{"@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/1361981471176928640.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1038/nature06588"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/nature06588.pdf"}},{"identifier":{"@type":"URI","@value":"https://www.nature.com/articles/nature06588"}}],"dc:title":[{"@value":"An early Cenozoic perspective on greenhouse warming and carbon-cycle dynamics"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981471176928640","@type":"Researcher","foaf:name":[{"@value":"James C. Zachos"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471176928642","@type":"Researcher","foaf:name":[{"@value":"Gerald R. Dickens"}]},{"@id":"https://cir.nii.ac.jp/crid/1381981471176928641","@type":"Researcher","foaf:name":[{"@value":"Richard E. Zeebe"}]}],"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":"2008-01-16","prism:volume":"451","prism:number":"7176","prism:startingPage":"279","prism:endingPage":"283"},"reviewed":"false","dc:rights":["https://www.springernature.com/gp/researchers/text-and-data-mining","https://www.springernature.com/gp/researchers/text-and-data-mining"],"url":[{"@id":"https://www.nature.com/articles/nature06588.pdf"},{"@id":"https://www.nature.com/articles/nature06588"}],"createdAt":"2008-01-16","modifiedAt":"2025-04-04","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1051693803412094464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Eighteen Coral Genomes Reveal the Evolutionary Origin of Acropora Strategies to Accommodate Environmental Changes"},{"@value":"Eighteen Coral Genomes Reveal the Evolutionary Origin of <i>Acropora</i> Strategies to Accommodate Environmental Changes"},{"@value":"Eighteen coral genomes reveal the evolutionary frigin of Acropora strategies to accommodate environmental changes."}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218350022144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of complex symbiotic relationships in a morphologically derived family of lichen‐forming fungi"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002218436371072","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Australian shelf sediments reveal shifts in Miocene Southern Hemisphere westerlies"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231247877120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Some like it hot: the physiological ecology of C4 plant evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232173802240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine Os isotopic fluctuations in the early Eocene greenhouse interval as recorded by metalliferous umbers from a Tertiary ophiolite in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233003303040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233021883520","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First discovery of Eocene coastal-estuarine ostracods from Japan, with the geological history of the migration of estuarine genera in the Far East"}]},{"@id":"https://cir.nii.ac.jp/crid/1360005516841536256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Planktonic adaptive evolution to the sea surface temperature in the Neoproterozoic inferred from ancestral NDK of marine cyanobacteria"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017280644956544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Enhanced continental chemical weathering during the multiple early Eocene hyperthermals: New constraints from the southern Indian Ocean"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021391860682624","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Evolution of Oceanography of the Central Northwest Pacific Over the Past 10 Million Years With Focus on Late Miocene Global Cooling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283691775476608","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Cenozoic record of the equatorial Pacific carbonate compensation depth"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283692749531136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Baleen boom and bust: a synthesis of mysticete phylogeny, diversity and disparity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283695394809344","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Miocene Ostracods from the Itahana Formation in the Tomioka District, Gunma Prefecture, Central Japan: Paleoenvironmental Significance and Systematics"}]},{"@id":"https://cir.nii.ac.jp/crid/1360284923839373824","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Limnobiophyllum expansum (Lemnoideae, Araceae) from the Early Miocene Hiramaki Formation in the Kani Basin, Gifu Prefecture, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705068637568","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Cenozoic climate change and diversification on the continental shelf and slope: evolution of gastropod diversity in the family Solariellidae (Trochoidea)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705096204928","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Depositional architecture, provenance, and tectonic/eustatic modulation of Miocene submarine fans in the Shikoku Basin: Results from <b>Nankai Trough Seismogenic Zone Experiment</b>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707396726144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of oceanic circulation patterns in the tropical Pacific across the early/middle Miocene boundary as inferred from radiolarian assemblages"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710748180352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contrasting diversification history between insular and continental species of three‐leaved azaleas (<i>Rhododendron</i> sect. <i>Brachycalyx</i>) in East Asia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285715169670528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Drastic shrinking of the Hadley circulation during the mid-Cretaceous supergreenhouse"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286995504269312","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Origin of the early Cenozoic belt boundary thrust and Izanagi–Pacific ridge subduction in the western Pacific margin"}]},{"@id":"https://cir.nii.ac.jp/crid/1360294643751871744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recent strategies for enhancing the catalytic activity of CO2 hydrogenation to formate/formic acid over Pd-based catalyst"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298339697936640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Middle Miocene climate–carbon cycle dynamics: Keys for understanding future trends on a warmer Earth?