Scientists use historical major geological and biological events to characterise the geological time scale.
Paleontologists, archaeologists, and geologists use the fossil record to put significant occurrences and species in the right geological epoch. The geologic time scale is fundamentally based on fossils. Because these time periods are frequently identified based on the presence of animal life, the names of the majority of the aeons and eras end in zoic. Fossil remains of relatively simple organisms, like bacteria, algae, and worm-like animals, have been found in rocks formed during the Proterozoic Eon.
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