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)

dc.date.accessioned	2019-01-22T20:40:15Z
dc.date.available	2019-01-22T20:40:15Z
dc.date.issued	2018
dc.identifier.issn	1028-334X
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/148217
dc.description.abstract	© 2018, Pleiades Publishing, Ltd. 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.
dc.relation.ispartofseries	Doklady Earth Sciences
dc.title	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)
dc.type	Article
dc.relation.ispartofseries-issue	2
dc.relation.ispartofseries-volume	480
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	710
dc.source.id	SCOPUS1028334X-2018-480-2-SID85050142877

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.