Methodological Issues in Pollen Analysis of Pleistocene Deposits in Denisova Cave
Methodological Issues in Pollen Analysis of Pleistocene Deposits
in Denisova Cave
doi:10.17746/1563-0110.2024.52.3.017-029
N.S. Bolikhovskaya1 and M.V. Shunkov2 1Lomonosov Moscow State University, Vorobyevy Gory, Moscow, 119992, Russia 2Institute of Archaeology and Ethnography, Siberian Branch, Russian Academy of Sciences, Pr. Akademika Lavrentieva 17, Novosibirsk, 630090, Russia
Denisova Cave, in the northwestern Altai, is a key Paleolithic complex in North Asia. Pleistocene deposits in the cave contain lithic industries and human fossils documenting the evolution of the cultural traditions of Denisovans in the second half of the Middle and in the Upper Pleistocene. This study addresses methodological issues in paleogeographic interpretation of pollen records relating to Quaternary deposits of cave sites. We present the results of the analysis of recent and subrecent spectra of cave sediments and soil samples taken at sites of characteristic plant communities in natural zones of the Anui River valley near Denisova Cave. Findings from taphonomic study of pollen microremains from loose sediments in the East Chamber of the cave make it possible to obtain a correct climato-stratigraphic and climato-phytocenotic interpretation of pollen spectra from Pleistocene deposits in Denisova Cave.
