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Open AccessJournal ArticleDOI

Reflections on O2 as a Biosignature in Exoplanetary Atmospheres.

Victoria S. Meadows
- 01 Oct 2017 - 
- Vol. 17, Iss: 10, pp 1022-1052
TLDR
Environmental factors for abiotic O2 have been identified and will improve the ability to choose optimal targets and measurements to guard against false positives, and thorough evaluation of potential biosignatures works to increase confidence in life detection.
Abstract
Oxygenic photosynthesis is Earth's dominant metabolism, having evolved to harvest the largest expected energy source at the surface of most terrestrial habitable zone planets. Using CO2 and H2O—molecules that are expected to be abundant and widespread on habitable terrestrial planets—oxygenic photosynthesis is plausible as a significant planetary process with a global impact. Photosynthetic O2 has long been considered particularly robust as a sign of life on a habitable exoplanet, due to the lack of known “false positives”—geological or photochemical processes that could also produce large quantities of stable O2. O2 has other advantages as a biosignature, including its high abundance and uniform distribution throughout the atmospheric column and its distinct, strong absorption in the visible and near-infrared. However, recent modeling work has shown that false positives for abundant oxygen or ozone could be produced by abiotic mechanisms, including photochemistry and atmospheric escape. Environm...

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Citations
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Modeling Repeated M Dwarf Flaring at an Earth-like Planet in the Habitable Zone: Atmospheric Effects for an Unmagnetized Planet.

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Evolved Climates and Observational Discriminants for the TRAPPIST-1 Planetary System

TL;DR: In this paper, a 1D terrestrial-planet climate model with line-by-line radiative transfer and mixing length convection (VPL Climate) coupled with a terrestrial photochemistry model was used to simulate environmental states for the TRAPPIST-1 planets.

Evidence for free oxygen in the Neoarchean ocean based on coupled iron-molybdenum isotope fractionation

TL;DR: In this article, a combination of Fe and Mo isotope systematics of Ca-Mg carbonates and shales from the 2.68 to 2.50 Ga Campbellrand-Malmani carbonate platform of the Kaapvaal Craton in South Africa was used to constrain free O2 levels in the photic zone of a Late Archean marine basin by the combined use of Fe-Mo isotope systems.
References
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Journal ArticleDOI

Evolution of a Habitable Planet

TL;DR: In this article, it is shown that Earth's climate has remained conducive to life for the past 3.5 billion years or more, despite a large increase in solar luminosity, probably because of previous higher concentrations of CO2 and/or CH4.
Journal ArticleDOI

Biogenic methane, hydrogen escape, and the irreversible oxidation of early Earth.

TL;DR: Expected irreversible oxidation (∼1012 to 1013 moles oxygen per year) may help explain how Earth's surface environment became irreversibly oxidized.
Journal ArticleDOI

The rise of atmospheric oxygen

TL;DR: Clues from ancient rocks are helping to produce a coherent picture of how Earth's atmosphere changed from one that was almost devoid of oxygen to one that is one-fifth oxygen.
Journal ArticleDOI

Abiotic methane on earth

TL;DR: In this article, the authors demonstrate that integrated geochemical diagnostic techniques, based on molecular composition of associated gases, noble gas isotopes, mixing models, and a detailed knowledge of the geologic and hydrogeologic context are necessary to confirm the occurrence of abiotic CH4 in natural gases, which are frequently mixtures of multiple sources.
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