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Applied and Environmental Microbiology, December 2002, p. 6094-6105, Vol. 68, No. 12
0099-2240/02/$04.00+0 DOI: 10.1128/AEM.68.12.6094-6105.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.
Department of Molecular and Cell Biology, Institute of Medical Sciences, University of Aberdeen, Foresterhill, Aberdeen AB25 2ZD,1 Soil-Plant Dynamics Group, Scottish Crop Research Institute, Invergowrie, Dundee DD2 5DA, United Kingdom,3 Department of Evolutionary Biology, Zoological Institute, University of Copenhagen, DK-2100 Copenhagen, Denmark2
Received 10 June 2002/ Accepted 16 September 2002
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Many of the interactions between protozoan grazers and their prey are probably similar in aquatic and soil habitats, but there are some important differences. For example, the physical nature of soil means that diffusion, mixing, and movement of organisms is severely constrained compared to aquatic systems. In addition, soil protozoan activity is restricted to water films and water-filled pores, and small pores may protect bacteria from grazing (45, 48, 64). Free-living protozoa fall into three broad categories: filter feeders, raptorial feeders, and diffusion feeders (16). Boenigk and Arndt (2) suggested restriction of the term "raptorial feeding" to forms that actively search for food particles, whereas forms that produce a feeding current and intercept each food particle individually should be referred to as interception feeders. Although filter-feeding ciliates (16) and choanoflagellates (12, 14) are found in soils, the dominant feeding strategies among typical soil protozoa are raptorial feeding and, to some extent, interception feeding. The naked amoebae, and many of the common heterotrophic flagellates, are associated with surfaces and mainly feed on attached bacteria, as demonstrated for Rhyncomonas nasuta and species of the genus Bodo (7, 54). Small chrysophyte flagellates (Spumella spp.) that mainly feed on suspended bacteria by direct interception (2, 54) are also common in soils (14).
Due to the differences between the environments, the results from pelagic systems cannot be directly extrapolated to soil systems. Recently, however, a study using DNA fingerprinting (denaturing gradient gel electrophoresis [DGGE] analysis of PCR-amplified 16S rRNA gene sequences), community level physiological profiling (using Biolog plates), and phospholipid fatty acid analysis demonstrated that protozoan grazing changed the compositions of the microbial communities in soil microcosms (18). Phospholipid fatty acid analysis indicated that the proportion of gram-positive bacteria increased in response to protozoan grazing, but a more specific analysis of grazing effects on the bacterial community was not carried out.
Protozoa are ubiquitous and very abundant in virtually all natural soils (13), but the performance of controlled experiments requires a control treatment with different bacteria but without protozoa. Removal of protozoa from the soil also affects the bacterial community; hence, it is not possible to study the effect of protozoa on an undisturbed bacterial community. In this study, we obtained a soil with a diverse bacterial community, but without protozoa, by reinoculating sterilized soil with two types of bacterial suspensions from which protozoa had been removed by filtering and dilution, respectively.
The aims of this study were (i) to investigate the potential importance of protozoan grazing for bacterial community structure in soil, (ii) to test the hypothesis that protozoan grazing changes the size distribution of bacteria in soil, (iii) to assess whether different protozoa with different feeding ecologies have different effects, and (iv) to obtain more detailed information about how individual types of bacteria respond to grazing. We studied the effects of a mixture of eight protozoan isolates (representing common and abundant morphotypes) in soil microcosms amended with two different carbon substrates (sterilized wheat roots and a nutrient solution). These substrates were chosen to represent two contrasting situations in soil where bacterial and protozoan activity is high, namely, during decomposition of dead plant material and in the rhizosphere zone around growing plant roots. When dead plant material is added to soil, protozoan populations usually increase for 1 to 3 weeks (11, 49, 60) or, in some cases, up to 6 weeks (8). Furthermore, the initial number of protozoa in the inoculum was low, and we therefore sampled after 25 and 52 days to allow full colonization of the soil systems. The taxonomic structure of the bacterial community was assessed by DGGE of PCR-amplified 16S rRNA gene fragments, and the physiological potential of the community was examined with Biolog plates. The bacterial cell size distribution was evaluated by counting and measuring bacterial cells by direct epifluorescence microscopy. To gain information about which bacteria respond to grazing, selected prominent bands from DGGE gels were excised and sequenced. Finally, we compared the effects of five different protozoan isolates representing common and abundant morphotypes; we used one amoeba, three surface-feeding flagellates, and one flagellate that feeds mainly on bacteria in suspension.
