Seep dynamics as revealed by authigenic carbonates from the eastern Qiongdongnan Basin, South China Sea

• Published in: Marine and petroleum geology Vol. 142; p. 105736
• Main Authors: Liu, Yujia, Wei, Jiangong, Li, Yuanyuan, Chang, Jingyi, Miao, Xiaoming, Lu, Hailong
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.08.2022
• Subjects: Authigenic carbonate; Gas hydrate; Methane seepage; MREE enrichment; South China Sea; X-ray computed tomography; Methane seepage; South China Sea; Gas hydrate; MREE enrichment; X-ray computed tomography; Authigenic carbonate
• ISSN: 0264-8172; 1873-4073
• DOI: 10.1016/j.marpetgeo.2022.105736

Methane-related authigenic carbonates play a significant role in the marine carbon cycle and atmospheric CH4 budget. To elucidate the relationship between seeping methane and authigenic carbonate precipitation, we analyze a 72-cm long methane-related carbonate column from the W08 site in the Qiongdongnan Basin, South China Sea. Mineralogical composition, stable carbon and oxygen isotopes, major and trace element contents, and three-dimensional internal structure have been analyzed. Based on the results obtained, four types of carbonate are identified. The first type recorded decreasing content of rare earth elements plus yttrium (REEY) and increasing carbonate porosity. This is attributed to the gradual increase in methane flux intensity, raising the rate of carbonate deposition and thus reducing the time for elemental uptake. The second type of carbonate displays the same δ18O values as the theoretical equilibrium results, the maximum REEY contents, and the densely cemented carbonate structure, indicating a reduction in gas hydrate decomposition. The third type of carbonate formation occurring at the sediment-water interface shows a synchronous and significant enrichment of Mo, V, and Cd contents, suggesting the high hydrogen sulfide flux, which is subject to intensive methane flux and sulfate reduction. The fourth type is the late infill aragonite, which exhibits lower elemental contents compared to early cement due to less exposure to host sediments, while the difference in δ18O and δ13C values is not significant. The compilation of (Tb/Yb)N and Y/Ho ratios of cold-seep carbonates worldwide suggests that the methane flux could alter the space of redox zones (e.g. Fe reduction zone) and thus affect the sink of MREE. X-ray computed tomography (CT) reveals the internal structure of the methane-related carbonate. The continuous pore system probably suggests an intense fluid/gas pressure, and the in situ brecciations imply the carbonate precipitation did not entirely block the methane release to the water column. A better understanding of authigenic carbonates is fundamental to evaluating how carbonates modulate the carbon balance in the methane seeps. •Methane seepage and hydrate growth might have affected cold-seep carbonate formation rate and geochemical characteristics.•The continuous pore system of the carbonate and the in situ brecciations imply an intense fluid/gas pressure.•(Tb/Yb)N versus Y/Ho patterns from cold-seeps worldwide are compiled to discuss the factors affecting MREE enrichment.