Abstract
Results of the study of Neogene-Quaternary deposits of Sardakh Island (the Lena Delta) are described here. Taxonomic composition and spore-pollen spectra structure analysis indicated that sandstones, which are located in the section bottom have middle-late Miocene age. The middle part of the studied section has a Pliocene - early Pleistocene age. The upper part has a late Pleistocene age. We assume that sediments were deposited in the river environments.
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