The Miocene (symbol MI) is a geological epoch of the Neogene Period and extends from about 23.03 to 5.332 million years ago (Ma). The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words μείων (meiōn, “less”) and καινός (kainos, “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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Some articles on Miocene:
... to overlap the Serravallian of the Middle Miocene epoch and Tortonian epoch of the Late Miocene ... shares lower boundary) Neogene Period Miocene Pliocene Aquitanian
... The "Middle Miocene disruption" refers to a wave of extinctions of terrestrial and aquatic life forms that occurred following the Miocene Climatic Optimum (18 to 16 Ma), around 14.8 ... A Middle Miocene delta 18O increase, that is, a relative increase in the heavier isotope of oxygen, has been noted in the Pacific, the Southern Ocean and the South ...
... Coast from the Zemorrian Epoch (comprising either the Oligocene or lower Miocene) until during the Upper Miocene subepoch, when tectonic uplift ... which is known from at least 2 whole fossils, and fossil scales from Upper Miocene strata of Southern California, and L ... fossil scales in Zemorrian strata (either Oligocene or Lower Miocene) from Oregon and California ...