A gradient of nutrient enrichment reveals nonlinear impacts of fertilization on Arctic plant diversity and ecosystem function

dc.contributor.author Prager, Case M.
dc.contributor.author Naeem, Shahid
dc.contributor.author Boelman, Natalie
dc.contributor.author Eitel, Jan U. H.
dc.contributor.author Greaves, Heather
dc.contributor.author Heskel, Mary
dc.contributor.author Magney, Troy
dc.contributor.author Menge, Duncan N. L.
dc.contributor.author Vierling, Lee
dc.contributor.author Griffin, Kevin L.
dc.date.accessioned 2017-05-24T18:25:06Z
dc.date.available 2017-05-24T18:25:06Z
dc.date.issued 2017-03-22
dc.description © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Ecology and Evolution 7 (2017): 2449–2460, doi:10.1002/ece3.2863. en_US
dc.description.abstract Rapid environmental change at high latitudes is predicted to greatly alter the diversity, structure, and function of plant communities, resulting in changes in the pools and fluxes of nutrients. In Arctic tundra, increased nitrogen (N) and phosphorus (P) availability accompanying warming is known to impact plant diversity and ecosystem function; however, to date, most studies examining Arctic nutrient enrichment focus on the impact of relatively large (>25x estimated naturally occurring N enrichment) doses of nutrients on plant community composition and net primary productivity. To understand the impacts of Arctic nutrient enrichment, we examined plant community composition and the capacity for ecosystem function (net ecosystem exchange, ecosystem respiration, and gross primary production) across a gradient of experimental N and P addition expected to more closely approximate warming-induced fertilization. In addition, we compared our measured ecosystem CO2 flux data to a widely used Arctic ecosystem exchange model to investigate the ability to predict the capacity for CO2 exchange with nutrient addition. We observed declines in abundance-weighted plant diversity at low levels of nutrient enrichment, but species richness and the capacity for ecosystem carbon uptake did not change until the highest level of fertilization. When we compared our measured data to the model, we found that the model explained roughly 30%–50% of the variance in the observed data, depending on the flux variable, and the relationship weakened at high levels of enrichment. Our results suggest that while a relatively small amount of nutrient enrichment impacts plant diversity, only relatively large levels of fertilization—over an order of magnitude or more than warming-induced rates—significantly alter the capacity for tundra CO2 exchange. Overall, our findings highlight the value of measuring and modeling the impacts of a nutrient enrichment gradient, as warming-related nutrient availability may impact ecosystems differently than single-level fertilization experiments. en_US
dc.description.sponsorship NASA Terrestrial Ecology Grant Number: NNX12AK83G; National Science Foundation Division of Graduate Education Grant Number: DGE-11-44155 en_US
dc.identifier.citation Ecology and Evolution 7 (2017): 2449–2460 en_US
dc.identifier.doi 10.1002/ece3.2863
dc.identifier.uri https://hdl.handle.net/1912/9000
dc.language.iso en_US en_US
dc.publisher John Wiley & Sons en_US
dc.relation.uri https://doi.org/10.1002/ece3.2863
dc.rights Attribution 4.0 International *
dc.rights.uri http://creativecommons.org/licenses/by/4.0/ *
dc.subject Arctic en_US
dc.subject Climate change en_US
dc.subject Ecosystem function en_US
dc.subject Ecosystem respiration en_US
dc.subject Gross primary productivity en_US
dc.subject Net ecosystem en_US
dc.subject CO2 exchange en_US
dc.subject Plant diversity en_US
dc.title A gradient of nutrient enrichment reveals nonlinear impacts of fertilization on Arctic plant diversity and ecosystem function en_US
dc.type Article en_US
dspace.entity.type Publication
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