{"@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/1362262944129061632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.palaeo.2004.12.028"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018205000052?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018205000052?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30005405615"}}],"dc:title":[{"@value":"Paleoenvironmental changes in the northern area of the East China Sea during the past 42,000 years"}],"description":[{"notation":[{"@value":"A 33.65-m-long IMAGES (MD982195) core with very high sedimentation rate (ca. 80 cm/kyr), retrieved from the northern part of the East China Sea, was analyzed at 10-cm intervals (about 125 years) for oxygen–carbon isotope of Globigerinoides ruber (sensu stricto), sea surface temperature (SST) from alkenones (U37′K), and principal component analysis of planktonic foraminiferal assemblage. The general pattern of the δ18O curve, resembling the alkenone SST curve, is similar to the standard open ocean oxygen isotope curve. It reveals many light δ18O peaks apparently corresponding to Dansgaard–Oeschger (D–O) cycles as observed in Greenland ice cores for the last 42 ka. The alkenone SST at the core top is 24 °C, which is close to the modern annual mean SST around the core site. On the other hand, SST during the last glacial maximum (LGM) was about 5 °C lower than that in the present day. Alkenone-derived SST does not correlate with the light negative δ18O peaks corresponding to the D–O cycles. The oxygen isotope ratios for the surface waters, based on oxygen isotopes of G. ruber and alkenone SSTs, indicate approximately 1.0‰ increase on average during the LGM and many light peaks at the warm D–O events. This suggests that fresh water was supplied to the core site during these events. The meandering of the westerlies during the cold and warm D–O cycles would have caused an atmospheric tele-connection between East Asia and Greenland.    The core was divided into four periods based on Q-mode factor analysis of the planktonic foraminiferal assemblage, i.e. (1) a strong upwelling period from 42 to 24 ka, indicated by abundant occurrence of Globigerina bulloides, (2) a cold and low salinity water mass period from 24 to 14 ka, suggested by increase of Neogloboquadrina pachyderma, Neogloboquadrina incompta, and Globigerina quinqueloba, (3) a transitional period from cold to warm water masses from 14 to 8 ka, as indicated by the increase of warm water species such as Pulleniatina obliquiloculata and Globigerinoides ruber, and (4) the present-day warm Kuroshio Current condition after 8 ka. The Kuroshio Current flowed into the ECS since the last 42 ka and weakened during the last glacial maximum (LGM) due to the expansion of the coastal water in the northern part of the ECS."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262944129061633","@type":"Researcher","foaf:name":[{"@value":"Akira Ijiri"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944129061634","@type":"Researcher","foaf:name":[{"@value":"Luejiang Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944129061760","@type":"Researcher","foaf:name":[{"@value":"Tadamichi Oba"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944129061632","@type":"Researcher","foaf:name":[{"@value":"Hodaka Kawahata"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944129061635","@type":"Researcher","foaf:name":[{"@value":"Chen-Yue Huang"}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944129061761","@type":"Researcher","foaf:name":[{"@value":"Chi-Yue Huang"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1893399491224709504","@type":"Researcher","foaf:name":[{"@value":"National Taiwan University Dept Phys"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2005-04","prism:volume":"219","prism:number":"3-4","prism:startingPage":"239","prism:endingPage":"261"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031018205000052?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031018205000052?httpAccept=text/plain"}],"createdAt":"2005-02-11","modifiedAt":"2019-01-28","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=550","dc:title":"550"},{"@id":"https://cir.nii.ac.jp/all?q=East%20China%20Sea","dc:title":"East China Sea"},{"@id":"https://cir.nii.ac.jp/all?q=Oxygen%20%26%20carbon%20isotope","dc:title":"Oxygen & carbon isotope"},{"@id":"https://cir.nii.ac.jp/all?q=Tele-connection","dc:title":"Tele-connection"},{"@id":"https://cir.nii.ac.jp/all?q=551","dc:title":"551"},{"@id":"https://cir.nii.ac.jp/all?q=Alkenone%20SST","dc:title":"Alkenone SST"},{"@id":"https://cir.nii.ac.jp/all?q=Planktonic%20foraminiferal%20assemblage","dc:title":"Planktonic foraminiferal assemblage"}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050869456410343808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Intense winter cooling of the surface water in the northern Okinawa Trough during the last glacial period"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216137145344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The role of tephras in developing a high-precision chronostratigraphy for palaeoenvironmental reconstruction and archaeology in southern Kyushu, Japan, since 30,000 cal. 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ages"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679410974208","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"九州西方海域における現生浮遊性有孔虫群集の季節変化"},{"@language":"en","@value":"Seasonal variation in living planktic foraminiferal assemblage in the northeastern part of the East China Sea"},{"@language":"ja-Kana","@value":"キュウシュウ セイホウ カイイキ ニ オケル ゲンセイ フユウセイ ユウコウチュウ グンシュウ ノ キセツ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680197309824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"半遠洋性泥の有機炭素沈積流量変化，最終氷期末期〜後氷期，南海トラフ沿い前弧海盆の例"},{"@language":"en","@value":"Accumulation rate of organic carbon in hemipelagic mud, examples from the forearc basins along the Nankai Trough Japan during the last glacial maximum to deglaciation"},{"@language":"ja-Kana","@value":"ハンエンヨウセイ デイ ノ ユウキ タンソチンセキ リュウリョウ ヘンカ,サイシュウヒョウ キマツキ~コウヒョウキ,ナンカイ トラフ ゾイ ゼン コカイボン ノ レイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213510656","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Abrupt change of sedimentary environment in ca. 7300 years ago recorded in the piston cores from the central Okinawa Trough floor"},{"@language":"ja","@value":"中部沖縄トラフ底で採取されたピストンコアに記録された約7300年前の堆積環境の急激な変化"},{"@language":"ja-Kana","@value":"チュウブ オキナワ トラフテイ デ サイシュサレタ ピストン コア ニ キロクサレタ ヤク 7300ネンマエ ノ タイセキ カンキョウ ノ キュウゲキナ ヘンカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472614400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial time scale changes in surface to intermediate-deep layer circulation recorded in sediment cores from the northwestern North Pacific"},{"@language":"ja","@value":"北西部北太平洋海底堆積物に記録された表層および中・深層循環の1,000年スケール変動"},{"@language":"ja-Kana","@value":"ホクセイブ キタタイヘイヨウ カイテイ タイセキブツ ニ キロク サレタ ヒョウソウ オヨビ チュウ シンソウ ジュンカン ノ 1 000ネン スケール ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681472781568","@type":"Article","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A series of researches on the Quaternary paleoceanographic environments based on oxygen and carbon isotopic ratios of foraminifera fossils in marine sediment cores"},{"@language":"ja","@value":"海底コア中の有孔虫化石の酸素・炭素同位体比を駆使した第四紀古海洋環境に関する一連の研究"},{"@value":"2008年度日本第四紀学会学会賞受賞記念論文 海底コア中の有孔虫化石の酸素・炭素同位体比を駆使した第四紀古海洋環境に関する一連の研究"},{"@language":"ja-Kana","@value":"2008ネンド ニホン ダイ4キ ガッカイ ガッカイショウ ジュショウ キネン ロンブン カイテイ コア チュウ ノ ユウコウチュウ カセキ ノ サンソ タンソ ドウイタイヒ オ クシ シタ ダイ4キ コ カイヨウ カンキョウ ニ カンスル イチレン ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390848250120748032","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Radiocarbon content of carbon dioxide and methane in hydrothermal fluids of Okinawa Trough 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