11 Apr 2022
11 Apr 2022

Effects of climate and forest composition on soil carbon cycling, soil organic matter stability and stocks in a humid boreal region

David Paré, Jérôme Laganière, Guy R. Larocque, and Robert Boutin David Paré et al.
  • Natural Resources Canada, Canadian Forest Service, Laurentian Forestry Centre, 1055 du P.E.P.S., P.O. Box 10380, Stn. Ste-Foy, Quebec, QC G1V 4C7, Canada

Abstract. The maintenance of the large soil organic carbon (SOC) stocks of the boreal forest under climate change is a matter of concern. In this study, major soil carbon pools and fluxes were assessed in twenty-two closed-canopy forests located along an elevation and latitudinal climatic gradient expanding 4 °C in mean annual temperature (MAT) for two important boreal conifer forest stand types: balsam fir (Abies balsamea) a fire avoider and black spruce (Picea mariana) a fire-tolerant species. SOC stocks were not influenced by climate or forest type. However, carbon fluxes, including aboveground litterfall rates as well as total soil respiration (Rs), heterotrophic (Rh) and autotrophic soil respiration (Ra) were linearly related to climate (cumulative degree days >5 °C). The sensitivity of SOM degradation to temperature, assessed by comparing Q10 (rate of change for a T increase of 10 °C) of soil respiration and Rs10 (soil respiration rates corrected to 10 °C) did not vary across the climate gradient, while the proportion of labile carbon and nitrogen showed higher values for balsam fir and for warmer sites. Balsam fir forests showed a greater litterfall rate, a better litter quality (lower C:N ratio) as well as a higher Rs10 than black spruce ones, suggesting that their soils cycle a larger amount of C and N under a similar climate regime. Altogether, these results suggest that a warmer climate and balsam fir forest composition induce a more rapid SOC turnover. Contrary to common soil organic matter stabilization hypotheses, greater SOC cycling rates did not lead to higher total SOC stocks nor to the depletion of labile soil C and N. Positive effects of warming both on fluxes to and from the soil as well as a potential saturation of stabilised SOC could explain these results which apply to the context of this study: a cold and wet environment and a stable vegetation composition along the climate gradient.

David Paré et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-136', Anonymous Referee #1, 18 May 2022
    • AC1: 'Reply on RC1', David Paré, 13 Jun 2022
    • AC3: 'Reply on RC1', David Paré, 13 Jun 2022
  • RC2: 'Comment on egusphere-2022-136', Anonymous Referee #2, 29 May 2022
    • AC2: 'Reply on RC2', David Paré, 13 Jun 2022

David Paré et al.


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Short summary
Major soil carbon pools and fluxes were assessed along a climatic gradient expanding 4 °C in (MAT) for two important boreal conifer forest stand types; Species and climate affected soil organic matter (SOM) cycling but not stocks. Contrarily to common hypotheses, SOM lability was not reduced by warmer climatic conditions and perhaps increased. Results apply to cold and wet conditions and a stable vegetation composition along the climate gradient.