Effects of ozone levels on climate through Earth history

<p>Molecular oxygen in our atmosphere has increased from less than a part per million in the Archean Eon to a fraction of a percent in the Proterozoic and finally to modern levels during the Phanerozoic. The ozone layer formed with the early Proterozoic oxygenation. While oxygen itself has onl...

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Bibliographic Details
Main Authors: R. Deitrick, C. Goldblatt
Format: Article
Language:English
Published: Copernicus Publications 2023-06-01
Series:Climate of the Past
Online Access:https://cp.copernicus.org/articles/19/1201/2023/cp-19-1201-2023.pdf