School of Biotechnology, Banaras Hindu University, Varanasi 221105, India.
Appl Microbiol Biotechnol. 2012 Feb;93(3):1337-50. doi: 10.1007/s00253-011-3778-1. Epub 2011 Dec 28.
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.
生物成因的大量煤层气表明了微生物群落在甲烷生成中的作用。通过使用非培养的方法,我们分析了印度一个深度在 600-700 米的煤层的地层水中存在的古菌和细菌群落,以了解它们在甲烷生成中的作用。通过荧光显微镜和 mcrA 基因的 PCR 扩增推断地层水中存在产甲烷菌。地层水微生物组的古菌 16S rRNA 基因克隆文库主要由产甲烷菌组成,与甲烷杆菌、甲烷八叠球菌和甲烷丝菌相似,而细菌 16S rRNA 基因文库的克隆则与 Azoexus、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烃的变形菌组成。通过在富集培养中产生甲烷,阐明了地层水中微生物群落的产甲烷潜力,该培养物中含有与甲烷杆菌属密切相关的 16S rRNA 基因序列。使用地层水作为培养基以及接种物和煤作为碳源的微宇宙产生了大量的甲烷,添加亚硝酸盐后甲烷产量显著增加。在添加亚硝酸盐的微宇宙中,Diaphorobacter sp. 的优势表明它们在支持煤层中甲烷生成方面的重要作用。这是首次表明印度煤层中存在能够将煤原位转化为甲烷的产甲烷菌和细菌群落的研究。