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Link to original content: http://www.ncbi.nlm.nih.gov/pubmed/9721097
A neoproterozoic snowball earth - PubMed Skip to main page content
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. 1998 Aug 28;281(5381):1342-6.
doi: 10.1126/science.281.5381.1342.

A neoproterozoic snowball earth

PF Hoffman  1 , AJ Kaufman, GP Halverson, DP Schrag
Affiliations

A neoproterozoic snowball earth

PF Hoffman et al. Science. .

Abstract

Negative carbon isotope anomalies in carbonate rocks bracketing Neoproterozoic glacial deposits in Namibia, combined with estimates of thermal subsidence history, suggest that biological productivity in the surface ocean collapsed for millions of years. This collapse can be explained by a global glaciation (that is, a snowball Earth), which ended abruptly when subaerial volcanic outgassing raised atmospheric carbon dioxide to about 350 times the modern level. The rapid termination would have resulted in a warming of the snowball Earth to extreme greenhouse conditions. The transfer of atmospheric carbon dioxide to the ocean would result in the rapid precipitation of calcium carbonate in warm surface waters, producing the cap carbonate rocks observed globally.

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