Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography
Genus Neosinocythere is described from the upper Miocene Itahana Formation in Central Japan, documenting the first record from Japan. The Neosinocythere species were discovered in gravity-flow sediments that were deposited below a depth of 84.9 m with a paleo-summer bottom temperature of 23.7°C and...
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| Veröffentlicht in: | Journal of paleontology 2019-07, Vol.93 (4), p.727-739 |
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| creator | Tanaka, Gengo Moriwaki, Hiroshi |
| description | Genus Neosinocythere is described from the upper Miocene Itahana Formation in Central Japan, documenting the first record from Japan. The Neosinocythere species were discovered in gravity-flow sediments that were deposited below a depth of 84.9 m with a paleo-summer bottom temperature of 23.7°C and a paleo-winter bottom temperature of 14.1°C, based on a modern analog technique using the ostracode assemblage. Paleobiogeographical and paleoenvironmental analyses indicate that Neosinocythere appeared around the southeastern coast of the Eurasian continent, extended distribution in the northern coast of the Eurasian continent before migrating southward along the coast of the Eurasian continent as global temperatures decreased. The high-diversity area shifted from high latitudes to low latitudes. |
| doi_str_mv | 10.1017/jpa.2018.103 |
| format | Article |
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The Neosinocythere species were discovered in gravity-flow sediments that were deposited below a depth of 84.9 m with a paleo-summer bottom temperature of 23.7°C and a paleo-winter bottom temperature of 14.1°C, based on a modern analog technique using the ostracode assemblage. Paleobiogeographical and paleoenvironmental analyses indicate that Neosinocythere appeared around the southeastern coast of the Eurasian continent, extended distribution in the northern coast of the Eurasian continent before migrating southward along the coast of the Eurasian continent as global temperatures decreased. The high-diversity area shifted from high latitudes to low latitudes.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1017/jpa.2018.103</identifier><language>eng</language><publisher>New York, USA: The Paleontological Society</publisher><subject>Analogs ; Arthropoda ; Asia ; assemblages ; biogeography ; Bottom temperature ; Cenozoic ; Conglomerates ; Crustacea ; electron microscopy data ; Far East ; faunal list ; Gangyo River ; Global temperatures ; Gravitation ; Gravity ; Gravity flow ; Gumma Japan ; Honshu ; Itahana Formation ; Japan ; Latitude ; lithostratigraphy ; Mandibulata ; marine environment ; microfossils ; Miocene ; morphology ; Neogene ; Neosinocythere ; New records ; Ostracoda ; Palaeoceanography ; paleo-oceanography ; paleobathymetry ; Paleoceanography ; paleoclimatology ; paleoenvironment ; paleogeography ; Paleontology ; paleotemperature ; Podocopida ; Sediments ; SEM data ; Stratigraphy ; Takasaki Japan ; taxonomy ; Tertiary ; upper Miocene</subject><ispartof>Journal of paleontology, 2019-07, Vol.93 (4), p.727-739</ispartof><rights>Copyright © 2019, The Paleontological Society</rights><rights>GeoRef, Copyright 2020, American Geosciences Institute. 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Abstract, Copyright, The Paleontological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a484t-6d03ffe7dd0da3e22d64e3de57b2ba14c66692ddec9b1e83a195b437f896a5373</citedby><cites>FETCH-LOGICAL-a484t-6d03ffe7dd0da3e22d64e3de57b2ba14c66692ddec9b1e83a195b437f896a5373</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/48572802$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022336018001038/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,314,776,780,799,27903,27904,55606,57995,58228</link.rule.ids></links><search><creatorcontrib>Tanaka, Gengo</creatorcontrib><creatorcontrib>Moriwaki, Hiroshi</creatorcontrib><title>Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>Genus Neosinocythere is described from the upper Miocene Itahana Formation in Central Japan, documenting