Investigating soils of barrows in the Rozumice Forest (SW Poland) – Dynamics of soil and landscape evolution in a Central European loess plateau

Soil properties reflect a host of environmental conditions and land-use patterns. Formation of cultural landscapes may well be studied at barrow cemeteries, which give the opportunity of comparing the properties of buried soils, the material building the mounds and the present-day soil cover. Current archaeo-pedological research on Late Neolithic long-barrows indicates a widespread Early Holocene presence of fertile chernozemic soils in the loess zone in Silesia (SW Poland) and their subsequent transformation (en masse) into Luvisols during the Subboreal and Subatlantic. Since the timing of the transformation remains a question – to elaborate the regional chronosequence of soil evolution – we examined the barrow cemetery in the Rozumice Forest, presumably of early medieval age. We assessed the chronology of the burial mounds and properties of the soil record by analysis of ALS data and magnetometer survey, as well as pedological and archaeobotanical analyses and ¹⁴C dating of samples from cores extracted from four of the barrows. The results show that the barrows in the Rozumice Forest were most likely built in the Early Middle Ages (7-9th c. AD) using local Luvisol (clay-illuvial soil) material, after vegetation clearance by fire. The buried Luvisols found beneath the mounds bear traces of human land-use – settlement and/or agriculture during the Late Neolithic, and may be polygenetic, being the result of transformation of Early Holocene chernozemic soils.