Eocene
The Eocene epoch (56-34 mya) is a major division of the geologic timescale and the second epoch of the Palaeogene period in the Cenozoic era. The Eocene spans the time from the end of the Paleocene epoch to the beginning of the Oligocene epoch. The start of the Eocene is marked by the emergence of the first modern mammals. The end is set at a major extinction event that may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. Still, as with other other geologic periods, the strata that define the start and end of the epoch are well identified, but their exact dates are slightly uncertain.
Eocene oceans
The Eocene oceans were warm and teeming with fish and other sea life. The first Carcharinid sharks appeared, as did early marine mammals, including Basilosaurus, an early species of whale that is thought to be descended from land animals, the hoofed predators called mesonychids, of which Mesonyx was a member.
Related Topics:
Fish - Carcharinid sharks - Basilosaurus - Whale - Mesonychid - Mesonyx
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~ Table of Content ~
| ► | Introduction |
| ► | Eocene subdivisions |
| ► | Eocene climate |
| ► | Eocene paleogeography |
| ► | Eocene flora |
| ► | Eocene fauna |
| ► | Eocene oceans |
| ► | See also |
| ► | External links |
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