Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Nadezhda Lavrova"'
Autor:
Olga Druzhinina, Anna Rudinskaya, Ksenia Filippova, Lyudmila Lazukova, Nadezhda Lavrova, Anton Zharov, Ivan Skhodnov, Aleksey Burko, Kasper van den Berghe
Publikováno v:
Biology, Vol 12, Iss 6, p 821 (2023)
This paper presents the results of a study on the Kulikovo section (south-eastern Baltic Sea coast), a sediment sequence exposing deposits of a post-glacial basin that existed along the edge of the glacier in the Late Pleistocene. The research was ta
Externí odkaz:
https://doaj.org/article/bc0f526ad6294d7b8ecd6a770e7be4bb
Autor:
Lyudmila Filimonova, Nadezhda Lavrova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 10, Pp 86-100 (2017)
The authors own and literary data on long-term paleogeographical research of Lake Onego and its drainage basin carried out using a set of methods are summarized in the article. The deglaciation, transgressive-regressive activity of Lake Onego, time a
Externí odkaz:
https://doaj.org/article/00c51f2f66554c6abb31db79cb0573cf
Autor:
Tatyana Shelekhova, Nadezhda Lavrova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 3 (2019)
The results of an integrated study of Late Glacial and Holocene lake-mire deposits on Andoma Ice-divide Upland, located in the Fennoscandian Crystalline Shield-Russian Plate contact zone, are reported. The geomorphological structure of the study area
Externí odkaz:
https://doaj.org/article/237a498e744249b69b58f7dc6469c3f9
Autor:
Nadezhda Lavrova, Lyudmila Filimonova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 10 (2018)
The paper summarizes the results of pollen and macrofossil studies of late glacial deposits in Karelia, encompassing the Older Dryas, Allerod, and Younger Dryas – 12350–10300 14С yrs BP (14100–11900 cal. yrs BP). Specific features of the compo
Externí odkaz:
https://doaj.org/article/0311b18612c04f83872144f0734cf14b
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 5, Pp 70-85 (2015)
New lithological, palinological and chronological data obtained through the study of bottom sediments from four small lake depressions on the Pomor Coast, Onega Bay, White Sea are presented. The integrated study of bottom sediments from lakes lying a
Externí odkaz:
https://doaj.org/article/1da79f3339db4b9b986fe0301e038569
Autor:
Lyudmila Filimonova, Nadezhda Lavrova
Publikováno v:
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, Iss 4, Pp 30-47 (2015)
The paper summarizes the results of long-term paleogeographical research of the Zaonezhye Peninsula conducted by the staff of the Institute of Biology and Institute of Geology of the Karelian Research Centre RAS, including the authors of the article.
Externí odkaz:
https://doaj.org/article/5b37f0ff845e4a738c332c55eae28e0d
Autor:
Berghe, Olga Druzhinina, Anna Rudinskaya, Ksenia Filippova, Lyudmila Lazukova, Nadezhda Lavrova, Anton Zharov, Ivan Skhodnov, Aleksey Burko, Kasper van den
Publikováno v:
Biology; Volume 12; Issue 6; Pages: 821
This paper presents the results of a study on the Kulikovo section (south-eastern Baltic Sea coast), a sediment sequence exposing deposits of a post-glacial basin that existed along the edge of the glacier in the Late Pleistocene. The research was ta
Autor:
Tatiana Shelekhova, Nadezhda Lavrova
Publikováno v:
Baltica. 32:190-201
Karelia, like the entire Fennoscandian Shield, is a region with a low seismic activity. An example of the best-studied locality is a paleoseismic dislocation on Mount Vottovaara, which bears traces of disastrous Holocene geological events following t
Publikováno v:
Doklady Earth Sciences. 485:312-316
This paper reports on the lithological, micropaleontological, and chronometric data (radiocarbon dating) for one of the areas of the White Sea coast. The sedimentary sequences were studied in the current lake basins, which were separated from the lar
Publikováno v:
Vestnik of Institute of Geology of Komi Science Center of Ural Branch RAS. 5:33-40