Articles | Volume 19, issue 14
Biogeosciences, 19, 3381–3393, 2022
Biogeosciences, 19, 3381–3393, 2022
BG Letters
 | Highlight paper
20 Jul 2022
BG Letters  | Highlight paper | 20 Jul 2022

Soil carbon loss in warmed subarctic grasslands is rapid and restricted to topsoil

Niel Verbrigghe et al.

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Cited articles

Abramoff, R. Z., Torn, M. S., Georgiou, K., Tang, J., and Riley, W. J.: Soil Organic Matter Temperature Sensitivity Cannot Be Directly Inferred from Spatial Gradients, Global Biogeochem. Cy., 33, 761–776, 2019. a
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Bárcena, T. G., Gundersen, P., and Vesterdal, L.: Afforestation Effects on SOC in Former Cropland: Oak and Spruce Chronosequences Resampled after 13 Years, Glob. Change Biol., 20, 2938–2952, 2014. a
The authors adopted a new and attractive approach, based on the use of thermal springs appearing at different times, to study the short-term and long-term (> 50 years) effect of warming on the soil C stock under subarctic grasslands. This new approach allows to take a new look at the question of a positive feedback between temperature and soils that can amplify global warming. Indeed, most studies on this subject are based on warming experiments conducted over the short term (some years) or on questionable correlative approaches where the temperature co-varies with many other factors (e.g., study of soil C stocks along latitudinal temperature gradients). Their study challenges the current dominant view on the effect of warming on the dynamics of SOM. Indeed, results suggest that soil C losses in the subarctic grasslands studied cease after 5 years of warming. These observations corroborate those obtained in the rare ecosystem warming experiments maintained beyond 10 years. In addition, results suggest that the C stocks present in the deep soil horizons, where plant roots are not or hardly present, are not affected by warming. These unexpected discoveries, together with other recent observations, show the glaring lack of knowledge on the fundamental mechanisms of the effect of temperature on catalytic processes, which seriously compromises our ability to predict the soil-climate feedback.
Short summary
In subarctic grassland on a geothermal warming gradient, we found large reductions in topsoil carbon stocks, with carbon stocks linearly declining with warming intensity. Most importantly, however, we observed that soil carbon stocks stabilised within 5 years of warming and remained unaffected by warming thereafter, even after > 50 years of warming. Moreover, in contrast to the large topsoil carbon losses, subsoil carbon stocks remained unaffected after > 50 years of soil warming.
Final-revised paper