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According to NASA, the Perseverance rover has collected a rock sample from Mars’ Jezero Crater that contains potential biosignatures, substances or structures that could indicate past microbial life. This discovery, detailed in a new paper published in the journal Nature, comes from a rock formation nicknamed “Cheyava Falls” and sampled in July 2024. While scientists are considering the possibility that chemical reactions within this rock billions of years ago could have supported microbial life, other explanations are also being explored.

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The sample, designated “Sapphire Canyon,” was retrieved from an ancient dry riverbed within Jezero Crater. The “Cheyava Falls” rock is part of the “Bright Angel” formation, located on the edges of Neretva Vallis, a valley carved by water that once flowed into Jezero Crater. Scientists observed that the sedimentary rocks in this formation are composed of clay and silt, materials that on Earth are known to effectively preserve signs of ancient microbial life. Furthermore, these rocks are notably rich in organic carbon, sulfur, oxidized iron (rust), and phosphorus.

The presence of these chemical compounds suggests that the Bright Angel formation could have provided a rich energy source for microbial metabolisms. The Perseverance rover’s PIXL and SHERLOC instruments, which collected initial data on the arrowhead-shaped rock, identified what appeared to be colorful spots. These spots, when examined at higher resolution, revealed a distinct pattern of minerals arranged into what scientists are calling “leopard spots.” These spots exhibit the chemical signature of two iron-rich minerals: vivianite, a hydrated iron phosphate frequently found in terrestrial sediments and around decaying organic matter, and greigite, an iron sulfide that can be produced by certain forms of microbial life on Earth.

The combination of vivianite and greigite, appearing to have formed from electron-transfer reactions between sediment and organic matter, is considered a potential indicator of microbial life, as such reactions could have been used by microbes for energy. However, it is important to note that these minerals can also be formed through non-biological processes, such as high temperatures, acidic conditions, or reactions catalyzed by organic compounds. The rocks examined at Bright Angel do not show evidence of extreme temperatures or acidity, and the specific role of the present organic compounds in catalyzing reactions at lower temperatures is still under investigation.

This discovery is particularly significant as it was found in some of the youngest sedimentary rocks the Perseverance mission has analyzed. Previous hypotheses suggested that signs of ancient life would likely be found in older rock formations. This new finding implies that Mars may have been habitable for a longer duration or later in its history than previously understood. It also raises the possibility that older Martian rocks might contain signs of life that are simply more difficult to detect. The scientific community utilizes established frameworks like the CoLD scale and Standards of Evidence to rigorously assess data concerning the search for extraterrestrial life, aiming to determine the level of confidence in signals suggesting past life beyond Earth.

Sapphire Canyon is one of 27 rock core samples collected by the Perseverance rover since its landing in Jezero Crater in February 2021. The rover is equipped with various science instruments, including a weather station designed to provide environmental data for future human missions, and swatches of spacesuit material to study their performance on the Martian surface. The Perseverance rover is managed for NASA by Caltech, with operations overseen by NASA’s Jet Propulsion Laboratory as part of NASA’s Mars Exploration Program.

Article by Mel Anara, based upon information from NASA News.


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