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Interactions of Bacteria, Fungi, and Their Nematode Grazers: Effects on Nutrient Cycling and Plant Growth

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Abstract

The most common system responses attributed to microfloral grazers (protozoa, nematodes, microarthropods) in the literature are increased plant growth, increased N uptake by plants, decreased or increased bacterial populations, increased CO"2 evolution, increased N and P mineralization, and increased substrate utilization. Based on this evidence in the literature, a conceptual model was proposed in which microfloral grazers were considered as separate state variables. To help evaluate the model, the effects of microbivorous nematodes on microbial growth, nutrient cycling, plant growth, and nutrient uptake were examined with reference to activities within and outside of the rhizosphere. Blue grama grass (Bouteloua gracilis) was grown in gnotobiotic microcosms containing sandy loam soil low in inorganic N, with or without chitin amendments as a source of organic N. The soil was inoculated with bacteria (Pseudomonas paucimobilis or P. stutzeri) or fungus (Fusarium oxysporum), with half the bacterial microcosms inoculated with bacterial-feeding nematodes (Pelodera sp. or Acrobeloides sp.) and half the fungal microcosms inoculated with fungal-feeding nematodes (Aphelenchus avenae). Similar results were obtained from both the unamended and the chitin-amended experiments. Bacteria, fungi, and both trophic groups of nematodes were more abundant in the rhizosphere than in nonrhizosphere soil. All treatments containing nematodes and bacteria had higher bacterial densities than similar treatments without nematodes. Plants growing in soil with bacteria and bacterial-feeding nematodes grew faster and initially took up more N than plants in soil with only bacteria, because of increased N mineralization by bacteria, NH"4^+-N excretion by nematodes, and greater initial exploitation of soil by plant roots. Addition of fungal-feeding nematodes did not increase plant growth or N uptake because these nematodes excreted less NH"4^+-N than did bacterial-feeding nematode populations and because the N mineralized by the fungus alone was sufficient for plant growth. Total shoot P was significantly greater in treatments with fungus or Pelodera sp. than in the sterile plant control or treatments with plants plus Pseudomonas stutzeri until the end of the experiment. The additional mineralization that occurs due to the activities of microbial grazers may be significant for increasing plant growth only when mineralization by microflora alone is insufficient to meet the plants' requirements. However, while the advantage of increased N mineralization by microbial grazers may be short-term, it may occur in many ecosystems in those short periods of ideal conditions when plant growth can occur. Thus, these results support other claims in the literature that microbial grazers may perform important regulatory functions at critical times in the growth of plants.
Interactions of Bacteria, Fungi, and their Nematode Grazers: Effects on Nutrient Cycling and
Plant Growth
Author(s): Russell E. Ingham, J. A. Trofymow, Elaine R. Ingham, David C. Coleman
Source:
Ecological Monographs,
Vol. 55, No. 1 (Mar., 1985), pp. 119-140
Published by: Ecological Society of America
Stable URL: http://www.jstor.org/stable/1942528
Accessed: 08/01/2009 15:10
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... However, relationships between different bacterial-feeding nematodes, bacterial diversity, and community composition when organic and inorganic fertilizers are used together remain unclear. Additionally, bacterial-feeding nematodes can excrete inorganic N (mainly NH 4 + -N) to stimulate bacterial growth (Ingham et al. 1985), which is particularly important for maintaining soil bacterial abundance and N availability in agroecosystems. However, whether bacterial-feeding nematodes affect soil N availability through their effect on bacterial diversity and which genera of bacterial-feeding nematodes mainly contribute to the improvement of soil N availability when organic and inorganic fertilizers are used together is still unclear. ...
... First, moderate predation by nematodes can promote bacterial growth (Fu et al. 2005). Second, nematodes supply nutrients to bacteria to stimulate their growth by excreting inorganic N (mainly NH 4 + -N) and organic matter (Ingham et al. 1985). Third, numerous bacterial species can attach to the body surface or digestive system of nematodes (Jiang et al. 2017). ...
... Additionally, in this study, bacterial community composition had stronger influence on the NO 3 − -N content than bacterial diversity and abundance, considering that NO 3 − -N showed no correlation with the bacterial diversity index, and bacterial community composition showed a stronger effect on the NO 3 − -N content than bacterial abundance. In other study, bacterial-feeding nematodes are found to secrete NH 4 + -N after feeding on bacteria (Ingham et al. 1985). The SNPK soil had a significantly higher bacterial-feeding nematode abundance than unfertilized soil, with bacterial-feeding nematodes being a critical factor driving the changes in the NH 4 + -N content in this study. ...
