Environmental changes in last 200 years from results of bottom-sediments analysis of lake Oron (Kodar ridge, Eastern Siberia, Russia)

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Abstract

Records of bottom sediments accumulated in Lake Oron over the last 200 years were analyzed. Chironomidological and palynological examinations of Lake Oron bottom sediments, based on a 10-cm-thick sample from drilling, were conducted. The dynamic climate effect on fauna was studied by examination of Chironomidae larvae from the lake. The lake’s hydrological status and the local and regional landscape and vegetation were also determined. As a result of these environmental studies, the effect of Lake Oron’s nearshore conversion to bog on the process of the lake water’s acidification was assumed, and the approximate dates of the process were defined as beginning in the 1940s.

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About the authors

I. V. Enushchenko

Limnological Institute, Siberian Branch of the Russian Academy of Sciences

Author for correspondence.
Email: deschampsia@yandex.ru
Russian Federation, Irkutsk

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Supplementary files

Supplementary Files
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1. JATS XML
2. Fig. 1. The geographical position of the lake. Oron with the designation of the sampling site of lake BS (core Or-2/13).

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3. Fig. 2. Biostratigraphic data of chironomid taxa established from the remains of larvae buried in layers of 10 cm DO lake. Oron, and their comparison with data on changes in average annual temperatures in the Northern Hemisphere [28].

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4. Fig. 3. Spore-pollen diagram of a layer of 10 cm core before Lake. Oron and their comparison with data on changes in average annual temperatures in the Northern Hemisphere [28].  

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