{"@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/1360869856053595392.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/s41467-024-50207-1"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41467-024-50207-1.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/s41467-024-50207-1"}},{"identifier":{"@type":"DOI","@value":"10.5445/ir/1000172575"}},{"identifier":{"@type":"HANDLE","@value":"11093/7332"}},{"identifier":{"@type":"HANDLE","@value":"11568/1251668"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Sustained North Atlantic warming drove anomalously intense MIS 11c interglacial"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Abstract</jats:title><jats:p>The Marine Isotope Stage (MIS) 11c interglacial and its preceding glacial termination represent an enigmatically intense climate response to relatively weak insolation forcing. So far, a lack of radiometric age control has confounded a detailed assessment of the insolation-climate relationship during this period. Here, we present <jats:sup>230</jats:sup>Th-dated speleothem proxy data from northern Italy and compare them with palaeoclimate records from the North Atlantic region. We find that interglacial conditions started in subtropical to middle latitudes at 423.1 ± 1.3 thousand years (kyr) before present, during a first weak insolation maximum, whereas northern high latitudes remained glaciated (sea level ~ 40 m below present). Some 14.5 ± 2.8 kyr after this early subtropical onset, peak interglacial conditions were reached globally, with sea level 6–13 m above present, despite weak insolation forcing. We attribute this remarkably intense climate response to an exceptionally long (~15 kyr) episode of intense poleward heat flux transport prior to the MIS 11c optimum.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380869856053595395","@type":"Researcher","foaf:name":[{"@value":"Hsun-Ming Hu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595648","@type":"Researcher","foaf:name":[{"@value":"Gianluca Marino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595662","@type":"Researcher","foaf:name":[{"@value":"Carlos Pérez-Mejías"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595521","@type":"Researcher","foaf:name":[{"@value":"Christoph Spötl"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595659","@type":"Researcher","foaf:name":[{"@value":"Yusuke Yokoyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595694","@type":"Researcher","foaf:name":[{"@value":"Jimin Yu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595783","@type":"Researcher","foaf:name":[{"@value":"Eelco Rohling"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801210243328","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"60231263"},{"@type":"NRID","@value":"1000060231263"},{"@type":"ORCID","@value":"0000-0003-3678-257X"},{"@type":"NRID","@value":"9000405633529"},{"@type":"NRID","@value":"9000386337169"},{"@type":"NRID","@value":"9000257917695"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0016991"}],"foaf:name":[{"@value":"Akihiro Kano"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595535","@type":"Researcher","foaf:name":[{"@value":"Patrick Ludwig"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595681","@type":"Researcher","foaf:name":[{"@value":"Joaquim G. Pinto"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595685","@type":"Researcher","foaf:name":[{"@value":"Véronique Michel"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595562","@type":"Researcher","foaf:name":[{"@value":"Patricia Valensi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595528","@type":"Researcher","foaf:name":[{"@value":"Xin Zhang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595397","@type":"Researcher","foaf:name":[{"@value":"Xiuyang Jiang"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595671","@type":"Researcher","foaf:name":[{"@value":"Horng-Sheng Mii"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595394","@type":"Researcher","foaf:name":[{"@value":"Wei-Yi Chien"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595690","@type":"Researcher","foaf:name":[{"@value":"Hsien-Chen Tsai"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595560","@type":"Researcher","foaf:name":[{"@value":"Wen-Hui Sung"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595556","@type":"Researcher","foaf:name":[{"@value":"Chia-Hao Hsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595692","@type":"Researcher","foaf:name":[{"@value":"Elisabetta Starnini"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595785","@type":"Researcher","foaf:name":[{"@value":"Marta Zunino"}]},{"@id":"https://cir.nii.ac.jp/crid/1380869856053595673","@type":"Researcher","foaf:name":[{"@value":"Chuan-Chou Shen"}]}],"contributor":[{"@id":"https://cir.nii.ac.jp/crid/1894243916266881042","@type":"Researcher","foaf:name":[{"@value":"Institut