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Paleosols and weathering leading up to Snowball Earth in central Australia
Australian Journal of Earth Sciences, 2021Gregory Retallack
exaly
Thin Ice on the Snowball Earth
2013Global ice-covered conditions during a Neoproterozoic snowball Earth seem inconsistent with the survival of eukaryotic algae. The presence of thin ice in the tropics remains a viable alternative to resolve this paradox. The simple method of McKay [2000] for computing ice thickness has been improved by considering separately a short wavelength interval (
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Abstract Because of its high albedo, the Snowball Earth seemed inescapably frozen. However, volcanism progressively delivered CO2 in the atmosphere. The ice-covered lands could not provide a CO2 sink by atmospheric weathering. Therefore, the atmospheric CO2 content increased until a threshold when the extreme greenhouse effect resulted ...
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How Should Snowball Earth Deglaciation Start
Journal of Geophysical Research D: Atmospheres, 2021Yonggang Liu +2 more
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Robust elements of Snowball Earth atmospheric circulation and oases for life
Journal of Geophysical Research D: Atmospheres, 2013Mark D Branson, Dorian Abbot
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Neoproterozoic “snowball Earth”: Dynamic sea ice over a quiescent ocean
Paleoceanography, 2003Andrew Weaver, M Eby
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