Astrobiological Potential of Venus Atmosphere Chemical Anomalies and Other Unexplained Cloud Properties
arXiv:2401.04708 · doi:10.1089/ast.2022.0060
Abstract
Long-standing unexplained Venus atmosphere observations and chemical anomalies point to unknown chemistry but also leave room for the possibility of life. The unexplained observations include several gases out of thermodynamic equilibrium (e.g. tens of ppm O2, the possible presence of PH3 and NH3, SO2 and H2O vertical abundance profiles), an unknown composition of large, lower cloud particles, and the "unknown absorber(s)". Here we first review relevant properties of the Venus atmosphere and then describe the atmospheric chemical anomalies and how they motivate future astrobiology missions to Venus.
Published in Astrobiology (in press); Partially based on the text of the Venus Life Finder Mission Study report (arXiv:2112.05153)
References in corpus (17)
- Re-analysis of the 267-GHz ALMA observations of Venus: No statistically significant detection of phosphine
- Claimed detection of PH in the clouds of Venus is consistent with mesospheric SO
- The statistical reliability of 267 GHz JCMT observations of Venus: No significant evidence for phosphine absorption
- Rocket Lab Mission to Venus
- Complications in the ALMA Detection of Phosphine at Venus
- Venus Life Finder Missions Motivation and Summary
- Phosphine in the Venusian Atmosphere: A Strict Upper Limit from SOFIA GREAT Observations
- Venus' Atmospheric Chemistry and Cloud Characteristics Are Compatible with Venusian Life
- Mission Architecture to Characterize Habitability of Venus Cloud Layers via an Aerial Platform
- Deducing the Composition of Venus Cloud Particles with the Autofluorescence Nephelometer (AFN)
- Constraints on the production of phosphine by Venusian volcanoes
- Aerial Platform Design Options for a Life-Finding Mission at Venus
- Venusian phosphine: a 'Wow!' signal in chemistry?
- A Simple Condensation Model for the H2SO4-H2O Gas-cloud System on Venus
- Venus Life Finder Habitability Mission: Motivation, Science Objectives, and Instrumentation
- Fully fluorinated non-carbon compounds NF3 and SF6 as ideal technosignature gases
- Large Uncertainties in the Thermodynamics of Phosphorus (III) Oxide (PO) Have Significant Implications for Phosphorus Species in Planetary Atmospheres