State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, Harbin 150090, China.
State Key Laboratory of Urban Water Resource and Environment, School of Environment, Harbin Institute of Technology, Harbin 150090, China.
Sci Total Environ. 2022 Feb 1;806(Pt 4):151362. doi: 10.1016/j.scitotenv.2021.151362. Epub 2021 Nov 2.
Methane, a potent greenhouse gas of global importance, has traditionally been considered as an end product of microbial methanogenesis of organic matter. Paradoxically, growing evidence has shown that some microbes, such as cyanobacteria, algae, fungi, purple non-sulfur bacteria, and cryptogamic covers, produce methane in oxygen-saturated aquatic and terrestrial ecosystems. The non-methanogenesis process could be an important potential contributor to methane emissions. This systematic review summarizes the knowledge of microorganisms involved in the non-methanogenesis process and the possible mechanisms of methane formation. Cyanobacteria-derived methane production may be attributed to either demethylation of methyl phosphonates or linked to light-driven primary productivity, while algae produce methane by utilizing methylated sulfur compounds as possible carbon precursors. In addition, fungi produce methane by utilizing methionine as a possible carbon precursor, and purple non-sulfur bacteria reduce carbon dioxide to methane by nitrogenase. The microbial methane distribution from the non-methanogenesis processes in aquatic and terrestrial environments and its environmental significance to global methane emissions, possible mechanisms of methane production in each open water, water-to-air methane fluxes, and the impact of climate change on microorganisms are also discussed. Finally, future perspectives are highlighted, such as establishing more in-situ experiments, quantifying methane flux through optimizing empirical models, distinguishing individual methane sources, and investigating nitrogenase-like enzyme systems to improve our understanding of microbial methane emission from the non-methanogenesis process.
甲烷是一种重要的温室气体,传统上被认为是有机质微生物甲烷生成的终产物。但矛盾的是,越来越多的证据表明,一些微生物,如蓝藻、藻类、真菌、紫色非硫细菌和隐生植物,会在含氧饱和的水生和陆地生态系统中产生甲烷。这种非甲烷生成过程可能是甲烷排放的一个重要潜在贡献者。本系统综述总结了参与非甲烷生成过程的微生物的知识,以及甲烷形成的可能机制。蓝藻产生的甲烷可能归因于甲基膦酸盐的去甲基化,或与光驱动的初级生产力有关,而藻类通过利用甲基化硫化合物作为可能的碳前体来产生甲烷。此外,真菌通过利用蛋氨酸作为可能的碳前体来产生甲烷,而紫色非硫细菌通过固氮酶将二氧化碳还原为甲烷。还讨论了水生和陆地环境中非甲烷生成过程中微生物甲烷的分布及其对全球甲烷排放的环境意义、每个开阔水域中甲烷产生的可能机制、水-气甲烷通量以及气候变化对微生物的影响。最后,强调了未来的展望,例如建立更多的原位实验,通过优化经验模型量化甲烷通量,区分单个甲烷源,并研究固氮酶样酶系统,以提高我们对非甲烷生成过程中微生物甲烷排放的理解。