Your browser has javascript turned off or blocked. This will lead to some parts of our website to not work properly or at all. Turn on javascript for best performance.

The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here:

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Analysis of 3.6 billion-year-old lake intensifies the search for life on Mars

Landscape with sand and rocks. Photo.
The image represents the crater area in which the Perseverance rover collected the images that have now been analysed in the study. Photo: Foto: NASA/JPL-Caltech/ASU.

Using 150 000 images from the Perseverance space rover, an international research team has studied the Western delta in Jezero crater, Mars, revealing evidence of deltas that advanced into a lake. The new discovery not only provides important keys to the geological history of our neighbouring planet, and it also intensifies the search for life.

A cloud of red smoke. And a couple of seconds of uncertainty. That is how you could describe the visually tantalising real-time images of National Aeronautics and Space Administration's (NASA) space rover Perseverance, swamped by its parachute, touching down on the dusty surface of the planet Mars in February. The applause knew no boundaries. The world’s planetary scientists rubbed their hands together at the thought of Perseverance spending several years gathering samples to answer the question of whether there has ever been any form of life on the iron-oxide-red planet. In the first scientific article based on the data gathered by Perseverance, an international research team, including Lund University, was able to study the hydrological evolution of the crater known as Jezero. The research study, published in the journal Science, reveals new facts about how a viable lake and its meandering river deltas evolved.

“We can see a transition in the nature of the fluvial system feeding the western delta. This could be interpreted as the area having gone from being potentially habitable to the opposite. The images have given us new knowledge about the history of paleolakes on Mars”, says Sanna Alwmark, geology researcher at Lund University.

Using advanced analysis of images selected from a total of 150 000, the research team formed an idea of the development of the prehistoric lake. It is too soon to say what caused the Jezero crater paleolake to eventually dry up, which began sometime after 3.6 billion years ago.

“Something drastic happened on Mars. What and when is unclear”, says Sanna Alwmark.

It is not only the deeper insight into the change in the climate on Mars and its impact on the lake system and river deltas in the Jezero crater that the researchers want to highlight in the study. The results also highlight areas of higher potential when it comes to the search for ancient life. For example, banks of fine-grained sediments have potential to preserve traces of possible past martian life, known as biosignatures.

“We have to concentrate on very tiny things, biosignatures and organic material. And that means searching in material in which the conditions for the preservation of tiny things are most favourable”, says Sanna Alwmark.

Besides Lund University, around twenty higher education institutions and organisations took part in the study.

The study has been published in the research journal Science.

Read the study “Perseverance rover reveals an ancient delta-lake system and flood deposits at Jezero crater, Mars” on the journal's website