NASA’s rover finds potential sign of life on Mars

NASA’s rover finds potential sign of life on Mars

NASA’s Perseverance rover has discovered potential biosignatures in a Martian rock sample, indicating the presence of iron-rich minerals and organic carbon, which suggests a past habitable environment that may have been sustained by microbial life.

At a Glance

  • NASA’s Perseverance rover discovered potential biosignatures within the “Bright Angel” formation in Jezero Crater, suggesting Mars may have once hosted microbial life.
  • The rock sample, named Sapphire Canyon, contains organic carbon alongside iron phosphate and iron sulfide minerals, which are identified as likely vivianite and greigite.
  • These minerals appear to have formed from chemical reactions that, on Earth, are often driven by microbes consuming organic matter for energy.
  • While these features could have formed without life, the geological evidence suggests the high heat or acidity needed for abiotic formation was absent.
  • Scientists emphasize that definitive proof requires analyzing the collected sample on Earth, making the Mars Sample Return mission critically important for this research.

NASA announced yesterday that its Perseverance rover has discovered a potential biosignature — a feature that could indicate ancient life — in an ancient riverbed within Mars’ Jezero Crater. The finding, detailed in the journal Nature, centers on a rock sample named “Sapphire Canyon” collected from an outcrop called “Bright Angel.” This location features a compelling mix of organic carbon and distinctive iron-rich minerals, suggesting that Mars may have been habitable later in its history than previously thought. The discovery marks a significant step in the search for extraterrestrial life, though scientists caution that further analysis is required to confirm a biological origin.

This close-up image from NASA’s Perseverance rover reveals the distinctive “leopard spots” on a rock nicknamed “Cheyava Falls” in Mars’ Jezero Crater. The small, circular features with dark rims, scattered across the reddish mudstone, are reaction fronts containing a mix of iron-rich minerals and organic carbon. This specific combination represents a potential biosignature, suggesting the rock’s chemistry could have once provided an energy source for ancient microbial life. (NASA/JPL-Caltech/MSSS, 2025)

The rover’s advanced instruments, SHERLOC and PIXL, detected unusual, colorful spots on a rock at the site. Closer inspection revealed these spots, nicknamed “leopard spots,” are reaction fronts where chemical changes occurred. They contain high concentrations of ferrous iron phosphate and sulfide minerals, likely vivianite and greigite. On Earth, these minerals often form in low-temperature, watery environments where microbes consume organic matter for energy. This process involves redox reactions, where electrons are transferred between molecules, releasing energy that living organisms can utilize. The presence of these specific minerals alongside organic carbon in Martian mudstone presents a tantalizing clue that similar microbial metabolisms may have been active on the Red Planet in the past.

The Confidence of Life Detection (CoLD) scale, a seven-level framework used by scientists to evaluate potential evidence of extraterrestrial life, outlines a rigorous, step-by-step process that begins with detecting a possible biological signal (Level 1) and progresses through ruling out contamination and non-biological sources (Levels 2-4). The recent discovery by the Perseverance rover represents a significant finding at this early stage; achieving higher levels of confidence will require analyzing the collected Martian samples in laboratories on Earth. (NASA, 2025)

While the combination of minerals and organic material is consistent with biological activity, it does not rule out non-biological, or abiotic, processes. Specific chemical reactions can produce the same signatures without the presence of life, but they typically require conditions such as sustained high temperatures or highly acidic water. According to the research team, the geology of the Bright Angel formation shows no evidence that it experienced such extreme conditions, making the abiotic explanation less likely. However, the possibility remains that unknown chemical pathways involving organic compounds could have catalyzed the reactions at low temperatures.

This animation illustrates how Mars’ Neretva Vallis may have looked billions of years ago when it was a river valley filled with water. It was in this ancient, habitable environment that the sedimentary rocks of the “Bright Angel” formation were deposited. Today, the valley is dry, but it is here that NASA’s Perseverance rover found potential biosignatures in a rock named “Cheyava Falls,” suggesting this once-watery world could have supported microbial life. (NASA, 2025)

Ultimately, a definitive answer awaits the return of the Sapphire Canyon sample to Earth. The Mars Sample Return mission is designed to bring rock cores collected by Perseverance back for analysis in advanced laboratories, which can perform tests far beyond the capabilities of the rover’s onboard instruments. Scientists will use frameworks like the Confidence of Life Detection (CoLD) scale to assess the evidence rigorously. While this discovery is not yet proof of life, it has identified one of the most promising targets ever found and underscores the critical importance of bringing pieces of Mars home for study.


References

  • Hurowitz, J. A., Tice, M. M., Allwood, A. C., Cable, M. L., Hand, K. P., Murphy, A. E., Uckert, K., Bell, J. F., Bosak, T., Broz, A. P., Clavé, E., Cousin, A., Davidoff, S., Dehouck, E., Farley, K. A., Gupta, S., Hamran, S.-E., Hickman-Lewis, K., Johnson, J. R., … Wolf, Z. U. (2025). Redox-driven mineral and organic associations in Jezero Crater, Mars. Nature, 645(8080), 332–340. https://doi.org/10.1038/s41586-025-09413-0

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