Organic matter preserved in 3-billion-year-old mudstones at Gale crater, Mars

J. L. Eigenbrode(Goddard Space Flight Center), Roger E. Summons(Massachusetts Institute of Technology), A. Steele(Carnegie Institution for Science), Caroline Freissinet(Goddard Space Flight Center), M. Millán(Centre National de la Recherche Scientifique), R. Navarro‐González(Universidad Nacional Autónoma de México), B. Sutter(Johnson Space Center), A. C. McAdam(Goddard Space Flight Center), H. B. Franz(Goddard Space Flight Center), D. P. Glavin(Goddard Space Flight Center), P. D. Archer(Jacobs (United States)), P. R. Mahaffy(Goddard Space Flight Center), P. G. Conrad(Goddard Space Flight Center), J. A. Hurowitz(Stony Brook University), J. P. Grotzinger(California Institute of Technology), Sanjeev Gupta(Imperial College London), Doug Ming(Johnson Space Center), D. Y. Sumner(Planetary Science Institute), Cyril Szopa(Centre National de la Recherche Scientifique), C. A. Malespin(Goddard Space Flight Center), A. Buch(Supélec), Patrice Coll(Centre National de la Recherche Scientifique)
Science
June 7, 2018
Cited by 520Open Access
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Abstract

Establishing the presence and state of organic matter, including its possible biosignatures, in martian materials has been an elusive quest, despite limited reports of the existence of organic matter on Mars. We report the in situ detection of organic matter preserved in lacustrine mudstones at the base of the ~3.5-billion-year-old Murray formation at Pahrump Hills, Gale crater, by the Sample Analysis at Mars instrument suite onboard the Curiosity rover. Diverse pyrolysis products, including thiophenic, aromatic, and aliphatic compounds released at high temperatures (500° to 820°C), were directly detected by evolved gas analysis. Thiophenes were also observed by gas chromatography-mass spectrometry. Their presence suggests that sulfurization aided organic matter preservation. At least 50 nanomoles of organic carbon persists, probably as macromolecules containing 5% carbon as organic sulfur molecules.


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