“…By inhabiting such disturbed territories, pioneer moss turfs form a new succession with changes in humidity (Shcherbachenko et al, 2015;Rabyk et al, 2017), mineral (Vilmundardóttir et al, 2018) and organic status of the substrate (Karpinets et al, 2016;Kyyak & Baik, 2016;Karpinets et al, 2017). The participation of bryophytes in the revitalization of plant cover of technogenic ecosystems is determined by their high tolerance to drying (Kyyak & Khorkavtsiv, 2015;Kyyak et al, 2017;, their ability to restore soil due to the structuring of its upper horizons (Carter & Arocena, 2000;Aronson & Alexander, 2013;Jackson, 2015), to prevent its erosion (Haig, 2016;Baughman et al, 2017;Stark, 2017), to absorb and retain moisture (Seitz et al, 2017;Batista et al, 2018;Delgado-Baquerizo et al, 2018), thereby reducing surface runoff (Greenwood & Stark, 2014;Zhao et al, 2014;García et al, 2016). Due to its specific properties of metabolism, moss turf has a significant effect on the soil chemical reaction, accelerating the exchange of cations in the biogeochemical cycle, affecting the circulation of organic carbon and nutrients through the release of mineral and organic compounds into soil solutions (Douma et al, 2007;Kyyak & Baik, 2016), synthesis of phenolic substances with a wide spectrum of antimicrobial action, which promotes the development of a substantial litter layer, in which the processes of mineralization are much slower, biogenic elements are accumulated and favourable conditions for the growth of the underground organs of vascu-lar plants are created (Cortina-Segarra et al, 2016;Bueno de Mesquita et al, 2017).…”