Microbial competition for phosphorus limits the CO2 response of a mature forest
Mingkai Jiang, Kristine Y. Crous, Yolima Carrillo, Catriona A. Macdonald, Ian C. Anderson, Matthias M. Boer, Mark Farrell, Andrew N. Gherlenda, Laura Castañeda‐Gómez, Shun Hasegawa, Klaus Jarosch, Paul J. Milham, Raúl Ochoa‐Hueso, Varsha S. Pathare, Johanna Pihlblad, J. Piñeiro, Jeff R. Powell, Sally A. Power, Peter B. Reich, Markus Riegler, Sönke Zaehle, Benjamin Smith, Belinda E. Medlyn, David S. Ellsworth
Abstract
Abstract The capacity for terrestrial ecosystems to sequester additional carbon (C) with rising CO 2 concentrations depends on soil nutrient availability 1,2 . Previous evidence suggested that mature forests growing on phosphorus (P)-deprived soils had limited capacity to sequester extra biomass under elevated CO 2 (refs. 3–6 ), but uncertainty about ecosystem P cycling and its CO 2 response represents a crucial bottleneck for mechanistic prediction of the land C sink under climate change 7 . Here, by compiling the first comprehensive P budget for a P-limited mature forest exposed to elevated CO 2 , we show a high likelihood that P captured by soil microorganisms constrains ecosystem P recycling and availability for plant uptake. Trees used P efficiently, but microbial pre-emption of mineralized soil P seemed to limit the capacity of trees for increased P uptake and assimilation under elevated CO 2 and, therefore, their capacity to sequester extra C. Plant strategies to stimulate microbial P cycling and plant P uptake, such as increasing rhizosphere C release to soil, will probably be necessary for P-limited forests to increase C capture into new biomass. Our results identify the key mechanisms by which P availability limits CO 2 fertilization of tree growth and will guide the development of Earth system models to predict future long-term C storage.