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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>2018-01-15T15:39:45Z</responseDate> <request identifier=oai:HAL:hal-00470360v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00470360v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-FCOMTE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:LGL-TPE</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:CHRONO-ENVIRONNEMENT</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>Changes in vegetation and marine environments in the eastern Mediterranean (Rhodes Island, Greece) during the Early and Middle Pleistocene</title> <creator>Joannin, Sebastien</creator> <creator>Cornée, J.-J.</creator> <creator>Moissette, Pierre</creator> <creator>Suc, J.P.</creator> <creator>Koskeridou, Efterpi</creator> <creator>Lecuyer, C.</creator> <creator>Buisine, Cédric</creator> <creator>Kouli, K.</creator> <creator>Ferry, S.</creator> <contributor>Laboratoire Chrono-environnement (LCE) ; Université Bourgogne Franche-Comté (UBFC) - Centre National de la Recherche Scientifique (CNRS) - Université de Franche-Comté (UFC)</contributor> <contributor>Paléoenvironnement et paléobiosphère (PP) ; Université Claude Bernard Lyon 1 (UCBL) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</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>Department of Historical Geology-Paleontology, University of Athens ; National Technical University of Athens</contributor> <description>International audience</description> <source>Journal of the Geological Society, London</source> <identifier>hal-00470360</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00470360</identifier> <source>https://hal.archives-ouvertes.fr/hal-00470360</source> <source>Journal of the Geological Society, London, 2007, 164, pp.1119-1131</source> <language>en</language> <subject lang=fr>STABLE-ISOTOPE</subject> <subject lang=fr>POLLEN RECORD</subject> <subject lang=fr>PLEISTOCENE</subject> <subject lang=fr>CLIMATE</subject> <subject lang=fr>OXYGEN</subject> <subject lang=fr>TIME</subject> <subject lang=fr>EVOLUTION</subject> <subject lang=fr>SEDIMENTS</subject> <subject lang=fr>NAUTILUS</subject> <subject lang=fr>SEA</subject> <subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</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>Pollen records, marine faunal associations and stable isotope compositions of sediments from Rhodes, Greece, have been determined to track environmental changes in the eastern Mediterranean during the Early and Middle Pleistocene. A detailed chronostratigraphic curve, based on magnetostratigraphic data, was obtained by correlating pollen spectra with the Mediterranean oxygen isotopic curve of Ocean Drilling Program Site 975. Five sedimentary sequences that correspond to marine oxygen isotope stage (MIS) 31–27 and to MIS 20–17 have been investigated in the confined Tsampika microbasin. High-amplitude Pinus variations confirm glacio-eustatic changes deduced from changes in marine faunal associations and sedimentary depositional environments. Reflecting climatic cycles identified in the marine carbonate oxygen isotope record, eight vegetation successions (characterized by the dominance first of mesothermic elements, then of mid- and high-altitude elements with Pinus, and ending with maxima in herb and steppe elements) have been documented. Most of them were probably driven by changes in insolation occurring in high northern latitudes (obliquity impact) during the late Early Pleistocene and early Middle Pleistocene.</description> <date>2007-05-04</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>