Dedysh S N, Panikov N S, Tiedje J M
Institute of Microbiology, Russian Academy of Sciences, Moscow, Russia.
Appl Environ Microbiol. 1998 Mar;64(3):922-9. doi: 10.1128/AEM.64.3.922-929.1998.
Highly enriched methanotrophic communities (> 25 serial transfers) were obtained from acidic ombrotrophic peat bogs from four boreal forest sites. The enrichment strategy involved using media conditions that were associated with the highest rates of methane uptake by the original peat samples, namely, the use of diluted mineral medium of low buffering capacity, moderate incubation temperature (20 degrees C), and pH values of 3 to 6. Enriched communities contained a mixture of rod-shaped bacteria arranged in aggregates with a minor contribution of Hyphomicrobium-like cells. The growth stoichiometry of isolates was characteristic of methanotrophic bacteria (CH4/O2/CO2 = 1:1.1:0.59), with an average apparent yield of 0.41 +/- 0.03 g of biomass C/g of CH4-C. DNA from each enrichment yielded a PCR product of the expected size with primers for both mmoX and mmoY genes of soluble methane monooxygenase. Two types of sequences were obtained for PCR-amplified fragments of mmoX. One of them exhibited high identity to the mmoX protein of the Methylocystis-Methylosinus group, whereas the other showed an equal level of divergence from both the Methylosinus-Methylocystis group and Methylococcus capsulatus (Bath) and formed a distinct branch. The pH optimum for growth and for CH4 uptake was 4.5 to 5.5, which is very similar to that for the optimum CH4 uptake observed in the original peat samples. These methanotrophs are moderate acidophiles rather than acidotolerant organisms, since their growth rate and methane uptake were much lower at neutral pH. The growth of the methanotrophic community was enhanced by using media with a very low salt content (20 to 200 mg/liter), more typical of their natural environment. All four enriched communities grew on N-free medium.
从四个北方森林站点的酸性雨养泥炭沼泽中获得了高度富集的甲烷营养群落(>25次连续传代)。富集策略包括使用与原始泥炭样品甲烷吸收速率最高相关的培养基条件,即使用低缓冲能力的稀释矿物培养基、适中的培养温度(20摄氏度)和pH值为3至6。富集的群落包含聚集排列的杆状细菌混合物,以及少量类生丝微菌细胞。分离株的生长化学计量是甲烷营养细菌的特征(CH4/O2/CO2 = 1:1.1:0.59),平均表观产量为0.41±0.03克生物量碳/克CH4-C。每个富集物的DNA用可溶性甲烷单加氧酶的mmoX和mmoY基因引物产生了预期大小的PCR产物。mmoX的PCR扩增片段获得了两种类型的序列。其中一种与甲基孢囊菌-甲基弯曲菌属的mmoX蛋白具有高度同一性,而另一种与甲基弯曲菌属-甲基孢囊菌属以及荚膜甲基球菌(巴斯)的差异水平相同,并形成了一个独特的分支。生长和CH4吸收的最适pH为4.5至5.5,这与在原始泥炭样品中观察到的CH4吸收最适值非常相似。这些甲烷营养菌是中度嗜酸菌而非耐酸菌,因为它们在中性pH下的生长速率和甲烷吸收要低得多。使用盐含量非常低(20至200毫克/升)的培养基可增强甲烷营养群落的生长,这更符合它们的自然环境。所有四个富集群落都能在无氮培养基上生长。