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Isolation of protozoa and preparation of protozoan-free inoculum.
The protozoa were isolated from microtiter plates with dilution cultures (diluted in tryptic soy broth [TSB] to 0.3 g liter-1) prepared from soil samples and incubated at 15°C. The wells were inspected using an inverted microscope several times during a 3-week period, and protozoa were isolated from wells that were free from fungal growth and contained only one protozoan morphotype. Isolates were kept in sterile 50-ml Nunc culture flasks with 10 ml of dilute TSB medium (0.3 g liter-1) and inspected several times during a 4-week period. Eight isolates (one amoeba and seven flagellates) that appeared to be pure cultures were examined by conventional light microscopy and were assigned to the following species or morphotypes: Acanthamoeba sp., Bodo designis, Heteromita globosa, Cercomonas sp. morphotype 1, Cercomonas sp. morphotype 2, Thaumatomonas sp., Spumella sp., and an undescribed species (referred to as type A by Ekelund et al. [14]).
A mixed protozoan-free community of soil bacteria was obtained by homogenizing 60 g of soil with 200 ml of amoeba saline (40) for 2 min in a kitchen blender and separating bacteria from soil particles by flotation in Percoll (Pharmacia Fine Chemicals, Uppsala, Sweden) according to the method of Priemé et al. (46). The resulting suspension was filtered through Nuclepore filters (Whatman International Ltd., Maidstone, United Kingdom) with successively smaller pore diameters (5, 3, 2, and 1 µm) in order to eliminate protozoa. The filtered suspensions were kept in culture flasks until the start of the experiment and were inspected for protozoan contamination prior to inoculation. Some flasks contained small flagellates and were discarded. The filtered suspensions were supplemented with bacteria obtained from protozoan-free wells in the microtiter plates used for isolation of protozoa to minimize the number of bacterial types present in the protozoan cultures but absent in the control soils. To reduce this number further, protozoan cultures in microtiter plates were diluted again and bacteria and protozoa were isolated as described above. This procedure was repeated twice.
Experimental design.
The first experiment was set up with a 2-by-2 factorial design with two different carbon substrates, each with and without a mixture of eight isolates of soil protozoa. Half the microcosms received an initial amendment of 0.1 g of sterilized ground wheat roots (N content, 6.9 mg g-1; C/N ratio, ca. 60) mixed into the soil. The other half was amended with 50 µl of a nutrient solution (12.3 g of fructose liter-1, 12.3 g of glucose liter-1, 23.4 g of sucrose liter-1, 4.05 g of succinic acid liter-1, 3.95 g of malic acid liter-1, 3.0 g of arginine liter-1, 2.05 g of cysteine liter-1, 6.25 g of malt extract liter-1, 3.75 g of TSB liter-1) at intervals of 3 to 5 days during the first 6 weeks of the experiment. The simple sugars, organic acids, and amino acids in the nutrient solution are typical of those found in root exudates (19). A total of 0.88 mg of N and 18.6 mg of C was added during the experiment, corresponding to a loading rate of 39 µg of C g of soil-1 day-1, reflecting projected levels of carbon exudation in the rhizosphere of living plant roots (19). All microcosms were inoculated with 1.95 ml of a protozoan-free inoculum of mixed soil bacteria. Half the microcosms were additionally inoculated with 50 µl of a mixture of soil protozoa, while control microcosms received 50 µl of the bacterial inoculum. After incubation at 15°C for 25 and 52 days, three replicate microcosms from each of the four treatments were destructively sampled and analyzed as described below.
The second experiment was designed to compare the effects of five individual protozoan isolates (Acanthamoeba sp., Cercomonas sp. morphotype 1, Cercomonas sp. morphotype 2, Thaumatomonas sp., and Spumella sp.) with the effect of the mixed community used in the first experiment. The microcosms were established as described above for those amended with nutrient solution, with sampling after 52 days.
Extraction and purification of DNA from soil samples.
