Paleoecological reconstruction of water level changes in a cascade of lakes on Lunkulansaari Island (Lake Ladoga) based on the analysis of Cladocera remains in lake sediments

Authors

  • Pastukhova Yu.A. 1
  • Tsyganov A.N. 1 ID
  • Sapelko T.V. 2 ID
  • Mazei N.G. 1
  • Zharov A.A. 3
  • Mazei Yu.A. 1 ID
  • 1 Lomonosov Moscow State University, Leninskie Gory, 1, Moscow, 119991, Russia
    2 Institute of Limnology of the Russian Academy of Sciences – St. Petersburg Federal Research Center of the Russian Academy of Sciences, Sevastyanova, 9, St.Petersburg, 196105, Russia
    3 A.N. Severtsov Institute of Ecology and Evolution, Russian Academy of Sciences, Leninskiy ave. 33, Moscow 119071, Russia

DOI:

https://doi.org/10.31951/2658-3518-2024-A-4-574

Keywords:

Lake Ladoga, island lakes, lake sediments, Cladocera, paleoecological reconstruction

Abstract

In this study we investigate the dynamics of Cladocera subfossil assemblages (taphocoenoses) during the formation of the cascade of three lakes located on the island of Lunkulansaari in the northeastern part of Lake Ladoga in the late Holocene. Since the last regression of Lake Ladoga and the formation of the lake cascade, Cladocera subfossil assemblages began to accumulate in bottom sediments. Their species structure was alternately dominated by species typical for aquatic vegetation in the littoral zone or species that prefer to live in open water. The data obtained allowed to reconstruct changes in lakes’ water levels and clarify the stages of their development, previously revealed on the basis of pollen spectra of aquatic vegetation.

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Published

2024-08-26

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Section

Articles