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dc.rights.licenseopenen_US
hal.structure.identifierLaboratoire d'Ecogéochimie des environnements benthiques [LECOB]
dc.contributor.authorPRUSKI, A.M.
hal.structure.identifierLaboratoire Environnement Profond [LEP]
dc.contributor.authorDECKER, C.
hal.structure.identifierInstitut des Sciences de la Terre de Paris [iSTeP]
hal.structure.identifierLaboratoire d'Ecogéochimie des environnements benthiques [LECOB]
dc.contributor.authorSTETTEN, E.
hal.structure.identifierLaboratoire d'Ecogéochimie des environnements benthiques [LECOB]
dc.contributor.authorVÉTION, G.
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorMARTINEZ, Philippe
IDREF: 154067628
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorCHARLIER, Karine
hal.structure.identifierLaboratoire d'Ecogéochimie des environnements benthiques [LECOB]
dc.contributor.authorSENYARICH, C.
hal.structure.identifierLaboratoire Environnement Profond [LEP]
dc.contributor.authorOLU, K.
dc.date.accessioned2024-09-30T09:43:55Z
dc.date.available2024-09-30T09:43:55Z
dc.date.issued2017
dc.identifier.issn0967-0645en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/202020
dc.description.abstractEnLarge amounts of recent terrestrial organic matter (OM) from the African continent are delivered to the abyssal plain by turbidity currents and accumulate in the Congo deep-sea fan. In the recent lobe complex, large clusters of vesicomyid bivalves are found all along the active channel in areas of reduced sediment. These soft-sediment communities resemble those fuelled by chemoautotrophy in cold-seep settings. The aim of this study was to elucidate feeding strategies in these macrofaunal assemblages as part of a greater effort to understand the link between the inputs of terrestrially-derived OM and the chemosynthetic habitats. The biochemical composition of the sedimentary OM was first analysed in order to evaluate how nutritious the available particulate OM is for the benthic macrofauna. The terrestrial OM is already degraded when it reaches the final depositional area. However, high biopolymeric carbon contents (proteins, carbohydrates and lipids) are found in the channel of the recent lobe complex. In addition, about one to two thirds of the nitrogen can be assigned to peptide-like material. Even if this soil-derived OM is poorly digestible, turbiditic deposits contain such high amounts of organic carbon that there is enough biopolymeric carbon and proteacinous nitrogen to support dense benthic communities that contrast with the usual depauperate abyssal plains.
dc.description.sponsorshipTransfert de carbone organique et fonctionnement des écosystèmes dans les lobes terminaux de l'éventail sous-marin du Congo - ANR-11-BS56-0030en_US
dc.language.isoENen_US
dc.subject.enCongo deep-sea fan
dc.subject.enFood webs
dc.subject.enVesicomyid bivalves
dc.subject.enChemoautotrophy
dc.subject.enIsotopic signatures
dc.subject.enFatty acid biomarkers
dc.title.enEnergy transfer in the Congo deep-sea fan: from terrestrially-derived organic matter to chemosynthetic food webs
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.dsr2.2017.05.011en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terre/Océanographieen_US
bordeaux.journalDeep Sea Research Part II: Topical Studies in Oceanographyen_US
bordeaux.page197-218en_US
bordeaux.volume142en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamPALEOen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01525997
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=Deep%20Sea%20Research%20Part%20II:%20Topical%20Studies%20in%20Oceanography&rft.date=2017&rft.volume=142&rft.spage=197-218&rft.epage=197-218&rft.eissn=0967-0645&rft.issn=0967-0645&rft.au=PRUSKI,%20A.M.&DECKER,%20C.&STETTEN,%20E.&V%C3%89TION,%20G.&MARTINEZ,%20Philippe&rft.genre=article


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