{"@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/1363670320177573248.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1046/j.1365-3121.2000.00295.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.2000.00295.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.2000.00295.x"}},{"identifier":{"@type":"NAID","@value":"30014972746"}}],"dc:title":[{"@value":"The marine osmium isotope record"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Over the past decade the marine osmium isotope record has been developed into a new tracer in palaeoceanographic research. Several analytical developments, particularly in the past few years, have significantly increased our ability to study the behaviour of osmium in the surficial environment. The <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os and osmium concentration of seawater, river water, rain, and hydrothermal vent fluids have been measured directly. Recently, the behaviour of osmium in estuaries–critical for estimating the marine residence time of osmium–has been studied. Our knowledge of the surficial osmium cycle has thus significantly improved. In addition, reconstructions of past variations in the marine <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os recently have been extended back into the Mesozoic. This review attempts to summarize our current understanding of the marine osmium system–present and past.</jats:p><jats:p>The <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os of seawater during the Cenozoic to first order mimics the marine <jats:sup>87</jats:sup>Sr/<jats:sup>86</jats:sup>Sr record. It is therefore tempting to interpret both records as reflecting increased input of radiogenic osmium and strontium resulting from enhanced continental weathering regulated by climatic/tectonic processes. However, the marine osmium isotope system differs fundamentally from the marine strontium isotope system. This review emphasizes three important differences. First, large impacts are capable of resetting the <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os to unradiogenic values without significantly affecting the marine strontium system. Second, organic‐rich sediments are characterized by high <jats:sup>187</jats:sup>Re/<jats:sup>188</jats:sup>Os; resulting <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os ingrowth‐trajectories are similar to the average slope of the Cenozoic <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os seawater record. Trends towards more radiogenic <jats:sup>187</jats:sup>Os/<jats:sup>188</jats:sup>Os seawater therefore can be caused by weathering of organic‐rich sediments at a constant rate. Third, the marine residence time of osmium is sufficiently short to capture short‐periodic (glacial‐interglacial) fluctuations that are inaccessible to the buffered marine strontium isotope system. This offers the opportunity to discriminate between high‐frequency (climatic) and low‐frequency (tectonic) forcing.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579819416880512","@type":"Researcher","foaf:name":[{"@value":"B. Peucker‐Ehrenbrink"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320177573249","@type":"Researcher","foaf:name":[{"@value":"G. Ravizza"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"09544879"},{"@type":"EISSN","@value":"13653121"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/09544879"}],"prism:publicationName":[{"@value":"Terra Nova"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2000-10-29","prism:volume":"12","prism:number":"5","prism:startingPage":"205","prism:endingPage":"219"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1365-3121.2000.00295.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1365-3121.2000.00295.x"}],"createdAt":"2003-03-12","modifiedAt":"2023-10-29","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050575520345165056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rapid coupling between solid earth and ice 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and osmium in two soil profiles"},{"@language":"ja-Kana","@value":"effect of weathering regime on uranium decay series and osmium in two soil profiles"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204552169344","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Osmium concentrations and <sup>187</sup>Os/<sup>188</sup>Os ratios of three sediment reference materials"},{"@value":"Osmium concentrations and 187Os/188Os ratios of three sediment reference materials"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288126901120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geochemical characterization of large impact event recorded in the bedded chert sequence from Japan"},{"@language":"ja","@value":"層状チャートに記録された巨大隕石衝突の地球化学的特徴"},{"@language":"ja-Kana","@value":"ソウジョウ チャート ニ キロク サレタ キョダイインセキ ショウトツ ノ チキュウ カガクテキ トクチョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679214762112","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"顕生代のグローバル気候変動と風化作用"},{"@language":"en","@value":"Global Climate Change and Weathering during the Phanerozoic"},{"@language":"ja-Kana","@value":"ケンセイダイ ノ グローバル キコウ ヘンドウ ト フウカ サヨウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679529697920","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re–Os isotope geochemistry in the surface layers of ferromanganese crusts from the Takuyo Daigo Seamount, northwestern Pacific Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680294295168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re and Os blanks of drill sampling and acid digestion toward the Os isotope stratigraphy of Fe-Mn crust"},{"@value":"ドリルを用いた微小サンプリングと酸分解に伴うRe-Osブランク : Fe-MnクラストのOs同位体比層序に向けて"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681216558080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Accretion of extraterrestrial matter recorded in the Triassic and Jurassic bedded chert sequence, southwest Japan"},{"@language":"ja","@value":"日本の三畳紀・ジュラ紀層状チャートに記録された地球外物質の付加"},{"@language":"ja-Kana","@value":"ニホン ノ サンジョウキ ・ ジュラキ ソウジョウ チャート ニ キロク サレタ チキュウ ガイブツシツ ノ フカ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763033362432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mid-Cretaceous climatic warmings and environmental changes recorded in the lower and middle part of the Yezo Group, Hokkaido, northern Japan"},{"@language":"ja","@value":"蝦夷層群下部～中部に記録された白亜紀中頃の温暖化と古環境変動"},{"@value":"巡検案内書 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