Investigating Microbial Biosignatures in Aeolian Environments Using Micro-X-Ray: Simulation of PIXL Instrument Analyses at Jezero Crater Onboard the Perseverance Mars 2020 Rover

被引:0
作者
Nachon, Marion [1 ]
Ewing, Ryan C. [1 ]
Tice, Michael M. [1 ]
Williford, Blake [2 ]
Marounina, Nadejda [3 ,4 ]
机构
[1] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA
[2] Texas A&M Univ, Dept Comp Sci & Engn, College Stn, TX USA
[3] Univ Chicago, Dept Astron & Astrophys, Chicago, IL 60637 USA
[4] Swiss Fed Inst Technol, Zurich, Switzerland
关键词
Biosignature; Microbial mats; X-ray fluorescence; Aeolian; Analogue; Mars rover; MERIDIANI-PLANUM; MATS; ISLAND; LIFE; SEDIMENTS; STROMATOLITES; DEPOSITS; MEXICO; ANALOG; BELT;
D O I
10.1089/ast.2022.0031
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Assessing the past habitability of Mars and searching for evidence of ancient life at Jezero crater via the Perseverance rover are the key objectives of NASA's Mars 2020 mission. Onboard the rover, PIXL (Planetary Instrument for X-ray Lithochemistry) is one of the best suited instruments to search for microbial biosignatures due to its ability to characterize chemical composition of fine scale textures in geological targets using a nondestructive technique. PIXL is also the first micro-X-ray fluorescence (XRF) spectrometer onboard a Mars rover. Here, we present guidelines for identifying and investigating a microbial biosignature in an aeolian environment using PIXL-analogous micro-XRF (mu XRF) analyses. We collected samples from a modern wet aeolian environment at Padre Island, Texas, that contain buried microbial mats, and we analyzed them using mu XRF techniques analogous to how PIXL is being operated on Mars. We show via mu XRF technique and microscope images the geochemical and textural variations from the surface to similar to 40 cm depth. Microbial mats are associated with heavy-mineral lags and show specific textural and geochemical characteristics that make them a distinct biosignature for this environment. Upon burial, they acquire a diffuse texture due to the expansion and contraction of gas-filled voids, and they present a geochemical signature rich in iron and titanium, which is due to the trapping of heavy minerals. We show that these intrinsic characteristics can be detected via mu XRF analyses, and that they are distinct from buried abiotic facies such as cross-stratification and adhesion ripple laminations. We also designed and conducted an interactive survey using the Padre Island mu XRF data to explore how different users chose to investigate a biosignature-bearing dataset via PIXL-like sampling strategies. We show that investigating biosignatures via PIXL-like analyses is heavily influenced by technical constraints (e.g., the XRF measurement characteristics) and by the variety of approaches chosen by different scientists. Lessons learned for accurately identifying and characterizing this biosignature in the context of rover-mission constraints include defining relative priorities among measurements, favoring a multidisciplinary approach to the decision-making process of XRF measurements selection, and considering abiotic results to support or discard a biosignature interpretation. Our results provide guidelines for PIXL analyses of potential biosignature on Mars.
引用
收藏
页码:498 / 517
页数:20
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