Understanding the chemical evolution of newly formed terrestrial planets involves uncertainties in atmospheric chemical composition and assessing the plausibility of biomolecule synthesis. In this study, an original scenario for the origin of methane on Mars and terrestrial planets is suggested. Carbon dioxide in Martian and other planetary atmospheres can be abiotically converted into a mixture of methane and carbon monoxide by ‘methanogenesis’ on porous mineral photoactive surfaces under soft ultraviolet irradiation. On young planets exposed to heavy bombardment by interplanetary matter, this process can be followed by biomolecule synthesis through the reprocessing of reactive reducing atmospheres by impact-induced shock waves. The proposed mechanism of methanogenesis may help to answer the question concerning the formation of methane and carbon monoxide by photochemical processes, the formation of biomolecules on early Earth and other terrestrial planets, and the source and seasonal variation of methane concentrations on Mars.
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This work is a part of a research series funded by the Czech Science Foundation (grants no. 17-05076S and 13-07724S), by the programme of Regional Cooperation between the Regions and the Institutes of the Czech Academy of Sciences in 2017 (project numbers: R200401721 and R200401521) and by the STS Missions programme within the COST Actions CM1401 and TD1308. The authors also thank the PALS facility staff for supporting the experiments, particularly L. Juha, J. Ullschmied, J. Skála, J. Dostál, P. Prchal and J. Mareš. We also thank the Ministry of Education, Youth and Sports of the Czech Republic for supporting the PALS infrastructure operation and research by grants LM2015083 and LG15013.
The authors declare no competing financial interests.
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Civiš, S., Knížek, A., Ivanek, O. et al. The origin of methane and biomolecules from a CO2 cycle on terrestrial planets. Nat Astron 1, 721–726 (2017). https://doi.org/10.1038/s41550-017-0260-8
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