Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei

Zhou Peng; Chen Xiaohong; Wei Kai

doi:10.19509/j.cnki.dzkq.2020.0207

Volume 39 Issue 2

Mar. 2020

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Zhou Peng, Chen Xiaohong, Wei Kai. Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207

Citation:

Zhou Peng, Chen Xiaohong, Wei Kai. Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207

Citation:

Zhou Peng, Chen Xiaohong, Wei Kai. Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei[J]. Bulletin of Geological Science and Technology, 2020, 39(2): 62-73, 93. doi: 10.19509/j.cnki.dzkq.2020.0207

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Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei

doi: 10.19509/j.cnki.dzkq.2020.0207

Received Date: 29 Jun 2019

Abstract

Abstract

The carbon isotope and TOC data of the Ediacaran in the southeastern margin of the Huangling anticline have been obtained by the testing analysis of core samples from the Well EYD5. The carbon isotope curves of the Ediacaran Doushantuo Formation to the Hamajing Member of the Dengying Formation have been established, and 4 negative excursions and 2 positive excursions are recongnized, as well as 1 negative excursion and 1 positive excursions interval in the Hamajing Member of the Dengying Formation. This can be compared with the reported curves from regional sections during this period. In this paper, the carbon isotope markers within the Ediacaran Doushantuo Formation to the Hamajing Member of the Dengying Formation for stratigraphic correlation are summarized, and the TOC variation in the Doushantou Formation has no relationship with carbon isotope anomaly, but the organic-rich shale usually has continuous negative value of delta δ¹³C.
- Huangling anticline,
- Ediacaran,
- carbon isotope,
- organic matter

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References(57)

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Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei

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Carbon isotope characteristics and organic matter development of the Ediacaran in the southeastern margin of the Huangling anticline, western Hubei

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