From: Smigrodzki, Rafal (SmigrodzkiR@msx.upmc.edu)
Date: Fri Apr 12 2002 - 21:30:15 MDT
Samantha Atkins [mailto:samantha@objectent.com]
Also, we are talking potential thermal run-away here, not simply
changes to coastline.
### This appears to be extremely unlikely - in the Cretaceous the
concentration of CO2 was more than ten times as high as it is now, with no
run-away (although the lower luminosity of the Sun at that time might have
been a mitigating factor).
Rafal
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