The role of locally adapted mycorrhizas and rhizobacteria in plant–soil feedback systems

Abstract

Summary1. The plant-soil feedback (PSF) framework has become an important theory in plant ecology, yet many ecological and evolutionary factors that influence PSFs have yet to be fully considered. Here, we discuss the importance of local adaptation among plants and root-associated fungi and bacteria. Furthermore, we show how inclusion of the optimal resource allocation (OA) model can help predict the direction and outcome of PSFs under environmental change. 2. Plants and associated soil microbes have co-evolved for millennia, generating adaptations to each other and to their local environment. This local co-adaptation is likely generated by a suite of multidirectional exchanges of goods and services among plants, fungi and bacteria, and the constant changes in above-ground-below-ground interactions. 3. Resource limitation may be a driver of local adaptation among organisms involved in nutritional symbioses. The OA model states that when an essential resource is limited, natural selection will favour taxa that forage optimally by adjusting their biomass and energy allocation such that productivity is equally limited by all resources. Co-adaptation will therefore respond to the local limiting resource conditions through taxa-specific resource transfer interactions. 4. The OA model can help predict the outcomes of PSFs across a range of resource gradients and environmental changes such as increasing drought or atmospheric nitrogen deposition. Positive feedback is predicted in systems where resource exchange among plants and associated soil microbes can ameliorate resource limitation, or in systems where microbes provide another important service such as pathogen defence. Feedback strength is expected to diminish as resources become less limiting. Negative feedback is predicted when resources are in luxury supply and populations of opportunistic plant pathogens increase relative to commensal or mutualist microbes. 5. Future, field-based studies that integrate naturally co-occurring systems of plants, microbes and their local soil are needed to further test the hypothesis that resource availability is an effective predictor of the direction and magnitude of PSFs. A more mechanistic understanding of PSFs will help land managers and farmers to manipulate plant-microbial soil interactions to respond to environmental change and to effectively harness beneficial symbioses for plant nutrition and pathogen control.

Biotic and abiotic plant–soil feedback depends on nitrogen‐acquisition strategy and shifts during long‐term ecosystem development

“…First, only common species from two plant functional groups (N‐fixing and non‐N‐fixing) were examined in the present study, which would only have accounted for a subset of the range of PSF present among the diverse spectrum of plant functional groups in species‐rich plant communities on these old, severely P‐impoverished soils (e.g., Lambers et al, ; Zemunik et al, ). In particular, plant functional groups associated with key below‐ground nutrient‐acquisition traits of AM, ECM, and non‐mycorrhizal cluster roots require further attention (Lekberg et al, ; Revillini et al, ; Teste et al, ; Zemunik et al, ). Second, the underlying mechanisms of how various groups of soil microorganisms (e.g., N‐fixing rhizobia, plant growth‐promoting rhizobacteria, and soil‐borne pathogens) influence PSF in this study remain something of a “black box.” Third, our chronosequence approach does not allow strong inference of the causal mechanisms between the observed shifts in PSF and soil N and P availability (Walker et al, ).…”

Mycorrhizal symbiosis increases the benefits of plant facilitative interactions

“…Optimal resource allocation can also influence the outcome of plant-soil feedbacks (Revillini et al 2016), and thus optimal partitioning theory predicts that plants should allocate more biomass to the organ that will alleviate resource limitation (Bloom et al 1985). Optimal resource allocation can also influence the outcome of plant-soil feedbacks (Revillini et al 2016), and thus optimal partitioning theory predicts that plants should allocate more biomass to the organ that will alleviate resource limitation (Bloom et al 1985).…”

Changing perspectives on terrestrial nitrogen cycling: The importance of weathering and evolved resource‐use traits for understanding ecosystem responses to global change

“…Accordingly, biomass of the former plant lineage does not significantly respond to N addition, while the biomass of the latter increases (Wooliver et al, ). Thus, N deposition can induce plants to decrease C investment to these symbionts below‐ground, thereby decreasing biomass and abundance of these formerly beneficial microbial symbionts (Treseder et al, ) and weakening the plant–soil feedbacks that had been positive in low‐nutrient soils (Revillini, Gehring, & Johnson, ). Based on these patterns, subsequent co‐evolution between plants and their nutrient‐acquiring microbial symbionts should diminish under N deposition, and lower abundances of mycorrhizal symbionts should leave pools of more complex SOM intact.…”