Agroecological Responses of Heavy Metal Pollution with Special Emphasis on Soil Health and Plant Performances
Vaibhav Srivastava1 
Abhijit Sarkar2* 
Sonu Singh3 
Pooja Singh4 
Ademir S. F. de Araujo5 
Rajeev P. Singh1,6*- 1Department of Environment and Sustainable Development, Institute of Environment and Sustainable Development, Banaras Hindu University, Varanasi, India
- 2Laboratory of Applied Stress Biology, Department of Botany, University of GourBanga, Malda, West Bengal, India
- 3Ministry of Environment, Forest and Climate Change, Govt. of India, New Delhi, India
- 4Society for Higher Education and Practical Applications, Varanasi, India
- 5Soil Quality Laboratory, Agricultural Science Center, Federal University of Piaui, Teresina, Brazil
- 6Department of Civil Engineering, University of Nebraska-Lincoln, Omaha, NE, United States
With modern day urbanization and industrialization, heavy metal (HM) contamination has become a prime concern for today's society. The impacts of metal contamination on agriculture range from the agricultural soil to the produce in our food basket. The heavy metals (HMs) and metalloids, including Cr, Mn, Co, Ni, Cu, Zn, Cd, Sn, Hg, Pb, among others, can result in significant toxic impacts. The intensification of agricultural land use and changes in farming practices along with technological advancement have led to heavy metal pollution in soil. Metals/metalloids concentrations in the soil are increasing at alarming rate and affect plant growth, food safety, and soil microflora. The biological and geological reorganization of heavy metal depends chiefly on green plants and their metabolism. Metal toxicity has direct effects to flora that forms an integral component of ecosystems. Altered biochemical, physiological, and metabolic processes are found in plants growing in regions of high metal pollution. However, metals like Cu, Mn, Co, Zn, and Cr are required in trace amounts by plants for their metabolic activities. The present review aims to catalog major published works related to heavy metal contamination in modern day agriculture, and draw a possible road map toward future research in this domain.
Introduction
Heavy metal contamination is a prime environmental concern that threatens plant, animal, and human health, as well as the quality of the environment. Like other metals and metalloids, heavy metals occur in the earth's crust, but due to their persistent and stable character, they cannot be degraded or destroyed. These heavy metals and metalloids are bio-accumulative and may slowly enter plants, animals, and humans through air, water, and the progression of the food chain over a certain period of time (Lenntech Water Treatment Air Purification, 2004; Nagajyoti et al., 2010). Heavy metal ores include sulfides of iron (Fe), lead (Pb), zinc (Zn), arsenic (As), cobalt (Co), silver (Ag), gold (Au), and nickel (Ni); and oxides of aluminum(Al), manganese (Mn), gold (Au), selenium (Se), and antimony (Sb). Also, some metals exist and can be retrieved both as sulfide and oxide ores such as iron (Fe), copper (Cu), and cobalt(Co) (Duruibe et al., 2007; Alloway, 2013). Heavy metals are extracted from their ores during mineral processing. During this process, some parts are left in the open and transported to other places through wind and flood processes, creating severe threats to the environment (Lenntech Water Treatment Air Purification, 2004; Nagajyoti et al., 2010). Various natural and anthropogenic processes may release these heavy metals into the ambient environment (Dembitsky and Rezanka, 2003). Modern agricultural practices have caused agricultural pollution leading to degradation of the ecosystem and the environment due to increased application of agrochemicals and inorganic fertilizers (Malik et al., 2017). Additionally, land application of sewage sludge, organic waste manure, industrial byproducts, and irrigation with waste water are major sources of heavy metals into agricultural systems (Khan et al., 2013; Srivastava et al., 2016; Tóth et al., 2016; Sharma et al., 2017; Woldetsadik et al., 2017) (Figure 1).
Figure 1. Overview of sources of heavy metal pollution and its agroecological consequences.
Plants are subjected to biotic and abiotic stresses such as heat, cold, drought, high light intensity, UV radiations, heavy metals, and pollutants such as O3 and SO2 (Dezhban et al., 2015; Kumar et al., 2016). Consequently, high level of reactive oxygen species (ROS) like singlet oxygen (1/2O2), hydroxyl radical (HO•), superoxide radical (), and hydrogen peroxide (H2O2) are produced (Wang et al., 2015). Although, ROS are important signaling molecules that are generally in equilibrium with antioxidant molecules (D'Autréaux and Toledano, 2007; Holmström and Finkel, 2014; Reczek and Chandel, 2015; Mittler, 2017), but they may also pose adverse effect on organisms (Mates, 2000; Rhee et al., 2013; Shahid et al., 2014; Thakur et al., 2016). ROS could also affect various biochemical molecules, membrane lipids, amino acid chain, carbohydrates, proteins, pigments, and nucleic acids (Gratão et al., 2005; Manikandan et al., 2015; Venkatachalam et al., 2017). Moreover, membrane leakage accompanied by loss of cell metabolites from cell protoplasm is also caused by ROS (Dingjan et al., 2016) and may result in a reduction in cell growth or may even cause death in a few cases (Gonçalves et al., 2007; Lee et al., 2007).
It is evident that due to multiple social-economical, technological, and developmental issues, heavy metal contamination in modern day agriculture has become a serious crisis in most of the developing and under developed countries. Finding eco-friendly, sustainable ways to combat heavy metal contamination issue is a major challenge. The present review aims to catalog major published works related to heavy metal contamination in modern day agriculture, and draw a possible road map toward future research.
