Conodont Biostratigraphy and Age of the Early Triassic Fish-Bearing-Nodule Levels from Nanjing and Jurong, Jiangsu Province, South China
Fish-bearing nodules are found in Early Triassic marine strata in many regions, including East Greenland, East Spitsbergen, Northwest Madagascar, Canada, Angola, and South China. A new Olenekian (Early Triassic) conodont biostratigraphic study for stratum that contains fish-bearing nodule levels is...
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creator | Liu, Shuang Sun, Zuoyu Ji, Cheng Zhou, Min Jiang, Dayong |
description | Fish-bearing nodules are found in Early Triassic marine strata in many regions, including East Greenland, East Spitsbergen, Northwest Madagascar, Canada, Angola, and South China. A new Olenekian (Early Triassic) conodont biostratigraphic study for stratum that contains fish-bearing nodule levels is conducted based on the Longtan (LT) Section of Nanjing City and the Qingshan (QS) Section of Jurong County, Jiangsu Province, South China. A total of 101 samples were collected at the two sections and three conodont zones were recognized: in ascending order, they are
Scythogondolella
(
Sc.
)
milleri
Zone,
Novispathodus
(
Nv.
)
pingdingshanensis
Zone, and
Triassospathodus
(
Tr.
) aff.
homeri
Zone. The
Scythogondolella milleri
Zone is globally recognized as the uppermost conodont zone of the Smithian and the base of the
Novispathodus pingdingshanensis
Zone was previously suggested as the marker of the Smithian-Spathian boundary in the Yangtze region. The fish-bearing-nodule levels of Nanjing and Jurong are within the conodont
Scythogondolella milleri
Zone, laterally correlated well with the upper part of the
Novispathodus waageni
Zone in Chaohu of Anhui Province that also contains fish-bearing-nodule levels. The conodont biostratigraphic correlation confirms the Early Triassic fish-bearing-nodule levels in the Lower Yangtze region are coeval, with an end-Smithian in age. |
doi_str_mv | 10.1007/s12583-019-1232-y |
format | Article |
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Scythogondolella
(
Sc.
)
milleri
Zone,
Novispathodus
(
Nv.
)
pingdingshanensis
Zone, and
Triassospathodus
(
Tr.
) aff.
homeri
Zone. The
Scythogondolella milleri
Zone is globally recognized as the uppermost conodont zone of the Smithian and the base of the
Novispathodus pingdingshanensis
Zone was previously suggested as the marker of the Smithian-Spathian boundary in the Yangtze region. The fish-bearing-nodule levels of Nanjing and Jurong are within the conodont
Scythogondolella milleri
Zone, laterally correlated well with the upper part of the
Novispathodus waageni
Zone in Chaohu of Anhui Province that also contains fish-bearing-nodule levels. The conodont biostratigraphic correlation confirms the Early Triassic fish-bearing-nodule levels in the Lower Yangtze region are coeval, with an end-Smithian in age.</description><identifier>ISSN: 1674-487X</identifier><identifier>EISSN: 1867-111X</identifier><identifier>DOI: 10.1007/s12583-019-1232-y</identifier><language>eng</language><publisher>Wuhan: China University of Geosciences</publisher><subject>Bearing ; Biogeosciences ; Biostratigraphy ; Earth and Environmental Science ; Earth Sciences ; Fish ; Geochemistry ; Geological time ; Geology ; Geotechnical Engineering & Applied Earth Sciences ; Nodules ; Paleontology ; Triassic</subject><ispartof>Journal of earth science (Wuhan, China), 2020-02, Vol.31 (1), p.9-22</ispartof><rights>China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2019</rights><rights>2019© China University of Geosciences (Wuhan) and Springer-Verlag GmbH Germany, Part of Springer Nature 2019</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c348t-3a6a1442d8bf635c2e50f95b16bbfe5534449c484bde047c15610bda80e79d2f3</citedby><cites>FETCH-LOGICAL-c348t-3a6a1442d8bf635c2e50f95b16bbfe5534449c484bde047c15610bda80e79d2f3</cites><orcidid>0000-0001-5371-5219 ; 0000-0002-7523-2880</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://www.wanfangdata.com.cn/images/PeriodicalImages/dqkx-e/dqkx-e.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s12583-019-1232-y$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s12583-019-1232-y$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27923,27924,41487,42556,51318</link.rule.ids></links><search><creatorcontrib>Liu, Shuang</creatorcontrib><creatorcontrib>Sun, Zuoyu</creatorcontrib><creatorcontrib>Ji, Cheng</creatorcontrib><creatorcontrib>Zhou, Min</creatorcontrib><creatorcontrib>Jiang, Dayong</creatorcontrib><title>Conodont Biostratigraphy and Age of the Early Triassic Fish-Bearing-Nodule Levels from Nanjing and Jurong, Jiangsu Province, South China</title><title>Journal of earth science (Wuhan, China)</title><addtitle>J. Earth Sci</addtitle><description>Fish-bearing nodules are found in Early Triassic marine strata in many regions, including East Greenland, East Spitsbergen, Northwest Madagascar, Canada, Angola, and South China. A new Olenekian (Early Triassic) conodont biostratigraphic study for stratum that contains fish-bearing nodule levels is conducted based on the Longtan (LT) Section of Nanjing City and the Qingshan (QS) Section of Jurong County, Jiangsu Province, South China. A total of 101 samples were collected at the two sections and three conodont zones were recognized: in ascending order, they are
Scythogondolella
(
Sc.
