oxidants on small icy bodies and snowball earth yuk l. yung (caltech) mao-chang liang (academia...
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Oxidants on Small Icy Bodies and Snowball Earth
Yuk L. Yung (Caltech)
Mao-Chang Liang
(Academia Sinica)
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Initiation of Snowball
Hoffman, 2000
Paleoclimate Dim Sun Greenhouse by CH4 (Kasting et al.) Loss of CH4: Oxidized by O2 produced by oxygen-synthet
ic bacteria
ice
albedo(reflectance)
Runaway ice-house
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Atmospheric Photochemistry during Snowball?
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Atmosphere of Snowball
Oxygen poor Cold
Surface temperature -40 C Low water vapor abundance Weak hydrological cycles (~1 mm/yr)
100 Myr to get rid of the Snowball, by assuming present CO2 outgassing rate
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Photochemical Calculation One-dimensional calculation
Continuity of mass ni/t + i/z = Pi Li
Close to present-day vertical mixing profile Temperature profiles
Surface temperature of 210, 240, 273 K Lapse rate of 6.5 and 10 K km-1
Deposition rate of ~109 molecules cm-2 s-1 for H2O2
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Principal Results
O3
H2O
H2O2
O2
H2CO
CO2
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H2O2
ice
H2O2
H2O2
H2O2H2O2
H2OHO2
HO2 H2O2
OH
H2O2
H2O2 H2O2
H2O2
H2O2H2O2
1 km
diffusion
Schematic Diagram
h (<200 nm)
h (<350 nm)
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Result Summary
High ratio of H2O2 and H2O
~1019 mole of H2O2 could be deposited ~0.1 bar of O2
Decomposition of H2O2
Release O2 into the atmosphere
Global oxidation on the planetary surface
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Evidence of the Rise of Oxygen/Oxidants
Farquhar et al. (2000) Mass-independent of sulfur isotopes
Karhu, J. A. & Holland (1996) 13C anomaly
Kirschvink et al. (2000) Large deposition of MnO2
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Farquhar et al., (2000)
SO2 + h → SO + O
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Karhu & Holland, 1996Karhu & Holland, 1996
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Kirschvink et al., 2000Kirschvink et al., 2000
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Impact on the Evolution of Life?
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Biological Evolution Associated with Snowball
Paleoproterozic (~2.4 Ga) global oxidation event first clear fossil of eukaryotic cell (Han & Runega
r, 1992) Neoproterozic (~0.7 Ga)
multi-cellular life Cambrian explosion
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Ages in Millions of Years
Oldest Stromatolite and Prokaryote Body Fossil
Oldest Eukaryote Body FossilIntroduction of OxygenSnowball Earth (Paleoproterozoic)
Cambrian ExplosionSnowball Earth (two?) (Precambrian)
3500
3000
2000
1000
Archaean
Proterozoic
CenozoicMesozoic
Paleozoic
Courtesy of Hyman Hartman
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Role of H2O2
Touati, 2000