Geology

The Pleistocene was known for its ice ages. An ice age is a time when many glaciers cover many parts of the earth. Scientists have come up with many reasons for an ice age:

  • The earth right now is on an approximate tilt of 23.1 degrees. Most scientists now support the theory that during earth' s many past ice ages, the earth was not on a tilt. If this happened, sunlight would not reach the poles, allowing much snow to accumulate. Once enough snow accumulated, the pressure of the glacier would cause a thin, slippery layer of water to form underneath the colossal ice sheet. When it moved southward, the sun melted the glacier, creating a thicker water layer underneath the ice. This is the most supported theory.
  • Another theory is that there was a lot of volcanic activity during this time, which caused a substantial amount of dust and particles to fly in the air. This, in turn, made the earth cooler, allowing glaciers to form.
  • Today, our orbit is almost circular. Some scientists say that in the ice ages, earth\rquote s orbit was more like an ellipse, and when earth was farther away, ice caps enlarged and glaciers could form.

Whatever the cause, animals of the Pleistocene had to stay tough to survive.

Animal Life

All living organisms had to cope with the ice age. Mammals evolved through adaptation. They adapted in the following ways:

  • A covering of hair. This kept in the heat and made them warmer.
  • They became smaller. Being smaller requires less food and it allows less heat to escape.
  • Animals migrated equator-ward. There it was warmer, and they could get a bite to eat.
  • Or they died out. That isn't really adapting, but that's what some animals did.

Plant Life

During the Pleistocene Epoch, Plants also evolved with the climate change. During the warmer, inter-glacial period, woodlands were dominant. As it got colder, grasses emerged. During the Ice ages, tundra was the main vegetation.

 

All animals needed to adapt in the Ice Ages.

 

A woolly mammoth.

Cenozoic Era: Quaternary Period: PleistoceneEpoch