The Mid-Brunhes Transition is not as prominent as the Mid-Pleistocene Transition, but nonetheless an important step in the Quaternary climate evolution. Here we assess the patterns of the Mid-Brunhes Transition in a suite of Lake records from Eurasia, i.a. from Gamma Ray borehole logging data. Consistent with other datasets, we find that Marine Isotope Stage 14 is expressed in different intensity. Finally, we expand our data synthesis to selected loess records to check for regional consistency in the Balkan Paninsula.