{"@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/1361699995488921728.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1130/0016-7606(1995)107<1164:mlccot>2.3.co;2"}}],"dc:title":[{"@value":"Middle–Late Cretaceous climate of the southern high latitudes: Stable isotopic evidence for minimal equator-to-pole thermal gradients"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699995488921728","@type":"Researcher","foaf:name":[{"@value":"Brian T. Huber"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995488921729","@type":"Researcher","foaf:name":[{"@value":"David A. Hodell"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699995488921730","@type":"Researcher","foaf:name":[{"@value":"Christopher P. Hamilton"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00167606"}],"prism:publicationName":[{"@value":"Geological Society of America Bulletin"}],"dc:publisher":[{"@value":"Geological Society of America"}],"prism:publicationDate":"1995-10","prism:volume":"107","prism:number":"10","prism:startingPage":"1164","prism:endingPage":"1191"},"reviewed":"false","createdAt":"2002-07-27","modifiedAt":"2018-03-06","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232050997888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the composition of deep-water masses in the Late Cretaceous ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280665785856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Abrupt episode of mid-Cretaceous ocean acidification triggered by massive volcanism"}]},{"@id":"https://cir.nii.ac.jp/crid/1360023712395041024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shallow-water temperature seasonality in the middle Cretaceous mid-latitude northwestern Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285713557040256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"Louisville Seamount Trail"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643757131904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhanced hydrological cycle during Oceanic Anoxic Event 2 at southern high latitudes: New insights from IODP Site U1516"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118733830656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Exploring the paleoceanographic changes registered by planktonic foraminifera across the Cenomanian-Turonian boundary interval and Oceanic Anoxic Event 2 at southern high latitudes in the Mentelle Basin (SE Indian Ocean)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640429630592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Pole to equator temperature gradient for coniacian time, late cretaceous: Oxygen and carbon isotopic data on the Koryak upland and Hokkaido"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861705562243840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Biotic and Paleoceanographic Changes Across the Late Cretaceous Oceanic Anoxic Event 2 in the Southern High Latitudes (IODP Sites U1513 and U1516, SE Indian Ocean)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204146519808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The origin of Cretaceous black shales: a change in the surface ocean ecosystem and its triggers"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229065856","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"白亜紀における大規模火山活動と地球環境変動のリンク"},{"@language":"en","@value":"Linkage between Massive Volcanic Events and Global Extreme Climatic Events in the Cretaceous Period"},{"@language":"ja-Kana","@value":"ハクアキ ニ オケル ダイキボ カザン カツドウ ト チキュウ カンキョウ ヘンドウ ノ リンク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204550032384","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strontium, .DELTA.18O and .DELTA.13C as palaeo-indicators of unconformities: Case of the Aleg and Abiod formations (Upper Cretaceous) in the Miskar Field, Southeastern Tunisia"}]},{"@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":"10.1130/0016-7606(1995)107<1164:mlccot>2.3.co;2"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0073-2_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1038/s41561-022-01115-w_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.3389/fmars.2024.1324436_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.2204/iodp.pr.330.2011_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.2343/geochemj.40.405_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.534_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1016/j.chemgeo.2013.08.008_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2022.103735_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1016/j.gloplacha.2021.103595_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1007/s12583-012-0230-0_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.2183/pjab.91.273_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"},{"@type":"CROSSREF","@value":"10.1029/2022pa004474_references_DOI_ZsCyf4LMyqOaRToCGczZqUDEf9l"}]}