(Credit: Mycatkins, flickr.com)

A close-up of oxygen bubbles. (Credit: Mycatkins, flickr.com)

The early Earth was characterized by the absence of oxygen which first rose due to photosynthesis during the Great Oxidation Event 2.3-2.5 billions years ago. Now, researchers have found markers in 2.95 billion year old rocks from South Africa that show oxygen was already at a significant levels. This finding shows that organisms were doing photosynthesis 500 millions years before the Great Oxidation Event in such a way that oxygen started to accumulate in shallow marine settings.

Original research paper published in the journal Nature Geoscience on March 23, 2014.

Names and affiliations of selected authors

Ernesto Pecoits, Department of Earth and Atmospheric Sciences, University of Alberta

Kurt O. Konhauser, Department of Earth and Atmospheric Sciences, University of Alberta