News Release

Use of carbon dioxide as fertilizer in tropical forests limited by phosphorus availability

Peer-Reviewed Publication

KeAi Communications Co., Ltd.

Structure of C–N–P cycles in DLEM-CNP and interactions with P uptake, available P, precipitation, temperature, and CO₂.

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Structure of C–N–P cycles in DLEM-CNP and interactions with P uptake, available P, precipitation, temperature, and CO2

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Credit: Zhuonan Wang,et al.

Tropical forests store approximately 72% of the global forest biomass carbon and contribute about one-third of the global net primary productivity (NPP). The carbon dioxide (CO2) fertilization effect, which enhances CO2 concentrations in leaves and boosts plants’ carbon fixation capacity, is a key mechanism for maintaining and increasing tropical forest productivity. However, the future of this fertilization effect is uncertain partly due to nutrient limitations.

In a study published in the KeAi journal Forest Ecosystems, researchers from the United States, Japan and China present a new carbon-nitrogen-phosphorus coupled biogeochemical model known as the “Dynamic Land Ecosystem Model (DLEM-CNP)”. It examines how phosphorus (P) limitation affects carbon fluxes in tropical forests.

"Tropical forests are vital carbon reservoirs, and their capacity could increase with more CO2," shares the study's lead author Zhuonan Wang, who is a postdoctoral researcher at the Natural Resource Ecology Laboratory, Colorado State University. "Our model simulates biogeochemical processes in tropical forests. It represents the interactive co-limitation of nitrogen and phosphorus on vegetation carbon fixation. Notably, the model allows us to explore how different factors impact the CO2 fertilization effect in these forests."

The multidisciplinary team found that phosphorus limitation reduced the productivity responses of tropical forests to rising atmospheric CO2 concentrations, and the combined nitrogen and phosphorus limitations diminished CO2 fertilization effect on gross primary production, net primary productivity and net ecosystem production by 45%, 46%, and 41%, respectively.

“Nevertheless, while CO2 fertilization had a significant positive impact on GPP and NPP, deforestation was the main factor contributing to reductions in these metrics,” explains Wang. “Our factorial experiment revealed that deforestation offset the CO2 fertilization effect on NPP by 135% from the 1860s to the 2010s.”

The finding represents a major advancement in terrestrial biosphere modeling. “Our novel approach highlights how increasing phosphorus limitation and deforestation reduce the carbon sink potential of tropical forests, emphasizing the critical role of phosphorus in the carbon cycle. We hope our results encourage further exploration of carbon-nitrogen-phosphorus models in understanding the global carbon cycle,” adds Wang.

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Contact the author: Zhuonan Wang; Natural Resource Ecology Laboratory Colorado State University; zhuonan.wang@colostate.edu

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