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Bacterial-feeding nematodes affect bacteria-mediated nitrogen (N) cycling processes by their predation on bacteria. However, the correlations between bacterial abundance, diversity, community composition, and the abundance of bacterial-feeding nematodes in the presence of organic combined with inorganic fertilizers, and their effects on soil N availability are unclear. Here, four field fertilization treatments, including unfertilized control (CK), chemical N, phosphorus (P) and potassium (K) fertilizers (NPK), NPK plus crop straw (SNPK), and NPK plus pig manure (MNPK), were performed for studying relationships among bacterial abundance, diversity, community composition, and the abundance of bacterial-feeding nematodes along with corresponding effects on soil N availability. Results showed that nitrate nitrogen (NO3−-N) content was significantly upregulated in the SNPK and MNPK treatments compared to that in the NPK treatment and showed a significant positive relationship with bacterial abundance and community composition. As revealed by partial least squares structural equation model (PLS-SEM), bacterial community composition had a stronger effect on the NO3−-N content, and bacterial-feeding nematodes indirectly affected the NO3−-N content by directly positively affecting the bacterial community composition, among which the bacterial-feeding nematode Eucephalobus played a stronger role in the production of NO3−-N. Overall, the findings of this study suggested that bacterial-feeding nematodes can improve soil N availability through impacting bacterial community composition rather than bacterial diversity and abundance. These results suggest that bacterial-feeding nematodes may play an important role in improving soil N availability in farmlands.
... However, soil nematodes, including plant-feeding (PF), bacterialfeeding (BF), fungal-feeding (FF), and omnivorous-carnivorous (OC) feeding-groups, have been shown to be sensitive to the increased availability of soil N in grasslands (Peng et al., 2022;Wardle et al., 2013;Xing et al., 2022). As widespread and diverse fauna groups in grasslands (Bardgett and Chan, 1999;, soil nematodes have potential effects on soil carbon (C) and nutrient cycling (Ferris, 2010;Ferris et al., 1997;Ingham et al., 1985). Many earlier studies examined the effects of N addition on nematode communities in grasslands at the local scale, with great variations in the direction and magnitude of responses to N enrichment across different studies (Chen et al., 2015a;Song et al., 2016;Treseder, 2008). ...
... For instance, PF nematodes can infect the roots of many plant species, which induce the leakage of carbohydrates and nutrients from injured roots; thus, increasing food supplies for microbial communities and accelerating C cycling in the rhizosphere soil (Gan and Wickings, 2020;Yeates et al., 1999;Yeates et al., 1998). In addition, BF and FF nematodes primarily feed on bacteria and fungi, respectively, which accelerates the growth and metabolism of microbes and promotes the C mineralization rate (Alkemade et al., 1992;Ingham et al., 1985;Trofymow and Coleman, 2021;Wu et al., 2007). However, the predation of OC nematodes on BF and FF nematodes can suppress the growth and reproduction of freeliving nematodes. ...
... After controlling the effects of lnRR of MBC, partial regression analysis showed that variations in the lnRR of the soil C min rate was primarily explained by the lnRR of nematode taxon richness, the lnRR of total abundance, and lnRRs of PF and FF abundances. The high diversity of nematode communities has been shown to stimulate a wider variety of microbes and thus increase microbial biomass Ingham et al., 1985). Therefore, the decline of nematode taxon richness and abundance under N enrichment may weaken its positive impacts on microbial biomass and contribute to the reduction of C min . ...
... Thus, growers need to be judicious in their use of biofumigant crops-restricting their use over time as to not impinge upon soil microbial functioning [22]. For example, biofumigant crops can have deleterious effects on essential beneficial microbes such as arbuscular mycorrhizal fungi (AMF) and free-living nematodes (FLNs) [23,24]). There is evidence that these crops may negatively affect AMF by inhibiting spore germination [25,26], suppressing the AM symbioses [27,28]. ...
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Farmers hoping to manage cropping systems sustainably are turning to cover crops to help mitigate plant pathogens. Plants with biofumigant properties are used to control soil-borne pathogens in agricultural settings, especially in till systems, where the brassicas are incorporated into the soil as green manure or seed meal. The effect of these crops is not well studied in no-till systems; thus, it is hard to know if they are as effective as green manure. Whether or not these cover crops can effect changes during a single growth season has not yet been studied. This study compared the response of the soil microbial community to four different brassica cover crops, two of which are commonly used in vineyards (Sinapis alba L. (white mustard) and Raphanus sativus (L.) Domin (tillage radish)) as well as two brassicas that are native or naturalized to the Okanagan (Capsella bursa-pastoris (L.) Medik. (Shepherd’s purse) and Boechera holboelli (Hornem.) Á. Löve and D. Löve (Holbøll’s rockcress)). Cover crops did not affect fungal species richness, but B. holboelli recover crops were associated with increased evenness among fungal taxa. Both C. bursa-pastoris and S. alba had lower levels of plant parasitic nematodes compared to non-brassica controls. These results were apparent only after a single growing season, which indicates growers could use this approach as needed, minimizing long-term exposure to biofumigants for beneficial soil microbes.
