scispace - formally typeset
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...

read more

Citations
More filters
Journal Article

Evolution of a Habitable Planet

TL;DR: In this paper, 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 CO 2 and/or CH4.
Journal ArticleDOI

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

TL;DR: In this article, the impact of active M dwarf stars on the atmospheric equilibrium and surface conditions of a habitable zone Earth-like planet is investigated, which is key to assessing M dwarf planet habitability.
Journal ArticleDOI

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
More filters
Journal ArticleDOI

A Decreased Probability of Habitable Planet Formation around Low-Mass Stars

TL;DR: In this article, the authors use dynamical simulations of terrestrial planet formation from planetary embryos and simple scaling arguments to explore the implications of correlations between terrestrial planet mass, disk mass, and the mass of the parent star.
Journal ArticleDOI

Seasonal amplitude increase in atmospheric CO2 concentration at Mauna Loa, Hawaii, 1959–1982

TL;DR: In this paper, a detailed examination of methods of calibration and of data analysis during this long record do not reveal any inconsistencies large enough to be responsible for the increase in CO/sub 2/ in the northern hemisphere.
Journal ArticleDOI

Isotopic evidence for an aerobic nitrogen cycle in the latest Archean.

TL;DR: Complementary molybdenum abundance and sulfur isotopic values suggest that nitrification occurred in response to a small increase in surface-ocean oxygenation, implying that nitrifying and denitrifying microbes had already evolved by the late Archean and were present before oxygen first began to accumulate in the atmosphere.
Journal ArticleDOI

The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth.

TL;DR: In this article, the authors present simulations of a habitable yet dramatically different phase of Earth's history, when the atmosphere contained a Titan-like, organic-rich haze, and demonstrate using coupled climate-photochemical-microphysical simulations that hazes can cool the planet's surface by about 20 K, but habitable conditions with liquid surface water could be maintained with a relatively thick haze layer (τ∼∼5 at 200nm) even with the fainter young Sun.
Related Papers (5)