PMID- 33226839 OWN - NLM STAT- MEDLINE DCOM- 20211015 LR - 20231110 IS - 1557-8070 (Electronic) IS - 1531-1074 (Print) IS - 1557-8070 (Linking) VI - 21 IP - 2 DP - 2021 Feb TI - Artificial Maturation of Iron- and Sulfur-Rich Mars Analogues: Implications for the Diagenetic Stability of Biopolymers and Their Detection with Pyrolysis-Gas Chromatography-Mass Spectrometry. PG - 199-218 LID - 10.1089/ast.2019.2211 [doi] AB - Acidic iron- and sulfur-rich streams are appropriate analogues for the late Noachian and early Hesperian periods of martian history, when Mars exhibited extensive habitable environments. Any past life on Mars may have left behind diagnostic evidence of life that could be detected at the present day. For effective preservation, these remains must have avoided the harsh radiation flux at the martian surface, survived geological storage for billions of years, and remained detectable within their geochemical environment by analytical instrument suites used on Mars today, such as thermal extraction techniques. We investigated the detectability of organic matter within sulfur stream sediments that had been subjected to artificial maturation by hydrous pyrolysis. After maturation, the samples were analyzed by pyrolysis-gas chromatography-mass spectrometry (py-GC-MS) to determine whether organic matter could be detected with this commonly used technique. We find that macromolecular organic matter can survive the artificial maturation process in the presence of iron- and sulfur-rich minerals but cannot be unambiguously distinguished from abiotic organic matter. However, if jarosite and goethite are present in the sulfur stream environment, they interfere with the py-GC-MS detection of organic compounds in these samples. Clay reduces the obfuscating effect of the oxidizing minerals by providing nondeleterious adsorption sites. We also find that after a simple alkali and acid leaching process that removes oxidizing minerals such as iron sulfates, oxides, and oxyhydroxides, the sulfur stream samples exhibit much greater organic responses during py-GC-MS in terms of both abundance and diversity of organic compounds, such as the detection of hopanes in all leached samples. Our results suggest that insoluble organic matter can be preserved over billions of years of geological storage while still retaining diagnostic organic information, but sample selection strategies must either avoid jarosite- and goethite-rich outcrops or conduct preparative chemistry steps to remove these oxidants prior to analysis by thermal extraction techniques. FAU - Tan, Jonathan S W AU - Tan JSW AD - Impacts and Astromaterials Research Centre, Department of Earth Science and Engineering, Imperial College London, London, UK. FAU - Royle, Samuel H AU - Royle SH AD - Impacts and Astromaterials Research Centre, Department of Earth Science and Engineering, Imperial College London, London, UK. FAU - Sephton, Mark A AU - Sephton MA AD - Impacts and Astromaterials Research Centre, Department of Earth Science and Engineering, Imperial College London, London, UK. LA - eng PT - Journal Article PT - Research Support, Non-U.S. Gov't DEP - 20201123 PL - United States TA - Astrobiology JT - Astrobiology JID - 101088083 RN - 0 (Biopolymers) RN - 70FD1KFU70 (Sulfur) RN - E1UOL152H7 (Iron) SB - IM MH - Biopolymers MH - *Exobiology MH - Extraterrestrial Environment MH - Gas Chromatography-Mass Spectrometry MH - Iron MH - *Mars MH - Pyrolysis MH - Sulfur PMC - PMC7876361 OTO - NOTNLM OT - Alkali/Acid leaching OT - Artificial maturation OT - Biosignature OT - Hydrous pyrolysis OT - Mars OT - py-GC-MS COIS- No competing financial interests exist. EDAT- 2020/11/24 06:00 MHDA- 2021/10/16 06:00 PMCR- 2021/02/04 CRDT- 2020/11/23 17:09 PHST- 2020/11/24 06:00 [pubmed] PHST- 2021/10/16 06:00 [medline] PHST- 2020/11/23 17:09 [entrez] PHST- 2021/02/04 00:00 [pmc-release] AID - 10.1089/ast.2019.2211 [pii] AID - 10.1089/ast.2019.2211 [doi] PST - ppublish SO - Astrobiology. 2021 Feb;21(2):199-218. doi: 10.1089/ast.2019.2211. Epub 2020 Nov 23.