributor.authorBRANDILY, C.
dc.contributor.authorMIRAMONTES, E.
dc.contributor.authorPÉRON, M.
dc.contributor.authorAPPÉRÉ, D.
dc.contributor.authorCHÉRON, S.
dc.contributor.authorBOISSIER, A.
dc.contributor.authorJOUET, Gwenael
dc.date.accessioned2024-01-23T13:18:22Z
dc.date.available2024-01-23T13:18:22Z
dc.date.issued2020-08
dc.identifier.issn0025-3227en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/187429
dc.description.abstractEnThe NW Madagascar continental margin receives high loads of terrigenous particulate organic matter during the wet season and especially linked to extreme events, originating from two major rivers, the Betsiboka and the Mahavavy Rivers. This particulate matter contains a high content of iron minerals from the weathering of red ferruginous/ferralitic soils of Madagascar. The presence of pockmarks, i.e. gas or fluid expulsion features on the continental slope, testifies to past/present methane migration through the sedimentary column, associated with early diagenetic processes. This study globally aims at deciphering the interactions between episodic sedimentation and geochemical processes influenced by fluids upward migration, using a sediment trap mooring and interface sediment cores at two sites on the continental slope. The present-day sedimentation along this margin undergoes two patterns. During the wet season, high continental fluxes generally result in an increase in particle fluxes on the slope. Longshore currents may deflect river plumes alongslope resulting in some periods of low particle flux on the slope during the wet season. During the dry season, the particles collected in the water column are probably originated from sediment remobilization from the shelf and slope. The observed progradation of the Mahavavy River delta and prodelta between 1984 and 2016 argues for an increase in temporary connections of the river with the canyon head during extreme events, inducing pulsed sedimentation offshore. This pulsed sedimentation could be responsible for enhancing pyritization on surface sediments, due to higher inputs of terrigenous organic matter and iron oxides. Finally, methane upward migration also influences the pyritization process through anaerobic oxidation of methane using sulfate as an electron acceptor and methanotrophs associated with this reaction significantly impact the δ13C of organic carbon towards more negative values.
dc.language.isoENen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/
dc.subject.enEpisodic sedimentation
dc.subject.enMadagascar margin
dc.subject.enBetsiboka river
dc.subject.enMahavavy river
dc.subject.enProgradation
dc.subject.enmethane
dc.subject.enGeochemistry
dc.subject.enSediment
dc.title.enModern sedimentation and geochemical imprints in sediments from the NW Madagascar margin
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.margeo.2020.106184en_US
dc.subject.halPlanète et Univers [physics]/Océan, Atmosphèreen_US
bordeaux.journalMarine Geologyen_US
bordeaux.page106184en_US
bordeaux.volume426en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03431785
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=Marine%20Geology&rft.date=2020-08&rft.volume=426&rft.spage=106184&rft.epage=106184&rft.eissn=0025-3227&rft.issn=0025-3227&rft.au=SCHMIDT,%20Sabine&PASTOR,%20L.&BRANDILY,%20C.&MIRAMONTES,%20E.&P%C3%89RON,%20M.&rft.genre=article


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