Effects of long-term simulated martian conditions on a freeze-dried and homogenized bacterial permafrost community

• Published in: Astrobiology Vol. 9; no. 2; p. 229
• Main Authors: Hansen, Aviaja A, Jensen, Lars L, Kristoffersen, Tommy, Mikkelsen, Karina, Merrison, Jonathan, Finster, Kai W, Lomstein, Bente Aa
• Format: Journal Article
• Language: English
• Published: United States 01.03.2009
• Subjects: Arctic Regions; Atmosphere - chemistry; Atmospheric Pressure; Bacteria - classification; Bacteria - isolation & purification; Bacteria - radiation effects; Base Sequence; Colony Count, Microbial; Dose-Response Relationship, Radiation; Exobiology; Extraterrestrial Environment; Freeze Drying; Freezing; Mars; Microbial Viability - radiation effects; Molecular Sequence Data; Phylogeny; Soil; Space Simulation; Temperature; Time Factors; Ultraviolet Rays
• DOI: 10.1089/ast.2008.0244

Indigenous bacteria and biomolecules (DNA and proteins) in a freeze-dried and homogenized Arctic permafrost were exposed to simulated martian conditions that correspond to about 80 days on the surface of Mars with respect to the accumulated UV dose. The simulation conditions included UV radiation, freeze-thaw cycles, the atmospheric gas composition, and pressure. The homogenized permafrost cores were subjected to repeated cycles of UV radiation for 3 h followed by 27 h without irradiation. The effects of the simulation conditions on the concentrations of biomolecules; numbers of viable, dead, and cultured bacteria; as well as the community structure were determined. Simulated martian conditions resulted in a significant reduction of the concentrations of DNA and amino acids in the uppermost 1.5 mm of the soil core. The total number of bacterial cells was reduced in the upper 9 mm of the soil core, while the number of viable cells was reduced in the upper 15 mm. The number of cultured aerobic bacteria was reduced in the upper 6 mm of the soil core, whereas the community structure of cultured anaerobic bacteria was relatively unaffected by the exposure conditions. As explanations for the observed changes, we propose three causes that might have been working on the biological material either individually or synergistically: (i) UV radiation, (ii) UV-generated reactive oxygen species, and (iii) freeze-thaw cycles. Currently, the production and action of reactive gases is only hypothetical and will be a central subject in future investigations. Overall, we conclude that in a stable environment (no wind-/pressure-induced mixing) biological material is efficiently shielded by a 2 cm thick layer of dust, while it is relatively rapidly destroyed in the surface layer, and that biomolecules like proteins and polynucleotides are more resistant to destruction than living biota.