Wednesday, June 17, 2009
A University of Colorado at Boulder
research team has discovered the first definitive evidence of shorelines on
Mars, an indication of a deep, ancient lake there and a finding with
implications for the discovery of past life on the Red Planet.
Estimated
to be more than 3 billion years old, the lake appears to have covered as much as
80 square miles and was up to 1,500 feet deep -- roughly the equivalent of Lake
Champlain bordering the United States and Canada, said CU-Boulder Research
Associate Gaetano Di Achille, who led the study. The shoreline evidence, found
along a broad delta, included a series of alternating ridges and troughs thought
to be surviving remnants of beach deposits.
"This is the first
unambiguous evidence of shorelines on the surface of Mars," said Di Achille.
"The identification of the shorelines and accompanying geological evidence
allows us to calculate the size and volume of the lake, which appears to have
formed about 3.4 billion years ago."
A paper on the subject by Di
Achille, CU-Boulder Assistant Professor Brian Hynek and CU-Boulder Research
Associate Mindi Searls, all of the Laboratory for Atmospheric and Space Physics,
has been published online in Geophysical Research Letters, a publication of the
American Geophysical Union.
Images used for the study were taken by a
high-powered camera known as the High Resolution Imaging Science Experiment, or
HiRISE. Riding on NASA's Mars Reconnaissance Orbiter, HiRISE can resolve
features on the surface down to one meter in size from its orbit 200 miles above
Mars.
An analysis of the HiRISE images indicate that water carved a
30-mile-long canyon that opened up into a valley, depositing sediment that
formed a large delta. This delta and others surrounding the basin imply the
existence of a large, long-lived lake, said Hynek, also an assistant professor
in CU-Boulder's geological sciences department. The lake bed is located within a
much larger valley known as the Shalbatana Vallis.
"Finding shorelines
is a Holy Grail of sorts to us," said Hynek.
In addition, the evidence
shows the lake existed during a time when Mars is generally believed to have
been cold and dry, which is at odds with current theories proposed by many
planetary scientists, he said. "Not only does this research prove there was a
long-lived lake system on Mars, but we can see that the lake formed after the
warm, wet period is thought to have dissipated."
Planetary scientists
think the oldest surfaces on Mars formed during the wet and warm Noachan epoch
from about 4.1 billion to 3.7 billion years ago that featured a bombardment of
large meteors and extensive flooding. The newly discovered lake is believed to
have formed during the Hesperian epoch and postdates the end of the warm and wet
period on Mars by 300 million years, according to the study.
The deltas
adjacent to the lake are of high interest to planetary scientists because deltas
on Earth rapidly bury organic carbon and other biomarkers of life, according to
Hynek. Most astrobiologists believe any present indications of life on Mars will
be discovered in the form of subterranean microorganisms.
But in the
past, lakes on Mars would have provided cozy surface habitats rich in nutrients
for such microbes, Hynek said.
The retreat of the lake apparently was
rapid enough to prevent the formation of additional, lower shorelines, said Di
Achille. The lake probably either evaporated or froze over with the ice slowly
turning to water vapor and disappearing during a period of abrupt climate
change, according to the study.
Di Achille said the newly discovered
pristine lake bed and delta deposits would be would be a prime target for a
future landing mission to Mars in search of evidence of past life.
"On
Earth, deltas and lakes are excellent collectors and preservers of signs of past
life," said Di Achille. "If life ever arose on Mars, deltas may be the key to
unlocking Mars' biological past."
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University of Colorado at
Boulder
Thanks to University of Colorado at Boulder for this article.