ВОЗДЕЙСТВИЕ КЛИМАТИЧЕСКИХ ИЗМЕНЕНИЙ НА РАЗВИТИЕ ГРЯДОВО-МОЧАЖИННОГО БОЛОТНОГО КОМПЛЕКСА В ГОЛОЦЕНЕ

The results of a comprehensive paleoecological study of ridge-hollow bog complex in the southern taiga of Western Siberia on the case of two sections of hollow and ridge are shown. Special attention is paid to the climatic impact on the formation of peat deposits in the Holocene which was manifested in the fact that the ridges were sensitive to the impact in eutrophic and mesotrophic stages, and the hollows were sensitive in oligotrophic stage.