Low productivity caused by paludification in some parts of the closed black spruce (Picea mariana (Mill.) B.S.P) dominated boreal forest threatens the provision of ecosystem services, including wood fiber production. The accumulation, over time, of organic matter in paludified soils leads to an anaerobic environment that reduces microbial activity, decelerates decomposition of organic matter, and generates nutrient-poor microsites for regeneration. Consequently, it results in significant impacts on site productivity. Considering its ability to disturb the soil, mechanical site preparation (MSP) is viewed as a potential treatment that can help restore productivity of paludified sites following harvesting. We conducted a field experiment to verify if (1) the availability of microsites conducive to reforestation varies with MSP, microtopography (slope and aspect) and initial OLT conditions; (2) the growth of planted seedlings depends on the intensity of mechanical disturbance of the organic layer, type of microsite, planting density, presence of Ericaceae, and the planting position and depth; (3) there are direct and indirect causal relationships between microsites availability after MSP, OLT, microtopography, planting quality and seedlings growth; and (4) if mechanical site preparation and microsite type exposed affect the Ericaceae cover after planting. Our results confirmed that MSP is effective in establishing conditions that permit a productive regeneration cohort on these paludified sites. To ensure successful establishment of plantations on these sites, it is necessary, however, to distinguish between those that are slightly or moderately paludified from those that are highly paludified, as treatment effectiveness of different MSP types depends on organic layer thickness. Our results also show that preference should be given to some microsite types as clay and mixed-substrate microsites for planting to ensure sufficient availability of water and nutrients for seedlings.(from top to bottom: fibric, mesic, humic) above the mineral soil [5,6]. Consequently, paludified soils have an organic layer thickness that exceeds 40 cm, and in some cases, 100 cm [7].On the Clay Belt of northeastern Canada, the long fire interval permits the accumulation of thick organic layers in this region [8,9] and the relatively cold climate and poorly drained soils [10] leads to an anaerobic soil environment that reduces microbial activity and decomposition of organic matter [8,9,11]. The resulting gradual accumulation of organic matter is often associated with Sphagnum species on the forest floor [12], leading in the long run to nutrient-poor microsites for regeneration [13,14], An abundance of such microsites contributes to reduced growth of trees, both mature and regenerating [15], with significant impact on site productivity.Successful establishment and growth of conifer plantations on paludified sites depends on the type of microsite, the microtopography, the presence of competing species (notably ericaceous shrubs) and the qualit...