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Tracking Late Holocene climate change and the 1908 Tunguska impact event from lake sediments in Central Siberia

Published online by Cambridge University Press:  13 February 2025

D.Y. Rogozin Open the ORCID record for D.Y. Rogozin [Opens in a new window] ,
L.B. Nazarova ,
N.A. Rudaya ,
L.A. Frolova Open the ORCID record for L.A. Frolova [Opens in a new window] ,
G.N. Bolobanshchikova ,
O.V. Palagushkina Open the ORCID record for O.V. Palagushkina [Opens in a new window] ,
A.V. Darin Open the ORCID record for A.V. Darin [Opens in a new window]  and
A.V. Meydus
D.Y. Rogozin*
Affiliation:
Institute of Biophysics, Siberian Branch of Russian Academy of Sciences, Akademgorodok 50-50, 660036, Krasnoyarsk, Russia Siberian Federal University, 79 Svobodnyi Ave., Krasnoyarsk 660041, Russia
L.B. Nazarova
Affiliation:
Kazan Federal University, 18 Kremlyovskaya str., 420008 Kazan, Russia Alfred Wegener Institute, Helmholtz Center for Polar and Marine Research, Research Unit Potsdam, Telegrafenberg A43, 14473 Potsdam, Germany
N.A. Rudaya
Affiliation:
Institute of Archaeology & Ethnography, Russian Academy of Sciences, Siberian Branch, 17 Lavrentieva Ave., 630090, Novosibirsk, Russia Biological Institute, Tomsk State University, 36 Lenina str., 634050, Tomsk, Russia
L.A. Frolova
Affiliation:
Kazan Federal University, 18 Kremlyovskaya str., 420008 Kazan, Russia Institute of Archaeology & Ethnography, Russian Academy of Sciences, Siberian Branch, 17 Lavrentieva Ave., 630090, Novosibirsk, Russia
G.N. Bolobanshchikova
Affiliation:
Institute of Biophysics, Siberian Branch of Russian Academy of Sciences, Akademgorodok 50-50, 660036, Krasnoyarsk, Russia
O.V. Palagushkina
Affiliation:
Kazan Federal University, 18 Kremlyovskaya str., 420008 Kazan, Russia
A.V. Darin
Affiliation:
Institute of Geology and Mineralogy Siberian Branch of Russian Academy of Sciences, 3 Prospekt Koptyuga, 630090, Novosibirsk, Russia
A.V. Meydus
Affiliation:
Astafiev Krasnoyarsk State Pedagogical University, 89 Ady Lebedevoi, 660049, Krasnoyarsk, Russia
*
Corresponding author: D.Y. Rogozin; Email: [email protected]
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Abstract

We studied a 2200-year-old sediment core from Lake Zapovednoye, a small, deep, freshwater lake near the site of the 1908 Tunguska impact event. Analysis of the sediment core for geochemistry, pollen, chironomids, Cladocera, and diatoms revealed traces of climatic fluctuations during the investigated time period during which a cool climate before 1000 CE was replaced by the Medieval Climatic Optimum, the Little Ice Age, and finally the modern warming. An increased content of terrigenous elements was identified at the depth corresponding to ca. 1908 CE. This layer presumably resulted from erosion of the soil cover after the tree fall caused by the Tunguska impact event (the largest recorded in history). For the first time, the reaction of lake biota to an impact event has been detected. Our study has demonstrated that the taxonomic diversity of hydrobionts (chironomids and cladocerans) significantly declined after the catastrophe, probably due to increased turbidity, and recovered in 6–10 years. The pollen and diatom assemblages, however, demonstrated weaker compositional shifts.

Keywords

Climate changeSiberia1908 Tunguska impact eventXRFpermafrostpollenchironomidsCladoceradiatoms
Type
Research Article
Information
Quaternary Research , First View , pp. 1 - 19
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Copyright © The Author(s), 2025. Published by Cambridge University Press on behalf of Quaternary Research Center

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