NOAA/WDS Paleoclimatology - Pappas - Southern Old Black Spruce - PCMA - ITRDB CANA610

The boreal biome accounts for approximately one third of the terrestrial carbon (C) sink. However, estimates of its individual C pools remain uncertain. Here, focusing on the southern boreal forest, we quantified the magnitude and temporal dynamics of C allocation to aboveground tree growth at a mature black spruce (Picea mariana)-dominated forest stand in Saskatchewan, Canada. We reconstructed aboveground tree biomass increments (AGBi) using a biometric approach, i.e., species-specific allometry combined with forest stand characteristics and tree ring widths collected with a C-oriented sampling design. We explored the links between boreal tree growth and ecosystem C input by comparing AGBi with eddy-covariance-derived ecosystem C fluxes from 1999 to 2015 and we synthesized our findings with a refined meta-analysis of published values of boreal forest C use efficiency (CUE). Mean AGBi at the study site was decoupled from ecosystem C input and equal to 71 +/- 7 g C m-2 (1999-2015), which is only a minor fraction of gross ecosystem production (GEP; i.e., AGBi / GEP ~= 9 %). Moreover, C allocation to AGBi remained stable over time (AGBi / GEP; -0.0001 yr-1; p-value=0.775), contrary to significant trends in GEP (+5.72 g C m-2 yr-2; p-value=0.02) and CUE (-0.0041 yr-1, p-value=0.007). CUE was estimated as 0.50 +/- 0.03 at the study area and 0.41 +/- 0.12 across the reviewed boreal forests. These findings highlight the importance of belowground tree C investments, together with the substantial contribution of understory, ground cover and soil to the boreal forest C balance. Our quantitative insights into the dynamics of aboveground boreal tree C allocation offer additional observational constraints for terrestrial ecosystem models that are often biased in converting C input to biomass, and can guide forest-management strategies for mitigating carbon dioxide emissions.