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<title lang=en>Stable carbon and oxygen isotope compositions of invertebrate carbonate shells and the reconstruction of paleotemperatures and paleosalinities-A case study of the early Pleistocene of Rhodes, Greece</title>
<creator>Lecuyer, Christophe</creator>
<creator>Daux, Valerie</creator>
<creator>Moissette, Pierre</creator>
<creator>Cornee, Jean-Jacques</creator>
<creator>Quillevere, Frederic</creator>
<creator>Koskeridou, Efterpi</creator>
<creator>Fourel, Francois</creator>
<creator>Martineau, Francois</creator>
<creator>Reynard, Bruno</creator>
<contributor>Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE) ; École normale supérieure - Lyon (ENS Lyon) - Université Claude Bernard Lyon 1 (UCBL) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE) ; Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) - Commissariat à l'énergie atomique et aux énergies alternatives (CEA) - Université Paris-Saclay - Centre National de la Recherche Scientifique (CNRS)</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>
<description>International audience</description>
<source>ISSN: 0031-0182</source>
<source>Palaeogeography, Palaeoclimatology, Palaeoecology</source>
<publisher>Elsevier</publisher>
<identifier>hal-00767568</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00767568</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00767568</source>
<source>Palaeogeography, Palaeoclimatology, Palaeoecology, Elsevier, 2012, 350, pp.39-48. 〈10.1016/j.palaeo.2012.06.009〉</source>
<identifier>DOI : 10.1016/j.palaeo.2012.06.009</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2012.06.009</relation>
<language>en</language>
<subject lang=en>Stable isotope</subject>
<subject lang=en>Pleistocene</subject>
<subject lang=en>Rhodes</subject>
<subject lang=en>Mediterranean</subject>
<subject lang=en>Temperature</subject>
<subject lang=en>Salinity</subject>
<subject lang=en>Mollusc</subject>
<subject>[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The coastal sediments of Rhodes in the eastern Mediterranean have recorded transgression-regression cycles that took place during the early Pleistocene. The sedimentary deposits from the Kritika Member of the Rhodes Formation consist in conglomerates, sandstones, siltstones and clays deposited in brackish to shallow marine environments. Faunal associations are dominated by molluscs and reveal rapid ecological changes. Carbon and oxygen isotope ratios of aquatic skeletal carbonates show that these ecological changes were most likely driven by large salinity changes while water temperature remained rather constant at about 22.0 ± 1.5 °C. The tectonic activity of the island rather than glacio-eustatic variations of climatic origin is advocated to be responsible for the ecological and salinity changes and sea-level variations recorded in the sedimentary sequence.</description>
<date>2012-09-15</date>
</dc>
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