Natural and Other Sources of Heavy Metals in Agro-Environment
Natural Sources
Weathering of rock is considered the most significant contributor of heavy metals. Generally, the weathering process is influenced by the nature of the rock and the environmental conditions on which the concentration and composition of heavy metals largely depends (Abdu et al., 2011). Materials of geologic origin have high concentrations of Mn, Cr, Co, Cu, Ni, Zn, Sn, Cd, Hg, and Pb. Volcanoes along with harmful and toxic gases are the high-level emitters of Al, Zn, Mn, Pb, Ni, Cu, and Hg (Seaward and Richardson, 1989; Nagajyoti et al., 2010). Volcanic eruptions and windblown dust particles are also the source of heavy metals. High concentration of Fe and low amount of Mn, Zn, Cr, Ni, and Pb occurs from wind-dust blowing from the desert region like the Sahara (Ross, 1994; Nagajyoti et al., 2010). Similarly, marine aerosols and forest fires also contribute to environmental heavy metals to some extent. Fire produces volatile heavy metals like Se and Hg which are part of carbonaceous matter (Ross, 1994; Naidu et al., 1997; Nagajyoti et al., 2010). Natural vegetation contributes heavy metals to the environment through leaching, decomposition, and volatilization (Nagajyoti et al., 2010; Cuypers et al., 2013). Likewise, oceanic activities produce sea sprays and aerosols that contribute heavy metal into inland coastal areas (Zverina et al., 2014; Monge et al., 2015) (Figure 1).
Agricultural Sources
A major contributor of heavy metals in agricultural soil is inorganic fertilizers that also include liming, irrigation waters, and sewage sludge (Table 1). Varying concentrations of Cd, Cr, Ni, Pb, and Zn have been contributed by other sources, predominantly by fungicides, phosphate fertilizers, and inorganic fertilizers (Kelepertzis, 2014; Tóth et al., 2016) (Figure 1). Cadmium bioaccumulation in plants is of prime concern as it deposits on leaves at high concentration and that may be consumed by animals or humans. Sewage sludge, manure, limes is also the cause of cadmium enrichment (Yanqun et al., 2005; Niassy and Diarra, 2012). High levels of major heavy metals are reached in agricultural soil (where concentration is generally low) by repeated use of phosphate fertilizer (Verkleij, 1993; Carnelo et al., 1997). Sewage sludge adds Cr, Cu, Zn, Pb, Ni, and Cd while animal manure augments the soil by adding Mn, Cu, Zn, and Co (Verkleij, 1993). Land application of sewage sludge is one of the most important contributors of heavy metal in the soil (Singh and Agrawal, 2008; Araújo et al., 2010; Singh et al., 2011, 2012; Srivastava et al., 2015, 2016; Sharma et al., 2017). Several pesticides are also a major source of heavy metal contamination in agricultural fields (Ross, 1994; Wei and Yang, 2010; Tóth et al., 2016; Marrugo-Negrete et al., 2017). Table 2 shows the concentrations of heavy metals in different agricultural amendments. Similarly, waste water irrigation is also a major contributor of heavy metal pollution (Sharma et al., 2007; Khan et al., 2008, 2013; Qureshi et al., 2016; Islam et al., 2017; Woldetsadik et al., 2017). Therefore, concentrations or amounts of heavy metals in agricultural soil depend on soil characteristics and the composition and application rate of inorganic fertilizers, pesticides, sewage sludge, and/or waste water. Table 3 shows the permissible level of heavy metals in agricultural soil.
Table 1. Sources of heavy metals in agricultural soil.
Table 2. Heavy metal concentrations (μg g−1) in agricultural amendments (Adapted from Ross, 1994).
Table 3. Permissible limit of heavy metals in agricultural soil.
Industrial Sources
Different industrial activities like mining and refinement are another major sources of heavy metal contamination (Figure 1). Mining activities emits various types of heavy metals which depend on the nature of mining practices used. For example, the use of Hg in gold mines has become a major contributor of this metal into the environment (Clemens and Ma, 2016; Pavilonis et al., 2017). Similarly, coal mines are the chief source of As, Cd, and Fe which can pollute adjacent soil. Vaporized heavy metals like Cu, Zn, Pb, As, Sn, and Cd combine with water and condense to form aerosols (Nagajyoti et al., 2010). These may be either dry deposited (dispersed by winds) or wet deposited (precipitated in the form of rainfall) causing water and soil contamination. Similarly, waste runoff from mines, dust from transportation of crude ores, corrosion and leaching of heavy metals also contaminate soil and water bodies (Carlisle and Clements, 2005; Vásquez-Murrieta et al., 2006; Alloway, 2013; Rout et al., 2013). Various refinery processes also contribute to heavy metal pollution in the soil. Heavy metals like B, Se, Cu, Zn, Cd, Ni, and Cs are emitted by petroleum industries, coal burning power stations, nuclear power stations, and high-tension wires (Verkleij, 1993; Ahmed and Ahmaruzzaman, 2016; Zhu et al., 2016). Another contributor of heavy metal pollution includes processing of plastic, paper, textiles, electronics, and wood preservation. Antiwear protectants for automobiles release Pb, Cd, Ni, Hg, Cr, and Zn especially in inefficient engines. The combustion lead containing gasoline emits Pb in the atmosphere and incinerators for MSW produces a considerable amount of Zn, Pb, Al, Sn, Fe, and Cu.
