Fig. 3From: Temperature sensitivity of mineral soil carbon decomposition in shrub and graminoid tundra, west GreenlandTemperature sensitivity of cumulative respiration for graminoid and shrub soils from two depths. Data points represent back-transformed means of Q-10 values (±1 back-transformed s.e.) for the low (gray) and high (black) moisture treatments. The black line represents the model predictions for the top ranked model (Table 5)Back to article page