Previous Article | Next Article ![]()
Applied and Environmental Microbiology, July 2002, p. 3358-3365, Vol. 68, No. 7
0099-2240/02/$04.00+0 DOI: 10.1128/AEM.68.7.3358-3365.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.
Département de Foresterie, Faculté des Sciences, Université de Tlemcen, Tlemcen 13000, Algeria,1 Institut des Sciences Végétales, CNRS, F-91198 Gif-sur-Yvette Cedex,2 BBCE-IPM, UMR INRA 1088, F-21065 Dijon Cedex,,3 Ecologie Microbienne, Université Claude Bernard-Lyon 1, UMR CNRS 5557, and INRA, F-69622 Villeurbanne Cedex, France4
Received 6 February 2001/ Accepted 25 April 2002
| ABSTRACT |
|---|
|
|
|---|
| INTRODUCTION |
|---|
|
|
|---|
Ti plasmids are large genetic elements, representing about 5% of the agrobacterial genome (1). As a consequence, they might negatively affect the fitness of Agrobacterium in the absence of opines. When population dynamics were monitored in the presence of opines, the closely related Ri plasmid was found to improve the growth and thus the fitness of a strain harboring this plasmid over those of a plasmid-free strain. Conversely, in the absence of opine, Ri and related plasmids hampered the bacterial growth and thus acted as a genetic load (15). After the removal of diseased plants from bulk soil, and hence after the disappearance of opine sources, pathogenic agrobacteria should be negatively selected and should decline more or less rapidly. Probably this has been the empirical rationale for leaving contaminated soils fallow to eliminate pathogenic agrobacteria. This assumption comes, however, in sharp contrast to regular outbursts of crown gall, which appears to be the main bacterial disease in stone-fruit tree nurseries in Mediterranean countries.
Almost all agrobacteria, including both pathogenic and nonpathogenic forms, are able to live as saprophytes in soil by consuming nutrients of soil or plant origin. However, the survival of pathogenic agrobacteria in soil and/or the rhizosphere is poorly documented in spite of interest in obtaining such information about the primary inoculum of a major soilborne disease. However, isolation of pathogenic strains from pasture soil that had never been tilled or cultivated (28) and from a contaminated soil left fallow for 6 years (2) demonstrates the potential for long-term survival of pathogenic agrobacteria in soil.
In the present study, we report data generated from the monitoring of pathogenic populations over 4 years in one plot and over several seasons in six plots that provide new insights into the ecology of Agrobacterium and Ti plasmids in soil.
| MATERIALS AND METHODS |
|---|
|
|
|---|
|
Pathogenicity determination.
The tumor-forming ability of each isolate was determined by the method of Moore et al. (21), by inoculating three wounded stems of 4-week-old tomato seedlings (cv. Marmande) and three wounded leaves of Kalanchoe daigremontiana cultivated in the greenhouse with dense suspensions of 48-h-old bacterial cultures. Tumor formation was assessed by visual inspection 3 weeks after inoculation. The presence of a Ti plasmid in pathogenic strains and its absence in nonpathogenic strains were verified by DNA hybridizations with Ti plasmid probes as indicated below.
Biovar affiliation.
Biovars were determined according to biochemical and physiological tests (21), which included Gram staining, oxidation of lactose to 3-ketolactose, growth on Simmon's citrate sodium medium, growth on L-tyrosine, tolerance to 2% sodium chloride, growth and pigmentation on ferric ammonium citrate medium, acid production from erythritol, and growth at 35°C on solid NGA (21). Results were scored after 7 days at 28°C. The biovar affiliation was determined for all pathogenic strains and for 180 nonpathogenic isolates arbitrarily chosen whatever the sampling season from Beni Tamou, Ouled Mimoun, and Boughrara plots (30 from soil and 30 from rhizosphere in each plot).
Sensitivity to agrocin 84.
