Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Ivan Skhodnov"'
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
Publikováno v:
Archaeologia Lituana, Vol 19 (2018)
[full article, abstract in English; abstract in Lithuanian] This article is devoted to the Central Nadruvians hillforts, located within the territory of the intercultural area of theWest Balt Circle (the so-called Inster-Pregolian group of sites),
Externí odkaz:
https://doaj.org/article/f7c0fa85c5b847a08239f0cc91dd96f7
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
Publikováno v:
Archaeologia Lituana, Vol 19 (2018)
[full article, abstract in English; abstract in Lithuanian] This article is devoted to the Central Nadruvians hillforts, located within the territory of the intercultural area of theWest Balt Circle (the so-called Inster-Pregolian group of sites), an
Autor:
Dmitry Subetto, Fedor Maksimov, Ivan Skhodnov, Khikmatulla A. Arslanov, S. B. Chernov, Pavel Dolukhanov, Segey Kovalenkov, Larisa Savelieva, Gennady Kuzmin, Olga Druzhinina
Publikováno v:
Geochronometria. 38:172-181
The raised bog sediments that have been continuously accumulated over time represent the most suitable natural object which enables us to reconstruct Late Glacial and Holocene vegetation and palaeoclimates. Bog peat consists of organic carbon formed