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dc.rights.licenseopenen_US
dc.contributor.authorDUBOSQ, Nicolas
dc.contributor.authorSCHMIDT, Sabine
dc.contributor.authorSUDRE, Joel
dc.contributor.authorRIGAUD, Sylvain
dc.contributor.authorLAMARQUE, Bastien
IDREF: 257511881
dc.contributor.authorDANILO, Martin
dc.contributor.authorGREMARE, Antoine
dc.contributor.authorDEFLANDRE, Bruno
IDREF: 170923509
dc.date.accessioned2022-11-22T17:41:07Z
dc.date.available2022-11-22T17:41:07Z
dc.date.issued2022-10-07
dc.identifier.issn2296-7745en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/170345
dc.description.abstractEnAlthough not systematically considered as oxygen minimum zones, River-dominated Ocean Margins are sensitive to oxygen depletions. For example, the continental shelf off the Gironde, which flows into the Bay of Biscay, had not yet been studied from this perspective although recent simulations suggested that this area should already have experienced deoxygenations in recent decades. To fill this gap, profiles of temperature, salinity and dissolved oxygen were performed in the water column of the continental shelf off the Gironde during seven cruises distributed over the different seasons between 2016 and 2021. Turbidity, chlorophyll-a and pH were also measured during some of these cruises. In winter, the water column was slightly stratified due to high river flows. Then, a seasonal thermal stratification was present from spring to autumn. Similarly, dissolved oxygen showed a seasonal dynamic with: a well-oxygenated water column in winter, an oxygen oversaturation in the first 20 meters during the spring bloom, and then a progressive oxygen depletion in bottom waters until reaching an oxygen saturation minimum down to 45% in autumn. These deoxygenations are explained by the seasonal stratification that isolates the bottom waters from spring to autumn, and are likely enhanced by the advection of deoxygenated waters from the north of the Bay of Biscay and the settling of the organic matter produced in surface waters. A better understanding of these processes in the context of global warming undoubtedly requires better documentation of dissolved oxygen variability through the implementation of a long-term and continuous in situ monitoring.
dc.description.sponsorshipCOntinental To coastal Ecosystems: evolution, adaptability and governance - ANR-10-LABX-0045en_US
dc.language.isoENen_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subject.enDeoxygenation
dc.subject.enContinental shelf
dc.subject.enSeasonal evolution
dc.subject.enStratification
dc.subject.enBay of Biscay
dc.subject.enDissolved oxygen
dc.title.enFirst observations of seasonal bottom water deoxygenation off the Gironde estuary (Bay of Biscay, North East Atlantic)
dc.typeArticle de revueen_US
dc.identifier.doi10.3389/fmars.2022.1006453en_US
dc.subject.halSciences de l'environnementen_US
dc.description.sponsorshipEuropeJoint European Research Infrastructure network for Coastal Observatory – Novel European eXpertise for coastal observaToriesen_US
bordeaux.journalFrontiers in Marine Scienceen_US
bordeaux.volume9en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.identifierhal-03824842
hal.version1
hal.exportfalse
dc.rights.ccPas de Licence CCen_US
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