4.6 Article

Increases in the dominance of species with higher N:P flexibility exacerbate community N-P imbalances following N inputs

Journal

BIOGEOCHEMISTRY
Volume 163, Issue 3, Pages 279-288

Publisher

SPRINGER
DOI: 10.1007/s10533-023-01033-y

Keywords

Community composition; Nitrogen addition; Nutrient imbalance; Stoichiometric homeostasis; Stoichiometric flexibility; Temperate steppe

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Increasing atmospheric nitrogen deposition leads to ecosystem N-P imbalances, which alters plant N:P ratios and has important consequences on ecosystem services. A field experiment in a temperate semiarid grassland showed that changes in species composition have a more sensitive effect on community-level plant N:P ratio than arithmetic means of different species. This exacerbation of plant N-P imbalances is caused by the dominance of two species with higher N:P stoichiometry flexibility stimulated by N inputs.
Increasing atmospheric nitrogen (N) deposition leads to ecosystem N-P imbalances worldwide, with important consequences on ecosystem services by altering plant N:P ratios. While the direct and positive effects of N inputs on plant N:P ratio at the species level is well established, it remains unclear how the N-induced changes in species composition contribute to the community-level alterations of N:P ratio, which are more closely related with ecosystem properties and functioning. Based on a field experiment with six N addition levels ranging from 0 to 50 g N m(-2) yr(-1) in a temperate semiarid grassland, we report more sensitive responses of community-level plant N:P ratio when considering changes in species composition than the expectation based only on arithmetic means of different species. Such exacerbation of plant N-P imbalances was caused by the fact that N inputs stimulated the dominance of two species with higher N:P stoichiometry flexibility. By linking species-specific variation of stoichiometry flexibility and the changes in species dominance with community-level variations of N:P ratio, our results uncover a new mechanism underlying the N-induced N-P imbalances in plant communities, which should be considered in biogeochemical modeling.

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