{"@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/1363670318232833280.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1002/jqs.1355"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1355"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1355"}}],"dc:title":[{"@value":"Orbital‐ and millennial‐scale fluctuations in late Quaternary marine pollen records from the Japan Sea"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title>\n                  <jats:p>\n                    Quaternary surface water conditions within the Japan Sea change with eustatic sea‐level changes and fluctuations in the East Asian Summer Monsoon (EASM), influencing regional climate and vegetation through the delivery of heat and moisture. Our marine pollen data suggest overall cooling from the Last Interglacial (ca. 125 ka) to the Last Glacial Maximum (LGM), a cold climate during Marine Isotope Stage (MIS) 2, gradual warming from 12 ka and rapid warming after 10 ka. These stages are concordant with published palaeoceanographic changes in the Japan Sea. During mid MIS 5 to MIS 3, marine sediments in the Japan Sea are characterised by fine alternations of dark‐ and light‐coloured layers that formed under the influence of fluctuations in the EASM, possibly correlated with Dansgaard–Oeschger cycles. During the deposition of dark layers, high levels of precipitation are inferred from the abundance of\n                    <jats:italic>Cryptomeria</jats:italic>\n                    . In contrast, a cool and dry climate is interpreted for the light layers, based on an abundance of subarctic conifer pollen. The palaeoclimate of the Japan Sea region appears to have been influenced by orbital‐scale changes in global climate and millennial‐scale fluctuations in the EASM. Copyright © 2009 John Wiley & Sons, Ltd.\n                  </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670318232833281","@type":"Researcher","foaf:name":[{"@value":"Ken Ikehara"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670318232833280","@type":"Researcher","foaf:name":[{"@value":"Hideaki Oshima"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02678179"},{"@type":"EISSN","@value":"10991417"}],"prism:publicationName":[{"@value":"Journal of Quaternary Science"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2009-11-26","prism:volume":"24","prism:number":"8","prism:startingPage":"866","prism:endingPage":"879"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1355"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1355"}],"createdAt":"2009-11-27","modifiedAt":"2025-11-25","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360025430667038720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Silicoflagellate assemblages in the North Pacific surface sediments: an application of the modern analog method to reconstruct the glacial sea surface temperature in the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182126920192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fluctuations in the East Asian monsoon recorded by pollen assemblages in sediments from the Japan Sea off the southwestern coast of Hokkaido, Japan, from 4.3 Ma to the present"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118767685376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Orbital-scale vegetation-ocean-atmosphere linkages in western Japan during the last 550 ka based on a pollen record from the IODP site U1427 in the Japan Sea"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307417113179136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanographic changes in the Northern East China Sea during the last 400 kyr as inferred from radiolarian assemblages (IODP Site U1429)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1002/jqs.1355"},{"@type":"CROSSREF","@value":"10.1186/s40645-024-00661-8_references_DOI_ArL8HXoIoCQlehm6Tq9UffsOCGb"},{"@type":"CROSSREF","@value":"10.1186/s40645-019-0256-3_references_DOI_ArL8HXoIoCQlehm6Tq9UffsOCGb"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2021.107103_references_DOI_ArL8HXoIoCQlehm6Tq9UffsOCGb"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2018.02.001_references_DOI_ArL8HXoIoCQlehm6Tq9UffsOCGb"}]}