Researchers detected extensive salty groundwater networks in Antarctica using a novel airborne electromagnetic mapping sensor system called SkyTEM.
The research provides compelling evidence that the underground lakes and brine-saturated sediments may support subsurface microbial ecosystems.
The findings allow scientists to better learn how Antarctica has responded to climate change over time and help them understand glacial dynamics.
"It may change the way people think about the coastal margins of Antarctica," said Jill Mikucki, a University of Tennessee, Knoxville, microbiology assistant professor.
The researchers believe the newly discovered brines harbour similar microbial communities in the deep, cold dark groundwater.
The brines may provide insight on how microbes survive such extreme conditions. They also may provide the basis for future exploration of a subsurface habitat on Mars.
Mikucki and the international interdisciplinary team used the airborne sensor to produce extensive imagery of the subsurface of the coldest, driest desert on earth, the McMurdo Dry Valleys in Antarctica.
The airborne sensor technology was developed at the University of Aarhus in Denmark and was used in Antarctica for the first time during this study.
The study was published in the journal Nature Communications.
