Publication details
Ukončenie revízného výskumu v jaskyni Dzeravá skala. Archeologické výskumy a nálezy na Slovensku v roku 2003.
| Title in English | Termination of revision excavation in the Dzeravá skala cave. |
|---|---|
| Authors | |
| Year of publication | 2004 |
| Type | Article in Proceedings |
| Conference | Archeologické výskumy a nálezy na Slovensku |
| MU Faculty or unit | |
| Citation | |
| Field | Archaeology, anthropology, ethnology |
| Keywords | Upper Paleolithic; Upper Pleistocene; fauna; industry; West Slovakia |
| Description | 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. |