
Earth Extremophile Grows Actively in Simulated Martian Subsurface Brines
UF-led study shows Haloferax volcanii grows under combined low-pressure, high-salinity, anoxic, perchlorate/nitrate conditions simulating Martian brines, adding evidence for possible extant subsurface habitability without claiming life exists there.
University of Florida researchers led by Adam Robinson have demonstrated that the salt-loving archaeon Haloferax volcanii can not only survive but actively grow and metabolize under a combination of conditions mimicking the shallow Martian subsurface. In experiments lasting 160 days, cultures in hypersaline media (over 7 times saltier than seawater) at 24 millibars pressure (about 2% of Earth's sea-level atmosphere), in a nearly pure CO2 anoxic environment at 21°C, showed measurable growth when supplied with nitrate or perchlorate—compounds detected on Mars that serve as alternative electron acceptors. Growth was confirmed via increased optical density, reduction of these chemicals, and biofilm formation that helped retain water (loss below 4%). Without these chemicals, cells remained viable but showed no growth. The peer-reviewed study, published November 5, 2026, in Applied and Environmental Microbiology, builds on a 2022 survival study and a bioRxiv preprint. Researchers emphasize this does not prove life exists on Mars but supports the potential habitability of localized hypersaline niches below the surface, where liquid water might persist despite low pressure and oxidizing conditions. Prior work had tested individual stressors; this combines multiple Mars-relevant factors simultaneously. The team notes limitations, including warmer lab temperatures than typical Martian subsurface and supplied nutrients.
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