Miocene  

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The Miocene is a geological epoch of the Neogene Period and extends from about Template:Mya (Ma). The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words Template:Lang (Template:Lang, “less”) and Template:Lang (Template:Lang, “new”) and means "less recent" because it has 18% fewer modern sea invertebrates than the Pliocene. The Miocene follows the Oligocene Epoch and is followed by the Pliocene Epoch. The Miocene is the first epoch of the Neogene Period.

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Unless indicated otherwise, the text in this article is either based on Wikipedia article "Miocene" or another language Wikipedia page thereof used under the terms of the GNU Free Documentation License; or on research by Jahsonic and friends. See Art and Popular Culture's copyright notice.

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