{"@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/1360580237014158208.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.epsl.2021.116881"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X21001400?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0012821X21001400?httpAccept=text/plain"}}],"dc:title":[{"@value":"Black Sea paleosalinity evolution since the last deglaciation reconstructed from alkenone-inferred Isochrysidales diversity"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380580237014158212","@type":"Researcher","foaf:name":[{"@value":"Yongsong Huang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580237014158208","@type":"Researcher","foaf:name":[{"@value":"Yinsui Zheng"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580237014158209","@type":"Researcher","foaf:name":[{"@value":"Patrick Heng"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580237014158210","@type":"Researcher","foaf:name":[{"@value":"Liviu Giosan"}]},{"@id":"https://cir.nii.ac.jp/crid/1380580237014158211","@type":"Researcher","foaf:name":[{"@value":"Marco J.L. Coolen"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"0012821X"}],"prism:publicationName":[{"@value":"Earth and Planetary Science Letters"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2021-06","prism:volume":"564","prism:startingPage":"116881"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license","http://www.elsevier.com/open-access/userlicense/1.0/","https://doi.org/10.15223/policy-017","https://doi.org/10.15223/policy-037","https://doi.org/10.15223/policy-012","https://doi.org/10.15223/policy-029","https://doi.org/10.15223/policy-004"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0012821X21001400?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0012821X21001400?httpAccept=text/plain"}],"createdAt":"2021-03-31","modifiedAt":"2025-09-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282190627328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Freshwater influx to the Eastern Mediterranean Sea from the melting of the Fennoscandian ice sheet during the last deglaciation"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266996491136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long-chain alkenones in the Shimosa Group reveal palaeotemperatures of the Pleistocene interglacial Palaeo-Tokyo Bays"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.epsl.2021.116881"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-12055-1_references_DOI_CZGtSp1fMfYH9cKLkKQmSWZhhVY"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00499-y_references_DOI_CZGtSp1fMfYH9cKLkKQmSWZhhVY"}]}