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Microbial biomass and community structure of a stromatolite from an acid mine drainage system as determined by lipid analysis

机译:脂质分析法测定酸性矿山排水系统中叠层石的微生物量和群落结构

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Lipids were extracted to determine the microbial biomass and community structure of a Fe-rich stromatolite from acid mine drainage (AMD) at the Green Valley coal mine site (GVS) in western Indiana. The distribution of biomarkers correlated well with layers in the laminated stromatolite. Our results show that the biomass of the top layer of the stromatolite was dominated by phototrophic organisms which constituted 83% of the total biomass. Biomass of the lower layers was dominated by prokaryotic microorganisms. The presence of terminal methyl-branched fatty acids and mid methyl-branched fatty acids suggests the presence of Gram-positive and sulfate-reducing bacteria, respectively. Fungi appear to also be an important part of the AMD microbial communities as suggested by sterol profiles and the presence of polyunsaturated fatty acids. Hydroxy fatty acids and C-19 cyclopropane fatty acids were also detected and likely originated from acid-producing, acidophilic, bacteria. The presence of Archaea is indicated by abundant phospholipid ether-linked isoprenoid hydrocarbons (phytane and phytadienes). The AMD Fe-rich stromatolites at GVS thus appear to be formed by interactions of microbial communities composed of all three domains of life; Archaea, Bacteria, and Eukarya. The identification of microeukaryote-dominated stromatolites implicates the prominent role of these organisms in the formation and preservation of these structures. In addition, the production of oxygen through photosynthesis by these organisms in AMD systems may be important for retrodicting the interaction of microbial communities in Precambrian environments in the production of microbially-mediated sedimentary structures and oxygenation of Earth's early atmosphere. (C) 2007 Elsevier B.V. All rights reserved.
机译:从印第安纳州西部绿谷煤矿场(GVS)的酸性矿井排水(AMD)中提取脂质,以确定富含铁的叠层石的微生物生物量和群落结构。生物标志物的分布与叠层叠层石中的层很好地相关。我们的结果表明,叠层石顶层的生物量主要由光养生物组成,占总生物量的83%。下层的生物质以原核微生物为主。末端甲基支链脂肪酸和中间甲基支链脂肪酸的存在分别表明存在革兰氏阳性细菌和硫酸盐还原细菌。固醇谱和多不饱和脂肪酸的存在表明,真菌似乎也是AMD微生物群落的重要组成部分。还检测到羟基脂肪酸和C-19环丙烷脂肪酸,它们很可能起源于产酸的嗜酸细菌。丰富的磷脂醚连接的类异戊二烯烃(植烷和植二烯)表明古细菌的存在。因此,GVS处富含AMD铁的叠层石似乎是由生命的所有三个方面组成的微生物群落相互作用形成的。古细菌,细菌和Eukarya。鉴定微真核生物为主的叠层石暗示了这些生物在这些结构的形成和保存中的重要作用。此外,AMD系统中这些生物通过光合作用产生的氧对于追溯前寒武纪环境中微生物群落在微生物介导的沉积结构产生和地球早期大气氧化中的相互作用可能很重要。 (C)2007 Elsevier B.V.保留所有权利。

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