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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Geophysical and geomorphological investigations of a Quaternary karstic paleolake and its underground marine connection in Cassis (Bestouan, Cassis, SE France)</title>
<creator>Romey, Carole</creator>
<creator>Rochette, Pierre</creator>
<creator>Vella, Claude</creator>
<creator>Arfib, Bruno</creator>
<creator>Andrieu-Ponel, Valérie</creator>
<creator>BRAUCHER, Regis</creator>
<creator>Champollion, Cedric</creator>
<creator>Douchet, Marc</creator>
<creator>DUSSOUILLEZ, Philippe</creator>
<creator>Hermitte, Daniel</creator>
<creator>Mattioli, Emanuela</creator>
<creator>Parisot, Jean-Claude</creator>
<creator>Schwenninger, Jean-Luc</creator>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Institut méditerranéen de biodiversité et d'écologie marine et continentale (IMBE) ; Université d'Avignon et des Pays de Vaucluse (UAPV) - Aix Marseille Université (AMU) - Institut national des sciences de l'Univers (INSU - CNRS) - INEE - INSB - Institut de recherche pour le développement [IRD] : UMR237 - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Claude Bernard Lyon 1 (UCBL) - École normale supérieure - Lyon (ENS Lyon)</contributor>
<contributor>University of Oxford [Oxford]</contributor>
<description>International audience</description>
<source>ISSN: 0169-555X</source>
<source>Geomorphology</source>
<publisher>Elsevier</publisher>
<identifier>hal-01054334</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01054334</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01054334</source>
<source>Geomorphology, Elsevier, 2014, 214, pp.402-415. 〈10.1016/j.geomorph.2014.02.021〉</source>
<identifier>DOI : 10.1016/j.geomorph.2014.02.021</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.geomorph.2014.02.021</relation>
<language>en</language>
<subject lang=en>Karst</subject>
<subject lang=en>Provence</subject>
<subject lang=en>Geophysical prospection</subject>
<subject lang=en>Submarine spring</subject>
<subject lang=en>Paleolake</subject>
<subject lang=en>Cassis</subject>
<subject lang=en>Bestouan</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<subject>[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>An original karstic system in a coastal alluvial plain located in a carbonate environment (Cassis, Provence -- SE France) was studied using a multi-method approach (electrical resistivity tomography, gravimetric, passive seismic survey), combined with geomorphologic methods, surface observations and drilling. Limestone dissolution and/or cavity collapse led to the development of a polje, which was filled rapidly by erosion of Aptian marls. The combination of several dating and paleoenvironmental proxies indicates that the polje was filled during a glacial period (MIS 6, 8 or 10, i.e. in the 130-360 ka age range). This discovery has implications for the understanding of karst processes. The connection between the polje and the three km-long Bestouan underwater karstic conduit with submarine outlet is strongly suggested by sedimentological studies and geophysical prospections.</description>
<date>2014-06-01</date>
</dc>
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