Abstract
Aim
Cadmium mitigation in crops is a worldwide concern. Selenium application has been suggested as a potential solution to reduce cadmium concentration in plants, but published results were contradictory. We analysed literature data with respect to the effect of selenium addition on cadmium uptake and elucidated processes possibly involved.
Method
A meta-analysis was performed on data collected from previously published studies presenting cadmium concentration in plants subjected to selenium treatments. Metaregression random models were run to test the impact of different factors. In addition, soil and crop inventory data exemplifying the natural variation of Cd and Se in soil were evaluated.
Results
The results highlighted a significant reduction of cadmium concentration in crops after selenium addition. The reduction was dose-dependent for crops growing under aerobic, but not for plants cultivated under anoxic conditions such as rice. This suggests that different process can be involved.
Conclusion
We demonstrated the potential of selenium fertilization to mitigate cadmium uptake and highlighted that for non-rice species, the main process seems to take place in the soil, while mechanisms in roots restricting uptake may be involved for all crops. The inventory data also indicated an impact of natural soil Se on Cd contents in crops.
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Introduction
Cadmium is classified as a human carcinogen (IARC 1993) and dietary intake is considered a health risk that may cause kidney failure, bone demineralization and increased risk of cancer in the lung, endometrium, bladder, and breast (EFSA 2009). As a consequence, tolerable dietary intake of Cd was reduced by 65% from 7.5 to 2.5 μg kg−1 body weight and week (EFSA 2017). The restrictive standard for dietary Cd intake requires strategies to minimize uptake of Cd by crops but few are available: identification of fields with high Cd contents, liming of acid Cd-rich soils (Rizwan et al. 2016) and use of Cd-rich crops exclusively for fodder (Söderström and Eriksson 2013). A further measure proposed is application of selenium compounds (Se) to soil in order to reduce Cd uptake by crops being the focus of this paper.
Selenium was identified as an essential element for mammals in the 1950s (Schwarz and Foltz 1957). Selenium deficiency was shown to increase the risk of cardiovascular diseases (Salonen et al. 1982). A newly revised recommendation by EFSA (2014) proposed a higher daily dietary Se intake, 70 instead of 50–60 μg Se per person. Today, it is estimated that hundreds of millions of people have an inadequate dietary intake of Se (Combs 2001; Jones et al. 2017). The reason for low Se concentrations in food are low or very low Se concentrations in most parent materials rarely exceeding 0.1 mg kg−1soil (Fordyce 2007). Diets rich in Se have shown to protect animals against Cd-toxicity (Zwolak and Zaporowska 2012). Crops and cereals in particular are a major Se source in diets (Rayman 2012).
Fertilizing crops with Se with the aim to decrease Cd uptake by crops could be a win-win situation: i) increasing Se in the diet and limiting Se deficiency, and ii) reducing Cd concentrations in crops and thereby dietary Cd intake and possible toxic effects of Cd in the body.
In this paper, existing literature about possible interactions between Se application and Cd uptake in the soil-crop-system was analyzed. So far, around 50 articles have been published related to the effect of Se application on Cd uptake by plants. However, large differences between experimental conditions provided highly variable and sometimes contradictory results. In order to gain a more conclusive answer, we extracted data from these studies for a meta-analysis. We aimed to i) verify if there are significant interactions between Cd uptake and Se application in crops, ii) analyse to what extend Se can affect Cd concentrations in crops and iii) elucidate if the data support mechanisms proposed in the literature.
Material and methods
Literature data sourcing and extraction
An extensive analysis of the literature from 1970 to 2019 was used to identify studies that measured the effect of Se addition on Cd absorption by plants. The literature research was performed on Web of Science and Google Scholar using the following keywords: selenium, cadmium, plants, crops and interactions. In addition, the reference section of each paper identified in the search was scanned for additional, undetected, relevant papers. Both hydroponic and pot experiments were considered. Data of Cd concentration in the plants parts were extracted from tables and graphs using the online freeware WebPlotDigitizer and compiled (Supplementary Material 1). When Cd concentrations in plants could not be extracted, for instance only 3D graphs were given, and/or standard error or standard deviation was not reported, data were excluded. Total concentrations of Cd (natural + exogenous) but only Se concentration achieved by exogenous input of Se were used in the analysis. When Cd and Se concentrations could not be converted into μmol kg−1 of growth medium or soil, data were excluded. Hence, field studies and foliar application studies were not included. We partitioned the data into data subsets in order to make distinction between Se effect on the plant species, “rice only” and “rice excluded” data, plant organs roots and shoots, and Se species added, selenite (SeO3) or selenate (SeO4). Both plant organs and Se species subsets were again divided into “rice only” and “rice excluded” data subsets. In total 11 subsets where considered for the meta-analysis: full dataset, “rice only”, “rice excluded”, roots of “rice only”, roots of “rice excluded”, shoots “rice only”, shoots of “rice excluded”, SeO3 added to “rice only”, SeO3 added to “rice excluded”, SeO4 added to “rice only” and SeO4 added to “rice excluded”.
