Greater ecosystem carbon in the Mojave Desert after ten years exposure to elevated CO2

Abstract

The response of terrestrial ecosystems to climate change remains a large source of uncertainty in the global carbon budget. Now results from a ten-year ecological manipulation experiment in the Mojave Desert provide direct evidence that CO2 fertilization can substantially increase ecosystem carbon storage in arid ecosystems. Carbon dioxide is the main greenhouse gas inducing climate change. Increased global CO2 emissions, estimated at 8.4 Pg C yr−1 at present, have accelerated from 1% yr−1 during 1990–1999 to 2.5% yr−1 during 2000–2009 (ref. 1). The carbon balance of terrestrial ecosystems is the greatest unknown in the global C budget because the actual magnitude, location and causes of terrestrial sinks are uncertain2; estimates of terrestrial C uptake, therefore, are often based on the residuals between direct measurements of the atmospheric sink and well-constrained models of ocean uptake of CO2 (ref. 3). Here we report significant terrestrial C accumulation caused by CO2 enhancement to net ecosystem productivity in an intact, undisturbed arid ecosystem4,5,6,7,8 following ten years of exposure to elevated atmospheric CO2. Results provide direct evidence that CO2 fertilization substantially increases ecosystem C storage and that arid ecosystems are significant, previously unrecognized, sinks for atmospheric CO2 that must be accounted for in efforts to constrain terrestrial and global C cycles.

Cite this article

Evans, R., Koyama, A., Sonderegger, D. et al. Greater ecosystem carbon in the Mojave Desert after ten years exposure to elevated CO₂. Nature Clim Change 4, 394–397 (2014). https://doi.org/10.1038/nclimate2184

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