{"@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/1361137044455289984.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/28367"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/28367.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/28367"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/doifinder/10.1038/28367"}}],"dc:title":[{"@value":"Influence of mesoscale eddies on new production in the Sargasso Sea"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380567181335190275","@type":"Researcher","foaf:name":[{"@value":"D. J. McGillicuddy"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289985","@type":"Researcher","foaf:name":[{"@value":"A. R. Robinson"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289990","@type":"Researcher","foaf:name":[{"@value":"D. A. Siegel"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289992","@type":"Researcher","foaf:name":[{"@value":"H. W. Jannasch"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289984","@type":"Researcher","foaf:name":[{"@value":"R. Johnson"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289986","@type":"Researcher","foaf:name":[{"@value":"T. D. Dickey"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289991","@type":"Researcher","foaf:name":[{"@value":"J. McNeil"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289988","@type":"Researcher","foaf:name":[{"@value":"A. F. Michaels"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044455289987","@type":"Researcher","foaf:name":[{"@value":"A. H. Knap"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"1998-07","prism:volume":"394","prism:number":"6690","prism:startingPage":"263","prism:endingPage":"266"},"reviewed":"false","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/28367.pdf"},{"@id":"http://www.nature.com/articles/28367"},{"@id":"http://www.nature.com/doifinder/10.1038/28367"}],"createdAt":"2002-07-26","modifiedAt":"2023-05-17","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338209104384","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Impact of cyclonic eddies and typhoons on biogeochemistry in the oligotrophic ocean based on biogeochemical/physical/meteorological time-series at station KEO"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002215398187648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Primary productivity at the time-series stations in the northwestern Pacific Ocean: is the subtropical station unproductive?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231381697152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biogeochemical responses associated with the passage of a cyclonic eddy based on shipboard observations in the western North Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233290973440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Linkage Between Dinitrogen Fixation and Primary Production in the Oligotrophic South Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005514422010880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Impact of Ocean Physics on Marine Ecosystems in the Kuroshio and Kuroshio Extension Regions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691101466496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Foraging spots of streaked shearwaters in relation to ocean surface currents as identified using their drift movements"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707077838592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrasted structuring effects of mesoscale features on the seabird community in the Mozambique Channel"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707329111936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial high-resolution estimation of net oxygen production during spring bloom in the western North Pacific using dissolved oxygen, nitrogen and argon"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708262152448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"New estimation of N<sub>2</sub> fixation in the western and central Pacific Ocean and its marginal seas"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179762132864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The formation processes of phytoplankton growth and decline in mesoscale eddies in the western <scp>N</scp>orth <scp>P</scp>acific <scp>O</scp>cean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181335190016","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Mesoscale eddy effects on temporal variability of surface chlorophyll a in the Kuroshio Extension"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567181335533568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Comparison of carbon cycle between the western Pacific subarctic and subtropical time-series stations: highlights of the K2S1 project"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848655052388736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Observations of vertical turbulent nitrate flux across the Kuroshio"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658222511744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"One‐Dimensional Turbulence‐Ecosystem Model Reveals the Triggers of the Spring Bloom in Mesoscale Eddies"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412889305565824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Structure and Impact of the Kuroshio Nutrient Stream"}]},{"@id":"https://cir.nii.ac.jp/crid/1390858518831357952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Evaluation of new production in the tropical and subtropical oligotrophic ocean"},{"@language":"ja","@value":"熱帯・亜熱帯貧栄養海域における新生産の評価"},{"@language":"ja-Kana","@value":"ネッタイ アネッタイヒンエイヨウ カイイキ ニ オケル シン セイサン ノ ヒョウカ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/28367"},{"@type":"CROSSREF","@value":"10.1007/s10872-016-0354-4_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1007/s10872-014-0244-6_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1029/2017gb005869_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1002/9781119428428.ch11_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.18.3_213_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1029/2009gb003620_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1002/2017jc012722_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1007/s10872-015-0286-4_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1007/s10872-017-0423-3_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1002/grl.50613_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1029/2018jc014089_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0196-3_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1016/j.pocean.2013.12.002_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1002/9781119428428.ch5_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1016/j.marchem.2013.01.001_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"},{"@type":"CROSSREF","@value":"10.1016/j.dsr2.2013.10.027_references_DOI_EKjcPvIbP4Gr021cfw1lzdytjv0"}]}