Zhang Guishan, Tian Jianqing, Jiang Na, Guo Xiaopeng, Wang Yanfen, Dong Xiuzhu
State Key Laboratory of Microbial Resources, Institute of Microbiology, Chinese Academy of Sciences, Beijing 100101, China.
Environ Microbiol. 2008 Jul;10(7):1850-60. doi: 10.1111/j.1462-2920.2008.01606.x. Epub 2008 Mar 28.
Zoige wetland of Tibetan plateau is characterized by being located at a low latitude (33 degrees 56'N, 102 degrees 52'E) region and under the annual temperature around 1 degrees C. Previous studies indicated that Zoige wetland was one of the CH(4) emission centres in Qinghai-Tibetan plateau; in this study, the methanogen community in this low-latitude wetland was analysed based on the homology of 16S rRNA and mcrA genes retrieved from the soil. The results indicated that members of Methanosarcinales and Methanomicrobiales constituted the majority of methanogens, and a novel uncultured methanogen cluster, Zoige cluster I (ZC-I) affiliated to Methanosarcinales, could be dominant. Using quantitative polymerase chain reaction (qPCR) assay, ZC-I methanogens were estimated to be 10(7) cells per gram of soil, accounting for about 30% of the total Archeae. By combining culturable enrichment with qPCR assay, the quantity of ZC-I methanogens in the methanogenic enrichment with acetate, H2/CO(2), methanol or trimethylamine was determined to increase to 10(8) cells ml(-1), but not with formate, which indicated that ZC-I methanogens could use the four methanogenic substrates. The growth rates at 30 degrees C and 15 degrees C were not pronounced different, implying ZC-I to be the cold-adaptive methanogens. The broad substrate spectrum identified the ZC-I methanogens to be a member of Methanosarcinaceae, and could represent a novel sub-branch specifically inhabited in cold ecosystems. Fluorescence in situ hybridization (FISH) images also visualized ZC-I methanogens the sarcina-like aggregate of the spherical cells. The prevalence and flexibility in substrate utilization and growth temperature suggested ZC-I methanogens to be an important player in the methanogenesis of Zoige wetland.
青藏高原若尔盖湿地位于低纬度地区(北纬33°56′,东经102°52′),年平均气温约1℃。以往研究表明,若尔盖湿地是青藏高原甲烷排放中心之一;本研究基于从土壤中提取的16S rRNA和mcrA基因的同源性,对该低纬度湿地的产甲烷菌群落进行了分析。结果表明,甲烷八叠球菌目和甲烷微菌目的成员构成了产甲烷菌的主体,且一个新的未培养产甲烷菌簇——隶属于甲烷八叠球菌目的若尔盖簇I(ZC-I)可能占主导地位。采用定量聚合酶链反应(qPCR)分析,估计ZC-I产甲烷菌为每克土壤10⁷个细胞,约占古菌总数的30%。通过将可培养富集与qPCR分析相结合,确定在以乙酸盐、H₂/CO₂、甲醇或三甲胺为底物的产甲烷富集培养物中,ZC-I产甲烷菌的数量增加到10⁸个细胞/毫升,但以甲酸盐为底物时数量未增加,这表明ZC-I产甲烷菌可以利用这四种产甲烷底物。在30℃和15℃下的生长速率没有明显差异,这意味着ZC-I是适应寒冷的产甲烷菌。广泛的底物谱表明ZC-I产甲烷菌是甲烷八叠球菌科的成员,可能代表了一个专门栖息在寒冷生态系统中的新亚分支。荧光原位杂交(FISH)图像也显示了ZC-I产甲烷菌呈球形细胞的八叠球菌样聚集体。底物利用和生长温度方面的普遍性和灵活性表明ZC-I产甲烷菌是若尔盖湿地甲烷生成中的重要参与者。