Statistical analysis
We performed calculations and statistical analyses using the R open source software environment (version 3.5.0, R Core Team 2018) and functions available in the metafor package (version 2.0.0, Viechtbauer 2010). We used mean, standard deviation of Cd concentration, and sample size of treatments and the control (no Se added) to calculate a Response Ratio (log Response Ratio), used as effect size, and its variance. The response ratio is the log ratio of a control over a treatment calculated as (Hedges et al. 1999):
where Cdc is the concentration of Cd in the control plant and Cdt is the concentration of Cd in the treated plant.
The variance of RR was calculated with:
where \( {\sigma}_c^2 \), nc,\( {\overline{x}}_c^2 \) are, respectively, the square of standard deviation for the control, the control sample size and the square of the average Cdc and \( {\sigma}_t^2 \), nt,\( {\overline{x}}_t^2 \) are, respectively, the square of standard deviation for the treatment, the treatment sample size and the square of the average Cdt.
A higher response ratio means a lower Cd concentration in the treated plant and therefore a higher effect of Se treatment on Cd mitigation. The effect size of the response ratio was plotted against Se treatments to visualize the relative change of Cd accumulation through Se additions.
Using the restricted maximum likelihood estimation (REML) in the function rma.mv(), we ran a metaregression model with random effect, with the log of Se concentration as moderator. We included a hierarchical random effect using article and individual observations in each model. Pseudo-R2 were calculated by computing the proportional reduction in the total variance. We ran separate metaregression models that included a single moderator for datasets presenting ≥10 effect sizes calculated from ≥5 different articles.
The publication bias was tested by modifying the metaregression models to include the variance of the effect size as a moderator. We considered analysis to be biased if the estimate of the slope of the variance differed from zero at α = 0.1. The heterogeneity was assessed using the Q-statistic within the data sets.
The full dataset (Supplementary Material 2), R code and output (Supplementary Material 3) used are available as supplementary information.
Inventory data and analysis
In addition to the meta-analysis, inventory data from the national monitoring program of Swedish arable soils and crops running since the 1990s (Eriksson et al. 1997, 2000, 2010) were included to test the outlined hypothesis. Sampling has been done every 10 years at the same location. In this evaluation, 280 soil and winter wheat samples from the latest sampling series were used. From each sampling point, nine plough layer samples (0–20 cm depth) were randomly taken with an auger within a radius of 3 m, pooled, dried and sieved. From the same sampling area, four crop samples were taken using a frame of 0.25 m2. Cereal ears within each frame were cut with scissors, samples were pooled, dried, threshed for grains. For trace element analysis in soil and crop, samples were digested in 7 M HNO3 for 30 min and run on an ICP-SFMS. In this evaluation, total concentrations of Se and Cd were used.
As Se fertilization is not practiced in Sweden, only the impact of native Se in soil (natural Se variation) and its effect on Cd concentrations in grains was investigated. Total concentrations of Cd and Se in soils and crops were log-transformed to gain a normal distribution. Elemental concentrations in soil were transformed into a molar ratio of Se over Cd expressing the variation of Se relative to Cd in soil. Pearson correlations were conducted using the R open source software environment (version 3.5.0, R Core Team 2018) to determine the correlation coefficient and the significance of the correlation.
Results
Database and publication bias
Among the 51 articles (Supplementary Material 1) found presenting Cd concentration in plants with and without Se addition, 33 remained suitable for inclusion in our meta-analysis. From the articles retained, we calculated 325 effect sizes, which were separated into 11 datasets (Table 1). The experiments described in the articles were conducted on 16 different plant species and were published between 2008 and 2019. The range of Se added and Cd concentration in the growth media was between 1 and 600 μmol kg−1 growth media for Cd and 0.1 to 255 μmol kg−1 growth media for Se.
We detected publication bias in the dataset evaluating the effect of Se on Cd content of the roots of “rice only” (P = 0.0071). A significant amount of residual heterogeneity remained for all models (p < 0.01). All datasets, except the SeO4 for “rice only”, had a sufficient number of articles and outcomes (using a cut-off rule of ≥5 and ≥ 10 respectively) to explore the potential relationship between Se addition and Cd concentration reduction. Therefore, data subsets discriminating roots and selenate for “rice only” were not analysed.
