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与甲烷氧化古菌相关的甲基辅酶M还原酶A(mcrA)基因的鉴定。

Identification of methyl coenzyme M reductase A (mcrA) genes associated with methane-oxidizing archaea.

作者信息

Hallam Steven J, Girguis Peter R, Preston Christina M, Richardson Paul M, DeLong Edward F

机构信息

Monterey Bay Aquarium Research Institute, Moss Landing, California 95039-9644, USA.

出版信息

Appl Environ Microbiol. 2003 Sep;69(9):5483-91. doi: 10.1128/AEM.69.9.5483-5491.2003.

Abstract

Phylogenetic and stable-isotope analyses implicated two methanogen-like archaeal groups, ANME-1 and ANME-2, as key participants in the process of anaerobic methane oxidation. Although nothing is known about anaerobic methane oxidation at the molecular level, the evolutionary relationship between methane-oxidizing archaea (MOA) and methanogenic archaea raises the possibility that MOA have co-opted key elements of the methanogenic pathway, reversing many of its steps to oxidize methane anaerobically. In order to explore this hypothesis, the existence and genomic conservation of methyl coenzyme M reductase (MCR), the enzyme catalyzing the terminal step in methanogenesis, was studied in ANME-1 and ANME-2 archaea isolated from various marine environments. Clone libraries targeting a conserved region of the alpha subunit of MCR (mcrA) were generated and compared from environmental samples, laboratory-incubated microcosms, and fosmid libraries. Four out of five novel mcrA types identified from these sources were associated with ANME-1 or ANME-2 group members. Assignment of mcrA types to specific phylogenetic groups was based on environmental clone recoveries, selective enrichment of specific MOA and mcrA types in a microcosm, phylogenetic congruence between mcrA and small-subunit rRNA tree topologies, and genomic context derived from fosmid sequences. Analysis of the ANME-1 and ANME-2 mcrA sequences suggested the potential for catalytic activity based on conservation of active-site amino acids. These results provide a basis for identifying methanotrophic archaea with mcrA sequences and define a functional genomic link between methanogenic and methanotrophic archaea.

摘要

系统发育分析和稳定同位素分析表明,两个类似产甲烷菌的古菌群体,即ANME-1和ANME-2,是厌氧甲烷氧化过程中的关键参与者。尽管在分子水平上对厌氧甲烷氧化仍一无所知,但甲烷氧化古菌(MOA)与产甲烷古菌之间的进化关系增加了一种可能性,即MOA采用了产甲烷途径的关键元素,逆转了其中许多步骤以厌氧氧化甲烷。为了探究这一假说,在从各种海洋环境中分离出的ANME-1和ANME-2古菌中,研究了催化产甲烷作用最后一步的酶——甲基辅酶M还原酶(MCR)的存在及基因组保守性。针对MCRα亚基(mcrA)保守区域构建了克隆文库,并对环境样本、实验室培养的微观世界以及fosmid文库进行了比较。从这些来源鉴定出的五种新型mcrA类型中,有四种与ANME-1或ANME-2群体成员相关。将mcrA类型分配到特定的系统发育群体是基于环境克隆的回收率、微观世界中特定MOA和mcrA类型的选择性富集、mcrA与小亚基rRNA树形拓扑结构之间的系统发育一致性以及源自fosmid序列的基因组背景。对ANME-1和ANME-2的mcrA序列分析表明,基于活性位点氨基酸的保守性,其具有催化活性的潜力。这些结果为用mcrA序列鉴定甲烷营养型古菌提供了基础,并定义了产甲烷古菌和甲烷营养型古菌之间的功能基因组联系。

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