Iron-rich minerals, such as hematite (α-Fe2O3), are prominent constituents of the Martian surface; they are considered to be potential indicators of past aqueous activity and habitability.
Rhinocladiella similis LaBioMMi 1217
Posted inAnalog Studies, Arctic / Antarctic / Alpine, Away Teams & Field Reports, Biophysics, Biosignatures & Paleobiology, Extremeophiles and Extreme Environments, Mars, Microbiology & Virology, Origin & Evolution of Life, Status Report
Rhinocladiella similis: A Model Eukaryotic Organism for Astrobiological Studies on Microbial Interactions with Martian Soil Analogs
The exploration of our solar system for microbial extraterrestrial life is the primary goal of several space agencies.