Abstract
Complexities of biotic-abiotic interactions in soils result in the lack of integrated understanding of environmental variables that restrict the survival of shiga toxin-producing E. coli O157:H7. Herein, we reanalyzed previously published data and highlighted the influence of soil abiotic factors on E. coli O157:H7 survivability and elucidated how these factors took effect indirectly through affecting indigenous bacterial community. Interaction network analysis indicated salinity and pH decreased the relative abundances of some bacterial taxa (e.g., Acidobacteria_Gp4, Acidobacteria_Gp6, and Deltaproteobacteria) which were positively correlated with the survival of E. coli O157:H7 in soils, and vice versa (e.g., Gammaproteobacteria and Flavobacteria) (P < 0.05). An array of multivariate statistical approaches including partial Mantel test, variation partition analysis (VPA), and structural equation model (SEM) further confirmed that biotic and abiotic factors interactively shaped the survival profile of E. coli O157:H7. This study revealed that some bacterial taxa were correlated with survival of E. coli O157:H7 directly, and salinity and pH could affect E. coli O157:H7 survival through changing these bacterial taxa. These findings suggest that salinity in soil might benefit the control of fecal pathogenic E. coli invasion, while soil acidification caused by anthropogenic influences could potentially increase the persistence of E. coli O157:H7 in agro-ecosystem.
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Introduction
Shiga toxin-producing Escherichia coli O157:H7 could be dangerous because of its low infective threshold (as few as 10-50 cells) and high pathogenicity (even death) (Ritchie et al. 2003), and thus, its transmission attracts great attention (Franz et al. 2018). Fresh fruit and vegetables served as vehicles for transmission of E. coli O157:H7 (Berger et al. 2010; Turner et al. 2019), because they could harbor pathogens on their surfaces or internalize pathogens during their growth (Kumar et al. 2017; Teplitski and de Moraes 2018). During the transmission process from manure to human, agricultural soils are a vital reservoir for the enteric pathogens because of the application of poorly composted manures and contaminated irrigation water (Berger et al. 2010; van Elsas et al. 2011). Infection probability of fresh produce depended on the survival time and physiological activity of E. coli cells in soils (Ongeng et al. 2015). Thus, a comprehensive understanding of the retention of E. coli O157:H7 in agricultural soils was critical to optimize agricultural management strategies and public health policies.
Study of the factors affecting E. coli O157:H7 survival was one of the core issues to understand the fate of pathogenic E. coli in the environment (Ongeng et al. 2015; van Elsas et al. 2011). Numerous studies have investigated the relationships between the survivals of E. coli O157:H7 in soils and environmental factors. From the abiotic factors perspective, nutrient availability generally had positive effects on E. coli O157:H7, due to the chemoheterotrophic nature of E. coli. It was found that dissolved organic carbon was one of the major determinants promoting the survival of E. coli O157:H7 in manure-amended soil (Franz et al. 2008). Furthermore, soil pH (Balamurugan et al. 2015; Xing et al. 2019), moisture (Ongeng et al. 2011), and texture (Cai et al. 2018) were also correlated to the E. coli O157:H7 survivability. From the biotic factors perspective, indigenous bacterial community constrained the survival and colonization of E. coli O157:H7 in soils (Mallon et al. 2015b; van Elsas et al. 2012). A possible reason for this phenomenon was that robust diversity increased resource competition and decreased invasion by niche preemption (Mallon et al. 2015a). In addition, agriculture management practices (Franz et al. 2008; Yao et al. 2013, 2015) and global climate change (Hellberg and Chu 2015) were also potential contributors to decline the concentration of E. coli in soils, which took effects mainly through changing soil abiotic and/or biotic variables. Undoubtedly, physicochemical properties and microbial community of soil were interactively correlated instead of working alone (Bahram et al. 2018), but how these complex interactions among biotic-abiotic factors of soils link to the persistence of invasive E. coli O157:H7 were not examined before. It was of importance to integrate the abiotic and biotic variables to obtain a full understanding of the survival mechanism of E. coli O157:H7 in soils.
