Characteristics of Pleistocene climate cycles identified in Cérna Valley loess-paleosol section (Vértesacsa, Hungary)

A climate cycle model was calculated using different methods (e.g., paleomagnetic, sedimentological and heavy mineral studies) on the loess sequence containing four paleosol and five loess layers in Cérna Valley. The model is based on the development of the sediment sequence created by the influence of the climatic, geological and geomorphological phenomena, and contains the following cycles: