Abstract

Abstract Plant–soil feedbacks regulate plant productivity and diversity, but potential mechanisms underpinning such feedbacks, such as the allocation of recent plant assimilate, remain largely untested especially for plants forming tripartite symbioses. We tested how soils from under alder Alnus glutinosa and beneath other species of the same and different families affected alder growth and nutrition, and colonization of roots by nitrogen‐fixing Frankia bacteria and ectomycorrhizal fungi. We also measured how the soil environment affected carbon capture and allocation by pulse labelling seedlings with 13CO2. We then tested for linkages between foliar nutrient stoichiometry and carbon capture and allocation and soil origin using statistical modelling approaches. Performance of alder and nitrogen nutrition were best on home and birch Betula pendula soils (both Betulaceae), whereas performance on Douglas fir Pseudotsuga menziesii (Pinaceae) soil was poor. Plants growing in P. menziesii soil were virtually devoid of Frankia and ectomycorrhizas, and the natural abundance 15N signatures of leaves were more enriched indicating distinct nitrogen acquisition pathways. Seedlings in these soils also had smaller 13C fixation and root allocation rates, leading to smaller 13C respiration rates by microbes. Statistical models showed that the best predictors of foliar N concentration were 13C allocation rates to fine roots and net CO2 exchange from the mesocosms. The best predictors for foliar phosphorus concentration were net CO2 exchange from the mesocosms and soil origin; seedlings in home soils tended to have greater foliar phosphorus compared to birch soils while seedlings from Douglas fir soils were no different from the other treatments. Foliar phosphorus concentration was not correlated with plant available or total soil phosphorus for any of the soils. Home soils also resulted in distinct ectomycorrhizal communities on seedlings roots, which could be responsible for greater foliar phosphorus concentration. Our findings show how the association of alder with nitrogen‐fixing Frankia relieved nitrogen limitation in the seedling triggering a performance feedback loop. We propose that relief of nitrogen limitation likely increases plant phosphorus demand, which may promote the formation of ectomycorrhizas in nutrient‐deficient soils. The formation of tripartite symbioses therefore generates positive plant–soil feedbacks, which enables plants to acquire mineral nutrients otherwise inaccessible in trade for carbon. A free Plain Language Summary can be found within the Supporting Information of this article.

Highlights

  • Plant–­soil feedback occurs when reciprocal interactions with abiotic and biotic components of the soil environment lead to positive or negative effects on plant performance (Bever et al, 2010)

  • The best predictors for foliar phosphorus concentration were net CO2 exchange from the mesocosms and soil origin; seedlings in home soils tended to have greater foliar phosphorus compared to birch soils while seedlings from Douglas fir soils were no different from the other treatments

  • We propose that relief of nitrogen limitation likely increases plant phosphorus demand, which may promote the formation of ectomycorrhizas in nutrient-­deficient soils

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Summary

| INTRODUCTION

Plant–­soil feedback occurs when reciprocal interactions with abiotic and biotic components of the soil environment lead to positive or negative effects on plant performance (Bever et al, 2010). In line with these findings, Teste et al (2017) reported that plant responses to soil biota differed according to their nutrient acquisition strategy, including positive feedbacks for ECM plants and negative feedback for N-­fixing plants The mechanisms underlying such effects are unclear but the ability to resist pathogens, while maintaining associations with beneficial nutritional symbionts, is likely to be a key factor. We predicted that (2a) leaf N content in seedlings would be tightly linked to Frankia nodulation and to C allocation below-­ground; and (2b) P content in leaves would be greater in seedlings grown in home soils because specialist ECM fungi enhance P acquisition These hypotheses were tested using mesocosms comprising intact soil cores collected from the field and maintained in a controlled environment facility. This approach enabled us to conduct a suite of analyses related to carbon and mineral nutrient cycling and interactions with key biodiversity groups to gain mechanistic insight into plant–­soil feedbacks

| MATERIALS AND METHODS
Findings
| DISCUSSION
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