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Published February 2020 | Published
Journal Article Open

Phosphine as a Biosignature Gas in Exoplanet Atmospheres

Abstract

A long-term goal of exoplanet studies is the identification and detection of biosignature gases. Beyond the most discussed biosignature gas O₂, only a handful of gases have been considered in detail. In this study, we evaluate phosphine (PH₃). On Earth, PH₃ is associated with anaerobic ecosystems, and as such, it is a potential biosignature gas in anoxic exoplanets. We simulate the atmospheres of habitable terrestrial planets with CO₂- and H₂-dominated atmospheres and find that PH₃ can accumulate to detectable concentrations on planets with surface production fluxes of 10¹⁰ to 10¹⁴ cm⁻² s⁻¹ (corresponding to surface concentrations of 10s of ppb to 100s of ppm), depending on atmospheric composition and ultraviolet (UV) irradiation. While high, the surface flux values are comparable to the global terrestrial production rate of methane or CH₄ (10¹¹ cm⁻² s⁻¹) and below the maximum local terrestrial PH₃ production rate (10¹⁴ cm⁻² s⁻¹). As with other gases, PH₃ can more readily accumulate on low-UV planets, for example, planets orbiting quiet M dwarfs or with a photochemically generated UV shield. PH₃ has three strong spectral features such that in any atmosphere scenario one of the three will be unique compared with other dominant spectroscopic molecules. Phosphine's weakness as a biosignature gas is its high reactivity, requiring high outgassing rates for detectability. We calculate that tens of hours of JWST (James Webb Space Telescope) time are required for a potential detection of PH₃. Yet, because PH₃ is spectrally active in the same wavelength regions as other atmospherically important molecules (such as H₂O and CH₄), searches for PH₃ can be carried out at no additional observational cost to searches for other molecular species relevant to characterizing exoplanet habitability. Phosphine is a promising biosignature gas, as it has no known abiotic false positives on terrestrial planets from any source that could generate the high fluxes required for detection.

Additional Information

© 2019 Mary Ann Liebert, Inc. Submitted 10 September 2018; Accepted 7 October 2019. Online Ahead of Print: November 22, 2019. We thank the MIT BOSE Fellow program and the Change Happens Foundation for partial funding of this work. We thank Elisabeth Matthews, Thomas Evans, Julien de Wit, and Jason Dittmann for their advice on detectability metrics. We also thank Antonio P. Silva, Fionnuala Cavanagh, Catherine Wilka, Sarah Ballard, Sarah Rugheimer, Jennifer Burt, Daniel Koll, Susan Solomon, Andrew Babbin, Tiffany Kataria, Antonio Silva, and Christopher Shea for their support and useful discussions. Finally, we would like to thank our two reviewers, whose contributions significantly improved this article. No competing financial interests exist. This research was supported in part by grants from the Simons Foundation (SCOL; Grant No. 495062 to S.R.), the Heising-Simons Foundation (51 Pegasi b Fellowship to C.SS.), and carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration.

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Created:
August 22, 2023
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October 18, 2023