Feedbacks between plant N demand and rhizosphere priming depend on type of mycorrhizal association |
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| Authors: | Benjamin N. Sulman Edward R. Brzostek Chiara Medici Elena Shevliakova Duncan N. L. Menge Richard P. Phillips |
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| Affiliation: | 1. Program in Atmospheric and Oceanic Sciences, Department of Geosciences, Princeton University, Princeton, New Jersey, USA;2. Department of Biology, West Virginia University, Morgantown, WV, USA;3. Princeton Environmental Institute, Princeton University, Princeton, NJ, USA;4. NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ, USA;5. Department of Ecology, Evolution and Environmental Biology, Columbia University, New York, NY, USA;6. Department of Biology, Indiana University, Bloomington, IN, USA |
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| Abstract: | Ecosystem carbon (C) balance is hypothesised to be sensitive to the mycorrhizal strategies that plants use to acquire nutrients. To test this idea, we coupled an optimality‐based plant nitrogen (N) acquisition model with a microbe‐focused soil organic matter (SOM) model. The model accurately predicted rhizosphere processes and C–N dynamics across a gradient of stands varying in their relative abundance of arbuscular mycorrhizal (AM) and ectomycorrhizal (ECM) trees. When mycorrhizal dominance was switched – ECM trees dominating plots previously occupied by AM trees, and vice versa – legacy effects were apparent, with consequences for both C and N stocks in soil. Under elevated productivity, ECM trees enhanced decomposition more than AM trees via microbial priming of unprotected SOM. Collectively, our results show that ecosystem responses to global change may hinge on the balance between rhizosphere priming and SOM protection, and highlight the importance of dynamically linking plants and microbes in terrestrial biosphere models. |
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| Keywords: | Biogeochemical model biogeochemistry carbon cycling forest productivity mycorrhizae N‐cycle feedbacks plant‐soil interactions soil carbon |
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