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NASA’s Curiosity rover has detected more than 20 organic molecules in 3.5‑billion‑year‑old clay‑bearing sandstones in Gale Crater’s Glen Torridon region, scientists reported on April 21, 2026 in Nature Communications.
The discovery came from the rover’s Sample Analysis at Mars (SAM) suite using a tetramethylammonium hydroxide (TMAH) thermochemolysis experiment — the first time that wet‑chemistry thermochemolysis has been run on another planet.
Identified compounds include benzothiophene, methyl benzoate and a suite of single and dicyclic aromatic molecules, plus nitrogen‑ and sulfur‑bearing species; researchers interpret many as breakdown products of preserved macromolecular carbon.
The sample came from the “Mary Anning 3” drill target in the Knockfarrill Hill member.
Scientists emphasize the molecules are not direct evidence of past life: they could be native abiotic products, or delivered by meteorites.
The paper was led by Amy Williams (Univ. of Florida) and confirms that complex organics can survive deep geologic time in Mars’ shallow subsurface.
Results will inform future TMAH experiments planned for ESA’s Rosalind Franklin rover and NASA’s Dragonfly mission.








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