Sensitivity of Boreal Forest Carbon Balance to Soil Thaw

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Science  09 Jan 1998:
Vol. 279, Issue 5348, pp. 214-217
DOI: 10.1126/science.279.5348.214

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We used eddy covariance; gas-exchange chambers; radiocarbon analysis; wood, moss, and soil inventories; and laboratory incubations to measure the carbon balance of a 120-year-old black spruce forest in Manitoba, Canada. The site lost 0.3 ± 0.5 metric ton of carbon per hectare per year (ton C ha−1 year−1) from 1994 to 1997, with a gain of 0.6 ± 0.2 ton C ha−1year−1 in moss and wood offset by a loss of 0.8 ± 0.5 ton C ha−1 year−1 from the soil. The soil remained frozen most of the year, and the decomposition of organic matter in the soil increased 10-fold upon thawing. The stability of the soil carbon pool (∼150 tons C ha−1) appears sensitive to the depth and duration of thaw, and climatic changes that promote thaw are likely to cause a net efflux of carbon dioxide from the site.

  • * Present address: Department of Earth System Science, University of California, Irvine, CA 92697, USA.

  • To whom correspondence should be addressed. E-mail: mgoulden{at}

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