Informace o publikaci
The 2002-2003 excavations in the Dzerava skala Cave, West Slovakia.
| Název česky | Výzkum jeskyně Dzeravá skala, západní Slovensko, v letech 2002-2003. |
|---|---|
| Autoři | |
| Rok publikování | 2004 |
| Druh | Článek v odborném periodiku |
| Časopis / Zdroj | Anthropologie 42 |
| Fakulta / Pracoviště MU | |
| Citace | |
| Obor | Archeologie, antropologie, etnologie |
| Klíčová slova | Upper Paleolithic; Upper Pleistocene; fauna; industry; West Slovakia |
| Popis | The new excavations at the Dzeravá skala cave opened a complex stratigraphic section, showing combination of in situ developed sediments, in-blown loess, and clays, paleosols and clasts removed from elswhere, most probably from the above cave chimneys. In terms of paleobotany and paleontology, this sequence illustrates the climatic record from the Holocene over the Last Glacial Maximum to the more temperate oscillations of the Interpleniglacial, and, possibly, even before that. Two aspects are of importance: the almost constant presence of cave bears throughout the Pleistocene layers, and the repeated human visits. The archaeological record comprises the Neolithic, probably Late Paleolithic, Gravettian (25 – 31,7 ka BP), and the Early Upper Paleolithic (34 – 37 ka BP). The isolated human molar (right lower M2), found by Hillebrand in 1913, may be correlated with the EUP layers. |