Increasing temperatures are expected to increase decomposition rates in soils, potentially reducing ecosystem carbon storage. Research now indicates that — in a tropical montane forest — soil carbon stocks are unaffected by higher temperatures despite substantially increased rates of CO2 release from the soil.
References
Giardina, C. P., Litton, C. M., Crow, S. E. & Asner, G. P. Nature Clim. Change 4, 822–827 (2014).
Schmidt, M. et al. Nature 478, 49–56 (2011).
Torn, M. et al. Nature 389, 170–173 (1997).
Luo, Y., Hui, D. & Zhang, D. Ecology 87, 53–63 (2006).
Hassink, J. Plant Soil 191, 77–87 (1997).
Wiesmeier, M. et al. Glob. Change Biol. 20, 653–665 (2014).
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Hartley, I. Resisting climate change. Nature Clim Change 4, 760–761 (2014). https://doi.org/10.1038/nclimate2356
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DOI: https://doi.org/10.1038/nclimate2356
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