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ABIOTIC OXYGEN-DOMINATED ATMOSPHERES ON TERRESTRIAL HABITABLE ZONE PLANETS
Open accessAbstract
Detection of life on other planets requires identification of biosignatures, i.e., observable planetary properties that robustly indicate the presence of a biosphere. One of the most widely accepted biosignatures for an Earth-like planet is an atmosphere where oxygen is a major constituent. Here we show that lifeless habitable zone terrestrial planets around any star type may develop oxygen-dominated atmospheres as a result of water photolysis, because the cold trap mechanism that protects H 2 O on Earth is ineffective when the atmospheric inventory of non-condensing gases (e.g., N 2 , Ar) is low. Hence the spectral features of O 2 and O 3 alone cannot be regarded as robust signs of extraterrestrial life.
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“Wordsworth and Pierrehumbert (2014) investigated oxygen and ozone formation in CO2-rich low-pressure atmospheres.”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Wordsworth and Pierrehumbert, 2014
Citations
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Items 101–167 of 167
Keeping M-Earths habitable in the face of atmospheric loss by sequestering water in the mantle
Moore, K., & Cowan, N. B. (2020) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/staa1796 · Cited by 26
“…al. 2018; Fleming et al. 2020); the lighter hydrogen is lost to space, while the heavier oxygen remains behind, either reacting with the surface or accumulating in the atmosphere and creating a biosignature false positive (see, e.g., Wordsworth & Pierrehumbert 2013, 2014; Wordsworth et al. 2018).”
BackgroundEffect of O3 on the atmospheric temperature structure of early Mars
von Paris, P., Selsis, F., Godolt, M., Grenfell, J. L., Rauer, H., & Stracke, B. (2015) · Icarus · doi:10.1016/j.icarus.2015.05.028 · Cited by 18
“g studies suggests that ozone can be formed from abiotically produced oxygen (e.g., Selsis et al. 2002, Segura et al. 2007, Domagal-Goldman and Meadows 2010; DomagalGoldman et al. 2014). In addition, Wordsworth and Pierrehumbert (2014) propose a (non-chemical) abiotic oxygen formation process based on hydrogen escape…”
BackgroundMethodInfluentialClimate diversity in the solar-like habitable zone due to varying background gas pressure
Paradise, A., Fan, B. L., Kristen Menou, A., & Lee, C. (2021) · Icarus · doi:10.1016/j.icarus.2020.114301 · Cited by 21
Ding, F., & Wordsworth, R. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/ab204f · Cited by 16
Self-citationThe Radiation Environment of Exoplanet Atmospheres
Linsky, J. L. (2014) · Challenges · doi:10.3390/challe5020351 · Cited by 17
“While several authors [7,11,42] have argued that the presence of atmospheric oxygen in various forms may not by itself be a robust biosignature, this question remains an important topic of debate.”
BackgroundSafonova, M., Murthy, J., & Shchekinov, Y. A. (2015) · International Journal of Astrobiology · doi:10.1017/s1473550415000208 · Cited by 25
Abiotic molecular oxygen production—Ionic pathway from sulfur dioxide
Wallner, M., Jarraya, M., Olsson, E., Ideböhn, V. D., Squibb, R. J., Yaghlane, S. B., Nyman, G., Eland, J. H. D., Feifel, R., & Hochlaf, M. (2022) · Science Advances · doi:10.1126/sciadv.abq5411 · Cited by 22
Bourgalais, J., Carrasco, N., Changeat, Q., Vénot, O., Jovanović, L., Pernot, P., Tennyson, J., Chubb, K. L., Yurchenko, S. N., & Tinetti, G. (2020) · The Astrophysical Journal · doi:10.3847/1538-4357/ab8e2d · Cited by 24
“…during the early phase of their evolution through interaction with the most abundant molecular species, but its long-term effect on the habitability of planets is complex and remains an open question (Wordsworth & Pierrehumbert 2014; Luger & Barnes 2015; Bolmont et al. 2016; Owen & Mohanty 2016).”
