Climate changes in the South of the Far East in the Late Pleistocene and Holocene (according to diatom analysis)

To solve the task, we have studied valves of diatoms from different sedimentation basins of Southern Primorye-1) from the sediments of the 1st terrace above flood-plain of the Razdolnaya River’s right bank; 2) from the quarry on the right bank of the Zerkalnaya River. Preparation of samples and estimation of valves were carried out with classical method of diatom analysis given in detail and described in “Fossil and modern diatoms of the USSR”, Volume I, 1974.