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Pekárna Cave. Magdalenian stratigraphy, environment and termination of the loess formation in Moravian Karst
- 1.0122204 - ARUB-Q 20000031 RIV CZ eng J - Journal Article
Svoboda, Jiří - Horáček, I. - Ložek, Vojen - Svobodová, Helena - Šilar, J.
Pekárna Cave. Magdalenian stratigraphy, environment and termination of the loess formation in Moravian Karst.
Sborník geologických věd. Antropozoikum. Roč. 24, - (2000), s. 61-79. ISSN 0036-5270
R&D Projects: GA AV ČR IAA9001901
Subject RIV: AC - Archeology, Anthropology, Ethnology
The Pekárna Cave is the key Magdalenian site in Moravia,showing the development of this Upper Paleolithic culturein a stratigraphy: the basal Weichselian loess, the overlying polygenetic soils, dated radiometrically to 13-12.5ky BP, and the layers above the Magdalenian. This development may be compared to the Barová site, a cave with a scarce archaeological record but a more complete stratigraphicdevelopment. In conclusion, it seems that the end of loessdeposition is slightly metachronous under different environmental conditions at the individual caves.
Permanent Link: http://hdl.handle.net/11104/0020488
Number of the records: 1