Earth's history to be rewritten: Oxygen appeared 700 million years earlier than previously thought

"We have readjusted the point in time when oxygen-producing bacteria, and photosynthesis, impacted land-based life on Earth and put oxygen into the atmosphere. This was a fundamental event that allowed for the life on Earth and evolution as we know it. It was not a localized event, but something that influenced the planet as a whole." Lasse Nørbye Døssing, Postdoc, Department of Geosciences and Natural Resources Management at the University of Copenhage.

It's been nearly 15 years since Professor Minik Rosing of the University of Copenhagen asserted that terrestrial life began with primitive bacteria living in Precambrian oceans some 3.8 billion years ago.

However, these microscopic organisms were in no way able to produce the amounts of oxygen necessary to alter Earth's atmospheric composition and thus form the basis of life as we know it. Millions upon millions of more years were needed to advance to this stage.

Planet's oldest soil

The new and dramatic aspect of Earth's history is based upon the analysis of ancient rock samples collected from 1000 metres beneath South Africa. The new chapter has been investigated, analysed and now co-written by among others, Postdoc Lasse Nørbye Døssing, of the University of Copenhagen's Department of Geosciences and Natural Resource Management.

Døssing and his colleagues have extended the 2.3 billion years that it was thought since large amounts of oxygen appeared in the atmosphere by an additional 700 million years. His project colleagues come from universities in Denmark and from around the world, including: the Nordic Center for Earth Evolution (NordCEE) in Odense, Denmark; The University of Southern Denmark; the University of Johannesburg, South Africa; Jacobs University in Bremen, Germany; and the University of British Columbia, Canada.

Døssing's colleague Sean Crowe from the University of British Columbia states:

"Our investigations indicate that bacteria were able produce large amounts of oxygen three billion-years-ago and thereby create the foundation for one of the most important chemical processes on earth -- photosynthesis. Microscopic bacteria's ability to allow trees and other plant life to take in CO2 and produce oxygen in return, for example. This was the beginning of a long and complicated process that brings us to today, a point in time when nearly 20 percent of Earth's atmosphere is composed of oxygen and the rest, nearly all nitrogen. These bacteria are the reason that we as humans, as well as other beings, have been able to breath and thus populate the planet.

The big question

Besides being of interest in relation to atmospheric chemistry, the results are of great significance for evolutionary history. And that includes the evolution of humans from primitive beings to top creatures in the animal kingdom.

Lasse Nørbye Dossing: "As a geologist, I'll leave it to the evolutionary biologists and philosophers to answer the question of where humans, as a species, would be today if we didn't have the extra 700 million years of sufficient oxygen in the atmosphere. But it is thought-provoking that our research results have provided evolutionary history with a new and not entirely insignificant chapter."

One who is prepared to comment on the gripping research is Professor Eske Willerslev, a DNA researcher and evolutionary biologist at the University of Copenhagen famous for his genetic mapping of extinct species and prehistoric humans.

"These are incredibly interesting results that Døssing and the other researchers have reached. The results point to the fact that forms of terrestrial life dependent upon oxygen have taken longer to evolve than we had previously thought. Conversely, it could also suggest that this type of life has been around for longer than believed. Whatever the case, this new research will prompt researchers to look for life further back than we had previously believed possible," stresses Professor Willerslev.