The Early Pleistocene climate dynamic in the Russian Far East (southern Primorye) was obtained from a total of 8 macrofloras (woods, leaves, fruits and seeds,) and 18 microfloras collected from a 10 m thick, terrigenous succession exposed in the Pavlovskoe brown coal field.According to magnetostratigraphy, the studied section covers the last 200 kyr of the Calabrian and comprises the early/middle Pleistocene transition.