Quantification of the effect of Se application on Cd content in plants
The full dataset covered a large range of Cd and Se concentration in the growth media. Results of the metaregression model for the full dataset are shown in Fig. 1a. A significant linear positive effect of log(Seadded) on the effect size was found. The effect size increased with Se addition indicating a dose dependent decrease of Cd concentrations in plants when Se was added to the growth media. The model intercept, corresponding to a zero-effect of added Se when log(Seadded) equals zero, or equivalently Seadded = 1. In the present case, the intercept showed that for an addition of 1 μmol Se kg−1 growth media, corresponding to 0.08 mg Se kg−1 of growth media, the expected effect size was 0.22 corresponding to a 19.7% Cd reduction in crops.
According to the model, the regression slope resembles the effect size of the increase of log(Seadded). The effect size increased by 0.063 per one unit of log(Seadded). Calculated pseudo-R2 values were low (0.03), highlighting a high variability of the data. Still, the significance of the model indicated that despite low fit to the model, a significant trend of the effect of Se addition on Cd reduction in plants was present. In concrete numbers, the model predicts a decrease of Cd concentration in crops of 10, 25 and 50% by the addition of 0.013, 0.082 and 142 mg Se kg−1 of growth media, respectively (Table 1).
Elucidation of possible mechanisms
In order to identify possible mechanisms causing the observed Se effect, subsets of data were extracted. In our case, data for redox conditions, speciation of Se and reduction of Cd concentration in roots and shoots were analysed in further detail.
Effect of soil redox conditions
In this subset, plants grown under anoxic conditions, “rice only”, were separated from plants grown under aerobic soil conditions, “rice excluded”, in order to highlight if Se acts differently under reducing and oxidizing conditions in the growth medium. However, only waterlogged pot experiments were considered for the “rice only” data (6 articles, 119 data points). There was no information given about the oxygen status of rice grown in hydroponic solutions and the data were excluded. In the pot experiments it was specified that rice was grown under flooded conditions, where the redox potential quickly drop under 0 mv and can reach −200 mV (Affholder et al. 2017). Results for “rice only” (low redox and anoxic conditions, Fig. 1b) showed no significant relationship between Se added and Cd reduction in plants. The model intercept of 0.26 was not significant showing that Se addition had no significant effect on the Cd reduction in rice grown under paddy conditions. Still, there was a tendency that Se also affected Cd in rice.
Results from the data subset excluding rice (aerobic soil conditions, Fig. 1c) showed a significant linear correlation between Se addition and the effect size and improved the fit of data (pseudo R2 = 0.12). An effect size of 0.075 per unit of log(Seadded) was found, i.e., addition of 0.06, 0.28 and 149 mg Se kg−1 growth media would reduce Cd concentration by 10, 25 and 50%, respectively (Table 1). The intercept was also significant, therefore for addition of 1 μmol Se kg−1 growth media, corresponding to 0.08 mg Se kg−1 of growth media, had an effect size of 0.12 equivalent to 12.1% reduction of Cd in crops.
Effect of selenium species added
The results of the model separating selenate (SeO42−) and selenite (SeO32−) additions on Cd uptake by crops, for the “rice excluded” dataset, are presented in Fig. 2. Data for “rice only” are not shown as the number of articles using SeO4 was insufficient (Table 1). Addition of selenate to crops excluding rice had no significant effect on the effect size, neither the intercept nor the slope of the model were significant (Fig. 2a). In contrary, selenite addition caused a significant linear response (Fig. 2b) with an increase of the effect size of 0.081 per unit of log(Seadded). Excluding the selenate data increased the fit of the “rice excluded” data to the model (pseudo-R2 = 0.16).
Effect of selenium on Cd content in roots and shoots
Figure 3 illustrates to what extent roots (Fig. 3a) and shoots (Fig. 3b) were affected by Se addition using the “rice excluded” dataset. Results for the “rice only” dataset were shown for shoots only (Fig. 3c) as there is a bias for the roots data subset (see 3.1. Database and publication bias). Crop data excluding rice showed a significant linear response of Se on Cd reduction in both roots and shoots with the best fit for roots (pseudo-R2 = 0.25) followed by shoots (pseudo-R2 = 0.19). The model predicted an increase of the effect size of 0.094 and 0.078 per unit of log(Seadded) for roots and shoots, respectively. Basically, 0.08, 0.27 and 40 mg Se kg−1 growth media reduced Cd by 10, 25 and 50% in roots and 0.08, 0.35 and 147 mg Se kg−1 growth media reduced Cd in shoots to the same extent (Table 1).
