about
Swansong biospheres: refuges for life and novel microbial biospheres on terrestrial planets near the end of their habitable lifetimesAtmospheric pressure as a natural climate regulator for a terrestrial planet with a biospherePalaeoclimates: the first two billion yearsImplications of a 3.472-3.333 Gyr-old subaerial microbial mat from the Barberton greenstone belt, South Africa for the UV environmental conditions on the early EarthAtmospheric composition and climate on the early EarthPaleoproterozoic snowball earth: extreme climatic and geochemical global change and its biological consequencesEarly Mars Climate ModelsGeochemistry of Carbonates on Mars: Implications for Climate History and Nature of Aqueous EnvironmentsClimate change. Lessons from Earth's past.Earth's early atmosphere.Polar front shift and atmospheric CO2 during the glacial maximum of the Early Paleozoic Icehouse.Geobiological constraints on Earth system sensitivity to CO₂ during the Cretaceous and Cenozoic.The rise of oxygen in Earth's early ocean and atmosphere.TimeTree: A Resource for Timelines, Timetrees, and Divergence Times.Future climate forcing potentially without precedent in the last 420 million years.The fluvial history of Mars.The faint young Sun paradox: an observational test of an alternative solar model.The influence of UV radiation on protistan evolution.A slightly more massive young Sun as an explanation for warm temperatures on early Mars.Walking over 4 Gya: Chemical Evolution from Photochemistry to Mineral and Organic Chemistries Leading to an RNA World.Increased insolation threshold for runaway greenhouse processes on Earth-like planets.Greenhouse warming by nitrous oxide and methane in the Proterozoic Eon.Space as a Tool for Astrobiology: Review and Recommendations for Experimentations in Earth Orbit and BeyondDrainage network development in the Keanakāko‘i tephra, Kīlauea Volcano, Hawai‘i: Implications for fluvial erosion and valley network formation on early MarsOn the initiation of a snowball EarthGreenhouse warming by CH4 in the atmosphere of early EarthThe honeycomb terrain on the Hellas basin floor, Mars: A case for salt or ice diapirismThe Precambrian emergence of animal life: a geobiological perspectiveClimates of the Earth and Cryosphere EvolutionNumerical evidence for thermohaline circulation reversals during the MaastrichtianChilean high-altitude hot-spring sinters: a model system for UV screening mechanisms by early Precambrian cyanobacteriaThe relative influence of H2 O and CO2 on the primitive surface conditions and evolution of rocky planetsEffects of primitive photosynthesis on Earth’s early climate systemModeling evidences for global warming, Arctic seawater freshening, and sluggish oceanic circulation during the Early Toarcian anoxic eventA mechanism for brief glacial episodes in the Mesozoic greenhouseA GEOCLIM simulation of climatic and biogeochemical consequences of Pangea breakupCold glacial oceans would have inhibited phyllosilicate sedimentation on early MarsThe faint young Sun problemHydrogen-nitrogen greenhouse warming in Earth's early atmosphereCan a variable gravitational constant resolve the faint young Sun paradox?
P2860
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P2860
description
1981 nî lūn-bûn
@nan
1981年の論文
@ja
1981年学术文章
@wuu
1981年学术文章
@zh
1981年学术文章
@zh-cn
1981年学术文章
@zh-hans
1981年学术文章
@zh-my
1981年学术文章
@zh-sg
1981年學術文章
@yue
1981年學術文章
@zh-hant
name
Solar interior structure and luminosity variations
@en
Solar interior structure and luminosity variations
@nl
type
label
Solar interior structure and luminosity variations
@en
Solar interior structure and luminosity variations
@nl
prefLabel
Solar interior structure and luminosity variations
@en
Solar interior structure and luminosity variations
@nl
P356
P1433
P1476
Solar interior structure and luminosity variations
@en
P2093
D. O. Gough
P2888
P356
10.1007/BF00151270
P407
P577
1981-11-01T00:00:00Z