DNA was extracted from 0.5-g soil samples using phenol and disruption by a Hybaid Ribolyser Cell Disrupter as described by Webster et al. (61). After centrifugation at 10,000 x g for 5 min, the supernatant was removed and mixed with an equal volume of phenol-chloroform-isoamyl alcohol (25:24:1). The suspension was centrifuged, and the supernatant was removed and mixed with an equal volume of chloroform-isoamyl alcohol (24:1). After centrifugation, the DNA present in the aqueous supernatant was purified by gel electrophoresis through a 1% (wt/vol) low-melting-point agarose gel. A band containing DNA was excised, and the agarose was digested with agarase (Roche Diagnostics Ltd., Lewes, United Kingdom) using the manufacturer's protocol.
PCR amplification.
PCR amplification of bacterial DNA was performed using primers p3 and p2 (39), which amplify a 194-bp fragment of the 16S rRNA gene, including the variable V3 region, and incorporating a 40-bp GC clamp at the 5' end of p3. PCR amplification was carried out in two stages, with bovine serum albumin omitted in the second step, to reduce background during silver staining. In the first stage, amplification was performed in 25-µl reaction mixtures containing
10 ng of soil DNA, 0.5 U of Taq polymerase (Promega UK Ltd., Southampton, United Kingdom), each deoxynucleoside triphosphate at a concentration of 50 µM, each primer at a concentration of 0.08 µM, 1.5 mM MgCl2, appropriate dilutions of the manufacturer's buffer, and 0.5 µl of a bovine serum albumin solution (10 mg ml-1; Roche Diagnostics Ltd.). The cycling parameters were 95°C for 5 min, followed by 10 cycles of 94°C for 30 s, 55°C for 30 s and 72°C for 30 s. In the second stage, 1 µl of the reaction mixture from the first stage was used as a template, and amplification was performed in 50-µl reaction mixtures as described by McCaig et al. (37) with the exception that only 25 cycles were applied. The amplification products were visualized on ethidium bromide-stained agarose gels.
DGGE.
DGGE analysis was carried out as described by McCaig et al. (37) using a 40 to 60% vertical denaturing gradient. Approximately 50 ng of each PCR product was loaded, and the gels were electrophoresed for 16 h at 75 V and 60°C. The gels were either stained in ethidium bromide (10 µg ml-1) for 15 min (for excising bands) or silver stained and fixed (37) for image analysis using Phoretix 1D gel analysis software version 4.00 (Phoretix International, Newcastle upon Tyne, United Kingdom) as described previously (37). To correct for variations in DNA loading between lanes, the band intensity in each lane was normalized to that of the lane with the lowest DNA load (37). The data for the relative intensities of the individual bands were analyzed by correspondence analysis (CANOCO for Windows version 4.0) on square-root-transformed values and with downweighting of rare species. Ordination diagrams were generated with scaling focusing on intersample distances. Data from the first experiment were analyzed using detrended correspondence analysis to remove an arch effect (29).
Excising of bands, cloning, and sequencing.
Selected bands were excised from the gels, stained with ethidium bromide, and placed in sterilized Eppendorf vials with 10 µl of sterilized distilled water. The gel slices were crushed, and the vials were left at 5°C overnight to allow diffusion of DNA from the gel slices. One microliter of the eluted DNA was used as a template in a PCR as described above. The resulting PCR product was rerun on a gel alongside the original sample to confirm the band position. Bands were excised for a second time, eluted, and reamplified as before. Where the second DGGE resulted in further resolution of the original band into two bands, both bands were excised. The amplified products were then sequenced with p1 and p2 (39), and the sequences were compared to the EMBL database using FastA searches.
Biolog.
Profiling of the physiological potential of the microbial community using Biolog (Biolog, Hayward, Calif.) was done at the sampling after 52 days for all four treatments of experiment 1 and for the treatment with Acanthamoeba and Cercomonas sp. morphotype 1 of experiment 2. Soil samples (2.5 g) were shaken with 20 ml of sterile amoeba saline for 15 min on a Stuart flask shaker. The resulting soil suspension was further diluted in sterile amoeba saline to give an absorbance of 0.4 at a wavelength of 595 nm, and 150 µl was inoculated into each well of a Biolog GN1 plate. The plates were incubated at 15°C, and the absorbance of each well at 595 nm was measured with an automatic plate reader after 3, 4, and 5 days. Wells with an optical density >1.4-fold greater than the control well were considered positive. The time course profiles of the Biolog data were analyzed from the area under the color development profile (23). The 95 areas (i.e., one for each substrate) were analyzed using principal-component analysis with GENSTAT version 5 release 3.2 (41).