the first record from Japan. The Neosinocythere species were discovered in gravity-flow sediments that were deposited below a depth of 84.9 m with a paleo-summer bottom temperature of 23.7°C and a paleo-winter bottom temperature of 14.1°C, based on a modern analog technique using the ostracode assemblage. Paleobiogeographical and paleoenvironmental analyses indicate that Neosinocythere appeared around the southeastern coast of the Eurasian continent, extended distribution in the northern coast of the Eurasian continent before migrating southward along the coast of the Eurasian continent as global temperatures decreased. The high-diversity area shifted from high latitudes to low latitudes.</description><subject>Analogs</subject><subject>Arthropoda</subject><subject>Asia</subject><subject>assemblages</subject><subject>biogeography</subject><subject>Bottom temperature</subject><subject>Cenozoic</subject><subject>Conglomerates</subject><subject>Crustacea</subject><subject>electron microscopy data</subject><subject>Far East</subject><subject>faunal list</subject><subject>Gangyo River</subject><subject>Global temperatures</subject><subject>Gravitation</subject><subject>Gravity</subject><subject>Gravity flow</subject><subject>Gumma Japan</subject><subject>Honshu</subject><subject>Itahana Formation</subject><subject>Japan</subject><subject>Latitude</subject><subject>lithostratigraphy</subject><subject>Mandibulata</subject><subject>marine environment</subject><subject>microfossils</subject><subject>Miocene</subject><subject>morphology</subject><subject>Neogene</subject><subject>Neosinocythere</subject><subject>New records</subject><subject>Ostracoda</subject><subject>Palaeoceanography</subject><subject>paleo-oceanography</subject><subject>paleobathymetry</subject><subject>Paleoceanography</subject><subject>paleoclimatology</subject><subject>paleoenvironment</subject><subject>paleogeography</subject><subject>Paleontology</subject><subject>paleotemperature</subject><subject>Podocopida</subject><subject>Sediments</subject><subject>SEM data</subject><subject>Stratigraphy</subject><subject>Takasaki Japan</subject><subject>taxonomy</subject><subject>Tertiary</subject><subject>upper Miocene</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2019</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNp9kM1v1DAQxS1EJZbCjSuSJW7QLP5I7IRbtYJSVNQLPUcTe7J4ldrGTlntf1-vsgIuVLI0mnk_zxs9Qt5wtuaM64-7CGvBeFs6-YyseCd1JaTUz8mKMSEqKRV7QV7mvGOMC8X5iuzvYsREv7tg0CO9zXMCEyxQ5ynQbYLfbj7QcQp7ajGG7OajskFfuIl-gwj-E81u693oDHiDNIw0woRhW16C-PNAwdtlZBD8afiKnI0wZXx9qufk7svnH5uv1c3t1fXm8qaCuq3nSlkmxxG1tcyCRCGsqlFabPQgBuC1UUp1wlo03cCxlcC7ZqilHttOQSO1PCfvlr0xhV8PmOd-Fx6SL5a9kIw1uuuUKtTFQpkUck449jG5e0iHnrP-GG1fou2P0ZZOFvztgu_yHNIftm4bLVomiv5h0UsG2TgssexDmuw_3ox3PVNS66bQ65M53A_J2S3-5f5j_375MLgQPD596yPY0aMl</recordid><startdate>20190701</startdate><enddate>20190701</enddate><creator>Tanaka, Gengo</creator><creator>Moriwaki, Hiroshi</creator><general>The Paleontological Society</general><general>Cambridge University Press</general><general>Paleontological Society</general><general>SEPM Society for Sedimentary Geology</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>4T-</scope><scope>4U-</scope><scope>7SN</scope><scope>7TN</scope><scope>7XB</scope><scope>88A</scope><scope>88I</scope><scope>8AF</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H95</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>LK8</scope><scope>M2O</scope><scope>M2P</scope><scope>M7P</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>R05</scope><scope>S0X</scope></search><sort><creationdate>20190701</creationdate><title>Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography</title><author>Tanaka, Gengo ; Moriwaki, Hiroshi</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a484t-6d03ffe7dd0da3e22d64e3de57b2ba14c66692ddec9b1e83a195b437f896a5373</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2019</creationdate><topic>Analogs</topic><topic>Arthropoda</topic><topic>Asia</topic><topic>assemblages</topic><topic>biogeography</topic><topic>Bottom temperature</topic><topic>Cenozoic</topic><topic>Conglomerates</topic><topic>Crustacea</topic><topic>electron