Shoot data of “rice only” were also significantly affected (pseudo R2 = 0.15) by Se addition (Fig. 3d). The model predicted an increase of the effect size of 0.14 per unit of log(Seadded), which means that addition of 0.12, 0.29 and 7.7 mg Se kg−1 growth media would reduce Cd by 10, 25 and 50% in rice shoots (Table 1).
Inventory analysis
In Swedish arable soils, concentrations of native Se and Cd were positively correlated (R = 0.43, P < 0.0001, Pearson’s correlation), Fig. 4a. Contents resembled the linked occurrence in sedimentary rocks from which soils were formed. Contamination of soils with Cd through P fertilizers (Roberts 2014) had a minor impact. Legacy Cd from P fertilization in soil was negligible as mineral P fertilizers low in Cd (< 1 mg Cd kg−1 P) have been used in Sweden since the end of the 80s. Considering that Se and Cd were natively associated in soil, relative variations between elements were obtained using molar ratios of Se over Cd. Plotting Cd concentrations in wheat grain against molar ratios showed a significant negative relationship (R = −0.22, P < 0.001, Pearson’s correlation), Fig. 4b. Again, this was interpreted as an indication for the possible reduction of Cd in crops even by native Se in soil.
Discussion
Results of the meta-analysis performed on the whole dataset (Fig. 1a) indicated a significant, dose dependent effect of Se on reduction of Cd concentration in plants. The relatively poor fits of the data to the model (pseudo-R2) were explained by the large difference in experimental conditions (different plant species and varieties, growing period, soils, etc.) of the 33 studies that matched the selection criteria. A low R2 is not invalidating the conclusion, but precision of predictions varied widely. Similarly, inventory data of Cd and Se concentrations in soil and wheat grains from samples all over Sweden (Fig. 4) supported the outcome of the meta-analysis. Higher concentration of native Se over native Cd in soil lowered concentrations of Cd in wheat grains. Although evidence of the effect of Se on Cd uptake by crops was shown, mechanisms are still not well understood. We outline potential mechanisms found in the literature (Fig. 5) that could be involved in Cd and Se interaction in soil and crop in the following discussion.
One reaction proposed is the formation of non-bioavailable cadmium selenide (CdSe) in soil first mentioned by Shanker et al. (1995). However, so far, no evidence for the formation of this compound in soil has been published. According to Gustafsson (2013), a non-bioavailable Cd-Se phase would only be stable at redox potentials lower than 100 mV, requiring reduction to elemental selenium and then to selenide (Fig. 5). Such reactions may occur under anoxic conditions in paddy soils, where redox potential values can drop up to −200 mV during flooding. However, such low redox potentials do not permanently exist in non-waterlogged arable top-soils (Husson 2013). By separating the data treating rice grown in flooded soil (“rice only”) separately from other species (“rice excluded”), we distinguished between low and high redox levels in soils. In case of non-bioavailable cadmium selenide being formed, a dose dependent decrease of plant available Cd would be expected. The results highlighted a dose dependent effect of Se on mitigation of Cd concentration for non-rice crop data (“rice excluded”). “Rice only” data showed a tendency of a positive effect but this was not significant. A wider range of Se additions to rice grown under anoxic conditions would be needed to confirm or reject this mechanism. However, knowing from the geochemistry of Se that selenide becomes a major species at low redox conditions and that selenide can substitute S in iron sulphide (Hatten Howard 1977), it was likely that iron selenide was formed whereby concentration of soluble selenium become very low (Masscheleyn et al. 1990). Iron bonding of Se in an environment with excess iron may explain why no dose dependent response of Se addition was observed in the “rice only” data. In addition, another iron-related mechanism, formation of iron plaques around roots of rice and wetland plants may also act as a barrier against uptake of Cu, Ni, Mn, and Cd (Taylor and Crowder 1983; Otte et al. 1989; Greipsson 1994; Ye et al. 1998; Wang and Peverly 1999). Recent studies suggested that the adsorption capacity of iron plaque around rice roots increased when Se was added, resulting in an increased sequestration of Cd (Huang et al. 2017) and Hg (Zhou and Li 2018). Thus, greater metal sequestration in iron plaques by Se may affect Cd absorption by roots and may explain the tendency observed of a non-dose dependent reduction of Cd. Unfortunately, there was no information available about the iron content of the soils in the studies.
