{"@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/1363670320473906688.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.2517/1342-8144-14.4.293"}}],"dc:title":[{"@value":"Panthalassan Seamount-Associated Permian-Triassic Boundary Siliceous Rocks, Mino Terrane, Central Japan"}],"description":[{"notation":[{"@value":"Abstract. We describe the lithology and age of an intact section (NF 1212R) and two reference sections of Panthalassan seamount-associated Permian-Triassic boundary (PTB) siliceous rocks. The sections occupy the upper part of the Hashikadani Formation of the Mino terrane in the Mt. Funabuseyama area, central Japan. Section NF 1212R comprises a lower unit of gray chert (ca. 1.7 m thick), a middle unit of dark gray to black chert (ca. 0.8 m) with a pyrite-rich layer at the top (ca. 0.1 m), and an upper unit of black claystone with thin, intermittent beds of black to dark gray chert (ca. 1.2 m), in ascending order. The chert of the lower and middle units is rich in radiolarian remains with minor siliceous sponge spicules. The black chert of the middle unit is carbonaceous and includes tiny pyrite grains. The black claystone consists of microcrystalline quartz and clay minerals rich in carbonaceous matter. The chert of the upper unit is also carbonaceous and rich in radiolarian remains. The lower and middle u..."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320473906690","@type":"Researcher","foaf:name":[{"@value":"Hiroyoshi Sano"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320473906691","@type":"Researcher","foaf:name":[{"@value":"Kiyoko Kuwahara"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320473906688","@type":"Researcher","foaf:name":[{"@value":"Akira Yao"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320473906689","@type":"Researcher","foaf:name":[{"@value":"Sachiko Agematsu"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"13428144"}],"prism:publicationName":[{"@value":"Paleontological Research"}],"dc:publisher":[{"@value":"The Paleontological Society of Japan"}],"prism:publicationDate":"2010-12","prism:volume":"14","prism:number":"4","prism:startingPage":"293","prism:endingPage":"314"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","createdAt":"2011-01-07","modifiedAt":"2025-01-08","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360009142693938304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Preservation of Permian–Triassic boundary section in the Jurassic accretionary complex of the Lake Hamana, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142741276288","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Scarcity of chert in upper Lower Triassic Panthalassic deep-sea successions of Japan records elevated clastic inputs rather than depressed biogenic silica burial flux following the end-Permian extinction"}]},{"@id":"https://cir.nii.ac.jp/crid/1360021391876789120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Conodont biostratigraphy of a Carboniferous–Permian boundary section in siliceous successions of pelagic Panthalassa revealed by X-ray computed microtomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283693329082496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural assemblages of <i><scp>H</scp>indeodus</i> conodonts from a <scp>P</scp>ermian–<scp>T</scp>riassic boundary sequence, <scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285705812751232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Permian and Triassic Submarine Landslide Deposits in a Jurassic Accretionary Complex in Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707396787200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Natural assemblages of the conodont Clarkina in lowermost Triassic deep-sea black claystone from northeastern Japan, with probable soft-tissue impressions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360572092695937792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Development of Deep-Sea Anoxia in Panthalassa During the Lopingian (Late Permian): Insights From Redox-Sensitive Elements and Multivariate Analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657103565440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sulfur isotope profiles in the pelagic Panthalassic deep sea during the Permian–Triassic transition"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657933426816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconstruction of the multielement apparatus of the earliest Triassic conodont, <i>Hindeodus parvus</i>, using synchrotron radiation X-ray micro-tomography"}]},{"@id":"https://cir.nii.ac.jp/crid/1360853567671418496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Recurrent deposition of organic-rich sediments in Early Triassic pelagic Panthalassa and its relationship with global oceanic anoxia: New data from Kyoto, Southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001277350983680","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Significantly High He Isotopic Signature from the End-Paleozoic (250 Ma) Extinction-related Interval: For Detecting Ancient Extraterrestrial Fluxes through the Earth's History since the Hadean"},{"@language":"ja","@value":"古生代末（2.5億年前）大量絶滅層準の高いヘリウム同位体記録"},{"@value":"古生代末(2.5億年前)大量絶滅層準の高いヘリウム同位体記録 : 冥王代以来の地球史を通した地球外物質流入同定方法の探索"},{"@language":"ja-Kana","@value":"コセイダイマツ(2.5オクネンマエ)タイリョウ ゼツメツソウ ジュン ノ タカイ ヘリウム ドウイタイ キロク : メイオウダイ イライ ノ チキュウシ オ トオシタ チキュウ ガイブツシツ リュウニュウ ドウテイ ホウホウ ノ タンサク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390286426511643136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and age of the oceanic rocks of the Mino Belt in the Funabuseyama area"},{"@language":"ja","@value":"舟伏山地域の美濃帯海洋性岩石の層序と年代"},{"@value":"巡検案内書 舟伏山地域の美濃帯海洋性岩石の層序と年代"},{"@language":"ja-Kana","@value":"ジュンケン アンナイショ シュウフクサンチイキ ノ ミノタイ カイヨウセイ ガンセキ ノ ソウ ジョ ト ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238010069120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy and age of the Permian to Triassic chert-dominant succession of the Mino Belt in the eastern part of the Funabuseyama rock mass, western Gifu Prefecture"},{"@language":"ja","@value":"岐阜県西部，舟伏山岩体東部の美濃帯ペルム系～三畳系チャート優勢層の層序と年代"},{"@language":"ja-Kana","@value":"ギフケン セイブ,シュウフクサンガンタイ トウブ ノ ミノタイ ペルムケイ~サンジョウケイ チャート ユウセイソウ ノ ソウ ジョ ト ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1521136279781203968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Upper Guadalupian to lower Lopingian latentifistularian (Radiolaria) interval zones of the Mino Belt in the Mt. 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