Subrecent spore–pollen spectra from the Lower Kolyma River basin and their importance for the reconstruction of the Quaternary paleogeography of the region

Resumo

Spore–pollen spectra of surface samples characterizing different plant associations in the Lower Kolyma River basin are studied. The formation features of the studied spore–pollen spectra are determined, as well as their potential for past vegetation reconstruction, paleogeographic constructions, and stratigraphic correlation of Quaternary deposits in Northeastern Russia.