Bronisław Wojtuń
University of Wrocław
47 Papers
259 Citations
Bronisław Wojtuń is an academic researcher from University of Wrocław. The author has contributed to research in topics: Tundra & Arctic. The author has an hindex of 15, co-authored 43 publications. Previous affiliations of Bronisław Wojtuń include Wroclaw University of Environmental and Life Sciences.
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Papers
The carbon stable isotopic composition of mosses: A record of temperature variation
TL;DR: In this article, a strong correlation between δ 13 C value of plant tissue cellulose and mean air temperature was noted for both areas and sampling periods (R 2 between 0.92 and 0.64).
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•Journal Article
Cyanoprokaryota and algae of Arctic terrestrial ecosystems in the Hornsund area, Spitsbergen
TL;DR: In 72 samples collected from various types of habitats of West Spitsbergen 150 algal taxa have been identified, including 100 taxa of Cyanoprokaryota, 40 of Chloro− phyceae, and 10 of Xanthophyceae.
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Soil moisture and temperature variation under different types of tundra vegetation during the growing season: A case study from the Fuglebekken catchment, SW Spitsbergen
TL;DR: In this article, the authors discuss the range of temperature and moisture differences and variability in tundra vegetation and Arctic soils in the context of weather changes during the growing season, and show that cold water inflow from melting snow cover greatly affects soil temperature in the first part of summer.
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Diatom communities in small water bodies at H. Arctowski Polish Antarctic Station (King George Island, South Shetland Islands, Antarctica)
TL;DR: An investigation of ponds, puddles and slow-flowing waters situated in the area of the Polish Antarctic Station distinguished two groups of diatom communities, one of which characterized waters poor in nutrients and brackish and the other characterized water richer in nutrient-rich waters.
43
•Journal Article
Stable isotope composition of plants and peat from Arctic mire and geothermal area in Iceland
TL;DR: The major goal of this study was to confirm that the original elements ratios, as well as the stable isotopic compositions of peat−forming plants are well preserved in a peat formed in cold regions, and may potentially be used in palaeoenvironmental reconstruction of Arctic environments.
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