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| Keywords | |
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intermediate line of Carboniferous |
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Lujuantun Formation |
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Qijianfang section |
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Bashkirian |
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conodonts |
| Authors | |
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LI Dong-Jin-1 |
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ZHOU Xiao-Dong-1 |
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WANG Guang-Qi-1 |
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CHEN Ming-1 |
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LANG Jia-Bin-2 |
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WANG Cheng-Yuan-3 |
| PubMed | |
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Article by Li, D. J. 1 |
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Article by Zhou, X. D. 1 |
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Article by Wang, G. Q. 1 |
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Article by Chen, M. 1 |
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Article by Lang, J. B. 2 |
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Article by Wang, C. Y. 3 |
Conodonts and their age from Carboniferous Lujuantun Formation of Qijianfang section in Panshi��Jilin Province
LI Dong-Jin-1, ZHOU Xiao-Dong-1, WANG Guang-Qi-1, CHEN Ming-1, LANG Jia-Bin-2, WANG Cheng-Yuan-3
1�� Regional Survey of Geology and Mineral Resources of Jilin Province��Changchun 130022��China; 2�� Research Center of Palaeontology and Stratigraphy��Jilin University��Changchun 130026��China; 3�� Nanjing Institute of Geology and Paleontology��Chinese Academy of Sciences��Nanjing 210008��China
Conodonts are found in two samples collected from the upper part of Qijianfang section in Panshi of central Jilin Province��including Declinognathodus bernesge��D�� inaequalis��D�� noduliferous sensu lato and D�� praenoduliferous�� This fauna clearly indicated that the the sampled strata were the early Bashkirian of Late Carboniferous�� precisely from the upper D�� praenoduliferous zone to lower D�� noduliferous zone�� The intermediate line of Carboniferous was determined in the interval of the Lujuantun Formation in Jilin��