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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>2018-01-15T18:28:24Z</responseDate> <request identifier=oai:HAL:hal-01054332v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01054332v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:MNHN</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:UNIV-PERP</setSpec> <setSpec>collection:IPH-ACTU</setSpec> <setSpec>collection:IPH</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Architecture and composition of the Upper Burdigalian z-coral build-ups of southern Corsica (Mediterranean)</title> <creator>Galloni, Francoise</creator> <creator>Chaix, Christian</creator> <creator>Cornee, Jean-Jacques</creator> <contributor>Histoire naturelle de l'Homme préhistorique (HNHP) ; Centre National de la Recherche Scientifique (CNRS) - Université de Perpignan Via Domitia (UPVD) - Muséum National d'Histoire Naturelle (MNHN)</contributor> <contributor>Bassins ; 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> <source>ISSN: 1631-0713</source> <source>Comptes Rendus Géoscience</source> <publisher>Elsevier Masson</publisher> <identifier>hal-01054332</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01054332</identifier> <source>https://hal.archives-ouvertes.fr/hal-01054332</source> <source>Comptes Rendus Géoscience, Elsevier Masson, 2014, 346 (1-2), pp.45-51. 〈10.1016/j.crte.2014.02.003〉</source> <identifier>DOI : 10.1016/j.crte.2014.02.003</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2014.02.003</relation> <language>en</language> <subject lang=en>Upper Burdigalian</subject> <subject lang=en>Mediterranean</subject> <subject lang=en>Corsica</subject> <subject lang=en>Coral reefs</subject> <subject lang=en>Biodiversity</subject> <subject lang=en>Sedimentary architecture</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>In southern Corsica, three successive Upper Burdigalian coral reef episodes (R1, R2 subdivided into R2A and R2B subunits, and R3) developed within the Cala di Labra Formation. Tabular corals dominated under high water energy and siliciclastic input conditions. The R1 reefs show the highest coral diversity with 16 species described for the first time. A coral impoverishment was recorded in the R2 and R3 reefal episodes. The reefs did not reach a climax growth stage, except the R1 ones. Analogous to North Sardinian reefs, they reflect local vanishing conditions in the Corsican-Sardinian block through Upper Burdigalian because of constant siliciclastic inputs and deepening of the Bonifacio straight.</description> <date>2014</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>