Abstract Anthropogenic elevated atmospheric carbon dioxide (eCO 2 ) increases carbon (C) availability to plants. Whether ecosystems store or release this additional C depends on the balance between net primary production (NPP) and soil respiration, where eCO 2 -stimulated NPP can be constrained by the provisioning of nutrients by microbial decomposers. Ecosystems gradually become more phosphorus (P)-limited as weathering of primary minerals and occlusion of available phosphate increase with age, making plant-microbial competition for P a potential key driver of the fate of C in mature ecosystems under eCO 2 . In a P-limited mature forest (EucFACE, Australia), we found that soil microbial growth was primarily limited by C, but that P was the secondary limiting resource. This suggests that increased plant-derived C inputs under eCO 2 could relieve microbial C limitation and intensify microbial demand for P. Surprisingly, a decade of eCO 2 instead exacerbated microbial C limitation. We posit that a fast growing copiotrophic decomposer community under eCO 2 required more C. This shift also resulted in exacerbated microbial P limitation under eCO 2 . These together primed microbial use of fresh litter inputs, truncating the ecosystem P cycle, and explaining the observed faster turnover of organic matter and more intense competition for P between microbes and plants under eCO 2 .
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Yuan et al. (Mon,) studied this question.
www.synapsesocial.com/papers/69ba427c4e9516ffd37a2c68 — DOI: https://doi.org/10.1038/s43247-026-03365-7
Mingyue Yuan
Catriona A. Macdonald
Lettice C. Hicks
Communications Earth & Environment
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