{"@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/1361418520648148992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.palaeo.2012.09.035"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018212005482?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0031018212005482?httpAccept=text/plain"}}],"dc:title":[{"@value":"Eocene monsoon prevalence over China: A paleobotanical perspective"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418520648148992","@type":"Researcher","foaf:name":[{"@value":"Cheng Quan"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520648148993","@type":"Researcher","foaf:name":[{"@value":"Yu-Sheng (Christopher) Liu"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418520648148994","@type":"Researcher","foaf:name":[{"@value":"Torsten Utescher"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2012-12","prism:volume":"365-366","prism:startingPage":"302","prism:endingPage":"311"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0031018212005482?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0031018212005482?httpAccept=text/plain"}],"createdAt":"2012-10-04","modifiedAt":"2018-11-20","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282189594880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"African Hydroclimate During the Early Eocene From the DeepMIP Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282206565248","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sedimentological and geochemical properties of authigenic carbonates in Kyushu, Japan: Implications for the transition from semi-arid to humid climate during the Eocene"}]},{"@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.palaeo.2012.09.035"},{"@type":"CROSSREF","@value":"10.1029/2022pa004419_references_DOI_YM9JeOfoaav4Tzc1fEx8kuDWeom"},{"@type":"CROSSREF","@value":"10.1016/j.sedgeo.2022.106280_references_DOI_YM9JeOfoaav4Tzc1fEx8kuDWeom"},{"@type":"CROSSREF","@value":"10.1186/s40645-016-0080-y_references_DOI_YM9JeOfoaav4Tzc1fEx8kuDWeom"},{"@type":"CROSSREF","@value":"10.1029/2022jd036510_references_DOI_YM9JeOfoaav4Tzc1fEx8kuDWeom"}]}