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)


Дәйексөз келтіру

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Аннотация

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 (14C AMS), new data on the paleoclimate in the Karelian Isthmus, in particular the quantitative reconstruction of the mean July temperature (TJuly, °C) in the Late Pleistocene and Holocene and the evolution of the ecosystem of Medvedevskoe Lake have been obtained.

Авторлар туралы

L. Nazarova

Potsdam University, Institute of Earth and Environmental Science; Kazan Federal University

Хат алмасуға жауапты Автор.
Email: Larisa.nazarova@awi.de
Германия, Potsdam; Kazan, 420008

D. Subetto

Northern Water Problems Institute, Karelian Science Center; Herzen Russian State Pedagogical University

Email: Larisa.nazarova@awi.de
Ресей, Petrozavodsk, Republic of Karelia, 185003; St. Petersburg, 191186

L. Syrykh

Kazan Federal University; Herzen Russian State Pedagogical University

Email: Larisa.nazarova@awi.de
Ресей, Kazan, 420008; St. Petersburg, 191186

I. Grekov

Herzen Russian State Pedagogical University

Email: Larisa.nazarova@awi.de
Ресей, St. Petersburg, 191186

P. Leontev

Herzen Russian State Pedagogical University

Email: Larisa.nazarova@awi.de
Ресей, St. Petersburg, 191186

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© Pleiades Publishing, Ltd., 2018