Our previous studies have profiled the correlations between survival parameters of E. coli O157:H7 and soil physicochemical properties (electrical conductivity or salinity, pH, water soluble organic carbon (WSOC) and total soluble nitrogen (TN), etc.), and noticed salinity and pH showed deleterious effects on E. coli invasion (Ma et al. 2012a). We also have found that survival parameters were linearly correlated to relative abundance of major bacterial phyla, e.g., Actinobacteria, Acidobacteria, Proteobacteria, and Bacteroidetes (Ma et al. 2013). Obviously, these finding still could not answer the question that how the interactions between soil properties and bacterial community influence the survival of E. coli O157:H7 in soils.
In this study, we reanalyzed survival data of E. coli O157:H7 EDL933, high-throughput sequencing data of soil indigenous bacterial community and soil properties of 32 vegetable producing soils. These soils were collected from three major leafy green producing areas in the USA: Salinas Valley of northern California (SA), Imperial Valley of southern California (IM), and Yuma Valley of Arizona (AZ). An array of statistical analytical tools including correlation analysis, random forest model, Mantel test, interaction network analysis, variation partition analysis (VPA), and structural equation model (SEM) was selected for data mining. The objectives of this study were to (1) disentangle how salinity and pH indirectly constrain E. coli O157:H7 survivability through shaping indigenous bacterial community and (2) quantify the individual and joint contributions of physicochemical properties and bacterial community to survival of E. coli O157:H7 in soils.
Materials and methods
Soil collection, characterization, DNA extraction, and sequencing
A total of 32 soil samples were collected from three major leafy green producing areas: Salinas Valley, northern California; Imperial Valley, southern California; and Yuma Valley, Arizona. The geographical location and environmental parameters were previously described by Ma et al. (2012b). Soil collection, pretreatment, and physicochemical properties characterization (including salinity (EC, dS m-1), water soluble organic carbon (WSOC, mg kg-1), total soluble nitrogen (TN, %), and pH) can be found in the study of Ma et al. (2012a). Soil DNA extraction, high-throughput sequencing, and sequence data processing can be found in the study of Ma et al. (2013). In brief, bacterial tag-encoded FLX amplicon pyrosequencing was carried out, and sequences that were < 200 bp after quality trimming were removed. Sequencing data were further analyzed using MOTHUR v1.9.1. The sequencing data could be downloaded in https://www.ars.usda.gov/ARSUSERFILES/20361500/PUBLIC%20DATA/SALINITY%20PRODUCE%20SEQUENCING%20DATA%202010-2015.ZIP.
Survival of E. coli O157:H7 EDL933 in soils and survival data modeling
Survival experiments have been reported previously (Ma et al. 2012a, 2013). In brief, an E. coli O157:H7 strain EDL933 (ATCC 43895) wild type was tagged with nalidixic acid in addition to rifampicin resistance to facilitate the enumeration; its growth in LB (Luria−Bertani) broth and survival in soils were found to be identical to that of the non-tagged wild-type strain (Ma et al. 2011). Cells were added in soils to a final density of about 5 × 106 CFU per gram soil dry weight (gdw−1) (Franz et al. 2008). All experiments were performed under room temperature (22 ± 1 °C), and moisture content was maintained constantly by adding more water to make up for evaporation according to non-inoculated control (Ma et al. 2013). The inoculated soils were sampled at days 0, 3, 6, 10, 14, 20, 27, 34, 40, and 48, and survivors of E. coli O157:H7 over time were counted (Ma et al. 2011). The measured data were fitted to the Weibull survival model (Albert and Mafart 2005) using GInaFiT version 1.5 (Geeraerd et al. 2005), and survival parameters including ttd (time needed to reach detection limit of 100 CFU gdw−1), δ (time needed for first decimal reduction), and p (shape parameter) were calculated at the same time (Franz et al. 2008). More details on survival data modeling could be found in the Method part in Supplementary Information.
Statistical analysis
Pearson correlation analysis, permutational MANOVA (PERMANOVA) with Bray-Curtis dissimilarity of OTU table, and detrended corresponding analysis (DCA) with Bray-Curtis dissimilarity of OTU table were performed using vegan package (Dixon 2003) in R 3.3.3. The first coordinate of DCA (DCA1) of bacterial community explained 37.9% of the overall variation (Fig. S1d).
