Decoding organic compounds in lava tube sulfates to understand potential biomarkers in the Martian subsurface
2024
Palma, Vera | Rosa Arranz, José M. de la | Onac, Bogdan P. | Sauro, Francesco | Martínez-Frías, J. | Caldeira, Ana Teresa | González-Pérez, José Antonio | Jiménez Morillo, N. T. | Miller, A. Z. | Ministerio de Ciencia e Innovación (España) | Agencia Estatal de Investigación (España) | Fundação para a Ciência e a Tecnologia (Portugal) | Consejo Superior de Investigaciones Científicas (España) | Rosa Arranz, José M. de la [0000-0003-2857-2345] | Onac, Bogdan P. [0000-0003-2332-6858] | Sauro, Francesco [0000-0002-1878-0362] | Martínez-Frías, J. [0000-0002-2609-4485] | Caldeira, Ana Teresa [0000-0001-5409-6990] | González-Pérez, José Antonio [0000-0001-7607-1444] | Jiménez Morillo, N. T. [0000-0001-5746-1922] | Miller, A. Z. [0000-0002-0553-8470] | Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
14 páginas.- 5 figuras.- 4 tablas.- 119 referencias.- Supplementary information The online version contains supplementary material available at https://doi.org/10.1038/s43247-024-01673-4
Afficher plus [+] Moins [-]Exploring molecular biomarkers in lava tube speleothems offers insights into environmental dynamics, biogeochemical processes, and subsurface life, with implications for astrobiology, particularly in Martian analog environments. Despite extensive biomarker research in marine and terrestrial settings, lava tube studies are limited. This study employed molecular, isotope and mineralogical characterization to analyze sulfate speleothems from six lava tubes of Lanzarote (Canary Islands), considered analog for the Moon and Mars. The combination of mass spectrometry, thermogravimetry, and mineralogical techniques, revealed geological processes, biomarkers and their biological sources. The identified minerals were primarily calcium and sodium sulfates. Sulfur isotope analyses indicated volcanic and oceanic origins, while carbon isotope composition and pyrolysis analyses suggested influences from vegetation and microbial activity. Lipidic profiles highlighted branched and n-alkanes, as well as palmitic and stearic acid methyl esters, suggesting microbial origins. These findings contribute to understanding geological and environmental dynamics in lava tubes and recognizing potential biosignatures on Earth and other planets.
Afficher plus [+] Moins [-]This work received support from the Spanish Ministry of Science and Innovation (MCIN/AEI 10.13039/501100011033) under the research project TUBOLAN PID2019-108672RJ-I00. We acknowledge the financial support from the Portuguese Foundation for Science and Technology (FCT) under the MICROCENO project (10.54499/PTDC/CTA-AMB/0608/2020) and from the Spanish National Research Council (CSIC) through the intramural project PIE_20214AT021. N.T.J.M. and A.Z.M. were supported by Ramón y Cajal contracts (RyC2021-031253-I and RYC2019-026885-I, respectively) from the MCIN. N.T.J.M. and A.Z.M. also acknowledge the Scientific Employment Stimulus (CEEC) contracts (2021/00711/CEECIND and CEECIND/01147/2017, respectively), funded by FCT.
Afficher plus [+] Moins [-]Peer reviewed
Afficher plus [+] Moins [-]Mots clés AGROVOC
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