{"@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/1362825893409695744.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.gr.2007.11.003"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1342937X07002018?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S1342937X07002018?httpAccept=text/plain"}}],"dc:title":[{"@value":"Preserved paleo-oceanic plateaus in accretionary complexes: Implications for the contributions of the Pacific superplume to global environmental change"}],"description":[{"notation":[{"@value":"Abstract   We have reinvestigated the mid-Cretaceous plume pulse in relation to paleo-oceanic plateaus from accretionary prisms in the circum-Pacific region, and we have correlated the Pacific superplume activity with catastrophic environmental changes since the Neoproterozoic. The Paleo-oceanic plateaus are dated at 75–150 Ma; they were generated in the Pacific superplume region and are preserved in accretionary prisms. The volcanic edifice composed of both modern and paleo-oceanic plateaus is up to 10.7 × 10 6  km 2  in area and 19.1 × 10 7  km 3  in volume. The degassing rate of CO 2  (0.82 − 1.1 × 10 18  mol/m.y.) suggests a significant impact on Cretaceous global warming. The synchronous occurrence of paleo-oceanic plateaus in accretionary complexes indicates that Pacific superplume pulse activities roughly coincided at the Permo-Triassic boundary and the Vendian–Cambrian boundary interval. The CO 2  expelled by the Pacific superplume probably contributed to environmental catastrophes. The initiation of the Pacific superplume contributed to the snowball Earth event near the Vendian–Cambrian boundary; this was one of the most dramatic events in Earth's history. The scale of the Pacific superplume activity roughly corresponds to the scale of drastic environmental change."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825893409695745","@type":"Researcher","foaf:name":[{"@value":"Atsushi Utsunomiya"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893409695746","@type":"Researcher","foaf:name":[{"@value":"Tsutomu Ota"}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893409695744","@type":"Researcher","foaf:name":[{"@value":"Norihito Suzuki"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"1342937X"}],"prism:publicationName":[{"@value":"Gondwana Research"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2008-08","prism:volume":"14","prism:number":"1-2","prism:startingPage":"115","prism:endingPage":"125"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S1342937X07002018?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S1342937X07002018?httpAccept=text/plain"}],"createdAt":"2007-12-06","modifiedAt":"2019-01-02","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360565165895618688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recognition of ocean plate stratigraphy in accretionary orogens through Earth history: A record of 3.8 billion years of sea floor spreading, subduction, and accretion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166128818048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Generation of hydrous-carbonated plumes in the mantle transition zone linked to tectonic erosion and subduction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182127355904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic setting required for the preservation of sedimentary mélanges in Palaeozoic and Mesozoic accretionary complexes of southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640872466432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Hadean Earth and primordial continents: The cradle of prebiotic life"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204237123328","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ontong-Java Plateau, the World's largest Oceanic Plateau, Has Been Subducted 50%, with the Remaining 50% on the Surface, and with a < 1% Accretion on the Hanging Wall of the Solomon Islands"},{"@language":"ja","@value":"世界最大のサイズのオントンジャワ海台は約50%すでにマントルに沈み込み，残りは西太平洋プレートの表層に残存するが，上盤側プレートに全体の質量の1%以下しかソロモン諸島付加体に付加していない"},{"@value":"The 100s : Significant Exposures of the World (No. 5) Ontong-Java Plateau, the World's largest Oceanic Plateau, Has Been Subducted 50%, with the Remaining 50% on the Surface, and with a < 1% Accretion on the Hanging Wall of the Solomon Islands"}]},{"@id":"https://cir.nii.ac.jp/crid/1390289475879746304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Testing the Ontong Java Nui Hypothesis: The Largest Supervolcano Ever on Earth"},{"@language":"ja","@value":"超オントンジャワ仮説の検証"},{"@value":"超オントンジャワ仮説の検証 : 地球最大の超巨大火山"},{"@language":"ja-Kana","@value":"チョウオントンジャワ カセツ ノ ケンショウ : チキュウ サイダイ ノ チョウキョダイ カザン"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.gr.2007.11.003"},{"@type":"OPENAIRE","@value":"doi_dedup___::2f8b3b9c2f2510d01c6fbcbe93f8b26a"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2013.01.004_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"},{"@type":"CROSSREF","@value":"10.1016/j.gsf.2016.07.005_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"},{"@type":"CROSSREF","@value":"10.5026/jgeography.130.559_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"},{"@type":"CROSSREF","@value":"10.5026/jgeography.120.1035_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2015.08.005_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"},{"@type":"CROSSREF","@value":"10.1016/j.gr.2019.03.006_references_DOI_1CRABJoJ4fWYsjm5z0LMs9rmV3S"}]}