Figure 5.

Effects of soil temperature on decomposer efficiency. Heterotrophic respiration of SOM, corrected for ¹³C respiration (a); microbial biomass C (b); mass‐specific respiration (c); respired ¹³C label (d); ¹³C label incorporated into microbial biomass (e); and substrate use efficiency (SUE, f). Full triangles represent the values from long‐term warmed soil (means ± SE, n = 3). Open circles represent the values of soil which had experienced the corresponding natural temperature conditions (means ± SE, n = 3). Mineral soil from each subplot was incubated simultaneously at the indicated soil temperatures for 24 h.