Domestic Sources
Effluents are most probably the largest contributor of the high concentration of metal found in ponds, lakes, and rivers (Zahra et al., 2014; Singh and Kumar, 2017). Effluents generally consist of (1) mechanically treated or untreated wastewater, (2) materials that have passed from the filters of biological treatment plants, and (3) waste material from sewage outfall which is discharged into water bodies like the sea. Urban runoff also presents a severe problem of heavy metal pollution (Figure 1).
Miscelleneous Sources
Other contributors of heavy metal pollution are comprised of refuse from incineration, industrial discharge, transportation or traffic emisssions, and open dumps or landfills (Singh et al., 2011; Srivastava et al., 2015; Aryal et al., 2017; Dubey et al., 2017). Vehicular sources include Zn and Cd associated with dust from tire wear (Gope et al., 2017), Cu and Cd from diesel engines (Nagajyoti et al., 2010), and Cr, Ni and Zn from aerosol emissions (Chen et al., 2013).
Agroecological Ramifications of Heavy Metals Contamination
Soil Health and Fertility
Management of good soil quality is a key factor for sustainable agriculture and soil biology plays an important role. Soil microbes are an essential component of the ecosystem (Harris, 2009). Microorganisms play a key role in maintaining soil fertility via organic matter disintegration and nutrient cycling. However, they can be negatively affected when exposed to stress factors like extreme temperature, pH, salinity, and chemical pollution (Schimel et al., 2007; Paz-Ferreiro and Fu, 2016). The soil may become contaminated with heavy metals from various anthropogenic activities including industrial, mining, and agricultural activities. For example, heavy metals present in wastes from mines, sewage sludge, inorganic fertilizers, and pesticides may enter into the soil system and affect microbes (Carlisle and Clements, 2005; Gupta et al., 2010; Tóth et al., 2016; Sharma et al., 2017).
Soil Microbial Dynamics
Microbial viability decreases with increasing levels of heavy metal contamination. For example, Greszta et al. (1979) found decreased colony forming units (CFUs) of bacteria and fungi in the forest soil mixed with Pb-Cu sludge, Pb-Cu dust, Pb-Zn dust, and Cd-Pb-Zn. Freedman and Hutchinson (1980) observed a significant decrease in fungal CFUs near Sudbury smelters however, the results were not statistically significant from the non-polluted sites. Brookes and McGrath (1984) observed the effect of sewage sludge (Cu = 40–90 μg g−1, Ni = 5–10 μg g−1) amended agricultural soil for a period of 20 years and noticed decreased soil microbial biomass. Likewise, Rühling et al. (1984) found a decreased number of species of fruitbody producing fungi with increasing proximity to Gusum smelter and found about 35 species at control sites (<100 μg Cu g−1 organic matter), about 25 species in moderately polluted (<1,000 μg Cu g−1 organic matter), and 13 species near the smelter (<1,000 μg Cu g−1 organic matter). Šmejkalová et al. (2003) observed decreased CFU of total bacteria and micromycetes with increasing heavy metal concentration. Yuan et al. (2015) reported a negative correlation of microbial viability to extended exposure to Pb. Similarly, dos Santos et al. (2016) studied the biological soil attributes in a heavy metal contaminated site located in close proximity to the Votorantim Metal Company in the municipality of Três Marias (MG), Brazil. They reported decreased CFU of bacteria (5.5 × 104 g−1 dry soil), actinobacteria (1.4 × 102 g−1 dry soil), and fungi (2.0 × 104 g−1 dry soil) in heavy metal contaminated site as compared to control site (CFUs were 2.0 × 107, 1.1 × 105, 5.0 × 104 g−1 dry soil for bacteria, actinobacteria, and fungi respectively). de Quadros et al. (2016) demonstrated a reduction in microbial biomass, richness, and diversity due to coal mining practices. Nayak et al. (2015) reported that 40 and 100% fly ash amendments increased the concentrations of Zn, Fe, Cu, Mn, Cd, and Cr in agricultural soils, and also affected the microbial population dynamics. They also reported that microorganisms differed in their responses to the rate of fly ash amendments. The population of both fungi and actinomycetes decreased by the application of fly ash, while the aerobic heterotrophic bacterial population did not change significantly up to 40% fly ash amendment. On the other hand, total microbial activity measured in terms of fluoresceindiacetate (FDA) assay, and denitrifiers showed an increasing trend up to 40% fly ash amendment. However, the activities of both alkaline and acid phosphatase were decreased by the application of fly ash. Likewise, Wang et al. (2007) demonstrated that heavy metals pollution had a significant impact on soil bacterial and actinomycetic community structure through the use of Polymerase chain reaction–denaturing gradient gel electrophoresis (PCR–DGGE) technique. According to their findings, negative correlations were observed between soil microbial biomass, phosphatase activity, and heavy metals concentrations. Also, soil microorganisms activity and community composition could be predicted using the availability of Cu and Zn. Effect of heavy metals on soil enzyme activities are given in Table 4.
Table 4. Effect of heavy metals on microbial population and their activities.
