“…At all depths, soil carbon accumulation under PM and PN species is significantly lower than that under QP species, which can be justified by several effects as site preparation (Fonseca et al, 2014;Ferré et al, 2014), management practices (Zhang et al, 2016) and the nature of the litterfall produced by each tree species (Vesterdal et al, 2013;Cools et al, 2014;Zhang et al, 2016;Fonseca and Figueiredo, 2018). These factors may promote the breakdown of soil aggregates, affect soil biological activity and, consequently, the mineralization rate of organic residues in the forest floor and of soil organic matter (Gonçalves et al, 2013;Herrero et al, 2016;Fonseca and Figueiredo, 2018). In general, carbon storage displays a vertical gradient, tending to decrease with increasing mineral soil depth.…”