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A subdivision of periods on the geologic time scale is known as an "epoch." Epochs represent distinct intervals of geological time characterized by specific environmental conditions, biological evolution, or significant geological events. For example, the Cenozoic Era includes the Paleocene, Eocene, and Oligocene epochs, each marked by unique developments in Earth's climate and life forms. Epochs help geologists and paleontologists organize Earth's history into more manageable and understandable segments.

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