Soil Microbial Functions and Processes
A. Litter decomposition
Heavy metal toxicity leads to reduced litter decomposition resulting in unrecompensed litter layer on the soil (Illmer and Schinner, 1991; Giller et al., 1998; Marschner and Kalbitz, 2003). Bringmark and Bringmark (2001) reported a significant correlation between respiration rates from forest litter and concentrations of lead (Pb) in soil organic layers at concentrations not much higher than those typical for uncontaminated areas. Similarly, the decomposition rate of mountain birch (Betula pubescens ssp. Czerepanovii) leaves were examined by Kozlov and Zvereva (2015) in a heavily polluted industrial area near the nickel-copper smelter in Monchegorsk. A significant reduction of 49% was found in relative mass loss of native leaves compared with the loss noted in unpolluted forest during 2 years of exposure. Also, microbial activity in soil was reduced by four-fold and almost complete extinction of saprophagous invertebrates was identified in the polluted soil. They concluded that the slow decomposition rate of birch leaves in an industrial barren resulted primarily due to high metal concentration in both soil and litter and from drastic environmental changes associated with the forest decline. Moreover, a number of studies have shown that anthropogenic heavy metal pollution poses adverse effect on litter decomposition in streams (Carlisle and Clements, 2005; Hogsden and Harding, 2012; Ferreira et al., 2016). For example, Zn from abandoned mines in the western United States pollutes nearby streams, thereby adversely affects the microbial fauna of streams and interferes with litter breakdown (Carlisle and Clements, 2005).
B. Carbon mineralization
The rate of soil organic carbon mineralization has been widely used as an assay for metal toxicity in both ecotoxicological and environmental monitoring studies (Giller et al., 1998). The soil respiration rate can be used to assess carbon mineralization. Usually, low concentrations of heavy metal have a slight effect on soil respiration, but the effect is decreased with increasing heavy metal pollution or toxicity. A number of studies suggest that heavy metal addition often results in a decreased respiratory rate for a wide range of substrates like cellulose (Hattori, 1992), glucose (Mikkelsen, 1974; Hattori, 1991), plant residues (Aoyama and Itaya, 1995), and sewage sludge (Dar and Mishra, 1994). Tyler (1975) reported a reduced decomposition rate of starch and cellulose in heavy metal polluted soil, while a negligible effect was seen for protein and glucose. By the 6th week post-treatment, the rates of carbon accumulated were high in the copper (6.03%) and copper: Zinc (5.80%) treatments, but low in the nickel and zinc (4.93 and 5.02% respectively). Nwuche and Ugoji (2008) observed a negative correlation between soil microbial respiration and heavy metal content. The rate of soil microbial respiration was reduced to 0.98, 1.08, and 1.61 μg of C/g in the Cu:Zn, Cu, and Zn treated soil respectively from an average rate of 2.51–2.56 μg of C/g at the beginning of the experiment. Reductions in respiration rate resulted in declined carbon mineralization and led to cabon accumulation. Among different treatments, Cu had the highest carbon accumulation (6.03%) followed by Cu:Zn (5.80%) and Cu:Ni (5.36%) treated soil from an average value of 4.87% at the beginning of the experiment. Vásquez-Murrieta et al. (2006) showed a negative correlation between C minerlization and the heavy metal (As, Pb, Cu, and Zn) content of the soil from mine spills in San Luis Potosí (Mexico). Similarly, reduction in carbon mineralization was noticed in a clay loam soil when subjected to hexavalent chromium (Dotaniya et al., 2017).
C. Nitrogen transformations
Heavy metal application can induce or inhibit N-mineralization that may be due to discrepancies in experimental procedure adopted, variation in soil properties and substrate concentrations. Generally, heavy metal pollution has a negative impact on nirogen transformation processes, which in turn affects N- mineralization (Dai et al., 2004; Vásquez-Murrieta et al., 2006; Zhang et al., 2010; Hamsa et al., 2017). Tyler (1975) reported decreased N-mineralization at very low Cu (100 μg g−1) concentration in the soil. The impact on nitrification is similar to that of N-mineralization after heavy metal exposure (i.e., with increasing concentration of heavy metals nitrification decreases and vice versa) (De Catanzaro and Hutchinson, 1985). Also, in most of the cases nitrification seems to be more sensitive to heavy metal pollution than N-mineralization (Rother et al., 1982; Bewley and Stotzky, 1983). Brookes et al. (1986) reported a significant decrease of 50% in N2 fixation rate for blue green algae grown on sludge amended soil with low concentrations of extractable heavy metals (Zn = 30 μg g−1 soil, Cu = 15 μg g−1, Ni and Cd = 2 μg g−1). Similarly, Nwuche and Ugoji (2008) studied the effects of heavy metals on soil microbial processes over a period of 6 weeks. The results showed that Cu and Cu:Zn (P < 0.05) significantly ineterered with microbial nitrogen mineralization and caused accumulation of N in the soil. At the end of the experiment N content was 0.41 and 0.44% in Cu and Cu:Zn treated soil as compared to 0.23% (Cu) and 0.24% (Cu:Zn) at the beginning of the experiment. Similar results were reported by Dai et al. (2004) where the wastes disposal of metallurgic industry in Nord-Pas-de-Calais, northern France led to heavy metal contamination (Zn, Pb, Cu, and Cd) and reduced N mineralization. Likewise, Zhang et al. (2010) observed reduced N mineralization in heavy metal contaminated mining soil at the Lawu mine of central Tibet, China.
