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Volume 23 Issue 3
Jun 2012
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Article Contents
Dongying Sun, Jinnan Tong, Yanlin Xiong, Li Tian, Hongfu Yin. Conodont Biostratigraphy and Evolution across Permian–Triassic Boundary at Yangou Section, Leping, Jiangxi Province, South China. Journal of Earth Science, 2012, 23(3): 311-325. doi: 10.1007/s12583-012-0255-4
Citation: Dongying Sun, Jinnan Tong, Yanlin Xiong, Li Tian, Hongfu Yin. Conodont Biostratigraphy and Evolution across Permian–Triassic Boundary at Yangou Section, Leping, Jiangxi Province, South China. Journal of Earth Science, 2012, 23(3): 311-325. doi: 10.1007/s12583-012-0255-4

Conodont Biostratigraphy and Evolution across Permian–Triassic Boundary at Yangou Section, Leping, Jiangxi Province, South China

doi: 10.1007/s12583-012-0255-4
Funds:

the National Natural Science Foundation of China 40830212

the National Natural Science Foundation of China 40921062

the China Postdoctoral Science Foundation 20080430147

the Program of Key Laboratory of Biogeology and the Environmental Geology of Ministry of Education, China University of Geosciences BGEG0802

the Science Project of Education Department in Jiangxi Province GJJ10623

More Information
  • Corresponding author: Jinnan Tong, jntong@cug.edu.cn
  • Received Date: 10 Jan 2012
  • Accepted Date: 01 Apr 2012
  • Publish Date: 01 Jun 2012
  • Series of large conodont samples with 20 species and 3 similar species in 3 genera were collected from the Permian-Triassic (P-T) boundary sequence in a shallow carbonate facies at Yangou (沿沟),Leping (乐平) County,Jiangxi (江西) Province,South China. On the basis of the distributions of the identified species,seven conodont zones have been recognized in ascending order as follows,Neogondolella changxingensis zone,Neogondolella yini zone,Hindeodus changxingensis zone,Neogondolella taylorae zone,Hindeodus parvus zone,Isarcicella staeschei zone,and Isarcicella isarcica zone. The successive occurrences of Hindeodus changxingensis,Neogondolella taylorae and Hindeodus parvus serve as proxies for defining the P-T biostratigraphy boundary at the base of Sub-bed 21-4 of Bed 21 in the Yangou Section. Correlations with the Meishan Section are also discussed in terms of conodont biostratigraphy. Three successive conodont faunal assemblages are grouped through the P-T transitional interval to examine the evolution of conodonts across the great transitional event.

     

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