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. 2010 Aug 10;107(32):14251-6.
doi: 10.1073/pnas.0914281107. Epub 2010 Jul 27.

Functional diversity of microbial decomposers facilitates plant coexistence in a plant-microbe-soil feedback model

Affiliations

Functional diversity of microbial decomposers facilitates plant coexistence in a plant-microbe-soil feedback model

Takeshi Miki et al. Proc Natl Acad Sci U S A. .

Abstract

Theory and empirical evidence suggest that plant-soil feedback (PSF) determines the structure of a plant community and nutrient cycling in terrestrial ecosystems. The plant community alters the nutrient pool size in soil by affecting litter decomposition processes, which in turn shapes the plant community, forming a PSF system. However, the role of microbial decomposers in PSF function is often overlooked, and it remains unclear whether decomposers reinforce or weaken litter-mediated plant control over nutrient cycling. Here, we present a theoretical model incorporating the functional diversity of both plants and microbial decomposers. Two fundamental microbial processes are included that control nutrient mineralization from plant litter: (i) assimilation of mineralized nutrient into the microbial biomass (microbial immobilization), and (ii) release of the microbial nutrients into the inorganic nutrient pool (net mineralization). With this model, we show that microbial diversity may act as a buffer that weakens plant control over the soil nutrient pool, reversing the sign of PSF from positive to negative and facilitating plant coexistence. This is explained by the decoupling of litter decomposability and nutrient pool size arising from a flexible change in the microbial community composition and decomposition processes in response to variations in plant litter decomposability. Our results suggest that the microbial community plays a central role in PSF function and the plant community structure. Furthermore, the results strongly imply that the plant-centered view of nutrient cycling should be changed to a plant-microbe-soil feedback system, by incorporating the community ecology of microbial decomposers and their functional diversity.

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Conflict of interest statement

The authors declare no conflict of interest.

Figures

Fig. 1.
Fig. 1.
Flow diagram of the plant–microbe–soil feedback model. Flows from the inorganic nutrient pool (N) to the plant compartments (PL and PN) represent primary production processes. Flows from the plant compartments to the two litter compartments (DR and DS) represent litter production. Flows from the litter compartments to the microbial biomasses (MR and MS) represent decomposition (gross mineralization) and subsequent microbial immobilization (microbial growth) processes. Flows from the litter compartments to the inorganic nutrient pool represent direct mineralization. Flows from the microbial biomass to the inorganic nutrient pool represent net mineralization through nutrient release from microbial biomass due to predation.
Fig. 2.
Fig. 2.
Consequences of PMSF on nutrient cycling, as a function of plant litter decomposability. (A) Relationship between litter decomposability (fL) and equilibrium nutrient pool size in systems with a better competitor for light (PL) only. Red, green, and blue lines correspond to systems with only MR, only MS, and both MR and MS, respectively. In the region with coexisting MR and MS, the slope of the line is zero. (B) Relationship between litter decomposability (fL), relative abundance of DR-preferring microbes (RA of MR, dimensionless), and readily decomposable DR and slowly decomposable DS accumulations in a system with PL only. (C) Relationship between the average litter decomposability (long-term average of formula image, from t = 45,000 to t = 50,000) and the average nutrient pool size (long-term average of N) in a system with two plant species. Consequences of PMSF on nutrient pool size for every combination of (fL and fN) from (0.0, 0.0) to (1.0, 1.0) with interval (ΔfL, ΔfN) = (0.01, 0.01) are plotted against the average litter decomposability in a system with microbial functional group MR only (red dots), MS only (green dots), and with two competing microbial groups (blue dots). All parameters are set as default values (Table S1).
Fig. 3.
Fig. 3.
Roles of microbial diversity in determining the sign of PSF. Dependence of the sign of PSF on litter decomposabilities fL and fN is shown in a system with PL only (“PL-dominant community”) (A) and PN only (“PN-dominant community”) (B), respectively. There are three distinct configurations for the microbial community: a system with MR only (“w/ MR only”), MS only (“w/ MS only”), and with microbial diversity (“w/ diversity”). The sign of PSF is positive (“Positive PSF”, ”Positive”, “+tive”, or “+”) or negative (“Negative PSF” or “Negative”). In a system with microbial diversity, the realized microbial composition depending on litter decomposability is shown as “Shifts in microbial composition” (MS, MR and MS, or MR). If the litter decomposability is too low, the system cannot persist (“no persistence”). Parameters are set to default values (Table S1).
Fig. 4.
Fig. 4.
Consequences of PMSF on plant communities, as a function of the plant litter decomposability (fL and fN). (A and B) Microbial community consisting of MR (A) or MS (B) only. (C) Microbial community consisting of MR and MS, and their realized community compositions as determined by PMSF. A better competitor for light (PL) is dominant in the plant community in region L, a better competitor for nutrient (PN) is dominant in region N, and the two plant species coexist in the region C. In region X, the ecosystem cannot persist because the plant litter decomposability of the dominant species or that of the invasible species is too low (see SI Text, Section 5). Coexistence or dominance of PN is realized in region C or N, and dominance of PL or PN is realized in region L or N, depending on the initial conditions. In a system with functional microbial diversity, dependence of the realized microbial composition (dominance of DR- or DS-preferring microbes or coexistence) on litter decomposability is not shown (Fig. S6). Although plant coexistence is realized by periodic succession with some combinations of litter decomposability, we did not distinguish this from coexistence at steady state. The presence of periodic succession may result in complex boundaries between region C or N, region N, and region L or N (see SI Text, Section 5). Parameters are set to default values (Table S1).

References

    1. Wedin DA, Tilman D. Species effects on nitrogen cycling: A test with perennial grasses. Oecologia. 1990;84:433–441. - PubMed
    1. Scott NA, Binkley D. Foliage litter quality and annual net N mineralization: comparison across North American forest sites. Oecologia. 1997;111:151–159. - PubMed
    1. Binkley D, Giardina C. Why do tree species affect soils? The warp and woof of tree-soil interactions. Biogeochemistry. 1998;42:89–106.
    1. Berendse F, Oudhof H, Bol J. A comparative study on nutrient cycling in wet heathland ecosystems. I. Litter production and nutrient losses from the plant. Oecologia. 1987;74:174–184. - PubMed
    1. Berendse F, Bobbink R, Rouwenhorst G. A comparative study on nutrient cycling in wet heathland ecosystems. II. Litter decomposition and nutrient mineralization. Oecologia. 1989;78:338–348. - PubMed

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