BackgroundMethodThe effect of high nitrogen pressures on the habitable zone and an appraisal of greenhouse states
Ramirez, R. M. (2020) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/staa603 · Cited by 16
“Moreover, the background nitrogen pressure is not only important for maintaining habitability on a planet (Goldblatt et al. 2009; Wordsworth and Pierrehumbert 2014), but atmospheric nitrogen pressure may reflect its speciation in the mantle and can directly influence the amount of oxygen released…”
BackgroundLimitation of Atmospheric Composition by Combustion–Explosion in Exoplanetary Atmospheres
Grenfell, J. L., Gebauer, S., Godolt, M., Stracke, B., Lehmann, R., & Rauer, H. (2018) · The Astrophysical Journal · doi:10.3847/1538-4357/aab2a9 · Cited by 16
Global or Local Pure Condensible Atmospheres: Importance of Horizontal Latent Heat Transport
Ding, F., & Pierrehumbert, R. (2018) · Astrophysical Journal · doi:10.3847/1538-4357/aae38c · Cited by 14
“…atmospheres themselves are of potential interest for very water-rich planets, but it is unclear if such atmospheres can exist except as transients because the absence of cold-trapping generally leads to hydrogen escape and buildup of a noncondensible O2 atmosphere (Wordsworth & Pierrehumbert 2014).”
BackgroundSelf-citationFox, S., & Strasdeit, H. (2017) · Frontiers in Microbiology · doi:10.3389/fmicb.2017.01622 · Cited by 19
“This view, however, has been challenged by the argument that abiotic water photolysis on a habitable-zone planet can also produce an oxygendominated atmosphere and thus may result in a false positive for life (Wordsworth and Pierrehumbert, 2014).”
BackgroundAmmonia and Phosphine in the Clouds of Venus as Potentially Biological Anomalies
Cleland, C. E., & Rimmer, P. B. (2022) · Aerospace · doi:10.3390/aerospace9120752 · Cited by 13
Venus as an Analog for Hot Earths
Arney, G. (2005) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816540068-ch014 · Cited by 12
“On Venus, it has been proposed that oxygen liberated by H2O photolysis and water loss (described in Section 3) could have been absorbed by the mantle, increasing its oxygen fugacity and releasing N2 to the atmosphere (Wordsworth and Pierrehumbert 2014).”
BackgroundInfluentialRemote Sensing of Potential Biosignatures from Rocky, Liquid, or Icy (Exo)Planetary Surfaces
Poch, O., Frey, J., Roditi, I. J., Pommerol, A., Jöst, B., & Thomas, N. (2017) · Astrobiology · doi:10.1089/ast.2016.1523 · Cited by 14
“But confirming their biogenic origin will require ruling out their possible production via abiotic processes such as geology or atmospheric chemistry (Domagal-Goldman et al., 2014; Tian et al., 2014; Wordsworth and Pierrehumbert, 2014; Harman et al., 2015).”
A CATALOG OF STELLAR EVOLUTION PROFILES AND THE EFFECTS OF VARIABLE COMPOSITION ON HABITABLE SYSTEMS
Truitt, A., Young, P. A., Spacek, A., Probst, L., & Dietrich, J. (2015) · The Astrophysical Journal · doi:10.1088/0004-637x/804/2/145 · Cited by 21
“…biosignatures, although recently that idea has been called into question; it has become more apparent that oxygen present in a planetary atmosphere may not necessarily indicate any sort of biogenic process (Domagal-Goldman et al. 2014; Wordsworth & Pierrehumbert 2014; Luger & Barnes 2015).”
BackgroundHall, S., Krissansen‐Totton, J., Robinson, T. D., Salvador, A., & Fortney, J. J. (2023) · The Astronomical Journal · doi:10.3847/1538-3881/ad03e9 · Cited by 12
Kaltenegger, L., Lin, Z., & Rugheimer, S. (2020) · The Astrophysical Journal · doi:10.3847/1538-4357/abb9b2 · Cited by 17
“…ozone in a terrestrial planet’s atmosphere through photolysis of H2O or CO2, for planets e.g. with low-H2/high-CO2 atmospheres (Domagal-Goldman et al. 2014), with lowpressure atmospheres (Wordsworth & Pierrehumbert 2014) or CO2-rich atmospheres orbiting M dwarfs (Hu et al. 2012; Tian et al. 2014).”
BackgroundBiosignature surveys to exoplanet yields and beyond
Sandora, M., & Silk, J. I. (2020) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/staa1284 · Cited by 12
“Most known abiotic production mechanisms produce a very high atmospheric O/H ratio, which leads to a lack of water vapor (Gao et al. (2015)) and clouds (Wordsworth & Pierrehumbert (2014)), and so can be ruled out if atmospheric water content is accurately measured.”