Strains were tested for agrocin sensitivity on MG agar plates by the method of Stonier (31) as modified by Cooksey and Moore (5). Mannitol glutamate plates were inoculated by spreading a loopful of strain K84, which had recently been cultivated on MG medium, at the center of each plate (over a circular zone about 3 mm in diameter). Plates were incubated for 48 h at room temperature. Resuspensions of the isolates in water for assay (ca. 108 CFU/ml) were sprayed as a fine mist onto the surface of the medium containing K84. Growth inhibition of the assayed strain was recorded after 72 h at 28°C. The agrocin 84-sensitive strain C58 and the agrocin 84-resistant strain B6 were used as positive and negative controls, respectively.
Opine synthesis and catabolism.
The presence of opines in tumors was investigated after extraction of opines from plant tissues and concentration and separation by high-voltage paper electrophoresis at pH 1.9 as previously described (9). Opine utilization was assayed by inoculating individual strains into 200 µl of a degradation cocktail, which consisted of AT minimal medium (25) supplemented with ammonium sulfate (1.0 g/liter); yeast extract (100 mg/liter); and the opines octopine (5 mM), nopaline (5 mM), cucumopine (4 mM), agropine (2.5 mM), mannopine (2.5 mM), and mannopinic acid (5 mM). The inoculated cocktail was incubated at 28°C for 7 days. Utilization of opines was assessed by investigating their disappearance from the degradation cocktail by high-voltage paper electrophoresis (9).
Extraction of DNA from soil.
Extraction of DNA from soil was done as described by Frostegård et al. (12). Extraction and purification of DNA from soil were performed immediately after soil samplings. The soil samples were sieved (2 by 2 mm), and 4x 250-mg soil aliquots were resuspended in 0.5 ml of TENP buffer (50 mM Tris, 20 mM EDTA disodium salt [pH 9.0], 100 mM NaCl, 1% [wt/vol] polyvinyl polypyrrolidone [Sigma Chemical Co. St. Louis, Mo]). The soil suspension was vortexed for 1 min and homogenized in a rotary shaker for 2 h at room temperature. The suspensions were centrifuged for 10 min at ca. 8,000 x g at 4°C. The DNA dissolved in the supernatant was precipitated with 3 M sodium acetate and isopropanol. DNA extracted from 4x 250 mg of soil was pooled and resuspended in 100 µl of TE8 buffer (50 mM Tris HCl, 20 mM EDTA [pH 8.0]) and then was further purified once on a Sephacryl S200 microtube purification cartridge (Pharmacia Biotech, Upsalla, Sweden) and twice on an Elutip d column (Schleicher & Schuell, Dassel, Germany), both as recommended by the manufacturers. The purified DNA was precipitated according to standard procedures with ethanol, and the pellet was resuspended in 10 µl of ultrapure water.
PCR detection and quantification of Ti plasmids.
The technique used for PCR detection of Ti plasmid sequences in soil microflora DNA was adapted from the method described by Picard et al. (26). A 246-bp conserved region of the vir region of the Ti plasmid was amplified with primers F14 (FGPvirG15') (GAA CGT GTT TCA ACG GTT CA) and F44 (FGPvirB11 + 21) (TGC CGC ATG GCG CGT TGT AG), which are highly efficient for specific detection of Ti plasmids (6, 24). The concentration of the target sequence was estimated by serially diluting the template DNAs before PCR as previously described (24). For this purpose, soil DNA extracts were diluted 10-fold up to 10-6. PCRs were performed in 0.5-ml microtubes in a final volume of 25 µl containing reaction buffer (10 mM Tris-HCl [pH 8.3], 50 mM MgCl2, 0.01% gelatin), the four deoxynucleoside triphosphates (dNTPs; 20 µM each), the two primers (1 µM each), 2 U of Taq DNA polymerase (Gibco-BRL), and 1 µl of the diluted template DNA. Cyclings were performed in a dry-block thermocycler (Perkin-Elmer) with an initial denaturation step of 5 min at 95°C followed by 40 cycles of denaturation for 1 min at 95°C, annealing for 1 min at 55°C, and extension for 1 min at 72°C. PCR products were separated by electrophoresis in 2% standard agarose gels and stained with ethidium bromide.
Colony hybridization.
