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Dynamics of Soil Carbon During Deglaciation of the Laurentide Ice Sheet
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Dynamics of Soil Carbon During Deglaciation of the Laurentide Ice Sheet
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Journal Article
Dynamics of Soil Carbon During Deglaciation of the Laurentide Ice Sheet
1992
Overview
Deglaciation of the Laurentide Ice Sheet in North America was accompanied by sequestration of organic carbon in newly exposed soils. The greatest rate of land exposure occurred around 12,000 to 8,000 years ago, and the greatest increase in the rate of carbon sequestration by soils occurred from 8,000 to 4,000 years ago. Sequestration of carbon in deglaciated peat lands continues today, and a steady state has not been reached. The natural rate of carbon sequestration in soils, however, is small relative to the rate of anthropogenic carbon dioxide production.
Publisher
American Society for the Advancement of Science,American Association for the Advancement of Science
