Abstract
“White horizon” archaeological units consisting of carbonate concretions occur in the archaeological settlement of “Orovački vinogradi”, located near Bjelovar (NW Croatia). During archaeological excavation these horizons were considered to be the inhabitation-levels within the historical layering profile. Further sedimentological and mineralogical research and comparison of the profile with an anthropogenically unaffected site nearby (“Ciglenska strana”) required re-evaluation of this interpretation. These horizons of carbonate concretions are interpreted as the result of diagenetic processes developed within the Upper Pontian sequence of sands, clayey sands and sandstones. A sedimentary-diagenetic model is suggested for their formation. These results had consequences for the archaeological evaluation of the settlement and influenced further investigations at the locality.
Highlights
When trying to problem solve in field investigations, it is often necessary, and useful for both disciplines, to relate geology to archaeology
Research activities were conducted on an early Bronze Age locality of the Vinkovciculture (2100–1900 BC), named “Orovački vinogradi”, located near Bjelovar (North-Western Croatia)
Archaeological stratigraphic units, the so-called “white horizon” archaeological units that randomly appear in the vertical section “Orovački vinogradi” and Ciglenska strana consist of spherical, and partly elongated, white concretions, which are mostly coalesced into semi-consolidated layers
Summary
When trying to problem solve in field investigations, it is often necessary, and useful for both disciplines, to relate geology to archaeology Results of such multidisciplinary research are mostly published jointly by the disciplines, and are known as geoarchaeological results. Archaeological research at the locality resulted in numerous multidisciplinary data, relevant for understanding everyday life at the beginning of the Bronze Age in North-. “White horizon” archaeological units observed in the investigated locality occur as an interesting and puzzling phenomenon Their characteristics and origin are described and their geoarchaeological significance is discussed. Carbonate concretions within the profile are interpreted and a model for their formation is proposed Both the results and the model influenced the archaeological interpretation and evaluation of the site and future excavation activities were directed according to the geological interpretation
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