Mantel test could be used to calculate correlations between corresponding positions of two distance matrices derived from multivariate data with significance test by permutation (Mantel 1967). Partial Mantel test is an extension of Mantel test, where the influence of third matrix is controlled while the relationship of the first two is determined (Smouse et al. 1986). In other words, partial Mantel test attempts to correct for the effect of another series of variables stored in an additional matrix or matrices (Buttigieg and Ramette 2014). When considering a set of explanatory variables, partial Mantel test excluded the influence of other factors when calculating one factor’s effect. Mantel test and partial Mantel test were performed with vegan package (Dixon 2003) in R 3.3.3.
Redundancy analysis (RDA) was used to extract and summarize the variation of response variables (i.e., E. coli O157:H7 survival parameters) that can be explained by a series of explanatory variables (i.e., soil properties and microbial community) (Buttigieg and Ramette 2014). Then, variation partition analysis (VPA) was performed to determine the partial effect of each explanatory matrix on the response data (Borcard et al. 1992), and its result was displayed in a Venn diagram. The shared partitions in VPA results meant the variation in response data could be explained by both explanatory matrices (Peres-Neto et al. 2006). A larger partition fraction means a more multicollinearity effect in the model. Thus, a larger shared partition indicates the complex interactions among explanatory variables. RDA and VPA were performed with vegan package (Dixon 2003) in R 3.3.3.
Random forest is an ensemble of unpruned regression or classification trees created using bootstrap samples of the training data and random feature selection in tree induction (Breiman 2001). Here, it was performed to quantitatively assess the important predictors to survival parameters (ttd, δ, and p) of E. coli O157:H7. The importance of each predictor was determined by assessing the decrease in prediction accuracy, i.e., increase in the mean square error (MSE) between observations and predictions, when the data for the predictor was randomly permuted (Breiman 2001). This decrease was averaged over all trees to produce the final measurement of importance. This accuracy of importance measure was calculated for each tree and averaged over the forest. These analyses were conducted using the randomForest package (Liaw and Wiener 2002), and the significance of predictor importance on the survival parameters was assessed by using the rfPermute package (Archer 2013) in R 3.3.3.
To visualize the associations among survival parameters (ttd, δ, and p) of E. coli O157:H7, soil physicochemical properties, and bacteria in the interaction network interface, a correlation matrix was constructed based on the possible pairwise Pearson’s rank correlations. The distribution matrix of bacteria was standardized based on their relative abundance for network construction (Barberán et al. 2011). To reduce network complexity, all connections within bacterial groups were deleted. A valid co-occurrence was considered a statistically significant correlation between species with the Pearson’s P value < 0.05. Network analysis was performed using the iGraph (Csardi and Nepusz 2006) and Hmisc (Harrell and Frank 2008) packages in R 3.3.3. The interaction network was visualized using Gephi 0.9.2 (Bastian et al. 2009).
Structural equation model (SEM) is an a priori method with the capacity to identify casual relationships between variables by fitting data to the models representing causal hypotheses (Byrne 2001; Eisenhauer et al. 2015). Here, SEM was used to gain a mechanistic understanding of how soil physicochemical properties and bacterial community influence survival of E. coli O157:H7, and direct and indirect standardized path coefficients (λ) of soil properties and bacterial community were calculated. Here, “direct” was defined as the link between an explanatory variable and a response variable, while “indirect” indicated an explanatory variable influenced another explanatory variable, and the latter directly influenced the response variable. The “total effect” was the combination of direct effect and indirect effect. This analysis was performed with lavaan package using the robust maximum likelihood estimation method (Rosseel 2012) in R 3.3.3. The χ2 value and its associated P value, ratio of χ2 and degrees of freedom (CMIN/DF), goodness-of-fit index (GFI), root mean square error of approximation (RMSEA), and Akaike information criterion (AIC) were used to judge the model fitness to the data. Concretely, these multiple goodness-of-fit criteria are as follows: P > 0.05, CMIN/DF < 2, GFI > 0.90, RMSEA < 0.08, and the AIC from the default model lower than that from saturated model and independence model (Hooper et al. 2008; Schermelleh-Engel et al. 2003).
