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The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth
Open accessAbstract
Recognizing whether a planet can support life is a primary goal of future exoplanet spectral characterization missions, but past research on habitability assessment has largely ignored the vastly different conditions that have existed in our planet's long habitable history. This study presents simulations of a habitable yet dramatically different phase of Earth's history, when the atmosphere contained a Titan-like, organic-rich haze. Prior work has claimed a haze-rich Archean Earth (3.8–2.5 billion years ago) would be frozen due to the haze's cooling effects. However, no previous studies have self-consistently taken into account climate, photochemistry, and fractal hazes. Here, we 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 200 nm) even with the fainter young Sun. We find that optically thicker hazes are self-limiting due to their self-shielding properties, preventing catastrophic cooling of the planet. Hazes may even enhance planetary habitability through UV shielding, reducing surface UV flux by about 97% compared to a haze-free planet and potentially allowing survival of land-based organisms 2.7–2.6 billion years ago. The broad UV absorption signature produced by this haze may be visible across interstellar distances, allowing characterization of similar hazy exoplanets. The haze in Archean Earth's atmosphere was strongly dependent on biologically produced methane, and we propose that hydrocarbon haze may be a novel type of spectral biosignature on planets with substantial levels of CO 2 . Hazy Archean Earth is the most alien world for which we have geochemical constraints on environmental conditions, providing a useful analogue for similar habitable, anoxic exoplanets. Key Words: Haze—Archean Earth—Exoplanets—Spectra—Biosignatures—Planetary habitability. Astrobiology 16, 873–899.
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TL;DR
Coupled climate-photochemical-microphysical simulations of hazy Archean Earth show that organic haze can cool the surface by about 20 K but still permit habitable temperatures with liquid surface water, because thick hazes self-limit via UV self-shielding. The haze also strongly shields surface UV and produces distinctive spectral features, suggesting hydrocarbon haze may be a biologically mediated spectral biosignature on anoxic, CO₂-rich exoplanets.
Key findings
- Hazy Archean climates were cold but likely habitable: for Cases A–D, stabilized surface temperatures with haze were 263, 274, 262, and 251 K, and with ice-albedo feedback 257, 271, 257, and 241 K, all above the adopted 248 K habitability threshold; haze cooling reached up to ∼20 K, with maximum haze optical thickness leveling off at τ ∼ 5 at 200 nm.
- Haze is self-limiting: optically thicker hazes shield CH₄ from photolysis, shutting down haze formation and preventing catastrophic cooling; the CH₄/CO₂ ratios needed to initiate haze formation were 0.18, 0.15, 0.19, and 0.28 for Cases A–D.
- UV shielding was substantial: for Case B with CH₄/CO₂ = 0.21, surface UVC flux was about 0.03 W/m² at SZA = 60° and 0.22 W/m² at SZA = 0°, compared with 0.93 and 2.62 W/m² for the haze-free case, a reduction of about 97%; this may have allowed survival of land-based organisms 2.7–2.6 billion years ago.
- Hazy Archean Earth would be a “pale orange dot,” with a broad UV absorption signature, a 6 μm transit-transmission haze feature, and a weaker 3 μm feature; the CH₄ flux needed to initiate haze was about 1 × 10¹¹ to 3 × 10¹¹ molecules/cm²/s, far above estimated maximum abiotic serpentinization fluxes of 6.8 × 10⁸ and 1.3 × 10⁹ molecules/cm²/s for 1 and 5 Earth-mass rocky planets.
Methods
- Used the coupled 1-D photochemical-climate model Atmos and the 1-D radiative transfer model SMART; the photochemical model has 200 plane-parallel layers from the surface to 100 km, 76 chemical species, and fractal hydrocarbon haze microphysics, while the climate model uses correlated-k absorption and a δ-2-stream radiative transfer scheme, iterating between models to convergence.
- Simulated four Archean cases spanning pCO₂ = 0.0036–0.018 bar and surface pressure = 0.5–1 bar, with solar constant at 2.7 Ga = 0.81 S/S₀, surface O₂ = 1.0 × 10⁻⁸, and varied CH₄/CO₂; about 60 coupled Atmos runs were required.
- Generated synthetic reflectance, thermal emission, and transit transmission spectra with SMART, including binned haze particle modes and, for Case B, tests with water clouds.
Limitations
- Stated in paper: the climate model could only be run to about 80 km while the photochemical model extends to 100 km, with isoprofiles above the climate grid; sensitivity tests showed <5% difference in largest haze particles and <0.5 K surface temperature effect. Older CH₄ coefficients may overestimate surface temperature by ≲5 K, while the model underpredicts Archean temperature by about 2–5 K compared with 3-D models, so these may cancel.
- Stated in paper: the 1-D model lacks atmospheric circulation, precipitation, cloud formation, cloud scattering and absorption, and long-wave cloud radiative forcing; comparison with GCMs suggests the presented temperatures may be underestimates by about 3–5 K, and ice-albedo feedback, haze deposition, haze circulation, and cloud feedbacks are left to future GCM studies.
- Stated in paper and evident from text: haze formation chemistry is not well understood, and the model assumes C₄H₂ and C₅H₄ condense directly to haze particles, possibly overestimating aerosol formation; only one Archean haze refractive index measurement exists, at 532 nm, and the study uses Titan-like Khare optical constants; NH₃ was not included in the photochemical scheme; nominal haze spectra exclude water clouds.
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A result the paper reports from its own data — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Here, we demonstrate using coupled climate-photochemical-microphysical simulations that hazes can cool the planet's surface by about 20 K”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
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In the paper
“We find that optically thicker hazes are self-limiting due to their self-shielding properties, preventing catastrophic cooling of the planet.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
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In the paper
“but habitable conditions with liquid surface water could be maintained with a relatively thick haze layer (τ ∼ 5 at 200 nm) even with the fainter young Sun”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesA result the paper reports from its own data — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“reducing surface UV flux by about 97% compared to a haze-free planet”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIn the paper
“The haze can produce a stronger UV shield compared to the low O2 atmosphere (0.1% PAL) proposed recently by Planavsky et al. (2014) for our atmospheric assumptions.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
What the sources say
- Not checked yetcites Planavsky et al., 2014
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In the paper
“By using the updated habitability threshold of Tsurf > 248 K, all our cases even with thick hazes are habitable.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
Load-bearingStrength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passes- Rests on an assumption: A planet with any nonzero fraction of open ocean is habitable.
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In the paper
“The Bond albedos produced in these cases including haze are 0.26, 0.24, 0.26, and 0.29.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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In the paper
“In the hotter atmosphere, τcoag is smaller than τsed through most of the atmospheric column.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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In the paper
“As the haze gets optically thicker, absorption of UV photons produces an atmospheric temperature inversion (Fig. 5) similar to that produced by ozone in the modern atmosphere.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesThe paper states this without a source or data behind it here, so there is nothing to check it against. The quote shows it is in the paper.
In the paper
“The insignificant haze present in the CH4/CO2 = 0.1 atmosphere is spectrally indistinguishable from an atmosphere with no haze.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results
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- Probably not a substantial claim. 40
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In the paper
“The particle mode sizes we use span from 0.001 to 2 μm; larger particles do not exist in our atmospheres due to rainout.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.2. The SMART model
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
The paper states this without a source or data behind it here, so there is nothing to check it against. The quote shows it is in the paper.
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“The largest particles produced by the 250 K atmosphere have a geometric radius of 0.8 μm compared to 0.65 μm radius particles for the 200 K atmosphere.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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In the paper
“In contrast, the surface UVC flux under a haze for Case B (CH4/CO2 = 0.21) would have been about 0.03 W/m2 for SZA = 60° and 0.22 W/m2 for SZA = 0°.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
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In the paper
“A modest amount of O2 in the Proterozoic (1% PAL) produces a stronger UV shield than the Archean haze, but the haze shown here cuts out more UVA (320–400 nm) and UVB (280–320 nm) radiation than ozone in all situations.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
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In the paper
“At short wavelengths in direct imaging, haze absorption decreases the planet's brightness; scattering brightens the planet at longer wavelengths.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
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“Thus, we find there is a maximum haze optical thickness—and a minimum temperature from haze-induced cooling—for each atmosphere.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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In the paper
“This table only includes Case B, but the other cases produce similar results for UV shielding because they have similar optical thicknesses.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
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In the paper
“According to these assumptions, Proterozoic Earth with 0.1% PAL O2 would have received 0.57 W/m2 of UVC at the surface, so in this case, the Archean hazy UV shield was stronger.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
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A result the paper reports from its own data — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Note that even using the conventional habitability threshold of 273 K, Cases A–C have a hazy solution space where Tsurf > 273 K, and Case B stabilizes at Tsurf = 274 K with its thickest haze.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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The paper states this without a source or data behind it here, so there is nothing to check it against. The quote shows it is in the paper.
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“We find that hazy Archean climates were cold but most likely habitable (Fig. 4).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
- Rests on an assumption: A planet with any nonzero fraction of open ocean is habitable.
A result the paper reports from its own data — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“For the haze-free Case B atmosphere (CH4/CO2 = 0.1), our models calculate the flux of UVC at the surface as about 0.93 W/m2 for a SZA of 60° and 2.62 W/m2 for SZA = 0°.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
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In the paper
“The temperatures of planets A, B, C, and D with ice-albedo feedbacks are 257, 271, 257, and 241 K, a decrease of 3–10 K compared with simulations with the nominal albedo.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
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In the paper
“These features can also be seen in the peaks of the haze imaginary refractive index (Fig. 2).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
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In the paper
“For this world, the CAM produces a global average surface temperature of 287.9 K. Our model produces 285.3 K for this configuration, a difference of 2.6 K.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
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In the paper
“its buildup in our spectra is not inconsistent with the results of Domagal-Goldman et al. (2011)”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
What the sources say
- Not checked yetcites Domagal-Goldman et al. (2011)
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In the paper
“We achieve the closest match to the Charnay et al. results for a modern continental land mass arrangement: in the GCM, this yields an average albedo of 0.34 and a temperature of 283.7 K, close to our result of 281.1 K for this configuration.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
What the sources say
- Not checked yetcites Charnay et al.
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In the paper
“This is comparable to, but 5 K warmer than, our global average 1-D result of 282 K.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
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In the paper
“There is also a very weak haze feature near 3 μm in transit transmission that can be most easily seen in Fig. 10.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
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In the paper
“the other cases produce similar spectra as discussed below.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
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In the paper
“of all the optical constants plotted in Fig. 14, the Khare indices actually produce the closest (although still too low) match to the Hasenkopf Archean real refractive index (n) near 532 nm and produce a reasonable match to the Hasenkopf Archean imaginary refractive index (k), agreeing to within approximately 40% near 532 nm.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
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None of the sources cited for this claim have been checked yet.
In the paper
“Following Wolf and Toon, we find our maximum haze thickness levels off at τ ∼ 5 at 200 nm, which results in a significantly shorter NH3 lifetime of 1 × 104 years, although we did not include NH3 in our photochemical scheme.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.3. Potential for NH3 greenhouse gas shielding
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In the paper
“This difference in temperature is smaller than the difference of using spherical versus fractal particles: our comparison to the Haqq-Misra et al. (2008) study in Section 4.2 shows that particle shape can result in temperature differences >10 K.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
What the sources say
- Not checked yetcites Haqq-Misra et al. (2008)
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
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In the paper
“Note the 1% CH4 Mahjoub imaginary refractive index agrees to within 5% of the Hasenkopf Archean measurement near 532 nm.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
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In the paper
“As we will show, hydrocarbon haze has profound spectral impacts for both reflected light and transit transmission spectra.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction
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In the paper
“Hazes may even enhance planetary habitability through UV shielding, reducing surface UV flux by about 97% compared to a haze-free planet and potentially allowing survival of land-based organisms 2.7–2.6 billion years ago.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
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In the paper
“the modeling work of Domagal-Goldman et al. (2008) suggests a longer Mesoarchean to Neoarchean hazy period between 3.2 and 2.7 Ga.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Domagal-Goldman et al., 2008
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In the paper
“S8 is the most important species to rain out S-MIF from the atmosphere; because a more reducing atmosphere enhances the ability of S8 to polymerize, S-MIF is more easily preserved under reducing conditions (Zahnle et al., 2006).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Zahnle et al., 2006
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In the paper
“The S-MIF signal is variable throughout the Archean, and it vanishes completely once O2 builds up to non-negligible levels in the atmosphere after the GOE at 2.5 Ga.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
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In the paper
“Several studies have proposed links between haze and the mass-independent sulfur isotope fractionation signal (S-MIF) (Farquhar et al., 2000) preserved in the geological record before the Great Oxygenation Event (GOE) at about 2.5 Ga”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Farquhar et al., 2000
- Not checked yetcites Domagal-Goldman et al., 2008
- Not checked yetcites Zerkle et al., 2012
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
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In the paper
“The broad UV absorption signature produced by this haze may be visible across interstellar distances, allowing characterization of similar hazy exoplanets.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > Abstract
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In the paper
“Early in Earth's history, an anoxic atmosphere could have supported the formation of an organic haze (Pavlov et al., 2001a; Trainer et al., 2004, 2006; DeWitt et al., 2009; Hasenkopf et al., 2010; Zerkle et al., 2012; Kurzweil et al., 2013; Claire et al., 2014; Izon et al., 2015) that strongly interacted with visible and UV radiation, cooling the planet's climate (Pavlov et al., 2001b; Domagal-Gol”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction
What the sources say
- Not checked yetcites Pavlov et al., 2001a
- Not checked yetcites Trainer et al., 2004, 2006
- Not checked yetcites DeWitt et al., 2009
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In the paper
“The climate model is considered converged when the change in temperature between time steps and change in flux out the top of the atmosphere are sufficiently small (typically on the order of 1 × 10−5).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✗ Based: failsProbably not a substantial claim. The paper’s conclusions may not depend on it. The paper may give no reason why it holds.