of Global environment change, Xi'an Jiaotong University"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881045","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 7329) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [Occitanie])"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881064","@type":"Researcher","foaf:name":[{"@value":"Universität Innsbruck [Innsbruck]"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881055","@type":"Researcher","foaf:name":[{"@value":"Department of Civilizations and Forms of Knowledge, University of Pisa"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881029","@type":"Researcher","foaf:name":[{"@value":"Key laboratory of humid subtropical eco-geographical processes, Fujian Normal University"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881050","@type":"Researcher","foaf:name":[{"@value":"European Project: 101052653,LATEUROPE"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881056","@type":"Researcher","foaf:name":[{"@value":"Toirano Cave, 17055, Toirano"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881024","@type":"Researcher","foaf:name":[{"@value":"Atmosphere and Ocean Research Institute [Kashiwa-shi] (AORI) ; The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881054","@type":"Researcher","foaf:name":[{"@value":"High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC) ; National Taiwan University [Taiwan] (NTU)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881046","@type":"Researcher","foaf:name":[{"@value":"Department of Earth and Planetary Science [Tokyo] ; Graduate School of Science [Tokyo] ; The University of Tokyo (UTokyo)-The University of Tokyo (UTokyo)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881052","@type":"Researcher","foaf:name":[{"@value":"Radiogenic Isotope Facility - School of Earth Sciences"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881036","@type":"Researcher","foaf:name":[{"@value":"Laoshan Laboratory"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881049","@type":"Researcher","foaf:name":[{"@value":"Research Center for Future Earth, National Taiwan University"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881032","@type":"Researcher","foaf:name":[{"@value":"Research School of Earth Sciences [ANU, Canberra] (RSES) ; ANU College of Science [Canberra] ; Australian National University (ANU)-Australian National University (ANU)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881025","@type":"Researcher","foaf:name":[{"@value":"Centro de Investigacion Marina, GEOMA, Universidade de Vigo"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881033","@type":"Researcher","foaf:name":[{"@value":"Department of Earth Sciences [Utrecht] ; Universiteit Utrecht / Utrecht University [Utrecht]"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881027","@type":"Researcher","foaf:name":[{"@value":"Histoire naturelle de l'Homme préhistorique (HNHP) ; Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881058","@type":"Researcher","foaf:name":[{"@value":"Institute of Meteorology and Climate Research ; Karlsruhe Institute of Technology = Karlsruher Institut für Technologie (KIT)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881041","@type":"Researcher","foaf:name":[{"@value":"Culture et Environnements, Préhistoire, Antiquité, Moyen-Age (CEPAM) ; Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Centre National de la Recherche Scientifique (CNRS)-Université Côte d'Azur (UniCA)"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881039","@type":"Researcher","foaf:name":[{"@value":"Michel, Veronique"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881059","@type":"Researcher","foaf:name":[{"@value":"Géoazur (GEOAZUR 7329) ; Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; Université Côte d'Azur (UniCA)-Université Côte d'Azur (UniCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD [France-Sud])"}]},{"@id":"https://cir.nii.ac.jp/crid/1894243916266881044","@type":"Researcher","foaf:name":[{"@value":"Ocean and Earth Science [Southampton] ; University of Southampton-National Oceanography Centre (NOC)"}]}],"publication":{"publicationIdentifier":[{"@type":"EISSN","@value":"20411723"}],"prism:publicationName":[{"@value":"Nature Communications"}],"dc:publisher":[{"@value":"Springer Science and Business Media LLC"}],"prism:publicationDate":"2024-07-15","prism:volume":"15","prism:number":"1","prism:startingPage":"5933"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","dc:rights":["https://creativecommons.org/licenses/by/4.0","https://creativecommons.org/licenses/by/4.0"],"url":[{"@id":"https://www.nature.com/articles/s41467-024-50207-1.pdf"},{"@id":"https://www.nature.com/articles/s41467-024-50207-1"}],"createdAt":"2024-07-15","modifiedAt":"2024-07-15","foaf:topic":[{"@id":"https://cir.nii.ac.jp/all?q=Vegetation","dc:title":"Vegetation"},{"@id":"https://cir.nii.ac.jp/all?q=2510.07%20Oceanograf%C3%ADa%20F%C3%ADsica","dc:title":"2510.07 