A sample obtained by NASA’s Perseverance rover of rock formed billions of years ago from sediment on the bottom of a lake contains potential signs of ancient microbial life on Mars, according to scientists, though the minerals spotted in the sample can also form through non-biological processes.
The discovery, detailed in research published on Wednesday, represents one of the best pieces of evidence to date about the possibility that Earth’s planetary neighbour once harboured life.
Since landing on the Martian surface in 2021, the six-wheeled rover has been exploring Jezero Crater, an area in the planet’s northern hemisphere that was once flooded with water and home to an ancient lake basin, as it seeks signs of ancient life. Perseverance has been collecting samples of rock and loose material called regolith and analyzing them with its various onboard instruments.
The rover obtained the newly described sample, called the Sapphire Canyon sample, in a place called the Bright Angel rock formation. This formation consists of fine-grained mudstones and coarse-grained conglomerates, a kind of sedimentary rock composed of gravel-sized particles cemented together by finer-grained sediments.
Stony Brook University planetary scientist Joel Hurowitz, who led the study published in the journal Nature, said that a “potential biosignature” was detected in multi-billion-year-old sedimentary rocks.
This came in the form of two minerals that appear to have formed as a result of chemical reactions between the mud of the Bright Angel formation and organic matter also present in that mud, Hurowitz said. They are: vivianite, an iron phosphate mineral, and greigite, an iron sulfide mineral.
“These reactions appear to have taken place shortly after the mud was deposited on the lake bottom. On Earth, reactions like these, which combine organic matter and chemical compounds in mud to form new minerals like vivianite and greigite, are often driven by the activity of microbes,” Hurowitz said.
“The microbes are consuming the organic matter in these settings and producing these new minerals as a byproduct of their metabolism,” Hurowitz said.
Caution needed
But Hurowitz offered some words of caution.
“The reason, however, that we cannot claim this is more than a potential biosignature is that there are chemical processes that can cause similar reactions in the absence of biology, and we cannot rule those processes out completely on the basis of rover data alone,” Hurowitz said.
Mars has not always been the inhospitable place it is today, with liquid water on its surface in the distant past. Scientists have suspected that microbial life once could have lived in Jezero Crater. They believe river channels spilled over the crater wall and created a lake more than 3.5 billion years ago.
WATCH | Meet the Mars Samples: Sapphire Canyon (Sample 25):
The Sapphire Canyon sample was collected in July 2024 from a set of rocky outcrops on the edges of Neretva Vallis, an ancient river valley carved by water rushing into Jezero Crater.
The sample collected and analyzed by Perseverance provides a new example of a type of potential biosignature that the research community can explore to try to understand whether or not these features were formed by life, Hurowitz said, “or alternatively, whether nature has conspired to present features that mimic the activity of life.”
“Ultimately, follow-on research will provide us with a suite of testable hypotheses for how to determine whether biology is responsible for the generation of these features in the Bright Angel formation, which we can evaluate by examining the Sapphire Canyon sample if it is returned to Earth,” Hurowitz added.