What the paper did — it cites no source for this, so there is none to check. The quote shows it is in the paper.
In the paper
“We have been unable to run the climate model to convergence using the same top-of-atmosphere pressure used for the photochemical model: the photochemical model extends to 100 km, but we have only been able to successfully run the climate model up to about 80 km for our 1 bar atmospheres.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“Δ36S/Δ33S in Archean sedimentary rocks is generally around −1, but stratigraphic variations in this slope have been observed in the geological record and interpreted as evidence of changes to the S-MIF production mechanism resulting from changes in atmospheric composition (Zerkle et al., 2012; Kurzweil et al., 2013; Izon et al., 2015), suggesting the influence of haze.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Zerkle et al., 2012
- Not checked yetcites Kurzweil et al., 2013
- Not checked yetcites Izon et al., 2015
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
In the paper
“In general, compared to spherical particles, fractal particles produce more extinction in the ultraviolet (UV) but less in the visible and near infrared (NIR).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
What the sources say
- Not checked yetcites Wolf and Toon, 2010
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
In the paper
“they discuss a change in the slope of Δ36S/Δ33S from −1.5 to −0.9 at 2.71 Ga and interpret this to be caused by a decrease in the CH4/CO2 ratio at 2.71 Ga, possibly indicating an organic haze was present for some period of time prior to 2.71 Ga and cleared afterward.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Kurzweil et al., 2013
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim. It may state two separate claims as one.
What the paper did — it cites no source for this, so there is none to check. The quote shows it is in the paper.
In the paper
“The photochemical model is considered converged when redox is conserved and a re-run of the model using last run's output as initial conditions occurs quickly (i.e., <50 time steps).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✗ Based: failsProbably not a substantial claim. The paper’s conclusions may not depend on it. The paper may give no reason why it holds. It may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“An upper atmosphere haze that decreased tropospheric SO2 photolysis by blocking UV photons and cooled the planet could explain both the glaciation and the decrease in S-MIF.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Domagal-Goldman et al., 2008
- Not checked yetcites Haqq-Misra et al., 2008
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
None of the sources cited for this claim have been checked yet.
In the paper
“In this interpretation, haze-free and reducing atmospheric conditions dominated after 2.71 Ga, with haze reappearing in brief intervals of time as suggested by the Zerkle et al. (2012) and Izon et al. (2015) measurements.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Zerkle et al., 2012
- Not checked yetcites Izon et al., 2015
Load-bearingStrength:hedged· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
What the paper did — it cites no source for this, so there is none to check. The quote shows it is in the paper.
In the paper
“In a real atmosphere, the molecules would be larger before aerosols condense, and back-reactions should occur, so this model may overestimate the rate of aerosol formation.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
- The authors state this as an assumption: C4H2 and C5H4 condense directly to haze particles.
In the paper
“Spherical particles in SMART are binned according to log-normal size distributions using the radii mentioned previously and a mode standard deviation of 1.5, which is realistic for an aerosol distribution (Tolfo, 1977).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.2. The SMART model
What the sources say
- Not checked yetcites Tolfo, 1977
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“Note that the version of the model used here can simulate atmospheres ranging from extremely anoxic (pO2 = 10−14) to modern-day O2 levels (Zahnle et al., 2006).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
What the sources say
- Not checked yetcites Zahnle et al., 2006
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“In addition, fractals tend to be more forward scattering in the visible and NIR and more isotropically scattering in the UV compared to equal-mass spherical particles.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.1. Coupled photochemical-climate model
What the sources say
- Not checked yetcites Wolf and Toon, 2010
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
In the paper
“Δ33S typically correlates with enrichments in δ34S and with depletions in δ36S”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Claire et al., 2014
Strength:plain· not yet calibratedCausal:correlational· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
In the paper
“In this conceptual model, the end of the cold period typified by low Δ33S may be due to a decrease in the atmospheric CH4/CO2 ratio, which would have cleared any haze present in the atmosphere.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Claire et al., 2014
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
In the paper
“Unlike previous studies of the Archean climate under a haze, we use realistic fractal (rather than spherical) particles, which have different spectral properties and climatic effects.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Wolf and Toon, 2010
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“Kurzweil et al. (2013) noted that an increase in magnitude of S-MIF signals after 2.73 Ga (Thomazo et al., 2009) occurred during a prolonged negative shift in δ13Corg, suggesting enhanced biological methane activity at this time.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 1. Introduction > 1.1. Evidence for an Archean haze
What the sources say
- Not checked yetcites Kurzweil et al., 2013
- Not checked yetcites Thomazo et al., 2009
Strength:hedged· not yet calibratedCausal:correlational· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
None of the sources cited for this claim have been checked yet.
In the paper
“However, more recent 3-D studies have shown that Archean Earth can maintain an open ocean fraction of >50% for TGAT ≥ 260 K and an equatorial open ocean belt for TGAT ≥ 248 K (Wolf and Toon, 2013; Charnay et al., 2013).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
What the sources say
- Not checked yetcites Wolf and Toon, 2013
- Not checked yetcites Charnay et al., 2013
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“These ice-albedo temperatures may be underestimates because once haze forms, deposition of dark hydrocarbons onto ice-covered areas will lower the albedo of the ice. This decreased ice albedo may then melt the ice, reverting parts of the surface back to ocean water.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
In the paper
“This might lead to cooling of the planet or even warming depending on cloud particle size and the altitude—and therefore temperature—of the cloud layer (Goldblatt and Zahnle, 2011).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
What the sources say
- Not checked yetcites Goldblatt and Zahnle, 2011
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
In the paper
“but a recent study of chromium isotopes suggests that the Proterozoic O2 mixing ratio was, at most, 0.1% PAL (Planavsky et al., 2014).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
What the sources say
- Not checked yetcites Planavsky et al., 2014
Load-bearingStrength:hedged· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
None of the sources cited for this claim have been checked yet.
In the paper
“Later purported hazy periods around 2.7 Ga (Kurzweil et al., 2013; Izon et al., 2015) and between 2.65 and 2.5 Ga (Zerkle et al., 2012) are not associated with glaciations and may be consistent with the thinner-haze solution space of Cases A and C or even the thickest haze solution space of the warmer Case B.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
What the sources say
- Not checked yetcites Kurzweil et al., 2013
- Not checked yetcites Izon et al., 2015
- Not checked yetcites Zerkle et al., 2012
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“DNA damage is most acute in the UVC (λ < 0.28 μm) wavelength range (Pierson et al., 1992; Dillon and Castenholz, 1999), but in the modern atmosphere, UVC is fully blocked by O2 and ozone.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
What the sources say
- Not checked yetcites Pierson et al., 1992
- Not checked yetcites Dillon and Castenholz, 1999
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
In the paper
“Unless otherwise specified, the surface albedo used by the climate model is 0.32. This includes the effect of clouds, which is standard in this 1-D treatment (Kopparapu et al., 2013) and is the albedo that reproduces the average temperature of present-day Earth (288 K) with modern atmospheric conditions.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.3. Model inputs
What the sources say
- Not checked yetcites Kopparapu et al., 2013
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it. It may state two separate claims as one.
In the paper
“We set the mixing ratio of O2 at the surface to 1.0 × 10−8, consistent with the Zerkle et al. (2012) study.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.3. Model inputs
What the sources say
- Not checked yetcites Zerkle et al., 2012
Load-bearingStrength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
In the paper
“Furthermore, Abbot et al. (2011) argued that ocean open belts can remain climatologically stable, even if the ice latitude is reduced to 5–15°.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.1. Hazy climates
What the sources say
- Not checked yetcites Abbot et al., 2011
Load-bearingStrength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Because methane-producing metabolisms evolved early and Earth's atmosphere was anoxic for about a billion years after the origin of life, pale orange dots may proliferate in the Galaxy if other habitable worlds evolve on similar paths to Earth.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
Tests✓ Asserted: passes✗ Checkable: fails✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. It may be too vague to check against evidence. The paper’s conclusions may not depend on it. It may state two separate claims as one.
- Rests on an assumption: Methane-producing metabolisms evolved early.
- Rests on an assumption: Earth's atmosphere was anoxic for about a billion years after the origin of life.
In the paper
“Of course, the true cloud distribution on Archean Earth is unknown, and clouds may have had important climatic effects on our early planet (Goldblatt and Zahnle, 2011).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.3. Model inputs
What the sources say
- Not checked yetcites Goldblatt and Zahnle, 2011
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it. It may state two separate claims as one.
In the paper
“The solar zenith angles (SZAs) used in the climate and photochemical models were chosen to best represent globally averaged behavior of the physics in each specific model, which Segura et al. (2003) found as SZA = 45° in the photochemical model and SZA = 60° in the climate model. These zenith angles are both tuned to reproduce modern-day Earth's average chemical profiles and climate, respectively.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 2. Models and Methods > 2.3. Model inputs
What the sources say
- Not checked yetcites Segura et al., 2003
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“The impact of these hazes on the biosphere goes beyond temperature reduction: their fractal nature makes them strong absorbers at short wavelengths and therefore a potential shield against damaging UV radiation for the anoxic Archean (Wolf and Toon, 2010), which would have received significantly more UV at the surface than the planet today (Rugheimer et al., 2015).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.2. UV shielding
What the sources say
- Not checked yetcites Wolf and Toon, 2010
- Not checked yetcites Rugheimer et al., 2015
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“so the occurrence of haze in the habitable zone may be a way to flag interesting planets for careful follow-up study that would search for other indicators of life and quantify the concentration of CH4 and other gases.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.1. Haze and biology
Tests✓ Asserted: passes✗ Checkable: fails✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim. It may be too vague to check against evidence.
In the paper
“which showed much greater C2H6 accumulation on planets orbiting low-mass stars compared to worlds orbiting the Sun.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
What the sources say
- Not checked yetcites Domagal-Goldman et al. (2011)
Strength:plain· not yet calibratedCausal:correlational· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“Based on their calculations, Guzmán-Marmolejo et al. (2013) suggested that an atmospheric CH4 concentration greater than 10 ppmv is suggestive of life.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.1. Haze and biology
What the sources say
- Not checked yetcites Guzmán-Marmolejo et al. (2013)
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
In the paper
“The Charnay et al. results for the same atmospheric properties but with an equatorial supercontinent result in the same overall planetary albedo (0.33) but a lower mean temperature of 285 K”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
What the sources say
- Not checked yetcites Charnay et al.
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Our study shows how an Archean haze would have profoundly impacted our planet's environment, habitability, and spectrum.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.1. Haze and biology
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
What the paper did — it cites no source for this, so there is none to check. The quote shows it is in the paper.
In the paper
“To consider the spectral effect of haze without contamination from other atmospheric aerosols, the spectra in this section do not include water clouds, even though cloud albedo is implicit in the parameterization of the Atmos model's surface albedo. This makes the albedos of the planets whose spectra are shown in this section darker than those in the Atmos parameterization.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Abundant stratospheric water vapor would imply that the planet is in the midst of a moist or runaway greenhouse state and thus is not conventionally habitable.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes? Based: unclearIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“Laboratory experiments on organic haze formation have shown that haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al., 1986; McDonald et al., 1994; DeWitt et al., 2009; Hörst et al., 2012; Trainer, 2013)”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.1. Haze and biology
What the sources say
- Not checked yetcites Khare et al., 1986
- Not checked yetcites McDonald et al., 1994
- Not checked yetcites DeWitt et al., 2009
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“We also tested our model results against the Community Atmosphere Model (CAM) GCM nominal Archean atmosphere reported by Wolf and Toon (2013).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
What the sources say
- Not checked yetcites Wolf and Toon (2013)
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
In the paper
“C2H6 is a greenhouse gas, and its ability to warm in a CH4- and haze-rich atmosphere has been discussed previously (Haqq-Misra et al., 2008).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 3. Results > 3.3. Spectra
What the sources say
- Not checked yetcites Haqq-Misra et al., 2008
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it. It may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Our comparison with these 3-D models suggests the temperatures we present in this work are reasonable but may be underestimates by about 3–5 K.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.2. Comparison with other climate studies
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“but haze formation is likely considerably more complex and is still not well understood.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
Strength:hedged· not yet calibratedTests✓ Asserted: passes✗ Checkable: fails✗ Load-bearing: fails✗ Based: failsProbably not a substantial claim. It may be too vague to check against evidence. The paper’s conclusions may not depend on it. The paper may give no reason why it holds. It may state two separate claims as one.
