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Open Access Publications from the University of California

Sensitivity of Boreal Forest Carbon Balance to Soil Thaw

  • Author(s): Goulden, M. L.;
  • Wofsy, S.C.;
  • Harden, J.W.;
  • Trumbore, S.E.;
  • Crill, P.M.;
  • Gower, S.T.;
  • Fries, T.;
  • Daube, B.C.;
  • Bazzaz, A.;
  • Munger, J.W.
  • et al.

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.

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