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RESEARCH PAPER
Evolution of the Bug River Valley during the Holocene in the environs of Janów Podlaski (Eastern Poland) in the light of malacological analysis of oxbow lake deposits
1
AGH University of Science and Technology, Faculty of Geology, Geophysics and Environment Protection, Chair of Environmental Analysis, Cartography and Economic Geology, Cracow, Poland
2
Department of Physical Geography and Palaeogeography, Maria Curie-Skłodowska University in Lublin, Poland
Submission date: 2012-01-12
Final revision date: 2012-04-20
Acceptance date: 2012-04-21
Publication date: 2020-04-08
Folia Malacol. 2012;20(4):295–304
KEYWORDS
ABSTRACT
The malacofauna of two profiles of deposits filling palaeomeanders of the Bug River Valley was studied. The first one (Zaczopki) represents an older phase of the valley development corresponding with the Early Holocene or even with the Late Glacial. Its assemblage contains numerous shells of cold-tolerant species. The second profile is situated near the village Woroblin. It represents a younger stage of the valley evolution (uppermost part of the Middle Holocene and Late Holocene). The mollusc fauna is typical of shallow and overgrown, stagnant water bodies. The sequences of mollusc aasemblages from both profiles characterise the development of these reservoirs, corresponding with climatic changes and differences in fluvial activity of the Bug River during the Holocene.
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CITATIONS (1):
1.
Mollusc assemblages from Subatlantic oxbow lake deposits in the Szreniawa River valley near Słomniki (Miechów Upland, southern Poland)
Witold Alexandrowicz
Folia Malacologica
Witold Alexandrowicz
Folia Malacologica
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