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 (33)
- Phosphine Gas in the Cloud Decks of Venus
- Revealing the Mysteries of Venus: The DAVINCI Mission
- Venusian Habitable Climate Scenarios: Modeling Venus through time and applications to slowly rotating Venus-Like Exoplanets
- The Venusian Lower Atmosphere Haze as a Depot for Desiccated Microbial Life: A Proposed Life Cycle for Persistence of the Venusian Aerial Biosphere
- No evidence of phosphine in the atmosphere of Venus by independent analyses
- Venus' Mass Spectra Show Signs of Disequilibria in the Middle Clouds
- The long-term evolution of the atmosphere of Venus: processes and feedback mechanisms
- Phosphine on Venus Cannot be Explained by Conventional Processes
- Re-analysis of the 267-GHz ALMA observations of Venus: No statistically significant detection of phosphine
- A stringent upper limit of the PH abundance at the cloud top of Venus
- 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
- Re-analysis of Phosphine in Venus' Clouds
- Recovery of Spectra of Phosphine in Venus' Clouds
- Stability of nucleic acid bases in concentrated sulfuric acid: Implications for the habitability of Venus' clouds
- Low levels of sulphur dioxide contamination of Venusian phosphine spectra
- Venus' Atmospheric Chemistry and Cloud Characteristics Are Compatible with Venusian Life
- The Venus Life Equation
- 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
- The CO Profile and Analytical Model for the Pioneer Venus Large Probe Neutral Mass Spectrometer
- Venusian phosphine: a 'Wow!' signal in chemistry?
- A Simple Condensation Model for the H2SO4-H2O Gas-cloud System on Venus
- Fully fluorinated non-carbon compounds NF3 and SF6 as ideal technosignature gases
- Proposed energy-metabolisms cannot explain the atmospheric chemistry of Venus
- Venus Life Finder Habitability Mission: Motivation, Science Objectives, and Instrumentation
- Large Uncertainties in the Thermodynamics of Phosphorus (III) Oxide (PO) Have Significant Implications for Phosphorus Species in Planetary Atmospheres
Cited by in corpus (5)
- Stability of nucleic acid bases in concentrated sulfuric acid: Implications for the habitability of Venus' clouds
- Venus' Atmospheric Chemistry and Cloud Characteristics Are Compatible with Venusian Life
- Simple lipids form stable higher-order structures in concentrated sulfuric acid
- Venus Cloud Research: Progress and Perspectives
- The effect of a biosphere on the habitable timespan of stagnant-lid planets and implications for the atmospheric spectrum