This study provides a compilation of the paleointensity records for the Cretaceous period derived from sediments of the Russian Plate and adjacent areas. The paleoinetensity values were calibrated using the laboratory redeposition experiments. Remarkable differences in the relative paleointensity variations were detected at the Berriasian-Early Barremian, Late Barremian-Santonian, and Early-Late Maastrichtian boundaries. In the Berriasian-Early Barremian interval, the paleointensity varied
