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late Eocene Epoch

geochronology

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The Late Eocene Epoch is the final part of the Eocene Epoch, a geological period that spanned from 56 to 33.9 million years ago. The Eocene itself is the second of three divisions of the Paleogene Period. The Late Eocene specifically covers the time from 38 to 33.9 million years ago. During this time, global temperatures, which had been warm and humid throughout the Eocene, began a steady decline towards the boundary with the Oligocene Epoch. This cooling trend is evidenced by shifts in vegetation zones towards the Equator and is thought to be influenced by tectonic movements, such as the opening of passages between Tasmania and Antarctica, and later the Drake Passage.12

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