In the paper
“The Mahjoub study tested the impact of methane concentration in the gas phase on the resultant hydrocarbon optical properties with gas mixtures containing 1%, 2%, 5%, and 10% CH4 in CH4-N2 mixtures.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
What the sources say
- Not checked yetcites Mahjoub et al.
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
None of the sources cited for this claim have been checked yet.
In the paper
“Following Sagan and Chyba (1997), Wolf and Toon calculated a NH3 atmospheric lifetime of 7 × 107 years for a solar incident flux at a 45° angle assuming τ ∼ 11 at 200 nm.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.3. Potential for NH3 greenhouse gas shielding
What the sources say
- Not checked yetcites Sagan and Chyba (1997)
- Not checked yetcites Wolf and Toon
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesProbably not a substantial claim.
In the paper
“As an example and test of the impact different refractive indices have on our spectra, we examined the sensitivity of our nominal spectra to varied refractive indices measured by Mahjoub et al. (2012).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
What the sources say
- Not checked yetcites Mahjoub et al. (2012)
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“Mass spectrometry of aerosol analogues formed with C/O = 0.1 indicates the formation of carbonyl and carboxyl groups rather than aromatic cycles and long-aliphatic chains, and even suggests the formation of organic acids such as succinic acid (C4H6O4) (DeWitt et al., 2009).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
What the sources say
- Not checked yetcites DeWitt et al., 2009
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“These results suggest that N2 chemical activation could be due to its reaction with the methylidyne (CH) radical formed from CH4 photolysis, to form two radical intermediates, diazomethyl HCNN and its isomer HNCN, which might then react to form HCN and other products.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“An additional advantage of the Khare refractive indices is that they span an extremely wide wavelength range, ranging from 0.02 to 920 μm, so only one set of optical constants is needed to cover all the wavelengths relevant to photochemistry, climate, and spectra.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
In the paper
“Unfortunately, only one study, that of Hasenkopf et al. (2010), has measured an Archean Earth haze refractive index (as opposed to a titanian haze), and this was only done at a single wavelength (532 nm).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
What the sources say
- Not checked yetcites Hasenkopf et al. (2010)
Load-bearingStrength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“Early Earth's atmosphere would have contained negligible O2 but significant amounts of CO2 (e.g., Kasting, 1993; Driese et al., 2011), whereas Titan's atmosphere is extremely reducing (de Kok et al., 2007).”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
What the sources say
- Not checked yetcites Kasting, 1993
- Not checked yetcites Driese et al., 2011
- Not checked yetcites de Kok et al., 2007
Load-bearingStrength:hedged· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
None of the sources cited for this claim have been checked yet.
In the paper
“In situ measurements by several instruments on board Cassini have found direct evidence for long hydrocarbons and nitriles chains, benzene (C6H6) and toluene (C6H5CH3), and indirect evidence for polycyclic aromatic hydrocarbons (PAHs) and nitrogen-containing polycyclic aromatic hydrocarbons (PANHs), indicating that these compounds might play a role in the formation of Titan's hazes (Waite et al.,”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
What the sources say
- Not checked yetcites Waite et al., 2007
- Not checked yetcites López-Puertas et al., 2013
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it. It may state two separate claims as one.
In the paper
“Wolf and Toon (2010) commented on the possibility of a fractal hydrocarbon haze shielding ammonia (NH3) from photolysis, allowing this greenhouse gas to build up in the Archean atmosphere.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.3. Potential for NH3 greenhouse gas shielding
What the sources say
- Not checked yetcites Wolf and Toon (2010)
Strength:hedged· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“These results bring to light a significant but still unknown mechanism regarding the activation of nitrogen and its inclusion in oxygenated organics, thus providing a new and quantifiable source for these two elements into the early Earth aerosols.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.4. Haze formation pathways
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Discovering habitable exoplanets dissimilar to modern Earth will increase the diversity of known habitable environments.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 5. Conclusions
Strength:plain· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✗ Based: failsProbably not a substantial claim. The paper’s conclusions may not depend on it. The paper may give no reason why it holds.
What the paper did — it cites no source for this, so there is none to check. The quote shows it is in the paper.
In the paper
“Of course this does not account for differences expected in the spectral shape of Archean haze analogues across the UV-visible-IR relative to the titanian haze analogues.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
Strength:plain· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“The climatic effects of this haze could have been part of feedbacks between biological CH4 production, atmospheric chemistry, and surface UV radiation.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 5. Conclusions
Strength:hedged· not yet calibratedCausal:conditional· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✓ Based: passesProbably not a substantial claim. The paper’s conclusions may not depend on it.
In the paper
“Mahjoub et al. found that refractive indices have a strong dependency on the CH4 concentration over 0.37–1 μm: results indicate that the imaginary index of refraction (k) decreases with increasing CH4 concentration, and the real index of refraction (n) increases with CH4 for the compositions tested.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
What the sources say
- Not checked yetcites Mahjoub et al.
Strength:boosted· not yet calibratedCausal:direct· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes? Load-bearing: unclear✓ Based: passesIt may state two separate claims as one.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“Due to the properties of fractal hazes, these particles are relatively transparent at wavelengths longer than approximately the visible range”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
Tests✓ Asserted: passes✓ Checkable: passes✓ Load-bearing: passes✗ Based: failsProbably not a substantial claim. The paper may give no reason why it holds.
A conclusion the paper draws from its own results — it cites no other source for it, so there is none to check. The quote shows it is in the paper.
In the paper
“The Mahjoub constants do not extend shortward of 0.37 μm, but we should anticipate variation at these shorter wavelengths as well.”
§ The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth > 4. Discussion > 4.5. Optical constants
Strength:hedged· not yet calibratedTests✓ Asserted: passes✓ Checkable: passes✗ Load-bearing: fails✗ Based: failsProbably not a substantial claim. The paper’s conclusions may not depend on it. The paper may give no reason why it holds. It may state two separate claims as one.
The authors state this as an assumption.
Fixed isoprofiles are assumed for CO2 and N2 in the atmospheres considered here.
“Fixed isoprofiles are assumed for CO2 and N2 in the atmospheres considered here.”
The authors state this as an assumption.
C4H2 and C5H4 condense directly to haze particles.
“it is assumed that C4H2 and C5H4 condense directly to haze particles (called HCAER and HCAER2 in Supplementary Table S1).”
The paper relies on this without support.
A planet with any nonzero fraction of open ocean is habitable.
“Since a planet with any nonzero fraction of open ocean is habitable, we regard these updated globally averaged temperatures—all of which are significantly below freezing—to be more realistic habitability thresholds than 273 K.”
The paper relies on this without support.
Methane-producing metabolisms evolved early.
“Because methane-producing metabolisms evolved early and Earth's atmosphere was anoxic for about a billion years after the origin of life, pale orange dots may proliferate in the Galaxy if other habitable worlds evolve on similar paths to Earth.”
The paper relies on this without support.
Earth's atmosphere was anoxic for about a billion years after the origin of life.
“Because methane-producing metabolisms evolved early and Earth's atmosphere was anoxic for about a billion years after the origin of life, pale orange dots may proliferate in the Galaxy if other habitable worlds evolve on similar paths to Earth.”
The paper relies on this without support.
Water vapor clouds have an approximately gray opacity from the visible into the NIR.
“water vapor clouds have an approximately gray opacity from the visible into the NIR.”
The paper relies on this without support.
The tropopause on Earth is at roughly 10 km.
“The tropopause on Earth is at roughly 10 km”
The paper relies on this without support.
Geochemical evidence suggests hazy conditions were not present throughout the entire Archean.
“geochemical evidence suggests hazy conditions were not present throughout the entire Archean”
The paper relies on this without support.
The geochemical constraints on Archean CO2 concentration and geological constraints on surface pressure used in the study are valid.
“consistent with geochemical constraints on CO2 concentration and geological constraints on surface pressure”
The paper relies on this without support.
UVC radiation is harmful to unshielded life.
“may have allowed survival of otherwise unshielded life at the surface of our Archean planet”
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
The cited source says what the claim attributes to it.
In the citing paper
“A cooling limit exists because as a haze becomes more UV absorbing, it shields CH4 molecules from the photolysis needed for further haze formation.”
From The Archean atmosphere (2020) · cites this paper as [1]
The cited source says what the claim attributes to it.
In the citing paper
“However, whether this shielding actually occurred depends on whether hazes actually existed and on the size and radiative properties of haze particles, which remain uncertain (1, 163).”
From The Archean atmosphere (2020) · cites this paper as [1]
The cited source says what the claim attributes to it.
In the citing paper
“However, too much CH4 relative to CO2 would create the high-altitude organic haze mentioned earlier, which may cool Earth by up to ~20 K (1, 215) by absorbing incoming solar radiation and radiating energy back to space in a so-called “anti-greenhouse effect” (216).”
From The Archean atmosphere (2020) · cites this paper as [1]
The cited source says what the claim attributes to it.
In the citing paper
“Thus, attenuation of sunlight saturates (1, 163).”
From The Archean atmosphere (2020) · cites this paper as [1]
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
Each contradiction between two passages listed here was confirmed by an independent check.
Conflicting criteria for haze-particle growth
MinorThe methods say particles can grow when the coagulation lifetime is longer than the removal lifetime, but the results say growth occurs when the coagulation timescale is shorter than the removal timescale.
“The aerosols can grow when the coagulation lifetime is longer than the lifetime for removal in a layer.”
“In the photochemical model, when the coagulation timescale (τcoag) is shorter than the timescale for removal in an atmospheric layer, the particles can grow.”
Sulfur isotope relationship uses the wrong isotope on its right-hand side
MinorThe text says δ36S is roughly twice δ34S, but the stated mass-dependent relationship makes δ36S proportional to itself instead.
“samples following MDF will have δ33S ∼ 0.515 × δ34S and δ36S ∼ 1.89 × δ36S.”
“the δ36S composition is roughly twice the δ34S amount.”
Example does not give equal log-space bin distances
MinorThe stated binning rule uses distance in log space, but 0.33 μm is not halfway in log space between 0.3 and 0.4 μm. Those bins therefore would not each receive 50% of the mass under the stated rule.
“if Atmos produces a particle of radius 0.33 μm in a layer, the corresponding layer in SMART will include 0.3 and 0.4 μm particles each comprising 50% of the layer's mass.”
“the mass density contributed by the two modes is selected based on the distance in log space of the Atmos particle radius to each neighboring SMART size bin.”
Citations
Cites
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InfluentialThe formation, properties and impact of secondary organic aerosol: current and emerging issues
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The HITRAN2012 molecular spectroscopic database
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Diffuse radiation in the Galaxy
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“Thus, S-MIF is generally regarded as robust evidence for an anoxic Archean atmosphere.”
InfluentialHABITABLE ZONES AROUND MAIN-SEQUENCE STARS: NEW ESTIMATES
Kopparapu, R. K., Ramirez, R., Kasting, J. F., Eymet, V., Robinson, T. D., Mahadevan, S., Terrien, R. C., Domagal-Goldman, S., Meadows, V., & Deshpande, R. (2013) · The Astrophysical Journal · doi:10.1088/0004-637x/765/2/131 · Cited by 1,615 · cited 7×
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A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
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“In addition, several abiotic processes including serpentinization (the hydration of ultramafic rocks, mainly olivine and pyroxenes) can form methane (Kelley et al. , 2005; Etiope and Sherwood Lollar, 2013; Guzma´n-Marmolejo et al. , 2013), but the biotic flux of methane to the Archean atmosphere was…”
Photochemistry of the atmosphere of Titan - Comparison between model and observations
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“Following the mechanism proposed for the formation of Titan’s hydrocarbon haze (Allen et al. , 1980; Yung et al. , 1984), every model of hydrocarbon haze formation in early Earth’s atmosphere—including ours—has assumed that aerosol formation will occur through the formation of acetylene (C 2 H 2 )…”
Clouds in the atmosphere of the super-Earth exoplanet GJ 1214b
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“Unlike the hazes that may exist around exoplanets with thick hydrogen-dominated atmospheres (Sing et al., 2011; Knutson et al., 2014; Kreidberg et al., 2014), the Archean (3.”
InfluentialPavlov, A. A., & Kasting, J. F. (2002) · Astrobiology · doi:10.1089/153110702753621321 · Cited by 912 · cited 2×
“After the GOE, all the sulfur in the atmosphere would have been oxidized into a single exit channel, eliminating any fractionation created in the atmosphere (Pavlov and Kasting, 2002).”
Stromatolite reef from the Early Archaean era of Australia
Allwood, A. C., Walter, M. R., Kamber, B. S., Marshall, C. P., & Burch, I. W. (2006) · Nature · doi:10.1038/nature04764 · Cited by 905 · cited 2×
“There is evidence that Archean stromatolitic communities lived in inter- and supratidal zones (Allwood et al., 2006; Noffke and Awramik, 2013) experiencing frequent, sometimes extended, exposure to the surface environment, and it has been suggested that microbial mats existed on land as early as 2.”
