NASA’s Perseverance rover has made a groundbreaking discovery on Mars, detecting complex macromolecular carbon on the surface of a rock at the Bright Angel site within Jezero Crater. This finding, reported by researcher Ashley E. Murphy from the Planetary Institute in Tucson, Arizona, marks the shallowest detection of organic matter on the Martian surface to date.
Significance of the Bright Angel Carbon Discovery
The presence of macromolecular carbon typically suggests a biological origin on Earth. However, the exact source of this carbon on Mars remains uncertain. According to Murphy, "The term kerogen implies biogenic source. Macromolecular carbon implies we don’t know whether its origin is biotic or abiotic." This ambiguity highlights the need for further investigation into the samples.
The carbon was detected using SHERLOC (Scanning Habitable Environments with Raman and Luminescence for Organics and Chemicals), a UV Raman spectrometer attached to Perseverance. The rover pointed this instrument at four targets between sols 1180 and 1218, revealing a distinctive spectral signature known as the G-band, indicative of a complex network of carbon atoms.
Potential Origins of the Macromolecular Carbon
The analysis of the carbon suggests it may have formed during at least two separate geological events. At one site, Apollo Temple, the carbon was found clustered with carbonate and sulfate minerals, indicating precipitation from ancient water flow. In contrast, at Walhalla Glades, the carbon was associated with silicate-rich sediment.





