Chen Yin, Dumont Marc G, McNamara Niall P, Chamberlain Paul M, Bodrossy Levente, Stralis-Pavese Nancy, Murrell J Colin
Department of Biological Sciences, University of Warwick, Coventry CV4 7AL, UK.
Environ Microbiol. 2008 Feb;10(2):446-59. doi: 10.1111/j.1462-2920.2007.01466.x. Epub 2007 Dec 17.
The active methanotroph community was investigated for the first time in heather (Calluna)-covered moorlands and Sphagnum/Eriophorum-covered UK peatlands. Direct extraction of mRNA from these soils facilitated detection of expression of methane monooxygenase genes, which revealed that particulate methane monooxygenase and not soluble methane monooxygenase was probably responsible for CH(4) oxidation in situ, because only pmoA transcripts (encoding a subunit of particulate methane monooxygenase) were readily detectable. Differences in methanotroph community structures were observed between the Calluna-covered moorland and Sphagnum/Eriophorum-covered gully habitats. As with many other Sphagnum-covered peatlands, the Sphagnum/Eriophorum-covered gullies were dominated by Methylocystis. Methylocella and Methylocapsa-related species were also present. Methylobacter-related species were found as demonstrated by the use of a pmoA-based diagnostic microarray. In Calluna-covered moorlands, in addition to Methylocella and Methylocystis, a unique group of peat-associated type I methanotrophs (Gammaproteobacteria) and a group of uncultivated type II methanotrophs (Alphaproteobacteria) were also found. The pmoA sequences of the latter were only distantly related to Methylocapsa and also to the RA-14 group of methanotrophs, which are believed to be involved in oxidation of atmospheric concentrations of CH(4). Soil samples were also labelled with (13)CH(4), and subsequent analysis of the (13)C-labelled phospholipid fatty acids (PLFAs) showed that 16:1 omega 7, 18:1 omega 7 and 18:1 omega 9 were the major labelled PLFAs. The presence of (13)C-labelled 18:1 omega 9, which was not a major PLFA of any extant methanotrophs, indicated the presence of novel methanotrophs in this peatland.
首次在石南(帚石楠)覆盖的高沼地和泥炭藓/羊胡子草覆盖的英国泥炭地中对活跃的甲烷氧化菌群落进行了研究。从这些土壤中直接提取mRNA有助于检测甲烷单加氧酶基因的表达,这表明颗粒态甲烷单加氧酶而非可溶性甲烷单加氧酶可能是原位CH₄氧化的原因,因为只有pmoA转录本(编码颗粒态甲烷单加氧酶的一个亚基)易于检测到。在帚石楠覆盖的高沼地和泥炭藓/羊胡子草覆盖的沟壑生境之间观察到了甲烷氧化菌群落结构的差异。与许多其他泥炭藓覆盖的泥炭地一样,泥炭藓/羊胡子草覆盖的沟壑以甲基孢囊菌属为主。甲基小孢菌属和与甲基帽菌属相关的物种也存在。通过使用基于pmoA的诊断微阵列证明发现了与甲基杆菌属相关的物种。在帚石楠覆盖的高沼地中,除了甲基小孢菌属和甲基孢囊菌属外,还发现了一组独特的与泥炭相关的I型甲烷氧化菌(γ-变形菌纲)和一组未培养的II型甲烷氧化菌(α-变形菌纲)。后者的pmoA序列与甲基帽菌属以及据信参与大气浓度CH₄氧化的RA-14甲烷氧化菌群仅具有远缘关系。土壤样品还用¹³CH₄进行了标记,随后对¹³C标记的磷脂脂肪酸(PLFA)的分析表明,16:1 ω7、18:1 ω7和18:1 ω9是主要的标记PLFA。¹³C标记的18:1 ω9的存在(它不是任何现存甲烷氧化菌的主要PLFA)表明该泥炭地存在新的甲烷氧化菌。