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Mradul Sharma

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  • Published: Sep 11 2025 02:59 PM
  • Last Updated: Sep 11 2025 03:12 PM

NASA’s Perseverance rover has detected organic carbon and unusual minerals in Jezero Crater, offering the strongest clues yet that Mars may once have hosted ancient microbial life.


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NASA's Perseverance rover has discovered what scientists say could be the strongest evidence yet of ancient microbial life on the surface of Mars. The new results reported in Nature describe unusual minerals and organic matter found in rocks on Jezero Crater, a potential area of ancient water billions of years ago.

Scientists express their excitement over the discovery, but caution against making claims. The evidence could indicate life present, but it may also be the result of natural chemical interactions through abiotic means.

What the Rover Found in Jezero Crater

Within a specific enclave of a set of mudstone rocks from the Bright Angel formation, Perseverance drilled. The mudstone rocks were likely part of a river or lakebed; they are largely composed fine clay and silt - materials that often capture and preserve chemical signatures through time.

Within the rocks, scientists found organic carbon, one of the building blocks of life. They also found two important minerals: vivianite (an iron phosphate) and greigite (an iron sulfide). The two minerals co-occur on Earth, generally in organic-rich environments - with the involvement of microbes.

nasa rover drilling

The researchers found small reaction fronts and mineral textures that were less than a millimetre wide that indicate chemical reactions associated with redox processes, which are based on electron movement and are often used by microbes for energy. Most importantly, there is evidence that suggests that the reactions occurred at low temperatures and makes it difficult to assume non-biological reactions occurred.

Still, the scientists make it clear that geology may sometimes produce the same patterns, and the only way to confirm whether life was involved is to return those samples to Earth for closer inspection, which is why NASA's future Mars Sample Return mission is so important.

Why the Discovery Matters

For decades, scientists have been looking for signs of past life on Mars, focused on the sites that had once been places where water traveled. Jezero Crater is one of the best bets because it used to be a river delta.

This latest discovery is significant for multiple reasons:

  1. It is the strongest potential biosignature - or, chemical fingerprint of life - so far discovered on Mars.
  2. The rocks examined are billions of years old, from a time when Mars had water, likely making it more hospitable.
  3. The minerals that were identified, along with the organic carbon, resemble the environments on Earth in which microbes flourish.

As much as they are trying not to overstate the point, experts acknowledge that equipment on Mars cannot match the sensitivity of equipment in laboratories on Earth, and until we had the samples back, it is possible that all we have seen is pure chemical processes, not biology.

Looking Ahead

The new findings demonstrate just how close the scientists may be to find out one of humanity's oldest questions: are we alone in the universe?

If further research can accurately support that microbes did once live on Mars, this would be the first evidence of life outside Earth. This would fundamentally shift our understanding of biology and what life could look like in the solar system and beyond.

For now, Perseverance is still on its mission. It is obtaining samples that if we're lucky one day can be brought back to Earth. Every discovery is helping to paint the picture of a planet that used to be far more Earth-like, possibly where life may have first began.

FAQ

A biosignature is a feature—such as certain chemicals, minerals, or textures—in rocks or soil that may be produced by living organisms. It is not proof of life by itself, but a clue that life might once have existed.

Vivianite is an iron phosphate mineral; greigite is an iron sulfide. On Earth, both can form in the presence of organic matter through redox chemical reactions, sometimes involving microbes. Their presence in the Martian samples is one reason scientists think the rocks might contain signs of ancient life.

There are multiple reasons: alternative non-biological processes can produce similar minerals; the instruments on Mars have limitations; and confirmation usually requires samples to be brought to Earth for more detailed testing. Without ruling out non-living causes, scientists must stay cautious.

The rocks studied are believed to date from between about 3.2 to 3.8 billion years ago, a time when Mars likely had liquid water. This period is considered more favorable for life (if it ever existed) because water is essential. The age and past environment of these rocks make them excellent candidates for finding ancient biosignatures.

Scientists plan to analyze the samples in Earth laboratories once they are returned. They will compare findings with Earth analogues and run experiments to test if the non-biological explanations hold. Future Mars missions might target similar formations and use more advanced instruments to home in on stronger evidence.

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