UIC scientists find ancient microbes in salty, ice-sealed Antarctic lake

The finding, described in this week's issue of the Proceedings of the National Academy of Sciences, is surprising because previous studies indicate that the brine has been isolated from the surface environment — and external sources of energy — for at least 2,800 years, according to two of the report's authors, Peter Doran and Fabien Kenig, both professors of earth and environmental sciences at the University of Illinois at Chicago.

“This provides us with new boundary conditions on the limits for life,” said Doran. “The low temperature or high salinity on their own are limiting, but combined with an absence of solar energy or any new inputs from the atmosphere, they make this a very tough place to make a living.”

The researchers drilled out cores of ice, using sanitary procedures and equipment. They collected samples of brine within the ice and assessed its chemical qualities and potential for sustaining life.

They found that the brine is oxygen-free, slightly acidic, and contains high levels of organic carbon, molecular hydrogen, and both oxidized and reduced compounds. The findings were unexpected because of the extremely salty, dark, cold, isolated ecosystem within the ice.

“Geochemical analyses suggest that chemical reactions between the brine and the underlying sediment generate nitrous oxide and molecular hydrogen,” said Kenig. “The hydrogen may provide some of the energy needed to support microbes.”

“We'd like to go back and find if there is a proper body of brine without ice down there,” said Doran. “We'd also like to get some sediment cores from below that to better establish the history of the lake. In the meantime, we are using radar and other geophysical techniques to probe what lies beneath.”

The research was conducted with Alison Murray and colleagues at the Desert Research Institute and scientists at other institutes.

Funding was provided by the National Science Foundation and NASA.

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