Nitrous oxide inhibition of methanogenesis represents an underappreciated greenhouse gas emission feedback

• Published in: The ISME Journal
• Main Authors: Yin, Yongchao, Kara-Murdoch, Fadime, Murdoch, Robert W, Yan, Jun, Chen, Gao, Xie, Yongchao, Sun, Yanchen, Löffler, Frank E
• Other Authors: Dimensions of Biodiversity Program of the US National Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Oxford University Press (OUP) 2024
• Subjects: Ecology, Evolution, Behavior and Systematics; Microbiology; permafrost
• Online Access: http://dx.doi.org/10.1093/ismejo/wrae027; https://academic.oup.com/ismej/advance-article-pdf/doi/10.1093/ismejo/wrae027/56879285/wrae027.pdf; https://academic.oup.com/ismej/article-pdf/18/1/wrae027/57073015/wrae027.pdf

Abstract Methane (CH4) and nitrous oxide (N2O) are major greenhouse gases that are predominantly generated by microbial activities in anoxic environments. N2O inhibition of methanogenesis has been reported, but comprehensive efforts to obtain kinetic information are lacking. Using the model methanogen Methanosarcina barkeri strain Fusaro and digester sludge-derived methanogenic enrichment cultures, we conducted growth yield and kinetic measurements and showed that micromolar concentrations of N2O suppress the growth of methanogens and CH4 production from major methanogenic substrate classes. Acetoclastic methanogenesis, estimated to account for two-thirds of the annual 1 billion metric tons of biogenic CH4, was most sensitive to N2O, with inhibitory constants (KI) in the range of 18–25 μM, followed by hydrogenotrophic (KI, 60–90 μM) and methylotrophic (KI, 110–130 μM) methanogenesis. Dissolved N2O concentrations exceeding these KI values are not uncommon in managed (i.e. fertilized soils and wastewater treatment plants) and unmanaged ecosystems. Future greenhouse gas emissions remain uncertain, particularly from critical zone environments (e.g. thawing permafrost) with large amounts of stored nitrogenous and carbonaceous materials that are experiencing unprecedented warming. Incorporating relevant feedback effects, such as the significant N2O inhibition on methanogenesis, can refine climate models and improve predictive capabilities.