The Pliocene (Pleiocene in older texts) was a short geological epoch at the end of the Neogene. It is also the fifth and final epoch of the former Tertiary period and the fifth epoch of the Cainozoic. It began 5.3 million years ago and ended 2.6 million years ago. 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. A new land bridge at Panama brought a Great American Interchange. Hominid evolution took a new turn as some apes started to live on the savannah instead of the forests (Australopithecines). Late in the Pliocene the Greenland ice cap grew and became permanent, and the ice sheet of Antarctica grew to cover most of Antarctica.
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References[change | change source]
- "The Pliocene Epoch". www.ucmp.berkeley.edu.