Reconstructions of palaeoecological and palaeoclimatic conditions of Late Pleistocene and Holocene as inferred from sediments of the Lake Medvedevskoe (Karelian Istmus)
Nazarova, Larisa 
ORCID: https://orcid.org/0000-0003-4145-9689, Subetto, D.A., Syrykh, L. S., Grekov, I. M. and Leontiev, P.A.
;
ORCID: https://orcid.org/0000-0003-4145-9689, Subetto, D.A., Syrykh, L. S., Grekov, I. M. and Leontiev, P.A.
;
Contact
Larisa.Nazarova [ at ] awi.de
Abstract
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.
Item Type
Article
Authors
Nazarova, Larisa ORCID: https://orcid.org/0000-0003-4145-9689, Subetto, D.A., Syrykh, L. S., Grekov, I. M. and Leontiev, P.A.
;
ORCID: https://orcid.org/0000-0003-4145-9689, Subetto, D.A., Syrykh, L. S., Grekov, I. M. and Leontiev, P.A.
;
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Primary Division
Programs
Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > PACES II (2014-2020) > TOPIC 3: The earth system from a polar perspective > WP 3.1: Circumpolar climate variability and global teleconnections at seasonal to orbital time scales
Publication Status
Published
Eprint ID
50778
DOI
10.1134/S1028334X18060144
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Cite as
Nazarova, L.
,
Subetto, D.
,
Syrykh, L. S.
,
Grekov, I. M.
and
Leontiev, P.
(2018):
Reconstructions of palaeoecological and palaeoclimatic conditions of Late Pleistocene and Holocene as inferred from sediments of the Lake Medvedevskoe (Karelian Istmus)
,
Doklady Earth Sciences,
480
(2),
pp. 710-714
.
doi: 10.1134/S1028334X18060144
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