U. MICHIGAN (US) — Beads of liquid brine may open the door to the possibility of microbial life on Mars, according to an international study.
The beads were photographed three years ago on one of the Phoenix lander’s legs.
“On Earth, everywhere there’s liquid water, there is microbial life,” says Nilton Renno, professor of atmospheric, oceanic and space sciences who is the principal investigator at the University of Michigan.
Scientists in the U.S. will create Mars conditions in lab chambers to study how and when brines form. The shoe-box-sized modules will have wispy carbon dioxide and water vapor atmospheres with 99 percent lower air pressure than the average pressure on Earth at sea level.
Temperatures will range from -100 to -80 Fahrenheit and will be adjusted to mimic daily and seasonal cycles. Instruments will alert the researchers to the formation of brine pockets, which could potentially be habitable by certain forms of microbial life.
Their colleagues overseas will seed similar chambers with salt-loving “extremophile” microorganisms from deep in Antarctic lakes and the Gulf of Mexico to observe whether the organisms survive, grow, and reproduce in brines just below the surface of the soil.
All known forms of life need liquid water to live. But microbes don’t need much. A droplet or a thin film could suffice, researchers say.
“If we find microbes that can survive and replicate in brines at Mars conditions, we would have demonstrated that microbes could exist on Mars today,” Renno says.
With his colleagues on the Mars Phoenix mission in 2008, Renno theorized that globules that moved and coalesced on the spacecraft’s leg were liquid saltwater. Independent physical and thermodynamic evidence as well as follow-up experiments have confirmed that the drops were liquid and not frost or ice. The Phoenix photos are believed to be the first pictures of liquid water outside the Earth.
The median temperature at the Phoenix landing site was -70 degrees Fahrenheit during the mission—too cold for liquid fresh water. But “perchlorate” salts found in the site’s soils could lower water’s freezing point dramatically, so that it could exist as liquid brine.
The salts are also capable of absorbing water from the atmosphere in a process called deliquescence.
Researchers from NASA, the University of Texas at Dallas, the University of Georgia, and the Centro de Astrobiologia in Madrid are also involved.
More news from University of Michigan: www.ns.umich.edu/