The third era of the Archean eon, spanning about 3.2 to 2.8 billion years ago. Localized oases of relatively oxygen rich water existed in some nearshore shallow marine settings during this era, an early precursor to the much later atmospheric oxygenation of the Paleoproterozoic. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Start (Million Years Ago) End (Million Years Ago) Key EventOases of relatively high oxygen levels existed in some nearshore shallow marine settings by the Mesoarchean. 1 Connections
Anticipated By
Has Geologic Rank
In Discipline
Precursor To
Sources
1. Wikipedia: Archean
WikipediaLead section
The Earth during the Archean was mostly a water world: there was continental crust, but much of it was under a superocean deeper than today's oceans.
Ocean and atmosphere chemistry section
Oases of relatively high oxygen levels existed in some nearshore shallow marine settings by the Mesoarchean.
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