Soil Enzymes
The bioavailability of metals in soils depend on metal contents, soil pH, organic matter, and clay content. Soil enzyme activities such as arylsulfatase, alkaline phosphatase, b-glucosidase, cellulase, dehydrogenase, invertase, protease, and urease are sensitive to the presence of heavy metals (Oliveira and Pampulha, 2006; Wang et al., 2008; Hu et al., 2013, 2014; Burges et al., 2015; Xian et al., 2015). Oliveira and Pampulha (2006) assessed the effect of heavy metals on soil microbiology and biochemistry in an area with a known history of pollution. The heavy metal concentration in soil was reported to be 1,558 and 109 mg/kg for As and Hg respectively. The pollution led to decreases in microbial activity and soil dehydrogenase activity. Similarly, the addition of MSW composts in soil led to decreased urease and protease activity that might have been due to the heavy metal induced toxicity present in the municipal solid waste (Garcia-Gil et al., 2000; Crecchio et al., 2004). Likewise, the application of different rates of Cd, Pb, and Cd/Pb mixture in soil reduced the activities of acid phosphatase (ACP), urease (URE), and microbial biomass carbon (MBC). The maximum reduction of 35.6% (ACP), 36.6% (URE), and 52.4% (MBC) was noticed in Cd/Pb treated samples in comparison to control. The DGGE profiling also revealed that addition of metals significantly affected the microbial community structure (Khan et al., 2010). Moreover, heavy metals can significantly affect the soil ecosystems and biological activity in the soil. In their study, Pan and Yu (2011) shown that the heavy metals (Cd or/ and Pb) negatively affect the activity of soil enzymes like acid phosphatase, urease, and dehydrogenase and also lowered the soil microbial population. Hu et al. (2013) investigated individual and combined effects of Cu and Se on soil enzyme activities in a lab-scale experiment. The results showed a negative correlation of four soil enzymes (urease, alkaline phosphatase, catalase, and nitrate reductase) to Cu and Se pollution, either singly or combined. The activity was found in order of nitrate reductase> urease> catalase> alkaline phosphatase. Hu et al. (2014) found reduced soil enzyme activities and microbial biomass in three heavily polluted paddy fields distributed in three different towns of Y County, northern Hunan Province. All three fields were badly polluted by heavy metals (Cu, Zn, and Cd) due to long term irrigation with contaminated water due to mining activities. The MBC and MBN in one of the severely polluted sites declined to 31.6 and 64.4% of the controls, respectively. Whereas, activities of acid phosphatase, catalase, dehydrogenase, sucrose, and urease were 94.7, 52.4, 25.2, 87.8, and 49.3% of the controls, respectively. Likewise, b-glucosidase and acid phosphatase activities were reduced significantly under repeated single-metal and multi-metal (Pb, Cu, Zn, Cd) pollution events on soil quality (Burges et al., 2015). Xian et al. (2015) assessed the joint effect of heavy metals and soil properties on soil activities and found that arylsulfatase is the most sensitive soil enzyme that could be used as an indicator for soil toxicity. Soil organic matter (SOM) is the dominant factor affecting the activity of arylsulfatase and when it is present above the critical level, then it minimizes the noxious effect of heavy metal and enhances soil microbial activity.
Plant Responses
Heavy metal pollution is one of the contemporary environmental issues contaminating water, air and soil. This not only leads to substantial losses in crop productivity, but also poses health hazards. When plants are exposed to heavy metal stress, then it provokes antioxidative systems of plants in order to minimize the damage (Figure 1). The current section deals with heavy metal-plant interaction and different physiological and biochemical responses of plants.
Oxidative Stress and ROS
“Reactive oxygen species” are chemically reactive species derived from molecular oxygen. Several different ROS are present transiently in all aerobic organisms, including: (a) oxygen derived non-radicals e.g., hydrogen peroxide (H2O2), singlet oxygen (1/2O2), organic hydroperoxide (ROOH); and (b) oxygen derived free radicals e.g., hydroxyl (HO•), peroxyl (), superoxide anion (), and alkoxyl (RO•) radicals (Pinto et al., 2003; Circu and Aw, 2010; Shahid et al., 2014; Tamás et al., 2017). Usually, ROS are natural byproducts of the oxidative metabolism that may pose damage to all aerobic organisms. Although some of them are known to be as important signaling molecules that have the potential to modulate the activity of specific defense proteins. ROS are highly unstable and reactive molecules having a very short life (Wang et al., 2010) that can oxidize proteins, lipids, and nucleic acids leading to cell structure alteration and mutagenesis (Malar et al., 2014; Manikandan et al., 2015, 2016; Venkatachalam et al., 2017). In photosynthetic organism's organelles like chloroplast, mitochondria, and peroxisomes are considered to be the centers of ROS production (Pinto et al., 2003; Pucciariello et al., 2012). Exposure of plants to toxic heavy metals leads to increased production of ROS as heavy metals interact with electron transport activities of chloroplast and mitochondrial membrane. ROS can disrupt the redox status of cells posing damage to the membrane resulting in ion leakage (Dingjan et al., 2016; Anjum et al., 2017). Also, it causes lipid peroxidation and biological macromolecule breakdown (Carrasco-Gil et al., 2012; Chen et al., 2012; Venkatachalam et al., 2017). The stage of plant physiological challenge developed due to an imbalance or disturbance between ROS formation and removal through antioxidative defense mechanism is known as oxidative stress (Kovácik et al., 2010; Morina et al., 2010; Manikandan et al., 2015; Venkatachalam et al., 2017). Anjum et al. (2017) reported increased levels of Cr toxicity in two genotypes of maize led to high proline, phenolic, and soluble sugar contents, and low soluble protein content. Increases in malondialdehyde and H2O2 content led to electrolyte leakage.
