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A period of time that
existed from 23 to 5.3 MYA.
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The climate of the
Miocene was warmer than the Oligocene before it, or the Pliocene
after it. The warmer temperatures allowed for two important
ecosystems to emerge: Grasslands
and Kelp forests.
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After the warming period,
the earth began to cool.
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Deserts and Tundras began
to expand, while Forests began to disappear.
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Antartica became
isolated.
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Many of the fossil
species of this time have close relatives alive today.
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Mammals and birds
developed to look like they do today.
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95% of plant species
today existed during the Miocene.
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In North America the
Sierra Nevada and
Cascade Mountains formed.