{"@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/1362825895478786944.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gloplacha.2006.05.002"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0921818106000907?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0921818106000907?httpAccept=text/plain"}}],"dc:title":[{"@value":"Paleoceanographic change off central Japan since the last 144,000 years based on high-resolution oxygen and carbon isotope records"}],"description":[{"notation":[{"@value":"Abstract   Very large sea surface temperature (SST) fluctuations are expected in the northwest Pacific Ocean between glacial and interglacial periods due to possible latitudinal migrations of the steep SST front between the Oyashio and Kuroshio Currents. To reconstruct the SST changes for the past 144,000 years, we conducted high-resolution oxygen and carbon isotope analysis of both benthic and planktonic foraminifera from an IMAGES core off central Japan. Using a newly developed method [Oba, T., Murayama, M., 2004. Sea surface temperature and salinity changes in the northwest Pacific since the last glacial maximum. J. Quat. Sci. 19(4), 335–346] for the reconstruction of the SST, we have found very large (∼ 20 °C) SST fluctuations, with minimum SSTs of 3–4 °C during Marine Isotope Stage (MIS) 2 and the MIS 6/5e transition, and with peak SSTs of 22–23 °C during early MIS 1 and the MIS 5a/4, 5c/5b and 5e/5d transitions. The SSTs varied in parallel with changing carbon isotope differences between  Globorotalia inflata  and  Globigerina bulloides , which suggests that the SST changes were primarily caused by the latitudinal displacements of the Kuroshio–Oyashio Currents. We have also found that northward shifts of the Kuroshio Current lagged up to several thousand years at these transitions. Strong correlation between the SST shifts and orbital forcing indicates that the latitudinal displacements of the Kuroshio–Oyashio Currents were influenced by summer insolation at 65°N associated with ENSO-like climatic variability in the tropical Pacific."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825895478786944","@type":"Researcher","foaf:name":[{"@value":"Tadamichi Oba"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895478786947","@type":"Researcher","foaf:name":[{"@value":"Tomohisa Irino"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895478786945","@type":"Researcher","foaf:name":[{"@value":"Masanobu Yamamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895478786946","@type":"Researcher","foaf:name":[{"@value":"Masafumi Murayama"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895478786948","@type":"Researcher","foaf:name":[{"@value":"Akira Takamura"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825895478786949","@type":"Researcher","foaf:name":[{"@value":"Kaori Aoki"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09218181"}],"prism:publicationName":[{"@value":"Global and Planetary Change"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2006-08","prism:volume":"53","prism:number":"1-2","prism:startingPage":"5","prism:endingPage":"20"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0921818106000907?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0921818106000907?httpAccept=text/plain"}],"createdAt":"2006-07-06","modifiedAt":"2019-01-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213761277952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnections with ice melt in the North Atlantic"},{"@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnection with ice melt in the North Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1050008763985565824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the EarlyeMiddle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records through Marine Isotope Stage 19 at the Chiba composite section, central Japan: A key reference for the Early–Middle Pleistocene Subseries boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early–Middle Pleistocene boundary"},{"@value":"Paleoclimatic and paleoceanographic records of Marine Isotope Stage 19 at the Chiba composite section, central Japan: a reference for the Early-Middle Pleisotocene boundary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216146325120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vegetation and endemic tree response to orbital-scale climate changes in the Japanese archipelago during the last glacial–interglacial cycle based on pollen records from Lake Biwa, western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232469004288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-resolution diatom record of paleoceanographic variations across the Early–Middle Pleistocene boundary in the Chiba Section, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233286387840","@type":"Article","resourceType":"学術雑誌論文(journal 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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/1390282681473831552","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Comparison of Interglacial Warm Events since the Marine Oxygen Isotope Stage 11"},{"@language":"ja","@value":"海洋酸素同位体ステージ11以降の間氷期最温暖期の比較"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681473938944","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast, Japan"},{"@language":"ja","@value":"鹿島沖海底コアMD01-2421の後期更新世テフラ層序"},{"@language":"ja-Kana","@value":"カシマオキ カイテイ コア MD01 2421 ノ コウキ コウシンセイ テフラ ソウジョ"},{"@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast, Japan (in Japanese with English summary)"},{"@value":"Late Pleistocene tephrostratigraphy of the sediment core MD01-2421 collected off the Kashima coast"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763107304576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A summary of the Chiba Section, Japan"},{"@language":"ja","@value":"千葉セクション"},{"@value":"千葉セクション : 下部-中部更新統境界の国際境界模式層断面とポイントへの提案書(要約)"},{"@language":"ja-Kana","@value":"チバ セクション : カブ-チュウブ コウシントウ キョウカイ ノ コクサイ キョウカイモシキソウ ダンメン ト ポイント エ ノ テイアンショ(ヨウヤク)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238110483712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy, distribution patterns, and ground motion characteristics of the 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