Perseverance landed in February in the Isidis Planitia region, just north of the equator in the eastern hemisphere of Mars. The region was chosen because images taken by orbiting spacecraft, such as this coloured pictured, showed the area resembled river deltas on Earth

Credit: News Scans

Freezing, arid and lifeless, the dusty Jezero crater on Mars is an inhospitable desert. Yet, 3.7 billion years ago it was full of water and could have harboured life, scientists believe.

The first analysis of images from Nasa’s Perseverance rover show the Jezero crater was once a huge 21-mile wide lake, which was fed by a river, and which suffered flash flooding.

Huge boulders now lie in the lake bed after being swept tens of miles downstream by the raging currents, the pictures show.

However, researchers are most excited by the discovery of layers of fine-grained clay and mudstones at the site, because they could preserve traces of ancient life.

Organics and biosignatures

Prof Sanjeev Gupta, of Imperial College London, one of the researchers who analysed the images, said: “The finest grained material at the bottom of the delta probably contains our best bet for finding evidence of organics and biosignatures.

“We’re not expecting to find fossils, but we could find evidence of microbial life.

Finding life on Mars

“We’ve already drilled two samples and put them into the Rover and we will be driving to the region in the next few years to take 38 samples and then there will be a joint European Space Agency and Nasa mission that will retrieve the samples so we can analyse the rocks on Earth.

“I think finding life is entirely likely. It would seem surprising that life only formed on Earth and these are definitely the right rocks to look for it.”

Rover’s landing spot carefully chosen 

Perseverance landed on Feb 18 in the Isidis Planitia region, just north of the equator in the eastern hemisphere of Mars, around one mile from the Delta.

The region was chosen because images taken by orbiting spacecraft showed the area resembled river deltas on Earth, where layers of sediment are deposited in the shape of a fan as the river feeds into a lake.

First images from latest Mars rover show ancient river delta in Jezero crater

Credit: News Scans

But without being on the ground it was impossible to know if the patterns were formed by the wind or other geological processes.

Steady water flow in ancient river

Zoomed images taken by Perseverance of the cliffs surrounding the crater show sloping rock beds sandwiched between horizontal layers that indicate rocky deposits from an ancient river.

The team says it suggests that there was steady water flow, consistent with a warm and humid Martian climate 3.7 billion years ago.

“If you look at these images, you’re basically staring at this epic desert landscape. It’s the most forlorn place you could ever visit,” said Benjamin Weiss, professor of planetary sciences in MIT’s Department of Earth, Atmospheric and Planetary Sciences, and a member of the analysis team.

The Jezero Crater, taken by instruments on Nasa's Mars Reconnaissance Orbiter (MRO), which regularly takes images of potential landing sites for future missions.
On ancient Mars, water carved channels and transported sediments to form fans and deltas within lake basins

Credit: Nasa/JPL-Caltech

“There’s not a drop of water anywhere, and yet, here we have evidence of a very different past. Something very profound happened in the planet’s history.

“Without driving anywhere, the rover was able to solve one of the big unknowns, which was that this crater was once a lake. Until we actually landed there and confirmed it was a lake, it was always a question.”

Lake level rose and fell

The lake was thought to be tens of feet deep, with water levels reaching high enough to break through the eastern crater rim, where images taken from orbit show an outflow event occurred.

Researchers found that the size of Jezero’s lake fluctuated greatly over time, with its depth rising and falling by tens of feet before eventually disappearing altogether.

The landing site for Nasa's Perseverance rover in relation to those of previous successful Mars missions

Credit: Nasa/JPL-Caltech

Boulders several feet across, and weighing several tons, were found to have come from outside the crater, and were probably part of the original bedrock.

The floods required to move the boulders were likely to have raged at 20 miles an hour and moved up to 10,500 cubic feet of water per second.

Clues about Earth’s past could be revealed

As well as providing more details about Mars, sampling the boulders could give important clues about Earth’s early geology which has since been destroyed by tectonic activity.

“The most surprising thing that’s come out of these images is the potential opportunity to catch the time when this crater transitioned from an Earth-like habitable environment, to this desolate landscape wasteland we see now,” added Prof Weiss.

“These boulder beds may be records of this transition, and we haven’t seen this in other places on Mars.”

Sue Horne, the head of space exploration, UK Space Agency, said: “These ancient environments provide the perfect place for the Perseverance rover to search for signs of past life on Mars.”

The research was published in the journal Science.