{"@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/1361981469976138752.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1751-908x.2013.00209.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1751-908X.2013.00209.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1751-908X.2013.00209.x"}}],"dc:title":[{"@value":"Nickel Isotope Variations in Terrestrial Silicate Rocks and Geological Reference Materials Measured by <scp>MC</scp>‐<scp>ICP</scp>‐<scp>MS</scp>"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Although initial studies have demonstrated the applicability of <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotopes for cosmochemistry and as a potential biosignature, the <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope composition of terrestrial igneous and sedimentary rocks, and ore deposits remains poorly known. Our contribution is fourfold: (a) to detail an analytical procedure for <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope determination, (b) to determine the <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope composition of various geological reference materials, (c) to assess the isotope composition of the <jats:styled-content style=\"fixed-case\">B</jats:styled-content>ulk <jats:styled-content style=\"fixed-case\">S</jats:styled-content>ilicate <jats:styled-content style=\"fixed-case\">E</jats:styled-content>arth relative to the <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope reference material <jats:styled-content style=\"fixed-case\">NIST SRM</jats:styled-content> 986 and (d) to report the range of mass‐dependent <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope fractionations in magmatic rocks and ore deposits. After purification through a two‐stage chromatography procedure, <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i isotope ratios were measured by <jats:styled-content style=\"fixed-case\">MC</jats:styled-content>‐<jats:styled-content style=\"fixed-case\">ICP</jats:styled-content>‐<jats:styled-content style=\"fixed-case\">MS</jats:styled-content> and were corrected for instrumental mass bias using a double‐spike correction method. Measurement precision (two standard error of the mean) was between 0.02 and 0.04‰, and intermediate measurement precision for <jats:styled-content style=\"fixed-case\">NIST SRM</jats:styled-content> 986 was 0.05‰ (2<jats:italic>s</jats:italic>). Igneous‐ and mantle‐derived rocks displayed a restricted range of δ<jats:sup>60/58</jats:sup><jats:styled-content style=\"fixed-case\">N</jats:styled-content>i values between −0.13 and +0.16‰, suggesting an average <jats:styled-content style=\"fixed-case\">BSE</jats:styled-content> composition of +0.05‰. Manganese nodules (Nod A1; P1), shale (<jats:styled-content style=\"fixed-case\">SDO</jats:styled-content>‐1), coal (<jats:styled-content style=\"fixed-case\">CLB</jats:styled-content>‐1) and a metal‐contaminated soil (<jats:styled-content style=\"fixed-case\">NIST SRM</jats:styled-content> 2711) showed positive values ranging between +0.14 and +1.06‰, whereas komatiite‐hosted <jats:styled-content style=\"fixed-case\">N</jats:styled-content>i‐rich sulfides varied from −0.10 to −1.03‰.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469976138754","@type":"Researcher","foaf:name":[{"@value":"Bleuenn Gueguen"}],"jpcoar:affiliationName":[{"@value":"Institut Universitaire Européen de la Mer UMR 6538 Université de Bretagne Occidentale BP 80 F‐29280 Plouzané France"},{"@value":"IFREMER Centre de Brest Unité Géosciences Marines 29280 Plouzané France"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469976138753","@type":"Researcher","foaf:name":[{"@value":"Olivier Rouxel"}],"jpcoar:affiliationName":[{"@value":"Institut Universitaire Européen de la Mer UMR 6538 Université de Bretagne Occidentale BP 80 F‐29280 Plouzané France"},{"@value":"IFREMER Centre de Brest Unité Géosciences Marines 29280 Plouzané France"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469976138752","@type":"Researcher","foaf:name":[{"@value":"Emmanuel Ponzevera"}],"jpcoar:affiliationName":[{"@value":"IFREMER Centre de Brest Unité Géosciences Marines 29280 Plouzané France"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469976138755","@type":"Researcher","foaf:name":[{"@value":"Andrey Bekker"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences University of Manitoba Winnipeg R3T 2N2 Canada"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981469976138756","@type":"Researcher","foaf:name":[{"@value":"Yves Fouquet"}],"jpcoar:affiliationName":[{"@value":"IFREMER Centre de Brest Unité Géosciences Marines 29280 Plouzané France"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"16394488"},{"@type":"EISSN","@value":"1751908X"}],"prism:publicationName":[{"@value":"Geostandards and Geoanalytical Research"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2013-04-19","prism:volume":"37","prism:number":"3","prism:startingPage":"297","prism:endingPage":"317"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1751-908X.2013.00209.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1751-908X.2013.00209.x"}],"createdAt":"2013-01-24","modifiedAt":"2023-10-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360013168843296896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Novel nickel isolation procedure for a wide range of sample matrices without using dimethylglyoxime for isotope measurements using MC-ICP-MS"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568466832764288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The non-chondritic Ni isotope composition of Earth’s mantle"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412891989456128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sources of particulate Ni and Cu in the water column of the northern South China Sea: Evidence from elemental and isotope ratios in aerosols and sinking particles"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1751-908x.2013.00209.x"},{"@type":"CROSSREF","@value":"10.1016/j.aca.2021.338934_references_DOI_KCasYqLO7IDDF4TQCzw0aZaCCtV"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2019.10.017_references_DOI_KCasYqLO7IDDF4TQCzw0aZaCCtV"},{"@type":"CROSSREF","@value":"10.1016/j.marchem.2020.103751_references_DOI_KCasYqLO7IDDF4TQCzw0aZaCCtV"}]}