geotimesheader  
Home Calendar Classifieds Subscribe Advertise

Geotimes
 Published by the American Geological Institute
Newsmagazine of the Earth Sciences

October 2000


News Notes

Ancient clouds trapped in stone

In back-to-back reports, University of California, San Diego, scientists have shown it is possible to wring out the chemical signatures of Earth’s atmosphere from Precambrian stone. As they hunt down isotopic anomalies never before seen in Earth’s rock record, the scientists are excited about the future prospects of their technique.

“People have been looking for a way to track the evolution of oxygen and the origin of life for at least 50 years and this is the first time there’s ever been a quantitative way to do that,” says Mark Thiemens, dean of physical sciences at UCSD.
 
Until now, analysis of ancient atmospheric signatures depended on the depth of glacial ice. The oldest known ice core comes from Vostok, Antarctica, where ice 3,000 meters deep provides some 400,000 years of history. But a core extending beyond 300,000 years becomes highly compressed at its base, making information difficult to extract, the scientists say.
 
Turning to terrestrial rocks offers an easier, and sometimes warmer, method for reading the longer story about Earth’s air. Reporting in the Aug. 4 Science, James Farquhar, Huiming Bao and Thiemens pried atmospheric secrets out of 3.8 billion-year-old rocks from Greenland; 3.4 billion-year-old rocks from Australia and South Africa; and 700 million-year-old rocks from Australia, China, Africa, Canada and the United States. 

Farquhar and colleagues found multiple isotope variations of a kind only recently considered possible in terrestrial solids: anomalous sulfur ratios incorporated into the rocks after the rocks oxidize in air. Their discovery pointed to a profound change in the sulfur cycle between 2.1 billion and 2.5 billion years ago, a time when Earth’s atmosphere is known to have shifted from primitive, oxygen-poor conditions to an oxygen-rich environment more like today’s. 


  Huiming Bao hard at work at the University of California, 
  San Diego. Photo courtesy of James Farquhar.
 
How much oxygen first flooded the skies is still up for debate and Farquhar is investigating whether the change in the sulfur cycle will offers clues. “We have to figure out what the atmospheric reaction was that produced the effect,” he says.
 
Their research indicates that before  2.5 billion years ago, oxidation of sulfur-bearing gases, which later incorporated into the sulfur and sulfide minerals in the rocks, mainly originated from the limited oxygen in the atmosphere.
 
During the critical period when oxygen and ozone began accumulating, the sulfur cycle began to favor a varied contribution relying more on continental oxidated weathering and microbial sulfate reduction.
 
In the past, scientists thought they could analyze a few stable isotopes and then mathematically determine other isotope relationships. Harold Urey first established these linear relationships in 1947, but it soon became clear that isotopes in nuclear synthetic reactions broke the rule.
 
Then in the 1970s, Robert Clayton of the University of Chicago found meteorites that also showed signs of disobedience. And in 1983 Thiemens showed Earth’s atmosphere included an exception — ozone contains excess oxygen-17 in comparison to what would be expected.
 
Following the ozone trail, Huiming Bao studied compounds such as dimethyl sulfide from the oceans and sulfur dioxide from volcanoes, which could be oxidized in the atmosphere and become branded with the excess oxygen-17. He discovered these sulfur-bearing atmospheric compounds became ingrained in the minerals of young sulfate rocks from the Namib Desert in Namibia and Miocene volcanic ash beds from the western United States. He and colleagues reported the first geologic link to these rare anomalies in the July 13  Nature.
 
Although, as Clayton says, the  two reports “have barely scratched the surface,” he believes the measurements offer geochemists a new tool for atmospheric research.
 
“We don’t really have very good fossil records of what atmospheric chemistry was like in the past,” he says. Using the anomalous isotopes is “a new way of getting a handle on the chemical evolution of the atmosphere.”

Christina Reed

Geotimes Home | AGI Home | Information Services | Geoscience Education | Public Policy | Programs | Publications | Careers

© 2014 American Geological Institute. All rights reserved. Any copying, redistribution or retransmission of any of the contents of this service without the express written consent of the American Geological Institute is expressly prohibited. For all electronic copyright requests, visit: http://www.copyright.com/ccc/do/showConfigurator?WT.mc_id=PubLink