{"@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/1362262943531504768.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0031-0182(94)90241-0"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0031018294902410?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:0031018294902410?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30005404420"}}],"dc:title":[{"@value":"Neogene paleogeography and marine climate of the Japanese Islands based on shallow-marine molluscs"}],"description":[{"notation":[{"@value":"Abstract   Based on a large amount of data on Neogene shallow-marine molluscs of the Japanese Islands, paleogeography and marine climate are reconstructed at 19−17 Ma, 16 Ma, 13 Ma, 10−6 Ma, 4−3 Ma and 2−1 Ma. The definition of marine climates such as warm-temperate, mild-temperate, cool-temperate, and so on basically follows that by  Nishimura (1981)  which is characterized by subdivisions of the transitional zone between the subtropical and subarctic regions in the modern sea around the Japanese Islands. The distribution patterns of shallow-marine molluscan genera/species along the Japanese Islands in both modern and Neogene seas are considered to reflect accurately the surface thermal conditions.  The middle Miocene climatic optimum at about 16 Ma is well displayed by the northward extension of mangrove swamp and  Vicaryella -bearing faunas within the Yatsuo-Kadonosawa faunal province in northeastern Honshu and southern Hokkaido. After this warming, a gradual cooling commenced at about 14−13 Ma, as indicated by the disappearance of tropical molluscs and the occurrence of survival elements such as the genera  Nanaochlamys, Kotorapecten, Sinum , and so on, which are descendants of earlier genera. However, this cooling is considered to be a minor climatic deterioration, from tropical to subtropical in southern Japan, and from subtropical to warm-temperate in central to northeastern Honshu. The late Miocene molluscan faunas of Japan are composed mainly of such endemic elements as  Miyagipecten matsumoriensis, Dosinia (Kaneharaia) kaneharai, Mercenaria chitaniana  and so on. This assemblage is interpreted as having flourished under mild-temperate conditions, on the basis of the thermal tolerances of these genera. Middle and late Miocene shallow-marine molluscs of the northern Pacific, including those from Hokkaido, Sakhalin and Kamchatka, are considered to have occupied a single temperate zoogeographic province.  Early Pliocene and Plio-Pleistocene molluscan faunas of Japan and the Northeast Pacific display a remarkable convergence of subtropical and subarctic/cool-temperate realms."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262943531504768","@type":"Researcher","foaf:name":[{"@value":"Kenshiro Ogasawara"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00310182"}],"prism:publicationName":[{"@value":"Palaeogeography, Palaeoclimatology, Palaeoecology"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1994-04","prism:volume":"108","prism:number":"3-4","prism:startingPage":"335","prism:endingPage":"351"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:0031018294902410?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:0031018294902410?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360008289761316480","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The Structure of the Miocene Northwestern Pacific Ichthyofauna as Revealed By Two Fossil Fish Assemblages From Sakhalin Island, Russia"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710769900544","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Oligocene–Neogene fossil history of Asian endemic conifer 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region"},{"@language":"ja","@value":"サハリン・カムチャッカ地域における新生代の古気候・地球環境変動"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204085852416","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Ophiura sarsii sarsii (Echinodermata, Ophiuroidea) from the Late Pliocene Hachioji Formation in Niigata Prefecture, Central Japan"},{"@language":"ja-Kana","@value":"Ophiura sarsii sarsii Echinodermata Oph"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204086049664","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A new Miocene <i>Yabepecten</i> (Bivalvia: Pectinidae) from the Hongô Formation in northeast Japan"},{"@value":"A new Miocene Yabepecten (Bivalvia: Pectinidae) from the Hongo Formation in northeast Japan"},{"@language":"ja-Kana","@value":"new Miocene Yabepecten Bivalvia Pectinidae from the Hongo Formation in northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204086332672","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Late Miocene ostracodes from the Kubota Formation, Higashi-Tanagura Group, Northeast Japan, and their implications for bottom