Izvorni znanstveni članak
https://doi.org/10.21857/mnlqgc5jzy
TWO SIDES OF THE 7.1 ka BP RCC EVENT IN THE SOUTHERN CARPATHIAN BASIN: HUMAN ADAPTATION TO THE CHANGES IN ENVIRONMENTAL CONDITIONS DURING THE MIDDLE AND LATE NEOLITHIC
Katarina Botić
orcid.org/0000-0002-2243-1149
; Institut za arheologiju
Sažetak
One of the rapid climate change (RCC) events, which had a lesser impact on the environmental
conditions of the Northern Hemisphere but had a stronger impact on the micro-regional scale, is the 7.1 ka BP event. Cooler and wetter conditions at its onset seem to have accompanied the initial dispersal of the central European LBK from its core area to the regions, among others, of western Transdanubia and beyond, populating the area south of the Drava River. In the local chronology, this change in the material culture is marked by the appearance of the Middle Neolithic around 5400 BC. The end of this climate event is, however, marked by an initial stage of dry and warmer conditions around 5000 BC which enabled settlement formation in the lowlands of the Eastern Slavonia. After this initial phase and the formation of the Late Neolithic tell settlements, over a period of about 500 years changes in humidity and temperature occurred, eventually leading to the abandonment of most of the tell sites. Human adaptation to the changes in environmental conditions in both micro-regions and archaeological contexts is discussed in this paper.
Ključne riječi
RCC 7.1 ka BP; LBK; Middle and Late Neolithic; tells
Hrčak ID:
278738
URI
Datum izdavanja:
1.2.2022.
Posjeta: 355 *