{"@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/1360855568614709632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000pa000557"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000PA000557"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000PA000557"}},{"identifier":{"@type":"NAID","@value":"30013358188"}}],"dc:title":[{"@value":"Millennial‐scale dynamics of the east Asian winter monsoon during the last 200,000 years"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The primary productivity dynamics of the last 200,000 years in the Sulu Sea was reconstructed using the abundance of the coccolithophore <jats:italic>Florisphaera profunda</jats:italic> in the IMAGES MD97‐2141 core. We find that primary productivity was enhanced during glacial periods, which we suggest is due to a stronger East Asian winter monsoon. During the last 80 kyr, eight significant increases in primary productivity (PP) in the Sulu Sea are similar to East Asian winter monsoon changes recorded in Chinese loess. The PP maxima are not linked with Heinrich events (HE) in the North Atlantic, although four PP peaks are synchronous with HE. The PP oscillations have frequencies near those of the Dansgaard‐Oeschger cycles in Northern Hemisphere ice records and indicate a teleconnection of the East Asian winter monsoon with Greenland climate. In this Sulu Sea record the East Asian winter monsoon oscillates with periodicities of ∼6, 4.2–3.4, 2.3, and 1.5 kyr. In particular, the 1.5 kyr cycle exhibits a strong and pervasive signal from stage 6 to the Holocene without any ice volume modulation. This stationarity suggests that the 1.5 kyr cycle is not driven by some high‐latitude forcing.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380016869940995328","@type":"Researcher","foaf:name":[{"@value":"Thibault de Garidel‐Thoron"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568614709633","@type":"Researcher","foaf:name":[{"@value":"Luc Beaufort"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568614709632","@type":"Researcher","foaf:name":[{"@value":"Braddock K. Linsley"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855568614709504","@type":"Researcher","foaf:name":[{"@value":"Stefanie Dannenmann"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08838305"},{"@type":"EISSN","@value":"19449186"}],"prism:publicationName":[{"@value":"Paleoceanography"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2001-10","prism:volume":"16","prism:number":"5","prism:startingPage":"491","prism:endingPage":"502"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000PA000557"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000PA000557"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004229805175936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the North Pacific Subtropical Gyre during the past 190 kyr through the interaction of the Kuroshio Current with the surface and intermediate waters"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233286779520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vertical thermal structure history in the western subtropical North Pacific since the Last Glacial Maximum"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707445722112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hydrographic variability in the northern South China Sea over the past 45,000 years: New insights based on temperature reconstructions by U k’ 37 and TEX H 86 proxies from a marine sediment core (MD972146)"}]},{"@id":"https://cir.nii.ac.jp/crid/1523106605360340864","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"N2 Fixation Variability in the Oligotrophic Sulu Sea, Western Equatorial Pacific Region over the past 83 kyr"},{"@language":"ja-Kana","@value":"N2 Fixation Variability in the Oligotrophic Sulu Sea Western Equatorial Pacific Region over the past 83 kyr"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417125251200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stalagmite evidence for East Asian winter monsoon variability and 18O-depleted surface water in the Japan Sea during the last glacial period"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000pa000557"},{"@type":"CIA","@value":"30013358188"},{"@type":"CROSSREF","@value":"10.1002/2015pa002914_references_DOI_LtbT0plyZkPOd1MnGrYnvCYvF5Q"},{"@type":"CROSSREF","@value":"10.1029/2010gl045827_references_DOI_LtbT0plyZkPOd1MnGrYnvCYvF5Q"},{"@type":"CROSSREF","@value":"10.1016/j.quaint.2017.09.029_references_DOI_LtbT0plyZkPOd1MnGrYnvCYvF5Q"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00409-8_references_DOI_LtbT0plyZkPOd1MnGrYnvCYvF5Q"}]}