The microfacies and sedimentary responses to the mass extinction during the Permian-Triassic transition at Yangou Section, Jiangxi Province, South China

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• 作者：Li Tian (1)
  JinNan Tong (1)
  DongYing Sun (2)
  YanLin Xiong (1)
  ChengGang Wang (3)
  HaiJun Song (1)
  HuYue Song (1)
  YunFei Huang (1)
  
• 关键词：Permian ; Triassic transition ; microfacies ; mass extinction ; sedimentary response ; Yangou ; Jiangxi Province
• 刊名：Science China Earth Sciences
• 出版年：2014
• 出版时间：September 2014
• 年：2014
• 卷：57
• 期：9
• 页码：2195-2207
• 全文大小：2,833 KB
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• 作者单位：Li Tian (1)
  JinNan Tong (1)
  DongYing Sun (2)
  YanLin Xiong (1)
  ChengGang Wang (3)
  HaiJun Song (1)
  HuYue Song (1)
  YunFei Huang (1)
  
  1. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China
  2. Tourism and Land Resources Faculty of Jiujiang University, Jiujiang, 332005, China
  3. Wuhan Center of Geological Survey, China Geological Survey, Wuhan, 430223, China
  
• ISSN：1869-1897

文摘

A Permian-Triassic (P-Tr) boundary section of continuous carbonate facies, which well recorded the biotic and environmental processes through the great P-Tr transition in the shallow non-microbialite carbonate facies, has been studied in Yangou, Leping County, Jiangxi Province. The P-Tr sequence is well correlated with the Meishan section according to the conodont biostratigraphy and the excursion of carbon isotopes. A series of high-resolution thin-sections from the P-Tr boundary carbonate rocks at the Yangou section are studied to explore the interrelation between environmental change and biological evolution during the transitional time. Six microfacies have been identified based upon the observation of the thin-sections under a microscope on the grains and matrix and their interrelation. Combined with the data of fossils and carbon isotopes, Microfacies 4 (MF-4), coated-grain-bearing foraminifer oolitic sparitic limestone, and Microfacies 6 (MF-6), dark shelly micritic limestone, should be the different responses to the two episodes of mass extinction and environmental events that can be correlated throughout South China and even over the world. The oolitic limestone of MF-4 is the first finding from the latest Permian strata in South China and it might be a proxy of an unusual environmental condition of high pCO2, low sulfate concentration and of microbial blooming in the aftermath of the latest Permian mass extinction. The micritic limestone of MF-6 containing rich micro-gastropods and ostracods probably represents the blooming event of disaster taxa in the earliest Triassic environment. The microfacies analysis at the Yangou section can well reveal the episodic process of the biological evolution and environmental change in the shallow non-microbialite carbonate facies throughout the great P-Tr transition, thus the Yangou section becomes an important complement to the Meishan section.