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“A d -2- stream method is used for radiative transfer (Toon et al. , 1989).”
InfluentialUSGS Digital Spectral Library splib06a
Clark, R. N., Swayze, G. A., Wise, R. A., Livo, K. E., Hoefen, T. M., Kokaly, R. F., & Sutley, S. J. (2007) · Data series · doi:10.3133/ds231 · Cited by 881 · cited 1×
“In cases where an icy surface is used, we use an albedo from the USGS Digital Spectral Library (Clark et al. , 2007).”
Low Mid-Proterozoic atmospheric oxygen levels and the delayed rise of animals
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“…been assumed that Proterozoic Earth’s surface received less UV than the Archean due to the rise of oxygen (O 2 ) and ozone ( e.g. , Rugheimer et al. , 2015), but a recent study of chromium isotopes suggests that the Proterozoic O 2 mixing ratio was, at most, 0.1% PAL (Planavsky et al. , 2014).”
InfluentialKhare, B. N., Sagan, C., Arakawa, E. T., Suits, F., Callcott, T. A., & Williams, M. W. (1984) · Icarus · doi:10.1016/0019-1035(84)90142-8 · Cited by 706 · cited 5×
“Refractive indices, shown in the bottom panels, are presented from information in Khare et al. (1984a). extends to 100 km, but we have only been able to successfully run the climate model up to about 80 km for our 1 bar atmospheres.”
InfluentialThe Process of Tholin Formation in Titan's Upper Atmosphere
Waite, J. H., Young, D. T., Cravens, T. E., Coates, A. J., Crary, F. J., Magee, B. A., & Westlake, J. H. (2007) · Science · doi:10.1126/science.1139727 · Cited by 699 · cited 2×
“…) and toluene (C 6 H 5 CH 3 ), and indirect evidence for polycyclic aromatic hydrocarbons (PAHs) and nitrogen-containing polycyclic aromatic hydrocarbons (PANHs), indicating that these compounds might play a role in the formation of Titan’s hazes (Waite et al. , 2007; Lo´pez-Puertas et al. , 2013).”
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Evidence from fluid inclusions for microbial methanogenesis in the early Archaean era
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“…thick hydrogen-dominated atmospheres (Sing et al. , 2011; Knutson et al. , 2014; Kreidberg et al. , 2014), the Archean (3.8–2.5 billion years ago) haze was likely biologically mediated via CH 4 produced from methanogenesis, one of the earliest metabolisms (Woese and Fox, 1977; Ueno et al. , 2006).”
InfluentialGreenhouse warming by CH 4 in the atmosphere of early Earth
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Biosignatures from Earth-Like Planets Around M Dwarfs
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“…(Kopparapu et al. , 2013), the climate of early Mars (Ramirez et al. , 2013), the atmospheres of Earth-like planets around various stellar types (Segura et al. , 2003, 2005, 2010; Rugheimer et al. , 2013), clouds in exoplanet THE PALE ORANGE DOT atmospheres (Kitzmann et al. , 2010, 2011a), and…”
Self-citationFarquhar, J., Savarino, J., Airieau, S., & Thiemens, M. H. (2001) · Journal of Geophysical Research: Planets · doi:10.1029/2000je001437 · Cited by 518 · cited 1×
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A search for life on Earth from the Galileo spacecraft
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“Additionally, although we anticipate planetary diversity in the exoplanet population, existing spectral studies are largely focused on the observables of modern-day Earth ( e.g. , Sagan et al. , 1993; Woolf et al. , 2002; Robinson et al. , 2011, 2014a).”
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“Our solar spectrum was modeled by Chance and Kurucz (2010) and was scaled by the solar evolution model (Claire et al. , 2012) mentioned previously.”
Fractal and projected structure properties of soot aggregates
Köylü, Ü. Ö., Faeth, G. M., Farias, T. L., et al. (1995) · Combustion and Flame · doi:10.1016/0010-2180(94)00147-k · Cited by 496 · cited 1×
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“Negative values of d (13)Corg below -37& are typically interpreted as evidence for methanogenesis (biological methane production) followed by subsequent incorporation into sediments by methanotrophy (methane consumption), which imparts a strongly negative d(13)Corg because organisms preferentially uptake the (12)C (Ur…”
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“It has been suggested that the Rayleigh scattering slope could be used to constrain atmospheric pressure on exoplanets (Benneke and Seager, 2012), but this would not be possible on planets with hydrocarbon hazes due to these strong short-wavelength absorption effects.”
Segura, A., Walkowicz, L. M., Meadows, V., Kasting, J., & Hawley, S. (2010) · Astrobiology · doi:10.1089/ast.2009.0376 · Cited by 446 · cited 2×
“…(Kopparapu et al. , 2013), the climate of early Mars (Ramirez et al. , 2013), the atmospheres of Earth-like planets around various stellar types (Segura et al. , 2003, 2005, 2010; Rugheimer et al. , 2013), clouds in exoplanet THE PALE ORANGE DOT atmospheres (Kitzmann et al. , 2010, 2011a), and…”
Self-citationSing, D. K., Pont, F. J., Aigrain, S., Charbonneau, D., Désert, J.-M., Gibson, N. P., Gilliland, R. L., Hayek, W., Henry, G. W., Knutson, H. A., et al. (2011) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2011.19142.x · Cited by 427 · cited 1×
“Unlike the hazes that may exist around exoplanets with thick hydrogen-dominated atmospheres (Sing et al. , 2011; Knutson et al. , 2014; Kreidberg et al. , 2014), the Archean (3.8–2.5 billion years ago) haze was likely biologically mediated via CH 4 produced from methanogenesis, one of the earliest…”
InfluentialThe Early Faint Sun Paradox: Organic Shielding of Ultraviolet-Labile Greenhouse Gases
Sagan, C., & Chyba, C. (1997) · Science · doi:10.1126/science.276.5316.1217 · Cited by 396 · cited 1×
“Following Sagan and Chyba (1997), Wolf and Toon calculated a NH 3 atmospheric lifetime of 7 · 10 7 years for a solar incident flux at a 45 (cid:2) angle assuming s * 11 at 200 nm.”
Climatic consequences of very high carbon dioxide levels in the earth’s early atmosphere
Kasting, J. F., & Ackerman, T. P. (1986) · Science · doi:10.1126/science.11539665 · Cited by 391 · cited 1×
“Our climate model was originally developed by Kasting and Ackerman (1986).”
Ozone Concentrations and Ultraviolet Fluxes on Earth-Like Planets Around Other Stars
Segura, A., Krelove, K., Kasting, J. F., Sommerlatt, D., Meadows, V., Crisp, D., Cohen, M., & Mlawer, E. (2003) · Astrobiology · doi:10.1089/153110703322736024 · Cited by 379 · cited 3×
“The solar zenith angles (SZAs) used in the climate and photo-chemical models were chosen to best represent globally averaged behavior of the physics in each specific model, which Segura et al. (2003) found as SZA = 45 (cid:2) in the photochemical model and SZA = 60 (cid:2) in the climate model.”
Self-citationOno, S., Eigenbrode, J. L., Pavlov, A. A., Kharecha, P., Rumble, D., Kasting, J. F., & Freeman, K. H. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(03)00295-4 · Cited by 363 · cited 1×
“…also has a long heritage of being used to study photochemistry in nonhazy atmospheres ( e.g. , Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et…”
A Revised, Hazy Methane Greenhouse for the Archean Earth
Haqq-Misra, J. D., Domagal-Goldman, S. D., Kasting, P. J., & Kasting, J. F. (2008) · Astrobiology · doi:10.1089/ast.2007.0197 · Cited by 357 · cited 18×
“…al. (1984a) to allow us to draw comparisons with previous works involving our suite of models (Pavlov et al. , 2001b; Domagal-Goldman et al. , 2008; Haqq-Misra et al. , 2008; Zerkle et al. , 2012; Kurzweil et al. , 2013; Claire et al. , 2014), as well as the Wolf and Toon (2010) study, which all…”
InfluentialSelf-citationMeadows, V. S., & Crisp, D. (1996) · Journal of Geophysical Research: Planets · doi:10.1029/95je03567 · Cited by 354 · cited 1×
“D line-by-line fully multiple scattering radiative transfer model (Meadows and Crisp, 1996; Crisp, 1997).”
Self-citationA featureless transmission spectrum for the Neptune-mass exoplanet GJ 436b
Knutson, H. A., Benneke, B., Deming, D., & Homeier, D. (2013) · Nature · doi:10.1038/nature12887 · Cited by 341 · cited 2×
“Unlike the hazes that may exist around exoplanets with thick hydrogen-dominated atmospheres (Sing et al., 2011; Knutson et al., 2014; Kreidberg et al., 2014), the Archean (3.”
InfluentialA RECIPE FOR IMAGE CHARACTERIZATION OF FRACTAL-LIKE AGGREGATES
Brasil, A. C. D. M., Farias, T. L., & Carvalho, M. D. G. (1999) · Journal of Aerosol Science · doi:10.1016/s0021-8502(99)00026-9 · Cited by 334 · cited 1×
“Additional information about fractal particles and their geometry can be found in the works of, for example, Ko¨ylu¨ et al. (1995) and Brasil et al. (1999).”
Atmospheric origins of perchlorate on Mars and in the Atacama
Catling, D. C., Claire, M. W., Zahnle, K. J., Quinn, R. C., Clark, B. C., Hecht, M. H., & Kounaves, S. P. (2010) · Journal of Geophysical Research Atmospheres · doi:10.1029/2009je003425 · Cited by 322 · cited 1×
“…Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014; Rugheimer et al. , 2013, 2015; Harman et al. , 2015; Schwieterman et al. , 2016).”
Self-citationA coupled atmosphere–ecosystem model of the early Archean Earth
KHARECHA, P., KASTING, J., & SIEFERT, J. (2005) · Geobiology · doi:10.1111/j.1472-4669.2005.00049.x · Cited by 321 · cited 4×
“…rocks, mainly olivine and pyroxenes) can form methane (Kelley et al. , 2005; Etiope and Sherwood Lollar, 2013; Guzma´n-Marmolejo et al. , 2013), but the biotic flux of methane to the Archean atmosphere was likely much higher than the abiotic flux (Kharecha et al. , 2005), as it is on Earth today.”
InfluentialIsotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry
Farquhar, J. D., Peters, M., Johnston, D. T., Strauß, H., Masterson, A. L., Wiechert, U., & Kaufman, A. J. (2007) · Nature · doi:10.1038/nature06202 · Cited by 319 · cited 1×
“While the precise mechanism (or mechanisms) that produces S-MIF is unknown, photolysis of sulfur gases in an anoxic atmosphere is the only known mechanism that produces large-magnitude D 33 S and D 36 S seen in the rock record (Farquhar et al. , 2001, 2007).”
ZAHNLE, K., CLAIRE, M., & CATLING, D. (2006) · Geobiology · doi:10.1111/j.1472-4669.2006.00085.x · Cited by 315 · cited 5×
“Note that the version of the model used here can simulate atmospheres ranging from extremely anoxic (pO 2 = 10 - 14 ) to modern-day O 2 levels (Zahnle et al. , 2006).”
InfluentialSelf-citationWarming early Mars with CO2 and H2
Ramirez, R. M., Kopparapu, R., Zugger, M. E., Robinson, T. D., Freedman, R., & Kasting, J. F. (2014) · Nature Geoscience · doi:10.1038/ngeo2000 · Cited by 303 · cited 7×
“The version we use here is based directly on that used by Kopparapu et al. (2013).”
InfluentialA model of Titan's aerosols based on measurements made inside the atmosphere
Tomasko, M. G., Doose, L. R., Engel, S., Dafoe, L. E., West, R. A., Lemmon, M. T., Karkoschka, E., & See, C. (2007) · Planetary and Space Science · doi:10.1016/j.pss.2007.11.019 · Cited by 303 · cited 2×
“The maximum radius of a spherical haze particle ( i.e. , a haze ‘‘monomer’’) is set to 0.05 l m, the same nominal value used by Wolf and Toon (2010) and similar to the size of the monomers of Titan’s fractal haze aggregates (Rannou et al. , 1997; Tomasko et al. , 2008).”
InfluentialUV shielding of NH3and O2by organic hazes in the Archean atmosphere
Pavlov, A. A., Brown, L. L., & Kasting, J. F. (2001) · Journal of Geophysical Research Atmospheres · doi:10.1029/2000je001448 · Cited by 297 · cited 11×
“While the climatic effects of this haze have been studied ( e.g. , Pavlov et al. , 2001b), impacts of haze on Archean Earth’s habitability have not been previously investigated using tightly coupled climate-photochemical models.”
InfluentialTHE EVOLUTION OF SOLAR FLUX FROM 0.1 nm TO 160 μm: QUANTITATIVE ESTIMATES FOR PLANETARY STUDIES
Claire, M. W., Sheets, J., Cohen, M., Ribas, I., Meadows, V., & Catling, D. C. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/757/1/95 · Cited by 292 · cited 3×
“…particle microphysics) is run first to generate an initial atmospheric state based on user-specified boundary conditions [gas mixing ratios or fluxes, the solar constant at 2.7 Ga (Claire et al. , 2012), the stellar spectral type, total atmospheric pressure, the initial temperature-pressure profile].”
