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Faster-and-tighter nitrogen cycle supports mature forest productivity under elevated CO2
Manon Rumeau1,2, Carolina Mayoral1,2, Fotis Sgouridis3
1Birmingham Institute of Forest Research, University of Birmingham, Birmingham B15 2TT, UK.
Elevated atmospheric carbon dioxide (CO2) boosts forest growth by increasing nitrogen (N) availability through enhanced N mineralization. This suggests forests can adapt to higher CO2 levels, but long-term N supply may be limited.
Area of Science:
- Forest Ecology
- Biogeochemical Cycles
- Climate Change Research
Background:
- Rising atmospheric carbon dioxide (CO2) concentrations are expected to increase forest carbon (C) uptake.
- Nitrogen (N) availability is often considered a limiting factor for forest productivity under elevated CO2.
- Previous studies showed significant biomass gains in a mature oak forest under Free Air CO2 Enrichment (eCO2).
Purpose of the Study:
- To investigate if changes in soil nitrogen (N) fluxes explain the observed biomass gains in an oak forest under eCO2.
- To understand the mechanisms of N cycling adaptation in forest ecosystems exposed to elevated CO2.
Main Methods:
- Conducted a 6-year Free Air CO2 Enrichment (eCO2) experiment in a mature oak forest.
- Measured in situ net and gross nitrogen (N) fluxes, including ammonification and nitrification.
- Assessed changes in fine root biomass and soil respiration in response to eCO2.
Main Results:
- Enhanced N mineralization and ecosystem N conservation were observed, supporting increased forest productivity under eCO2.
- In situ net and gross N ammonification rates increased by approximately 30%, particularly during oak budburst.
- Higher N ammonification correlated with increased fine root biomass and soil respiration, while gross nitrification decreased.
Conclusions:
- Forest nitrogen cycling can adapt to support increased carbon (C) uptake under elevated CO2 (eCO2) through enhanced N availability.
- Plant-soil interactions facilitate a faster-yet-tighter N cycle, promoting productivity.
- Long-term C uptake capacity may be limited by soil organic N stocks and reduced anthropogenic N deposition.
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