A team of researchers from NASA's Mars Science Laboratory (MSL) Curiosity rover mission analysed a set of sedimentary rock outcrops at a site named Yellowknife Bay in Gale Crater, near the Martian equator.
These mud-stones have revealed that Gale Crater, a 150 km wide impact basin with a mountain at its centre, sustained at least one lake around 3.6 billion years ago.
The scientists believe that the lake may have lasted for tens if not hundreds of thousands of years.
Such a lake would provide perfect conditions for simple microbial life such as chemolithoautotrophs to thrive in.
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On Earth, chemolithoautotrophs are commonly found in caves and around hydrothermal vents. The microbes break down rocks and minerals for energy.
Mud-stones generally form in calm conditions. They are created by very fine sediment grains settling layer-by-layer on each other, in still water.
"It is important to note that we have not found signs of ancient life on Mars. What we have found is that Gale Crater was able to sustain a lake on its surface at least once in its ancient past that may have been favourable for microbial life, billions of years ago. This is a huge positive step for the exploration of Mars," Professor Sanjeev Gupta from Imperial College London and a co-author of the research, said.
In previous studies, Gupta and the MSL team have found evidence of water on Mars' surface in other rocks such as conglomerates.
However, the new research provides the strongest evidence yet that Mars could have been habitable enough for life to take hold.
The next step will see the team using the rover to explore Gale Crater for further evidence of ancient lakes or other habitable environments in the thick pile of sedimentary rocks scattered across the crater's surface.
The study was published in the journal Science.