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Plant stoichiometric responses to elevated CO(2) vary with nitrogen and phosphorus inputs: Evidence from a global-scale meta-analysis
Rising levels of atmospheric CO(2) have been implicated in changes in the nitrogen (N) and phosphorus (P) content of terrestrial vegetation; however, questions remain over the role of C, N and P interactions in driving plant nutrient stoichiometry, particularly whether N and P additions alter vegeta...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2015
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4677399/ https://www.ncbi.nlm.nih.gov/pubmed/26656752 http://dx.doi.org/10.1038/srep18225 |
Sumario: | Rising levels of atmospheric CO(2) have been implicated in changes in the nitrogen (N) and phosphorus (P) content of terrestrial vegetation; however, questions remain over the role of C, N and P interactions in driving plant nutrient stoichiometry, particularly whether N and P additions alter vegetation responses to CO(2) enrichment singly. Here we use meta-analysis of 46 published studies to investigate the response of plant N and P to elevated CO(2) alone and in combination with nutrient (N and P) additions across temperate vs. tropical biomes. Elevated CO(2) reduces plant N concentrations more than plant P concentrations in total biomass pools, resulting in a significant decline in vegetation N/P. However, elevated CO(2) treatments in combination with N additions increase plant P concentrations, whereas P additions have no statistical effect on plant N concentrations under CO(2) enrichment. These results point to compensatory but asymmetrical interactions between N, P and CO(2); that changes in N rapidly alter the availability of P, but not the converse, in response to increased CO(2). Our finding implies widespread N limitation with increasing atmospheric CO(2) concentrations alone. We also suggest that increased anthropogenic N deposition inputs could enhance plant N and P in a progressively CO(2)-enriched biosphere. |
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