Results
Survival of E. coli O157:H7 in soils and its influential factors
Based on Weibull model, the survival of E. coli O157:H7 was quantified by model parameters including ttd (time needed to reach detection limit of 100 CFU gdw−1), δ (time needed for first decimal reduction), and p (shape parameter). E. coli O157:H7 survived longer in soils from Salinas Valley, California (SA, ttd = 29.55 ± 3.01 days, δ = 11.90 ± 2.80 days) than Imperial Valley, California (IM, ttd = 18.83 ± 3.53 days, δ = 6.14 ± 2.22 days) and Yuma Valley, Arizona (AZ, ttd = 21.15 ± 6.74 days, δ = 4.43 ± 1.37 days) (P < 0.001) (Fig. S1). Meanwhile, salinity and pH in SA were significantly lower than in soils from Imperial Valley and Yuma (P < 0.05); bacterial community in SA soil was also different compared with Imperial and Yuma soils (P < 0.001, PERMANOVA) (Figs. S1 and S2).
Bacterial community, salinity, pH, WSOC, and TN were used to explain survival parameters (ttd, δ, and p) based on random forest model, and 59.52% variation of ttd, 62.11% variation of δ, and 37.82% variation of p could be explained by abovementioned variables (Table 1). In random forest model, the bigger mean square error (MSE) value means the greater influence of observations on predictions. For instance, the MSE of ttd increased 11.94% when removing the predictor of bacterial community (P < 0.01) and increased 12.99% when removing the predictor of salinity (P < 0.01) (Table 1). In addition, Mantel test also correlated environmental factors and survival parameters (Table 2). For instance, ttd was significantly correlated with bacterial community (r = 0.391, P < 0.001), salinity (r = 0.444, P < 0.001), and pH (r = 0.220, P < 0.05) by Mantel test. The results of random forest model and Mantel test confirmed the results of the correlation analysis (Table S1).
Interaction network among survival parameters, soil properties, and bacteria
To explore the specific Pearson correlations among survival parameters (ttd, δ, and p) of E. coli O157:H7, soil physicochemical properties, and major bacterial groups (at class level), interaction network was depicted (Fig. 1). An edge represented a significant (P < 0.05) correlation, and more details were shown in Table S2. Soil physicochemical properties were associated with few bacterial groups, and these groups were further associated with survival parameters (Fig. 1), which were indicated as green edges (i.e., survival parameters) and pink edges (i.e., physicochemical properties) linking blue nodes (i.e., bacterial groups) at the same times. A total of six major bacterial groups at class level whose relative abundance > 1%, including Gammaproteobacteria, Solirubrobacterales, Acidobacteria_Gp6, Deltaproteobacteria, Acidobacteria_Gp4, and Flavobacteria, had significant correlation with both soil physicochemical properties and survival parameters (Fig. 1, Table 3). Salinity and pH were negatively correlated with Acidobacteria_Gp4, Acidobacteria_Gp6, and Deltaproteobacteria, and these taxa were positively correlated with ttd. Salinity and pH were positively correlated with Gammaproteobacteria and Flavobacteria, and these taxa were negatively correlated with ttd (P < 0.05, Table 3). Similar trends were found in the influencing factors of δ and p. In addition, WSOC and TN were positively correlated with Solirubrobacterales, which was positively correlated with ttd (P < 0.05, Table 3). The interaction network showed that the bacterial community was associated with soil properties and survival parameters at the same time.
Correlation analysis between accumulated bacterial abundance at class level and survival parameters
Based on results of network analysis, plenty of bacterial taxa were found to be positively or negatively correlated with the survival parameters of E. coli. It was also interesting to explore the links between survival parameters and cumulative relative abundance of class who were correlated with survival parameters. Concretely, the sums of relative abundance of classes who were positive with ttd, negative with ttd, positive with δ, and positive with p (P < 0.05) were calculated. Corresponding accumulated bacterial class abundance significantly correlated with survival parameters of E. coli O157 (P < 0.05, Fig. 2). In addition, similar phenomena were found between accumulated bacterial class abundance and soil physicochemical properties (P < 0.05, Fig. S3).