Genotoxicity
The mechanisms behind metal induced genotoxicity are complex in nature and still not well-understood (Cuypers et al., 2011; Shen et al., 2013). It has been determined that heavy metal induced genotoxicity/DNA damage occurs indirectly through the production of ROS under oxidative stress (Barbosa et al., 2010; Shahid et al., 2014; Malar et al., 2015; Aslam et al., 2017) (Figure 1). Heavy metal toxicity induces chromosomal aberrations and also decreases the cell division rate. A number of studies have previously identified heavy metal induced nucleic acid impairments in plants like Allium cepa (Steinkellner et al., 1998; Barbosa et al., 2010; Arya et al., 2013; Arya and Mukherjee, 2014; Qin et al., 2015), Vicia faba (Qun and Xiao, 1995; Steinkellner et al., 1998; Marcato-Romain et al., 2009; Pourrut et al., 2011; Arya et al., 2013; Arya and Mukherjee, 2014), Helainthus annuus (Chakravarty and Srivastava, 1992), Solanum tuberosum, and Nicotiana tabacum (Gichner et al., 2006) etc. Genotoxic responses differ among plant species to the same metal and usually depends on the number and total length of the diploid chromosomes and also the number of metacentric chromosomes (Ma et al., 1995; Patra et al., 2004). The concentration of heavy metal, its oxidation state and extent of exposure greatly affects the genotoxic response of any plant (Malar et al., 2015; Aslam et al., 2017). Hydroxyl radical (OH•) is the highly reactive species among ROS, damaging all the components of the DNA molecule (Jones et al., 2011). ROS interaction with DNA leads to base deletion, base modification, strand breaks, and damages to cross links and pyrimidine dimers (Gastaldo et al., 2008). There are four different potential sites for metal binding in DNA viz. (i) the ribose hydroxyls; (ii) the exocyclic base keto groups, (iii) the negatively charged phosphate oxygen atoms; and (iv) the base ring nitrogens (Oliveira et al., 2008). A promutagenic damage caused by metal binding to the cell nucleus leads to DNA base modifications, inter- and intra-molecular cross-linking of DNA and proteins, DNA strand breaks, rearrangements, and de-purination (Kasprzak, 1995). Oxidized bases are usually generated upon the interaction of ROS with DNA and 8-oxoguanine is the most abundant and studied form modified DNA bases (Fortini et al., 2003) that may cause neoplastic transformation (Bal and Kasprzak, 2002). Cunningham (1997) reported that a promutagenic adduct 7,8-dihydro-8-oxoguanine (8-OxoG) is generated due to ROS interaction with DNA that have the ability to pair with adenine causing C to T transversion mutations. Yang et al. (1999) observed generation in 8-hydroxydeoxyguanosine (8-OHdG) adducts when Cd and Pb interacted with DNA lead in strand breakage. Similarly, Hirata et al. (2011) identified Cr and As induced translesion DNA synthesis resulting due to generation of 8-OHdG.
Qin et al. (2015) studied genotoxic effects of copper (Cu) in root tip cells of A. cepa var. agrogarum L. The exposure to ionization Cu led to reduced mitotic index and chromosomal aberrations (viz. C-mitosis, chromosome stickiness, chromosome bridges, and micro nucleus). Also, Cu toxicity caused impaired microtubules arrangement at different concentrations and decreased content of α-tubulin in comparison to controls. Venkatachalam et al. (2017) reported Pb induced genotoxicity due to the amplification of new bands and absence of normal amplicons in treated plants in random amplified polymorphic DNA (RAPD) analysis. Likewise, when seeds and seedlings of Lactuca sativa were subjected to increasing levels of Pb (NO3)2 (2–20 mg l−1), higher doses caused DNA fragmentation (>5 mg l−1), and the presence of micronuclei (20 mg l−1). Also, cell cycle impairment was observed even under low Pb doses (0.05 and 0.5 mg l−1) (Silva et al., 2017).