Enumeration of bacteria and protozoa and measurement of inorganic nitrogen.
Soil samples (2.5 g) were shaken with 30 ml of sterile amoeba saline for 15 min on a Stuart flask shaker. Appropriate dilutions of this suspension were spread in triplicate on agar plates (0.3 g of TSB and 15 g of agar liter of amoeba saline-1). The plates were incubated at 14°C, and bacterial colonies were enumerated after 2, 4, 7, 9, 13, 17, 22, and 31 days. Protozoa were enumerated with a modified version of the most-probable-number method (10, 47). Threefold dilution series were prepared in microtiter plates (8 by 12 wells; Costar 3598; Biotech Line ag., Slangerup, Denmark) containing TSB (0.3 g · liter-1). The plates were incubated at 14°C, and individual wells were inspected for the presence or absence of protozoa using an inverted microscope (x200 magnification) after 1 and 4 weeks. A 4-ml sample of the soil suspension was fixed with formaldehyde (final concentration, 4%), stained with acridine orange (final concentration, 0.1 mg ml-1), and filtered through 0.2-µm-pore-size polycarbonate membrane filters (Nuclepore). The bacteria on the filters were enumerated by fluorescence microscopy at x1,250 magnification (49) and scored into size classes using a Porton graticule (36). This graticule contains 11 globes increasing in size with a
2 progression so that, at the given magnification, the size group limits are 0.19, 0.27, 0.38, 0.55, 0.77, 1.1, 1.5, 2.2, 3.1, 4.4, and 6.2 µm. Inorganic nitrogen was extracted and measured as described by Webster et al. (61).
Calculation of diversity indices.
DGGE banding data were used to estimate diversity indices. The Shannon diversity index (H') was calculated from the equation H'= -
pi · ln pi, where pi is the proportion of the total intensity of the ith band (35). Evenness (E) was calculated as E = H'/Hmax = H'/ln S (35), where S is the number of bands. The evenness varies between 0 and 1 and gives a measure of the ratio of the observed diversity (H') to the maximum diversity (Hmax = ln S). Simpson's index of dominance (D =
pi2) estimates the probability that any two individuals drawn from a community belong to different species. It is often expressed as 1/D so that an increase in the index reflects an increase in diversity (35). The Berger-Parker index (d) measures dominance as the proportion of the most abundant species, hence, d = Nmax/N, where Nmax represents the intensity of the most intense band.
An index based on the morphologies of the bacterial colonies appearing on the agar plates was calculated at the final counting. This index, the sequential-sampling index, does not require an absolute identification of colony morphology types. Colonies were inspected in a sequence, and decisions were made as to whether each new colony was different from the last one inspected. The index is calculated as the number of times an observed individual is different from the previous one observed divided by the total number of individuals (63). It has a range between 0 and 1, with a value of 1 representing the situation where each new individual observed is different from the last one observed.
Statistical analyses were performed using SigmaStat for Windows (version 2.03 package).
Nucleotide sequence accession numbers.
The sequences in this study were submitted to the EMBL database and assigned accession numbers AJ488008 through AJ488032.
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FIG. 1. Numbers of protozoa (a) and bacteria (b) and amount of inorganic nitrogen (c) in microcosms amended either with sterilized wheat roots or with a nutrient solution (sol.) and with (+P) and without (-P) a mixed protozoan community. The number of bacteria was estimated both by direct epifluorescence microscopy (AODC) and by plate counts (CFU). The error bars represent 1 standard error. Values marked with different letters are significantly different (P < 0.05; Tukey). For the bacterial counts, the letters a and b refer only to AODC values and the letters x, y, and z refer only to CFU values. For inorganic nitrogen (panel c), the error bars and letters (a, b, and c) refer to values for total inorganic nitrogen (NH4+ + NO3-).
