Articles | Volume 13, issue 15
https://doi.org/10.5194/bg-13-4315-2016
https://doi.org/10.5194/bg-13-4315-2016
Research article
 | 
01 Aug 2016
Research article |  | 01 Aug 2016

Decadal and long-term boreal soil carbon and nitrogen sequestration rates across a variety of ecosystems

Kristen L. Manies, Jennifer W. Harden, Christopher C. Fuller, and Merritt R. Turetsky

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Cited articles

Allison, S. D., Gartner, T. B., Mack, M. C., Mcguire, K., and Treseder, K.: Nitrogen alters carbon dynamics during early succession in boreal forest, Soil Biol. Biochem., 42, 1157–1164, https://doi.org/10.1016/j.soilbio.2010.03.026, 2010.
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Aurela, M., Laurila, T., and Tuovinen, J.-P.: The timing of snow melt controls the annual CO2 balance in a subarctic fen, Geophys. Res. Lett., 31, L16119, https://doi.org/10.1029/2004GL020315, 2004.
Aurela, M., Lohila, A., Tuovinen, J. P., Hatakka, J., Riutta, T., and Laurila, T.: Carbon dioxide exchange on a northern boreal fen, Boreal Environ. Res., 14, 699–710, 2009.
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Short summary
Boreal soils are important to the global C cycle. We need to understand what controls how C accumulates and is lost from this soil. To help we examined C & N accumulation rates for five boreal ecosystems. Most ecosystems were similar. But the rich fen had higher long-term C & N accumulation rates, likely due to differences in nutrient cycling & because it burns less. Therefore, shifts among ecosystems will not change regional C & N dynamics much, unless there is a shift to or from a rich fen.
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