Increasing CO<sub>2</sub> levels fertilize C<sub>4</sub> grass production.
meta_analysis · Level I
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- Record sourced from PubMed, PMID 42618790.
- Also identified by DOI 10.1038/s41586-026-10935-4.
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Abstract
Rising atmospheric CO<sub>2</sub> concentrations are impacting the global terrestrial biosphere through indirect climate effects and direct effects on plant performance<sup>1-3</sup>. In tropical forests, long-term monitoring indicates a substantial CO<sub>2</sub>-driven carbon sink<sup>4</sup>. C<sub>4</sub>-grass-dominated tropical and subtropical savannas contribute approximately 30% of terrestrial net primary production<sup>5</sup>, and yet equivalent long-term analyses of CO<sub>2</sub> responses are lacking. Here we show a clear and consistent result across a meta-analysis of 70 CO<sub>2</sub>-addition experiments and 32 years of in situ field observations from southern Africa: CO<sub>2</sub> fertilization of wild C<sub>4</sub> grasses is widespread in dry conditions. In experiments, grasses reduced stomatal conductance under higher levels of CO<sub>2</sub>, limiting water loss while increasing carbon gain. In the field, improved water use efficiency translated into increased C<sub>4</sub> grass biomass production across three decades of observations. Finally, simulations via the Community Land Model<sup>6</sup> suggest that CO<sub>2</sub> fertilization of C<sub>4</sub> grass aboveground productivity may continue to increase under future conditions. Together, these results challenge the view that C<sub>4</sub> grasses are unresponsive to increasing levels of CO<sub>2</sub>, demonstrating instead that annual aboveground production of grasses in the field in southern Africa has increased by 28% over three decades (a CO<sub>2</sub>-driven increase of 75.1 g m<sup>-2</sup> (95% confidence interval of 74.5-75.8 g m<sup>-2</sup>) or 0.37 tons C ha<sup>-1</sup> of annual production). Although the fate of this carbon is uncertain (depending on feedbacks with fire, herbivory and woody vegetation), effects on the global carbon cycle may be profound.