InfluentialSelf-citationOrganic haze on Titan and the early Earth
Trainer, M. G., Pavlov, A. A., DeWitt, H. L., Jimenez, J. L., McKay, C. P., Toon, O. B., & Tolbert, M. A. (2006) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0608561103 · Cited by 280
Self-citationSpectral Evolution of an Earth‐like Planet
Kaltenegger, L., Traub, W. A., & Jucks, K. W. (2007) · The Astrophysical Journal · doi:10.1086/510996 · Cited by 274 · cited 2×
“Those spectral studies that consider Archean Earth and anoxic planets have not examined hazes (Meadows, 2006; Kaltenegger et al. , 2007; Domagal-Goldman et al. , 2011).”
Late Archean rise of aerobic microbial ecosystems
Eigenbrode, J. L., & Freeman, K. H. (2006) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0607540103 · Cited by 251 · cited 2×
“Negative values of d (13)Corg below -37& are typically interpreted as evidence for methanogenesis (biological methane production) followed by subsequent incorporation into sediments by methanotrophy (methane consumption), which imparts a strongly negative d(13)Corg because organisms preferentially uptake the (12)C (Ur…”
A bistable organic-rich atmosphere on the Neoarchaean Earth
Zerkle, A. L., Claire, M. W., Domagal-Goldman, S. D., Farquhar, J., & Poulton, S. W. (2012) · Nature Geoscience · doi:10.1038/ngeo1425 · Cited by 239 · cited 17×
“In this interpretation, haze-free and reducing atmospheric conditions dominated after 2.71 Ga, with haze reappearing in brief intervals of time as suggested by the Zerkle et al. (2012) and Izon et al. (2015) measurements.”
InfluentialSelf-citationGeochemical evidence for terrestrial ecosystems 2.6 billion years ago
Watanabe, Y., Martini, J., & Ohmoto, H. (2000) · Nature · doi:10.1038/35046052 · Cited by 232 · cited 1×
“…communities lived in inter-and su-pratidal zones (Allwood et al. , 2006; Noffke and Awramik, 2013) experiencing frequent, sometimes extended, exposure to the surface environment, and it has been suggested that microbial mats existed on land as early as 2.7–2.6 Ga (Watanabe et al. , 2000).”
InfluentialThe Spectrum of Earthshine: A Pale Blue Dot Observed from the Ground
WOOLF, N. J., Smith, P. S., Traub, W. A., & Jucks, K. W. (2002) · The Astrophysical Journal · doi:10.1086/340929 · Cited by 230 · cited 2×
“Additionally, although we anticipate planetary diversity in the exoplanet population, existing spectral studies are largely focused on the observables of modern-day Earth ( e.g. , Sagan et al. , 1993; Woolf et al. , 2002; Robinson et al. , 2011, 2014a).”
Bardeen, C. G., Toon, O. B., Jensen, E. J., Marsh, D. R., & Harvey, V. L. (2008) · Journal of Geophysical Research: Atmospheres · doi:10.1029/2007jd009515 · Cited by 217 · cited 1×
“Additionally, stratospheric and mesospheric circulation patterns on Earth presently impact high-altitude aerosol distributions by transporting particles preferentially to the poles (Bardeen et al. , 2008).”
Nitrogen Isotopic Composition and Density of the Archean Atmosphere
Marty, B., Zimmermann, L., Pujol, M., Burgess, R., & Philippot, P. (2013) · Science · doi:10.1126/science.1240971 · Cited by 215 · cited 1×
“…pressure (pCO 2 ) in the Archean at 2.7 Ga to be be-tween 0.0036 and 0.018 bar [10–50 · the present atmospheric level (PAL)] (Driese et al. , 2011), while recent estimates of Archean surface pressure ( P surf ) are consistent with values as low as 0.5 bar (Som et al. , 2012; Marty et al. , 2013).”
InfluentialABIOTIC O2LEVELS ON PLANETS AROUND F, G, K, AND M STARS: POSSIBLE FALSE POSITIVES FOR LIFE?
Harman, C. E., Schwieterman, E. W., Schottelkotte, J. C., & Kasting, J. F. (2015) · The Astrophysical Journal · doi:10.1088/0004-637x/812/2/137 · Cited by 210 · cited 1×
“…Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014; Rugheimer et al. , 2013, 2015; Harman et al. , 2015; Schwieterman et al. , 2016).”
Self-citationFormation of Amino Acids and Nucleotide Bases in a Titan Atmosphere Simulation Experiment
Hörst, S. M., Yelle, R. V., Buch, A., Carrasco, N., Cernogora, G., Dutuit, O., Quirico, E., Sciamma-O'Brien, E., Smith, M. A., Somogyi, Á., et al. (2012) · Astrobiology · doi:10.1089/ast.2011.0623 · Cited by 208 · cited 2×
“…haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al. , 1986; McDonald et al. , 1994; DeWitt et al. , 2009; Ho¨rst et al. , 2012; Trainer, 2013)—see also our discussion of haze formation pathways in Section 4.4.”
InfluentialSom, S. M., Catling, D. C., Harnmeijer, J. P., Polivka, P. M., & Buick, R. (2012) · Nature · doi:10.1038/nature10890 · Cited by 207 · cited 1×
“…pressure (pCO 2 ) in the Archean at 2.7 Ga to be be-tween 0.0036 and 0.018 bar [10–50 · the present atmospheric level (PAL)] (Driese et al. , 2011), while recent estimates of Archean surface pressure ( P surf ) are consistent with values as low as 0.5 bar (Som et al. , 2012; Marty et al. , 2013).”
InfluentialUrey, H. C., & Greiff, L. J. (1935) · Journal of the American Chemical Society · doi:10.1021/ja01305a026 · Cited by 206 · cited 2×
“Negative values of d (13)Corg below -37& are typically interpreted as evidence for methanogenesis (biological methane production) followed by subsequent incorporation into sediments by methanotrophy (methane consumption), which imparts a strongly negative d(13)Corg because organisms preferentially uptake the (12)C (Ur…”
Earth as an Extrasolar Planet: Earth Model Validation Using EPOXI Earth Observations
Robinson, T. D., Meadows, V., Crisp, D., Deming, D., A’Hearn, M. F., Charbonneau, D., Livengood, T. A., Seager, S., Barry, R. K., Hearty, T., et al. (2011) · Astrobiology · doi:10.1089/ast.2011.0642 · Cited by 204 · cited 3×
“Additionally, although we anticipate planetary diversity in the exoplanet population, existing spectral studies are largely focused on the observables of modern-day Earth ( e.g. , Sagan et al. , 1993; Woolf et al. , 2002; Robinson et al. , 2011, 2014a).”
Self-citationOrganic haze, glaciations and multiple sulfur isotopes in the Mid-Archean Era
Domagal-Goldman, S. D., Kasting, J. F., Johnston, D. T., & Farquhar, J. (2008) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.01.040 · Cited by 204 · cited 14×
“…2015), supporting theoretical studies on the causes and consequences of photochemical haze formation in the atmosphere (Pavlov et al. , 2001a, 2001b; Domagal-Goldman et al. , 2008; Haqq-Misra et al. , 2008; Kurzweil et al. , 2013; Claire et al. , 2014) as well as experimental data (Trainer et al.…”
InfluentialSelf-citationABIOTIC OZONE AND OXYGEN IN ATMOSPHERES SIMILAR TO PREBIOTIC EARTH
Domagal-Goldman, S. D., Segura, A., Claire, M. W., Robinson, T. D., & Meadows, V. S. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/792/2/90 · Cited by 198 · cited 1×
“…Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014; Rugheimer et al. , 2013, 2015; Harman et al. , 2015; Schwieterman et al. , 2016).”
Self-citationShields, A. L., Meadows, V., Bitz, C. M., Pierrehumbert, R. T., Joshi, M., & Robinson, T. D. (2013) · Astrobiology · doi:10.1089/ast.2012.0961 · Cited by 197 · cited 2×
“Because of this, planets orbiting stars emitting a high proportion of radiation at NIR wavelengths are harder to freeze (Shields et al. , 2013).”
Self-citationUsing Biogenic Sulfur Gases as Remotely Detectable Biosignatures on Anoxic Planets
Domagal-Goldman, S. D., Meadows, V. S., Claire, M. W., & Kasting, J. F. (2011) · Astrobiology · doi:10.1089/ast.2010.0509 · Cited by 191 · cited 4×
“Those spectral studies that consider Archean Earth and anoxic planets have not examined hazes (Meadows, 2006; Kaltenegger et al. , 2007; Domagal-Goldman et al. , 2011).”
InfluentialSelf-citationMethane and climate during the Precambrian era
KASTING, J. (2005) · Precambrian Research · doi:10.1016/j.precamres.2005.03.002 · Cited by 190 · cited 4×
“…of 1 and 5 Earth masses, respectively (Guzma´n-Marmolejo et al. , 2013), although there has been earlier speculation of higher abiotic production rates (Kasting, 2005; Shaw, 2008), especially if ancient seafloor spreading rates were faster or the amount of iron-rich ancient seafloor rock was…”
InfluentialLittler, M. M., Littler, D. S., Blair, S. M., & Norris, J. N. (1986) · Deep Sea Research Part A Oceanographic Research Papers · doi:10.1016/0198-0149(86)90003-8 · Cited by 190 · cited 1×
“Note that photo-synthetic organisms would not likely have been photon limited by the lower light levels under the haze: the lower light limit for red algae is 6 · 10 15 photons/m 2 /s (Littler et al. , 1986).”
Young, G. M., Brunn, V. V., Gold, D. J. C., & Minter, W. E. L. (1998) · The Journal of Geology · doi:10.1086/516039 · Cited by 189 · cited 2×
“By using the updated habitability threshold of T surf > 248 K, all our cases even with thick hazes are habitable. be consistent with a reported glaciation event at 2.9 Ga (Young et al. , 1998) as a previous study has suggested (Domagal-Goldman et al. , 2008).”
InfluentialThe Jormungand global climate state and implications for Neoproterozoic glaciations
Abbot, D. S., Aiko Voigt, A., & Koll, D. D. B. (2011) · Journal of Geophysical Research Atmospheres · doi:10.1029/2011jd015927 · Cited by 181 · cited 1×
“Furthermore, Abbot et al. (2011) argued that ocean open belts can remain climatologically stable, even if the ice latitude is reduced to 5–15 (cid:2) .”
Chemical Investigation of Titan and Triton Tholins
McDonald, G. D., Thompson, W. R., Heinrich, M., Khare, B. N., & Sagan, C. (1994) · Icarus · doi:10.1006/icar.1994.1046 · Cited by 180 · cited 1×
“…haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al. , 1986; McDonald et al. , 1994; DeWitt et al. , 2009; Ho¨rst et al. , 2012; Trainer, 2013)—see also our discussion of haze formation pathways in Section 4.4.”
InfluentialBiological Effects of High Ultraviolet Radiation on Early Earth—a Theoretical Evaluation
Cockell, C. S. (1998) · Journal of Theoretical Biology · doi:10.1006/jtbi.1998.0738 · Cited by 177 · cited 1×
“On the other hand, if organisms remained protected by some other UV shield such as minerals, layers of overlying microbial mat, or water (Cockell, 1998), changes in UV radiation levels should not affect them as strongly, so the colder conditions created by the haze might have been the larger source…”
Fractal Organic Hazes Provided an Ultraviolet Shield for Early Earth
Wolf, E. T., & Toon, O. B. (2010) · Science · doi:10.1126/science.1183260 · Cited by 172 · cited 15×
“…et al. , 2012; Kurzweil et al. , 2013; Claire et al. , 2014; Izon et al. , 2015) that strongly interacted with visible and UV radiation, cooling the planet’s climate (Pavlov et al. , 2001b; Domagal-Goldman et al. , 2008; Haqq-Misra et al. , 2008; Wolf and Toon, 2010; Ha-senkopf et al. , 2011).”
InfluentialSelf-citationLARGE ABUNDANCES OF POLYCYCLIC AROMATIC HYDROCARBONS IN TITAN'S UPPER ATMOSPHERE
López‐Puertas, M., Dinelli, B. M., Adriani, A., Funke, B., Garcı́a-Comas, M., Moriconi, M. L., D'Aversa, E., Boersma, C., & Allamandola, L. J. (2013) · The Astrophysical Journal · doi:10.1088/0004-637x/770/2/132 · Cited by 169 · cited 1×
“…) and toluene (C 6 H 5 CH 3 ), and indirect evidence for polycyclic aromatic hydrocarbons (PAHs) and nitrogen-containing polycyclic aromatic hydrocarbons (PANHs), indicating that these compounds might play a role in the formation of Titan’s hazes (Waite et al. , 2007; Lo´pez-Puertas et al. , 2013).”
