{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1360004229805610368.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/2016gc006764"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2F2016GC006764"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GC006764"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/full-xml/10.1002/2016GC006764"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1002/2016GC006764"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Distinct control mechanism of fine‐grained sediments from <scp>Y</scp>ellow <scp>R</scp>iver and <scp>K</scp>yushu supply in the northern <scp>O</scp>kinawa <scp>T</scp>rough since the last glacial"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>High‐resolution multiproxy records, including clay minerals and Sr‐Nd‐Pb isotopes of the clay‐sized silicate fraction of sediments from IODP Site U1429 in the northern Okinawa Trough, provide reliable evidence for distinct control mechanism on fine‐grained sediments input from the Yellow River and the southern Japanese Islands to the northern Okinawa Trough since 34 ka BP. Provenance analysis indicates that the sediments were mainly derived from the Yellow River and the island of Kyushu. Since the last glacial, clay‐sized sediments transported from the Yellow River to the study site were strongly influenced by sea‐level fluctuation. During low sea‐level stage (∼34–14 ka BP), the paleo‐Yellow River mouth was positioned closer to the northern Okinawa Trough, favoring large fluvial discharge or even direct input of detrital sediments, which resulted about four times more flux of clay‐sized sediments supply to the study area as during the relatively high sea‐level stage (∼14–0 ka BP). The input of Kyushu‐derived clay‐sized sediments to the study site was mainly controlled by the Kuroshio Current and Tsushima Warm Current intensity, with increased input in phase with weakened Kuroshio Current/Tsushima Warm Current. Our study suggests that the Kuroshio Current was very likely flowed into the Okinawa Trough and thus influenced the fine‐grained sediment transport in the area throughout the last glacial and deglacial. During ∼34–11 ka BP, the Kyushu clay‐sized sediment input was mainly controlled by the Kuroshio Current. Since ∼11 ka BP, the occurrence of Tsushima Warm Current became important in influencing the Kyushu fine‐grained sediment input to the northern Okinawa Trough.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004229805609987","@type":"Researcher","foaf:name":[{"@value":"Debo Zhao"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences Qingdao China"},{"@value":"College of Earth Sciences University of Chinese Academy of Sciences Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610496","@type":"Researcher","foaf:name":[{"@value":"Shiming Wan"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences Qingdao China"},{"@value":"Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology Qingdao China"},{"@value":"Centre de Recherches Pétrographiques et Géochimiques (CRPG), CNRS‐Université de Lorraine  Cedex France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610244","@type":"Researcher","foaf:name":[{"@value":"Samuel Toucanne"}],"jpcoar:affiliationName":[{"@value":"IFREMER, Unité de Recherche Géosciences Marines, Laboratoire Géophysique et Enregistrements Sédimentaires Plouzané France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610241","@type":"Researcher","foaf:name":[{"@value":"Peter D. Clift"}],"jpcoar:affiliationName":[{"@value":"Department of Geology and Geophysics Louisiana State University Baton Rouge Louisiana USA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610115","@type":"Researcher","foaf:name":[{"@value":"Ryuji Tada"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Planetary Science University of Tokyo Tokyo Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805609857","@type":"Researcher","foaf:name":[{"@value":"Sidonie Révillon"}],"jpcoar:affiliationName":[{"@value":"SEDISOR/UMR 6538 “Domaines Oceaniques”, IUEM, Place Nicolas Copernic Plouzané France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805609984","@type":"Researcher","foaf:name":[{"@value":"Yoshimi Kubota"}],"jpcoar:affiliationName":[{"@value":"Department of Geology National Museum of Nature and Science Ibaraki Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610118","@type":"Researcher","foaf:name":[{"@value":"Xufeng Zheng"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marginal Sea Geology South China Sea Institute of Oceanology, Chinese Academy of Sciences Guangzhou China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610117","@type":"Researcher","foaf:name":[{"@value":"Zhaojie Yu"}],"jpcoar:affiliationName":[{"@value":"Laboratoire GEOsciences Paris‐Sud (GEOPS), UMR8148, CNRS‐Université de Paris‐Sud, Université Paris‐Saclay Orsay Cedex France"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805609988","@type":"Researcher","foaf:name":[{"@value":"Jie Huang"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences Qingdao China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610112","@type":"Researcher","foaf:name":[{"@value":"Hanchao Jiang"}],"jpcoar:affiliationName":[{"@value":"State Key Laboratory of Earthquake Dynamics Institute of Geology, China Earthquake Administration Beijing China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610242","@type":"Researcher","foaf:name":[{"@value":"Zhaokai Xu"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences Qingdao China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610113","@type":"Researcher","foaf:name":[{"@value":"Xuefa Shi"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Sedimentology and Environmental Geology First Institute of Oceanography, SOA Qingdao China"}]},{"@id":"https://cir.nii.ac.jp/crid/1380004229805610116","@type":"Researcher","foaf:name":[{"@value":"Anchun Li"}],"jpcoar:affiliationName":[{"@value":"Key Laboratory of Marine Geology and Environment Institute of Oceanology, Chinese Academy of Sciences Qingdao China"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1890865117698165505","@type":"Researcher","foaf:name":[{"@value":"China Earthquake Adm, Inst Geol, State Key Lab Earthquake 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Technologies - Bordeaux 1-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) ; Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165385","@type":"Researcher","foaf:name":[{"@value":"IFREMER, Unite Rech Geosci Marines, Lab Geophys & Enregistrements Sedimentaires, Plouzane, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165510","@type":"Researcher","foaf:name":[{"@value":"Laboratoire Géosciences Océan (LGO) ; Institut Français de Recherche pour l'Exploitation de la Mer - Brest (IFREMER Centre de Bretagne) ; Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Bretagne Sud (UBS)-Université de Brest (UBO)-Centre National de la Recherche 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Earth and Planetary Science [Tokyo] ; Graduate School of Science [Tokyo] ; The University of Tokyo (UTokyo)-The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165396","@type":"Researcher","foaf:name":[{"@value":"Laboratoire Géosciences Océan (LGO) ; Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165383","@type":"Researcher","foaf:name":[{"@value":"Natl Museum Nat & Sci, Dept Geol, Ibaraki, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165392","@type":"Researcher","foaf:name":[{"@value":"Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China."}]},{"@id":"https://cir.nii.ac.jp/crid/1890865117698165395","@type":"Researcher","foaf:name":[{"@value":"Géosciences Paris Sud (GEOPS) ; Université Paris-Sud - 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