{"@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/1363670319024003584.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1184480"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1184480"}}],"dc:title":[{"@value":"Subpolar Link to the Emergence of the Modern Equatorial Pacific Cold Tongue"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Birth of the Cool</jats:title>\n          <jats:p>\n            Over the past 4 million years or so, tropical sea surface temperatures have experienced a cooling trend (see the Perspective by\n            <jats:bold>\n              <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"5985\" page=\"1488\" related-article-type=\"in-this-issue\" vol=\"328\" xlink:href=\"10.1126/science.1189748\">Philander</jats:related-article>\n            </jats:bold>\n            ).\n            <jats:bold>\n              Herbert\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"1530\" related-article-type=\"in-this-issue\" vol=\"328\" xlink:href=\"10.1126/science.1185435\">1530</jats:related-article>\n            ) analyzed sea surface temperature records of the past 3.5 million years from low-latitude sites spanning the world's major ocean basins in order to determine the timing and magnitude of the cooling that has accompanied the intensification of Northern Hemisphere ice ages since the Pliocene.\n            <jats:bold>\n              Martínez-Garcia\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"1550\" related-article-type=\"in-this-issue\" vol=\"328\" xlink:href=\"10.1126/science.1184480\">1550</jats:related-article>\n            ) found that the enigmatic eastern equatorial Pacific cold tongue, a feature one might not expect to find in such a warm region receiving so much sunlight, first appeared between 1.8 and 1.2 million years ago. Its appearance was probably in response to a general shrinking of the tropical warm water pool caused by general climate cooling driven by changes in Earth's orbit.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670319024003586","@type":"Researcher","foaf:name":[{"@value":"Alfredo Martínez-Garcia"}],"jpcoar:affiliationName":[{"@value":"Geological Institute, ETH Zürich, 8092 Zürich, Switzerland."},{"@value":"DFG-Leibniz Center for Surface Process and Climate Studies, Institute for Geosciences, Potsdam University, D-14476 Potsdam, Germany."},{"@value":"Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona, Bellaterra, 08193 Catalonia, Spain."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319024003587","@type":"Researcher","foaf:name":[{"@value":"Antoni Rosell-Melé"}],"jpcoar:affiliationName":[{"@value":"Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona, Bellaterra, 08193 Catalonia, Spain."},{"@value":"Institució Catalana de Recerca i Estudis Avançats, Barcelona, 08010 Catalonia, Spain."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319024003585","@type":"Researcher","foaf:name":[{"@value":"Erin L. McClymont"}],"jpcoar:affiliationName":[{"@value":"School of Geography Politics and Sociology, Newcastle University, Newcastle upon Tyne NE1 7RU, UK."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319024003588","@type":"Researcher","foaf:name":[{"@value":"Rainer Gersonde"}],"jpcoar:affiliationName":[{"@value":"Alfred Wegener Institute for Polar and Marine Research, D-27568 Bremerhaven, Germany."}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319024003584","@type":"Researcher","foaf:name":[{"@value":"Gerald H. Haug"}],"jpcoar:affiliationName":[{"@value":"Geological Institute, ETH Zürich, 8092 Zürich, Switzerland."},{"@value":"DFG-Leibniz Center for Surface Process and Climate Studies, Institute for Geosciences, Potsdam University, D-14476 Potsdam, Germany."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2010-06-18","prism:volume":"328","prism:number":"5985","prism:startingPage":"1550","prism:endingPage":"1553"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1184480"}],"createdAt":"2010-06-17","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232564381824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biogenic opal production changes during the Mid-Pleistocene Transition in the Bering Sea (IODP Expedition 323 Site U1343)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142452844672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Latest Pliocene Northern Hemisphere glaciation amplified by intensified Atlantic meridional overturning circulation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708408856704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pliocene cooling enhanced by flow of low-salinity Bering Sea water to the Arctic Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617500280192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Lessons from a high-CO\n                    <sub>2</sub>\n                    world: an ocean view from  ∼ 3 million years ago"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092626898304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Life on the ice-edge: Paleoenvironmental significance of the radiolarian species Amphimelissa setosa in the northern hemisphere"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658396468608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Asynchrony between Antarctic temperature and CO2 associated with obliquity over the past 720,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815671408256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variability of the Indonesian Throughflow and Australian monsoon across the mid Pleistocene transition (IODP 363, Site U1483)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792011723008","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanography of the northwestern Pacific across the Early–Middle Pleistocene boundary (Marine Isotope Stages 20–18)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1184480"},{"@type":"CROSSREF","@value":"10.1016/j.yqres.2013.10.001_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1038/s43247-020-00023-4_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1038/ncomms8587_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.5194/cp-16-1599-2020_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1016/j.quascirev.2020.106565_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1038/s41467-018-03328-3_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1186/s40645-020-00395-3_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2023.118437_references_DOI_ZgSnJDGPe4khvnhOjIn4ECnCBVK"}]}