Isolates were tested for the presence of a Ti plasmid by hybridization of colonies patched onto a nylon membrane, with nonradioactive probes obtained by PCR amplification of Ti plasmid regions of C58 by the procedure described by Mougel et al. (22). The occurrence of a Ti plasmid was probed with a fragment of the common tmr gene obtained with primers F49 (=FGPtmr530) (CCA TGT TGT TTG CTA GCC AG) and F50 (=FGPtmr701') (CCT TCG AAT CCG TCG AAA GC), while nopaline-type Ti plasmids were specifically probed with a fragment of the nos gene of C58 obtained with primers F139 (=FGPnos975) (GGC AAT TAC CTT ATC CGC AA) and F140 (=FGPnos1236') (CAC CAT CTC GTC CTT ATT GA). Patched colonies of C58 (pTiC58, nopaline-type Ti plasmid) and B6 (pTiB6, octopine-type Ti plasmid) and the Ti plasmid-free derivative strains C58C1 were used as positive and negative controls, respectively. The presence and characterization of a Ti plasmid were verified for all pathogenic strains and for the 180 arbitrarily chosen nonpathogenic isolates described above.
Statistical analyses.
Statistical analyses were done as described by Dagnelie (8) for testing the independence of proportions. The confidence interval of proportions, determined by a table obtained from Hald (16), was used to determine the confidence intervals of percentages of pathogenic strains over the total agrobacterial populations and, in turn, their densities in samples. The chi-square test was used to compare the relative distributions of pathogenic and nonpathogenic strains in different samples.
| RESULTS |
|---|
|
|
|---|
|
The density of total, cultivable agrobacteria was found to fluctuate over the season at Boughrara, Ouled Mimoun, and as at Beni Tamou (Fig. 1). The average Agrobacterium densities in these three plots were 3.3 x 103, 2.0 x 103, 1.3 x 106, and 3.8 x 106 CFU/g of bulk soil for fall, winter, spring, and summer samples, respectively. As an indication, in March 1990 at Beni Tamou, the total number of Agrobacterium-like colonies was 3 x 107 CFU/g of bulk soil. Conversely, in the plots located at Sidi Abdli 1 and 2 and Saf Saf, where no pathogenic isolates were recovered, the densities of cultivable agrobacteria were found to be low during all seasons: 3.3 x 103, 3.0 x 103, 3.3 x 103, and 5 x 103 CFU/g of bulk soil in fall, winter, spring, and summer samples, respectively.
Similar results were obtained with the weed rhizosphere samples. The average Agrobacterium densities in Boughrara, Ouled Mimoun, and Beni Tamou plots were 2.1 x 104, 2.3 x 103, 3.1 x 107, and 2.7 x 107 CFU/g of root for fall, winter, spring, and summer samples, respectively. At Sidi Abdli 1 and 2 and Saf Saf, there were 6 x 103, 5.3 x 103, 4.7 x 104, and 5.3 x 104 CFU/g of root for fall, winter, spring, and summer samples, respectively.
Seasonal fluctuations of pathogenic agrobacterial population at various plots.
The newly investigated plots were stone-fruit nurseries reported to have a history of high crown gall incidences. Pathogenic agrobacteria were isolated in only two out of five plots (Fig. 1). In these two plots (Boughrara and Ouled Mimoun), the number of pathogenic isolates was also found to fluctuate over time. In both cases, pathogenic agrobacteria were not isolated in fall or winter (October 1997 and February 1998), but only in spring and summer (April and July 1998). Statistical analyses showed a highly significant effect of the season of the relative number of pathogenic versus nonpathogenic strains at each site for soil isolates (Beni Tamou, chi-square result = 50.8, df = 3, P < 10-4; Boughrara, chi-square result = 26.8, df = 3, P < 10-4; Ouled Mimoun, chi-square result = 28.0, df = 3, P < 10-4) as well as for rhizosphere isolates (Beni Tamou, chi-square result = 41.9, df = 3, P < 10-4; Boughrara, chi-square result = 27.6, df = 3, P < 10-4; Ouled Mimoun, chi-square result = 36.9, df = 3, P < 10-4). Our hypothesis of a fluctuation of pathogenic agrobacteria in soil according to the season was therefore verified at several plots.
