20
November
2015
|
08:00
America/Tegucigalpa

Supporting life on Earth

We are tracking atmospheric changes through time to understand how oxygen increased to the level needed to support complex life.
Rob Creaser

Black rock sample reveals turbulent path to our planet’s oxygenated atmosphere.

By JENNIFER PASCOE

Earth's transition to a permanently oxygenated atmosphere was anything but smooth, according to new evidence from scientists from the University of Alberta, University of Waterloo, Arizona State University, University of California Riverside, and Georgia Institute of Technology. 

Their paper, published this month in Science Advances, uses geochemical data from sedimentary rocks in Western Australia to show that a burst of oxygen production by photosynthetic cyanobacteria temporarily increased O2 concentrations in Earth's atmosphere and shallow oceans roughly 2.5 billion years ago.

“We are tracking atmospheric changes through time to understand how oxygen increased to the level needed to support complex life,” says Rob Creaser, professor of Earth and atmospheric sciences at the U of A. “When the Earth first formed, there was no oxygen in the atmosphere. Our analytical facilities here at the U of A allowed us to conduct precise analyses of this rock sample to understand the tempo at which that oxygen built up through photosynthesis."

Leading-edge laboratory facilities

Creaser’s lab at the U of A in the Canadian Centre for Isotopic Microanalysis is one of only a few in the world with the ability to take the precise measurements of osmium needed to conduct this type of analysis. “Without this type of facility, we wouldn’t be able to write this paper or investigate this process,” he notes.

The new data suggest that O2 levels in the Earth's atmosphere fluctuated until enough finally accumulated to create a permanently oxygenated atmosphere around 2.4 billion years ago, a transition widely known as the "Great Oxidation Event.” 

“The onset of Earth's surface oxygenation may have been a complex process characterized by multiple ‘whiffs’ of O2 until a tipping point was crossed,” says Creaser’s former PhD student and U of A alumnus Brian Kendall, a professor of Earth and environmental sciences at the University of Waterloo and lead author on the paper.

A profound puzzle

“How and why Earth developed an oxygenated atmosphere is one of the most profound puzzles in understanding the history of our planet,” says professor Ariel Anbar of Arizona. 

The new study is a followup to work published in 2007 by the same group indicating that a small amount of O2 was present on Earth's surface 2.5 billion years ago.

Now that they’ve solved the part of puzzle to determine whether O2 concentrations were fluctuating or stable at that time, Creaser and his colleagues hope to take their inquiry a step further to address some of the remaining unanswered questions. 

“One issue is preservation. You can only do this kind of analysis on beautifully preserved samples, and there’s very few of these that are 2.5 billion years old. You’re always somewhat restricted in how far you can push your conclusions.”