The six-wheeled geologist found a
fascinating rock that has some indications it may have hosted microbial life
billions of years ago, but further research is needed.
A vein-filled rock is catching the eye
of the science team of NASA’s Perseverance rover. Nicknamed “Cheyava Falls” by
the team, the arrowhead-shaped rock contains fascinating traits that may bear
on the question of whether Mars was home to microscopic life in the distant
past.
Analysis by instruments aboard the rover
indicates the rock possesses qualities that fit the definition of a possible
indicator of ancient life. The rock exhibits chemical signatures and structures
that could possibly have been formed by life billions of years ago when the
area being explored by the rover contained running water. Other explanations
for the observed features are being considered by the science team, and future
research steps will be required to determine whether ancient life is a valid explanation.
The rock — the rover’s 22nd rock core sample — was collected on July 21, as the rover explored the northern edge of Neretva Vallis, an ancient river valley measuring a quarter-mile (400 meters) wide that was carved by water rushing into Jezero Crater long ago.
“We have designed the route for
Perseverance to ensure that it goes to areas with the potential for interesting
scientific samples,” said Nicola Fox, associate administrator, Science Mission
Directorate at NASA Headquarters in Washington. “This trip through the Neretva
Vallis riverbed paid off as we found something we’ve never seen before, which
will give our scientists so much to study.”
Multiple scans of Cheyava Falls by the
rover’s SHERLOC (Scanning Habitable Environments with Raman & Luminescence for
Organics & Chemicals) instrument indicate it contains organic compounds.
While such carbon-based molecules are considered the building blocks of life,
they also can be formed by non-biological processes.
“Cheyava Falls is the most puzzling, complex, and potentially important rock yet investigated by Perseverance,” said Ken Farley,Perseverance project scientist of Caltech in Pasadena. “On the one hand, we have our first compelling detection of organic material, distinctive colorful spots indicative of chemical reactions that microbial life could use as an energy source, and clear evidence that water — necessary for life — once passed through the rock. On the other hand, we have been unable to determine exactly how the rock formed and to what extent nearby rocks may have heated Cheyava Falls and contributed to these features.”
NASA’s Perseverance rover used its Mastcam-Z instrument to capture this 360-degree panorama of a region on Mars called “Bright Angel,” where an ancient river flowed billions of years ago. “Cheyava Falls” was discovered in the area slightly right of center, about 361 feet (110 meters) from the rover. NASA/JPL-Caltech/ASU/MSSS
Other details about the rock, which measures 3.2 feet by 2 feet (1 meter by
0.6 meters) and was named after a Grand Canyon waterfall, have intrigued the
team, as well.
How Rocks Get
Their Spots
In its search for signs of ancient
microbial life, the Perseverance mission has focused on rocks that may have
been created or modified long ago by the presence of water. That’s why the team
homed in on Cheyava Falls.
“This is the kind of key
observation that SHERLOC was built for — to seek organic matter as it is an
essential component of a search for past life,” said SHERLOC’s principal
investigator Kevin Hand of NASA’s Jet Propulsion Laboratory in Southern
California, which manages the mission.
Running the length of the rock are
large white calcium sulfate veins. Between those veins are bands of material
whose reddish color suggests the presence of hematite, one of the minerals that
gives Mars its distinctive rusty hue.
When Perseverance took a closer look at these red regions, it found dozens of irregularly shaped, millimeter-size off-white splotches, each ringed with black material, akin to leopard spots. Perseverance’s PIXL (Planetary Instrument for X-ray Lithochemistry) instrument has determined these black halos contain both iron and phosphate.
As shown in this graphic, astrobiologists catalog a seven-step scale, called the CoLD (Confidence of Life Detection) scale, to research whether a sample could indicate life. This “Cheyava Falls” sample is an example of Step One: “Detect possible signal.” Much additional research must be conducted to learn more. NASA/Aaron Gronstal
“These spots are a big surprise,” said David Flannery, an astrobiologist
and member of the Perseverance science team from the Queensland University of
Technology in Australia. “On Earth, these types of features in rocks are often
associated with the fossilized record of microbes living in the subsurface.”
Spotting of this type on
sedimentary terrestrial rocks can occur when chemical reactions involving
hematite turn the rock from red to white. Those reactions can also release iron
and phosphate, possibly causing the black halos to form. Reactions of this type
can be an energy source for microbes, explaining the association between such
features and microbes in a terrestrial setting.
In one scenario the Perseverance science team is considering, Cheyava Falls was initially deposited as mud with organic compounds mixed in that eventually cemented into rock. Later, a second episode of fluid flow penetrated fissures in the rock, enabling mineral deposits that created the large white calcium sulfate veins seen today and resulting in the spots.
NASA’s Perseverance rover has made very
compelling observations in a Martian rock that, with further study, could prove
that life was present on Mars in the distant past — but how can we determine
that from a rock, and what do we need to do to confirm it?
Morgan Cable, a scientist on the Perseverance team, takes a closer look.
Credit: NASA/JPL-Caltech
Another Puzzle
Piece
While both the organic matter and
the leopard spots are of great interest, they aren’t the only aspects of the
Cheyava Falls rock confounding the science team. They were surprised to find
that these veins are filled with millimeter-size crystals of olivine, a mineral
that forms from magma. The olivine might be related to rocks that were formed
farther up the rim of the river valley and that may have been produced by
crystallization of magma.
If so, the team has another
question to answer: Could the olivine and sulfate have been introduced to the
rock at uninhabitably high temperatures, creating an abiotic chemical reaction
that resulted in the leopard spots?
“We have zapped that rock with
lasers and X-rays and imaged it literally day and night from just about every
angle imaginable,” said Farley. “Scientifically, Perseverance has nothing more
to give. To fully understand what really happened in that Martian river valley
at Jezero Crater billions of years ago, we’d want to bring the Cheyava Falls
sample back to Earth, so it can be studied with the powerful instruments
available in laboratories.”
More Mission
Information
A key objective of Perseverance’s
mission on Mars is astrobiology, including caching samples that may contain signs of
ancient microbial life. The rover will characterize the planet’s geology and
past climate, to help pave the way for human exploration of the Red Planet and
as the first mission to collect and cache Martian rock and regolith.
NASA’s Mars Sample Return Program,
in cooperation with ESA (European Space Agency), is designed to send spacecraft
to Mars to collect these sealed samples from the surface and return them to
Earth for in-depth analysis.
The Mars 2020 Perseverance mission
is part of NASA’s Moon to Mars exploration approach, which includes Artemis missions to the Moon that will help prepare for
human exploration of the Red Planet.
NASA’s Jet Propulsion Laboratory,
which is managed for the agency by Caltech, built and manages operations of the
Perseverance rover.
For more about Perseverance:
science.nasa.gov/mission/mars-2020-perseverance
Source: NASA’s
Perseverance Rover Scientists Find Intriguing Mars Rock - NASA
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