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<title lang=en>Sedimentary responses to the Pleistocene climatic variations recorded in the South China Sea</title>
<creator>Boulay, S.</creator>
<creator>Colin, Christophe</creator>
<creator>Trentesaux, A.</creator>
<creator>Clain, S.</creator>
<creator>Liu, Z. F.</creator>
<creator>Leredde, Christine</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>Processus et bilan des domaines sédimentaires (PBDS) ; Université de Lille, Sciences et Technologies - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Laboratoire de Mathématiques Blaise Pascal (LMBP) ; Université Blaise Pascal - Clermont-Ferrand 2 (UBP) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>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: 0033-5894</source>
<source>EISSN: 1096-0287</source>
<source>Quaternary Research</source>
<publisher>Elsevier</publisher>
<identifier>hal-00404671</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00404671</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00404671</source>
<source>Quaternary Research, Elsevier, 2007, 68 (1), pp.162-172. 〈10.1016/j.yqres.2007.03.004〉</source>
<identifier>DOI : 10.1016/j.yqres.2007.03.004</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2007.03.004</relation>
<language>en</language>
<subject lang=en>South China Sea</subject>
<subject lang=en>Grain size</subject>
<subject lang=en>End-members modelling</subject>
<subject lang=en>East Asian monsoon</subject>
<subject lang=en>Mid-Pleistocene Transition</subject>
<subject>[SDU.STU.OC] Sciences of the Universe [physics]/Earth Sciences/Oceanography</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Grain-size analyses, coupled with end-member modelling, have been performed on the terrigenous fraction of two Leg 184 Ocean Drilling Program sites (1144 and 1146) from the South China Sea. The grain-size distributions over the last 1.8 Ma enable a new interpretation of their connections to sea-level variations and East Asian monsoon strength. Previous investigations in this area have associated grain-size variability with enhanced eolian input during glacial stages. End-member modelling downgrades the importance of this eolian contribution and indicates that the sediments can be described as a mixture of three end-members: fluvial mud inputs, shelf reworking and river mouth migration. Grain-size variations in the Pleistocene section of the cores indicate a multiple-stage evolution: (i) from 1.8 to 1.25 Ma, the downcore grain-size variations are low but show a correspondence between monsoon rainfall intensity and the fine grain-sized fluvial inputs; no link with sea-level variations is noticeable; (ii) from 1.25 to 0.9 Ma, there is an increase (decrease) in the intermediate (fine) end-member (not, vert, similar 100 kyr cycle) that is associated with the onset of a stronger summer monsoon and modest shelf reworking; (iii) from 0.9 to 0 Ma the grain-size record is dominated by global sea-level variations; each glacial stage is associated with extensive shelf reworking and conveyance of coarse particles to the basin.</description>
<date>2007</date>
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