The effect of temperature increase and more specifically its upper and low level correlates on soil microbial biomass, activity and N-cycle variables was studied in a Mediterranean shrubland. Experimental manipulation succeeded in establishing three treatments which, in comparison with the monthly ambient temperature, displayed an increase in mean monthly temperature by 2.1, 4.9 and 7.4 o C respectively. Also the upper limit temperature values (T max ), but not the low limit counterparts (T min ), differed significantly among the three treatments. T max changes seemed to affect directly only the microbial biomass, while it exerted an indirect effect on the majority of the other soil variables. With increased T max the values of the estimated soil microbial variables (microbial biomass and activity) increased, while other soil chemical variables, such as the inorganic forms of N, were found reducing. Organic N was the only variable remaining independent from changing T max at any treatment. The results of this paper indicate that the level of T max increase could be crucial for the structure of the microbial community. A T max increase up to 7 o C induced by climate change could favour the dominance of the soil bacterial populations, while larger increases could be in favour of the fungal populations.