Study shows planet's atmospheric oxygen rose through glaciers
A University of Wyoming researcher contributed to a paper that determined a "Snowball Earth" event actually took place 100 million years earlier than previously projected, and a rise in the planet's oxidation resulted from a number of different continents—including what is now Wyoming—that were once connected.
|Illustraton of Snowball Earth [Credit: Neethis/WikiCommons]|
Chamberlain is the second author of a paper, titled "Timing and Tempo of the Great Oxidation Event," which appears in the Proceedings of the National Academy of Sciences. The journal is one of the world's most prestigious multidisciplinary scientific serials, with coverage spanning the biological, physical and social sciences.
Ashley Gumsley, a doctoral student at Lund University in Lund, Sweden, is the paper's lead author. Other contributors were from the Geological Survey of Canada in Ottawa; Swedish Museum of Natural History; University of Johannesburg, South Africa; and the University of California-Riverside.
The research relates to a period in Earth's history about 2.45 billion years ago, when climate swung so extremely that the polar ice caps extended to the equator and the Earth was a snowball, and the atmosphere was largely isolated from the hydrosphere, Chamberlain says. Recovery from this Snowball Earth led to the first and largest, rapid rise in oxygen content in the atmosphere, known as the Great Oxygenation Event (GOE), setting the stage for the dominance of aerobic life, he says.
|Kevin Chamberlain, a University of Wyoming professor of geology, points to a glacial diamictite exposed|
in the Snowy Range of Wyoming [Credit: UW]
"So, both Snowball Earth periods had extreme impacts on the development of life," he says. "It helps us understand the evolution of Earth and Earth's atmosphere, and evolution of life, for that matter."
Chamberlain's contribution focuses on igneous rocks exposed in South Africa that record the existence of equatorial glaciers and contain chemical indicators for the rise of atmospheric oxygen. Chamberlain's in situ method to determine the age of the rocks does not require removing baddeleyite crystals from the rock. This process allows for analysis of key samples with smaller crystals than previously allowed. Using a mass spectrometer, the age of the rocks is determined by measuring the buildup of lead from the radioactive decay of uranium, he says.
"The basic story had been worked out earlier by others, but our results have significantly refined the timing and duration of the 'event,' which is more of a transition actually," Chamberlain explains. "With all the discussion of climate change in the present day, understanding how Earth responded and the effects on the atmosphere in the past may help us predict the future."
Chamberlain points to a Wyoming connection in this research. From paleomagnetic data, many of the continents, at the time, including the basement rocks of Wyoming, were all connected into a single, large continent and situated near the equator. Other continents connected included parts of what are now Canada and South Africa. This situation is part of the trigger for the "Snowball Earth" conditions.
"There are glacial deposits exposed in the Medicine Bow Mountains and Sierra Madre that are from this same event," he says.
These rocks, known as diamictites, have large drop stones that depress very fine-grained mudstone. The large stones dropped from the underside of glacial sheets as they spread out and melted over shallow seas, similar to sediments beneath the Ross sea ice sheet of Antarctica today.
"The fact that these sediments were at the equator at 2.45 billion years ago comes from the paleomagnetic data from associated igneous rocks," Chamberlain says. "I think that it's interesting that part of the story is just 40 miles away in the Snowies."
Source: University of Wyoming [February 06, 2017]