BackgroundJoseph, R. G., Duxbury, N. S., Kidron, G. J., Gibson, C. H., & Schild, R. E. (2020) · Open Astronomy · doi:10.1515/astro-2020-0020 · Cited by 8
Harman, C. E., & Domagal-Goldman, S. D. (2018) · Springer eBooks · doi:10.1007/978-3-319-55333-7_71 · Cited by 8
“For the gentler water loss mechanism outlined by Wordsworth and Pierrehumbert (2014), measuring the amount of N 2 directly is very difficult, but much like O 2 there exists a spectrally active dimer (N 2 -”
InfluentialThe Fundamental Connections between the Solar System and Exoplanetary Science
Kane, S. R., Arney, G., Byrne, P. K., Dalba, P. A., Desch, S. J., Horner, J., Izenberg, N. R., Mandt, K. E., Meadows, V. S., & Quick, L. C. (2021) · Journal of Geophysical Research Planets · doi:10.1029/2020je006643 · Cited by 41
Habitable zone predictions and how to test themPreprint
Ramirez, R. M., Abbot, D. S., Fujii, Y., Hamano, K., Kite, E. S., Levi, A., Lingam, M., Lueftinger, T., Robinson, T. D., Rushby, A., et al. (2019) · arXiv (Cornell University) · doi:10.48550/arxiv.1903.03706 · Cited by 6
“Such a process also leads to build up of abiotic oxygen, which has been argued to suggest uninhabitable conditions [39].”
BackgroundSelf-citationThe Inner Solar System's Habitability Through Time
Genio, A. D., Brain, D., Noack, L., & Schaefer, L. (2018) · doi:10.48550/arxiv.1807.04776 · Cited by 10
“ting H atoms can escape to space. The extent to which this occurs depends on the strength of the tropopause cold trap, which depends on the partial pressure of non-condensing gases in the atmosphere (Wordsworth and Pierrehumbert, 2014; Kleinböhl et al., 2018). Thus diffusion-limited escape of H can be tied to troposph…”
BackgroundAncient air caught by shooting stars
Zahnle, K., & Buick, R. (2016) · Nature · doi:10.1038/533184a · Cited by 9
Wavelength Requirements for Life Detection via Reflected Light Spectroscopy of Rocky Exoplanets
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“For this study, we considered only low noncondensable oxygen false positives (Wordsworth and Pierrehumbert, 2014), waterworld oxygen false positives (Krissansen-Totton et al., 2021), photochemical oxygen false positives (Gao et al., 2015), methane degassing false positives (Wogan et al., 2020), and…”
InfluentialTracing the inner edge of the habitable zone with sulfur chemistry
Jordan, S., Shorttle, O., & Rimmer, P. (2025) · Science Advances · doi:10.1126/sciadv.adp8105 · Cited by 8
“…limits on the oxygen abundance would imply, suggesting that there are unknown mechanisms for enriching the ratio of O 3 : O 2 in planetary atmospheres ( 11 , 12 ); (iii) oxygenated atmospheres may be produced on planets as a result of passing through the runaway greenhouse transition ( 13 , 14 ).”
Implications of Abiotic Oxygen Buildup for Earth-like Complex Life
Lingam, M. (2020) · The Astronomical Journal · doi:10.3847/1538-3881/ab737f · Cited by 6
“A number of models suggest that high XUV fluxes play a vital role in the buildup of massive O2 atmospheres by way of desiccation and photolysis (Kasting 1988; Wordsworth & Pierrehumbert 2014; Ramirez & Kaltenegger 2014; Luger & Barnes 2015; Bolmont et al. 2017; Palubski et al. 2020).”
BackgroundBiosignatures Search in Habitable Planets
Claudi, R., & Alei, E. (2019) · Galaxies · doi:10.3390/galaxies7040082 · Cited by 14
The first high frequency technosignature search survey with the Sardinia Radio Telescope
Manunza, L., Vendrame, A., Pizzuto, L., Mulas, M., Perez, K. I., Gajjar, V., Melis, A., Pilia, M., Perrodin, D., Aresu, G., et al. (2025) · Acta Astronautica · doi:10.1016/j.actaastro.2025.04.007 · Cited by 9
“However, due to the limitations of atmospheric characterization for such distant systems, any detected biosignatures could also result from abiotic processes [1] and Fig.”
