湖南嘉禾大窝岭剖面吴家坪阶-长兴阶界线牙形石生物地层及一次碳同位素负偏

叶茜; 江海水

doi:10.3799/dqkx.2016.130

Volume 41 Issue 11

Nov. 2016

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Article Navigation > Earth Science > 2016 > 41(11): 1883-1892

Ye Qian, Jiang Haishui, 2016. Conodont Biostratigraphy and a Negative Excursion in Carbonate Carbon Isotopes across the Wuchiapingian-Changhsingian Boundary at the Dawoling Section, Hunan Province. Earth Science, 41(11): 1883-1892. doi: 10.3799/dqkx.2016.130

Citation:

Ye Qian, Jiang Haishui, 2016. Conodont Biostratigraphy and a Negative Excursion in Carbonate Carbon Isotopes across the Wuchiapingian-Changhsingian Boundary at the Dawoling Section, Hunan Province. Earth Science, 41(11): 1883-1892. doi: 10.3799/dqkx.2016.130

Citation:

Ye Qian, Jiang Haishui, 2016. Conodont Biostratigraphy and a Negative Excursion in Carbonate Carbon Isotopes across the Wuchiapingian-Changhsingian Boundary at the Dawoling Section, Hunan Province. Earth Science, 41(11): 1883-1892. doi: 10.3799/dqkx.2016.130

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Conodont Biostratigraphy and a Negative Excursion in Carbonate Carbon Isotopes across the Wuchiapingian-Changhsingian Boundary at the Dawoling Section, Hunan Province

doi: 10.3799/dqkx.2016.130

Ye Qian^{1,2
,},
Jiang Haishui^{1,2
,
,}

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

Received Date: 2016-03-02
Publish Date: 2016-11-15

Abstract

Abstract

The research of conodont biostratigraphy and carbon isotope change at the Dawoling section provides basic materials for the exploration of creatures and environment change in the Wuchiapingian-Changhsigian period. The Dawoling section at Yuanjia Town, Jiahe county, Hunan Province, recorded basinal deposition during the Late Permian. The Talung Formation is well-exposed and displays siliceous rock, siliceous limestone, limestone and claystone. Three conodont taxa (one is undetermined) of genus Clarkina: C. wangi, C. deflecta and C. sp. are identified, and these enable the tentative assignment of a C. wangi Zone overlain by a C. changxingensis-C. deflecta assemblage Zone. The Wuchiapingian-Changhsingian boundary (Wuchiapingian-Changhsingian boundary, WCB) is placed at the first occurrence (FO) of C. wangi at the base of bed 11 at this Dawoling section. A rapid negative shift from 2.18‰ to -1.39‰ in carbonate carbon isotope in beds 13-15 correlates well with the Changhsingian GSSP(Global Stratotype Section and Point) section at Meishan in Zhejiang and the Shangsi section of Sichuan. Therefore, this negative excursion could be a regionally correlation horizon in south China.
- Wuchiapingian-Changhsingian boundary,
- conodont,
- carbon isotope,
- Dawoling section,
- stratigraphy

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References(40)

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Conodont Biostratigraphy and a Negative Excursion in Carbonate Carbon Isotopes across the Wuchiapingian-Changhsingian Boundary at the Dawoling Section, Hunan Province

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