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dc.rights.licenseopenen_US
hal.structure.identifierUnité Biogéochimie et Ecotoxicologie [BE]
dc.contributor.authorCOSSA, Daniel
dc.contributor.authorDE MADRON, Xavier Durrieu
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHAFER, Jorg
dc.contributor.authorGUÉDRON, Stéphane
dc.contributor.authorMARUSCZAK, Nicolas
dc.contributor.authorCASTELLE, Sabine
dc.contributor.authorNAUDIN, Jean-Jacques
dc.date.accessioned2024-05-10T16:18:27Z
dc.date.available2024-05-10T16:18:27Z
dc.date.issued2018-04
dc.identifier.issn0079-6611en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199750
dc.description.abstractEnOcean margins are focal regions in terms of mercury (Hg) exchanges between the continent and the open sea. The aim of this paper is to describe the distribution and partition of Hg between the gaseous, dissolved and particulate phases in the waters of the Northwestern Mediterranean (NWM) margin, in order to assess the Hg sources and exchanges within the continuum between the continental shelf (Gulf of Lions) and the open sea (Northern Gyre).Mean (± standard deviation) of total Hg species (HgT) concentrations in unfiltered water samples were 1.52 ± 1.00 pmol L-1 (n=36) in the inner shelf, 1.09 ± 0.15 pmol L-1 (n=30) along the slope, and 1.10 ± 0.13 pmol L-1 (n=99) in the Northern Gyre. The dissolved phase (<0.45µm) average concentrations were 0.80 ± 0.47 pmol L-1 (n=37) in the inner shelf, 0.93 ± 0.20 pmol L-1 (n=4) along the slope and 0.84 ± 0.10 (n=20) pmol L-1 in the Northern Gyre. The particulate fraction of Hg decreased very strongly seaward from around 60% on the shelf to 10-25% above the Northern Gyre. Very low dissolved HgT concentrations occurred in the inner shelf water, consistent with the results of incubation experiments, which demonstrated that shelf water is very efficient in both production and release of dissolved gaseous Hg into the atmosphere. In the North Gyre waters column HgT presents a distribution pattern inverse to that of dissolved oxygen, and a slight Hg enrichment in the deep layer (Western Mediterranean Deep Water).The Hg from the open sea water is the largest Hg input to the Gulf of Lions (∼5.7 kmol yr-1), whereas inputs from the riverine source account for ∼3.4 kmol yr-1 and atmospheric deposition for less than 0.5 kmol yr-1. The Hg accumulated in the sediments of the shelf is ∼4.5 kmol yr-1, including 0.6-1.7 kmol yr-1 in the Rhône prodelta sediments. The evasion to the atmosphere represents a Hg flux of ∼2.6 kmol yr-1.
dc.language.isoENen_US
dc.title.enSources and exchanges of mercury in the waters of the Northwestern Mediterranean margin
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.pocean.2017.05.002en_US
dc.subject.halSciences du Vivant [q-bio]en_US
dc.description.sponsorshipEuropeHotspot Ecosystem Research and Man\'s Impact on European seasen_US
bordeaux.journalProgress in Oceanographyen_US
bordeaux.page172-183en_US
bordeaux.volume163en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamTGMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-04201873
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=Progress%20in%20Oceanography&rft.date=2018-04&rft.volume=163&rft.spage=172-183&rft.epage=172-183&rft.eissn=0079-6611&rft.issn=0079-6611&rft.au=COSSA,%20Daniel&DE%20MADRON,%20Xavier%20Durrieu&SCHAFER,%20Jorg&GU%C3%89DRON,%20St%C3%A9phane&MARUSCZAK,%20Nicolas&rft.genre=article


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