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    Volume 48 Issue 1
    Jan.  2023
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    Ding Jianghui, Sun Jinsheng, Zhang Jinchuan, Yang Xiangtong, Shi Gang, Wang Ruyi, Huang Bo, Li Huili, 2023. Characteristics and Geological Significance of Biomarker for the Upper Permian Dalong Formation Shale in Southern Anhui Province. Earth Science, 48(1): 235-251. doi: 10.3799/dqkx.2022.140
    Citation: Ding Jianghui, Sun Jinsheng, Zhang Jinchuan, Yang Xiangtong, Shi Gang, Wang Ruyi, Huang Bo, Li Huili, 2023. Characteristics and Geological Significance of Biomarker for the Upper Permian Dalong Formation Shale in Southern Anhui Province. Earth Science, 48(1): 235-251. doi: 10.3799/dqkx.2022.140

    Characteristics and Geological Significance of Biomarker for the Upper Permian Dalong Formation Shale in Southern Anhui Province

    doi: 10.3799/dqkx.2022.140
    • Received Date: 2022-01-23
      Available Online: 2023-02-01
    • Publish Date: 2023-01-25
    • In order to elucidate shale characteristics of the Upper Permian Dalong Formation in southern Anhui Province in the Lower Yangtze, a total of 20 shale samples collected from Gangdi-1 Well were analyzed by conducting organic geochemical test, argon ion polishing-scanning electron microscopy (SEM) observation, and mineral composition analysis. Results show that total organic carbon (TOC) content for the Dalong Formation shale in southern Anhui Province is in the range of 1.18%-4.35%. The kerogen type is dominated by type Ⅰ and followed by type Ⅱ1. The vitrinite reflectance (Ro) is between 1.15% and 1.29%, demonstrating that the Dalong Formation shale is in a mature stage of hydrocarbon generation. Moreover, the Dalong Formation shale extracts display a full range of C11-C35 n-alkanes and acyclic isoprenoids. The chromatograms are characterized by a unimodal distribution of n-alkanes with carbon peak in the range of nC18-nC22 and low quantities of long-chain (nC25+) n-alkanes. Furthermore, the steranes are dominated by C27, C28, and C29 sterane homologs of regular steranes, with the following relative distributions: C27≈C29>C28 regular steranes, which belongs to the V-shaped distribution, indicating that the organic matters in Dalong Formation black shale are mainly originated from lower aquatic organisms (e.g., bacteria and algae) and followed by higher plants in a local area. This conclusion is also supported by the variations of the δ13C values of C13-C26 n-alkanes for the target samples being in the range of 3.0‰-5.6‰ offset, which is slightly higher than the corresponding value (1.6‰) of n-alkanes from a single source. In addition, the cross plot of TOC vs. TS as well as the Pr/Ph ratio and the Pr/nC17-Ph/nC18 diagram indicate that Dalong Formation black shale was mainly formed in a marine anoxic-dysoxic environment, which is beneficial to the preservation of organic matter.

       

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