Pekárna Cave. Magdalenian stratigraphy, environment and termination of the loess formation in Moravian Karst

0122204 - ARUB-Q 20000031 RIV CZ eng J - Článek v odborném periodiku
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
Grant CEP: GA AV ČR IAA9001901
Kód oboru RIV: AC - Archeologie, antropologie, etnologie

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.
Trvalý link: http://hdl.handle.net/11104/0020488