Almagro et al. (2009) showed, under Mediterranean conditions, different soil CO 2 effluxes between land uses and, within uses, between beneath-and intercanopy sites. These findings have been weakly explained by soil temperature regime or soil water content, suggesting that microbial activity, as with other factors, could play a role in the soil C dynamic.Soil microbial properties are known to exhibit high space-time variability (Cavigelli et al., 2005). Understanding the spatial variability of soil properties and its functions is important in determining soil constraints to plant nutrition and appropriate management of soil resources (Keil et al., 2011).Studies carried out in natural systems showed that trees' distribution affects soil organic matter mineralization (Chatterjee and Jenerette, 2011) and soil microbial community seasonal dynamics (Waldrop et al., 2006). However, the combined effects of long-term management and trees' spatial distribution on C cycling and microbial activity have not been sufficiently investigated so far.