Interference with Signaling Pathways
The mechanisms explaining how heavy metals affect the cell signaling are still poorly understood. Cell signaling process may be directly affected during the interaction of heavy metals with proteins or indirectly during formation of the metal-induced ROS (Foyer and Noctor, 2005; Mittler et al., 2011; Islam et al., 2015) (Figure 1). Studies suggest that dysregulation of the signaling events caused by heavy metal interactions are the main reason for heavy metal toxicity and its negative impacts. Cellular interactions with the heavy metals leads to changes in various significant processes like regulation of gene expression, interference with signaling processes by affecting the G-proteins, growth factor receptors, and receptor tyrosine kinases (Harris and Shi, 2003). Signal transduction under stress is a complex process that starts with the plant sensing the heavy metal followed by activation of responsive genes by transcription, ultimately reducing the deleterious effect on plants (Maksymiec, 2007). Activation of stress related genes are involved in certain signal transduction pathways such as mitogen-activated protein kinase (MAPK) phosphorylation, ROS signaling system, Ca-calmodulin, and hormones (Islam et al., 2015). Numerous studies have shown that in plants heavy metals like Cu, Zn, Pb, and Cd can affect the mitogen kinase signaling pathways (Xiong and Yang, 2003; Nakagami et al., 2005). The generally affected pathways include MAPK pathways as they are activated by ROS and are easily affected by various signaling stimuli (Zhang and Klessig, 2001; Yeh et al., 2003; Rodriguez et al., 2010). Jonak et al. (2004) reported that in Medicago sativa, MAPK pathways were reported to be rapidly activated with increased concentration of Cu. However, the same pathway was delayed with Cd exposure (Jonak et al., 2004). Heavy metals also increase the level of H2O2 generation by enhancing the synthesis of salicylic acid (SA), jasmonic acid (JA), and ethylene (ET) in plants and this in turn interferes with the cell signaling process (Maksymiec, 2007; Schellingen et al., 2014; Van de Poel et al., 2015). For example, the elevated levels of JA during As exposure of plants promotes the expression of some signaling and stress responsive genes like MAPK, CDC25 and those responsive to glutathione metabolism (Agrawal et al., 2003; Thapa et al., 2012; Islam et al., 2015).
Physiological and Biochemical Response
Heavy metals interact with structural components (cell, tissue, and organs) either directly or indirectly by modulating cell signaling or metabolism that appears in the form of visible injuries (Shahid et al., 2014). Studies at both structural and sub-structural level will help to identifying the sites of primary heavy metal toxicity and better understanding of their consequences on plant response. In order to combat with metal phyto-toxicity, plants have evolved an anti-oxidative defense system having many enzymes such as those of ascorbate peroxidase (APX), catalase (CAT), superoxide dismutase (SOD), glutathione (GSH), glutathione reductase (GR), peroxidase (POX), and guaiacol peroxidase (GPX), which play a pivotal role in scavenging excess ROS (Zhang et al., 2007; Li et al., 2012, 2013; Hattab et al., 2016; Sidhu et al., 2016; Venkatachalam et al., 2017) (Figure 1).
Zhang et al. (2007), examined the effect of heavy metal stress on two mangrove plants found increased ROS as evidenced by MDA production. Similar results were obtained in a number of studies done in the past on higher plants (Singh and Agrawal, 2007; Zhang et al., 2007; Sidhu et al., 2016; Alves et al., 2017). This suggests that free radicals play a significant role in heavy metal induced toxicity of higher plants. Likewise, superoxide dismutase (SOD) activity was improved significantly in roots and leaves at low heavy metal concentration, however its activity was decreased sharply at high concentrations indicating impairment of SOD scavenging function. Similar results were noticed in Allium sativum (Zhang et al., 2005) and Alyssum species (Schickler and Caspi, 1999). SOD activity peaked in roots of Kandelia candel at higher doses of heavy metal than in roots of Bruguiera gymnorrhiza suggesting better tolerance ability of K. candel against oxidative damage (Takemura et al., 2000). In photosynthetic organisms plasma cell membranes are the primary target of heavy metal action that cause lipid peroxidation via ROS production (Chen et al., 2012; Dingjan et al., 2016; Anjum et al., 2017). Enhanced lipoxygenase activity causes lipid peroxidation through the formation of oxylipins (Porta and Rocha-Sosa, 2002; Alemayehu et al., 2013). Lipoxygenase play a significant role in heavy metal induced oxidative stress in Arabidopsis thaliana and Lessonia nigrescens (Vanhoudt et al., 2011). Singh and Agrawal (2009) studied the biochemical response of Abelmoschus esculentus plants grown in different application rates of sewage sludge. The results showed a significant increase of 27 and 89% in chlorophyll content of plants grown in 20 and 40% sewage sludge amendments (SSA) respectively at 40 days after sowing (DAS), however, it was decreased by 10% (20% SSA) and 47% (40% SSA) at 60 DAS. Accumulation of heavy metals in plants at later stages of growth might have been the reason behind the decrease of chlorophyll content. Similarly, a reduction in photosynthetic rate, increased level of phenol, peroxide, and ascorbic acid content was noticed with increasing level of sewage sludge application, suggesting a defensive response against heavy metal induced oxidative stress experienced by the plants. Similar results were observed in A. esculentus (Singh and Agrawal, 2009), Vigna radiata (Singh and Agrawal, 2010a), and Oryza sativa (Singh and Agrawal, 2010b). Chen et al. (2003) observed the effect of Cd on the physiology of carrot and radish plant roots grown under different concentrations/ levels of Cd. The results indicate a significant decrease in germination and root growth of both the plants at and above 20 mg/l of Cd. Similarly, the activities of superoxide dismutase (SOD), catalase (CAT), polyphenol oxidase (PPO), and peroxidase (POX) were decreased significantly with increasing Cd concentration. Also, proline concentration increased at 20 mg/l of Cd and decreased further with increasing Cd concentration.
Thounaojam et al. (2012) examined the effect of Cu on rice plants (O. sativa. L. var. MSE-9). Plants readily absorbed the Cu though maximum accumulation was noticed in the root than shoot system. Also, H2O2 and malondialdehyde (MDA) content were increased significantly with the elevated Cu concentration inducing oxidative stress. The level of antioxidative enzymes like APX, GPX, SOD, GR, ascorbic acid (ASH), and GSH was increased significantly, however CAT did not show statistically significant changes. The results suggested that excess Cu induced oxidative stress by ROS production, however, the plant's antioxidative system scavenged the deleterious effect of excess Cu in an active manner.