The evolution of atmospheric ozone
Kasting, J. F., & Donahue, T. M. (1980) · Journal of Geophysical Research: Oceans · doi:10.1029/jc085ic06p03255 · Cited by 165 · cited 1×
“This model also has a long heritage of being used to study photochemistry in nonhazy atmospheres ( e.g. , Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010;…”
Arney, G., Meadows, V., Crisp, D., Schmidt, S. J., Bailey, J., & Robinson, T. D. (2014) · Journal of Geophysical Research Planets · doi:10.1002/2014je004662 · Cited by 164 · cited 1×
“SMART has been validated against observations of multiple solar system planets (Robinson et al. , 2011; Arney et al. , 2014).”
Self-citationSulfur, ultraviolet radiation, and the early evolution of life
Kasting, J. F., Zahnle, K. J., Pinto, J. P., & Young, A. T. (1989) · Origins of life and evolution of the biosphere · doi:10.1007/bf01808144 · Cited by 164 · cited 1×
“Aerosol formation follows the method used in Kasting et al. (1989) and described and updated in Pavlov et al. (2001b).”
Amino acids derived from Titan Tholins
Khare, B. N., Sagan, C., Ogino, H., Nagy, B., Er, C., Schram, K. H., & Arakawa, E. T. (1986) · Icarus · doi:10.1016/0019-1035(86)90080-1 · Cited by 164 · cited 2×
“Laboratory experiments on organic haze formation have shown that haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al., 1986; McDonald et al., 1994; DeWitt et al., 2009; Hörst et al., 2012; Trainer, 2013)—see also our discussion of ha…”
Abiotic formation of O2and O3in high-CO2terrestrial atmospheres
Segura, A., Meadows, V. S., Kasting, J. F., Crisp, D., & Cohen, M. (2007) · Astronomy and Astrophysics · doi:10.1051/0004-6361:20066663 · Cited by 163 · cited 1×
“…of being used to study photochemistry in nonhazy atmospheres ( e.g. , Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014;…”
Self-citationDriese, S. G., Jirsa, M. A., Ren, M., Brantley, S. L., Sheldon, N. D., Parker, D., & Schmitz, M. (2011) · Precambrian Research · doi:10.1016/j.precamres.2011.04.003 · Cited by 155 · cited 13×
“Recent paleosol measurements have constrained the CO 2 partial pressure (pCO 2 ) in the Archean at 2.7 Ga to be be-tween 0.0036 and 0.018 bar [10–50 · the present atmospheric level (PAL)] (Driese et al. , 2011), while recent estimates of Archean surface pressure ( P surf ) are consistent with values as low as 0.5 bar…”
InfluentialStromatolites and MISS—Differences between relatives
Noffke, N., & Awramik, S. M. (2013) · GSA Today · doi:10.1130/gsatg187a.1 · Cited by 155 · cited 1×
“There is evidence that Archean stromatolitic communities lived in inter-and su-pratidal zones (Allwood et al. , 2006; Noffke and Awramik, 2013) experiencing frequent, sometimes extended, exposure to the surface environment, and it has been suggested that microbial mats existed on land as early as…”
Oxygen levels in the prebiological atmosphere
Kasting, J. F., Liu, S. C., & Donahue, T. M. (1979) · Journal of Geophysical Research: Oceans · doi:10.1029/jc084ic06p03097 · Cited by 153 · cited 1×
“D photochemical code developed originally by Kasting et al. (1979), but the version we use here was significantly modernized and updated by Zahnle et al. (2006) and uses the haze formation scheme described by Pavlov et al. (2001b).”
Oxygen compounds in Titan's stratosphere as observed by Cassini CIRS
de Kok, R. J., Irwin, P. G. J., Teanby, N. A., Lellouch, E., Bézard, B., Vinatier, S., Nixon, C. A., Fletcher, L. N., Howett, C. J. A., Calcutt, S. B., et al. (2006) · Icarus · doi:10.1016/j.icarus.2006.09.016 · Cited by 152 · cited 1×
“Early Earth’s atmosphere would have contained negligible O 2 but significant amounts of CO 2 ( e.g. , Kasting, 1993; Driese et al. , 2011), whereas Titan’s atmosphere is extremely reducing (de Kok et al. , 2007).”
Exploring the faint young Sun problem and the possible climates of the Archean Earth with a 3‐D GCM
Charnay, B., Forget, F., Wordsworth, R., Leconte, J., Millour, E., Codron, F., & Spiga, A. (2013) · Journal of Geophysical Research: Atmospheres · doi:10.1002/jgrd.50808 · Cited by 144 · cited 4×
“However, as we have argued, a mean surface temperature of the freezing point of water is not a useful threshold for global habitability (Charnay et al. , 2013; Shields et al. , 2013; Wolf and Toon, 2013; Kunze et al. , 2014), so some of the Haqq-Misra et al. spherical haze results may actually be…”
InfluentialSelf-citationSpectral Fingerprints of Earth-like Planets Around FGK Stars
Rugheimer, S., Kaltenegger, L., Zsom, A., Segura, A., & Sasselov, D. (2013) · Astrobiology · doi:10.1089/ast.2012.0888 · Cited by 143 · cited 2×
“…climate of early Mars (Ramirez et al. , 2013), the atmospheres of Earth-like planets around various stellar types (Segura et al. , 2003, 2005, 2010; Rugheimer et al. , 2013), clouds in exoplanet THE PALE ORANGE DOT atmospheres (Kitzmann et al. , 2010, 2011a), and the climate of early Earth…”
Hospitable Archean Climates Simulated by a General Circulation Model
Wolf, E. T., & Toon, O. B. (2013) · Astrobiology · doi:10.1089/ast.2012.0936 · Cited by 143 · cited 6×
“D studies have shown that Archean Earth can maintain an open ocean fraction of > 50% for T GAT ‡ 260 K and an equatorial open ocean belt for T GAT ‡ 248 K (Wolf and Toon, 2013; Charnay et al. , 2013).”
InfluentialSelf-citationCharnay, B., Meadows, V., Misra, A., Leconte, J., & Arney, G. (2015) · The Astrophysical Journal Letters · doi:10.1088/2041-8205/813/1/l1 · Cited by 140 · cited 1×
“The planet colors were calculated using the ‘‘Spectral Color Spreadsheet’’ from brucelindbloom.com with the same method used by Charnay et al. (2015) for GJ 1214b.”
Self-citationKhare, B. N., Sagan, C., Thompson, W. R., Arakawa, E. T., Suits, F., Callcott, T. A., Williams, M. W., Shrader, S. A., Ogino, H., Willingham, T. O., et al. (1984) · Advances in Space Research · doi:10.1016/0273-1177(84)90545-3 · Cited by 139 · cited 5×
“Refractive indices, shown in the bottom panels, are presented from information in Khare et al. (1984a). extends to 100 km, but we have only been able to successfully run the climate model up to about 80 km for our 1 bar atmospheres.”
InfluentialDillon, J. G., & Castenholz, R. W. (1999) · Journal of Phycology · doi:10.1046/j.1529-8817.1999.3540673.x · Cited by 137 · cited 2×
“28 lm) wavelength range (Pierson et al., 1992; Dillon and Castenholz, 1999), but in the modern atmosphere, UVC is fully blocked by O2 and ozone.”
InfluentialUV SURFACE ENVIRONMENT OF EARTH-LIKE PLANETS ORBITING FGKM STARS THROUGH GEOLOGICAL EVOLUTION
Rugheimer, S., Segura, A., Kaltenegger, L., & Sasselov, D. (2015) · The Astrophysical Journal · doi:10.1088/0004-637x/806/1/137 · Cited by 131 · cited 3×
“…Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014; Rugheimer et al. , 2013, 2015; Harman et al. , 2015; Schwieterman et al. , 2016).”
InfluentialGrenfell, J. L., Stracke, B., von Paris, P., Patzer, B., Titz, R., Segura, A., & Rauer, H. (2006) · Planetary and Space Science · doi:10.1016/j.pss.2006.09.002 · Cited by 124 · cited 2×
“This model also has a long heritage of being used to study photochemistry in nonhazy atmospheres (e.g., Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al., 2003; Segura et al., 2003, 2005, 2007, 2010; Zahnle et al., 2006; Grenfell et al., 2007; Catling et al., 2010; Domagal-Goldman et al., 2011, 2014; Rug…”
GLANCING VIEWS OF THE EARTH: FROM A LUNAR ECLIPSE TO AN EXOPLANETARY TRANSIT
Muñoz, A. G., Osorio, M. R. Z., Barrena, R., Montañés-Rodríguez, P., Martín, E. L., & Pallé, E. (2012) · The Astrophysical Journal · doi:10.1088/0004-637x/755/2/103 · Cited by 120 · cited 1×
“In Earth-like clear-sky atmospheres, the minimum atmospheric altitude transit observations are able to probe will typically be limited by refraction (Garcı´a Mun˜oz et al. , 2012; Be´tre´mieux and Kaltenegger, 2014; Misra et al. , 2014b), but in hazy atmospheres, haze controls the minimum effective…”
Bétremieux, Y., & Kaltenegger, L. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/791/1/7 · Cited by 117 · cited 1×
“…the minimum atmospheric altitude transit observations are able to probe will typically be limited by refraction (Garcı´a Mun˜oz et al. , 2012; Be´tre´mieux and Kaltenegger, 2014; Misra et al. , 2014b), but in hazy atmospheres, haze controls the minimum effective tangent height, especially…”
DETECTION OF OCEAN GLINT AND OZONE ABSORPTION USINGLCROSSEARTH OBSERVATIONS
Robinson, T. D., Ennico, K., Meadows, V., Sparks, W. B., Bussey, D. B. J., Schwieterman, E. W., & Breiner, J. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/787/2/171 · Cited by 115 · cited 2×
“Additionally, although we anticipate planetary diversity in the exoplanet population, existing spectral studies are largely focused on the observables of modern-day Earth ( e.g. , Sagan et al. , 1993; Woolf et al. , 2002; Robinson et al. , 2011, 2014a).”
Self-citationEarth's atmosphere – Hadean to early Proterozoic
Shaw, G. H. (2008) · Geochemistry · doi:10.1016/j.chemer.2008.05.001 · Cited by 114 · cited 1×
“…of 1 and 5 Earth masses, respectively (Guzma´n-Marmolejo et al. , 2013), although there has been earlier speculation of higher abiotic production rates (Kasting, 2005; Shaw, 2008), especially if ancient seafloor spreading rates were faster or the amount of iron-rich ancient seafloor rock was greater.”
Imanaka, H., Cruikshank, D. P., Khare, B. N., & McKay, C. P. (2011) · Icarus · doi:10.1016/j.icarus.2011.11.018 · Cited by 113 · cited 1×
“…ranges indicate disagreement with the Khare measurements (Ramirez et al. , 2002; Tran et al. , 2003; Vuitton et al. , 2009; Hasenkopf et al. , 2010; Imanaka et al. , 2012; Mahjoub et al. , 2012; Sciamma-O’Brien et al. , 2012), although these measurements themselves show considerable variation…”
Crisp, D. (1997) · Geophysical Research Letters · doi:10.1029/97gl50245 · Cited by 113 · cited 1×
“D line-by-line fully multiple scattering radiative transfer model (Meadows and Crisp, 1996; Crisp, 1997).”
Schwieterman, E. W., Meadows, V. S., Domagal-Goldman, S. D., Deming, D., Arney, G. N., Luger, R., Harman, C. E., Misra, A., & Barnes, R. (2016) · The Astrophysical Journal Letters · doi:10.3847/2041-8205/819/1/l13 · Cited by 111 · cited 1×
“…Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et al. , 2011, 2014; Rugheimer et al. , 2013, 2015; Harman et al. , 2015; Schwieterman et al. , 2016).”
Self-citationModeling the signature of sulfur mass-independent fractionation produced in the Archean atmosphere
Claire, M. W., Kasting, J. F., Domagal-Goldman, S. D., Stüeken, E. E., Buick, R., & Meadows, V. S. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.06.032 · Cited by 108 · cited 11×
“…mass-independent sulfur isotope fractionation signal (S-MIF) (Farquhar et al. , 2000) preserved in the geological record before the Great Oxygenation Event (GOE) at about 2.5 Ga (Domagal-Goldman et al. , 2008; Zerkle et al. , 2012; Kurzweil et al. , 2013; Claire et al. , 2014; Izon et al. , 2015).”
InfluentialSelf-citationTitan solar occultation observations reveal transit spectra of a hazy world
Robinson, T. D., Maltagliati, L., Marley, M. S., & Fortney, J. J. (2014) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1403473111 · Cited by 107 · cited 2×
“Additionally, although we anticipate planetary diversity in the exoplanet population, existing spectral studies are largely focused on the observables of modern-day Earth ( e.g. , Sagan et al. , 1993; Woolf et al. , 2002; Robinson et al. , 2011, 2014a).”
