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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>2018-01-15T18:38:01Z</responseDate> <request identifier=oai:HAL:halshs-00758748v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:halshs-00758748v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:shs</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:EPHE</setSpec> <setSpec>collection:AO-GEOGRAPHIE</setSpec> <setSpec>collection:INRAP</setSpec> <setSpec>collection:GEODE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:UNIV-AMU</setSpec> <setSpec>collection:MMSH</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-TLSE2</setSpec> <setSpec>collection:SHS</setSpec> <setSpec>collection:PSL</setSpec> <setSpec>collection:IRD</setSpec> <setSpec>collection:LAMPEA</setSpec> <setSpec>collection:INRAP-TEST</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Hurricanes and climate in the Caribbean during the past 3700 years BP</title> <creator>Malaizé, Bruno</creator> <creator>Bertran, Pascal</creator> <creator>Carbonel, Pierre</creator> <creator>Bonnissent, Dominique</creator> <creator>Charlier, Karine</creator> <creator>Galop, Didier</creator> <creator>Imbert, Daniel</creator> <creator>Serrand, Nathalie</creator> <creator>Stouvenot, Christian</creator> <creator>Pujol, C.</creator> <contributor>Environnements et Paléoenvironnements OCéaniques (EPOC) ; Observatoire aquitain des sciences de l'univers (OASU) ; Université Sciences et Technologies - Bordeaux 1 - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - Université Sciences et Technologies - Bordeaux 1 - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Institut National de Recherches Archéologiques Préventives (INRAP) ; Institut national de recherches archéologiques préventives (Inrap)</contributor> <contributor>Laboratoire méditerranéen de préhistoire Europe-Afrique (LAMPEA) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Ministère de la Culture et de la Communication (MCC) - Institut national de recherches archéologiques préventives (Inrap) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Géographie de l'environnement (GEODE) ; Université Toulouse 2 (UT2) - Centre National de la Recherche Scientifique (CNRS)</contributor> <contributor>Université des Antilles et de la Guyane (UAG)</contributor> <contributor>Service régional de l'archéologie - Guadeloupe (SRA Guadeloupe) ; DRAC Guadeloupe</contributor> <contributor>UMR 5805 Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC) ; Observatoire aquitain des sciences de l'univers (OASU) ; Université Sciences et Technologies - Bordeaux 1 - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - Université Sciences et Technologies - Bordeaux 1 - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS)</contributor> <description>International audience</description> <source>ISSN: 0959-6836</source> <source>Holocene</source> <publisher>SAGE Publications</publisher> <identifier>halshs-00758748</identifier> <identifier>https://halshs.archives-ouvertes.fr/halshs-00758748</identifier> <identifier>https://halshs.archives-ouvertes.fr/halshs-00758748/document</identifier> <identifier>https://halshs.archives-ouvertes.fr/halshs-00758748/file/Malaize_et_al._2011_cor.pdf</identifier> <source>https://halshs.archives-ouvertes.fr/halshs-00758748</source> <source>Holocene, SAGE Publications, 2011, 21 (6), pp. 911-924. 〈10.1177/0959683611400198〉</source> <identifier>DOI : 10.1177/0959683611400198</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1177/0959683611400198</relation> <language>en</language> <subject lang=en>Caribbean sea</subject> <subject lang=en>coastal lake</subject> <subject lang=en>hurricanes</subject> <subject lang=en>late-Holocene climate</subject> <subject lang=en>ostracods</subject> <subject lang=en>Saint-Martin island</subject> <subject lang=en>stable isotopes</subject> <subject>[SHS.GEO] Humanities and Social Sciences/Geography</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>A multiproxy analysis of lacustrine sediments cored in Grand-Case Pond at Saint-Martin, north of the Lesser Antilles archipelago, reveals three distinct climatic periods for the last 3700 years. From 3700 to ~2500 yr cal. BP and from 1150 yr cal. BP to the present, carbonate mud deposition occurred in connection with pond lowstands. These periods were also punctuated by severe drought events, marked by gypsum laminae, and hurricane landfalls, leading to marine sand inputs into the pond. The intermediate time interval, from 2500 to 1150 yr cal. BP, is typified by black organic mud deposition, suggesting that hypoxic to anoxic conditions prevailed at the pond bottom. These were probably linked with a perennial pond highstand and reflect more uniform and wetter climatic conditions than today. The carbon isotopic composition of the ostracod Perissocytheridea bisulcata shows that the lowest δ13C values are recorded during the hypoxic periods, as a consequence of bacterial recycling of isotopically depleted organic matter. Such a climatic history agrees closely with that documented from other records in the Caribbean area, such as the Cariaco Basin, central coast of Belize or Barbados. By constrast, discrepancies seem to emerge from the comparison between hurricane activity recorded at Saint-Martin on the one hand and Vieques (Puerto Rico) on the other hand. We explain this apparent contradiction by a balance between two distinct storm paths in response to latitudinal shifts of the Intertropical Convergence Zone (ITCZ). Stronger storm activity over the Gulf coast and the inner Caribbean Sea is favoured by a southern position of the ITCZ in connection with dry climatic conditions. Plausible links with the North Atlantic Oscillation (NAO) are also suggested.</description> <date>2011</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>