Pliocene

From Wikipedia, the free encyclopedia
Jump to: navigation, search
The Pilocene

The Pliocene (Pleiocene in older texts) was a short geological epoch at the end of the Neogene.[1] It began 5.3 million years ago (mya), and ended 2.6 mya. The Pliocene follows the Miocene and is followed by the Pleistocene.
The world continued to get cooler and drier in the Pliocene. Tropical rain forests and deciduous forests shrank. Grasslands grew, and many herbivorous mammals became grazers instead of browsers. Hominid evolution took a new turn as some apes started to live on the savannah instead of the forests (Australopithecines).

Gallery[change | change source]

References[change | change source]