Earth Sciences

Pleistocene

The Pleistocene is the period in Earth's history commonly referred to as the Ice Age. For most of this period, the regions that were located north and south of the Earth were completely covered by glaciers, approximately one kilometer thick. It is important to recognize that the Pleistocene was a series of actual glaciations, separated by relatively short inter glacial periods. This period began 2.6 million years ago and lasted until the end of the glaciation.

Pleistocene

Related topics

Cenozoic era, Mesozoic era, Paleozoic era, geological eras

What is Pleistocene?

Also called the Ice Age, it is the first part of the Cenozoic Quaternary and covers the ice age. Its end coincides with the end of the Paleolithic when the continents were already in their present positions.

What happened in the Pleistocene?

During this stage, the Earth cooled down, which had a great effect on its animal life; the different types of animals, or ecological populations, were severely altered and even some of them were completely eliminated. Some of these species became extinct, and at the same time new ones were born. As the ice caps accumulated in greater numbers, sea levels fell. Under the sea began to emerge land bridges, the most famous was the Bering land bridge and the land bridge between North America and South America and because of this, a wave of animal migrations to the continents began.

Pleistocene characteristics

The main characteristics of the Pleistocene are mentioned below:

Pleistocene periods

The Pleistocene periods were as follows:

Weather

The climate was extremely cold and ice sheets were found covering all of Antarctica, large parts of Europe, North and South America, and small areas in Asia. In North America, the ice sheets spread over Greenland and Canada and parts of the northern United States. The remains of Ice Age glaciers can still be seen in some parts of the world, including Greenland and Antarctica. All of this was known as glaciations.

Glaciations

Glaciations was the name that was used to designate the set of glaciers or cold phases that were interspersed by phases that were a little warmer. These cold phases occurred mainly in the northern part of the earth; however, they reached the rest of the world.

During these phases, extremely cold temperatures were present, there was no rain, and large masses of ice, sometimes even larger than a thousand meters, covered the earth.

When the temperature rose, these masses of ice began a process of defrosting and the rains began causing the seas to rise their levels, and as a result, most of the coast of the seas suffered great changes, including the flora and fauna of these places.

The scientist Milutin Milankovitch, of Yugoslavian origin, made several calculations on the solar receptions that were obtained during this phenomenon, and according to his studies great variations happened in the form in which the orbit of the earth is positioned around the sun, there were changes in the angle obliquity with the Earth’s orbit and there was a fluctuation of the earth’s axis.

Pleistocene flora

The flora looked for more sheltered areas to develop as the bottoms of the valleys, from which the forests later arose. With each glaciation changes arose, it also had an advance in becoming a tundra, making the species more resistant to the climate. Humidity caused new species to emerge, such as deciduous trees and thermophilus plants. In the third period, the temperate forest arose, there were prairies and steppes.

Fauna

It was known by the name of Megafauna. In the first period, the animals were large carnivores, apes and three-toed horses; there were also mammoths, bears, lynxes, rhinoceroses and cave lions. In the transition period, deer, elephants, and split-nosed rhinoceros could be found.

Written by Gabriela Briceño V.
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