T h e   l a s t   G l a c i a l    E p o c h .
Flora and fauna.
   The decrease of temperature on the planet and the formation of  large ice systems in the north  caused  global modifications in the vegetative and animal world of the Northern hemisphere. The borders of all natural zones began to shift to the south. On the territory of  Siberia the following natural zones were located:

   The zone of cold tundra and tundra –steppes   extended along the glaciers  ten kilometers wide. It was located in those areas, where  wood land and  taiga are now.
  In the South  tundra-steppe gradually turned in  wood-steppe and   wood land. The wood regions were very small, and were not everywhere. More often   woods placed on southern shores of  ice lakes, both in river valleys and on spurs of mountains.
  More to the south
dry steppes were located; in the west of Siberia gradually turning to the Sayn-Altai mountain system, in the east bounding with half-deserts of Mongolia. In   some areas  tundra –steppes and  steppes were not divided by stripes of   wood and gradually replaced one another.

  In  new climatic conditions of the Glacial Epoch the world of animals was changing also. The new kinds of  fauna became to form for the last stages of the Quaternary Age in the northern hemisphere. The appearance of the so-called Mammoth Fauna Complex was the most significant demonstration of these modifications, and it consisted of  more cold-enduring kinds of animals.