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FIG. 2. Numbers of protozoa (a) and bacteria (b) and amount of inorganic nitrogen (c) in microcosms without protozoa (control), with a mixed community of eight isolates of soil protozoa (mixed), or with only one protozoan isolate (Acanth., Acanthamoeba; Cerc. 1 and 2, Cercomonas sp. morphotypes 1 and 2; Thaum., Thaumatomonas sp.; Spum., Spumella sp.). The data refer to the sampling after 52 days. For further details, see the legend to Fig. 1.
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FIG. 3. Frequency distribution of bacterial size classes in experiment 1 after 25 (a) and 52 days (b). The mean bacterial cell length (± standard error) for each treatment is given in parentheses. Values followed by different letters are significantly different (P < 0.05; Tukey). +P and -P, with and without a mixed protozoan community.
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subdivisions or the Cytophaga-Flavobacterium group. However, bands C and H, which were related to gram-negative bacteria of the genera Pseudomonas and Achromobacter, tended to increase in intensity during grazing. The sequenced bands accounted for 33 to 43% of the total intensity in the lanes. The percentage of intensity found in bands related to high-G+C gram-positive bacteria was significantly higher in the nutrient solution treatment than in the root treatments and increased significantly in response to grazing (Table 2), indicating that these bacteria had a selective advantage in the presence of protozoa.
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FIG. 4. DGGE analysis of 16S rRNA gene fragments amplified from DNA extracted from three replicate microcosms of the four treatments of experiment 1 using eubacterial primers. Sterile soil microcosms were amended with either sterile wheat roots (Roots) or repeated additions of a liquid nutrient solution (Nut. sol.) containing various carbohydrates, organic acids, and amino acids (see the text) and inoculated with a mixture of soil bacteria (-P) or with bacteria and a mixture of eight soil protozoan isolates (+P). Bands marked with letters to the left of the lane correspond to bands that were excised from an ethidium bromide-stained gel with the same amplified DNA.
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TABLE 1. Similarities of sequences obtained from excised DGGE bands (see Fig. 4) to sequences in the EMBL database, Gram status and phylogenetic position of the OTU, and response of the band intensity to presence of protozoa in microcosms amended with wheat root material or nutrient solution
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TABLE 2. Relative intensities of sequenced bandsa
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FIG. 5. DGGE analysis of 16S rRNA gene sequences amplified from DNA extracted from three replicate microcosms amended with nutrient solution and inoculated with bacteria only (control), bacteria and a mixture of eight soil protozoan isolates (mixed), or bacteria and one of five individual protozoan isolates (Acanth., Acanthamoeba sp.; Cerc. 1 and 2, Cercomonas sp. morphotypes 1 and 2; Thaum., Thaumatomonas sp.; Spum., Spumella sp.). The bands marked with letters are presumed to be similar to the excised bands marked in Fig. 4. The bands marked with arrows are bands that respond differently in the different treatments.
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FIG. 6. Correspondence analysis plot of the DGGE banding patterns obtained from soil microcosms inoculated with bacteria alone (-P), with mixed protozoa (+P), or with one of the five individual protozoan isolates (see the legend to Fig. 5). The error bars represent the least significant difference (Tukey); hence, the coordinates are significantly different (P < 0.05) when the error bars do not overlap the mean from another treatment.
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-lactose, while the utilization of the other substrates varied according to protozoa and environment (Table 3). Principal-component analysis based on rates of substrate utilization could not distinguish the microbial communities in the two treatments without protozoa (Fig. 7). However, the presence of a mixed protozoan inoculum resulted in a significantly different pattern, and likewise, the patterns of utilization in the treatments with mixed protozoa were significantly different for the two substrate types. The patterns of utilization were also significantly different in the nutrient treatments amended with mixed protozoa, Acanthamoeba, and Cercomonas. |
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TABLE 3. Substrates from Biolog GN plates utilized differentially by the four treatments of experiment 1 and the treatments with Acanthamoeba and Cercomonas sp. morphotype 1 of experiment 2
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FIG. 7. Principal-component (PC) plot of the community level physiological profile of soil microcosms amended with sterile roots and with (+P) or without (-P) the presence of a mixed protozoan community and soil microcosms amended with a nutrient solution (nut. sol.) without protozoa, with mixed protozoa, or with either Acanthamoeba (+Acanth. sp.) or Cercomonas sp. morphotype 1 (+Cerc. sp.1). The error bars represent the least significant difference (see the legend to Fig. 6).