Complex Refractive Index of Titan's Aerosol Analogues in the 200–900 nm Domain
Ramírez, S. I. (2002) · Icarus · doi:10.1006/icar.2001.6783 · Cited by 105 · cited 1×
“…more recent measurements of hydrocarbon refractive indices over more restricted wavelength ranges indicate disagreement with the Khare measurements (Ramirez et al. , 2002; Tran et al. , 2003; Vuitton et al. , 2009; Hasenkopf et al. , 2010; Imanaka et al. , 2012; Mahjoub et al. , 2012;…”
Thomazo, C., Ader, M., Farquhar, J. D., & Philippot, P. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.12.036 · Cited by 103 · cited 2×
“Kurzweil et al. (2013) noted that an increase in magnitude of S-MIF signals after 2.73 Ga (Thomazo et al. , 2009) oc-curred during a prolonged negative shift in d 13 C org , suggesting enhanced biological methane activity at this time.”
InfluentialMean-field approximation of Mie scattering by fractal aggregates of identical spheres
Botet, R. S., Rannou, P., & Cabane, M. (1997) · Applied Optics · doi:10.1364/ao.36.008791 · Cited by 100 · cited 5×
“The mean field approximation we use for fractal scattering has been validated against scattering by silica fractal aggregates (Botet et al. , 1997) and Titan’s hazes (Rannou et al. , 1997; Larson et al. , 2015).”
InfluentialTitan - Aerosol photochemistry and variations related to the sunspot cycle
Allen, M., Yung, Y. L., & Pinto, J. P. (1980) · The Astrophysical Journal · doi:10.1086/183416 · Cited by 99 · cited 2×
“Following the mechanism proposed for the formation of Titan’s hydrocarbon haze (Allen et al. , 1980; Yung et al. , 1984), every model of hydrocarbon haze formation in early Earth’s atmosphere—including ours—has assumed that aerosol formation will occur through the formation of acetylene (C 2 H 2 )…”
Multiple oscillations in Neoarchaean atmospheric chemistry
Izon, G., Zerkle, A. L., Zhelezinskaia, I., Farquhar, J., Newton, R. J., Poulton, S. W., Eigenbrode, J. L., & Claire, M. W. (2015) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2015.09.018 · Cited by 99 · cited 17×
“In this interpretation, haze-free and reducing atmospheric conditions dominated after 2.71 Ga, with haze reappearing in brief intervals of time as suggested by the Zerkle et al. (2012) and Izon et al. (2015) measurements.”
InfluentialSelf-citationAbiotic Production of Methane in Terrestrial Planets
Guzmán-Marmolejo, A., Segura, A., & Escobar-Briones, E. (2013) · Astrobiology · doi:10.1089/ast.2012.0817 · Cited by 96 · cited 3×
“…primary nonbiological source, has been estimated as 6.8 · 10 8 and 1.3 · 10 9 molecules/cm 2 /s for rocky planets of 1 and 5 Earth masses, respectively (Guzma´n-Marmolejo et al. , 2013), although there has been earlier speculation of higher abiotic production rates (Kasting, 2005; Shaw, 2008),…”
InfluentialA new interpretation of scattered light measurements at Titan's limb
Rannou, P., Cabane, M., Botet, R. S., & Chassefière, É. (1997) · Journal of Geophysical Research Atmospheres · doi:10.1029/97je00719 · Cited by 95 · cited 5×
“The mean field approximation we use for fractal scattering has been validated against scattering by silica fractal aggregates (Botet et al. , 1997) and Titan’s hazes (Rannou et al. , 1997; Larson et al. , 2015).”
InfluentialAtmospheric sulfur rearrangement 2.7 billion years ago: Evidence for oxygenic photosynthesis
Kurzweil, F., Claire, M., Thomazo, C., Peters, M., Hannington, M., & Strauss, H. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.01.028 · Cited by 91 · cited 15×
“…of an organic haze (Pavlov et al. , 2001a; Trainer et al. , 2004, 2006; DeWitt et al. , 2009; Hasenkopf et al. , 2010; Zerkle et al. , 2012; Kurzweil et al. , 2013; Claire et al. , 2014; Izon et al. , 2015) that strongly interacted with visible and UV radiation, cooling the planet’s…”
InfluentialSelf-citationPierson, B. K., Mitchell, H. K., & Ruff-Roberts, A. L. (1993) · Origins of Life and Evolution of Biospheres · doi:10.1007/bf01581902 · Cited by 90 · cited 3×
“We compare these values to the tolerances of Chloroflexus aurantiacus (Pierson et al. , 1992), a deep-branching, mat-forming anoxygenic phototroph with UV resistance that has been studied as an analogue for Archean phototrophs.”
InfluentialClouds in the atmospheres of extrasolar planets
Kitzmann, D., Patzer, A. B. C., von Paris, P., Godolt, M., Stracke, B., Gebauer, S., Grenfell, J. L., & Rauer, H. (2010) · Astronomy and Astrophysics · doi:10.1051/0004-6361/200913491 · Cited by 88 · cited 1×
“…(Ramirez et al. , 2013), the atmospheres of Earth-like planets around various stellar types (Segura et al. , 2003, 2005, 2010; Rugheimer et al. , 2013), clouds in exoplanet THE PALE ORANGE DOT atmospheres (Kitzmann et al. , 2010, 2011a), and the climate of early Earth (Haqq-Misra et al. , 2008).”
Optical properties of Titan and early Earth haze laboratory analogs in the mid-visible
Hasenkopf, C. A., Beaver, M. R., Trainer, M. G., DeWitt, H. L., Freedman, M. A., Toon, O. B., McKay, C. P., & Tolbert, M. A. (2009) · Icarus · doi:10.1016/j.icarus.2009.12.015 · Cited by 84 · cited 8×
“…an anoxic atmosphere could have supported the formation of an organic haze (Pavlov et al. , 2001a; Trainer et al. , 2004, 2006; DeWitt et al. , 2009; Hasenkopf et al. , 2010; Zerkle et al. , 2012; Kurzweil et al. , 2013; Claire et al. , 2014; Izon et al. , 2015) that strongly interacted with…”
InfluentialSelf-citationUsing Dimers to Measure Biosignatures and Atmospheric Pressure for Terrestrial Exoplanets
Misra, A., Meadows, V., Claire, M., & Crisp, D. (2014) · Astrobiology · doi:10.1089/ast.2013.0990 · Cited by 84 · cited 1×
“To generate transit transmission spectra, we use the SMART-T model (Misra et al. , 2014a, 2014b).”
Self-citationTHE EFFECTS OF REFRACTION ON TRANSIT TRANSMISSION SPECTROSCOPY: APPLICATION TO EARTH-LIKE EXOPLANETS
Misra, A., Meadows, V., & Crisp, D. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/792/1/61 · Cited by 83 · cited 1×
“…transit observations are able to probe will typically be limited by refraction (Garcı´a Mun˜oz et al. , 2012; Be´tre´mieux and Kaltenegger, 2014; Misra et al. , 2014b), but in hazy atmospheres, haze controls the minimum effective tangent height, especially at shorter wavelengths where it…”
Self-citationThe JWST MIRI instrument concept
Wright, G., Rieke, G. H., Colina, L., et al. (2004) · Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIE · doi:10.1117/12.551717 · Cited by 79 · cited 2×
“Absorption from the haze itself can be seen as the ‘‘bump’’ in the ‘‘thick’’ haze (CH 4 /CO 2 = 0.21) transit transmission spectrum at 6 l m, a wavelength region accessible with the James Webb Space Telescope (Wright et al. , 2004).”
InfluentialHaze Aerosols in the Atmosphere of Early Earth: Manna from Heaven
Trainer, M. G., Pavlov, A. A., Curtis, D. B., McKay, C. P., Worsnop, D. R., Delia, A. E., Toohey, D. W., Toon, O. B., & Tolbert, M. A. (2004) · Astrobiology · doi:10.1089/ast.2004.4.409 · Cited by 79 · cited 2×
“…, 2001a, 2001b; Domagal-Goldman et al. , 2008; Haqq-Misra et al. , 2008; Kurzweil et al. , 2013; Claire et al. , 2014) as well as experimental data (Trainer et al. , 2004, 2006; DeWitt et al. , 2009; Hasenkopf et al. , 2010, 2011) and theory on their potential radiative effects (Wolf and Toon,…”
Self-citationInfluence of methane concentration on the optical indices of Titan’s aerosols analogues
Mahjoub, A., Carrasco, N., Dahoo, P., Gautier, T., Szopa, C., & Cernogora, G. (2012) · Icarus · doi:10.1016/j.icarus.2012.08.015 · Cited by 76 · cited 2×
“…with the Khare measurements (Ramirez et al. , 2002; Tran et al. , 2003; Vuitton et al. , 2009; Hasenkopf et al. , 2010; Imanaka et al. , 2012; Mahjoub et al. , 2012; Sciamma-O’Brien et al. , 2012), although these measurements themselves show considerable variation among each other (Fig.”
Simulation of Titan haze formation using a photochemical flow reactor
Tran, B. N., Joseph, J. C., Ferris, J. P., Persans, P. D., & Chera, J. J. (2003) · Icarus · doi:10.1016/s0019-1035(03)00209-4 · Cited by 75 · cited 1×
“…of hydrocarbon refractive indices over more restricted wavelength ranges indicate disagreement with the Khare measurements (Ramirez et al. , 2002; Tran et al. , 2003; Vuitton et al. , 2009; Hasenkopf et al. , 2010; Imanaka et al. , 2012; Mahjoub et al. , 2012; Sciamma-O’Brien et al. , 2012),…”
Nitrogen Incorporation in CH 4 -N 2 Photochemical Aerosol Produced by Far Ultraviolet Irradiation
Trainer, M. G., Jimenez, J. L., Yung, Y. L., Toon, O. B., & Tolbert, M. A. (2012) · Astrobiology · doi:10.1089/ast.2011.0754 · Cited by 74 · cited 1×
“Studies have shown the formation of HCN, CH 3 CN, and other nitrile gas species are formed using the same type of UV source in a CH 4 /N 2 gas mixture, thus corroborating the indirect nitrogen photochemistry (Trainer et al. , 2012; Yoon et al. , 2014).”
Self-citationInvestigating the early Earth faint young Sun problem with a general circulation model
Kunze, M., Godolt, M., Langematz, U., Grenfell, J. L., Hamann-Reinus, A., & Rauer, H. (2013) · Planetary and Space Science · doi:10.1016/j.pss.2013.09.011 · Cited by 71 · cited 2×
“…have argued, a mean surface temperature of the freezing point of water is not a useful threshold for global habitability (Charnay et al. , 2013; Shields et al. , 2013; Wolf and Toon, 2013; Kunze et al. , 2014), so some of the Haqq-Misra et al. spherical haze results may actually be ‘‘habitable.’’”
Clouds and the Faint Young Sun Paradox
Goldblatt, C., & Zahnle, K. J. (2011) · Climate of the Past · doi:10.5194/cp-7-203-2011 · Cited by 71 · cited 2×
“Of course, the true cloud distribution on Archean Earth is unknown, and clouds may have had important climatic effects on our early planet (Goldblatt and Zahnle, 2011).”
Thomassot, É., OʼNeil, J., Francis, D., Cartigny, P., & Wing, B. A. (2015) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1419681112 · Cited by 66 · cited 2×
“8 billion years of Earth’s formation, a common mechanism for S-MIF production was already established in the atmosphere (Thomassot et al., 2015).”
InfluentialAtmospheric Prebiotic Chemistry and Organic Hazes
Trainer, M. G. (2013) · Current Organic Chemistry · doi:10.2174/13852728113179990078 · Cited by 66 · cited 4×
“Laboratory experiments on organic haze formation have shown that haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al., 1986; McDonald et al., 1994; DeWitt et al., 2009; Hörst et al., 2012; Trainer, 2013)—see also our discussion of ha…”
InfluentialSelf-citationIN SITU MEASUREMENTS OF THE SIZE AND DENSITY OF TITAN AEROSOL ANALOGS
Hörst, S. M., & Tolbert, M. A. (2013) · The Astrophysical Journal Letters · doi:10.1088/2041-8205/770/1/l10 · Cited by 64 · cited 1×
“Ho¨rst and Tolbert (2013) measured a similar effective particle density, 0.65 g/ cm 3 , for a 0.1% CH 4 haze experiment using a UV lamp.”
InfluentialReduction in Haze Formation Rate on Prebiotic Earth in the Presence of Hydrogen
DeWitt, H. L., Trainer, M. G., Pavlov, A. A., Hasenkopf, C. A., Aiken, A. C., Jimenez, J. L., McKay, C. P., Toon, O. B., & Tolbert, M. A. (2009) · Astrobiology · doi:10.1089/ast.2008.0289 · Cited by 59 · cited 9×
“…haze-formation chemistry can involve the formation of important prebiotic molecules such as amino acids and nucleotide bases (Khare et al. , 1986; McDonald et al. , 1994; DeWitt et al. , 2009; Ho¨rst et al. , 2012; Trainer, 2013)—see also our discussion of haze formation pathways in Section 4.4.”
