Streptognathodus isolatus new species (Conodonta): Proposed index for the Carboniferous-Permian boundary
Davydov et al. (1995) recently proposed the Aidaralash Creek section in northern Kazakhstan (Figures 2 and 3) as the Global Stratotype Section and Point (GSSP) for the base of the Permian System. The proposed boundary is the level in an evolutionary sequence where Streptognathodus wabaunsensis Gunne...
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Veröffentlicht in: | Journal of paleontology 1997-01, Vol.71 (1), p.162-164 |
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creator | Chernykh, Valery V. Ritter, Scott M. Wardlaw, Bruce R. |
description | Davydov et al. (1995) recently proposed the Aidaralash Creek section in northern Kazakhstan (Figures 2 and 3) as the Global Stratotype Section and Point (GSSP) for the base of the Permian System. The proposed boundary is the level in an evolutionary sequence where Streptognathodus wabaunsensis Gunnell gives rise to a descendent with an isolated node field on the inside of the upper platform surface. This morphotype constitutes a new and distinct species for which we propose the name Streptognathodus isolatus new species. |
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(1995) recently proposed the Aidaralash Creek section in northern Kazakhstan (Figures 2 and 3) as the Global Stratotype Section and Point (GSSP) for the base of the Permian System. The proposed boundary is the level in an evolutionary sequence where Streptognathodus wabaunsensis Gunnell gives rise to a descendent with an isolated node field on the inside of the upper platform surface. This morphotype constitutes a new and distinct species for which we propose the name Streptognathodus isolatus new species.</description><identifier>ISSN: 0022-3360</identifier><identifier>EISSN: 1937-2337</identifier><identifier>DOI: 10.1017/S0022336000039068</identifier><language>eng</language><publisher>New York, USA: Cambridge University Press</publisher><subject>Biostratigraphy ; Conodonta ; Geological surveys ; Geology ; Global stratotype section and point ; Marine ; New species ; Paleontological Notes ; Paleontology ; Streptognathodus isolatus</subject><ispartof>Journal of paleontology, 1997-01, Vol.71 (1), p.162-164</ispartof><rights>Copyright © The Paleontological Society</rights><rights>Copyright 1997 The Paleontological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c339t-7370c4d98dd65d38bef068bc2e84a3887ba5b0109d7926471293f817f326e9a83</citedby><cites>FETCH-LOGICAL-c339t-7370c4d98dd65d38bef068bc2e84a3887ba5b0109d7926471293f817f326e9a83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/1306552$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/1306552$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,27901,27902,57992,58225</link.rule.ids></links><search><creatorcontrib>Chernykh, Valery V.</creatorcontrib><creatorcontrib>Ritter, Scott M.</creatorcontrib><creatorcontrib>Wardlaw, Bruce R.</creatorcontrib><title>Streptognathodus isolatus new species (Conodonta): Proposed index for the Carboniferous-Permian boundary</title><title>Journal of paleontology</title><addtitle>J. Paleontol</addtitle><description>Davydov et al. (1995) recently proposed the Aidaralash Creek section in northern Kazakhstan (Figures 2 and 3) as the Global Stratotype Section and Point (GSSP) for the base of the Permian System. The proposed boundary is the level in an evolutionary sequence where Streptognathodus wabaunsensis Gunnell gives rise to a descendent with an isolated node field on the inside of the upper platform surface. This morphotype constitutes a new and distinct species for which we propose the name Streptognathodus isolatus new species.</description><subject>Biostratigraphy</subject><subject>Conodonta</subject><subject>Geological surveys</subject><subject>Geology</subject><subject>Global stratotype section and point</subject><subject>Marine</subject><subject>New species</subject><subject>Paleontological Notes</subject><subject>Paleontology</subject><subject>Streptognathodus isolatus</subject><issn>0022-3360</issn><issn>1937-2337</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1997</creationdate><recordtype>article</recordtype><recordid>eNp9UE1LxDAQDaLguvoDBA85iR6qSbNtGm9S_IIFF1bPJW2mu1napCYp6r83yy54EJzLDPPmPd48hM4puaGE8tslIWnKWE5iMUHy4gBNqGA8iUt-iCZbONnix-jE-w0hNM0pnaD1MjgYgl0ZGdZWjR5rbzsZ4mDgE_sBGg0eX5XWWGVNkNd3eOHsYD0orI2CL9xah8MacCldbY1uwdnRJwtwvZYG13Y0SrrvU3TUys7D2b5P0fvjw1v5nMxfn17K-3nSMCZCwhknzUyJQqk8U6yooY3P1E0KxUyyouC1zGpCiVBcpPmM01SwtqC8ZWkOQhZsii53uoOzHyP4UPXaN9B10kD0VdFMcCZoFg_p7rBx1nsHbTU43UenFSXVNtPqT6aRc7HjbHyw7pfASJ5laYTZXlL2tdNqBdXGjs7Ef_8R_QGEDYLl</recordid><startdate>199701</startdate><enddate>199701</enddate><creator>Chernykh, Valery V.</creator><creator>Ritter, Scott M.</creator><creator>Wardlaw, Bruce R.</creator><general>Cambridge University Press</general><general>Paleontological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H95</scope><scope>L.G</scope></search><sort><creationdate>199701</creationdate><title>Streptognathodus isolatus new species (Conodonta): Proposed index for the Carboniferous-Permian boundary</title><author>Chernykh, Valery V. ; Ritter, Scott M. ; Wardlaw, Bruce R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c339t-7370c4d98dd65d38bef068bc2e84a3887ba5b0109d7926471293f817f326e9a83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1997</creationdate><topic>Biostratigraphy</topic><topic>Conodonta</topic><topic>Geological surveys</topic><topic>Geology</topic><topic>Global stratotype section and point</topic><topic>Marine</topic><topic>New species</topic><topic>Paleontological Notes</topic><topic>Paleontology</topic><topic>Streptognathodus isolatus</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chernykh, Valery V.</creatorcontrib><creatorcontrib>Ritter, Scott M.</creatorcontrib><creatorcontrib>Wardlaw, Bruce R.</creatorcontrib><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 1: Biological Sciences & Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of paleontology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chernykh, Valery V.</au><au>Ritter, Scott M.</au><au>Wardlaw, Bruce R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Streptognathodus isolatus new species (Conodonta): Proposed index for the Carboniferous-Permian boundary</atitle><jtitle>Journal of paleontology</jtitle><addtitle>J. Paleontol</addtitle><date>1997-01</date><risdate>1997</risdate><volume>71</volume><issue>1</issue><spage>162</spage><epage>164</epage><pages>162-164</pages><issn>0022-3360</issn><eissn>1937-2337</eissn><abstract>Davydov et al. (1995) recently proposed the Aidaralash Creek section in northern Kazakhstan (Figures 2 and 3) as the Global Stratotype Section and Point (GSSP) for the base of the Permian System. The proposed boundary is the level in an evolutionary sequence where Streptognathodus wabaunsensis Gunnell gives rise to a descendent with an isolated node field on the inside of the upper platform surface. This morphotype constitutes a new and distinct species for which we propose the name Streptognathodus isolatus new species.</abstract><cop>New York, USA</cop><pub>Cambridge University Press</pub><doi>10.1017/S0022336000039068</doi><tpages>3</tpages></addata></record> |
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subjects | Biostratigraphy Conodonta Geological surveys Geology Global stratotype section and point Marine New species Paleontological Notes Paleontology Streptognathodus isolatus |
title | Streptognathodus isolatus new species (Conodonta): Proposed index for the Carboniferous-Permian boundary |
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