{"@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/1361418520051241216.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1146/annurev.ecolsys.35.021103.105715"}},{"identifier":{"@type":"URI","@value":"https://www.annualreviews.org/doi/pdf/10.1146/annurev.ecolsys.35.021103.105715"}}],"dc:title":[{"@value":"Consequences of the Cretaceous/Paleogene Mass Extinction for Marine Ecosystems"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p> ▪ Abstract  One of the greatest mass extinctions in Earth's history occurred at the end of the Cretaceous era, sixty-five million years (Myr) ago. Considerable evidence indicates that the impact of a large asteroid or comet was the ultimate cause of this extraordinary event. At the time of mass extinction, the organic flux to the deep sea collapsed, and production of calcium carbonate by marine plankton radically declined. These biogeochemical processes did not fully recover for a few million years. The drastic decline and long lag in final recovery of these processes are most simply explained as consequences of open-ocean ecosystem alteration by the mass extinction. If this explanation is correct, the extent and timing of marine biogeochemical recovery from the end-Cretaceous event was ultimately contingent on the extent and timing of open-ocean ecosystem recovery. The biogeochemical recovery may in turn have created new evolutionary opportunities for a diverse array of marine organisms. </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381418520051241344","@type":"Researcher","foaf:name":[{"@value":"Steven D'Hondt"}],"jpcoar:affiliationName":[{"@value":"Graduate School of Oceanography, University of Rhode Island, Narragansett Bay Campus, Narragansett, Rhode Island 02882;"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"1543592X"},{"@type":"EISSN","@value":"15452069"}],"prism:publicationName":[{"@value":"Annual Review of Ecology, Evolution, and Systematics"}],"dc:publisher":[{"@value":"Annual Reviews"}],"prism:publicationDate":"2005-12-01","prism:volume":"36","prism:number":"1","prism:startingPage":"295","prism:endingPage":"317"},"reviewed":"false","url":[{"@id":"https://www.annualreviews.org/doi/pdf/10.1146/annurev.ecolsys.35.021103.105715"}],"createdAt":"2005-08-17","modifiedAt":"2021-10-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360017282425755520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Species extinction in different time scales"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708512385792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Global climate change driven by soot at the K-Pg boundary as the cause of the mass extinction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565170056182400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"South Pacific Gyre : Subseafloor life and habitability in the South Pacific Gyre"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657283117312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Latest Cretaceous/Paleocene deep-sea ostracode fauna at IODP Site U1407 (western North Atlantic) with special reference to the Cretaceous/Paleogene boundary and the Latest Danian Event"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206496788352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Applications of Isotope-Ratio Mass Spectrometry to Paleoenvironmental Reconstruction"},{"@language":"ja","@value":"同位体質量分析計を用いた環境変動解析"},{"@language":"ja-Kana","@value":"ドウイ タイシツリョウ ブンセキケイ オ モチイタ カンキョウ ヘンドウ カイセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942001216000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Authigenic carbonate precipitation at the end-Guadalupian (Middle Permian) in China : implications for the carbon cycle in ancient anoxic oceans"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1146/annurev.ecolsys.35.021103.105715"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0073-2_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"},{"@type":"CROSSREF","@value":"10.1016/j.plrev.2023.01.014_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"},{"@type":"CROSSREF","@value":"10.1038/srep28427_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"},{"@type":"CROSSREF","@value":"10.2204/iodp.pr.329.2011_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2017.07.003_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"},{"@type":"CROSSREF","@value":"10.5702/massspec.14-59_references_DOI_8UKDfEnIrHtA9Jdx5747AOvlYgJ"}]}