Redundancy analysis between environmental factors and survival profile
Redundancy analysis (RDA) and further variation partition analysis (VPA) were used to calculate the proportional contribution of environmental factors to E. coli O157 survival variation. Results of RDA and VPA indicated that selected environmental factors explained over 67% of the total variation of survival profile of E. coli O157 (Fig. 3). In VPA, all variables were divided into three groups including biotic factor (bacterial community), negative abiotic factors of survival (salinity and pH), and positive abiotic factors of survival (WSOC and TN). Notably, bacterial community alone and negative abiotic factors alone contributed only 3.32%, 7.92% to overall variation of survival profile, respectively, while the joint contribution of bacterial community and negative abiotic factors to overall variation of survival profile was 30.49% (Fig. 3). Similarly, the joint effect of bacterial community and positive abiotic factors was greater than the effect of bacterial community alone (5.39% > 3.32%). Overall, the joint effect of all biotic and abiotic variables contributed 49.15% (30.49% + 13.27% + 5.39%) to the variation of survival profile, while biotic variables and abiotic variables alone contributed 3.32% and 15.20% (7.92% + 1.14% + 6.14%) to the variation of survival profile, respectively. The VPA results indicated the effect of bacterial community on the survival of E. coli O157:H7 was mainly reflected in the joint effects with abiotic variables. In addition, the unmeasured soil variables (e.g., unmeasured physicochemical properties, bacteriophage) might contribute to the unexplained part (32.32%) in VPA.
Indirect and direct effects of soil properties and bacteria on survival parameters
To obtain deeper understanding of the “joint effect” of biotic and abiotic factors revealed by VPA, partial Mantel test and structural equation model (SEM) were performed. The correlation coefficient (r) of partial Mantel test was generally smaller than that of Mantel test (Table 2), indicating the actual effect of one environmental variable was corrected when controlling the effects of other variables. For instance, the correlation coefficient between ttd and salinity was 0.444 (P < 0.001) by Mantel test and 0.377 (P < 0.01) by partial Mantel test, indicating partial influence of salinity reflected by other environmental factors (i.e., bacterial community). The correlation coefficient between ttd and pH was 0.220 (P < 0.05) by Mantel test and − 0.009 (P > 0.05) by partial Mantel test, indicating almost all influence of pH reflected by other environmental factors (i.e., bacterial community). In short, these tests suggest the survival of E. coli O157:H7 was interactively influenced by biotic and abiotic factors.
Based on structural equation model (SEM), the interactions among environmental variables were quantitatively depicted as the indirect and direct effects of soil properties and bacterial community on survival parameters (Fig. 4). Salinity, pH, and TN had indirect links to ttd, δ, and p through bacterial community. Concretely, salinity and pH showed negative effects on survival parameters, while TN showed positive effects (Fig. 4). The deleterious effect of salinity on ttd was the combination of direct effect and indirect effect through bacterial community, while the deleterious effect of pH on ttd was only obtained as indirect pathway. A similar trend was found in the deleterious effect of salinity and pH on δ and p. The SEM results clearly showed the indirect and direct effects of soil properties and bacteria on survival parameters of E. coli O157:H7. Notably, the R2 value of p was smaller than that of ttd and δ, indicating p was shaped by more unmeasured variables.
Discussion
Based on multivariate statistical methods, this study systematically disentangled the direct and indirect effects of soil biotic and abiotic factors on the survival profile of E. coli O157:H7, and highlighted salinity and pH constrained the survival of E. coli O157:H7 through changing indigenous bacterial community. To the best of our knowledge, this study may be the first to reveal the deleterious influence of high soil salinity and pH on E. coli O157:H7 through biotic-abiotic interaction perspective. The longer survival of E. coli O157:H7 in Salinas Valley, California, in comparison with others might be shaped by plenty of factors, and the lower salinity, lower pH, and distinct indigenous bacterial community in Salinas Valley, California, might make sense (Fig. S1). In fact, although the three sampling sites of this study were all major fresh produce growing areas in the USA, some outbreaks of this pathogen caused by fresh produce have been traced back to Salinas Valley, California, instead of Imperial Valley, California, or Yuma Valley, Arizona, (Cooley et al. 2007). It was meaningful to disentangle the adverse effects of high salinity and pH on E. coli O157:H7 for further agriculture management strategies.
