4.5 Article

A plant-microbe interaction framework explaining nutrient effects on primary production

Journal

NATURE ECOLOGY & EVOLUTION
Volume 2, Issue 10, Pages 1588-1596

Publisher

NATURE RESEARCH
DOI: 10.1038/s41559-018-0662-8

Keywords

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Funding

  1. International Program CryoCARB [MSM 7E10073-CryoCARB]
  2. Austrian Science Fund (FWF) [I370-B17]
  3. German Federal Ministry of Education and Research [03F0616A]
  4. MEYS CZ grants [LM2015075, EF16 013/0001782]
  5. Swedish Research Councils [2015-468, 2016-04146]
  6. Bolin Centre for Climate Research
  7. Czech Science Foundation [16-18453S]
  8. project COUP
  9. Swedish Research Council [E0689701]
  10. Academy of Finland [132045]
  11. U.S. Department of Energy (DOE) Office of Science, Biological and Environmental Research (BER)
  12. [GA17-15229S]
  13. Academy of Finland (AKA) [132045, 132045] Funding Source: Academy of Finland (AKA)
  14. Swedish Research Council [2016-04146] Funding Source: Swedish Research Council

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In most terrestrial ecosystems, plant growth is limited by nitrogen and phosphorus. Adding either nutrient to soil usually affects primary production, but their effects can be positive or negative. Here we provide a general stoichiometric framework for interpreting these contrasting effects. First, we identify nitrogen and phosphorus limitations on plants and soil microorganisms using their respective nitrogen to phosphorus critical ratios. Second, we use these ratios to show how soil microorganisms mediate the response of primary production to limiting and non-limiting nutrient addition along a wide gradient of soil nutrient availability. Using a meta-analysis of 51 factorial nitrogen-phosphorus fertilization experiments conducted across multiple ecosystems, we demonstrate that the response of primary production to nitrogen and phosphorus additions is accurately predicted by our stoichiometric framework. The only pattern that could not be predicted by our original framework suggests that nitrogen has not only a structural function in growing organisms, but also a key role in promoting plant and microbial nutrient acquisition. We conclude that this stoichiometric framework offers the most parsimonious way to interpret contrasting and, until now, unresolved responses of primary production to nutrient addition in terrestrial ecosystems.

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