A team of scientists, led by the University of Toronto's Barbara Sherwood Lollar, has mapped the location of hydrogen-rich waters found trapped kilometres beneath Earth's surface in rock fractures in Canada, South Africa and Scandinavia. Common in Precambrian Shield rocks -- the oldest rocks on Earth -- the ancient waters have a chemistry similar to that found near deep sea vents¹, suggesting these waters can support microbes living in isolation² from the surface.

 

The study, to be published in Nature on December 18, includes data from 19 different mine sites that were explored by Sherwood Lollar, a geoscientist at U of T's Department of Earth Sciences, U of T senior research associate Georges Lacrampe-Couloume, and colleagues at Oxford³ and Princeton universities.

 

The scientists also explain how two chemical reactions combine to produce substantial quantities of hydrogen, doubling estimates of global production from these processes which had previously⁴ been based only on hydrogen coming out of the ocean floor.

 

"This represents a quantum change in our understanding of the total volume of Earth's crust that may be habitable," said Sherwood Lollar.

 

"Until now, none of the estimates of global hydrogen production sustaining deep microbial populations had included a contribution from the ancient continents. Since Precambrian rocks make up more than 70 per cent of the surface of Earth's crust, Sherwood Lollar likens these terrains⁵ to a "sleeping giant," a huge area that has now been discovered to be a source of possible energy for life," she said.

 

One process, known as radiolytic decomposition⁶ of water, involves water undergoing a breakdown⁷ into hydrogen when exposed to radiation. The other is a chemical reaction called serpentization, a mineral alteration⁸ reaction that is common in such ancient rocks.

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