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11: Proterozoic Eon

  • Page ID
    33565
    • Kelly Ruppert, Tor Lacy, and Emily Haddad
    • Cerritos College, Coastline College, and East Los Angeles College

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    Introduction

    The Proterozoic Eon, meaning “earlier life,” follows the Archean Eon and ranges from 2.5 billion to 541 million years old. During this time, most of the continental cores (cratons) had formed, and plate tectonic processes started. The formation and breakup of supercontinents dramatically disturbed the carbon cycle, leading to global glaciations known as "Snowball Earths".

    Photosynthesis by microbial organisms, like cyanobacteria, completely transformed the oceans and later the atmosphere by adding massive amounts of free oxygen gas (\(\ce{O2}\)), initiating what is called the Great Oxygenation Event (GOE). Cyanobacteria were incorporated into larger cells through endosymbiosis, making the first eukaryotes, then multicellular organisms, then the first animals near the end of the Proterozoic Eon.

    Here is the the simplified geologic time scale used in the Geologic Time chapter of this book. The Proterozoic Eon is highlighted at the bottom.

    geologic time scale with Proterozoic identified

    Figure \(\PageIndex{1}\): The geological time scale. (Creative Commons License. This work is licensed under a Creative Commons Attribution-ShareAlike 4.0 International License; Edited. Original image by Jonathan R. Hendricks.)


    This page titled 11: Proterozoic Eon was last modified on Sat, 11 Apr 2026 22:09:16 GMT and is shared under a CC BY-NC 4.0 license and was authored, remixed, and/or curated by Kelly Ruppert, Tor Lacy, and Emily Haddad via source content that was edited to the style and standards of the LibreTexts platform.