Reconstruction of palaeotemperatures of pleistocene interglacial intervals of Belarus from palynological evidences

In this article you will find the results of palaeoclimatical reconstructions made for Belovezhian, Mogilevian, Alexandrian, Muravian interglacials Pleistocene of Belarus on the basis of detailed palynological studying of composition fossil pollen flora. It was used the method of overlapping of "climatic areals" plants -- components of the fossil flora. Reconstruction of palaeotemperature ranges are made for each of the picked up regional pollen zones that has allowed to trace process of changing palaeotemperatures during chronologically consecutive phases in development of flora and vegetation of every interglacials. The reconstructions performed for four interglacials of the Pleistocene of Belarus have shown that temperatures of the warmest and coldest months were similar to each other and the highest ones recorded during the climatic optima of the Belovezhian and Muravian interglacials. The Mogilevian and Alexandrian interglacials were also similar in palaeotemperature parameters, but colder than the above-mentioned interglacial