)
milleri
Zone,
Novispathodus
(
Nv.
)
pingdingshanensis
Zone, and
Triassospathodus
(
Tr.
) aff.
homeri
Zone. The
Scythogondolella milleri
Zone is globally recognized as the uppermost conodont zone of the Smithian and the base of the
Novispathodus pingdingshanensis
Zone was previously suggested as the marker of the Smithian-Spathian boundary in the Yangtze region. The fish-bearing-nodule levels of Nanjing and Jurong are within the conodont
Scythogondolella milleri
Zone, laterally correlated well with the upper part of the
Novispathodus waageni
Zone in Chaohu of Anhui Province that also contains fish-bearing-nodule levels. The conodont biostratigraphic correlation confirms the Early Triassic fish-bearing-nodule levels in the Lower Yangtze region are coeval, with an end-Smithian in age.</description><subject>Bearing</subject><subject>Biogeosciences</subject><subject>Biostratigraphy</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Fish</subject><subject>Geochemistry</subject><subject>Geological time</subject><subject>Geology</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Nodules</subject><subject>Paleontology</subject><subject>Triassic</subject><issn>1674-487X</issn><issn>1867-111X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kctKxDAYhYsoKDoP4C7gwo3R3Nq0Sx0cLwyjoIK7kLZJm3FMxqRV-wY-thkruDKbBPKd8_-ckySHGJ1ihPhZwCTNKUS4gJhQAoetZA_nGYcY4-ft-M44gyznz7vJJIQliocSnmO-l3xNnXW1sx24MC50Xnam8XLdDkDaGpw3CjgNulaBS-lXA3j0RoZgKjAzoYUXSnpjG7hwdb9SYK7e1SoA7d0rWEi7jF8_Lre9d7Y5AbdG2ib04N67d2MrdQIeXN-1YNoaKw-SHS1XQU1-7_3kaXb5OL2G87urm-n5HFaU5R2kMpOYMVLnpc5oWhGVIl2kJc7KUqs0pYyxomI5K2uFGK9wmmFU1jJHihc10XQ_OR59P6TVcR-xdL23caKo314-hSKIIBRTJZE8Gsm1d2-9Ct0fSmhKEC9IsaHwSFXeheCVFmtvXqUfBEZi044Y2xGxHbFpRwxRQ0ZNWG_yU_7P-X_RNztTkqI</recordid><startdate>20200201</startdate><enddate>20200201</enddate><creator>Liu, Shuang</creator><creator>Sun, Zuoyu</creator><creator>Ji, Cheng</creator><creator>Zhou, Min</creator><creator>Jiang, Dayong</creator><general>China University of Geosciences</general><general>Springer Nature B.V</general><general>College of Earth Science and Engineering,Shandong University of Science and Technology,Qingdao 266590,China%CAS Key Laboratory of Economic Stratigraphy and Paleogeography,Nanjing Institute of Geology and Paleontology,Center for Excellence in Life and Paleoenvironment,Chinese Academy of Sciences,Nanjing 210008,China%Laboratory of Orogenic Belt and Crustal Evolution,Ministry of Education,Department of Geology and Geological Museum,Peking University,Beijing 100871,China</general><general>Laboratory of Orogenic Belt and Crustal Evolution,Ministry of Education,Department of Geology and Geological Museum,Peking University,Beijing 100871,China</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TN</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>SOI</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope><orcidid>https://orcid.org/0000-0001-5371-5219</orcidid><orcidid>https://orcid.org/0000-0002-7523-2880</orcidid></search><sort><creationdate>20200201</creationdate><title>Conodont Biostratigraphy and Age of the Early Triassic Fish-Bearing-Nodule Levels from Nanjing and Jurong, Jiangsu Province, South China</title><author>Liu, Shuang ; Sun, Zuoyu ; Ji, Cheng ; Zhou, Min ; Jiang, Dayong</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c348t-3a6a1442d8bf635c2e50f95b16bbfe5534449c484bde047c15610bda80e79d2f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Bearing</topic><topic>Biogeosciences</topic><topic>Biostratigraphy</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Fish</topic><topic>Geochemistry</topic><topic>Geological