TY - JOUR
T1 - Nitrogen and phosphorus constrain the CO2 fertilization of global plant biomass
AU - Terrer, César
AU - Jackson, Robert B.
AU - Prentice, I. Colin
AU - Keenan, Trevor F.
AU - Kaiser, Christina
AU - Vicca, Sara
AU - Fisher, Joshua B.
AU - Reich, Peter B.
AU - Stocker, Benjamin D.
AU - Hungate, Bruce A.
AU - Peñuelas, Josep
AU - McCallum, Ian
AU - Soudzilovskaia, Nadejda A.
AU - Cernusak, Lucas A.
AU - Talhelm, Alan F.
AU - Van Sundert, Kevin
AU - Piao, Shilong
AU - Newton, Paul C.D.
AU - Hovenden, Mark J.
AU - Blumenthal, Dana M.
AU - Liu, Yi Y.
AU - Müller, Christoph
AU - Winter, Klaus
AU - Field, Christopher B.
AU - Viechtbauer, Wolfgang
AU - Van Lissa, Caspar J.
AU - Hoosbeek, Marcel R.
AU - Watanabe, Makoto
AU - Koike, Takayoshi
AU - Leshyk, Victor O.
AU - Polley, H. Wayne
AU - Franklin, Oskar
PY - 2019/9/1
Y1 - 2019/9/1
N2 - Elevated CO2 (eCO2) experiments provide critical information to quantify the effects of rising CO2 on vegetation1–6. Many eCO2 experiments suggest that nutrient limitations modulate the local magnitude of the eCO2 effect on plant biomass1,3,5, but the global extent of these limitations has not been empirically quantified, complicating projections of the capacity of plants to take up CO2 7,8. Here, we present a data-driven global quantification of the eCO2 effect on biomass based on 138 eCO2 experiments. The strength of CO2 fertilization is primarily driven by nitrogen (N) in ~65% of global vegetation and by phosphorus (P) in ~25% of global vegetation, with N- or P-limitation modulated by mycorrhizal association. Our approach suggests that CO2 levels expected by 2100 can potentially enhance plant biomass by 12 ± 3% above current values, equivalent to 59 ± 13 PgC. The global-scale response to eCO2 we derive from experiments is similar to past changes in greenness9 and biomass10 with rising CO2, suggesting that CO2 will continue to stimulate plant biomass in the future despite the constraining effect of soil nutrients. Our research reconciles conflicting evidence on CO2 fertilization across scales and provides an empirical estimate of the biomass sensitivity to eCO2 that may help to constrain climate projections.
AB - Elevated CO2 (eCO2) experiments provide critical information to quantify the effects of rising CO2 on vegetation1–6. Many eCO2 experiments suggest that nutrient limitations modulate the local magnitude of the eCO2 effect on plant biomass1,3,5, but the global extent of these limitations has not been empirically quantified, complicating projections of the capacity of plants to take up CO2 7,8. Here, we present a data-driven global quantification of the eCO2 effect on biomass based on 138 eCO2 experiments. The strength of CO2 fertilization is primarily driven by nitrogen (N) in ~65% of global vegetation and by phosphorus (P) in ~25% of global vegetation, with N- or P-limitation modulated by mycorrhizal association. Our approach suggests that CO2 levels expected by 2100 can potentially enhance plant biomass by 12 ± 3% above current values, equivalent to 59 ± 13 PgC. The global-scale response to eCO2 we derive from experiments is similar to past changes in greenness9 and biomass10 with rising CO2, suggesting that CO2 will continue to stimulate plant biomass in the future despite the constraining effect of soil nutrients. Our research reconciles conflicting evidence on CO2 fertilization across scales and provides an empirical estimate of the biomass sensitivity to eCO2 that may help to constrain climate projections.
UR - http://www.scopus.com/inward/record.url?scp=85070793012&partnerID=8YFLogxK
U2 - 10.1038/s41558-019-0545-2
DO - 10.1038/s41558-019-0545-2
M3 - Letter
AN - SCOPUS:85070793012
SN - 1758-678X
VL - 9
SP - 684
EP - 689
JO - Nature Climate Change
JF - Nature Climate Change
IS - 9
ER -