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  • and altered further into a chernozem cambisol during a phase of slope stability of about 3 000 years between the Bronze Age and medieval times. The detected brunification processes took place at unexpected high rates.
  • (Saale). The chronology is based on 8 radiocarbon ages of charcoal, soil organic matter as well as on archaeological age estimations of embedded artefacts. The results imply that the chernozem at the site might have been altered by prehistoric land use
  • 2013