This story is a part of Welcome to Mars, our sequence exploring the pink planet.
There is a rising sense of pleasure round NASA’s future Mars Pattern Return mission, an effort to convey the Perseverance rover’s rock assortment again to Earth. A brand new rock pattern is including to the anticipation as a result of it would comprise proof of historical water and (fingers crossed) long-ago microbial life — if it existed there.
The rock in query is now Perseverance’s fifteenth core pattern. It is named “Kukaklek” after a lake and river in Alaska. On Wednesday, the Perseverance group trumpeted the profitable assortment of the “good piece of sandstone.”
My assortment is rising! 🪨 I’ve now bought my fifteenth rock core: a pleasant piece of sandstone.
Up subsequent, I’m heading again to a close-by dune to interrupt out a brand new software – my regolith assortment bit – for gathering free, sandy materials. #SamplingMars continues… pic.twitter.com/RkYYpSAoUE
— NASA’s Perseverance Mars Rover (@NASAPersevere) November 30, 2022
Astrobiologist Erin Gibbons of McGill College supplied extra particulars on the rock in a rover replace this week. Gibbons identified a set of skinny, white veins seen within the sandstone after the rover abraded the floor away to get a glance beneath. The veins are proof of previous water exercise that stuffed small factures with mineral deposits.
NASA had beforehand talked up the sandstone rock previous to the rover gathering a pattern, expressing hope that it would maintain biosignatures, which the company defines as “any attribute, ingredient, molecule, substance, or characteristic that may function proof for historical life.” Gibbons’ replace highlights an much more particular dream of maybe discovering water hidden inside.
NASA picked the Jezero Crater as the Perseverance rover’s landing site due to its intriguing history of water. It appears to be home to an ancient lake bed and river delta from a time long ago when Mars was wetter.
The rock was part of an outcrop named Hidden Harbor that likely formed back when Jezero was a lake. “This was an exciting find because the veins are strikingly different than the sedimentary rock surrounding them, suggesting that they formed at a different time and under different conditions,” said Gibbons. It’s like cracking open a tiny window into the Martian past.
The veins could hold hidden clues to Mars’ history of microbial life, if it was ever in residence there. “It is even possible that, during crystallization, the minerals in the veins trapped a droplet or two of the ancient water that carried them through the network of fractures in the first place, providing a time capsule of Mars’ watery past,” said Gibbons.
Miniscule fluid inclusions have been found in ancient Earth rocks. A study earlier this year described the discovery of microorganisms 830 million years old in fluid inclusions in halite crystals, raising the possibility that a similar find from Mars could preserve organic matter. “Do the veins in Jezero contain such fluid inclusions? It’s possible, but we cannot know for certain until we bring a sample back to Earth for detailed analysis,” Gibbons wrote.
The Mars Sample Return mission will be complicated and challenging, but necessary to truly understand Mars’ past and, hopefully, answer the question of whether the red planet was once home to microbial life.