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Qu'est-ce (qui) est proterozoic$64781$ - définition
![Columbia]], about 1,590 Mya](https://commons.wikimedia.org/wiki/Special:FilePath/Paleoglobe NO 1590 mya-vector-colors.svg?width=200 "Columbia]], about 1,590 Mya")
![[[Rodinia]], about 750 Mya](https://commons.wikimedia.org/wiki/Special:FilePath/Rodinia reconstruction.jpg?width=200 "[[Rodinia]], about 750 Mya")
![[[Pannotia]], 545 Mya (disputed), centered on South Pole](https://commons.wikimedia.org/wiki/Special:FilePath/Pannotia.svg?width=200 "[[Pannotia]], 545 Mya (disputed), centered on South Pole")
 (18940551220).jpg?width=200)
Wikipédia
The Proterozoic (IPA: ) is a geological eon spanning the time interval from 2500 to 538.8 million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided into three geologic eras (from oldest to youngest): the Paleoproterozoic, Mesoproterozoic, and Neoproterozoic.
The Proterozoic covers the time from the appearance of oxygen in Earth's atmosphere to just before the proliferation of complex life (such as trilobites or corals) on the Earth. The name Proterozoic combines two forms of ultimately Greek origin: protero- meaning 'former, earlier', and -zoic, 'of life'.
Well-identified events of this eon were the transition to an oxygenated atmosphere during the Paleoproterozoic; the evolution of eukaryotes; several glaciations, which produced the hypothesized Snowball Earth during the Cryogenian Period in the late Neoproterozoic Era; and the Ediacaran Period (635 to 538.8 Ma) which is characterized by the evolution of abundant soft-bodied multicellular organisms and provides the first obvious fossil evidence of life on Earth.