Fisher, T. M., Janin, E., & Walker, S. I. (2025) · The Planetary Science Journal · doi:10.3847/psj/adcc27 · Cited by 5
“…— most prevalent among them O 2 — have come under more scrutiny due to the risks for false positives ( S. D. Domagal-Goldman et al. 2014; R. Wordsworth & R. Pierrehumbert 2014; C. E. Harman & S. Domagal-Goldman 2018; V. S. Meadows et al. 2018 ) and false negatives ( C. T. Reinhard et al.…”
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BackgroundCharacteristics of aquatic biospheres on temperate planets around Sun-like stars and M dwarfs
Lingam, M., & Loeb, A. (2021) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stab611 · Cited by 7
Okuya, A., Fujii, Y., & Ida, S. (2019) · The Astrophysical Journal · doi:10.3847/1538-4357/ab29e7 · Cited by 8
Late Delivery of Nitrogen to the Earth
Chen, C., Smallwood, J. L., Martin, R. G., & Livio, M. (2019) · The Astronomical Journal · doi:10.3847/1538-3881/aaf96a · Cited by 6
“The nitrogen content in the atmosphere plays a significant role in the rate of water–loss from a planet (e.g. Wordsworth & Pierrehumbert 2013, 2014).”
BackgroundPhotochemical Oxygen in Non-1-bar CO2 Atmospheres of Terrestrial Exoplanets
James, T., & Hu, R. (2018) · The Astrophysical Journal · doi:10.3847/1538-4357/aae2bb · Cited by 10
“In the case of an N2-dominated atmosphere, it has been shown that if the partial pressure of N2 is too small, water vapor cannot be trapped in the troposphere and the upper part of the atmosphere would be wet (Wordsworth & Pierrehumbert 2014).”
BackgroundThe high-energy radiation environment of the habitable-zone super-Earth LHS 1140b
Spinelli, R., Borsa, F., Ghirlanda, G., Ghisellini, G., Campana, S., Haardt, F., & Poretti, E. (2019) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201935636 · Cited by 11
“…greenhouse effect after planet formation due to the superluminous pre-main sequence phase of M-dwarfs (Luger & Barnes 2015), or in atmospheres with low amounts of noncondensing gases without a cold trap (Wordsworth & Pierrehumbert 2014; see also Schwieterman et al. 2018 for a recent review).”
BackgroundThe Drake Equation as a Function of Spectral Type and Time
Haqq-Misra, J. D., & Kopparapu, R. (2018) · Elsevier eBooks · doi:10.1016/b978-0-12-811940-2.00013-7 · Cited by 7
“Some calculations with climate and photochemistry models suggest abiotic sources for O2 and O3 (Segura et al., 2007; Domagal-Goldman et al., 2014; Wordsworth and Pierrehumbert, 2014), although such a ‘false positive’ spectral signature might be discernable from inhabited planets by the detection of species such as CO…”
BackgroundA next step in exoplanetology: exo-moons
Schneider, J. L., Lainey, V. J., & Cabrera, J. (2015) · International Journal of Astrobiology · doi:10.1017/s1473550414000299 · Cited by 16
“The possibility of this configuration is strengthened by the possibility of abiotic oxygen-dominated atmospheres on terrestrial HZ planets (Wordsworth & Pierrehumbert 2014).”
BackgroundThe Early Earth as an Analogue for Exoplanetary Biogeochemistry
Stüeken, E. E., Olson, S. L., Moore, E. K., & Foley, B. J. (2024) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2024.90.14 · Cited by 5
The Origin of Earth's Mantle Nitrogen: Primordial or Early Biogeochemical Cycling?
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“Our study suggests that the pN2 of extrasolar rocky planets in habitable zones may provide useful constraints not only on present climate (Vladilo et al., 2013; Wordsworth & Pierrehumbert, 2014) but also on the biogeochemical processes that have acted on such planets.”
BackgroundGebauer, S., Vilović, I., Grenfell, J. L., Wunderlich, F., Schreier, F., & Rauer, H. (2021) · The Astrophysical Journal · doi:10.3847/1538-4357/abd9cc · Cited by 5
Retrievals Applied to a Decision Tree Framework Can Characterize Earthlike Exoplanet Analogs
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“Atmospheric pressure is included in the decision tree to rule out a low pressure atmosphere false positive for O 2 that can leave interpretation of O 2 in absence of a detection of CH 4 ambiguous for modern Earth (Wordsworth & Pierrehumbert 2014).”
BackgroundCritical review on the origin of atmospheric oxygen: Where is organic matter?
