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    Volume 38 Issue 5
    Sep.  2013
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    Article Contents
    GUAN Hong-xiang, WU Neng-you, MAO Sheng-yi, ZHU Xiao-wei, WU Dai-dai, YANG Sheng-xiong, 2013. Hopanoid Acids and Their Geochemistry Significance Detected in Seep Carbonates from the South China Sea Continental Slope. Earth Science, 38(5): 1014-1022. doi: 10.3799/dqkx.2013.099
    Citation: GUAN Hong-xiang, WU Neng-you, MAO Sheng-yi, ZHU Xiao-wei, WU Dai-dai, YANG Sheng-xiong, 2013. Hopanoid Acids and Their Geochemistry Significance Detected in Seep Carbonates from the South China Sea Continental Slope. Earth Science, 38(5): 1014-1022. doi: 10.3799/dqkx.2013.099

    Hopanoid Acids and Their Geochemistry Significance Detected in Seep Carbonates from the South China Sea Continental Slope

    doi: 10.3799/dqkx.2013.099
    • Received Date: 2012-12-22
    • Publish Date: 2013-09-15
    • The lipid biomarkers of hopanoid acids in cold seep carbonates from the South China Sea continental slope are investigated. In the hopanoid acids, 17β(H), 21β(H)-30-hopanoid acid-17β(H), 21β(H)-33-hopanoid acid are identified with 17β(H), 21β(H)-32-hopanoid acid being the most aboundant. The 17β(H), 21β(H)-32-hopanoic acid depleted in 13C and the δ13C value(-69.8‰) fall close to the range of SRB (sulfate-reducing bacteria)-derived iso-/anteiso-C15:0 (-75.2‰ to -90.0‰) in site1 seep carbonate(TVG3-C2, ANME-2 dominated), suggesting the incorporation of methane-derived carbon. Although they show non-seep isotopic signatures (-30.7‰ to -40.3‰, ANME-1 dominated) in site3 (TVG8-C5) and site2 seep carbonates (TVG13-C3 and TVG14-C2), hopanoids δ13C values fall close to the range of SRB-derived iso-/anteiso-C15:0 (-32.5‰ to -49.8‰). The majority of SRB are not involved in AOM (anaerobic oxidization of methane) possibly because ANME-1 cells often occur as monospecific aggregates.

       

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