Do you believe there was past life on Mars? Here’s what new NASA evidence indicates.
Dry, cold and barren.
Mars doesn’t seem like a haven for life—at least not the kind humans are
familiar with.
Scientists have
wondered for decades if microbial life could have inhabited Mars in the distant
past. One study, based on data collected by NASA’s Curiosity rover, is peeling
back a layer of the mystery. Researchers measured the isotopic composition of
carbon-rich minerals found in Gale Crater. This region is laced with dried
rivers and gullies and was explored by the rover.
The findings Curiosity
sent to Earth were not optimistic about the potential for life above ground.
But that doesn’t rule out the possibility of an underground biosphere or even a
surface biosphere that began and ended before the carbonates were formed.
This suggests two
possible ways carbon-rich minerals could have form at Gale crater: a series of
alternating wet and dry periods or salty-ice conditions. These two climate
scenarios could be called ‘bleak’ and ‘bleaker’ when it comes to supporting
life.
In an environment that
swings from wet to dry, the region would shift from more habitable to less
habitable. In the frigid temperatures near Mars’ equator, that environment
would be hostile for life because most water would be frozen and inaccessible
for chemistry or biology. Plus, what water was there was extremely salty, not
pleasant for life.
This isn’t the first
time scientists have theorized these climate scenarios for ancient Mars.
Previous computer models have indicated these conditions before, but now they
have isotopic evidence from Martian rocks.
Scientists have sought
life on Mars since the first spacecraft touched down there in 1976. Mounting
evidence from robotic explorers has shown the Red Planet to have been warmer
and wetter, perhaps more than 3 billion years ago.
The Perseverance rover discovered
a spotted rock with compelling signs of ancient dead Martian life, but a sample
would need to be shipped to Earth for confirmation. A research team also
reported evidence of a vast ocean of water below the planet’s surface. On
Earth, where there’s water, there’s often life.
Scientists are
interested in Mars’ carbon-rich rocks because they can hold clues about the
environment in which they formed, such as the temperature and acidity of the
water, and ingredients in the water and air.
The sampled rocks
indicate lots of evaporation, suggesting a climate that could only support
transient liquid water—that is, ice that melts when temperatures rise and the
surface pressure is right.
The heavy isotope
values in the rocks are much higher than what’s seen on Earth. They are the
heaviest carbon and oxygen isotope values recorded for any Martian materials.
Although evaporation can cause oxygen isotope changes on Earth, the changes in
the Martian samples were two to three times greater.
But this doesn’t negate
the possibility of life. Mars has a network of deep caves formed by ancient
volcanic vents. Within the caves could be liquid water, traces of long-deceased
bacteria or fungi, or perhaps even existing microbial life.
Caves can host complex
ecosystems, including extremophiles that munch on rocks and convert the
material into energy for life. So, many astrobiologists want to go spelunking
on Mars. Would you like to join them?
https://www.msn.com/en-us/news/technology/past-life-on-mars-here-s-what-new-nasa-evidence-points-to/ar-AA1rWIgJ?ocid=hpmsn&cvid=5432d20e554e4f3ea664d26edcf277ee&ei=74