EGU23-2787
https://doi.org/10.5194/egusphere-egu23-2787
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Chemical identification of fossil filament entrapped in Messinian gypsum using space Laser Mass Spectrometry, application for Mars astrobiology.

Youcef Sellam1, Salome Gruchola1, Matteo Reghizzi2,3, Stefano Lugli3, Andreas Riedo1, and Peter Wurz1
Youcef Sellam et al.
  • 1Physics Institute, University Bern, 3012 Bern, Switzerland
  • 2Department of Chemistry, Life Sciences and Environmental Sustainability, University of Parma, 43121 Parma, Italy
  • 3Department of Chemical and Geological Sciences, University of Modena and Reggio Emilia, 41121 Modena MO, Italy

The search for evidence of extant and extinct life on Mars is of big interest for future robotic and human exploration missions. The properties and characteristics of evaporites such as gypsum make them an easily accessible target in the search for biosignatures of extraterrestrial life. On Earth, a diverse microbial community inhabits gypsum in modern brines. These microbes are easily entombed within gypsum due to its fast precipitation. Studies of primary lower gypsum deposits, accumulated in the Mediterranean Basin during the Messinian salinity crisis (5.97 – 5.33 Ma), revealed a well-preserved and prominent archive of diverse microbial life. Similar archives might exist on Mars considering the desiccation of large bodies of water there, representing a promising target for exploring the possibility of life on Mars. The recent imaging mapping and analysis done by orbiters and rovers on the surface of Mars led to the discovery of abundant gypsum and evaporite minerals suggesting the evaporation of large lakes and lacustrine systems and as the surface of Mars dried out, hypersaline lakes would have filled the ancient lake system. A similar scenario happened on Earth when thick layers of gypsum were deposited during the Messinian salinity crisis when the Mediterranean was turned into the youngest salt giant in Earth’s history.

Previous chemical and molecular laser mass spectrometry analyses done on microfossils preserved in different rock records showed these instruments’ ability to detect biosignatures related to ancient life. In this study, we successfully investigated the chemical composition of fossil filaments interpreted to be benthic microbial assemblages dominated by chemotrophic sulfide-oxidizing bacteria, sulfate-reducing bacteria, and planktonic cyanobacteria. This study demonstrated the efficiency of a miniaturized next-generation Laser based Mass Spectrometer (LMS) designed for future space explorations in the detection of microbial chemical biosignatures trapped in Messinian gypsum, shading light to the potential application to the search for life on Mars.

 

 

 

 

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How to cite: Sellam, Y., Gruchola, S., Reghizzi, M., Lugli, S., Riedo, A., and Wurz, P.: Chemical identification of fossil filament entrapped in Messinian gypsum using space Laser Mass Spectrometry, application for Mars astrobiology., EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-2787, https://doi.org/10.5194/egusphere-egu23-2787, 2023.