Institute of Biogeochemistry and Pollutant Dynamics, ETH Zurich, Zurich, Switzerland.
FEMS Microbiol Ecol. 2012 Jul;81(1):52-65. doi: 10.1111/j.1574-6941.2011.01278.x. Epub 2012 Jan 18.
In landfill-cover soils, aerobic methane-oxidizing bacteria (MOB) convert CH(4) to CO(2), mitigating emissions of the greenhouse gas CH(4) to the atmosphere. We investigated overall MOB community structure and assessed spatial differences in MOB diversity, abundance and activity in a Swiss landfill-cover soil. Molecular cloning, terminal restriction-fragment length polymorphism (T-RFLP) and quantitative PCR of pmoA genes were applied to soil collected from 16 locations at three different depths to study MOB community structure, diversity and abundance; MOB activity was measured in the field using gas push-pull tests. The MOB community was highly diverse but dominated by Type Ia MOB, with novel pmoA sequences present. Type II MOB were detected mainly in deeper soil with lower nutrient and higher CH(4) concentrations. Substantial differences in MOB community structure were observed between one high- and one low-activity location. MOB abundance was highly variable across the site [4.0 × 10(4) to 1.1 × 10(7) (g soil dry weight)(-1)]. Potential CH(4) oxidation rates were high [1.8-58.2 mmol CH(4) (L soil air)(-1) day(-1) ] but showed significant lateral variation and were positively correlated with mean CH(4) concentrations (P < 0.01), MOB abundance (P < 0.05) and MOB diversity (weak correlation, P < 0.17). Our findings indicate that Methylosarcina and closely related MOB are key players and that MOB abundance and community structure are driving factors in CH(4) oxidation at this landfill.
在垃圾填埋场覆盖土壤中,好氧甲烷氧化菌(MOB)将 CH(4)转化为 CO(2),从而减少温室气体 CH(4)向大气中的排放。我们研究了瑞士垃圾填埋场覆盖土壤中 MOB 总体群落结构,并评估了 MOB 多样性、丰度和活性的空间差异。通过对土壤中 pmoA 基因的克隆、末端限制性片段长度多态性(T-RFLP)和定量 PCR 分析,研究了土壤中 MOB 群落结构、多样性和丰度;使用气体推拉试验在现场测量 MOB 活性。MOB 群落高度多样,但以 Type Ia MOB 为主,存在新的 pmoA 序列。Type II MOB 主要存在于深层土壤中,其养分较低,CH(4)浓度较高。一个高活性和一个低活性位置之间的 MOB 群落结构存在显著差异。MOB 丰度在整个场地内变化很大[4.0×10(4)至 1.1×10(7)(g 土壤干重)(-1)]。潜在的 CH(4)氧化速率很高[1.8-58.2 mmol CH(4)(L 土壤空气)(-1)天(-1)],但表现出显著的横向变化,与平均 CH(4)浓度(P < 0.01)、MOB 丰度(P < 0.05)和 MOB 多样性(弱相关,P < 0.17)呈正相关。我们的研究结果表明,Methylosarcina 和密切相关的 MOB 是关键的参与者,并且 MOB 丰度和群落结构是该垃圾填埋场 CH(4)氧化的驱动因素。