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高盐环境中甲基辅酶 M 还原酶 (mcrA) 基因的系统发育多样性与三甲基胺的产甲烷作用。

Phylogenetic diversity of methyl-coenzyme M reductase (mcrA) gene and methanogenesis from trimethylamine in hypersaline environments.

机构信息

Laboratory of Molecular Microbial Ecology, Northwestern Center for Biological Research (CIBNOR), La Paz, Mexico.

出版信息

Int Microbiol. 2012 Mar;15(1):33-41. doi: 10.2436/20.1501.01.156.

Abstract

Methanogens have been reported in complex microbial communities from hypersaline environments, but little is known about their phylogenetic diversity. In this work, methane concentrations in environmental gas samples were determined while methane production rates were measured in microcosm experiments with competitive and non-competitive substrates. In addition, the phylogenetic diversity of methanogens in microbial mats from two geographical locations was analyzed: the well studied Guerrero Negro hypersaline ecosystem, and a site not previously investigated, namely Laguna San Ignacio, Baja California Sur, Mexico. Methanogenesis in these microbial mats was suspected based on the detection of methane (in the range of 0.00086 to 3.204 %) in environmental gas samples. Microcosm experiments confirmed methane production by the mats and demonstrated that it was promoted only by non-competitive substrates (trimethylamine and methanol), suggesting that methylotrophy is the main characteristic process by which these hypersaline microbial mats produce methane. Phylogenetic analysis of amino acid sequences of the methyl coenzyme-M reductase (mcrA) gene from natural and manipulated samples revealed various methylotrophic methanogens belonging exclusively to the family Methanosarcinaceae. Moderately halophilic microorganisms of the genus Methanohalophilus were predominant (>60 % of mcrA sequences retrieved). Slightly halophilic and marine microorganisms of the genera Methanococcoides and Methanolobus, respectively, were also identified, but in lower abundances.

摘要

已在高盐环境的复杂微生物群落中报道了产甲烷菌,但对其系统发育多样性知之甚少。在这项工作中,通过环境气体样本中甲烷浓度的测定和微宇宙实验中竞争性和非竞争性底物条件下甲烷生成率的测量,研究了产甲烷菌的情况。此外,还分析了来自两个地理位置的微生物垫中产甲烷菌的系统发育多样性:研究充分的下加利福尼亚湾格雷罗内格罗(Guerrero Negro)高盐生态系统,以及一个以前未调查过的地点,即南下加利福尼亚州圣伊格纳西奥湖(Laguna San Ignacio)。基于环境气体样本中甲烷(范围为 0.00086 至 3.204%)的检测,怀疑这些微生物垫中存在产甲烷作用。微宇宙实验证实了微生物垫的甲烷生成,并表明只有非竞争性底物(三甲胺和甲醇)才能促进甲烷生成,这表明甲基营养是这些高盐微生物垫产生甲烷的主要特征过程。来自自然和人工处理样本的甲基辅酶 M 还原酶(mcrA)基因的氨基酸序列的系统发育分析揭示了各种专性甲基营养产甲烷菌,它们仅属于 Methanosarcinaceae 科。属于 Methanohalophilus 属的中度嗜盐微生物占主导地位(回收的 mcrA 序列中>60%)。分别属于 Methanococcoides 和 Methanolobus 属的轻度嗜盐和海洋微生物也被鉴定出来,但丰度较低。

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