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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T15:41:32Z</responseDate> <request identifier=oai:HAL:hal-00411189v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00411189v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-BREST</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:UMR5140</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:GEOPS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-PSUD</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Reconstruction of paleostorm events in a coastal lagoon (Herault, South of France)</title> <creator>Sabatier, Pierre</creator> <creator>Dezileau, Laurent</creator> <creator>Condomines, Michel</creator> <creator>Briqueu, Louis</creator> <creator>Colin, Christophe</creator> <creator>Bouchette, Frederic</creator> <creator>Le Duff, M.</creator> <creator>Blanchemanche, P.</creator> <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>Interactions et dynamique des environnements de surface (IDES) ; Université Paris-Sud - Paris 11 (UP11) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Université de Brest (UBO)</contributor> <contributor>Archéologie des Sociétés Méditerranéennes (ASM) ; Centre National de la Recherche Scientifique (CNRS) - Université Paul-Valéry - Montpellier 3 (UM3) - Ministère de la Culture et de la Communication (MCC)</contributor> <source>ISSN: 0025-3227</source> <source>Marine Geology</source> <publisher>Elsevier</publisher> <identifier>hal-00411189</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00411189</identifier> <source>https://hal.archives-ouvertes.fr/hal-00411189</source> <source>Marine Geology, Elsevier, 2008, 251 (3-4), pp.224-232, doi:. 〈10.1016/j.margeo.2008.03.001〉</source> <identifier>DOI : 10.1016/j.margeo.2008.03.001</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.margeo.2008.03.001</relation> <language>en</language> <subject lang=en>paleostorms</subject> <subject lang=en>lagoon</subject> <subject lang=en>Mediterranean Sea</subject> <subject lang=en>grain size</subject> <subject lang=en>accumulation rates</subject> <subject lang=en>210Pb-Pb-210 geochronology</subject> <subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>Finding records of past catastrophic storm events is essential to evaluate the long term climatic evolution in a given coastal area. This question has been addressed by the study of sediment cores sampled in a small coastal lagoon of the French Mediterranean coast (Pierre Blanche lagoon). Two cores were studied in detail and revealed the presence of three main storm events. The sedimentation rates calculated using the CFCS Pb-210 model, in agreement with Cs-137 data, are 3 +/- 0.4 and 4.2 +/- 0.7 mm y(-1) near the border and in the center of the lagoon respectively. This suggests that the 0.6 m deep lagoon could be filled with sediments over the next 150 yr. Our study shows that storm events can be characterized in sedimentary sequences identified by facies, grain size and faunal assemblages (lagoonal and marine species). Comparison of Pb-210, C-14 chronology and historical accounts suggest that the three identified storm events took place in 1742, 1839 and 1893 A.D. (i.e. about one catastrophic event per century).</description> <date>2008</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>