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<title lang=en>Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: The Mediterranean GOLD project#</title>
<creator>Rabineau, Marina</creator>
<creator>Cloetingh, S</creator>
<creator>Kuroda, J</creator>
<creator>Aslanian, D</creator>
<creator>Droxler, A</creator>
<creator>Gorini, Christian</creator>
<creator>Garcia-Castellanos, D</creator>
<creator>Moscariello, A</creator>
<creator>Burov, Evgenii</creator>
<creator>Sierro, F</creator>
<creator>Lirer, F</creator>
<creator>Roure, F</creator>
<creator>Pezard, P.A.</creator>
<creator>Matenco, L</creator>
<creator>Hello, Y</creator>
<creator>Mart, Y</creator>
<creator>Camerlenghi, A</creator>
<creator>Tripati, A</creator>
<contributor>Domaines Océaniques (LDO) ; Centre National de la Recherche Scientifique (CNRS) - Institut d'écologie et environnement - Observatoire des Sciences de l'Univers - Université de Brest (UBO) - Institut national des sciences de l'Univers (INSU - CNRS)</contributor>
<contributor>Utrecht University [Utrecht]</contributor>
<contributor>Japan Agency for Marine-Earth Science and Technology (JAMSTEC)</contributor>
<contributor>Unité de recherche Géosciences Marines (Ifremer) (GM) ; Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)</contributor>
<contributor>department of earth science ; Rice University [Houston]</contributor>
<contributor>Institut des Sciences de la Terre de Paris (iSTeP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Instituto de Ciencias de la Tierra Jaume Almera</contributor>
<contributor>University of Geneva ; Université de Genève (UNIGE)</contributor>
<contributor>University of Salamanca</contributor>
<contributor>Istituto Ambiente Marino Costiero ; Consiglio Nazionale delle Ricerche (CNR)</contributor>
<contributor>IFP Energies nouvelles (IFPEN)</contributor>
<contributor>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)</contributor>
<contributor>Géoazur (GEOAZUR) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire de la Côte d'Azur - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>University of Haifa [Haifa]</contributor>
<contributor>OGS—Istituto Nazionale di Oceanografia e Geofisica Sperimentale ; OGS—Istituto Nazionale di Oceanografia e Geofisica Sperimentale</contributor>
<contributor>Institute of the Environment and Sustainability, Los Angeles, CA 90095, United States</contributor>
<contributor>Departments of Atmospheric and Oceanic Sciences, Los Angeles, CA 90095, United States</contributor>
<description>International audience</description>
<source>ISSN: 0264-8172</source>
<source>Marine and Petroleum Geology</source>
<publisher>Elsevier</publisher>
<identifier>insu-01197393</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01197393</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01197393/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-01197393/file/Rabineau%20et%20al.-final-MPG2014_REVISED-FINAL-No-Marked_FINAL%2BFigures.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-01197393</source>
<source>Marine and Petroleum Geology, Elsevier, 2015, pp.6-17. 〈10.1016/j.marpetgeo.2015.03.018〉</source>
<identifier>DOI : 10.1016/j.marpetgeo.2015.03.018</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.marpetgeo.2015.03.018</relation>
<language>en</language>
<subject lang=en>Paleoclimate</subject>
<subject lang=en>Georesources</subject>
<subject lang=en>Messinian erosional and salinity crisis</subject>
<subject lang=en>Deep biosphere</subject>
<subject lang=en>Deep drilling</subject>
<subject lang=en>Geodynamics</subject>
<subject lang=en>Passive margins</subject>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>During the last decade, the interaction of deep processes in the lithosphere and mantle with surface processes (erosion, climate, sea-level, subsidence, glacio-isostatic readjustment) has been the subject of heated discussion. The use of a multidisciplinary approach linking geology, geophysics, geodesy, modelling, and geotechnology has led to the awareness of coupled deep and surface processes. Deep earth dynamics (topography, erosion, tectonics) are strongly connected to natural hazards such as earthquakes, landslides, and tsunamis; sedimentary mass transfers have important consequences on isostatic movements and on georesources, geothermal energy repartitions. The ability to read and understand the link between deep Earth dynamics and surface processes has therefore important societal impacts. Ground-truthing at carefully-selected sites of investigation is imperative to better understand these connections.Due to its youth (<30 Ma) and its subsidence history, the almost land-locked Gulf of Lion–Sardinia continental margins system provides a unique record of sedimentary deposition from the Miocene to present. Due to its high subsidence rate, palaeoclimatic variations, tectonic events and vertical evolution are all recorded here at very high resolution. The late Miocene isolation and desiccation of the Mediterranean, the youngest and most catastrophic event, the Messinian Salinity Crisis (MSC), induced drastic changes in marine environments: widespread deposition of evaporite (gypsum, anhydrite and halite) in the central basin, and intense subaerial erosion along its periphery. These extraordinary mass transfers from land to sea induced strong isostatic re-adjustments that are archived in the sedimentary record and represent a window to the lithospheric rheology and the deep processes.The GOLD (Gulf of Lion Drilling) project, proposes to explore this unique sedimentary record as well as the nature of the deep crustal structure, providing valuable information about the mechanisms underlying vertical motions in basins and their margins.</description>
<date>2015-09-01</date>
<contributor>ANR-10-LABX-0019/10-LABX-0019, LabexMER, LabexMER Marine Excellence Research: a changing ocean(2010)</contributor>
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