Pathogenic strains could be isolated only when densities of Agrobacterium-like isolates were over 105 CFU/g in bulk soil and in the rhizosphere (Fig. 1). When pathogens were recovered, their estimated densities varied from 5 x 104 to 106 CFU/g of bulk soil and from 2 x 105 to 1.5 x 107 CFU/g of rhizosphere. When no pathogens were isolated, since from less than 1 of 20 up to less than 1 of 98 agrobacterial strains were pathogenic, the absolute numbers of pathogenic strains were at a maximum 140 and 900 CFU/g of bulk soil and rhizosphere, respectively (dotted lines in Fig. 1).
PCR-based quantification of pathogenic agrobacteria in soil DNAs.
Since the results provided above were based on counting of cultivable agrobacteria, seasonal fluctuations of pathogens might be due to fluctuations in their cultivability instead of fluctuations in their actual population densities. To avoid the potential bias caused by the isolation techniques, densities of pathogenic populations in soils were estimated by direct PCR detection of Ti plasmid (i.e., vir) sequences in the whole DNA extracted from soil. DNA was extracted from soil samples obtained at Beni Tamou and Ouled Mimoun in fall (October 1999), winter (January 2000), and summer (July 2000). No amplifications were observed with fall or winter samples, while PCRs revealed the presence of sequences of the expected size with DNA templates obtained from soils collected in summer in both Beni Tamou and Ouled Mimoun (Fig. 2). The density of the target sequence was determined by a robust template dilution technique. The results indicated that the densities of vir sequences per gram of soil were below 103 copies of vir per g of soil in fall or winter and about 106 copies of vir per g of soil in summer in both Beni Tamou and Ouled Mimoun. Assuming that vir copies are likely individual Ti plasmids, the densities of Ti plasmid determined by direct PCR in summer 2000 (about 106/g in the two plots) and the densities of cultivable pathogenic agrobacteria determined in the summers of 1994 and 1998 (0.8 x 106 and 0.5 x 105 per g, for Beni Tamou and Ouled Mimoun, respectively) were equivalent. Similarly, in the absence of pathogens, both methods led to comparable results: less than 103 Ti plasmids per g or less than 140 CFU/g of soil. Fluctuations of the density of cultivable pathogenic agrobacteria over different seasons therefore appear to follow fluctuations of all physically present, pathogenic agrobacteria within the soil microflora.
|
|
| DISCUSSION |
|---|
|
|
|---|
Conducive soils are probably those that are the most favorable for Agrobacterium spp. either harboring or not harboring a Ti plasmid. In the present study, pathogenic agrobacteria were isolated in the soils that exhibited the highest densities of cultivable agrobacteria in both the bulk soil and the rhizosphere. However, the presence of bacteria hosting a Ti plasmid is not sufficient to allow the total population of Agrobacterium to reach these levels, since nonpathogenic strainsharboring no Ti plasmidwere isolated as well as pathogenic strainsfrequently in higher numbers in favorable instances (Fig. 1). Members of the genus Agrobacterium are common in soil, but precise information on their density and seasonal fluctuations are not available, especially when compared to the wealth of information about the survival of Rhizobium inoculant in soils. Edaphic factors such as pH and texture have been reported to affect the population density of plant-associated microbes (23), including members of Rhizobiaceae such as Rhizobium (27). In our study, conducive soils did not show marked pH or texture differences from the suppressive ones (Table 1). A lower percentage of sand found in the conducive soils could perhaps provide them with a better capacity for water retention than suppressive soils. Indeed, soil moisture content and the variation of this parameter are key determinants of the composition of the microflora (7), but such data were not available for the studied soils.
The total number of cultivable agrobacteria fluctuated according to the season (Fig. 1), and the relatively low agrobacterial densities reached in fall and winter in conducive soils were similar to the densities recorded all during the year in suppressive soils. The bloom of total agrobacteria in spring is probably a response to a flush of nutrients in the weed rhizosphere, and this flush should be sufficient to have also caused a bloom of agrobacteria in the distant bulk soil. While rhizodeposition is known to be cyclical and to depend upon active plant growth (19), such a bloom, for unknown reasons, was not observed in the rhizospheres of suppressive plots. Interestingly, in a field study over three growing seasons, the populations of Rhizobium trifolii were found to vary from ca. 103 to 106 g of soil-1 according to soil and seasons (29). These numbers are comparable to those found in the present study. Moreover, in unlimed soils, the rhizobial populations fluctuated with season, with the smallest numbers following the summer-fall months, but where the soil was limed, the survival of rhizobia was less seasonally dependent. Whether soil plots in the present study were limed or not is not known. Our results, however, showed that seasonal fluctuation of the soil bacterium densities is a feature shared by several species of Rhizobiaceae.
