A Potential Global Standard Stratotype-Section and Point of the Moscovian Stage (Carboniferous)
基金项目:

This study was supported by the Ministry of Science and Technology of China (2006FY120300-8), the Chinese Academy of Sciences (KZCX2-YW-122,KZCX2-YW-Q050603), National Natural Science Foundation of China (NSFC), and the CAS/SAFEA International Partnership Program for Creative Research Teams.


A Potential Global Standard Stratotype-Section and Point of the Moscovian Stage (Carboniferous)
Author:
  • WANG Xiangdong

    WANG Xiangdong

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • QI Yuping

    QI Yuping

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • Lance LAMBERT

    Lance LAMBERT

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • WANG Zhihao

    WANG Zhihao

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • WANG Yue

    WANG Yue

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • HU Keyi

    HU Keyi

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • LIN Wei

    LIN Wei

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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  • CHEN Bo

    CHEN Bo

    1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China; 2 Department of Geological Sciences, University of Texas at San Antonio, San Antonio, Texas, 78249-0663, USA
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    摘要:

    Conodonts and fusulinids are the two most widely used biotic groups for subdividing and correlating Bashkirian and Moscovian strata. The definition of the base of the Global Moscovian Stage is undecided because there are many disagreements among existing boundary definition proposals, each of which has disadvantages. Declinognathodus donetzianus is easily recognized but somewhat limited in its paleogeographic distribution. Idiognathoides postsulcatus is slightly more widespread, but it is less easily identified and its occurrences may be diachronous from region to region. Diplognathodus ellesmerensis is easily recognized and even more widespread, but it is usually rare and its ancestry is not adequately known. The Naqing Section of South Guizhou, South China contains diverse conodont evolutionary lineages among different taxa, including Idiognathoides, Idiognathodus, Diplognathodus, Neognathodus, Gondolella and Mesogondolella. There are numerous transitional forms in almost every lineage of the Naqing section, which shows that the prospects for South China to play a critical role in determining the basal Moscovian Stage definition are good.

    Abstract:

    Conodonts and fusulinids are the two most widely used biotic groups for subdividing and correlating Bashkirian and Moscovian strata. The definition of the base of the Global Moscovian Stage is undecided because there are many disagreements among existing boundary definition proposals, each of which has disadvantages. Declinognathodus donetzianus is easily recognized but somewhat limited in its paleogeographic distribution. Idiognathoides postsulcatus is slightly more widespread, but it is less easily identified and its occurrences may be diachronous from region to region. Diplognathodus ellesmerensis is easily recognized and even more widespread, but it is usually rare and its ancestry is not adequately known. The Naqing Section of South Guizhou, South China contains diverse conodont evolutionary lineages among different taxa, including Idiognathoides, Idiognathodus, Diplognathodus, Neognathodus, Gondolella and Mesogondolella. There are numerous transitional forms in almost every lineage of the Naqing section, which shows that the prospects for South China to play a critical role in determining the basal Moscovian Stage definition are good.

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WANG Xiangdong, QI Yuping, Lance LAMBERT, WANG Zhihao, WANG Yue, HU Keyi, LIN Wei, CHEN Bo.2011. A Potential Global Standard Stratotype-Section and Point of the Moscovian Stage (Carboniferous)[J]. ACTA GEOLOGICA SINICA(English edition),(2):366~372

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  • 收稿日期:2010-10-01
  • 最后修改日期:2010-12-30
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