State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China.
Guangdong Key Laboratory of Integrated Agro-environmental Pollution Control and Management, Guangdong Institute of Eco-environmental Science & Technology, Guangzhou 510650, China.
Sci Total Environ. 2019 Apr 20;662:863-872. doi: 10.1016/j.scitotenv.2019.01.307. Epub 2019 Jan 25.
Lake is an important natural source of methane, a potential greenhouse gas, in the atmosphere. Aerobic methanotrophs can consume a notable proportion of the methane produced in lacustrine ecosystems. However, previous studies mainly focused on aerobic methanotrophs in deep and oligotrophic lakes, while little is known about these organisms in shallow and eutrophic lakes. Lake eutrophication leads to more abundant substrates for methanogenesis, and a subsequent higher methane flux. Therefore, the methanotrophs in eutrophic lakes might play a more important role in mediating lacustrine methane emission. In the current study, aerobic methanotrophs in the sediments of two adjacent shallow freshwater lakes at different trophic status (mesotrophic and eutrophic, respectively) were investigated. Abundant methanotrophs and active aerobic methane oxidation were observed in both lakes. While the eutrophic lake harbored a higher abundance of methanotrophs. The result of pmoA-based high-throughput sequencing suggested that methanotrophic communities in the two studied lakes were dominated by unique groups (Type Ib and Type II), dependent on lake and season. But generally, eutrophication might lead to a higher proportion of Type II methanotrophs. The abundance and uniqueness of methanotrophic community could be attributed to lake eutrophication, and were regulated by environmental variables of both sediment and overlying water. This work provides a new insight towards methanotrophs in shallow freshwater lake impacted by eutrophication.
湖泊是大气中甲烷这一潜在温室气体的重要自然来源。好氧甲烷营养菌可以消耗湖泊生态系统中产生的甲烷的很大一部分。然而,以前的研究主要集中在深而贫营养的湖泊中的好氧甲烷营养菌,而对浅水富营养湖泊中的这些生物了解甚少。湖泊富营养化导致更多丰富的产甲烷底物,随后甲烷通量更高。因此,富营养湖泊中的甲烷营养菌可能在调节湖泊甲烷排放方面发挥更重要的作用。在本研究中,调查了两个相邻的不同营养状态(中营养和富营养)浅水淡水湖的沉积物中的好氧甲烷营养菌。在两个湖泊中均观察到丰富的甲烷营养菌和活跃的好氧甲烷氧化作用。而富营养湖中含有更高丰度的甲烷营养菌。基于 pmoA 的高通量测序结果表明,两个研究湖泊中的甲烷营养菌群落主要由独特的菌群(Ib 型和 II 型)主导,依赖于湖泊和季节。但是,一般来说,富营养化可能导致 II 型甲烷营养菌的比例更高。甲烷营养菌群落的丰度和独特性可归因于湖泊富营养化,并受沉积物和上覆水的环境变量调节。这项工作为受富营养化影响的浅水淡水湖中甲烷营养菌提供了新的见解。