{"@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/1380011145954894722.json","@type":"Researcher","foaf:Person":[{"foaf:name":[{"@value":"George E. A. Swann"}],"foaf:familyName":[{"@value":"Swann"}],"foaf:givenName":[{"@value":"George E. A."}]}],"career":[{"institution":{"notation":[{"@value":"Environmental Change Research Centre, Department of Geography University College London  London UK"}]}}],"product":[{"@id":"https://cir.nii.ac.jp/crid/1360011145954894592","@type":"Article","productIdentifier":[{"@type":"DOI","@value":"10.1029/2005pa001147"},{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2005PA001147"},{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2005PA001147"}],"notation":[{"@value":"Diatom δ<sup>18</sup>O evidence for the development of the modern halocline system in the subarctic northwest Pacific at the onset of major Northern Hemisphere glaciation"}],"relation":[{"type":"creator"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2005pa001147_MdGglQmn6zJ3Ao9PPBOjvuR3Kdv"}]}