{"@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/1360565166752125440.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature10902"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature10902.pdf"}},{"identifier":{"@type":"URI","@value":"http://www.nature.com/articles/nature10902"}},{"identifier":{"@type":"PMID","@value":"22460897"}},{"identifier":{"@type":"HANDLE","@value":"20.500.11820/69f5f94a-184f-40a5-9553-8f885c7f8075"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Ice-sheet collapse and sea-level rise at the Bølling warming 14,600 years ago"}],"description":[{"notation":[{"@value":"Past sea-level records provide invaluable information about the response of ice sheets to climate forcing. Some such records suggest that the last deglaciation was punctuated by a dramatic period of sea-level rise, of about 20 metres, in less than 500 years. Controversy about the amplitude and timing of this meltwater pulse (MWP-1A) has, however, led to uncertainty about the source of the melt water and its temporal and causal relationships with the abrupt climate changes of the deglaciation. Here we show that MWP-1A started no earlier than 14,650 years ago and ended before 14,310 years ago, making it coeval with the Bølling warming. Our results, based on corals drilled offshore from Tahiti during Integrated Ocean Drilling Project Expedition 310, reveal that the increase in sea level at Tahiti was between 12 and 22 metres, with a most probable value between 14 and 18 metres, establishing a significant meltwater contribution from the Southern Hemisphere. This implies that the rate of eustatic sea-level rise exceeded 40 millimetres per year during MWP-1A."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380284919964211844","@type":"Researcher","foaf:name":[{"@value":"Pierre Deschamps"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211845","@type":"Researcher","foaf:name":[{"@value":"Nicolas Durand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211846","@type":"Researcher","foaf:name":[{"@value":"Edouard Bard"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211840","@type":"Researcher","foaf:name":[{"@value":"Bruno Hamelin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211842","@type":"Researcher","foaf:name":[{"@value":"Gilbert Camoin"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211843","@type":"Researcher","foaf:name":[{"@value":"Alexander L. Thomas"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211841","@type":"Researcher","foaf:name":[{"@value":"Gideon M. Henderson"}]},{"@id":"https://cir.nii.ac.jp/crid/1420564276180621440","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"00376542"},{"@type":"NRID","@value":"1000000376542"},{"@type":"NRID","@value":"9000002439827"},{"@type":"NRID","@value":"9000254740287"},{"@type":"NRID","@value":"9000000649648"},{"@type":"NRID","@value":"9000414499672"},{"@type":"NRID","@value":"9000409996139"},{"@type":"NRID","@value":"9000344128513"},{"@type":"NRID","@value":"9000398626657"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0067813"}],"foaf:name":[{"@value":"Jun'ichi Okuno"}]},{"@id":"https://cir.nii.ac.jp/crid/1380284919964211968","@type":"Researcher","foaf:name":[{"@value":"Yusuke Yokoyama"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1890866216247809921","@type":"Researcher","foaf:name":[{"@value":"Collège de France - Chaire Evolution du climat et de l'océan"}]},{"@id":"https://cir.nii.ac.jp/crid/1890866216247809922","@type":"Researcher","foaf:name":[{"@value":"Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890866216247809920","@type":"Researcher","foaf:name":[{"@value":"Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967926238343","@type":"Researcher","foaf:name":[{"@value":"Collège de France - Chaire Evolution du climat et de l'océan ; Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967926238340","@type":"Researcher","foaf:name":[{"@value":"Collège de France - Chaire Evolution du climat et de l'océan ; Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1892553967926238339","@type":"Researcher","foaf:name":[{"@value":"Chaire Evolution du climat et de l'océan ; Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)"}]},{"@id":"https://cir.nii.ac.jp/crid/1890866216247809923","@type":"Researcher","foaf:name":[{"@value":"Pin, Thierry"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00280836"},{"@type":"EISSN","@value":"14764687"}],"prism:publicationName":[{"@value":"Nature"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2012-03","prism:volume":"483","prism:number":"7391","prism:startingPage":"559","prism:endingPage":"564"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["http://www.springer.com/tdm"],"url":[{"@id":"http://www.nature.com/articles/nature10902.pdf"},{"@id":"http://www.nature.com/articles/nature10902"}],"createdAt":"2012-03-27","modifiedAt":"2023-05-18","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Time%20Factors","dc:title":"Time 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science"},{"@id":"https://cir.nii.ac.jp/all?q=Polynesia","dc:title":"Polynesia"},{"@id":"https://cir.nii.ac.jp/all?q=Earth%20sciences","dc:title":"Earth sciences"},{"@id":"https://cir.nii.ac.jp/all?q=0028-0836","dc:title":"0028-0836"},{"@id":"https://cir.nii.ac.jp/all?q=Geophysics","dc:title":"Geophysics"},{"@id":"https://cir.nii.ac.jp/all?q=Freezing","dc:title":"Freezing"},{"@id":"https://cir.nii.ac.jp/all?q=Climate%20science","dc:title":"Climate science"},{"@id":"https://cir.nii.ac.jp/all?q=Animals","dc:title":"Animals"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU.STU.GP%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D/Earth%20Sciences/Geophysics%20%5Bphysics.geo-ph%5D","dc:title":"[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]"},{"@id":"https://cir.nii.ac.jp/all?q=Ice%20Cover","dc:title":"Ice Cover"},{"@id":"https://cir.nii.ac.jp/all?q=Seawater","dc:title":"Seawater"},{"@id":"https://cir.nii.ac.jp/all?q=History,%20Ancient","dc:title":"History, Ancient"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257043611264","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"21253001"},{"@type":"JGN","@value":"JP21253001"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-21253001/"}],"notation":[{"@language":"ja","@value":"第四紀後期の東南極氷床変動史の復元と地球環境変動システムの解明"},{"@language":"en","@value":"The elucidation of a global environment change system on the basis of the East Antarctic Ice history"}]},{"@id":"https://cir.nii.ac.jp/crid/1040282257133149312","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23501255"},{"@type":"JGN","@value":"JP23501255"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23501255/"}],"notation":[{"@language":"ja","@value":"南極大陸周縁域の大陸棚はなぜ深いのか？"},{"@language":"en","@value":"Why the continental margin around the Antarctica is deeper than other continental shelves ?"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001338815093376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late glacial to deglacial variation of coralgal assemblages in the Great Barrier Reef, Australia"}]},{"@id":"https://cir.nii.ac.jp/crid/1050846638688967168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A sea-level plateau preceding the Marine Isotope Stage 2 minima revealed by Australian sediments"}]},{"@id":"https://cir.nii.ac.jp/crid/1050866882760045824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Regional sea-level highstand triggered Holocene ice sheet thinning across coastal Dronning 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