NASA’s Curiosity Mars rover sees its tracks receding
into the distance at a site nicknamed “Ubajara” on April 30, 2023. This site is
where Curiosity made the discovery of siderite, a mineral that may help explain
the fate of the planet’s thicker ancient atmosphere.
Credit: NASA/JPL-Caltech/MSSS
New findings from NASA’s Curiosity Mars rover could provide an answer to
the mystery of what happened to the planet’s ancient atmosphere and how Mars
has evolved over time.
Researchers have long believed that
Mars once had a thick, carbon dioxide-rich atmosphere and liquid water on the
planet’s surface. That carbon dioxide and water should have reacted with
Martian rocks to create carbonate minerals. Until now, though, rover missions
and near-infrared spectroscopy analysis from Mars-orbiting satellites haven’t
found the amounts of carbonate on the planet’s surface predicted by this
theory.
Reported in an April paper in Science, data from three of Curiosity’s drill sites revealed
the presence of siderite, an iron carbonate mineral, within the sulfate-rich rocky layers of Mount Sharp in Mars’ Gale Crater.
“The discovery of abundant siderite
in Gale Crater represents both a surprising and important breakthrough in our
understanding of the geologic and atmospheric evolution of Mars,” said Benjamin
Tutolo, associate professor at the University of Calgary, Canada, and lead
author of the paper.
To study the Red Planet’s chemical
and mineral makeup, Curiosity drills three to four centimeters down into the
subsurface, then drops the powdered rock samples into its CheMin instrument.
The instrument, led by NASA’s Ames Research Center in California’s Silicon
Valley, uses X-ray diffraction to analyze rocks and soil. CheMin’s data was
processed and analyzed by scientists at the Astromaterials Research and
Exploration Science (ARES) Division at NASA’s Johnson Space Center in Houston.
“Drilling through the layered
Martian surface is like going through a history book,” said Thomas Bristow,
research scientist at NASA Ames and coauthor of the paper. “Just a few
centimeters down gives us a good idea of the minerals that formed at or close
to the surface around 3.5 billion years ago.”
The discovery of this carbonate
mineral in rocks beneath the surface suggests that carbonate may be masked by
other minerals in near-infrared satellite analysis. If other sulfate-rich
layers across Mars also contain carbonates, the amount of stored carbon dioxide
would be a fraction of that needed in the ancient atmosphere to create
conditions warm enough to support liquid water. The rest could be hidden in
other deposits or have been lost to space over time.
In the future, missions or analyses
of other sulfate-rich areas on Mars could confirm these findings and help us
better understand the planet’s early history and how it transformed as its
atmosphere was lost.
Curiosity, part of NASA’s Mars
Exploration Program (MEP) portfolio, was built by NASA’s Jet Propulsion
Laboratory, which is managed by Caltech in Pasadena, California. JPL leads the
mission on behalf of NASA’s Science Mission Directorate in Washington.
For more information on Curiosity, visit: https://science.nasa.gov/mission/msl-curiosity
Source: NASA’s Curiosity Rover May Have Solved Mars' Missing Carbonate Mystery - NASA
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