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Soil organic carbon (SOC) stocks are a function of the SOC concentration and the bulk density of the fine soil. Both variables are prone to changes and are influenced by abiotic and biotic processes. To determine the effect of variations of both variables on SOC stocks at two grassland sites, one with Stagnic Vertisols and one with Orthoeutric Arenosols, 440 soil cores were sampled down to 60cm depth. Bulk density and C and N concentrations were measured in 5cm intervals (0–10cm depth) and 10cm intervals (10–60cm depth). SOC stocks at the clay rich site with Vertisols were almost twice as high (86t C ha⁻¹ in 0–60cm depth) as at the sandy site with Arenosols (48t C ha⁻¹). Variations in the SOC stocks were determined by the thickness of the loess layer at the clay rich site. Underlying clay horizons hampered the C translocation into the subsoil which resulted in lower SOC stocks of the whole profile …