Glycerol ether biomarkers and their carbon isotopic compositions in a cold seep carbonate chimney from the Shenhu area, northern South China Sea

• Published in: Chinese science bulletin 2011-06, Vol.56 (16), p.1700-1707
• Main Authors: Ge, Lu, Jiang, ShaoYong, Yang, Tao, Yang, JingHong, Wu, NengYou, Zhang, GuangXue, Liu, Jian
• Format: Article
• Language: English
• Subjects: biomarkers; carbon; Chemistry/Food Science; cold; Earth Sciences; Engineering; glycerol; Humanities and Social Sciences; Life Sciences; lipids; Marine; marine sediments; methane; methane production; multidisciplinary; oxidation; Physics; Science; Science (multidisciplinary); sulfate-reducing bacteria; 中国南海; 冷泉; 南海北部; 烟囱结构; 甘油醚; 生物标志物; 碳同位素组成; 自生碳酸盐
• ISSN: 1001-6538; 1861-9541
• DOI: 10.1007/s11434-011-4486-z

At modem cold seeps, the anaerobic oxidation of methane （AOM） is the dominant pathway for methane consumption in marine sediments. AOM, which is mediated by a consortium of methane oxidizing archaea and sulfate reducing bacteria, is proposed to be responsible for authigenic carbonate formation. A methane-derived carbonate chimney was collected from the Shenhu area, not~hem South China Sea. The membrane lipids and their very low carbon isotopic compositions （-115%o to -104%o） in the Shenhu chimney suggest the presence of an AOM process. Three specific archaeal and bacterial biomarkers were detected, including Ar, DAGE If, and monocyclic MDGD. Their strongly depleted δ13C values （-115‰ to -104‰）, which are lower than those of the normal marine lipids in sediments, reveal biogenic methane as their origin. The carbonate deposits exhibiting a chimney structure indicate that a vigorous methane-rich fluid expulsion may have occurred at the seafloor. We propose that the decomposition of gas hydrates at depth is the likely cause of seepage and cold seep carbonate formation in the Shenhu area.