environments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266394880","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"茨城県桂村で発見された中期中新世Stegolopbodon属(長鼻類)の下顎骨化石"},{"@language":"en","@value":"A middle Miocene mandible of Stegolophodon (Proboscidea, Mammalia) discovered in Katsura Village, Ibaraki Prefecture, eastern Japan"},{"@value":"茨城県桂村で発見された中期中新世Stegolophodon属(長鼻類)の下顎骨化石"},{"@language":"ja-Kana","@value":"イバラキケン カツラムラ デ ハッケン サレタ チュウキ チュウ シンセイ Stegolophodonゾク チョウ ビルイ ノ カガクコツ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204266413952","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"新潟県津川地域の中部〜上部中新統の珪藻化石層序およびテフラ層序に基づく年代層序"},{"@language":"en","@value":"Integrated chronostratigraphy of diatom biostratigraphy and tephrostratigraphy for the middle to upper Miocene sequence in the Tsugawa basin, Niigata Prefecture, central Japan"},{"@language":"ja-Kana","@value":"ニイガタケン ツガワ チイキ ノ チュウブ ジョウブ チュウ シントウ ノ ケイソウ カセキソウ ジョ オヨビ テフラソウ ジョ ニ モトヅク ネンダイソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205194244992","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Cenozoic molluscan faunas and climatic changes in the northern Pacific related to Pacific gateways: review and perspective"},{"@language":"ja","@value":"太平洋と他の海洋の開閉事件に関連した北太平洋地域新生代の貝類化石群集と古気候変動：レビューと今後の展望"},{"@value":"Cenozoic molluskan faunas and climatic changes in the northern Pacific related to Pacific 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Dosiniinae)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205194383872","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"宮城県南部・福島県北部に分布する中新統の珪藻化石層序と貝類化石"},{"@language":"en","@value":"Diatom biostratigraphy and molluscan fossils of the Miocene formations in the southern part of Miyagi Prefecture and the northern part of Fukushima Prefecture, Japan."},{"@language":"ja-Kana","@value":"ミヤギケン ナンブ フクシマケン ホクブ ニ ブンプ スル チュウシントウ ノ ケイソウ カセキソウ ジョ ト カイルイ カセキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205219468160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High-resolution sequence stratigraphy in an incised-valley system on the basis of sedimentary organic matter, sulfur content and fossil diatom: An example from Miocene to Pliocene Tatsunokuchi Formation, Iwate Prefecture, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206236913664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Molluscan fossils from the middle Miocene in Kenbuchi-cho, northern Hokkaido, and their significance"},{"@language":"ja","@value":"北海道北部, 剣淵町の中部中新統の貝類化石とその意義"},{"@language":"ja-Kana","@value":"ホッカイドウ ホクブ ケンブチチョウ ノ チュウブ チュウ シントウ ノ カイルイ カセキ ト ソノ イギ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237158784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influx of warm-water current to Japan Sea during the Pliocene"},{"@language":"ja","@value":"鮮新世における日本海への暖流の流入"},{"@value":"鮮新世における日本海への暖流の流入--富山市八尾町の三田層産軟体動物群の検討を通じて"},{"@language":"ja-Kana","@value":"センシンセイ ニ オケル ニホンカイ エノ ダンリュウ ノ リュウニュウ トヤマシ ヤツオマチ ノ ミタソウサン ナンタイ ドウブツグン ノ ケントウ オ ツウジテ"},{"@value":"Influx of warm-water current to Japan Sea during the Pliocene (in Japanese with English abstract)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237572992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influence of a warm-water current on the northern Fossa Magna Region during the Pliocene, based on analyses of molluscan fauna from the Shitoka Formation and the lowest part of the Uonuma Group along the Kamakurazawa River in Minami-Uonuma City, Niigata Prefecture"},{"@language":"ja","@value":"鮮新世における北部フォッサマグナ地域への暖流の影響－新潟県南魚沼市鎌倉沢川の四十日層および魚沼層群最下部産軟体動物群の検討を通じて－"},{"@language":"ja-Kana","@value":"センシンセイ ニ オケル ホクブ フォッサマグナ チイキ エ ノ ダンリュウ ノ エイキョウ ニイガタ ケンナン ウオヌマシ カマクラ ザワガワ ノ シトカソウ オヨビ ウオヌマソウグン サイ カブ サン ナンタイドウブツグン ノ ケントウ オ ツウジテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241144576","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Middle to Upper Miocene and Pliocene sequences of southwest Sendai, as a standard referential stratigraphy in the Pacific side of NE Japan"},{"@language":"ja","@value":"仙台南西部に分布する東北日本太平洋側標準層序としての中・上部中新統および鮮新統"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241861120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Influence of environment change on benthic fauna during the early Pleistocene in the central part of Japan Sea Borderland:"},{"@language":"ja","@value":"日本海中部沿岸域における前期更新世の環境変動による底生動物群への影響："},{"@value":"日本海中部沿岸域における前期更新世の環境変動による底生動物群への影響 : 富山県小矢部市田川周辺の大桑層産軟体動物群の検討を通じて"},{"@language":"ja-Kana","@value":"ニホンカイ チュウブ エンガンイキ ニ オケル ゼンキ コウシン セイ ノ カンキョウ ヘンドウ ニ ヨル テイセイ ドウブツグン エ ノ エイキョウ : トヤマケン オヤベシ タガワ シュウヘン ノ ダイソウソウサン ナンタイドウブツグン ノ ケントウ オ ツウジテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679041255168","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Events of Japanese Cenozoic geology and paleoenvironments and their causes"},{"@language":"ja","@value":"本邦新生代の地質・古環境事件とその原因"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679062944768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Latest