Pedogenesis in automorphic landscapes of Bolshezemelskaya tundra

Cryometamorthic (non-gleyic) soils and gleezems (profile-gleyic) of automorphic landscapes of the southeast of Bolshezemelskaya tundra (mezo-micromorphology, analytical indicators) are studied. Structural оrganization properties, cryogenic and pedogenic processes intensity, inherited signs are established. It is shown that the differentiation of soils profiles is caused by peculiarities of Holocene evolution of landscapes.