Abstract
The natural setting and prehistoric human activity on Holocene floodplains in Central Europe is a compelling issue from several points of view. This environment presents an important sedimentary archive reflecting past human behaviour in interactions with climate change.
Two sedimentary sections recorded in the alluvial zone of Svratka River (Moravia) with a buried soil dated to the time span between the Neolithic and Late Bronze Age, and comprising one paleo-catena, were investigated using a multiproxy approach. The buried paleo-catena presents evidence of long-term (ancient) soil development, and the use of the site for human settlement and farming ca. 4500 BC until 1000 BC.
Buried soil horizons indicate (climate) stability, which according to archaeological evidence lasted for at least 3500 years, until at least 1000 BC. The architecture and the lithology of the river floodplain changes approximately 0 AD.
Anthropogenic settlement activity was not detected at the site in the subsequent period, and this is very likely to be associated with increased sedimentation rates and less optimal conditions for human settlement.