广西乐业地区吴家坪期牙形石的发现及其意义

谢雨荷; 覃斌贤; 江海水; 陈发垚; 颜佳新

doi:10.3799/dqkx.2022.062

Volume 49 Issue 4

Apr. 2024

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Xie Yuhe, Qin Binxian, Jiang Haishui, Chen Fayao, Yan Jiaxin, 2024. Discovery and Significance of Wuchiapingian Conodonts from Leye of Guangxi. Earth Science, 49(4): 1524-1540. doi: 10.3799/dqkx.2022.062

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Xie Yuhe, Qin Binxian, Jiang Haishui, Chen Fayao, Yan Jiaxin, 2024. Discovery and Significance of Wuchiapingian Conodonts from Leye of Guangxi. Earth Science, 49(4): 1524-1540. doi: 10.3799/dqkx.2022.062

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Discovery and Significance of Wuchiapingian Conodonts from Leye of Guangxi

doi: 10.3799/dqkx.2022.062

Xie Yuhe^{1
,
,},
Qin Binxian¹,
Jiang Haishui^{1, 2
,
,
,},
Chen Fayao¹,
Yan Jiaxin^{1, 2}

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-09-24
Available Online: 2024-04-30
Publish Date: 2024-04-25

Abstract

Abstract

Wuchiapingian is a key interval as a fast ecosystem recovery period between two mass extinctions, the End-Guadalupian crisis and the End-Permian mass extinction. Carbonate platforms were widely distributed in the middle of Yangtze platform and the Dian-Qian-Gui area during this interval. Among them, the Leye carbonate platform is one of the typically isolated carbonate platforms within the Nanpanjiang basin. The continuous Wuchiapingian marine carbonate (Heshan Formation) was deposited above the disconformity surface on the top of Guadalupian Maokou Formation. The traditional Middle-Late Permian stratigraphic frame scale in this area mainly relies on the fusulinids biozones, while only a few Wuchiapingian conodonts have been reported. Here, conodonts from the base of Heshan Formation at the Shuabacun Section and the Liuwei Section in the Leye platform have been obtained and studied. Eight conodont species (including one new species) belonging to two genera in total were identified, and they are Clarkina asymmetrica, C. aff. asymmetrica, C. daxianensis, C. dukouensis, C. leveni, Hindeodus julfensis, H. typicalis and Hindeodus praechangxingensis sp. nov.. In ascending order, two conodont zones, the C. asymmetrica Zone and the C. leveni Zone can be identified at the Shuabacun Section. And one conodont zone, the C. asymmetrica Zone is also identified at the Liuwei Section. Based on this, we surmise that the beginning of the early Wuchiapingian carbonate deposition occurs in the C. asymmetrica Zone at Leye carbonate platform, after the global end-Guadalupian regression. It can provide important data for studying the local carbonate platform and basin evolution and also regional stratigraphic correlation.
- conodont,
- Heshan Formation,
- Wuchiapingian,
- Leye platform,
- paleontology,
- stratigraphy

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References(75)

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Discovery and Significance of Wuchiapingian Conodonts from Leye of Guangxi

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