Fig. 1: The temperature sensitivity of forest soil microbial CH4 oxidation across the 84 sites in eastern China.
From: Higher temperature sensitivity of forest soil methane oxidation in colder climates
a Geographic variation in the temperature sensitivity of soil microbial CH4 oxidation. b Distribution of the temperature sensitivity of soil microbial CH4 oxidation (n = 84). Horizontal lines inside the box represent the median. Box limits are the upper and lower quartiles. Whiskers are 1.5 times interquartile range. The temperature sensitivity of forest soil microbial CH4 oxidation was quantified using the partial derivative of the soil microbial CH4 oxidation rate with respect to temperature (parameter a values, see “Methods”).