Oceanografía Física"},{"@id":"https://cir.nii.ac.jp/all?q=Isotope","dc:title":"Isotope"},{"@id":"https://cir.nii.ac.jp/all?q=Science","dc:title":"Science"},{"@id":"https://cir.nii.ac.jp/all?q=Events","dc:title":"Events"},{"@id":"https://cir.nii.ac.jp/all?q=Q","dc:title":"Q"},{"@id":"https://cir.nii.ac.jp/all?q=Greenland%20ice-sheet","dc:title":"Greenland ice-sheet"},{"@id":"https://cir.nii.ac.jp/all?q=Global%20temperature","dc:title":"Global temperature"},{"@id":"https://cir.nii.ac.jp/all?q=Article","dc:title":"Article"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSHS%5DHumanities%20and%20Social%20Sciences","dc:title":"[SHS]Humanities and Social Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU%5D%20Sciences%20of%20the%20Universe%20%5Bphysics%5D","dc:title":"[SDU] Sciences of the Universe [physics]"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSDU%5DSciences%20of%20the%20Universe%20%5Bphysics%5D","dc:title":"[SDU]Sciences of the Universe [physics]"},{"@id":"https://cir.nii.ac.jp/all?q=2502.05%20Paleoclimatolog%C3%ADa","dc:title":"2502.05 Paleoclimatología"},{"@id":"https://cir.nii.ac.jp/all?q=Record","dc:title":"Record"},{"@id":"https://cir.nii.ac.jp/all?q=North%20Atlantic%20warming,%20Marine%20Isotope%20Stage%2011c,%20interglacial,%20sea%20level,%20230Th-dated%20speleothem,%20Toirano,%20Ba%CC%80sura%20Cave,%20northern%20Italy","dc:title":"North Atlantic warming, Marine Isotope Stage 11c, interglacial, sea level, 230Th-dated speleothem, Toirano, Bàsura Cave, northern Italy"},{"@id":"https://cir.nii.ac.jp/all?q=%5BSHS%5D%20Humanities%20and%20Social%20Sciences","dc:title":"[SHS] Humanities and Social Sciences"},{"@id":"https://cir.nii.ac.jp/all?q=Mediterranean%20climate","dc:title":"Mediterranean climate"},{"@id":"https://cir.nii.ac.jp/all?q=Climate%20variability","dc:title":"Climate variability"},{"@id":"https://cir.nii.ac.jp/all?q=2503.04%20Geocronolog%C3%ADa%20y%20Radiois%C3%B3topos","dc:title":"2503.04 Geocronología y Radioisótopos"},{"@id":"https://cir.nii.ac.jp/all?q=Glacial%20cycles","dc:title":"Glacial cycles"},{"@id":"https://cir.nii.ac.jp/all?q=Sea-level","dc:title":"Sea-level"}],"project":[{"@id":"https://cir.nii.ac.jp/crid/1040297504286188160","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23KK0013"},{"@type":"JGN","@value":"JP23KK0013"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23KK0013/"}],"notation":[{"@language":"ja","@value":"ヒプシサーマル：完新世の気温復元不一致問題に挑む"},{"@language":"en","@value":"Study to investigate the Holocene Temperature Conundrum"}]},{"@id":"https://cir.nii.ac.jp/crid/1040848250647685888","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"20H00191"},{"@type":"JGN","@value":"JP20H00191"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20H00191/"}],"notation":[{"@language":"ja","@value":"石筍とトゥファのレアアイソトープで復元する温暖期日本列島の高解像度気候記録"},{"@language":"en","@value":"High-resolution paleoclimate records of the Japanese Islands during warm periods reconstructed from rare isotopes in stalagmites and tufas"}]},{"@id":"https://cir.nii.ac.jp/crid/1040859757891745024","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"23K17696"},{"@type":"JGN","@value":"JP23K17696"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-23K17696/"}],"notation":[{"@language":"ja","@value":"三重炭酸凝集同位体による新たな温度プロキシの開発"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360011142931095168","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The configuration of Northern Hemisphere ice sheets through the Quaternary"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142931301760","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Ice Age Terminations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360011142931979392","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A Pliocene‐Pleistocene stack of 57 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ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292621386670464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Asian monsoon over the past 640,000 years and ice age terminations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298754841411712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tracking westerly wind directions over Europe since the middle Holocene"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298765155712128","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Speleothem record attests to stable environmental conditions during Neanderthal–modern human turnover in southern Italy"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302870441307904","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Abrupt CO\n            <sub>2</sub>\n            release to the atmosphere under glacial and early interglacial climate 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