{"@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/1361137045213487104.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/98gb01927"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98GB01927"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98GB01927"}}],"dc:title":[{"@value":"Does atmospheric CO<sub>2</sub> police the rate of chemical weathering?"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>A case is made that in the absence of an effective feedback control on the rate of delivery of CaO to the oceans, the CO<jats:sub>2</jats:sub> content of the Earth's atmosphere would have wandered over a large range threatening life either by overheating or by carbon dioxide starvation. In this paper, we defend the suggestion by <jats:italic>Walker et al.</jats:italic> [1981] that control is exerted by the interaction between the CO<jats:sub>2</jats:sub> content of the atmosphere and the continental weathering rates. We contend that in spite of the arguments raised against it [<jats:italic>Raymo and Ruddiman</jats:italic>, 1992; <jats:italic>Edmond and Huh</jats:italic>, 1997] the CO<jats:sub>2</jats:sub>‐ chemical weathering feedback is the dominant mechanism that stabilizes the atmospheric carbon dioxide content.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137045213487104","@type":"Researcher","foaf:name":[{"@value":"Wallace S. Broecker"}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045213487105","@type":"Researcher","foaf:name":[{"@value":"Abhijit Sanyal"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"08866236"},{"@type":"EISSN","@value":"19449224"}],"prism:publicationName":[{"@value":"Global Biogeochemical Cycles"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1998-09","prism:volume":"12","prism:number":"3","prism:startingPage":"403","prism:endingPage":"408"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98GB01927"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98GB01927"}],"createdAt":"2004-02-04","modifiedAt":"2023-09-26","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/2050025942136465280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Perspective on the response of marine calcifiers to global warming and ocean acidification : behavior of corals and foraminifera in a high CO2 world “hot house”"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/98gb01927"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0239-9_references_DOI_6I8oXmdlLSm1rGMiabRK6rju3dB"}]}