Paleoecology of peatland in the vicinity of the dune massif – Linde tukulan (Central Yakutia)

Authors

  • Pavlova M.R. 1
  • Lytkin V.M. 1
  • Shaposhnikov G.I. 1
  • 1 Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Science, Merzlotnaya Str., 36, Yakutsk, 677010, Russian

DOI:

https://doi.org/10.31951/2658-3518-2024-A-4-516

Keywords:

peatland, tukulan, pollen analysis, radiocarbon dating, Younger Dryas, Holocene

Abstract

Results of investigation of peatland uncovered within an ancient deflationary basin in the south-eastern part of the Linde tukulan (Central Yakutia) are presented. On the basis of lithological, palynological and radiocarbon data, we reconstruction structure of peatland, performed a preliminary reconstruction of the end Late Pleistocene ‒ Holocene landscape and climatic conditions of the peatland and surrounding areas. Three stages of the peatland development were identified: 1) Younger Dryas – Early Holocene, 2) first half of the Holocene, 3) Late Holocene.

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Published

2024-08-26

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Section

Articles