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Microbial methane emissions from the non-methanogenesis processes: A critical review

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 806, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.151362

Keywords

Non-methanogenesis process; Cyanobacteria; Algae; Fungi; Purple non-sulfur bacteria

Funding

  1. Natural Science Foundation of China [51808167, 51778173, 31870110]
  2. Fundamental Research Funds for the Central Universities [HIT. BRET.2021014]
  3. Fok Ying Tung Education Foundation
  4. State Key Laboratory of Urban Water Resource and Environment, Harbin Institute of Technology [2021TS01]
  5. Heilongjiang Nature Science Foundation [YQ2021E028]
  6. Heilongjiang Touyan Team
  7. Australian Research Council Discovery Project [DP200100933]
  8. Australian Research Council [DP200100933] Funding Source: Australian Research Council

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This study summarizes the microorganisms involved in the non-methanogenesis process and the possible mechanisms of methane production, including cyanobacteria, algae, fungi, and purple non-sulfur bacteria. These microbes produce methane by utilizing different carbon precursors, which is of significant importance to global methane emissions.
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 nonmethanogenesis process. (c) 2021 Elsevier B.V. All rights reserved.

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