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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Cisuralian-Guadalupian conodont sequence from the Shaiwa section, Ziyun, Guizhou, South China
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Cisuralian-Guadalupian conodont sequence from the Shaiwa section, Ziyun, Guizhou, South China

机译:中国南部贵州紫云Shaiwa断层的Cural-Guadalupian牙形石序列

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摘要

A sequence of successive conodont datums and zones for the Cisuralian and Guadalupian series for the South China region of the Equatorial Warm Water Province is proposed based on the Shaiwa section, Ziyun, Guizhou. The seven conodont zones in ascending order are: Sweetognathus aff. whitei Zone of Artinskian Stage, a set of three new Kungurian zones of Sweetognathus guizhouensis Zone, Sweetognathus subsymmetricus Zone, Mesogondolella nashuiensis Zone; the Mesogondolella idahoensis lamberti Zone of uppermost Kungurian, the Guadalupian zones of Jinogondolella aserrata followed by Jinogondolella postserrata. The base of the Kungurian Stage is tentatively defined by the first occurrence of S. guizhouensis, 174.5 m above the base of the Sidazhai Formation. This suite of conodont datums and zones will help to improve the global correlations of Permian strata of the Kungurian Stage. (C) 2016 Elsevier B.V. All rights reserved.
机译:基于贵州紫云Shaiwa断层,提出了赤道暖水省华南地区的Cusuralian和Guadalupian系列连续牙形体基准面和层序。七个牙形石区域按升序排列是:Sweetognathus aff。 Artinskian阶段的whitei区域,一组由贵州甜蜜新区,甜蜜新亚对称区,nashuiensis的三个新的昆古兰区组成;最上层的昆古里亚山脉中的伊达荷中生拉贝蒂带,奇诺冈多拉阿塞拉塔的瓜达鲁普安带,其次是奇诺冈多拉后塞拉塔。昆古里阶期的基部由西达寨组基部以上174.5 m的贵州链球菌的首次出现初步定义。这套牙形体基准面和地带套件将有助于改善昆古里阶二叠纪地层的整体相关性。 (C)2016 Elsevier B.V.保留所有权利。

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