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首页> 外文期刊>Applied Microbiology and Biotechnology >Cultivation-independent analysis of archaeal and bacterial communities of the formation water in an Indian coal bed to enhance biotransformation of coal into methane
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Cultivation-independent analysis of archaeal and bacterial communities of the formation water in an Indian coal bed to enhance biotransformation of coal into methane

机译:独立于耕作的印度煤层中地层水古细菌和细菌群落的分析,以增强煤炭向甲烷的生物转化

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Biogenic origin of the significant proportion of coal bed methane has indicated the role of microbial communities in methanogenesis. By using cultivation-independent approach, we have analysed the archaeal and bacterial community present in the formation water of an Indian coal bed at 600–700 m depth to understand their role in methanogenesis. Presence of methanogens in the formation water was inferred by epifluorescence microscopy and PCR amplification of mcrA gene. Archaeal 16S rRNA gene clone library from the formation water metagenome was dominated by methanogens showing similarity to Methanobacterium, Methanothermobacter and Methanolinea whereas the clones of bacterial 16S rRNA gene library were closely related to Azonexus, Azospira, Dechloromonas and Thauera. Thus, microbial community of the formation water consisted of predominantly hydrogenotrophic methanogens and the proteobacteria capable of nitrogen fixation, nitrate reduction and polyaromatic compound degradation. Methanogenic potential of the microbial community present in the formation water was elucidated by the production of methane in the enrichment culture, which contained 16S rRNA gene sequences showing close relatedness to the genus Methanobacterium. Microcosm using formation water as medium as well as a source of inoculum and coal as carbon source produced significant amount of methane which increased considerably by the addition of nitrite. The dominance of Diaphorobacter sp. in nitrite amended microcosm indicated their important role in supporting methanogenesis in the coal bed. This is the first study indicating existence of methanogenic and bacterial community in an Indian coal bed that is capable of in situ biotransformation of coal into methane.
机译:很大比例的煤层气的生物成因表明了微生物群落在甲烷生成中的作用。通过使用与耕种无关的方法,我们分析了印度煤层深度为600-700 m的地层水中存在的古细菌和细菌群落,以了解它们在甲烷生成中的作用。通过表观荧光显微镜和mcrA基因的PCR扩增推断地层水中甲烷菌的存在。来自地层水基因组的古细菌16S rRNA基因克隆文库以产甲烷菌为主,显示出与甲烷杆菌,甲烷杆菌和甲醇的相似性,而细菌16S rRNA基因文库的克隆与Azonexus,Azospira,Dechloromonas和Thauera密切相关。因此,地层水的微生物群落主要由氢营养型产甲烷菌和能够固氮,还原硝酸盐和降解多环芳族化合物的细菌组成。通过富集培养物中甲烷的产生来阐明存在于地层水中的微生物群落的产甲烷潜力,该甲烷含有与甲烷杆菌属密切相关的16S rRNA基因序列。使用地层水作为介质以及接种源和煤作为碳源的缩影产生了大量的甲烷,甲烷的添加量明显增加。泛影杆菌属的优势。在亚硝酸盐中修改的缩影表明其在支持煤层甲烷生成中的重要作用。这是第一项表明印度产煤床中存在甲烷生成和细菌群落的研究,该煤层能够将煤原位生物转化为甲烷。

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