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Euhabitability: A New Term to Aid in the Search for Life in Addition to the Habitable Zone Framework
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“Additionally, planets with global surface oceans may accumulate abiotic O 2 with no geologic sinks, resulting in a false positive biosigna-ture (Wordsworth and Pierrehumbert 2014; Kleinböhl et al. 2018; Krissansen-Totton et al. 2021b).”
ThousandWorlds: A benchmark for climate emulation of potentially habitable exoplanets
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“But these signatures are ambiguous – does an O 2 detection mean life, or just photodissociation of water [Wordsworth and Pierrehumbert, 2014]?”
Walton, C. R., White, & Rimmer, P. B. (2026) · Astrobiology · doi:10.1177/15311074261435780 · Cited by 2
“…interact with oxygen at all but that either affect the climate (and therefore the abundance of oxygen-containing condensable molecules, like water, in the atmosphere) (Wordsworth and Pierrehumbert, 2014) or that affect the transport of ultraviolet light through the atmosphere (Rimmer et al., 2019).”
The Diversity of Planetary Atmospheric Chemistry
Mills, F. P., Moses, J. I., Gao, P., & Tsai, S. (2021) · Space Science Reviews · doi:10.1007/s11214-021-00810-1 · Cited by 3
Collapse of the General Circulation in Shortwave-absorbing Atmospheres: An Idealized Model Study
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“Higher concentrations of ozone due to either biological or abiotic (Wordsworth & Pierrehumbert 2014; Luger & Barnes 2015) oxygen production can also enhance the shortwave absorption from Sun-like stars.”
BackgroundSelf-citationThe Habitability of GJ 357D: Possible Climate and Observability
Kaltenegger, L., Madden, J., Lin, Z., Rugheimer, S., Segura, A., Luque, R., Pallé, E., & Espinoza, N. (2019) · The Astrophysical Journal Letters · doi:10.3847/2041-8213/ab3d40 · Cited by 6
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“The former is not a good choice because abiotic oxygen might arise as result of photodissociation of water molecules (Wordsworth and Pierrehumbert 2014); the latter is not a good choice because the controversial discovery of methane on Mars is still so difficult to understand that a new paper on…”
BackgroundUV astronomy and the investigation of the origin of life
de Castro, A. I. G., & Canet, A. (2021) · Elsevier eBooks · doi:10.1016/b978-0-12-819170-5.00002-6 · Cited by 7
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“Ocean salinity can also be important in modulating the climate of rocky planets (Olson et al., 2022).”
Currie, M. H., & Meadows, V. (2025) · The Planetary Science Journal · doi:10.3847/psj/adc004 · Cited by 4
“We can also consider other gas disequilibria as an indicator for life: CO 2 and CH 4 may be an alternative pair of biosignature disequilibrium gases that were first proposed for Earth’s O 2 -poor ancient Archean atmosphere (Krissansen-Totton et al. 2018; Meadows et al. 2023).”
Vilović, I., Schulze‐Makuch, D., & Heller, R. (2023) · Scientific Reports · doi:10.1038/s41598-023-39716-z · Cited by 6
“Measuring atmospheric biosignatures of terrestrial exoplanets and interpreting atmospheric features in terms of such chemical disequilib-ria, however, are non-trivial tasks 50,55–57 .”
Climate Diversity in the Habitable Zone due to Varying pN$_2$ Levels
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“…for longer continuous integration times, and tidally-locked planets at moderate insolations typically have sea ice fractions above 0.5 due to the cold night-side, with open ocean only found near the center of the day-side (Pierrehumbert, 2011; Heng and Vogt, 2011; Yang et al., 2013, 2014).”
BackgroundInfluentialThe Power of Self-Skepticism in Astrobiology
Domagal-Goldman, S. (2017) · Astrobiology · doi:10.1089/ast.2017.1764 · Cited by 2
RETRACTED ARTICLE: Exoplanet Habitability: Potential O2/O3 Biosignatures in the Ultraviolet
Sachkov, M. E., & Shematovich, V. I. (2019) · Solar System Research · doi:10.1134/s003809461905006x · Cited by 1
RetractedYoung, A. V., Arney, G., Domagal-Goldman, S. D., Robinson, T. D., Juanola-Parramon, R., Stark, C., Hu, R.-Y., Tokadjian, A., & Damiano, M. (2026) · doi:10.48550/arxiv.2610.19081
“52–55 In this study, we focus on a different regime where these Proterozoic Earth-like atmospheres are weakly oxygenated and fundamentally assume that O 2 is biologically sourced at the 0.1% and 1% PAL, but the emphasis on evaluating species detections based on the atmospheric and environmental…”
InfluentialJaziri, Y., Carrasco, N., & Charnay, B. (2026) · Scientific Reports · doi:10.1038/s41598-026-37144-3 · Cited by 2
“As O 3 abundance is more pronounced on our TRAPPIST-1e scenario than on Earth (see Fig.”
