Title : Climatic consequences of very high carbon dioxide levels in the earth's early atmosphere.

Pub. Date : 1986 Dec 12

PMID : 11539665






1 Functional Relationships(s)
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1 A 10- to 20-bar carbon dioxide atmosphere, such as may have existed during the first several hundred million years of the earth"s history, would have had a surface temperature of approximately 85 degrees to 110 degrees C. The early stratosphere should have been dry, thereby precluding the possibility of an oxygenic prebiotic atmosphere caused by photodissociation of water vapor followed by escape of hydrogen to space. Hydrogen immunoglobulin kappa variable 6D-21 (non-functional) Homo sapiens