Space research

DTU researchers are "closer than ever" to proving that there has been life on Mars

Leopard-spotted deposits in fossilized mud on Mars may have been left behind by living organisms. But to be absolutely sure, we need to bring the samples down to Earth, researchers from DTU and NASA write in the scientific journal Nature.

The Perseverance rover has been searching for signs of past life on Mars since 2020. The PIXL instrument at the top of the rover was developed in collaboration with DTU Space. Photo: NASA/JPL-Caltech/MSSS

Facts

DTU Space has played a central role in the development of the advanced PIXL instrument, which is mounted on the end of Perseverance's robotic arm. PIXL has been used to examine and analyze the chemical compounds in the Jezero crater.

DTU researchers have worked closely with NASA’s Jet Propulsion Laboratory to design and build the PIXL instrument and have supplied several of the subsystems:

  • The hyperspectral camera, which can "see" ultraviolet, visible, and infrared light. The camera is used to provide visual context for the other instruments, to determine the geological composition of rock types, to measure grain sizes, and to identify the target areas to be scanned by the X-ray microscope.
  • The two structured lasers, which, together with the context camera, accurately measure the distance to the target.
  • The ultra-precise navigation system "Terrain Relative Navigation", which uses the camera system to ensure, among other things, that PIXL scans the desired area and does not collide with the uneven rocks.

All three systems are key technologies that PIXL cannot function without.

DTU researchers perform all image interpretations from the systems and have thus played a fundamental role in understanding the data on which the new scientific article is based.

Home to Earth

The promising chemical signatures have been found on a rock in a now-dry river delta that flowed into a crater on Mars called Jezero.

On the banks of the river, fossilised material has been found embedded in petrified mud, containing elements that here on Earth would be interpreted as signs of the former presence of microorganisms.

It is these chemical compounds, including oxygen, organic carbon, hydrogen and phosphorus, that the researchers in their article refer to as "potential biosignatures" – i.e. evidence of biological life.

The big question is whether there could be other explanations for how these particular chemical compounds ended up on the dried-up riverbank:

"The research team has been searching intensively for a non-biological process that can explain what we have seen on Mars. But so far, we have not been able to come up with a plausible explanation that does not involve life," says John Leif Jørgensen.

However, in order to determine with certainty whether the substances originate from living organisms and to establish their age, we need to be able to examine them thoroughly in a laboratory:

"We can only determine this conclusively if we bring the samples collected from Mars back to Earth for further examination. That is why NASA has proposed the Mars Sample Return mission, to which we are also contributing, and which will bring our samples back to Earth. So we are closer than ever to a definitive answer," says John Leif Jørgensen.

The Mars Sample Return mission has not yet been finally approved, but is being planned in collaboration between NASA and the European Space Agency, ESA.

Find the complete research article in Nature and DTU Orbit.

Contact

John Leif Jørgensen

John Leif Jørgensen Professor and Head of Measurement and Instrumentation National Space Institute

David Arge Klevang

David Arge Klevang Associate Professor National Space Institute Phone: +45 45253609