Previous studies have noticed the sublethal effects of salt on E. coli (Anderson et al. 1979), and the adverse effects of salinity on E. coli cells might include a general osmotic effect and specific ion toxicity, causing decrease of enzymatic activities in metabolic process (Shabala et al. 2009). The rpoS gene was critical for E. coli to acquire resistance to multiple-stress, e.g., salinity, and the regulation of rpoS gene expression was useful for the understanding of E. coli O157:H7 survival mechanisms (Munro et al. 1995).
In addition, our data showed Acidobacteria and Deltaproteobacteria positively correlated with the survival of E. coli O157:H7, while Gammaproteobacteria and Flavobacteria were negatively correlated with the survival of E. coli O157:H7 (Fig. 1, Table 3). Acidobacteria and Deltaproteobacteria could promote carbon turnover by depleting the low molecular weight of carbon sources for E. coli to use easily (Eichorst et al. 2011; Westphal et al. 2011), which might be the possible reason of their positive correlations with ttd. As a member of Gammaproteobacteria, E. coli O157:H7 shared similar ecological niche with indigenous Gammaproteobacteria, and abundant Gammaproteobacteria in soils might restrain the colonization of invasive E. coli. As a major class of Bacteroidetes, Flavobacteria showed suppressive effect on the survival of E. coli O157:H7 in sand-based dairy livestock bedding (Westphal et al. 2011), which was in line with our data. Interestingly, salinity increased the abundance of Gammaproteobacteria and Flavobacteria while decreased the abundance of Acidobacteria and Deltaproteobacteria. In other words, salinity increased the bacteria negatively correlated to E. coli O157:H7, while decreased bacteria beneficial for E. coli O157:H7. Such indirect influence was shown in specific correlations among soil properties, bacterial taxa, and survival parameters, and was also proved by multivariate statistical methods (Table 2, Figs. 3 and 4).
Because of the exposure of E. coli O157:H7 to acidic pH in the gastrointestinal tract of animals, this pathogen seems to have developed molecular mechanisms to resist acid stress (Lin et al. 1996). Plenty of studies have also noticed the shorter survival time in alkaline pH than in acidic pH (Balamurugan et al. 2015; Franz et al. 2005; Wang et al. 2014; Xing et al. 2019; Yao et al. 2015). As mentioned previously, Acidobacteria was helpful for E. coli O157:H7 to survive in soils (Eichorst et al. 2011). Notably, our data revealed higher pH decreased the abundance of Acidobacteria_Gp4, which was positive correlated with survival time of E. coli (Fig. 1, Table 3). Thus, the adverse effect of high pH on E. coli seems to be the combination of direct stress and decrement of beneficial bacterial taxa for this pathogen, e.g., Acidobacteria. In addition, WSOC and TN increased the abundance of Solirubrobacterales and Deltaproteobacteria, which were beneficial for E. coli O157:H7 (Fig. 1, Table 3).
In the current study, multiple statistical methods were used, and each method had its goal. Firstly, correlation analysis, Mantel test, and random forest were used to explore the impact of environmental factors on E. coli O157 survival in soil. Secondly, network analysis could provide detailed information on the correlation between bacterial taxa and survival parameters of E. coli O157. Thirdly, both biotic and abiotic variables were considered at the same time in redundancy analysis (RDA) and further variation partition analysis (VPA), and their proportional contributions to variation of E. coli O157 survival were explored; VPA also indicated the importance of interactions among biotic and abiotic factors shaping E. coli O157 survival. Finally, partial Mantel test and structural equation model (SEM) were used to disentangle abovementioned “interaction,” and direct and indirect influence of environmental factors on E. coli O157 survival were obtained. These multivariate statistical approaches have been applied in research on microbial ecology, but some of them might be used for E. coli survival data for the first time. Liang et al. (2015) explored the relationship between temperature and microbial community structure controlling for plant and soil variables by partial Mantel test. Zhu et al. (2017) used VPA to differentiate the effects of environmental factors on ARG structures in Chinese estuary samples. The current study attempted to extend the use of those methods on data mining for E. coli survival dynamic as indicated in a recent study (Huang et al. 2020).