A major result generated by the present study is the characterization of seasonal fluctuations in the ratio of pathogenic populations of Agrobacterium in soils and rhizospheres. This unforeseen finding was observed in several independent plots and, to the best of our knowledge, has not been reported previously for particular (i.e., pathogenic) strains of Agrobacterium. Seasonal shifts in the abundance and composition of the whole bacterial communities in rhizospheres have recently been reported (14, 30), but these results did not deal with relative fluctuations of particular strains within a single taxon. A seasonal pattern of ribotype reoccurrence was observed within the pseudomonad populations associated with sugar beet leaves (11), showing that seasonal fluctuation in the relative ratio of finely typed strains over the total population should also occur in other taxa.
No pathogenic strains were isolated in fall and winter in Boughrara, Ouled Mimoun, Sidi Abdli, and Saf Saf in spite of a probable high population density of pathogenic strains in all of those plots resulting from the previous outburst of crown gall reported 1 year ago (Fig. 1). This was not caused by fluctuations of the cultivability of pathogenic strains as verified by direct PCR detection and quantification of Ti plasmids (i.e., vir) sequences in the DNA extracted from soils (Fig. 2). Ti plasmids were not detected by PCR during winter 1999 in Beni Tamou and Ouled Mimoun in spite of their previous detection in pathogenic strains during summer 1994 in Beni Tamou and summer 1998 in Ouled Mimoun and later by PCR in summer 2000 in both plots. This indicates an annual periodicity in seasonal fluctuation of Ti plasmid populations. The disappearanceor at least their decrease below a detectable levelof pathogenic strains in fall and winter could simply fit the seasonal fluctuation of the total cultivable agrobacteria described above. Some of our data suggest, however, that the presence of a Ti plasmid in the host Agrobacterium decreased the fitness of the bacteria in soil and in symptomless rhizosphere. This occurred at least in Beni Tamou between March 1990 (2) and November 1993 (Fig. 1), when the ratio of pathogenic populations over total cultivable agrobacteria decreased significantly between the two sampling dates. The decrease in the pathogenic strain ratio in fall and winter experienced in Beni Tamou and suspected in other plots could be related to a low fitness in the bulk soil in the absence of an opine niche. This is substantiated by Guyon et al. (15) and by our own work performed with soil microcosms showing a faster decline of the population density of strain C58 compared to that of its plasmid-free derivatives (unpublished results). It is suspected, but remains to be experimentally confirmed, that in the suppressive soils, pathogenic invaders were less fit than Ti plasmid-free strains and thus decreased rapidly below the detection limit.
A troubling fact was the increase in the ratio of pathogenic over total agrobacteria between winter and spring samplings (Fig. 1), suggesting that pathogenic strains are more fit than nonpathogenic strains during the growing season of plants. A similar increase in plasmid incidence in the rhizosphere and phytosphere over time has been reported in pseudomonad populations by Lilley and Bailey (18). A study performed with a marked strain introduced as a seed dressing to sugar beets focused on acquisition of various indigenous plasmids that confer mercury resistance. Under those experimental conditions, Lilley and Bailey demonstrated that the fluctuation in plasmid-carrying strain numbers was related to an increase in the number of transconjugants of the marked strain, which could be collected only within a narrow temporal window coincident with the midseason maturation of crop. While the results are similar in the two studies, there is no evidence that the relative increase in pathogenic agrobacteria observed in the present study results directly from seasonal transconjugant events, even if Ti plasmid conjugations probably have a greater chance to occur during the growing season of plants. In our field survey of indigenous populations, the Ti plasmid-free strains are not totally the same strains as the plasmid-containing pathogenic strains, since the majority of the former belonged to biovar 2, while the latter were equally distributed into biovars 1 and 2. The difference in fitness survival between those different populations could thus be at least partly due to a host (chromosomal) difference(s) and not only to the presence or acquisition of a Ti plasmid. Actually, this phenomenon