“…It has been welldocumented, however, that temperature changes typically have little effect on overall methanotrophic activity in soils, with Q 10 values typically between 1-2 (Börjesson et al, 2004;Crill, et al, 1994;King and Adamsen, 1992;Roslev et al, 1997;Whalen et al, 1990). Such low values are attributed to slow mass transfer of methane (Dunfield, 2007), although occasionally higher Q 10 values are reported in soils that may have higher gas diffusivity (Christophersen, et al, 2000;MacDonald, et al, 1997) or exposed to methane concentrations greater than 10,000 ppmv (De Visscher, et al, 2001). At temperature extremes, however, i.e., <10 ºC and >40 ºC, methane oxidation is significantly limited in forest and landfill cover soil samples Christophersen, et al, 2000;Czepial, et al, 1996;Whalen and Reeburgh, 1996), likely due to inhibition of mesophilic methanotrophs.…”