{"@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/1363670319618411648.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1440-1738.2003.00421.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.2003.00421.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.2003.00421.x"}}],"dc:title":[{"@value":"Middle Miocene to Pleistocene radiolarian biostratigraphy in the Northwest Pacific Ocean, ODP Leg 186"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p><jats:bold>Abstract </jats:bold> The Upper Cenozoic sedimentary sequences drilled at Sites 1150 and 1151, Ocean Drilling Program Leg 186, enabled establishment of radiolarian zonation and calibration of the age of bioevents in the forearc area of the northern Japan Islands. The sequences were divided into nine zones from the Pleistocene <jats:italic>Botryostrobus aquilonaris</jats:italic> Zone to the Upper Miocene <jats:italic>Lipmanella redondoensis</jats:italic> Zone at Site 1150, and 11 zones from the Pleistocene <jats:italic>Stylatractus universus</jats:italic> Zone to the Middle Miocene <jats:italic>Dendrospyris</jats:italic>? <jats:italic>sakaii</jats:italic> Zone at Site 1151. These zones correlate successfully with the studied sequences of many of deep‐sea cores in the Northwest Pacific Ocean and with some sections of onshore Japan. Of 67 important radiolarian bioevents recognized during the study, 29 Pleistocene to Upper Miocene events were directly tied to the geomagnetic polarity time scale through the well‐defined paleomagnetic polarity records, and 21 Upper Miocene events were calibrated based on the diatom biostratigraphy. Of these events, 24 geographically widespread events were selected to test synchroneity and usefulness as time‐horizons within the mid‐to‐high latitude of the Northwest Pacific, involving eight other offshore and onshore sections. Examination showed that most of the zonal boundary events are synchronous within the considered region, and that many diachronous events, most of which are eliminated from the zonal scheme, are unreliable events linked to rare and sporadic occurrences of the species. Radiolarian biostratigraphy of the studied cores clearly indicates three major hiatuses in the Middle Pleistocene, Late Miocene and late Middle Miocene. The latter two hiatuses can be correlated to two global oceanic hiatuses, NH6 and NH3, respectively.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380579819312281088","@type":"Researcher","foaf:name":[{"@value":"Shin‐ichi Kamikuri"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319618411650","@type":"Researcher","foaf:name":[{"@value":"Hiroshi Nishi"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319618411649","@type":"Researcher","foaf:name":[{"@value":"Isao Motoyama"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670319618411651","@type":"Researcher","foaf:name":[{"@value":"Saneatsu Saito"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"2004-02-16","prism:volume":"13","prism:number":"1","prism:startingPage":"191","prism:endingPage":"226"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.2003.00421.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.2003.00421.x"}],"createdAt":"2004-02-16","modifiedAt":"2023-10-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232101151104","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Bering Sea radiolarian biostratigraphy and paleoceanography at IODP Site U1341 during the last four million years"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232352976896","@type":"Article","resourceType":"学術雑誌論文(journal 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specimens"},{"@language":"ja","@value":"安房層群清澄層の石灰質ナンノ化石層序と地質時代－<i>Reticulofenestra</i>属の大きさの変化に基づく年代の決定－"},{"@value":"安房層群清澄層の石灰質ナンノ化石層序と地質時代--Reticulofenestra属の大きさの変化に基づく年代の決定"},{"@language":"ja-Kana","@value":"アワソウグン キヨスミソウ ノ セッカイシツ ナンノ カセキソウ ジョ ト チシツ ジダイ Reticulofenestraゾク ノ オオキサ ノ ヘンカ ニ モトズク ネンダイ ノ ケッテイ"},{"@value":"Calcareous nannofossil biostratigraphy and geologic age of the Kiyosumi Formation of the Awa Group, Boso Peninsula, central Jaman: age determination based on size variations of Reticulafwnwstra specimens"},{"@value":"Calcareous nannofossil biostratigraphy and geologic age of the Kiyosumi Formation of the Awa Group, Boso Peninsula, central Japan: Age determination based on size variations of Reticulofenestra specimens (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241645312","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geologic traverse from the Mineoka Belt to the Hayama 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fluid flow near the splay fault zone in the Nankai Trough, off Kii Peninsula"},{"@language":"ja","@value":"潮岬海底谷に露出する南海トラフ分岐断層付近の付加体堆積物の構造・組織・物性と流体移動"},{"@language":"ja-Kana","@value":"シオノミサキ カイテイコク ニ ロシュツ スル ナンカイ トラフ ブンキ ダンソウ フキン ノ フカタイ タイセキブツ ノ コウゾウ ソシキ ブッセイ ト リュウタイ イドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213783424","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology and radiolarian biostratigraphy of the Miocene and Pliocene Series exposed along the Koitogawa River, Boso Peninsula, Japan"},{"@language":"ja","@value":"房総半島，小糸川流域の中新・鮮新統の地質と放散虫化石層序"},{"@language":"ja-Kana","@value":"ボウソウ ハントウ コイトガワ リュウイキ ノ チュウ シン センシントウ ノ チシツ ト ホウサンチュウ カセキソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214177152","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"New age constraints on the Miocene tectonic evolution of southwestern Japan:"},{"@language":"ja","@value":"西南日本の中新世テクトニクスに対する新たな年代制約："},{"@value":"西南日本の中新世テクトニクスに対する新たな年代制約:愛知県設楽地域におけるフィッション・トラック年代測定"},{"@language":"ja-Kana","@value":"セイナン ニホン ノ チュウシンセイ テクトニクス ニ タイスル アラタ ナ ネンダイ セイヤク アイチケンシタラ チイキ ニ オケル フィッション トラック ネンダイ ソクテイ"},{"@value":"New age constraints on the Miocene tectonic evolution of southwestern Japan:fission track ages from the Shitara district, Aichi Prefecture"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214959872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Radiolarians from the Pliocene of the Hokushin district, Nagano Prefecture, Japan"},{"@language":"ja","@value":"長野県北信地域の鮮新統より産出した放散虫化石"},{"@language":"ja-Kana","@value":"ナガノケン ホクシン チイキ ノ センシントウ ヨリ サンシュツ シタ ホウサンチュウ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763106444416","@type":"Article","resourceType":"学術雑誌論文(journal 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