{"@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/1361981469169971968.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.palaeo.2010.11.028"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018210007042?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018210007042?httpAccept=text/plain"}}],"dc:title":[{"@value":"Step-wise change of Asian interior climate preceding the Eocene–Oligocene Transition (EOT)"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469169971969","@type":"Researcher","foaf:name":[{"@value":"Hemmo A. Abels"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469169971970","@type":"Researcher","foaf:name":[{"@value":"Guillaume Dupont-Nivet"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469169971972","@type":"Researcher","foaf:name":[{"@value":"Guoqiao Xiao"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469169971971","@type":"Researcher","foaf:name":[{"@value":"Roderic Bosboom"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469169971968","@type":"Researcher","foaf:name":[{"@value":"Wout Krijgsman"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2011-01","prism:volume":"299","prism:number":"3-4","prism:startingPage":"399","prism:endingPage":"412"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031018210007042?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031018210007042?httpAccept=text/plain"}],"createdAt":"2010-12-10","modifiedAt":"2018-12-06","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360848658466709504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Response of the Pacific inter-tropical convergence zone to global cooling and initiation of Antarctic glaciation across the Eocene Oligocene Transition"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151841908060032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution and variability of the Asian monsoon and its potential linkage with uplift of the Himalaya and Tibetan Plateau"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2010.11.028"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0080-y_references_DOI_R6VMcQJAU39tHhsAAKHbysLrPBt"},{"@type":"CROSSREF","@value":"10.1038/srep30647_references_DOI_R6VMcQJAU39tHhsAAKHbysLrPBt"}]}