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<datestamp>2018-01-11</datestamp>
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<title lang=en>Reconstruction of Northern African monsoon between 6.2 and 4.9 Ma and possible relationships with Late Miocene events</title>
<creator>Colin, Christophe</creator>
<creator>Siani, G.</creator>
<creator>Seguenia, F.</creator>
<creator>Blamart, D.</creator>
<creator>Giunta, S.</creator>
<creator>Suc, J. P.</creator>
<creator>Liu, Z.</creator>
<creator>Frank, N.</creator>
<creator>Briqueu, Louis</creator>
<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>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>Dipartimento di Scienze del Mare ; Università Politecnica delle Marche [Ancona] (UNIVPM)</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>State Key Laboratory of Marine Geology, Tongji University, Shanghai ; Université du Québec</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>
<source>ISSN: 1631-0713</source>
<source>Comptes Rendus Géoscience</source>
<publisher>Elsevier Masson</publisher>
<identifier>hal-00412151</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00412151</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00412151</source>
<source>Comptes Rendus Géoscience, Elsevier Masson, 2008, 340 (11), pp.749-760. 〈10.1016/j.crte.2008.07.005〉</source>
<identifier>DOI : 10.1016/j.crte.2008.07.005</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2008.07.005</relation>
<language>en</language>
<subject lang=en>African monsoon</subject>
<subject lang=en>dust input</subject>
<subject lang=en>Messinian salinity crisis</subject>
<subject lang=en>stable-isotope stratigraphy</subject>
<subject lang=en>atlantic-ocean</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</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>Reconstruction of Northern African monsoon between 6.2 and 4.9 Ma and possible relationships with Late Miocene events. Mineralogical and geochemical investigations have been realized on ODP Site 659 in order to better understand the detrital sedimentation of the Cap Verde plateau and to reconstruct African monsoon intensity variations between 6.2 and 4.9 Ma. Time intervals corresponding to an intensification of the summer African monsoon rainfall are associated to a reduction of eolian input from the Sahara and an intensification of the African river input. The reflooding of the Mediterranean Sea at the end of the Messinian salinity crisis (MSC) (5.33 Ma) is correlated to a greater aridity in the Sahara.</description>
<date>2008</date>
</dc>
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