Soil particles reworking evidences by AMS 14C dating of charcoal

Soil charcoal dating is a time proxy for soil pedogenesis. I test the stratification hypothesis by AMS 14C dating of charcoal fragments from soil profiles between 1700 and 1900 m with respect to altitude within the Alps. The charcoal fragments are around 1 mm in size. There is no age/depth relationship for charcoal particles of the size millimeter. The results are discussed in light of the role of soil fauna, up-rooting and colluvial processes. Although biotic pedoturbation is poorly described in mountain and sub-alpine elevation, I hypothesize that this process is very active and plays a major role on the soil functioning. (author)