As a biological pollutant, invasive E. coli O157:H7 undoubtedly interacts with biotic variables in soils, as evidenced that indigenous microbial composition (Yao et al. 2014), biodiversity (van Elsas et al. 2012), niche breadth (Mallon et al. 2015a), and fitness difference (Li et al. 2019) showed close linkages to the survival of E. coli O157:H7. In this study, biotic and abiotic factors of soils were integrated using multivariate statistical methods to explore the effects of the interactions of complex environmental factors on E. coli O157:H7. The VPA results indicated the influence of bacterial community was interaction with soil properties (49.15%) rather than individual contribution (3.32%) (Fig. 3), and SEM results showed salinity restricted the survival of E. coli O157:H7 directly and indirectly, and pH restriction was mainly indirect (Fig. 4). The influence of bacterial community on the survival of E. coli O157:H7 might be influenced by the soil physicochemical properties as indicated in a recent study.
Disentangling the survival of E. coli O157:H7 was useful to establish its control strategies. Recently, plasma-activated water, a promising alternative of traditional sanitizer, was used to decontaminate fresh produce polluted by pathogens (Ma et al. 2015). Clay was used as an additive in manure compost to shorten the survival of pathogenic bacteria (Awasthi et al. 2019). Our results indicated that appropriate salinity in soil might be beneficial for the control of E. coli O157:H7, while soil acidification caused by anthropogenic influences could potentially increase the persistence of E. coli O157:H7 in preharvest environment. The interactions among biotic and abiotic factors controlling the E. coli O157:H7 survival were highlighted, and more verification experiments and in situ experiments in future must be done to further explore the interaction mechanisms between biotic and abiotic factors in survival studies, as well as practical E. coli O157:H7 control protocols.
Conclusions
This research revealed that salinity and pH decreased the survival time of E. coli O157:H7 in soils through changing indigenous bacterial community to a more adverse state for the survival. The interactions between soil properties and bacterial community explained more variation of E. coli O157:H7 survival than soil properties or bacterial community alone, indicating the integration of biotic and abiotic factors in understanding the survival profile of invasive pathogenic E. coli. In practice, appropriate soil salinity and controlled soil acidification might be meaningful approaches to restrict E. coli O157:H7 in agro-ecosystem.
Data availability
The sequencing data could be downloaded in https://www.ars.usda.gov/ARSUSERFILES/20361500/PUBLIC%20DATA/SALINITY%20PRODUCE%20SEQUENCING%20DATA%202010-2015.ZIP.
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Acknowledgments
We thank Drs. Jorge Fonseca of the University of Arizona Yuma, Mark Trent, UC-Davis, Imperial Agricultural Experiment Station, and James McCreight of USDA-ARS Salinas, CA for providing soil samples for this study. We also thank Damon Baptista for technical help and Qiuting Zhang for statistical analysis.
Funding
This research was financed by the National Natural Science Foundation of China (no. 41571304), CSREES NIFA Agreement 2008-35201-18709, and the 206 Manure and Byproduct Utilization Project of the USDA-ARS.
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Ziming Han: conceptualization, methodology, formal analysis, and writing—original draft preparation; Jincai Ma: methodology, conceptualization, supervision, funding acquisition, and writing—reviewing and editing; Abasiofiok Mark Ibekwe: project administration, funding acquisition, resources, and writing—reviewing and editing; Ching-Hong Yang: methodology and writing—reviewing and editing. All authors read and approved the final manuscript.
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Additional experimental methodology showed survival experiment of E. coli O157:H7 in soils and survival data modeling; additional tables related to correlation analysis among survival parameters, physicochemical properties, and bacterial groups; additional figures were comparisons of survival parameters, salinity, pH, and bacterial community among different sampling sites, concentrations of Na+, K+, Ca2+, and Mg2+ in soil water extracts, and the relationships between soil physicochemical properties and accumulated bacterial class abundance. (DOCX 3.86 MB)
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Han, Z., Ma, J., Yang, CH. et al. Soil salinity, pH, and indigenous bacterial community interactively influence the survival of E. coli O157:H7 revealed by multivariate statistics. Environ Sci Pollut Res 28, 5575–5586 (2021). https://doi.org/10.1007/s11356-020-10942-6
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DOI: https://doi.org/10.1007/s11356-020-10942-6