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• W2114992792 startingPage "214" @default.
• W2114992792 abstract "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 −1 year −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." @default.
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• W2114992792 date "1998-01-09" @default.
• W2114992792 modified "2023-10-02" @default.
• W2114992792 title "Sensitivity of Boreal Forest Carbon Balance to Soil Thaw" @default.
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• W2114992792 doi "https://doi.org/10.1126/science.279.5348.214" @default.
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