could also result from the occurrence of associations between hosts and Ti plasmids that fit particularly well. The recovery of a significantly higher proportion of pathogenic agrobacteria in spring than in winter suggested that those strains were a better fit than the Ti plasmid-free strains in three different plots. It cannot be excluded, however, that the same close association between Ti plasmid and bacterial host was dispatched by human activity in the various stone-fruit nurseries. Nevertheless, in the conducive soils, the pathogenic invaders that exhibited poor fitness during fall and winter recovered better fitness in spring, allowing them to become soil inhabitant. The improved fitness of strains with a Ti plasmid during spring was observed in bulk soil and/or symptomless weed rhizospheres, probably in the absence of the favorable opine niche. Unknown factors are able to specifically improve the growth of strains harboring Ti plasmid in the bulk soil and the rhizosphere of symptomless plants. These unknown factors could in part be opines secreted by plants with asymptomatic lesions or cryptic tumors. The discovery of the opine deoxy-fructosyl-glutamine (4, 33), which is a naturally occurring compound in wounded plant material (10), supports this hypothesis. On the other hand, other compounds of plant origin might be responsible for the selection of particular bacterial cells harboring or not harboring Ti plasmids. As a matter of fact, the related bacterium Rhizobium meliloti is selected at the root system of nonhost, nonlegume plants, such as hedge bindweed or belladona, because they efficiently degrade some alkaloid compounds synthesized by these plants (32).
The pathogenic population of Beni Tamou evolved between 1990 and 1994. Both octopine- and nopaline-type Ti plasmids were found in 1990, while only nopaline-type Ti plasmids were recovered in 1994, suggesting that the nopaline-type Ti plasmid itself provided better survivability to pathogenic agrobacteria in that soil. However, a correlative association was found between chromosomes and Ti plasmids in 1990 (2). Thus, the survival capacity of pathogenic strains could be determined by the associated chromosome as well. The particular host strain that harbored an octopine-type Ti plasmid in 1990 disappeared or dropped below the limit of detection in 1994, while those harboring a nopaline-type Ti plasmid survived better in that plot. The correlative association was, however, disrupted later, since only biovar 1 was found in 1990, while the prevalent nopaline-type Ti plasmid was found to be equally distributed in biovars 1 and 2 in 1994. An explanation could be that pathogenic biovar 2 was present with Ti plasmid in 1990, but in low numbers and was therefore not detected. For some reason, biovar 2 became more competitive and was then detected in 1994. Alternatively, nopaline-type Ti plasmids could have spread from biovar 1 to biovar 2. The spread of a Ti plasmid among various strains or species is thought to result from conjugal events. However, the conjugation of Ti plasmids is strongly repressed in the absence of the so-called conjugal opines (10). Here again, the evolution of the pathogenic population suggests that an effect normally mediated by opines could occur in a plot apparently bearing only symptomless plants and no opines. Whatever its cause, the shift of pathogenic populations from biovar 1 to biovar 2 suggests a selection in favor of biovar 2. Considering this fact, it is relevant to note that the Ti plasmid-free agrobacteria from that plot are predominantly biovar 2. Assuming that the Ti plasmid-free strains are the former indigenous agrobacteria of that soil, it is thus likely that the pathogenic population showed a shift toward the most adapted biovar of that soil, through a process of "naturalization" of a Ti plasmid in indigenous agrobacterial populations of the conducive soil.
Overall, the survival of Ti plasmid-harboring strains appeared to be the result of an equilibrium between the genetic load on the one hand and the fitness improvement determined by the Ti plasmid and/or the favorable association between Ti plasmid and particular chromosome on the other, this equilibrium being finely tuned by environmental conditions.
| ACKNOWLEDGMENTS |
|---|
This research was supported by funds from EU contract ERBIC18CT970198 "Integrated control of crown gall in Mediterranean countries."
| FOOTNOTES |
|---|
| REFERENCES |
|---|
|
|
|---|
This article has been cited by other articles:
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| J. Bacteriol. | Microbiol. Mol. Biol. Rev. | Eukaryot. Cell | All ASM Journals |
|---|