{"title":"Сonodonts来自南乌拉尔巴什科尔托斯坦Mechetlino剖面的边界Artinskian-Kungurian矿床。第二条。牙形刺的地层分布","authors":"V. Chernykh","doi":"10.24930/1681-9004-2018-18-3-363-381","DOIUrl":null,"url":null,"abstract":"They are represented in the Table X: Neostreptognathodus aff. clinei Behnken, N. clinei Behnken, Sweetognathus nov. sp. 2 , Uralognathus cochleatus Chern. Section Mechetlino is recommended as limitotype of lower boundary (GSSP) of the Kungurian stage of the International stratigraphic scale.","PeriodicalId":32819,"journal":{"name":"Litosfera","volume":"30 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2018-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Сonodonts from the boundary Artinskian-Kungurian deposits of Mechetlino section (Bashkortostan, the South Urals). Article II. Stratigrafic distribution of conodonts\",\"authors\":\"V. Chernykh\",\"doi\":\"10.24930/1681-9004-2018-18-3-363-381\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"They are represented in the Table X: Neostreptognathodus aff. clinei Behnken, N. clinei Behnken, Sweetognathus nov. sp. 2 , Uralognathus cochleatus Chern. Section Mechetlino is recommended as limitotype of lower boundary (GSSP) of the Kungurian stage of the International stratigraphic scale.\",\"PeriodicalId\":32819,\"journal\":{\"name\":\"Litosfera\",\"volume\":\"30 1\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2018-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Litosfera\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.24930/1681-9004-2018-18-3-363-381\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"Earth and Planetary Sciences\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Litosfera","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.24930/1681-9004-2018-18-3-363-381","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"Earth and Planetary Sciences","Score":null,"Total":0}
引用次数: 2
摘要
它们在表X中有代表:Neostreptognathodus af . clininei Behnken, N. clininei Behnken, Sweetognathus nov. sp. 2, Uralognathus cochleatus Chern。建议将Mechetlino剖面作为国际地层尺度Kungurian阶段下边界(GSSP)的极限类型。
Сonodonts from the boundary Artinskian-Kungurian deposits of Mechetlino section (Bashkortostan, the South Urals). Article II. Stratigrafic distribution of conodonts
They are represented in the Table X: Neostreptognathodus aff. clinei Behnken, N. clinei Behnken, Sweetognathus nov. sp. 2 , Uralognathus cochleatus Chern. Section Mechetlino is recommended as limitotype of lower boundary (GSSP) of the Kungurian stage of the International stratigraphic scale.
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