20Termite mounds have recently been confirmed to mitigate approximately half of termite 21 methane (CH4) emissions, but the aerobic methane-oxidizing bacteria (methanotrophs) 22 responsible for this consumption have not been resolved. Here we describe the 23 abundance, composition, and kinetics of the methanotroph communities in the mounds 24 of three distinct termite species. We show that methanotrophs are rare members of the 25 termite mound biosphere and have a comparable abundance, but distinct composition, to 26 those of adjoining soil samples. Across all mounds, the most abundant and prevalent 27 particulate methane monooxygenase sequences detected were affiliated with Upland Soil 28Cluster α (USCα), with sequences homologous to Methylocystis and Tropical Upland Soil 29Cluster also detected. The Michaelis-Menten kinetics of CH4 oxidation in mounds were 30 estimated from in situ reaction rates. The apparent CH4 affinities of the communities were 31 in the low micromolar range, which is one to two orders of magnitude higher than those 32 of upland soils, but significantly lower than those measured in soils with a large CH4 33 source such as landfill-cover soils. The rate constant of CH4 oxidation, as well as the 34 porosity of the mound material, were significantly positively correlated with the abundance 35 of methanotroph communities of termite mounds. We conclude that termite-derived CH4 36 emissions have selected for unique methanotroph communities that are kinetically 37 adapted to elevated CH4 concentrations. However, factors other than substrate 38 concentration appear to limit methanotroph abundance and hence these bacteria only 39 partially mitigate termite-derived CH4 emissions. Our results also highlight the 40 predominant role of USCα in an environment with elevated CH4 concentrations and 41 suggest a higher functional diversity within this group than previously recognised. 42 43 5 to 10 cm of the mound. For a subset of the investigated mounds, soil was collected from 132