Abstract
The dolmen known as Shepsi was accidentally discovered on the Black Sea coast (Tuapse region, Russia). Radiocarbon dates show that the classic trapezoidal construction of the Caucasian dolmens with a port-hole appeared in the region as early as 3250 BC. The distinctive structural characteristic for dolmens of that time was a floor slab laid between the side slabs, which were embedded in the ground. The material complex and C-14 dates show that this type of dolmen coexisted with the Novosvobodnaya-type of the Maikop culture, located on the northern slope of the main Caucasus ridge. This leads to a new hypothesis concerning the regional origin and further development of the megalithic structures in the western Caucasus.
| Original language | English |
|---|---|
| Pages (from-to) | 743-752 |
| Number of pages | 10 |
| Journal | Radiocarbon |
| Volume | 56 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 2014 |