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Updated: Aug 20, 2025

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations
Published on: August 8, 2018
Aqueous alteration processes in Jezero crater, Mars-implications for organic geochemistry
Eva L Scheller1,2, Joseph Razzell Hollis3,4, Emily L Cardarelli3
1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA, USA.
Abstract:
The Perseverance rover landed in Jezero crater, Mars, in February 2021. We used the Scanning Habitable Environments with Raman and Luminescence for Organics and Chemicals (SHERLOC) instrument to perform deep-ultraviolet Raman and fluorescence spectroscopy of three rocks within the crater. We identify evidence for two distinct ancient aqueous environments at different times. Reactions with liquid water formed carbonates in an olivine-rich igneous rock. A sulfate-perchlorate mixture is present in the rocks, which probably formed by later modifications of the rocks by brine. Fluorescence signatures consistent with aromatic organic compounds occur throughout these rocks and are preserved in minerals related to both aqueous environments.
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