Reconstructions of Paleoecological and Paleoclimatic Conditions of the Late Pleistocene and Holocene according to the Results of Chironomid Analysis of Sediments from Medvedevskoe Lake (Karelian Isthmus)

  • The use of chironomids (Diptera: Chironomidae) as indicators of changes in natural and climatic settings allows one to reconstruct paleoclimatic and paleoenvironmental conditions. Based on the results of lithological and chironomid analyses, the loss on ignition (LOI) values, as well as the results of radiocarbon dating (C-14 AMS), new data on the paleoclimate in the Karelian Isthmus, in particular the quantitative reconstruction of the mean July temperature (T (July), A degrees C) in the Late Pleistocene and Holocene and the evolution of the ecosystem of Medvedevskoe Lake have been obtained.

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Author details:Larisa B. NazarovaORCiD, D. A. Subetto, Lydmila S. SyrykhORCiD, I. M. Grekov, P. A. Leontev
DOI:https://doi.org/10.1134/S1028334X18060144
ISSN:1028-334X
ISSN:1531-8354
Title of parent work (English):Doklady Earth Sciences
Publisher:Pleiades Publ.
Place of publishing:New York
Publication type:Article
Language:English
Date of first publication:2018/07/14
Publication year:2018
Release date:2021/11/22
Volume:480
Issue:2
Number of pages:5
First page:710
Last Page:714
Funding institution:Russian Science FoundationRussian Science Foundation (RSF) [16-17-10118]; Russian Foundation for Basic ResearchRussian Foundation for Basic Research (RFBR) [13-05-41457 RGO_a]
Organizational units:Mathematisch-Naturwissenschaftliche Fakultät / Institut für Geowissenschaften
DDC classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
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