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DOI10.1126/science.281.5381.1342
A neoproterozoic snowball earth
Hoffman P.F.; Kaufman A.J.; Halverson G.P.; Schrag D.P.
发表日期1998
ISSN0036-8075
起始页码1342
结束页码1346
卷号281期号:5381
英文摘要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.
英文关键词calcium carbonate; carbon dioxide; surface water; carbonate rock; glaciation; paleoclimate; primary production; article; geology; greenhouse effect; metazoon; priority journal; rock; sea; Metazoa
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/244036
作者单位Dept. of Earth and Planet. Sciences, Harvard University, Cambridge, MA 02138, United States; Department of Geology, University of Maryland, College Park, MD 20742, United States
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Hoffman P.F.,Kaufman A.J.,Halverson G.P.,et al. A neoproterozoic snowball earth[J],1998,281(5381).
APA Hoffman P.F.,Kaufman A.J.,Halverson G.P.,&Schrag D.P..(1998).A neoproterozoic snowball earth.Science,281(5381).
MLA Hoffman P.F.,et al."A neoproterozoic snowball earth".Science 281.5381(1998).
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