InfluentialSelf-citationVIEWS FROMEPOXI: COLORS IN OUR SOLAR SYSTEM AS AN ANALOG FOR EXTRASOLAR PLANETS
Crow, C. A., McFadden, L. A., Robinson, T. D., Meadows, V., Livengood, T. A., Hewagama, T., Barry, R. K., Deming, D., Lisse, C. M., & Wellnitz, D. D. (2011) · The Astrophysical Journal · doi:10.1088/0004-637x/729/2/130 · Cited by 59
Self-citationThe role of benzene photolysis in Titan haze formation
Yoon, Y. H., Hörst, S. M., Hicks, R. K., Li, R. S., de Gouw, J. A., & Tolbert, M. A. (2014) · Icarus · doi:10.1016/j.icarus.2014.02.006 · Cited by 57 · cited 2×
“Studies have shown the formation of HCN, CH3CN, and other nitrile gas species are formed using the same type of UV source in a CH4/N2 gas mixture, thus corroborating the indirect nitrogen photochemistry (Trainer et al., 2012; Yoon et al., 2014).”
Chemical Evolution on Titan: Comparisons to the Prebiotic Earth
Clarke, D. W., & Ferris, J. P. (1997) · Springer eBooks · doi:10.1007/978-94-015-8907-9_12 · Cited by 55
Clouds in the atmospheres of extrasolar planets
Kitzmann, D., Patzer, A. B. C., von Paris, P., Godolt, M., & Rauer, H. (2011) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201014343 · Cited by 52 · cited 3×
“…(Ramirez et al. , 2013), the atmospheres of Earth-like planets around various stellar types (Segura et al. , 2003, 2005, 2010; Rugheimer et al. , 2013), clouds in exoplanet THE PALE ORANGE DOT atmospheres (Kitzmann et al. , 2010, 2011a), and the climate of early Earth (Haqq-Misra et al. , 2008).”
InfluentialDespinning of the earth rotation in the geological past and geomagnetic paleointensities
Denis, C., Schreider, A. A., Varga, P., et al. (2002) · Journal of Geodynamics · doi:10.1016/s0264-3707(02)00049-2 · Cited by 48 · cited 1×
“Our SZA = 60 (cid:2) flux, 0.03 W/m 2 , is low enough to allow growth of Chloroflexus aurantiacus over the length of a day in the late Archean [about 18–19 h for a day-night cycle; Denis et al. (2002)].”
InfluentialAtmospheric Production of Glycolaldehyde Under Hazy Prebiotic Conditions
Harman, C. E., Kasting, J. F., & Wolf, E. T. (2013) · Origins of Life and Evolution of Biospheres · doi:10.1007/s11084-013-9332-7 · Cited by 44 · cited 1×
“Subsequent studies using this model or other versions of it to study fractal haze formation include those of Harman et al. (2013), Kurzweil et al. (2013), and Claire et al. (2014), with the latter two of these studies also derived from the same Zahnle et al. (2006) model branch used here.”
Self-citationPotential Climatic Impact of Organic Haze on Early Earth
Hasenkopf, C. A., Freedman, M. A., Beaver, M. R., Toon, O. B., & Tolbert, M. A. (2011) · Astrobiology · doi:10.1089/ast.2010.0541 · Cited by 43 · cited 4×
“, 2015) that strongly interacted with visible and UV radiation, cooling the planet’s climate (Pavlov et al., 2001b; Domagal-Goldman et al., 2008; Haqq-Misra et al., 2008; Wolf and Toon, 2010; Hasenkopf et al., 2011).”
InfluentialMicrophysical modeling of Titan’s detached haze layer in a 3D GCM
Larson, E. J. L., Toon, O. B., West, R. A., & Friedson, A. J. (2015) · Icarus · doi:10.1016/j.icarus.2015.03.010 · Cited by 41 · cited 2×
“The mean field approximation we use for fractal scattering has been validated against scattering by silica fractal aggregates (Botet et al. , 1997) and Titan’s hazes (Rannou et al. , 1997; Larson et al. , 2015).”
IS THE PALE BLUE DOT UNIQUE? OPTIMIZED PHOTOMETRIC BANDS FOR IDENTIFYING EARTH-LIKE EXOPLANETS
Krissansen‐Totton, J., Schwieterman, E. W., Charnay, B., Arney, G., Robinson, T. D., Meadows, V., & Catling, D. C. (2016) · The Astrophysical Journal · doi:10.3847/0004-637x/817/1/31 · Cited by 38 · cited 2×
“Colors and photometric bands have been considered as indicators of Earth-like worlds (Traub, 2003; Crow et al. , 2011; Krissansen-Totton et al. , 2016), but hazy Archean Earth suggests that not all Earth-like planets will be pale blue dots.”
Self-citationSebree, J. A., Stern, J. C., Mandt, K. E., et al. (2015) · Icarus · doi:10.1016/j.icarus.2015.04.016 · Cited by 38
Modelling the Diversity of Extrasolar Terrestrial Planets
Meadows, V. (2005) · Proceedings of the International Astronomical Union · doi:10.1017/s1743921306009033 · Cited by 32 · cited 3×
“Those spectral studies that consider Archean Earth and anoxic planets have not examined hazes (Meadows, 2006; Kaltenegger et al. , 2007; Domagal-Goldman et al. , 2011).”
Self-citationVuitton, V., Tran, B. N., Persans, P. D., & Ferris, J. P. (2009) · Icarus · doi:10.1016/j.icarus.2009.04.016 · Cited by 26 · cited 1×
“…indices over more restricted wavelength ranges indicate disagreement with the Khare measurements (Ramirez et al. , 2002; Tran et al. , 2003; Vuitton et al. , 2009; Hasenkopf et al. , 2010; Imanaka et al. , 2012; Mahjoub et al. , 2012; Sciamma-O’Brien et al. , 2012), although these…”
Diminished greenhouse warming from Archean methane due to solar absorption lines
Byrne, B., & Goldblatt, C. (2015) · Climate of the past · doi:10.5194/cp-11-559-2015 · Cited by 20 · cited 1×
“Our older CH 4 coefficients may overestimate the surface temperature by ( 5 K at the CH 4 mixing ratios used here (Byrne and Goldblatt, 2015).”
McLinden, C. A., McConnell, J. C., Griffoen, E., McElroy, C. T., & Pfister, L. (1997) · Journal of Geophysical Research Atmospheres · doi:10.1029/97jd01079 · Cited by 18
A simplified model of aerosol coagulation
Tolfo, F. (1977) · Journal of Aerosol Science · doi:10.1016/0021-8502(77)90058-1 · Cited by 17 · cited 2×
“Spherical particles in SMART are binned according to log-normal size distributions using the radii mentioned previously and a mode standard deviation of 1.5, which is realistic for an aerosol distribution (Tolfo, 1977).”
InfluentialHicks, R. K., Day, D. A., Jimenez, J. L., et al. (2015) · Analytical Chemistry · doi:10.1021/ac504014g · Cited by 15 · cited 2×
“Since the full chemical scheme that leads to aerosol formation is not well understood despite both laboratory and theoretical studies (e.g., Hallquist et al., 2009; Hicks et al., 2015), it is assumed that C4H2 and C5H4 condense directly to haze particles (called HCAER and HCAER2 in Supplementary Table S1).”
Convective Motion in a Rotating Stratified Fluid Due to Non-Uniform Horizontal Heating
Barcilon, V. (1967) · Journal of the Atmospheric Sciences · doi:10.1175/1520-0469(1967)024 · Cited by 2
Middle Archean continent formation by crustal delamination
Zegers, T. E., & van Keken, P. E. (2001) · Geology · doi:10.1130/0091-7613(2001)029
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- Sciamma-O'Brien E., , Dahoo P.-R., , Hadamcik E., , Carrasco N., , Quirico E., , Szopa C., , and Cernogora G. (2012) Optical constants from 370nm to 900nm of Titan tholins produced in a low pressure RF plasma discharge. Icarus, 218:353–363.
- Traub W.A. (2003) Extrasolar planet characteristics in the visible wavelength range. In Proceedings of the Conference on Towards Other Earths: DARWIN/TPF and the Search for Extrasolar Terrestrial Planets, Heidelberg, Germany, pp 231–239.
- Workman J., editor. (2000) The Handbook of Organic Compounds, Three-Volume Set: NIR, IR, R, and UV-Vis Spectra Featuring Polymers and Surfactants, Academic Press, San Diego, CA.
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Living at the Extremes: Extremophiles and the Limits of Life in a Planetary Context
Merino, N., Aronson, H. S., Bojanova, D. P., Feyhl‐Buska, J., Wong, M. L., Zhang, S. J., & Giovannelli, D. (2019) · Frontiers in Microbiology · doi:10.3389/fmicb.2019.00780 · Cited by 707
Catling, D. C., & Zahnle, K. J. (2020) · Science Advances · doi:10.1126/sciadv.aax1420 · Cited by 568
“Thus, attenuation of sunlight saturates (1, 163).”
BackgroundExoplanet Biosignatures: A Review of Remotely Detectable Signs of Life
Schwieterman, E. W., Kiang, N. Y., Parenteau, M. N., Harman, C. E., DasSarma, S., Fisher, T. M., Arney, G. N., Hartnett, H. E., Reinhard, C. T., Olson, S. L., et al. (2018) · Astrobiology · doi:10.1089/ast.2017.1729 · Cited by 630
“…al., 2013), a purple Archean ocean due to photosynthetic purple bacteria (Sanromá et al., 2014); an orange Archean Earth due to an organic-rich atmospheric haze (Arney et al., 2016); and trajectories of O2 fluxes over geologic time given estimated atmospheric concentrations (Gebauer et al., 2017).”
BackgroundMethodInfluentialSelf-citationExoplanet Biosignatures: A Review of Remotely Detectable Signs of Life
Schwieterman, E. W., Kiang, N. Y.-L., Parenteau, M. N., Harman, C. E., DasSarma, S., Fisher, T. M., Arney, G., Hartnett, H. E., Reinhard, C. T., Olson, S. L., et al. (2017) · eScholarship (California Digital Library) · Cited by 452
Self-citationExoplanet Biosignatures: Understanding Oxygen as a Biosignature in the Context of Its Environment
Meadows, V., Reinhard, C. T., Arney, G., Parenteau, M. N., Schwieterman, E. W., Domagal-Goldman, S. D., Lincowski, A., Stapelfeldt, K. R., Rauer, H., DasSarma, S., et al. (2018) · Astrobiology · doi:10.1089/ast.2017.1727 · Cited by 341
“Such hazes may have been present during early periods of Earth’s history when the atmosphere was more reducing (Arney et al., 2016).”
BackgroundMethodSelf-citation
Metadata
- Authors
- Arney, G., Domagal-Goldman, S. D., Meadows, V. S., Wolf, E. T., Schwieterman, E., Charnay, B., Claire, M., Hébrard, E., & Trainer, M. G.
- Affiliations
- Goddard Space Flight Center (US)
- University of Washington (US)
- University of Colorado Boulder (US)
- University of California, Riverside (US)
- University of St Andrews (GB)
- NASA Goddard Space Flight Center
- Corresponding author
- Arney, Giada
- ORCID
- Charnay, Benjamin
- Venue
- Astrobiology
- Publisher
- SAGE Publications
- Published
- 2016-11
- Volume
- 16
- Issue
- 11
- Pages
- 873-899
- ISSN
- 1531-1074 (ISSN-L)
- 1557-8070
- PMC
- PMC5148108
- OpenAlex
- W2534050968
- Semantic Scholar
- 62da501fd3e70b940830188582e2e383e75193d3
- Cited by
- 327
- References
- 136
- Citations by year
- 2026: 22 · 2025: 59 · 2024: 28 · 2023: 33 · 2022: 33 · 2021: 30 · 2020: 33 · 2019: 25 · 2018: 45 · 2017: 18 · 2016: 1
- FWCI
- 14.17
- Type
- journal article
- Language
- en
- Open access
- hybrid
- doi.org
- Licence
- Locations
- Astrobiology (publishedVersion, cc-by-nc)
- PubMed Central (publishedVersion, cc-by-nc)
- PubMed (publishedVersion)
- Open Research Exeter (University of Exeter) (acceptedVersion)
- arXiv (Cornell University) (submittedVersion)
- HAL (submittedVersion)
- eScholarship (California Digital Library) (submittedVersion, cc-by-nc)
- St Andrews Research Repository (St Andrews Research Repository) (submittedVersion, cc-by-nc)
- arXiv (Cornell University)
- Funders
- Natural Environment Research Council (NE/J022802/2)
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Space Science and Extraterrestrial Life
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Keywords
- Archean, atmospheric haze, habitability, faint young Sun, UV protection, biosignatures, methane, self-shielding, exoplanet atmospheres, surface cooling
- MeSH terms
- Atmosphere, Climate, Extraterrestrial Environment, Gases, Models, Theoretical, Particle Size, Spectrophotometry, Ultraviolet, Temperature, Ultraviolet Rays, Water, Earth, Planet, Exobiology
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
A language model drew the claims from the paper on 2026-10-08, under version 3 of the claim definition (model deepseek-v4.1-flash, prompt extract-v3).
A second model labelled each claim on 2026-10-08 (model jev-1.13-20260917, definition revision gold-guideline-v0.2).
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