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TABLE 4. Diversity indices based on DGGE data, colony morphology, and Biolog data for the four treatments of experiment 1
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For analysis of the DGGE profiles, it was assumed that each band represented 1 bacterial operational taxonomic unit (OTU) and that the intensity of the band reflected the relative abundance of this OTU in the community. However, factors such as differences in DNA extraction efficiency, primer affinity (52), amplification efficiencies of different sequences (44), and differences in the numbers of ribosomal DNA copies per cell (15) may introduce bias. Consequently, DGGE profiles do not necessarily reflect the structures of the actual bacterial communities. Furthermore, as DGGE separates sequences only on the basis of migration distance, each band may represent different sequences which comigrate to the same position in the gel. However, mixed sequences were found only rarely in excised bands and were closely related, belonging to the same phylogenetic group, while consistency in treatment and analysis of samples will reduce differential biases. The clear difference in the banding patterns of DGGE profiles for the two different substrates and between grazed and ungrazed systems indicates that the bacterial community structure was significantly affected both by bottom-up effects (substrate quality) and top-down effects (predation). Similarly, the Biolog data indicate that grazing affected the physiological profiles of the communities for both substrate types. The assay suggested a decreased physiological potential of the grazed communities, particularly in the nutrient solution treatment, where the number of positive wells was significantly lower in the presence of protozoa. Similarly, the diversity indices based on the DGGE banding pattern and on colony morphology both suggested that grazing decreased bacterial diversity (Table 4). The decreased diversity is mainly due to a decrease in evenness, presumably caused by the dominance of a few high-G+C gram-positive bacteria related to Arthrobacter. The larger proportion of high-G+C gram-positive bacteria in the presence of protozoa is consistent with previous reports (18).
Several mechanisms may contribute to the effect that grazing has on the bacterial community structure. Generally, size-selective predation has an important influence on the composition of planktonic bacterial communities (26, 31, 42, 43, 55), and we found evidence for preferential feeding on cells larger than 0.5 µm in the nutrient solution amendments. This is in accordance with the previous finding that small cells may escape predation (26). For example, a community of small flagellates dominated by Spumella guttula showed a higher rate of uptake of bacteria between 0.8 and 1.5 µm in length than of smaller or larger bacteria (34). Cells larger than 0.5 µm probably have higher growth rates than smaller cells (53), and hence, the importance of size selectivity could be underestimated by simply comparing the distributions of cell sizes. However, grazing did not affect bacterial cell size following amendment with roots, and the abundances of all bacterial size classes decreased significantly in the presence of grazers in all treatments of both experiments. Furthermore, the effect of grazing on bacterial size distribution was most evident at the first sampling and rather low at the last sampling, when the effect of grazing on DGGE and community level physiological profiles was estimated. Therefore, preferential feeding on the larger cells is probably not the most important factor for the observed changes in the taxonomic compositions of the bacterial communities. Similarly, we found no evidence for increased abundance of long grazing-resistant filamentous bacteria, as observed in plankton communities grazed by flagellates (25). Gram-positive bacteria may be less suitable protozoan food than gram-negative bacteria (1, 62), and some, e.g., the rod-shaped high-G+C gram-positive bacterium Mycobacterium chlorophenolicum, appear to be completely unaffected by grazing by indigenous soil protozoa (50). The lower edibility of gram-positive bacteria may be related to a lower rate of digestion of the gram-positive cell wall (17, 28), which may enable survival during passage through the protozoan cell (28). The flagellates, Ochromonas and Spumella, egested indigestible particles 2 to 3 min after ingestion (4, 5). Rapid excretion of unsuitable bacteria provides a very plausible explanation for active food selectivity among protozoa (5). Hence, the increased proportion of high-G+C gram-positive bacteria affiliated with Arthrobacter could be due to a low protozoan preference for these cells. Many gram-negative bacteria are good food sources for protozoa, and nonpigmented Enterobacteriaceae produce high protozoan growth yields (47, 62). If protozoa show a preference for these cells, this may explain the decrease in band E in grazed microcosms, as this band showed close affiliation with species of the Enterobacteriaceae. The intensities of two bands (D and F) related to Bdellovibrio spp., bacterial predators of gram-negative bacteria, decreased in the presence of protozoa, possibly through reductions in the abundance of their host bacteria. The direct predation pressure on the free-living stages of Bdellovibrio is probably low, since they are highly motile (6).
