A revised, hazy methane greenhouse for the Archean Earth.
about
The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean EarthThe Astrobiology Primer v2.0Photosynthesis in hydrogen-dominated atmospheresAbiotic production of methane in terrestrial planetsAtmospheric Prebiotic Chemistry and Organic HazesAir density 2.7 billion years ago limited to less than twice modern levels by fossil raindrop imprints.Explaining the structure of the Archean mass-independent sulfur isotope record.The future of spectroscopic life detection on exoplanets.Using biogenic sulfur gases as remotely detectable biosignatures on anoxic planetsThe rise of oxygen in Earth's early ocean and atmosphere.Isotope composition and volume of Earth's early oceans.Nitrogen incorporation in CH(4)-N(2) photochemical aerosol produced by far ultraviolet irradiation.Shifting microbial communities sustain multiyear iron reduction and methanogenesis in ferruginous sediment incubations.Spectral fingerprints of Earth-like planets around FGK stars.Rapid oxygenation of Earth's atmosphere 2.33 billion years agoLimited role for methane in the mid-Proterozoic greenhouse.The geobiological nitrogen cycle: From microbes to the mantle.Biological regulation of atmospheric chemistry en route to planetary oxygenation.Availability of O(2) and H(2)O(2) on pre-photosynthetic Earth.Methanotrophy in a Paleoproterozoic oil field ecosystem, Zaonega Formation, Karelia, Russia.An inorganic geochemical argument for coupled anaerobic oxidation of methane and iron reduction in marine sediments.Faint young Sun paradox remains.Biomass recycling and Earth's early phosphorus cycle.Organic Haze as a Biosignature in Anoxic Earth-like Atmospheres.Geoscience: Fossil raindrops and ancient air.The geologic history of seawater pH.Greenhouse warming by nitrous oxide and methane in the Proterozoic Eon.The Habitability of Proxima Centauri b: Environmental States and Observational Discriminants.Fractal organic hazes provided an ultraviolet shield for early Earth.Exoplanet Biosignatures: A Framework for Their Assessment.A Hydrothermal-Sedimentary Context for the Origin of Life.Methane bursts as a trigger for intermittent lake-forming climates on post-Noachian MarsEffects of primitive photosynthesis on Earth’s early climate systemThe faint young Sun problemA bistable organic-rich atmosphere on the Neoarchaean EarthHydrogen-nitrogen greenhouse warming in Earth's early atmosphereAtmospheric science. How was early Earth kept warm?Faint young Sun problem more severe due to ice-albedo feedback and higher rotation rate of the early EarthAtmospheric hydrogen peroxide and Eoarchean iron formationsMineralogical constraints on Precambrian pCO2
P2860
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P2860
A revised, hazy methane greenhouse for the Archean Earth.
description
2008 nî lūn-bûn
@nan
2008年の論文
@ja
2008年学术文章
@wuu
2008年学术文章
@zh-cn
2008年学术文章
@zh-hans
2008年学术文章
@zh-my
2008年学术文章
@zh-sg
2008年學術文章
@yue
2008年學術文章
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2008年學術文章
@zh-hant
name
A revised, hazy methane greenhouse for the Archean Earth.
@en
A revised, hazy methane greenhouse for the Archean Earth.
@nl
type
label
A revised, hazy methane greenhouse for the Archean Earth.
@en
A revised, hazy methane greenhouse for the Archean Earth.
@nl
prefLabel
A revised, hazy methane greenhouse for the Archean Earth.
@en
A revised, hazy methane greenhouse for the Archean Earth.
@nl
P356
P1433
P1476
A revised, hazy methane greenhouse for the Archean Earth.
@en
P2093
James F Kasting
Patrick J Kasting
P304
P356
10.1089/AST.2007.0197
P407
P577
2008-12-01T00:00:00Z