晚泥盆世牙形刺及软骨鱼类在西准噶尔塔克台组中的发现及意义

王志宏; 纵瑞文; 龚一鸣; 王成源

doi:10.3799/dqkx.2015.046

Volume 40 Issue 3

Mar. 2015

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Wang Zhihong, Zong Ruiwen, Gong Yiming, Wang Chengyuan, 2015. Late Devonian Conodonts and Chondrichthyes from TaketaiFormation in Western Junggar, NW China. Earth Science, 40(3): 588-596. doi: 10.3799/dqkx.2015.046

Citation:

Wang Zhihong, Zong Ruiwen, Gong Yiming, Wang Chengyuan, 2015. Late Devonian Conodonts and Chondrichthyes from TaketaiFormation in Western Junggar, NW China. Earth Science, 40(3): 588-596. doi: 10.3799/dqkx.2015.046

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Late Devonian Conodonts and Chondrichthyes from TaketaiFormation in Western Junggar, NW China

doi: 10.3799/dqkx.2015.046

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China

Received Date: 2014-07-22
Publish Date: 2015-03-15

Abstract

Abstract

The Devonian Famennian conodont and chondrichthy have been found from the newly established Taketai Formation which previously was assigned to the Early Carboniferous Hebukehe Formation in Halayemen region, western Junggar. Conodont fossils include 3 genera, 6 species and 1 indeterminate species: Icriodus alternatus alternatus, Icriodus cornutus, Icriodus expansus, Icriodus sp.1, Icriodus sp.2, Polygnathus krestovnikovi, Polygnathus procerus, Polygnathus makhlinae, Polygnathus sp.1, Polygnathus sp.2, Polygnathus sp.3, Ancyrognathus sp.. Chondrichthyes include 2 genera: Protacrodus sp. and Phoebodus sp.. It indicates that Taketai Formation belongs to early Famennian of Late Devonian.
- conodont,
- chondrichthy,
- Taketai Formation,
- Late Devonian,
- western Junggar,
- paleoenvironment,
- paleontology

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References(51)

References

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Late Devonian Conodonts and Chondrichthyes from TaketaiFormation in Western Junggar, NW China

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