microscopy data</topic><topic>Far East</topic><topic>faunal list</topic><topic>Gangyo River</topic><topic>Global temperatures</topic><topic>Gravitation</topic><topic>Gravity</topic><topic>Gravity flow</topic><topic>Gumma Japan</topic><topic>Honshu</topic><topic>Itahana Formation</topic><topic>Japan</topic><topic>Latitude</topic><topic>lithostratigraphy</topic><topic>Mandibulata</topic><topic>marine environment</topic><topic>microfossils</topic><topic>Miocene</topic><topic>morphology</topic><topic>Neogene</topic><topic>Neosinocythere</topic><topic>New records</topic><topic>Ostracoda</topic><topic>Palaeoceanography</topic><topic>paleo-oceanography</topic><topic>paleobathymetry</topic><topic>Paleoceanography</topic><topic>paleoclimatology</topic><topic>paleoenvironment</topic><topic>paleogeography</topic><topic>Paleontology</topic><topic>paleotemperature</topic><topic>Podocopida</topic><topic>Sediments</topic><topic>SEM data</topic><topic>Stratigraphy</topic><topic>Takasaki Japan</topic><topic>taxonomy</topic><topic>Tertiary</topic><topic>upper Miocene</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Tanaka, Gengo</creatorcontrib><creatorcontrib>Moriwaki, Hiroshi</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Docstoc</collection><collection>University Readers</collection><collection>Ecology Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Biology Database (Alumni Edition)</collection><collection>Science Database (Alumni Edition)</collection><collection>STEM Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>eLibrary</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Biological Science Collection</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Biological Science Database</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>University of Michigan</collection><collection>SIRS Editorial</collection><jtitle>Journal of paleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tanaka, Gengo</au><au>Moriwaki, Hiroshi</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography</atitle><jtitle>Journal of paleontology</jtitle><addtitle>J. Paleontol</addtitle><date>2019-07-01</date><risdate>2019</risdate><volume>93</volume><issue>4</issue><spage>727</spage><epage>739</epage><pages>727-739</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>Genus Neosinocythere is described from the upper Miocene Itahana Formation in Central Japan, documenting the first record from Japan. The Neosinocythere species were discovered in gravity-flow sediments that were deposited below a depth of 84.9 m with a paleo-summer bottom temperature of 23.7°C and a paleo-winter bottom temperature of 14.1°C, based on a modern analog technique using the ostracode assemblage. Paleobiogeographical and paleoenvironmental analyses indicate that Neosinocythere appeared around the southeastern coast of the Eurasian continent, extended distribution in the northern coast of the Eurasian continent before migrating southward along the coast of the Eurasian continent as global temperatures decreased. The high-diversity area shifted from high latitudes to low latitudes.</abstract><cop>New York, USA</cop><pub>The Paleontological Society</pub><doi>10.1017/jpa.2018.103</doi><tpages>13</tpages></addata></record> |
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| subjects | Analogs Arthropoda Asia assemblages biogeography Bottom temperature Cenozoic Conglomerates Crustacea electron microscopy data Far East faunal list Gangyo River Global temperatures Gravitation Gravity Gravity flow Gumma Japan Honshu Itahana Formation Japan Latitude lithostratigraphy Mandibulata marine environment microfossils Miocene morphology Neogene Neosinocythere New records Ostracoda Palaeoceanography paleo-oceanography paleobathymetry Paleoceanography paleoclimatology paleoenvironment paleogeography Paleontology paleotemperature Podocopida Sediments SEM data Stratigraphy Takasaki Japan taxonomy Tertiary upper Miocene |
| title | Upper Miocene Ostracoda in a gravity flow deposit in Central Japan: significance of paleogeography and paleoceanography |
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