J4 ›› 2010, Vol. 40 ›› Issue (3): 603-609.

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Conodonts from the Lujuantun Formation Strata in Panshi Area,Jilin Province

LANG Jia-bin1|WANG Cheng-yuan1,2   

  1. 1.Research Center of Paleontology &|Stratigraphy/Key-Lab for Evolution of Past Life &|Environment in NE Asia, MEOC, Jilin University, Changchun 130026,China;
    2.Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008,China
  • Received:2010-01-14 Online:2010-05-26 Published:2010-05-26

Abstract:

The Lujuantun Formation has been listed as “Lower Carboniferous” since its founding. Some conodonts are found in four samples from the upper part of Lujuantun Formation in Mingcheng，Panshi area, Jilin Province. Among them, Idiognathoides corrugatus, Id. lanei, Id. sinuatus, Id. sulcatus, Idiognathodus sinuosus are representative species of the Early Pennylvanian. Moreover, the fact that both Idiognathodus and Streptognathodus originally appear indicates that the age of the upper part of the Lujuantun Formation approximately corresponds to the middle-late Bashkirian.

Key words: conodont, Lujuantun Formation, Bashkirian, Panshi area, Jilin Province

CLC Number: 

  • P52
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