Lichtenberg, T., Schaefer, L., Krissansen‐Totton, J., Miguel, Y., Sergeev, D. E., Baumeister, P., Cmiel, J., Janssen, L. J., Nguyen, T. G., Miyazaki, Y., et al. (2026) · The Planetary Science Journal · doi:10.3847/psj/ae593b · Cited by 9
“The super-luminous pre-main sequence of M-dwarfs may drive extreme rates of H 2 O photolysis and hydrogen escape, causing O 2 buildup that could later mimic an in-habited planet with oxygen production via photosynthesis (R. Luger & R. Barnes 2015; R. Wordsworth & R. Pierrehumbert 2014).”
Parkinson, C. D., Bougher, S. W., Mills, F. P., Yung, Y. L., Brecht, A. S., Li, J., Hu, R., & Gronoff, G. (2025) · Journal of Geophysical Research Planets · doi:10.1029/2024je008540
“This is consistent with previous work published by other authors discussing habitable zone placement (e.g., Kasting, 1995; Luger & Barnes, 2015; Meadows, 2017; Wordsworth & Pierrehumbert, 2014).”
Exoplanetary Biosignatures for Astrobiology
Grenfell, J. L. (2018) · Advances in astrobiology and biogeophysics · doi:10.1007/978-3-319-96175-0_11 · Cited by 4
The Imprecise Search for Habitability
Heng, K. (2016) · doi:10.48550/arxiv.1604.05078
Sanders, C. (2014) · Zenodo (CERN European Organization for Nuclear Research) · doi:10.5281/zenodo.31745
“If O2 is abiogenically produced by the high-energy irradiation of surface oceans, there could be a mass-independent effect distinct from the effect of oxygenic photosynthesis (Wordsworth & Pierrehumbert 2014).”
BackgroundHost Star Driven Photochemistry in Exoplanet Atmospheres
Linsky, J. L. (2019) · Lecture notes in physics · doi:10.1007/978-3-030-11452-7_11
Reinhard, C. T., Schwieterman, E. W., Olson, S. L., Planavsky, N. J., Arney, G. N., Ozaki, K., Som, S., Robinson, T. D., Domagal-Goldman, S. D., Lisman, D., et al. (2019) · arXiv · doi:10.48550/arxiv.1903.05611 · Cited by 7
“…phase water loss around M-stars [Luger and Barnes, 2015] and slow hydrogen escape from thin atmospheres lacking noncondensible gases [Wordsworth and Pierrehumbert, 2014] (previous scenarios invoking CO2 photolysis [Tian et al., 2014; Harman et al., 2015] have recently been shown to result from a…”
BackgroundInfluential
Metadata
- Authors
- Wordsworth, R., & Pierrehumbert, R.
- Affiliations
- University of Chicago (US)
- Venue
- The Astrophysical Journal
- Publisher
- American Astronomical Society
- Published
- 2014-04-01
- Volume
- 785
- Issue
- 2
- Pages
- L20
- ISSN
- 2041-8205 (ISSN-L)
- 2041-8213
- OpenAlex
- W2101682039
- Cited by
- 222
- References
- 28
- Citations by year
- 2026: 15 · 2025: 16 · 2024: 19 · 2023: 12 · 2022: 18 · 2021: 12 · 2020: 26 · 2019: 22 · 2018: 29 · 2017: 21 · 2016: 18 · 2015: 9 · 2014: 4
- FWCI
- 9.34
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- Locations
- The Astrophysical Journal Letters (publishedVersion)
- arXiv (Cornell University) (submittedVersion)
- Digital Access to Scholarship at Harvard (DASH) (Harvard University) (submittedVersion, cc-by)
- arXiv (Cornell University)
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Space Science and Extraterrestrial Life
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Stellar, planetary, and galactic studies
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Keywords
- biosignatures, habitable zone planets, terrestrial planets, water photolysis, atmospheric nitrogen, atmospheric argon, ozone, exoplanet atmospheres, life detection
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