early-earliest middle Miocene deep-sea molluscs in the Japan Sea borderland — the warm-water Higashibessho fauna in Toyama Prefecture, central Japan"},{"@value":"Latest early-earliest middle Miocene deep-sea molluscs in the Japan Sean borderland--the warm-water Higashibessho fauna in Toyama Prefecture, central Japan"},{"@value":"Latest early-earliest middle Miocene deep-sea molluscs in the Japan Sea borderland – the warm-water Higashibessho fauna in Toyama Prefecture, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679063843712","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"<i>Trophonopsis</i> Bucquoy, Dautzenberg and Dollfus, 1882 (Gastropoda, Muricidae) from the Plio-Pleistocene deposits in Japan"},{"@value":"Trophonopsis Bucquoy, Dautzenberg and Dollfus, 1882 (Gastropoda, Muricidae) from the Plio-Pleistocene deposits in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679063866240","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fossil crabs (Crustacea : Decapoda : Brachyura) from the latest Miocene Senhata Formation, Boso Peninsula, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064109696","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Taxonomy and distribution of Macoma (Rexithaerus) (Bivalvia : Tellinidae) in the northwestern Pacific"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064235648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Taxonomy and evolution of the genus Ocinebrellus (Gastropoda : Muricidae) in Japan"},{"@language":"ja-Kana","@value":"Taxonomy and evolution of the genus Oci"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679064681984","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Biogeography of the genus Neptunea (Gastropoda : Buccinidae) from the Pliocene and the lower Pleistocene of the Japan Sea borderland"},{"@language":"ja-Kana","@value":"Biogeography of the genus Neptunea Gast"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680170932608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"福島県東棚倉地域に分布する上部中新統久保田層の浮遊性有孔虫生層序"},{"@language":"en","@value":"Planktonic foraminiferal biostratigraphy of the upper Miocene Kubota Formation in the eastern Tanagura area,Northeast Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214117632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The occurrence of the fossil mytilid bivalve <i>Mytilus tichanovitchi</i> Makiyama from the Miocene Shimonita Formation, Gunma Prefecture, central Japan: Re-examination of its biostratigraphic and marine paleoclimatic significance"},{"@language":"ja","@value":"群馬県の中新統下仁田層から産出した化石イガイ科二枚貝 <i>Mytilus tichanovitchi</i> Makiyama－その生層序学的・海洋古気候学的意義の再検討－"},{"@value":"群馬県の中新統下仁田層から産出した化石イガイ科二枚貝Mytilus tichanovitchi Makiyama--その生層序学的・海洋古気候学的意義の再検討"},{"@language":"ja-Kana","@value":"グンマケン ノ チュウ シントウ シモニタソウ カラ サンシュツ シタ カセキ イガイカ ニマイガイ Mytilus tichanovitchi Makiyama ソノ セイソウ ジョガクテキ カイヨウ コ キコウガクテキ イギ ノ サイケントウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681214147840","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Stratigraphy of the Early Miocene Daijima Formation, Oga Peninsula, NE Japan."},{"@language":"ja","@value":"東北日本男鹿半島，台島層の層序"},{"@language":"ja-Kana","@value":"トウホク ニホン オガ ハントウ ダイシマソウ ノ ソウ ジョ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215003264","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of <i>Geloina</i> (Bivalvia: Corbiculidae) from the Miocene Kadonosawa Formation in the Ninohe area, Iwate Prefecture, northeastern Japan, and its paleobiogeographic significance"},{"@language":"ja","@value":"岩手県二戸地域の中新統門ノ沢層から発見された<i>Geloina</i> (二枚貝綱: シジミガイ科) とその古生物地理学的意義"},{"@value":"岩手県二戸地域の中新統門ノ沢層から発見されたGeloina(二枚貝綱:シジミガイ科)とその古生物地理学的意義"},{"@language":"ja-Kana","@value":"イワテケン ニノヘ チイキ ノ チュウ シントウカド ノ サワソウ カラ ハッケン サレタ Geloina 2マイガイ コウ シジミガイカ ト ソノ コ セイブツ チリガクテキ イギ"},{"@value":"Discovery of Geloina (Bivalvia: Corbiculidae) from the Miocene Kadonosawa Formation in the Ninohe area, Iwate Prefecture, northeastern Japan, and its paleobiogeographic significance"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681215375872","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Discovery of mangrove (<i>Kandelia</i> sp.) pollen from the Miocene Kadonosawa Formation, Ninohe district, Iwate Prefecture, Northeast Japan"},{"@language":"ja","@value":"岩手県二戸地域の門ノ沢層（中部中新統）からマングローブ（メヒルギ属）花粉化石の発見"},{"@language":"ja-Kana","@value":"イワテケン ニノヘ チイキ ノ カドノ サワソウ チュウブ チュウ シントウ カラ マングローブ メヒルギゾク カフン カセキ ノ ハッケン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390290617368250752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Middle Miocene Paleoceanography of the Niigata oil field, northern Japan, based on calcareous nannofossils"},{"@language":"ja","@value":"石灰質ナンノ化石から復元する新潟油田地域の中期中新世古海洋"},{"@language":"ja-Kana","@value":"セッカイシツ ナンノ カセキ カラ フクゲン スル ニイガタ ユデン チイキ ノ チュウキ チュウシンセイ コ 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