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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorFOUET, Marie
hal.structure.identifierLaboratoire de Planétologie et Géosciences - Angers [LPG-ANGERS]
dc.contributor.authorDAVIRAY, Maxime
hal.structure.identifierLaboratoire de Planétologie et Géosciences - Angers [LPG-ANGERS]
dc.contributor.authorGESLIN, Emmanuelle
hal.structure.identifierLaboratoire de Planétologie et Géosciences [UMR_C 6112] [LPG]
dc.contributor.authorMETZGER, Edouard
hal.structure.identifierLaboratoire de Planétologie et Géosciences - Angers [LPG-ANGERS]
dc.contributor.authorJORISSEN, Frans
dc.date.accessioned2025-04-09T09:14:31Z
dc.date.available2025-04-09T09:14:31Z
dc.date.issued2024
dc.identifier.issn1631-0713en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/206064
dc.description.abstractEnForaminiferal mudflat communities in the Auray estuary, located along the French Northwest Atlantic coast, were investigated in September 2020. Numerous living specimens of calcareous species showed marks of dissolution. The number of affected individuals, together with their dissolution degree, varied from one site to another. Moreover, pH profiles showed porewater acidification of the subsurface sediment at several stations. We propose two metrics quantifying the degree of dissolution: (i) the “Foraminiferal Test Dissolution” (FTD), based on binocular observations of the foraminiferal community, and (ii) the “Calcareous Test Preservation Ratio” (CTPR), surface ratio (0– 0.5 cm) of total living foraminiferal densities (0–1 cm). In stations showing sediment acidification, the O2-pH profiles show the typical biogeochemical signatures of cable bacteria activity (pH increase in the oxic zone followed by strong acidification in the suboxic zone). This suggests that bacterial activity could be responsible for the strong pH decrease leading to corrosive porewaters affecting calcareous tests, hence severe FTD in the first centimetre of sediment leading to high CTPR. Furthermore, observations of FTD in other estuaries on the French Atlantic coast indicate that the phenomenon has becomewidespread. Re-investigated foraminiferal tests sampled in 1995–1996 in the Auray estuary show no dissolution marks, suggesting that the dissolution process observed in 2020 appeared over the last thirty years. Therefore, the FTD and CTPR could be used as rapid tools to establish the occurrence of dissolution processes, pending geochemical confirmation. The FTD could also be used as sediment acidification proxy in historical records, where geochemical analyses are not possible.
dc.language.isoENen_US
dc.subject.enBenthic foraminifera
dc.subject.enCable bacteria
dc.subject.enTest preservation
dc.subject.enSediment acidification proxy
dc.titleLa dissolution de tests de foraminifères révèle une acidification sévère des sédiments dans les vasières estuariennes : nouvelles perspectives pour l’évaluation actuelle et historique
dc.title.enForaminiferal test dissolution reveals severe sediment acidification in estuarine mudflats: new perspectives for present and historical assessment
dc.typeArticle de revueen_US
dc.identifier.doi10.5802/crgeos.269en_US
dc.subject.halPlanète et Univers [physics]/Sciences de la Terreen_US
bordeaux.journalComptes Rendus. Géoscienceen_US
bordeaux.page83-96en_US
bordeaux.volume356en_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
bordeaux.import.sourcehal
hal.identifierhal-04634736
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
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