The genesis of the soils having second humus horizon in the North-East of the European part of Russia was considered in the paper. The theory of the relict origin of the second humus horizon in sod-podzolic soils was confirmed on the basis of paleopalynological analysis. Data of paleopalinological study of sod-podzolic soils with complex organic profile are presented. In these soils, the remains of the relict humus horizon, which formed in the warmer Atlantic period of the Holocene under broad-leaved forests, have been preserved. It was revealed that despite the significant degree of destruction of the relict horizon, paleomorphs (pollen and plant spores) were preserved in it, which formed phytocenoses of broad-leaved forests. During the optimal period of the Holocene, the northern boundary of the spread of phytocenoses of coniferous-deciduous forests within the borders of the modern Kirov region of Russia presumably passed north of 58 degrees north latitude. Currently, in the region, broad-leaved forests in natural conditions have been preserved south of 56 degrees north latitude. The results will clarify the species composition of vegetation and the history of landscape development in the Kirov region of Russia in the Holocene.