{"@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/1361418521294634752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1130/g25667a.1"}},{"identifier":{"@type":"URI","@value":"http://pubs.geoscienceworld.org/geology/article-pdf/37/7/591/3536300/i0091-7613-37-7-591.pdf"}}],"dc:title":[{"@value":"The 1500-year climate oscillation in the midlatitude North Pacific during the Holocene"}],"description":[{"notation":[{"@value":"Suborbital climate variability during the last glacial period is suggested to have involved a 1500-year pacing cycle, but the expression and spatial distribution of the ~1500-year oscillation during interglacials remains unclear. We generated a multidecade resolution record of alkenone sea surface temperature (SST) in the northwestern Pacific off central Japan during the Holocene. The SST record showed centennial and millennial variability with an amplitude of ~1 °C throughout the entire Holocene. Spectral analysis for SST variation revealed a statistically significant peak with 1470-year periodicity. The SST variation partly correlated with the variations of ice-rafted hematite-stained grain content in North Atlantic sediments. These findings indicate that the mean latitude of the Kuroshio Extension has varied on a 1500-year cycle, and suggest that a climatic link exists between the North Pacific gyre system and the high-latitude North Atlantic thermohaline circulation. The regular pacing at 1500-year intervals seen throughout both the Holocene and the last glacial period suggests that the oscillation was a response to external forcing."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418521294634753","@type":"Researcher","foaf:name":[{"@value":"Dai Isono"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634756","@type":"Researcher","foaf:name":[{"@value":"Masanobu Yamamoto"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634757","@type":"Researcher","foaf:name":[{"@value":"Tomohisa Irino"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634752","@type":"Researcher","foaf:name":[{"@value":"Tadamichi Oba"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634624","@type":"Researcher","foaf:name":[{"@value":"Masafumi Murayama"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634755","@type":"Researcher","foaf:name":[{"@value":"Toshio Nakamura"}]},{"@id":"https://cir.nii.ac.jp/crid/1381418521294634754","@type":"Researcher","foaf:name":[{"@value":"Hodaka Kawahata"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"19432682"},{"@type":"PISSN","@value":"00917613"}],"prism:publicationName":[{"@value":"Geology"}],"dc:publisher":[{"@value":"Geological Society of America"}],"prism:publicationDate":"2009-07","prism:volume":"37","prism:number":"7","prism:startingPage":"591","prism:endingPage":"594"},"reviewed":"false","url":[{"@id":"http://pubs.geoscienceworld.org/geology/article-pdf/37/7/591/3536300/i0091-7613-37-7-591.pdf"}],"createdAt":"2009-06-27","modifiedAt":"2024-03-14","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050002213761277952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnections with ice melt in the North Atlantic"},{"@value":"Millennial-scale hydrographic changes in the northwestern Pacific during marine isotope stage 19: teleconnection with ice melt in the North Atlantic"}]},{"@id":"https://cir.nii.ac.jp/crid/1050587981430434048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Climate reconstruction based on GDGT-based proxies in a paleosol sequence in Japan: Postdepositional effect on the estimation of air temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002216146325120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Vegetation and endemic tree response to orbital-scale climate changes in the Japanese archipelago during the last glacial–interglacial cycle based on pollen records from Lake Biwa, western 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