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dc.rights.licenseopenen_US
hal.structure.identifierDepartamento de Geoquímica
dc.contributor.authorCOTOVICZ, Luiz
hal.structure.identifierDepartamento de Geoquímica
dc.contributor.authorKNOPPERS, Bastiaan
hal.structure.identifierPrograma de Pós-Graduação em Geografia - Universidade Federal do Rio Grande do Sul [POSGEA-UFRGS]
dc.contributor.authorBRANDINI, Nilva
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorPOIRIER, Dominique
hal.structure.identifierDepartamento de Geoquímica
dc.contributor.authorCOSTA SANTOS, Suzan
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
hal.structure.identifierLaboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques [LOCEAN]
dc.contributor.authorABRIL, Gwenaël
dc.date.accessioned2024-04-24T09:12:44Z
dc.date.available2024-04-24T09:12:44Z
dc.date.issued2018-04
dc.identifier.issn0025-326Xen_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/199296
dc.description.abstractEnThe dynamics of the aragonite saturation state (Ωarag) were investigated in the eutrophic coastal waters of Guanabara Bay (RJ-Brazil). Large phytoplankton blooms stimulated by a high nutrient enrichment promoted the production of organic matter with strong uptake of dissolved inorganic carbon (DIC) in surface waters, lowering the concentrations of dissolved carbon dioxide (CO2aq), and increasing the pH, Ωarag and carbonate ion (CO32 −), especially during summer. The increase of Ωarag related to biological activity was also evident comparing the negative relationship between the Ωarag and the apparent utilization of oxygen (AOU), with a very close behavior between the slopes of the linear regression and the Redfield ratio. The lowest values of Ωarag were found at low-buffered waters in regions that receive direct discharges from domestic effluents and polluted rivers, with episodic evidences of corrosive waters (Ωarag < 1). This study showed that the eutrophication controlled the variations of Ωarag in Guanabara Bay.
dc.language.isoENen_US
dc.subject.enCarbonate chemistry
dc.subject.enCoastal eutrophication
dc.subject.enCoastal acidification
dc.subject.enPhytoplankton blooms
dc.subject.enCarbonate chemistry
dc.title.enAragonite saturation state in a tropical coastal embayment dominated by phytoplankton blooms (Guanabara Bay – Brazil)
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.marpolbul.2017.10.064en_US
dc.subject.halPhysique [physics]/Physique [physics]/Géophysique [physics.geo-ph]en_US
dc.subject.halSciences de l'environnement/Milieux et Changements globauxen_US
bordeaux.journalMarine Pollution Bulletinen_US
bordeaux.page729 - 739en_US
bordeaux.volume129en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.issue2en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamECOBIOCen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-01835874
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&amp;rft_val_fmt=info:ofi/fmt:kev:mtx:journal&amp;rft.jtitle=Marine%20Pollution%20Bulletin&amp;rft.date=2018-04&amp;rft.volume=129&amp;rft.issue=2&amp;rft.spage=729%20-%20739&amp;rft.epage=729%20-%20739&amp;rft.eissn=0025-326X&amp;rft.issn=0025-326X&amp;rft.au=COTOVICZ,%20Luiz&amp;KNOPPERS,%20Bastiaan&amp;BRANDINI,%20Nilva&amp;POIRIER,%20Dominique&amp;COSTA%20SANTOS,%20Suzan&amp;rft.genre=article


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