NASA's Mars Research at Mono Lake
Click here for some info and links on October 2010 Mars rover tests at Mono Lake, and a NASA press release on the 2010 discovery of bacteria that can grow using arsenic in place of phosphorus. The following article was written in 1996 and updated in 2003, with a photo added in 2010.
Click on footnotes -- 1 -- to see
the notes at the bottom of the profiles. Click on words
in italics to see the definition in the glossary.
In 1976,
Viking landers sent to Mars analyzed soil samples and
found no conclusive evidence that life had existed there.
However, water once flowed freely on Mars, it might have
had a thicker atmosphere, and the temperatures that
occurred there didn't rule out life.1
In order to figure out where the next Mars probe
should look for evidence of life, NASA scientists looked
at where they could find evidence of life on Earth.
Fossils of 3.5-billion-year-old microbes have been found
on Earth, but they are rare. On Mars, however, fossils
would not have been destroyed by the heat and pressure of
plate tectonics, therefore probes looking in the right
spot might have a better chance of finding them, if they
do exist.2
Calcium carbonate precipitating out of water often
traps microbes, a process which occurs at Mono Lake, and
might have occurred on Mars.3
Mars also has basins which likely held lakes like Mono
Lake, which contains hydrothermal
vents. Upwellings like these of volcanically heated water
from the ocean floor are thought by scientists to be a
possible place where bacteria developed.4
"There is strong evidence that all life on Earth
evolved from such bacteria and that life's origins trace
back to hydrothermal vents," stated Carol Stoker,
the project director.5
In August 1995, researchers from the Monterey Bay
Aquarium Research Institute, the Navy Postgraduate School
(involved because of Navy research on improving
underwater minefield surveillance), Stanford University,
and project director Carol Stoker from NASA Ames Research
Center all converged on Mono Lake. From a houseboat they
operated a Telepresence
Controlled Remotely Operated Vehicle (TROV) equipped
with 1000 feet of cable, a state of the art high
frequency sonar system, stereoscopic cameras, an acoustic
positioning system, and a sample grabbing arm. Something
like TROV will travel to Mars perhaps as early as 2003,
so bugs were being worked out first here on earth.6
Visibility was only about one foot, the murkiest the
researchers had ever seen, and the chemical quality of
the water reduced the sonar range from 30 meters to 2
meters. Tufa
samples were taken from the bases of tufa towers, and
were analyzed over the next few months to see how well
they preserved microbes.7
A three step strategy to recover fossils from Mars,
developed by paleontologist Jack Farmer, also with NASA
Ames Research Center, is to (1) identify likely sites
from an orbiting spacecraft, (2) drop a lander at these
sites to find fossil-bearing rocks, and (3) send a probe
to retrieve rock samples for firsthand studies on Earth.
To assist in the first step, in 1996 an aircraft was
flown at high altitude above Yellowstone National Park
and other hot spring sites to determine how well infrared
cameras could pick out silica, iron, and carbonate
deposits formed by the springs.8
Also helping with step one was the Mars Observer,
which was going to map the surface of Mars, but went mute
in August 1993 when it was about to enter into Mars
orbit. The next mission to Mars, the beginning of step 2,
launched in December 1996, and parachuted to Mars'
surface on July 4, 1997. This $170 million Mars Pathfinder
mission landed on giant airbags and released a
2-foot-long rover to explore the surface in a 30-foot
radius. It landed on Ares Vallis, an expansive plain with
different rock types funneled over it by ancient floods.9
The Mars Surveyor program is NASA's plan to send a
low-cost orbital probe and lander to Mars every 2 years until 2006.
NASA's Mars rover Spirit will land in
the Gusev Crater on Mars in 2004. It's unlikely that any microbes
are alive in Gusev Crater now, but their fossils might be there. A good
place to look would be inside evaporated mineral deposits or tufa
towers, if the crater has any.
Scientists recently
have grown bacteria that were trapped in 200 million year-old Miocene salt
crystals--another way to look for evidence of past life on Mars. This
was first done with Cambrian and Devonian salt crystals in 1962, but was
not widely accepted and the author of the paper was fired.
Richard B. Hoover, NASA microbiologist, has
discovered bacteria fossils inside meteorites. He has been looking at
varnishes on rocks as well. In his search for life in extreme environments,
Hoover found 3 new species of bacteria in Mono Lake from mud and water
samples he collected in September 2000: Spirochaeta
americana (also in Owens Lake), Tindallia californiensis, and
Desulfonatronum thiodismutans. The last is responsible for the
sulfur smell in Mono Lake's mud. Hoover wanted to name it paiutaeum
(after the Mono Lake Kutzadika'a Paiute Indians), however in the peer
review it was pointed out that you can't name a species after a group of
people--hence thiodismutans.
Notes:
(1)Cole, Richard, Associated Press, NASA
Probes Mono Lake to Find Clues to Life on Mars, Los
Angeles Times, October 8, 1995
(2)p. 129, Blake Edgar, Jack Farmer, Exopaleontologist,
Discover, October 1995
(3)p. 129, Blake Edgar, Jack Farmer, Exopaleontologist,
Discover, October 1995
(4)Cole, Richard, Associated Press, NASA Probes Mono
Lake to Find Clues to Life on Mars, Los Angeles
Times, October 8, 1995
(5)Quoted in Cole, Richard, Associated Press, NASA
Probes Mono Lake to Find Clues to Life on Mars, Los
Angeles Times, October 8, 1995
(6)Cole, Richard, Associated Press, NASA Probes Mono
Lake to Find Clues to Life on Mars, Los Angeles
Times, October 8, 1995
(7)Cole, Richard, Associated Press, NASA Probes Mono
Lake to Find Clues to Life on Mars, Los Angeles
Times, October 8, 1995
(8)p. 129, Blake Edgar, Jack Farmer, Exopaleontologist,
Discover, October 1995
(9)p. 129, Blake Edgar, Jack Farmer, Exopaleontologist,
Discover, October 1995
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