Temperature responses of carbon mineralization in conifer forest soils from different regional climates incubated under standard laboratory conditions

C-14-labelled straw was mixed with soils collected from seven coniferous fo rests located on a climatic gradient in Western Europe ranging from boreal to Mediterranean conditions. The soils were incubated in the laboratory at 4 degrees, 10 degrees, 16 degrees, 23 degrees and 30 degreesC with constant moisture over 550 days. The temperature coefficient (Q(10)) for straw carb on mineralization decreased with increasing incubation temperatures. This w as a characteristic of all the soils with a difference of two Q(10) units b etween the 4-10 degrees and the 23-30 degreesC temperature ranges. It was a lso found that the magnitude of the temperature response function was relat ed to the period of soil incubation. Initial temperature responses of micro bial communities were different to those shown after a long period of labor atory incubation and may have reflected shifts in microbial species composi tion in response to changes in the temperature regime. The rapid exhaustion of the labile fractions of the decomposing material at higher temperatures could also lead to underestimation of the temperature sensitivity of soils unless estimated for carbon pools of similar qualities. Finally, the therm al optima for the organic soil horizons (Of and Oh) were lower than 30 degr eesC even after 550 days of incubation. It was concluded that these respons es could not be attributed to microbial physiological adaptations, but rath er to the rates at which recalcitrant microbial secondary products were for med at higher temperatures. The implication of these variable temperature r esponses of soil materials is discussed in relation to modelling potential effects of global warming.