Although Gram status may relate to the edibility of bacteria, it is by no means an absolute factor, as many gram-positive bacteria are edible (58, 62) and many Gram-negative bacteria are completely unsuitable as food for protozoa. For example, representatives of both groups produce substances that are toxic to protozoa (9, 20), and several other factors that affect the grazing resistance of bacteria (e.g., size, cell morphology, and motility) are not related to Gram status. Furthermore, the bacterial community structure may be affected by grazing even if protozoan feeding is not selective. For example, grazing may favor bacteria with high growth rates because they will be able to replace cells lost to predation (22, 57). Grazing will also affect bacterial community structure indirectly as bacterial numbers decrease and nutrients are mineralized; hence, the competition for substrates and limiting nutrients is reduced. In this study, grazing reduced bacterial numbers for all treatments, and inorganic nitrogen increased in the nutrient solution treatment in the presence of the mixed protozoan community and Thaumatomonas. Nitrogen, however, was probably never a strong limiting factor for microbial growth, since nitrate was always present. Nitrifying bacteria are sensitive and very slow colonizers, so when sterilized soils are reinoculated, the nitrifying potential of the soil is reestablished only very slowly (51). Protozoan grazing may also affect the interaction between bacteria and other organisms in the soil. For example, protozoa were found to stimulate viral activity in freshwater systems (56). The mechanism behind this interaction is presently unknown but could be related to reduced bacterial diversity in grazing-enhanced treatments or to a change in the properties of individual bacterial cells caused by higher bacterial growth rates (56). It is possible that virus-induced mortality also changed in response to the presence of grazers in our systems, but we have no direct evidence to support this.
The protozoa chosen for these experiments are common and abundant in soil (13, 40), and their combined effects may represent that of a natural soil protozoan community. Nevertheless, the observation that the five single protozoan isolates affected the bacterial community in different ways suggests that the actual composition of the protozoan communities is important for the impact of grazing on the microbial communities. Interestingly the correspondence analysis of the DGGE profiles clearly separated the bacterial communities treated with amoebae from those treated with the suspension-feeding Spumella, whereas the effects of the three surface-feeding flagellates were similar. This suggests a correlation between the overall feeding ecology of the flagellates and their effect on the bacterial community. However, even among the three surface-feeding species, differences in banding patterns could be observed by direct visual inspection of the DGGE profiles, in agreement with the results of Boenigk and Arndt (3) and Boenigk et al. (5), who found considerable species-specific differences in the feeding behaviors of different flagellates.
The short generation times of bacteria and protozoa mean that changes in population sizes may occur rapidly, and sampling on only two occasions would not have detected all fluctuations in bacterial community structure. In aquatic systems, significant changes in bacterial community structure have been observed after a few days with increased grazing pressure (32). However, the physical constraints on mixing and movement in soil probably mean that oscillations in the overall dynamics of protozoan and bacterial populations are reduced compared to aquatic systems. Furthermore, effects of grazing were found on both samplings, and even if fluctuations in community structure occurred, the results clearly indicate that protozoan grazing may have an important impact on the bacterial community structure in soil. The observation that high-G+C gram-positive bacteria related to Arthrobacter appeared to be favored by grazing was interesting, given their high relative abundance in soil. Protozoan grazing probably affects bacterial communities through a wide array of interacting mechanisms, such as selective feeding, differences in the susceptibilities of bacteria to predation, and indirect effects on the conditions for growth of bacterial populations (e.g., nutrient and substrate availability). The finding that even rather similar flagellate species had different effects on the community structure indicates that species-specific food preferences may be important. In future studies, it will be of great interest to gain deeper insight into the bacterial characteristics that affect their responses to grazers with different feeding ecologies. This would provide a better basis for understanding how microfaunal grazing on microbial communities affects the functioning of those communities.
We thank Gordon Webster for analysis of inorganic nitrogen and Flemming Ekelund for help with identification of flagellates and for comments on the manuscript.
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