Methane seepage intensities traced by biomarker patterns in authigenic carbonates from the South Chi

• 作 者: Hongxiang Guan Dong Feng Nengyou Wu Duofu Chen
• 机 构: Key Laboratory of Gas Hydrate, Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences
• 出 处: 2015年“海洋地质、矿山资源与环境”学术研讨会
• 发表日期: 2015年6期
• 关键词: Biomarkers cold seep authigenic carbonate stable isotopes methane seepage intens

　　Authigenic carbonate rocks from an active seep (Site F) located in the South China Sea (SCS)at a water depth of 1120 m were studied using mineralogical and lipid biomarker analyses.Carbonate mineral compositions, in specific samples, were predominantly aragonite, high-Mg calcite (HMC), or a mixture of both.Abundant 13C-depleted lipid biomarkers diagnostic for archaea provide evidence that anaerobic oxidation of methane (AOM), mediated by anaerobic methane oxidizing archaea (ANME) and their bacterial partners, are the major processes leading to formation of the carbonates.High Methane Index, dominance of ANME-2 assemblages and the predominant contribution of AOM-related biomarkers in the aragonitic carbonate point to the strong impact of AOM communities during its precipitation, which is likely caused by high seepage intensities.The relatively low Methane Index and abundant allochthonous input of the HMC carbonate are a result of the weak impact of AOM microbial communities under conditions of low methane seepage.Evidence for this interpretation also comes from relatively higher carbonate content, lesser contribution of allochthonous organic matter and lower pyrite content in the aragonitic carbonate than in the HMC carbonate.High concentrations of 13C-depleted hopanoids were observed in the aragonitic sample which may be a result of the intermittent presence of oxic conditions in an overall anoxic condition, possibly induced by changing seepage intensities.Our data suggests that lipid biomarkers in authigenic carbonate from seep sites can be helpful for improving assessments of the fluid dynamics in such a complex system.