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1 NASA Ames Research Center
Moffett Field CA 94035-1000, USA
E-mail:
Kevin.J.Zahnle{at}nasa.gov
The aftermath of the Moon-forming impact left Earth with a hot,
CO2-rich steam atmosphere. Water oceans condensed from the steam
after 2 Myr, but for some 10-100 Myr the surface stayed warm (
500K), the
length of time depending on how quickly the CO2 was removed into
the mantle. Thereafter a lifeless Earth, heated only by the dim light of the
young Sun, would have evolved into a bitterly cold ice world. The cooling
trend was frequently interrupted by volcanic- or impact-induced thaws.
KEYWORDS: Hadean Earth, Moon-forming impact, origin, evolution of the atmosphere, zircon
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