... They play crucial roles in ecosystem processes, such as improving soil physical properties, participating in carbon and nitrogen cycling by feeding on bacteria and fungi (Ingham et al. 1985), and maintaining ecosystem health by occupying key positions in the soil food cycle (Ferris 2010;Zhang et al. 2017). In contrast, soil nematode communities are affected by subtle changes in both abiotic and biotic factors (Neher et al. 2005). ...
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... 3. Dave Coleman, Pat Reid, Don Klein, and Vern Cole measured belowground processes including microbes, fauna, roots, and nutrient cycling studied in gnotobiotic microcosms. The major findings of this research concluded that trophic interactions by microbivorous fauna (protists, nematodes, and microarthropods) led to significantly enhanced nutrient return to soils, followed by enhanced plant growth (Coleman et al., 1983;Ingham et al., 1985). 4. The need for simulation modeling expertise encouraged Bill Hunt to rejoin NREL. ...
... For instance, soil nematodes had a C: N ratio similar to that of their microbial prey that would be lower in the predator through respiration of C (Ferris et al., 1997). The extra N and Nrich compounds such as inorganic N were released to soil (Ingham et al., 1985). In conclusion, strong abiotic-biotic interactions indirectly promoted ecosystem functions through stimulating growth and metabolism of plants and soil biota. ...
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Grasslands across arid and semi‐arid regions are predicted to experience reductions in precipitation frequency. Besides, grassland degradation has become a serious problem in many of these areas. Despite increasing evidence suggesting compound effects of these synchronous alterations on biotic and abiotic ecosystem constituents, we still do not know how they will impact the coupling among ecosystem constituents and its consequences on ecosystem functioning. Here, we assessed the effects of decreased precipitation frequency and grassland degradation on ecosystem coupling, quantified based on the mean strength of pairwise correlations among multispecies communities and their physicochemical environment, individual functions and ecosystem multifunctionality, and reported their relationships within a mechanistic plant–nematode–micro‐organism–soil interactions framework. Decreased precipitation frequency led to poorly coupled ecosystems, and reduced aboveground plant biomass, soil water content, soil nutrient levels, soil biota abundance and multifunctionality. By contrast, belowground plant biomass and soil potential enzyme activities increased under decreased precipitation frequency treatment. Severe degradation resulted in decoupled ecosystems and suppressed most of individual functions and multifunctionality. Using structural equation modelling, we showed that coupling had a strong direct positive effect on multifunctionality (standardized total effect: 0.74), while multifunctionality was weakened by greater soil water variation (−0.54) and higher soil pH (−0.53). The great sensitivity of ecosystem coupling to altered precipitation regimes and degradation highlights the importance of considering interactions among biotic and abiotic components when predicting early ecological impacts under changing environments. Moreover, the positive relationship between ecosystem coupling and functioning suggests that restoration of degraded grasslands may be achieved by intensifying ecological interactions. Read the free Plain Language Summary for this article on the Journal blog.
... Nematodes are a dominant component of soil biodiversity [1,2] that play fundamental roles in nutrient cycling [3][4][5] and controlling the structure and activities of the microbial community [6,7]. Free-living nematodes enhance plant growth and crop production [5,[8][9][10] whereas plant-parasitic nematodes are a major pest group in agriculture causing considerable economic losses [11,12]. ...
... The increased food web structure thus obtained is thought to enhance the natural regulation of soilborne pests and diseases, including that of plant-parasitic nematodes, thus supplying an important regulation ecosystem service to agroecosystems, and reducing the dependence on chemical pesticides [112]. Moreover, through their regulatory role in the decomposer community, bacterial-and fungal-feeding nematodes have the capacity to increase resource partitioning, substrate-use efficiency, and nutrient mineralization by bacteria and fungi, thus contributing to plant nutrition whilst promoting C sequestration [113]. Finally, increasing crop diversity, either in space (intercropping, polycropping) or in time (rotation) may be able to dilute herbivory and antagonism by specialist organisms-a well-described soil-feedback mechanism that leads to overyielding or increased plant productivity [114]. ...
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