The Pliocene epoch ended by glaciers and the beginning of the ice age. This is what started the pliostocene era
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The Miocene was from about 26 million to 5 million years ago. It is part of the Tertiary Period and the Cenozoic Era. The word Miocene comes from the Greek for "less than present." It is the age of the first hominids.
The smallest unit of geologic time is an age, followed by epoch, period, era, eon, and super eon.
The Oligocene Epoch.
Oligocene
This is called the Oligocene Epoch.
Dinohyus ruled from the Oligocene epoch to the miocene, it ruled for about 13 million years.
baluchitherium , extinct primitive rhinoceros, belonging to the genus Baluchitherium, of the Oligocene epoch, fossilized bones of which were found in central Asia
The megalodon shark existed alongside many other plants and animals in the Oligocene Epoch. An example is the hyaenodon horridus.
Megalodons were a huge species of shark that lived from the Oligocene epoch through the Pleistocene epoch. Megalodons lived in almost every sea in the world and, like the modern sharks of today, were fish. Woolly mammoths were a large, hairy elephant that lived during the Pleistocene epoch. They lived on the tundra ,among other habitats, and were mammals.
The Tertiary Period (including the Pliocene, Miocene, Oligocene, Eocene, and Paleocene Epochs) lasted from about 65 million years ago to 1.8 million years ago. It is part of the Cenozoic Era, along with the Quarternary Period.
The Pliocene epoch ended by glaciers and the beginning of the ice age. This is what started the pliostocene era
Of or belonging to the geologic time, rock series, or sedimentary deposits of the third epoch of the Tertiary Period, characterized by futher development of modern mammalian fauna, including the rise of the true carnivores and their gradual replacement of the creodonts.
Of or belonging to the geologic time, rock series, or sedimentary deposits of the third epoch of the Tertiary Period, characterized by futher development of modern mammalian fauna, including the rise of the true carnivores and their gradual replacement of the creodonts.
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