华北寒武系芙蓉统底界附近的碳同位素组成演化特征

左景勋; 朱学剑; 方怀宾; 陈泳霖

doi:10.3799/dqkx.2019.017

Volume 45 Issue 3

Mar. 2020

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Zuo Jingxun, Zhu Xuejian, Fang Huaibin, Chen Yonglin, 2020. Carbon Isotope Trend across the Base of Furongian Series of Cambrian, Northern Henan, North China. Earth Science, 45(3): 728-738. doi: 10.3799/dqkx.2019.017

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Zuo Jingxun, Zhu Xuejian, Fang Huaibin, Chen Yonglin, 2020. Carbon Isotope Trend across the Base of Furongian Series of Cambrian, Northern Henan, North China. Earth Science, 45(3): 728-738. doi: 10.3799/dqkx.2019.017

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Carbon Isotope Trend across the Base of Furongian Series of Cambrian, Northern Henan, North China

doi: 10.3799/dqkx.2019.017

1.
Henan Key Laboratory for Geological Process of Metal Mineralization and Resource Utilization, Henan Institute of Geological Survey, Zhengzhou 450001, China
2.
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology of Chinese Academy of Sciences, Nanjing 210008, China

Received Date: 2018-12-20
Publish Date: 2020-03-15

Abstract

Abstract

In order to define the base of the Drumian Stage and the base of the Paibian Stage of Cambrian in North China, carbon isotope trend is studied on the Shatan section, northern Henan. Data of carbon isotope suggest that three positive excursions and two negative excursions have been examined within the measured stratigraphical interval. Positive carbon isotope excursions occur separately in the lower part and the middle part of the Changhia Formation and in the upper part of the Chaumitien Formation, maximum δ¹³C values of these positive excursions reach to 2.0‰, 1.0‰ and 3.0‰ respectively. Negative δ¹³C excursions occur in the basal and the lower-middle part of the Changhia Formation with the minimum values of -3.4‰ and -1.0‰ respectively. Especially, the remarkable positive excursion examined in the upper part of the Chaumitien Formation commences on the base of the trilobite Chuangia zone, which corresponds to the base of the Paibian Stage in South China and is equivalent to the SPICE excursion detected in the Paibian Stage in USA, Australia, and Kazakhstan. The negative excursion examined in the basal part of the Changhia Formation is equivalent to the DICE excursion. Both the two carbon isotope excursions are not only used as tools for the regional stratigraphical classification and correlation, but also used as key indicators in defining the Drumian Stage and the Paibian Stage in North China. In addition, carbon isotope excursions are interpreted to be associated with global scale sea-level fluctuations, paleoecological environmental changes. Seawater transgression together with enlargement of paleoecological environment played an important role in positive carbon isotope excursions during the Late Miaolingian to the Early Furongian.
- carbon isotope,
- base of Furongian Series,
- Cambrian,
- northern Henan,
- North China Platform,
- stratigraphy

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Carbon Isotope Trend across the Base of Furongian Series of Cambrian, Northern Henan, North China

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