Mars may have once been capable of supporting microbial life for hundreds of millions of years in the distant past, new findings from a long-lived Red Planet rover suggest.
NASA's Opportunity rover, which celebrates 10 years of Mars exploration on Friday (Jan. 24), has uncovered evidence that benign, nearly neutral-pH water flowed on the Red Planet around 4 billion years ago.
These results, reported today (Jan. 23) in the journal Science, complement the recent work of NASA's bigger, newer Curiosity rover, which discovered a potentially habitable lake and groundwater system in a different Martian locale dating from about 3.7 billion years ago. [Video: Mars Could Have Supported Life, NASA Finds]
"These [benign] water conditions existed over a long period of time," said Ray Arvidson, lead author of the new study and Opportunity deputy principal investigator.
Therefore, primitive organisms may have been able to survive on Mars for long stretches during a period when life was getting a foothold on Earth, said Arvidson, director of the Earth and Planetary Remote Sensing Laboratory at Washington University in St. Louis.
"That wouldn't be a surprise," he told SPACE.com. "Maybe not globally; [habitable environments] could have occurred here and there regionally. And it may not have been for the whole time continuously. We don't know."
The rover made the new discovery at an outcrop on the rim of Endeavour Crater, a 14-mile-wide (22 kilometers) hole in the ground that Opportunity reached in August 2011.
NASA's Mars Reconnaissance Orbiter spotted evidence of exposed, aluminum-rich clay minerals at a site along the rim called Matijevic Hill. Such clays generally form in the presence of benign, mildly acidic water, so the rover team commanded Opportunity to go check out the rock formation.
When Opportunity got there, the rover encountered the oldest rocks it has ever studied on Mars. Fine-grained, layered rocks in the Matijevic outcrop date from Mars' Noachian period, making them perhaps 4 billion years old, Arvidson said. (It's tough to date Mars rocks and formations definitively, so such numbers have large uncertainties associated with them, he stressed.)
These clay-enriched rocks are studded with BB-size "spherules" and cut by numerous fractures, through which liquid water flowed long ago, Arvidson said.
"The groundwaters that moved through those fractures were only mildly acidic, and mildly oxidizing to reducing," he said. "So, the earlier you go, the more clement the conditions were."
These ancient rocks predate the asteroid or comet impact that created Endeavour Crater, and they're covered in most places by younger material that bears the signature of hypersalty and much more acidic water — the signature, in other words, of a much less hospitable Mars.
Teaming up with Curiosity
Opportunity's new results take on deeper meaning when combined with the observations of the 1-tonCuriosity rover, which touched down on a different part of Mars in August 2012.
Curiosity was designed to extend and advance the discoveries of Spirit and Opportunity. It sports 10 different science instruments — a suite crafted specifically to determine if the Red Planet could ever have supported microbial life.
Last month, the Curiosity team announced that an area near the rover's landing site harbored a large, shallow and potentially habitable lake system during Mars' Hesperian era, which follows the Noachian in Red Planet chronology. This lake and its feeder streams likely existed about 3.7 billion years ago, or perhaps even a bit more recently, mission scientists said.
So researchers are starting to get a better idea of the Martian surface's window of habitability, Arvidson said. It appears that window might have been open — off and on, perhaps, and here and there — for hundreds of millions of years in the distant past.
Liquid water cannot exist for long periods on the surface of present-day Mars, whose atmosphere is just 1 percent as thick as that of Earth. That atmosphere was likely thicker long ago, if lakes and river systems were, indeed, stable for lengthy stretches, Arvidson said.
"One way to do it is to have massive impacts, and to have a [temporarily thicker] atmosphere," he said. "So it could be that you have multiple impacts over that extended period of time, and collectively they made for a sustained presence of water on the surface and in the shallow subsurface. But we don't know, at this point, with just two examples."