P024-0003
Life Detection in Gypsum-Rich Environments: Lessons for Space Exploration
Abstract:
Field observation and petrographic microscopy revealed that this gypsum is likely primary, conclusions supported by previous researchers. Gas chromatography/mass spectroscopy analyses demonstrated that samples from the Blaine Formation contain biomarkers, while the shale units found stratigraphically above and below did not. Similarly, fluorescence microscopy established that the Blaine Formation contains autofluorescing compounds within equant gypsum crystals, unlike either of the adjoining units. Together, these techniques suggest that this gypsum contains the remnants of an ancient Permian microbial mat: the morphology of the gypsum crystals is consistent with those precipitated in the presence of organic inhibitors, the biomarker distribution is identical to that found in modern microbial mats growing in gypsum-precipitating environments, and the distribution and color of the autofluorescing compounds speaks to aliphatic hydrocarbons trapped within the mineral lattice. This study shows that combining techniques from various fields and examining samples from environments that are not usual targets for searching for signs of life on Earth can help develop further strategies for off-planet life detection.