time</topic><topic>Geology</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Nodules</topic><topic>Paleontology</topic><topic>Triassic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Shuang</creatorcontrib><creatorcontrib>Sun, Zuoyu</creatorcontrib><creatorcontrib>Ji, Cheng</creatorcontrib><creatorcontrib>Zhou, Min</creatorcontrib><creatorcontrib>Jiang, Dayong</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Environment Abstracts</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Journal of earth science (Wuhan, China)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Shuang</au><au>Sun, Zuoyu</au><au>Ji, Cheng</au><au>Zhou, Min</au><au>Jiang, Dayong</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Conodont Biostratigraphy and Age of the Early Triassic Fish-Bearing-Nodule Levels from Nanjing and Jurong, Jiangsu Province, South China</atitle><jtitle>Journal of earth science (Wuhan, China)</jtitle><stitle>J. Earth Sci</stitle><date>2020-02-01</date><risdate>2020</risdate><volume>31</volume><issue>1</issue><spage>9</spage><epage>22</epage><pages>9-22</pages><issn>1674-487X</issn><eissn>1867-111X</eissn><abstract>Fish-bearing nodules are found in Early Triassic marine strata in many regions, including East Greenland, East Spitsbergen, Northwest Madagascar, Canada, Angola, and South China. A new Olenekian (Early Triassic) conodont biostratigraphic study for stratum that contains fish-bearing nodule levels is conducted based on the Longtan (LT) Section of Nanjing City and the Qingshan (QS) Section of Jurong County, Jiangsu Province, South China. A total of 101 samples were collected at the two sections and three conodont zones were recognized: in ascending order, they are
Scythogondolella
(
Sc.
)
milleri
Zone,
Novispathodus
(
Nv.
)
pingdingshanensis
Zone, and
Triassospathodus
(
Tr.
) aff.
homeri
Zone. The
Scythogondolella milleri
Zone is globally recognized as the uppermost conodont zone of the Smithian and the base of the
Novispathodus pingdingshanensis
Zone was previously suggested as the marker of the Smithian-Spathian boundary in the Yangtze region. The fish-bearing-nodule levels of Nanjing and Jurong are within the conodont
Scythogondolella milleri
Zone, laterally correlated well with the upper part of the
Novispathodus waageni
Zone in Chaohu of Anhui Province that also contains fish-bearing-nodule levels. The conodont biostratigraphic correlation confirms the Early Triassic fish-bearing-nodule levels in the Lower Yangtze region are coeval, with an end-Smithian in age.</abstract><cop>Wuhan</cop><pub>China University of Geosciences</pub><doi>10.1007/s12583-019-1232-y</doi><tpages>14</tpages><orcidid>https://orcid.org/0000-0001-5371-5219</orcidid><orcidid>https://orcid.org/0000-0002-7523-2880</orcidid></addata></record> |
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language | eng |
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source | Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings |
subjects | Bearing Biogeosciences Biostratigraphy Earth and Environmental Science Earth Sciences Fish Geochemistry Geological time Geology Geotechnical Engineering & Applied Earth Sciences Nodules Paleontology Triassic |
title | Conodont Biostratigraphy and Age of the Early Triassic Fish-Bearing-Nodule Levels from Nanjing and Jurong, Jiangsu Province, South China |
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