This 360-degree mosaic from the “Airey Hill” location inside Jezero Crater was generated using 993 individual images taken by the Perseverance Mars rover’s Mastcam-Z from Nov. 3-6. The rover remained parked at Airey Hill for several weeks during solar conjunction. NASA/JPL-Caltech/ASU/MSSS
Now at 1,000 days on Mars, the mission has traversed an ancient river and
lake system, collecting valuable samples along the way.
Marking its 1,000th Martian day on
the Red Planet, NASA’s Perseverance rover recently completed its exploration of
the ancient river delta that holds evidence of a lake that filled Jezero Crater
billions of years ago. The six-wheeled scientist has to date collected a total
of 23
samples, revealing
the geologic history of this region of Mars in the process.
One sample called “Lefroy Bay”
contains a large quantity of fine-grained silica, a material known to preserve
ancient fossils on Earth. Another, “Otis Peak,” holds a significant amount of
phosphate, which is often associated with life as we know it. Both of these
samples are also rich in carbonate, which can preserve a record of the
environmental conditions from when the rock was formed.
The discoveries were shared
Tuesday, Dec. 12, at the American Geophysical Union fall meeting in San
Francisco.
“We picked Jezero Crater as a
landing site because orbital imagery showed a delta – clear evidence that a
large lake once filled the crater. A lake is a potentially habitable
environment, and delta rocks are a great environment for entombing signs of ancient
life as fossils in the geologic record,” said Perseverance’s project scientist,
Ken Farley of Caltech. “After thorough exploration, we’ve pieced together the
crater’s geologic history, charting its lake and river phase from beginning to
end.”
This image of Mars’ Jezero Crater is overlaid with mineral data detected from orbit. The green color represents carbonates – minerals that form in watery environments with conditions that might be favorable for preserving signs of ancient life. NASA’s Perseverance is currently exploring the green area above Jezero’s fan (center). NASA/JPL-Caltech/MSSS/JHU-APL
Jezero formed from an asteroid impact almost 4 billion years ago. After
Perseverance landed in February 2021, the mission team discovered the crater
floor is made of igneous rock formed from magma underground or from volcanic activity at the
surface. They have since found sandstone and mudstone, signaling the arrival of
the first river in the crater hundreds of millions of years later. Above these
rocks are salt-rich mudstones, signaling the presence of a shallow lake
experiencing evaporation. The team thinks the lake eventually grew as wide as
22 miles (35 kilometers) in diameter and as deep as 100 feet (30 meters).
Later, fast-flowing water carried
in boulders from outside Jezero, distributing them atop of the delta and elsewhere in the crater.
“We were able to see a broad
outline of these chapters in Jezero’s history in orbital images, but it
required getting up close with Perseverance to really understand the timeline
in detail,” said Libby Ives, a postdoctoral fellow at NASA’s Jet Propulsion
Laboratory in Southern California, which manages the mission.
Enticing
Samples
The samples Perseverance gathers are about as big as a piece of classroom chalk and are stored in special metal tubes as part of the Mars Sample Return campaign, a joint effort by NASA and ESA (European Space Agency). Bringing the tubes to Earth would enable scientists to study the samples with powerful lab equipment too large to take to Mars.
This animated artist’s concept depicts water
breaking through the rim of Mars’ Jezero Crater, which NASA’s Perseverance
rover is now exploring. Water entered the crater billions of years ago, forming
a lake, delta, and rivers before the Red Planet dried up. NASA/JPL-Caltech
To decide which samples to collect,
Perseverance first uses an abrasion tool to wear away a patch of a prospective
rock and then studies the rock’s chemistry using precision science instruments,
including the JPL-built Planetary Instrument for X-ray Lithochemistry, or PIXL.
At a target the team calls “Bills
Bay,” PIXL spotted carbonates – minerals that form in watery environments with
conditions that might be favorable for preserving organic molecules. (Organic
molecules form by both geological and biological processes.) These rocks were
also abundant with silica, a material that’s excellent at preserving organic
molecules, including those related to life.
“On Earth, this fine-grained silica
is what you often find in a location that was once sandy,” said JPL’s Morgan
Cable, the deputy principal investigator of PIXL. “It’s the kind of environment
where, on Earth, the remains of ancient life could be preserved and found
later.”
Perseverance’s instruments are capable of detecting both microscopic, fossil-like structures and chemical changes that may have been left by ancient microbes, but they have yet to see evidence for either.
At another target PIXL examined, called “Ouzel Falls,” the instrument
detected the presence of iron associated with phosphate. Phosphate is a
component of DNA and the cell membranes of all known terrestrial life and is
part of a molecule that helps cells carry energy.
After assessing PIXL’s findings on
each of these abrasion patches, the team sent up commands for the rover to
collect rock cores close by: Lefroy Bay was collected next to Bills Bay, and
Otis Peak at Ouzel Falls.
“We have ideal conditions for
finding signs of ancient life where we find carbonates and phosphates, which
point to a watery, habitable environment, as well as silica, which is great at
preservation,” Cable said.
Perseverance’s work is, of course,
far from done. The mission’s ongoing fourth science campaign will explore
Jezero Crater’s margin, near the canyon entrance where a river once flooded the
crater floor. Rich carbonate deposits have been spotted along the margin, which
stands out in orbital images like a ring within a bathtub.
More About the
Mission
A key objective for Perseverance’s
mission on Mars is astrobiology, including the search for signs of ancient microbial
life. The rover will characterize the planet’s geology and past climate, pave
the way for human exploration of the Red Planet, and be the first mission to
collect and cache Martian rock and regolith (broken rock and dust).
Subsequent NASA missions, in
cooperation with ESA (European Space Agency), would 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.
JPL, which is managed for NASA by
Caltech in Pasadena, California, built and manages operations of the
Perseverance rover.
For more about Perseverance: mars.nasa.gov/mars2020/
Source: NASA’s Perseverance Rover Deciphers Ancient History of Martian Lake - NASA
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