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Eocene

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The Eocene epoch (55.8 ± 0.2 - 33.9 ± 0.1 Ma) is a major division of the geologic timescale and the second epoch of the Paleogene 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 called Grande Coupure (the "Great Break" in continuity), which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and end of the epoch are well identified,[1] though their exact dates are slightly uncertain. The Eocene epoch is the second and among the longest epochs in the Cenozoic era, lasting from 55 to 34 million years ago. It marked a milestone in mammal diversity in which the modern orders of mammals become apparent in the fossil record. It is marked with two major changes to the planet: the Thermal Maximum and Le Grande Compure. The Eocene was an epoch in Earth's history. During that point in time, the birds had become the top predators on Earth since the absence of the dinosaurs. The mammal, though small during the early Eocene, eventually rose above the birds and diversified. The Eocene was an epoch in Earth's history. It was the second epoch of the Palaeogene period and Cenozoic era.

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Oligocene epoch

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Paleogene period

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Episode 3.1 Episode 3.9 Sea Monsters: Into the Jaws of Death Walking with Beasts: New Dawn Walking with Beasts: Whale Killer

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Paleocene epoch

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Eocene

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The Eocene was an epoch in Earth's history. It was the second epoch of the Palaeogene period and Cenozoic era. The Eocene epoch is the second and among the longest epochs in the Cenozoic era, lasting from 55 to 34 million years ago. It marked a milestone in mammal diversity in which the modern orders of mammals become apparent in the fossil record. It is marked with two major changes to the planet: the Thermal Maximum and Le Grande Compure. The Eocene epoch (55.8 ± 0.2 - 33.9 ± 0.1 Ma) is a major division of the geologic timescale and the second epoch of the Paleogene 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 called Grande Coupure (the "Great Break" in continuity), which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and end of the epoch are well identified,[1] though their exact dates are slightly uncertain. The name Eocene comes from the Greek ἠώς (eos, dawn) and καινός (kainos, new) and refers to the "dawn" of modern ('new') mammalian fauna that appeared during the epoch. The Eocene was an epoch in Earth's history. During that point in time, the birds had become the top predators on Earth since the absence of the dinosaurs. The mammal, though small during the early Eocene, eventually rose above the birds and diversified.

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