{"@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/1363388844749950208.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.jseaes.2011.05.013"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1367912011002148?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1367912011002148?httpAccept=text/plain"}}],"dc:title":[{"@value":"Early Eocene Asian climate dominated by desert and steppe with limited monsoons"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388844749950208","@type":"Researcher","foaf:name":[{"@value":"Zhongshi Zhang"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844749950210","@type":"Researcher","foaf:name":[{"@value":"Frode Flatøy"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844749950211","@type":"Researcher","foaf:name":[{"@value":"Huijun Wang"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844749950213","@type":"Researcher","foaf:name":[{"@value":"Ingo Bethke"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844749950209","@type":"Researcher","foaf:name":[{"@value":"Mats Bentsen"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388844749950212","@type":"Researcher","foaf:name":[{"@value":"Zhengtang Guo"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13679120"}],"prism:publicationName":[{"@value":"Journal of Asian Earth Sciences"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-01","prism:volume":"44","prism:startingPage":"24","prism:endingPage":"35"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/","https://www.elsevier.com/legal/tdmrep-license"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S1367912011002148?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S1367912011002148?httpAccept=text/plain"}],"createdAt":"2011-06-25","modifiedAt":"2025-10-24","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360580230584002432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of Mountains in Southern China on the Eocene Climates of East Asia"}]},{"@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.jseaes.2011.05.013"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0080-y_references_DOI_5RmTgoAIC3wA0OowYBTugqKSDAv"},{"@type":"CROSSREF","@value":"10.1029/2022jd036510_references_DOI_5RmTgoAIC3wA0OowYBTugqKSDAv"}]}