Oxygenated False Positive Biosignatures in Mars-like Exoplanet Atmospheres
Margaret Turcotte Seavey, Shawn Domagal-Goldman, Amber Young, Jaime Crouse, Jacob Lustig-Yaeger, and Giada Arney

TL;DR
This study uses photochemical simulations to evaluate abiotic oxygen buildup in Mars-like exoplanet atmospheres, revealing conditions that can produce false positive biosignatures, which is crucial for future exoplanet characterization.
Contribution
It provides a reassessment of abiotic O2 and O3 accumulation mechanisms, showing lower maximum O2 levels due to water vapor effects, refining the understanding of false biosignatures.
Findings
Maximum O2 abundance is about 2.7% at specific hydrogen levels.
Elevated water vapor enhances HOx recycling, reducing O2 and O3 buildup.
Results suggest previous models overestimated abiotic oxygen levels.
Abstract
Oxygen is a well-studied biosignature. Studying potential abiotic pathways for O2 build-up in exoplanet atmospheres is essential for evaluating whether the detection of O2 would constitute a biosignature detection on other worlds. Previous modeling efforts in the literature demonstrated that detectable abiotic O2 and O3 can be produced through CO2 photolysis for rocky planets around M dwarf stars. Building on modeling approaches from previous studies, we use photochemical simulations to reassess the conditions under which O2 and O3 may accumulate through similar photochemical mechanisms. Using a Mars-like atmospheric composition and planetary parameters, we vary the hydrogen mole fraction to assess how changes in HOx chemistry can affect the resulting accumulation of abiotic O2 and O3. Across the range of hydrogen mole fractions explored, we obtain a maximum O2 abundance of ~2.7% for H…
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Taxonomy
TopicsPlanetary Science and Exploration · Astro and Planetary Science · Stellar, planetary, and galactic studies
