{"@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/1360011142932817792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/91pa00560"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F91PA00560"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/91PA00560"}},{"identifier":{"@type":"NAID","@value":"30034782702"}}],"dc:title":[{"@value":"Paleoenvironmental Changes in the Japan Sea During the Last 85,000 Years"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Five distinct changes in the paleoenvironment of the Japan Sea within the last 85,000 years are revealed from the sedimentary record of a piston core recovered from the Oki Ridge. Changes in both surface and deepwater conditions are registered by changes in lithology, calcium carbonate content, organic carbon content, oxygen and carbon isotope ratios, and microfossil assemblages including calcareous nannoplankton, diatoms, radiolaria, and foraminifera. Between 85 and 27 ka the warm Tsushima Current did not flow into the Japan Sea, and cold surface water conditions prevailed. Environments at the seafloor fluctuated between dysaerobic to weakly oxic conditions. Between 27 and 20 ka, freshwater input to the Japan Sea, probably from the Huang Ho River in China, stratified the water column, and the severe anoxic conditions eliminated most benthic fauna. Between 20 and 10 ka the cold Oyashio Current flowed into the Japan Sea through the Tsugaru Strait, reestablishing deepwater ventilation. Shallow water benthic assemblages of the North Pacific Ocean subsequently colonized the Japan Sea and occupied the vacant niches of the deep basins. Between 10 and 8 ka the foraminifer compensation level (FCL) gradually rose to a depth shallower than 1000 m, and bottom conditions changed from dysaerobic to oxic. At 10 ka the warm Tsushima Current started to flow into the Japan Sea through the Tsushima Strait to establish the modern oceanographic regime which has existed since 8 ka. The eustatic sea level during the last glacial maximum was above the sill depths (130 m) of the Tsushima and Tsugaru straits, assuming that tectonic movements at these straits were negligible for the last 20 ka.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1580854176423868160","@type":"Researcher","foaf:name":[{"@value":"T. Oba"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817798","@type":"Researcher","foaf:name":[{"@value":"M. Kato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817797","@type":"Researcher","foaf:name":[{"@value":"H. Kitazato"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817793","@type":"Researcher","foaf:name":[{"@value":"I. Koizumi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817792","@type":"Researcher","foaf:name":[{"@value":"A. Omura"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817795","@type":"Researcher","foaf:name":[{"@value":"T. Sakai"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011142932817794","@type":"Researcher","foaf:name":[{"@value":"T. Takayama"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08838305"},{"@type":"EISSN","@value":"19449186"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/08838305"}],"prism:publicationName":[{"@value":"Paleoceanography"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1991-08","prism:volume":"6","prism:number":"4","prism:startingPage":"499","prism:endingPage":"518"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F91PA00560"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/91PA00560"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282676670281984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Population 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Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855118504832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The population structure and demography of an intertidal gastropod Lunella correensis around the Japanese Archipelago affected by past environmental change"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412890800589568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Genetic isolation by distance in the yellowfin goby populations revealed by RAD sequencing"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204086233600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Water temperature, salinity ranges and ecological significance of the three families of Recent cold-water ostracods in and around the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204228649472","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of Recent Benthic Foraminifera in the Methane Seepage Area off Joetsu in the Eastern Japan Sea"},{"@language":"ja","@value":"上越沖海底メタン湧出地域の現世底生有孔虫群集"},{"@language":"ja-Kana","@value":"ジョウエツオキ カイテイ メタン ユウシュツ チイキ ノ ゲンセイ テイセイ ユウコウチュウ グンシュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266156672","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"北部日本海盆深海底より採取された柱状試料"},{"@language":"en","@value":"Piston core sample collected from the northern Japan Basin deep-sea floor"},{"@value":"北部日本海盆深海底より採取された柱状資料"},{"@language":"ja-Kana","@value":"ホクブ ニホンカイボン シンカイテイ ヨリ サイシュ サレタ チュウジョウ シリョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204434608384","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"過去64万年間の日本海における深海性放散虫の変遷(<特集>日本海の生物相の変遷と環境変動-過去,現在そして未来へ向けて)"},{"@language":"en","@value":"Historical changes of deep-sea radiolarians in the Japan Sea during the last 640 kyrs"},{"@value":"過去64万年間の日本海における深海性放散虫の変遷"},{"@language":"ja-Kana","@value":"カコ 64マンネンカン ノ ニホンカイ ニ オケル シンカイセイ ホウサンチュウ ノ ヘンセン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204434752128","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"日本海における深海生物相形成と海洋環境変動 : 深海性底魚を例として(<特集>日本海の生物相の変遷と環境変動-過去,現在そして未来へ向けて)"},{"@language":"en","@value":"Formation of deep-sea fauna and changes of marine environment in the Japan Sea"},{"@value":"日本海における深海生物相形成と海洋環境変動--深海性底魚を例として"},{"@language":"ja-Kana","@value":"ニホンカイ ニ オケル シンカイ セイブツソウ ケイセイ ト カイヨウ カンキョウ ヘンドウ シンカイセイ ソコウオ オ レイ ト シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204551716608","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Carbon isotopic composition of sterols in geochemical samples."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205265515520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Genetic divergence of <i>Argis lar</i> and <i>A. hozawai</i>, distinct sibling species of deep-sea crangonid shrimp from the Sea of Japan"},{"@value":"Genetic divergence of Argis lar and A. hozawai, distinct sibling species of deep-sea crangonid shrimp from the Sea of Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205473300608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy","isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Phylogeography and population structure of the Dall's porpoise, Phocoenoides dalli, in Japanese waters revealed by mitochondrial DNA."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234599552","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Marine sediments and late Quaternary stratigraphy in the southeastern part of the Japan Sea. Concerning the timing of dark layer deposition."},{"@value":"日本海南東部における海底堆積物と後期第四紀層序　特に暗色層の形成時期に関連して"},{"@language":"ja-Kana","@value":"ニホンカイ ナントウブ ニ オケル カイテイ タイセキブツ ト コウキ ダイ4"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206235331584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tephrostratigraphy of the piston cored sediment KT96-17 P-2 in the southern Japan Sea. 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