{"@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/1361137044805336192.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000jc900005"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JC900005"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JC900005"}}],"dc:title":[{"@value":"An oxygen isotope data set for marine waters"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The proportion of <jats:sup>18</jats:sup>O in a sample of seawater is an excellent tracer of its past history as, away from the surface, it is conservative and also nondynamical. The range of values in source waters is also large, and the accuracy achievable in modern measurement high. Here we bring together for the first time a global data set of over 6000 individual measurements from the past 40 years. The properties of this data set are described. Noteworthy features include the hitherto unnoticed, but distinctive, contribution of North Pacific Upper Water to the δ<jats:sup>18</jats:sup>O:salinity relationship, and different origins of the deeper waters of the Atlantic and Pacific Oceans. We also make a plea here to the international community to contribute unpublished data to the archive for the use of all.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137044805336193","@type":"Researcher","foaf:name":[{"@value":"Grant R. Bigg"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044805336192","@type":"Researcher","foaf:name":[{"@value":"Eelco J. Rohling"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Oceans"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2000-04-15","prism:volume":"105","prism:number":"C4","prism:startingPage":"8527","prism:endingPage":"8535"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000JC900005"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000JC900005"}],"createdAt":"2002-09-17","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360009142883986688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Discrimination of eastward trans-Pacific migration of the Pacific bluefin tuna Thunnus orientalis through otolith δ13C and δ18O analyses"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662759680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal variation in the oxygen isotopic composition of different‐sized planktonic foraminifer <i>Neogloboquadrina pachyderma</i> (sinistral) in the northwestern North Pacific and implications for reconstruction of the paleoenvironment"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659068039680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"<i>Crenostrea</i> sp. cf. <i>C</i>. <i>cannoni</i> (Marwick, 1928) (Bivalvia: Ostreoidea) and associated fauna from east of Heard Island, Kerguelen Plateau: age and palaeoenvironmental value"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204439515136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review and Perspective on the Water Cycle Processes using Stable Isotope of Water"},{"@language":"ja","@value":"水の酸素・水素安定同位体を用いた地球水循環研究と今後の展望"},{"@language":"ja-Kana","@value":"ミズ ノ サンソ スイソ アンテイ ドウイタイ オ モチイタ チキュウ ミズ ジュンカン ケンキュウ ト コンゴ ノ テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205194250112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Magnitude of Middle Miocene warming in North Pacific high latitudes: stable isotope evidence from <i>Kaneharaia </i>(Bivalvia, Dosiniinae)"},{"@language":"ja","@value":"北太平洋高緯度における中期中新世最温暖期の温暖化の度合： 二枚貝<i>Kaneharaia </i>の成長断面の安定同位体分析に基づいて"},{"@value":"Magnitude of Middle Miocene warming in North Pacific high latitudes: stable isotope evidence from Kaneharaia (Bivalvia, Dosiniinae)"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317043070592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characterization of water masses around the southern Ryukyu Islands based on isotopic compositions"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000jc900005"},{"@type":"CROSSREF","@value":"10.1007/s00227-020-03723-9_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"},{"@type":"CROSSREF","@value":"10.1029/2011pa002153_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.59.339_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"},{"@type":"CROSSREF","@value":"10.3178/jjshwr.21.158_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"},{"@type":"CROSSREF","@value":"10.1080/03115518.2015.965545_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"},{"@type":"CROSSREF","@value":"10.1186/s40645-022-00503-5_references_DOI_RcWH3uLK15lZUi1D9psiWzJdc95"}]}