Extended Data Fig. 7: Temperature sensitivity (Q10) estimated on each measurement occasion during the 60-day laboratory incubation for the six sampling sites.
From: Enhanced response of soil respiration to experimental warming upon thermokarst formation
a, Q10 between collapsed and non-collapsed areas at the Shaliuhe site. Samples (n = 30) were collected from three thermo-erosion gullies in 2020. b-f, Q10 between collapsed and non-collapsed areas for the five additional sites. Samples (n = 5) were collected in 2020. SLH, Shaliuhe site; EB, Ebo site; ML, Mole site; RS, Reshui site; HSX, Huashixia site; HH, Huanghe site. Data are presented with mean values ± s.e.m. Significant differences between collapsed and non-collapsed areas were determined based on linear mixed-effects models. †, P < 0.1; *, P < 0.05; **, P < 0.01; ***, P < 0.001. Samples were collected and analyzed in 2020.
