The Miocene epoch is a period of time that extends from about 23.03 to 5.332 million years before the present. As with other older geologic periods, the rock beds that define the start and end are well identified, but the exact dates of the start and end of the period are uncertain. The Miocene was named by Sir Charles Lyell. Its name comes from the Greek words μείων (meioon, less) and καινός (kainos, new) and means "less recent" because it has 18% (less than the Pliocene) of modern sea invertebrates. The Miocene follows the Oligocene Epoch and is followed by the Pliocene Epoch. The Miocene is the first epoch of the Neogene period.
|Messinian||(7.246 – 5.332 mya)|
|Tortonian||(11.608 – 7.246 mya)|
|Serravallian||(13.65 – 11.608 mya)|
|Langhian||(15.97 – 13.65 mya)|
|Burdigalian||(20.43 – 15.97 mya)|
|Aquitanian||(23.03 – 20.43 mya)|
These subdivisions within the Miocene are defined by the relative abundance of different species of calcareous nanofossils (calcite platelets shed by brown single-celled algae) and foraminifera (single-celled protists with diagnostic shells). Two subdivisions each form the Early, Middle and Late Miocene.
|Hemphillian||(9 – 4.75 mya); includes much of the Early Pliocene|
|Clarendonian||(11.8 – 9 mya)|
|Barstovian||(15.5 – 11.8 mya)|
|Hemingfordian||(19 – 15.5 mya)|
|Arikareean||(30.5 – 19 mya); includes much of the Oligocene|
|Delmontian||(7.5 – 2.9 mya); includes much of the Pliocene|
|Mohnian||(13.5 – 7.5 mya)|
|Luisian||(15.5 – 13.5 mya)|
|Relizian||(16.5 – 15.5 mya)|
|Saucesian||(22 – 16.5 mya)|
|Zemorrian||(33.5 – 22 mya); includes nearly all the Oligocene|
Although a long-term cooling trend was well underway, there is evidence for a warm period during the Miocene when the global climate rivalled that of the Oligocene. The Miocene warming began 21 million years ago and continued until 14 million years ago, when global temperatures took a sharp drop. By 8 million years ago, temperatures dropped sharply once again, and the Antarctic ice sheet was already approaching its present-day size and thickness. Greenland may have begun to have large glaciers as early as 7 to 8 million years ago, although the climate for the most part remained warm enough to support forests there well into the Pliocene.
Mountain building took place in Western North America and Europe. Both continental and marine Miocene deposits are common worldwide with marine outcrops common near modern shorelines. Well studied continental exposures occur in the American Great Plains and in Argentina. India continued to collide with Asia, creating more mountain ranges. The Tethys Seaway continued to shrink and then disappeared as Africa collided with Eurasia in the Turkish-Arabian region between 19 and 12 mya. Subsequent uplift of mountains in the western Mediterranean region and a global fall in sea levels combined to cause a temporary drying up of the Mediterranean Sea (known as the Messinian salinity crisis) near the end of the Miocene.
Grasslands underwent a major expansion as forests fell victim to a generally cooler and drier climate overall. Grasses also diversified greatly into a number of species and also caused a major increase in the biodiversity of large herbivores and grazers, including ruminants (of which modern cattle and deer belong).
Both marine and continental fauna were fairly modern, although marine mammals were less numerous. Only in isolated South America and Australia did widely divergent fauna exist.
Recognizable crows, ducks, auks, grouses and owls appear in the Miocene. By the epoch's end, all or almost all modern families are believed to have been present; the few post-Miocene bird fossils which cannot be placed in the evolutionary tree with full confidence are simply too badly preserved instead of too equivocal in character. Marine birds reached their highest diversity ever in the course of this epoch.
Brown algae plants, called kelp, proliferate, supporting new species of sea life, including otters, fish and various invertebrates. The cetaceans diversified and some modern genera have already appeared, such as the sperm whales. The pinnipeds, who appeared near the end of the Oligocene, became more and more aquatic.
The oceans continue to cool as the poles were transformed into glaciers.
|Aquitanian | Burdigalian | Langhian
Serravallian | Tortonian | Messinian
|Zanclean | Piacenzian|
- Ogg, Jim; (2004): Overview of Global Boundary Stratotype Sections and Points (GSSP's). HTML fulltext. Retrieved 2006-APR-30.
- Rohde, Robert A. (2005): GeoWhen Database. Retrieved 2006-SEP-23.