For “rice excluded” data, a dose dependent effect of Cd mitigation was observed (Fig. 1c). suggesting involvement of non-mobile cadmium selenide. However, chemical reduction of selenate/selenite to elemental Se is thermodynamically only favoured under anaerobic conditions (Masscheleyn et al. 1990) but other mechanisms making Cd less bioavailable can be involved. Biological reduction through bacteria reducing selenate (Se(VI)) and selenite (Se(IV)) into elemental selenium (Se0) and selenide (Se(-II)) has been found (Nancharaiah and Lens 2015). Selenite was more easily reduced than selenate (Doran 1982). This would be consistent with observations presented in the literature showing that selenite was more effective to reduce Cd concentration in plants than selenate (Shanker et al. 1995, 1996; Zhou et al. 2017; Yu et al. 2018). However, we were unable to confirm these observations, which would have required a wider range of selenate concentrations.
Recently, microbial formation of CdSe quantum dots was shown (Kumar et al. 2007; Cui et al. 2009) and a Pseudomonas sp. strain showing this ability was isolated from soil samples (Ayano et al. 2014). Gomez Ojeda et al. (2013) suggested that Cd and Se can interact in plants and form a poorly soluble compounds, which could be CdSe quantum dots. More evidence that a Cd-Se interaction can be located in the plant was suggested by other studies showing a Cd reduction when Se was applied on leaves (Wang et al. 2013; Abd Allah et al. 2016; Liao et al. 2016; Ahmad et al. 2016; Chi et al. 2017) or roots were treated with Se before Cd exposure (Lin et al. 2012; Saidi et al. 2014; Mozafariyan et al. 2014).
Plants have several detoxification mechanisms. The main strategies used by plants to tolerate and minimize detrimental effects of high metal concentrations are to restrict uptake, limit translocation or detoxify through chelation and subcellular compartmentalization to avoid accumulation in the whole plant (Jan and Parray 2016). Root related mechanisms, which may contribute to the Cd reduction uptake, could be an enhanced development of apoplastic barriers in the endodermis of roots and a lower activity of the membrane transporters activity (Wang et al. 2014). Moreover, more lignin and thicker cell walls may be formed in cells being exposed to Se (Cui et al. 2018) and therefore restrict the translocation of Cd that will be adsorbed. A further mechanism can be restriction of Cd translocation by compartmentalization. Gomez Ojeda et al. (2013) found an increase of Cd in poorly soluble cell fractions upon Se addition. One would expect that compartmentalization of Cd in root cells would reduce Cd translocation and therefore lead to greater Cd reduction in the shoots than in the roots. However, results for shoots and roots for the data “rice excluded” did not show any evidence of compartmentalization. Cadmium reduction in roots and shoots increased both linearly and significantly with Se addition in the growth medium (Fig. 4a and b). Comparison of both models (Fig. 4c) highlighted that Cd reduction in roots and shoots were similar. This would suggest that the main mechanism involved would be a restricted uptake of Cd by roots, which would be possible either by reduction of the bioavailability of Cd in the soil or reduced absorption by roots.
Concerning “rice only”, we cannot conclude about a mechanism in the crop (Fig. 4d) as a larger data set would be required to verify different hypotheses.
Conclusions and perspective
The aim of this paper was to identify if there are significant interactions between Se and Cd in the soil-crop system which may reduce Cd uptake by plants.
The impact of Se addition on Cd reduction in plants was found to be significant and dose-dependent including all crops, different selenium compounds, and different plant organs in the analysis. Excluding rice from the data (aerobic soil conditions only) resulted in a more pronounced effect with higher significance. Analyzing all plant organs of rice (anaerobic soil conditions only) showed that there was a tendency but no dose-dependent reduction of Cd by Se. Treating rice shoots separately showed that there was dose-dependent and significant effect of Se addition. The results implied that a Cd-Se compound may be formed presupposing reducing conditions locally in microsites of the soil or at the root surface. More investigations are needed to fully understand possible mechanisms involved.
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Acknowledgements
The authors would like to thank Dr. J.E. Eriksson from the Swedish Agricultural University for sharing the inventory data from the national monitoring program of Swedish arable soils and crops. Affholder MC held a post-doctoral fellowship funded by the Faculty of Natural Resources and Agricultural Sciences from the Swedish University of Agricultural Sciences (SLU).
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Affholder, MC., Flöhr, A. & Kirchmann, H. Can Cd content in crops be controlled by Se fertilization? A meta-analysis and outline of Cd sequestration mechanisms. Plant Soil 440, 369–380 (2019). https://doi.org/10.1007/s11104-019-04078-x
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DOI: https://doi.org/10.1007/s11104-019-04078-x