The burrowing activity of the wild boar (Sus scrofa L.) as one of the types of the habitat-modifying activity of terrestrial mammals has been considered. The typical species and the area of the burrowing sites in winter and summer, as well as the dynamics of humus substances are given. The literature indicates that loosening and mixing the upper soil layers cause changes in the chemical characteristics of the soil, disturb vegetation, and reduce evaporation from the soil surface, which leads to a change in the hydrothermal regime of edaphotop and an increase in both the soil climate continentality and the active layer of edaphotop. Soils of different granulometric composition were considered for comparative characteristic: loams and loamy sands in different geographical zones – steppe (the Dnipropetrovsk region, Ukraine) and taiga (wood sorrel spruce forest, Gryazovets district of the Vologda region, Russia). The steppe zone is dominated by blacktop soils, while podzolic soils prevail in the taiga zone. Although the primary characteristics of the soils were different, the tendency of changing the humus substances content in the soils under the wild boars’ burrowing sites had similar qualities. The nature of the humus substances dynamics depends on the decomposition period of organic substances left on the burrowing sites in the form of wild boar’s excreta and plant food residues. Further mineralization of dead plant remains of damaged roots of tree and shrub vegetation resulting from loosening and trophic activity of wild boar occurs on fellings after spruce indigenous forests. Part of the plant remains on the surface of the loosened soil, and the other part in the soil. As a result of the conducted researches the positive functional impact of the wild boar on any types of biogeocenoses due to its burrowing activity was confirmed.
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