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Investigating Microbial Biosignatures in Aeolian Environments Using Micro-X-Ray: Simulation of PIXL Instrument
Marion Nachon1, Ryan C Ewing1, Michael M Tice1
1Department of Geology and Geophysics and Texas A&M University, College Station, Texas, USA.
Astrobiology
|May 20, 2024
Summary
Researchers studied ancient microbial mats in a Mars-analog environment using micro-X-ray fluorescence (μXRF) to identify biosignatures. This helps guide the Planetary Instrument for X-ray Lithochemistry (PIXL) on the Perseverance rover for Mars exploration.
Area of Science:
- Astrobiology and Planetary Science
- Geochemistry and Mineralogy
- Microbiology and Biosignature Detection
Background:
- NASA's Mars 2020 mission, utilizing the Perseverance rover, aims to assess Mars' past habitability and search for ancient life, particularly in Jezero crater.
- The Planetary Instrument for X-ray Lithochemistry (PIXL) is crucial for detecting microbial biosignatures by analyzing fine-scale geological textures and chemical compositions non-destructively.
- PIXL is the first micro-X-ray fluorescence (μXRF) spectrometer deployed on a Mars rover, necessitating the development of effective analytical strategies.
Purpose of the Study:
- To establish guidelines for identifying and investigating microbial biosignatures in aeolian environments using PIXL-analogous μXRF techniques.
- To analyze geochemical and textural variations in buried microbial mats within a modern wet aeolian setting.
- To assess how technical constraints and user approaches influence biosignature investigation using PIXL-like sampling strategies.
Main Methods:
- Collected and analyzed samples from a modern wet aeolian environment at Padre Island, Texas, containing buried microbial mats.
- Employed μXRF techniques analogous to PIXL's operational methods to analyze samples from the surface down to approximately 40 cm depth.
- Conducted an interactive survey using μXRF data to evaluate different user strategies for investigating biosignature-bearing datasets with PIXL-like sampling.
Main Results:
- Microbial mats were identified, associated with heavy-mineral lags, exhibiting distinct textural and geochemical characteristics (rich in iron and titanium) due to trapped minerals.
- Buried microbial mats showed diffuse textures resulting from gas-filled void expansion/contraction, differentiating them from abiotic facies like cross-stratification and adhesion ripple laminations.
- μXRF analysis successfully detected these intrinsic characteristics, confirming their potential as detectable biosignatures. User surveys revealed that technical constraints and diverse scientific approaches significantly impact biosignature investigation.
Conclusions:
- Microbial biosignatures in aeolian environments possess detectable geochemical and textural signatures that can be identified using μXRF analysis, analogous to PIXL's capabilities.
- Effective biosignature detection on Mars requires careful consideration of PIXL's technical constraints, prioritizing measurements, and adopting a multidisciplinary approach.
- Understanding abiotic facies and their signatures is crucial for accurately interpreting potential biosignatures and supporting or refuting their existence in the Martian context.

