Time-scale and astronomical forcing of Serbian loess-paleosol sequences

Around 800 kyr in SRSLχ time scale and between 900 kyr and 600 kyr in SRSLχfd series the 100 kyr cycles become dominant, which could be identified as the period of Mid-Pleistocene Transition. This is the first record of this paleoclimate transition in the Pannonian basin. The results presented in this study highlight the potential of Serbian loess-paleosol sequences for investigation of detailed and long-term climate reconstruction over continental Eurasian extent.