{"@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/1360011144091159552.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1119365"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1119365"}}],"dc:title":[{"@value":"Rapid Uplift of the Altiplano Revealed Through\n            <sup>13</sup>\n            C-\n            <sup>18</sup>\n            O Bonds in Paleosol Carbonates"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            The elevation of Earth's surface is among the most difficult environmental variables to reconstruct from the geological record. Here we describe an approach to paleoaltimetry based on independent and simultaneous determinations of soil temperatures and the oxygen isotope compositions of soil waters, constrained by measurements of abundances of\n            <jats:sup>13</jats:sup>\n            C-\n            <jats:sup>18</jats:sup>\n            O bonds in soil carbonates. We use this approach to show that the Altiplano plateau in the Bolivian Andes rose at an average rate of 1.03 ± 0.12 millimeters per year between ∼10.3 and ∼6.7 million years ago. This rate is consistent with the removal of dense lower crust and/or lithospheric mantle as the cause of elevation gain.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144091159680","@type":"Researcher","foaf:name":[{"@value":"Prosenjit Ghosh"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."},{"@value":"Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144091159553","@type":"Researcher","foaf:name":[{"@value":"Carmala N. Garzione"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."},{"@value":"Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144091159552","@type":"Researcher","foaf:name":[{"@value":"John M. Eiler"}],"jpcoar:affiliationName":[{"@value":"Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA."},{"@value":"Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2006-01-27","prism:volume":"311","prism:number":"5760","prism:startingPage":"511","prism:endingPage":"515"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1119365"}],"createdAt":"2006-01-26","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232487904000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spectroscopic isotope ratio measurement of doubly-substituted methane"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567180242619136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Precision and long‐term stability of clumped‐isotope analysis of CO\n                    <sub>2</sub>\n                    using a small‐sector isotope ratio mass spectrometer"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182369840512","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Stable carbon isotopic variation of long chain n-alkanoic acids in the equatorial Pacific sediments over the last 40Ma: Implications for expansion of C4 grassland in South America"}]},{"@id":"https://cir.nii.ac.jp/crid/1360568467936695808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid and Precise Analysis of Carbon Dioxide Clumped Isotopic Composition by Tunable Infrared Laser Differential Spectroscopy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118693143296","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"InterCarb: A Community Effort to Improve Interlaboratory Standardization of the Carbonate Clumped Isotope Thermometer Using Carbonate Standards"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657096930816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seasonal temperature changes obtained from carbonate clumped isotopes of annually laminated tufas from Japan: Discrepancy between natural and synthetic calcites"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241166592","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Principles and development of the stalagmite paleoclimatology"},{"@language":"ja","@value":"石筍古気候学の原理と展開"},{"@language":"ja-Kana","@value":"セキジュンコ キコウガク ノ ゲンリ ト テンカイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792011725824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Carbonate clumped isotope thermometry of fault rocks and its possibilities : tectonic implications from calcites within Himalayan Frontal Fold-Thrust Belt"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1119365"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2018.10.016_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1002/rcm.6431_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1029/2020gc009588_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1186/s40645-021-00435-6_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1016/j.saa.2012.08.028_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2011.0025_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1016/j.orggeochem.2014.07.004_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"},{"@type":"CROSSREF","@value":"10.1021/acs.analchem.9b04466_references_DOI_W9ekIjnnN9WsQ1bqBuAnsJipsbF"}]}