Newfound Bacteria Fueled by Radiation

First, water molecules -- H2O -- are split by radioactive particles. The result is hydrogen, oxygen and hydrogen peroxide. The latter two substances then attack the mineral pyrite (also known as iron sulfide or "fool's gold"), making sulfate through a process called oxidation.

The bacteria then uses the hydrogen to turn the sulfate back to sulfide, a process known as reduction. In doing so, it captures some of the energy in the sulfate's chemical bonds, which it uses to make ATP, the molecule that is the universal coin of energy exchange in living things.

Radiation then splits more water, producing more hydrogen peroxide, which turns the sulfide back to sulfate, effectively "recharging the battery."

The deep underground water where the bacteria live is loaded with these nutrients. But the exceedingly torpid organisms are using only a fraction -- perhaps as little as one-billionth -- of what is available to them. They live 45 to 300 years between cell divisions; in comparison, some strains of E. coli bacteria can divide every 20 minutes under ideal conditions.

"For some reason it is advantageous to grow slow rather than fast in this environment," said Lisa M. Pratt, a geologist and astrobiologist at Indiana University, who is one the authors of the Science paper.

"Philosophically, that is very interesting, because on the surface it is advantageous to grow fast and use nutrients before something else does," she added.

All of the microbes are members of the phylum Firmicutes . One strain dominates, and there are a few others.

The dominant bacterium does not yet have a scientific name. Some of the researchers have almost finished reading its entire genome, which will allow them to figure out how closely related it is to Firmicutes found elsewhere. A study published last winter established that large phylum as unusually ancient -- it was the first branch after the common ancestor of all bacteria, which emerged about 3.5 billion years ago, according to the fossil record.

A chief obstacle in research on deep-subsurface microbial communities is proving that what people find was not carried in by them, their equipment or the drilling apparatus.

This team -- which included American, Taiwanese, German and South African scientists -- showed that none of the microbes they found were like ones found in surface water near the mine.

They also dated the water by measuring the amount of helium in it. Helium is produced by radioactive decay, and thus is evidence of how long the water had been underground. It appears to be a mixture of water that came from the surface as recently as 3 million years ago, mingled with water already there from 2.5 billion years ago.

"They did a nice job of constraining and characterizing the environment of that system," said James K. Fredrickson, a geomicrobiologist at Pacific Northwest National Laboratory in Richland, Wash., who was not on the team.

The research was principally done by Li-Hung Lin, a former graduate student of Onstott's who is now on the faculty of National Taiwan University.

He descended three times to the part of the tunnel where the fissure was hit to get samples. It was 1.7 miles underground, and the temperature of the rock was 125 degrees Fahrenheit.