海平面变化在湖南西部桑植地区栖霞组富有机碳沉积物形成中的作用

韦恒叶; 汪建国; 遇昊; 黄宝华

doi:10.3799/dqkx.2013.027

Volume 38 Issue 2

Mar. 2013

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WEI Heng-ye, WANG Jian-guo, YU Hao, HUANG Bao-hua, 2013. Role of Sea Level Fluctuation on the Formation of Organic-Carbon-Rich Sediments in the Chihsian Formation in Sangzhi Area, Western Hunan Province. Earth Science, 38(2): 266-276. doi: 10.3799/dqkx.2013.027

Citation:

WEI Heng-ye, WANG Jian-guo, YU Hao, HUANG Bao-hua, 2013. Role of Sea Level Fluctuation on the Formation of Organic-Carbon-Rich Sediments in the Chihsian Formation in Sangzhi Area, Western Hunan Province. Earth Science, 38(2): 266-276. doi: 10.3799/dqkx.2013.027

Citation:

WEI Heng-ye, WANG Jian-guo, YU Hao, HUANG Bao-hua, 2013. Role of Sea Level Fluctuation on the Formation of Organic-Carbon-Rich Sediments in the Chihsian Formation in Sangzhi Area, Western Hunan Province. Earth Science, 38(2): 266-276. doi: 10.3799/dqkx.2013.027

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Role of Sea Level Fluctuation on the Formation of Organic-Carbon-Rich Sediments in the Chihsian Formation in Sangzhi Area, Western Hunan Province

doi: 10.3799/dqkx.2013.027

WEI Heng-ye^{1, 2
,},
WANG Jian-guo³,
YU Hao^{3, 4},
HUANG Bao-hua²

1.
State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China
2.
Department of Earth Science, East China Institute of Technology, Nanchang 330013, China
3.
Institute of Geology and Geophysics, Chinese Academy of Science, Beijing 100029, China
4.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 2012-04-15
Publish Date: 2013-03-01

Abstract

Abstract

The Middle Permian Chihsian Formation in Sangzhi area in western Hunan Province shows remarkable cyclicity, where organic matter cycles also occurred. The study of origin of organic matter accumulation in the Chihsian Formation helps understand the role of sea level fluctuation on the formation of organic-carbon-rich sediments. Using a cycle as the study interval, based on the study of pyrite morphology and geochemical parameters, such as TOC, δ³⁴S, DOP and trace elements, we find out that the variation of ocean surface water primary productivity parameters, such as Ba, Ni, Cu and Zn, are consistent with TOC contents, suggesting organic matter accumulation was controlled by primary productivity. The redox condition in bottom water is related to primary productivity. The ultimate origin for the organic matter accumulation should be the high-frequency sea level fluctuation. Rapid sea level rising brought rich nutrients, flourishing surface water biologic productivity. The decomposition of organic matter from dead body demanded more oxygen concentration, resulting in dysoxic-anoxic environment in bottom water.
- primary productivity,
- redox condition,
- Chihsian Formation,
- relative sea level change

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References(71)

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Role of Sea Level Fluctuation on the Formation of Organic-Carbon-Rich Sediments in the Chihsian Formation in Sangzhi Area, Western Hunan Province

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