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- W2185269223 abstract "Biśnik Cave is situated in a limestone rock about 50 km northeast of Krakow, southern Poland. Its importance stems from the fact that it is one of the few sites in Europe, and the only one in Poland, with 300,000-year-long sequence of uninterrupted sediments, that cover the time span from before the Saalian to the Holocene. The excavations yielded about 200,000 animal bones and more than 4,000 stone, bone and antler artifacts. Bird remains from Biśnik Cave consist of nearly 1,600 skeletal fragments of at least 96 taxa that represent a minimum of 285 individuals. The majority of the remains belong to Galliformes; relatively numerous are also Corvidae, Falconiformes, Anseriformes and the genus Turdus. The remains include one extinct taxon (Falco tinnunculus atavus) and four species new for the Polish fossil avifauna (Aquila heliaca, Pinicola enucleator, Loxia pytyopsittacus and Carduelis flammea). Avian remains indicate a mosaic of various habitats in the surroundings of Biśnik Cave. Some kind of mature forest or at least sparsely growing trees, as well as water bodies, marshes, wet meadows, steppe and tundra habitats must have been present during the entire time of sedimentation. It is postulated that the Krakow-Czestochowa Upland was a local refugium for the forest fauna during the Saalian and Vistulian glaciations." @default.
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- W2185269223 date "2012-01-01" @default.
- W2185269223 modified "2023-10-13" @default.
- W2185269223 title "Continuous 300,000-year fossil record: changes in the ornithofauna of Biśnik Cave, Poland" @default.
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- W2185269223 doi "https://doi.org/10.26879/277" @default.
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