Diatoms in a sediment core of Lake Raifskoye (Volzhsko-Kamsky Nature Reserve, Republic of Tatarstan): lake development over the past 1200 years

Authors

  • Palagushkina O.V. 1
  • Li H.C. 2
  • Unkovskaya E.N. 3
  • Frolova L.A. 4
  • 1 Kazan (Volga region) Federal University, Kremlevskaya street, 18, Kazan, 420008, Russia
    2 Department of Geosciences, National Taiwan University Taipei, 106, Taiwan, ROC
    3 Volzhsko-Kamsky State Natural Biosphere Reserve, Republic of Tatarstan, Zelenodolsk district, village Sadovy, st. Vekhova, 1, 422537, Russia
    4 Institute of archaeology and ethnography of the Russian Academy of Sciences, Acad. Lavrentiev Avenue 17, Novosibirsk, 630090, Russia

DOI:

https://doi.org/10.31951/2658-3518-2024-A-4-556

Keywords:

bottom sediments, diatoms, Lake Raifskoye, climate change

Abstract

Studies of the diatom assembly in a 130-cm sediment core from Lake Raifskoye reveal 79 taxa of diatoms ranking below the genus of two classes (centric - 14, pennate - 65). 14C, 210Pb and 137Cs dating results show that the sediment core covers a continuous deposition since 1200 cal. yr BP. During the development of the lake, three periods were identified. In the range of 600-1200 years ago unfavourable conditions for the development of diatoms were noted, presumably due to low environmental temperatures. Period from 150-450 years ago reflects good conditions for the development of diatoms and, as a consequence, an increase in the productivity of algal communities in the lake against the backdrop of rising air temperatures. In the third, modern period, the processes of increasing the productivity of algal communities continue, which can also be associated with an increase in air temperature.

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Published

2024-08-26

Issue

Section

Articles