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118786465152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal Evolution of the Global Species Diversity of\n                    <i>Rhododendron</i>"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584339758356864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleozoic Extinctions in Cosmoclimatological Context: ‘Non-Bolide’ Extraterrestrial Causes for Global Chilling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846639280307840","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interglacials of the last 800,000 years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658410899456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earth system feedback statistically extracted from the Indian Ocean deep-sea sediments recording Eocene hyperthermals"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848662554980224","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The turnover of continental planktonic diatoms near the middle/late Miocene boundary and their Cenozoic evolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707133856000","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Automated detection of microfossil fish teeth from slide images using combined deep learning models"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815672454784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Porcelaneous larger foraminiferal responses to Oligocene–Miocene global changes"}]},{"@id":"https://cir.nii.ac.jp/crid/1361975841943639040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Variation in the eastern North Pacific subtropical gyre (California Current system) during the Middle to Late Miocene as inferred from radiolarian assemblages"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238051584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Re-examination of the cause of the Paleocene-Eocene thermal maximum, based on global carbon-cycle modeling"},{"@language":"ja","@value":"地球表層炭素循環モデリングに基づく暁新世／始新世境界温暖化極大の発生原因の再検討"},{"@language":"ja-Kana","@value":"チキュウ ヒョウソウ タンソ ジュンカン モデリング ニ モトズク ギョウシンセイ シシンセイ キョウカイ オンダンカ キョクダイ ノ ハッセイ ゲンイン ノ サイケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390002184893412352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Effect of ocean acidification on marine phytoplankton and biogeochemical cycles"},{"@language":"ja","@value":"海洋酸性化が植物プランクトンの動態および物質循環に及ぼす影響"},{"@language":"ja-Kana","@value":"カイヨウ サンセイカ ガ ショクブツ プランクトン ノ ドウタイ オヨビ ブッシツ ジュンカン ニ オヨボス エイキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215185792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Quantitative examination of the cause of the Paleocene-Eocene thermal maximum using an atmosphere-ocean box model"},{"@language":"ja","@value":"大気―海洋ボックスモデルによる暁新世／始新世境界温暖化極大の発生原因の定量的検討"},{"@language":"ja-Kana","@value":"タイキ カイヨウ ボックス モデル ニ ヨル ギョウ シン セイ シシンセイ キョウカイ オンダンカ キョクダイ ノ ハッセイ ゲンイン ノ テイリョウテキ ケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217928576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The depositional environment of the singular Middle Miocene strata from southwestern Tomioka City, Gunma Prefecture, central Japan, from the view point of fossil ostracod assemblage"},{"@language":"ja","@value":"介形虫化石群からみた群馬県富岡市南西部に分布する中部中新統の特異な岩相の堆積環境"},{"@language":"ja-Kana","@value":"カイケイチュウ カセキグン カラ ミタ グンマケン トミオカシ ナンセイブ ニ ブンプ スル チュウブ チュウ シントウ ノ トクイ ナ ガンソウ ノ タイセキ カンキョウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390292572064494720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modelling the Past and Future Climate by Dr. Syukuro Manabe"},{"@language":"ja","@value":"眞鍋淑郎先生による気候の過去と将来の研究"}]},{"@id":"https://cir.nii.ac.jp/crid/1390849376470215168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"SIMS を用いた中生代放散虫岩の酸素同位体分析"},{"@language":"en","@value":"Oxygen isotope analysis of Mesozoic radiolarites using SIMS"}]},{"@id":"https://cir.nii.ac.jp/crid/1523388079575916160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Radiolarian biostratigraphy and faunal turnover across the early/middle Miocene boundary in the equatorial Pacific"}]},{"@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”"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942185017728","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Long period astronomical cycles from the Triassic to Jurassic bedded chert sequence (Inuyama, Japan) : geologic evidences for the chaotic behavior of solar planets"}]},{"@id":"https://cir.nii.ac.jp/crid/2051996266972605440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleoceanographic history of the Japan Sea over the last 9.5 million years inferred from radiolarian assemblages (IODP Expedition 346 Sites U1425 and U1430)"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1038/nature06588"},{"@type":"CROSSREF","@value":"10.1111/nph.13553_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1126/sciadv.1602567_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1007/s00442-018-4191-6_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1017/jpa.2018.103_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1017/s0016756817000693_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.2517/1342-8144-17.2.138_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2019.06.014_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.2517/2018pr018_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.gca.2022.05.022_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1029/2023pa004789_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1038/nature11360_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1098/rsos.140434_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1002/ece3.513_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1002/ggge.20107_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1111/jbi.12924_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5047/eps.2012.09.004_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1111/iar.12320_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.jcou.2021.101765_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1130/2022.2556(05)_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0204-7_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5575/geosoc.117.217_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5575/geosoc.116.418_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.2517/2018pr024_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1093/molbev/msab314_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5363/tits.27.2_14_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.2517/prs220002_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1002/2015rg000482_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5194/cp-8-1323-2012_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1038/s41598-017-11470-z_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1186/s40645-018-0239-9_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1371/journal.pone.0198003_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2012.0074_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2010.12.007_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2017.08.028_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1093/molbev/msaa216_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.acags.2022.100092_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.palaeo.2023.111916_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.9795/bullgsj.71.355_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.1016/j.marmicro.2019.101817_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"},{"@type":"CROSSREF","@value":"10.5928/kaiyou.20.5_101_references_DOI_KDQlPokhOPvJ737NtJDcjkSuvtE"}]}