Similarly, Li et al. (2013) studied the antioxidative response and proline metabolism in roots and seeds of wheat plants under different doses of Zn (0.5, 1, and 3 mM). The highest dose of Zn caused significant reduction in total chlorophyll (chl) and chl a, while chl b content decreased under all doses. H2O2 and malondialdehyde (MDA) level were increased significantly in comparison with control. Likewise, APX, CAT, GR, POX activities were improved significantly.
Plant-Soil Interaction and Dynamics/Translocation of Heavy Metals
The present section deals with several aspects of phytoremediation including uptake of metal ion from soil, translocation, and mechanisms of HM hypertolerance in plants (Figure 1). To enhance the bio-availability of metal ions, plants use various strategies. For instance, rhizosphere acidification, carboxylate formation, and secretion of phytosiderophores so as to assist the solubilization and chelation of metal ions (Rajkumar et al., 2010; O'Brien et al., 2014). Another important role in managing the accessibility of metal ions to plant roots is played by soil micro-organisms in the rhizosphere as well as the enzymes secreted by them (Burns and Dick, 2002). The portion of metal ions that can translocate and get absorbed by the plants is called the bioavailable portion. Therefore, it is very crucial to identify the bioavailable portion of the total heavy metals in the soil for successful reclamation of polluted soil (Olaniran et al., 2013). There are two processes that facilitate the uptake of metal ions into roots, one is passive diffusion from the cell membrane and the other is active transport against concentration or electrochemical potential gradients intervened by carriers. These carriers may be complexing agents, like proteins or organic acids that react with metal ions (Fergusson, 1990).
Generally, metal ions penetrate root cells through two available pathways: apoplastic and symplastic. The former is feasible in only as non-cationic metal chelates, as increased cation exchange capacity is exhibited by the cell wall (Raskin et al., 1997). Therefore, immobilization in apoplastic and symplastic compartments is achieved by forming phosphates, sulfates, or carbonate precipitates, because many of the metal/metalloid cannot translocate themselves in vascular system (Garbisu and Alkorta, 2001). For symplastic movement metal ions must traverse through the plasma membrane. The internal movement of metal ions is facilitated by electrochemical gradients produced due to the high negative resting potential of the plasma membrane (Raskin et al., 1994). Also, through stele the bio-accumulated metal ions in the vacuoles may penetrate xylem tissue. Therefore, the penetration of metals into the xylem through root is decided by three processes: (i) metal ion sequestration into root cells; (ii) symplasmic transport in the stele; and (iii) release into the xylem (Saxena and Misra, 2010).
For instance, it has been reported that under Al-stress, the roots of buckwheat secret oxalic acid to form non-toxic Al-oxalate complexes which gets transferred into the leaves (Ma et al., 1998; Hall, 2002). Likewise, several fern species have been examined for their As accumulation potential in their fronds. Ma et al. (2001) was the first to identify the ability of Chinese brake fern (Pteris vittata) to hyper-accumulate As (more than 1,000 mg As/ kg shoot dry weight, DW). This plant has the capacity to transform As (V) to As (III) and transports it via xylem as an As (III)-S compound along with water and minerals, and gets accumulated in the fronds as As (III). Likewise, Wang et al. (2002) also investigated that P. vittata, when introduced to high doses of As in hydroponic media, has the capability to hyper-accumulate up to 27,000 mg kg−1 DW of As. Few other plant species like A. thaliana and Brassica juncea also reduce As (V) but have lower capacity than P. vittata (Singh and Ma, 2006). Additionally, the improper removal of Cd waste has caused emission problems in densely populated regions of the world (Järup, 2003). The plasma membrane of the root cells is characterized by electrochemical potential gradient that forces Cd or other ions in the root cells (Blaylock and Huang, 2000). Though, the concentration of Fe ion inhibits the uptake of Cd. For example, Fe concentrations of 0–10 μM inhibit Cd uptake in Hordeum vulgare (barley) (Sharma et al., 2004). Conversely, in Thlaspi caerulescens Ganges ecotype, the expression of encoding genes for Fe(II) gets upregulated by the deficiency in Fe that supports the uptake of Cd (Lombi et al., 2002). Furthermore, in Arabidopsis halleri, the translocation of Cd into the xylem of roots is partly shared with Fe and/or Zn transport (Ueno et al., 2008). However, in maize plants (Zea mays), phytosiderophore 2-deoxymugineic acid (DMA) is discharged due to introduction of Cd under Fe deficit conditions and chelates Cd. The uptake of Fe and Cd is facilitated by this weak complex. Transmission of toxic metal from soil to plant and then ultimately to humans has been poorly examined. Evidence shows that mostly end consumers are at risk when agricultural production contains excessive toxic metals. However, with the advancement in phytoremediation studies and genetic modification of plants to enhance their bio-accumulation capacity, the possibility of undesired danger of metal contamination through bio-accumulation in plants has increased. For this reason, risk assessment analysis must be incorporated in phytoremediation projects along with precautions to minimize the transfer of toxic metals to higher trophic level.
Plants have to continuously deal with abiotic and biotic stress. However, a few plants (hyperaccumulator) function extremely well under high ROS generation due to heavy metal stress. To counter oxidative damage the plants have derived an array of defense mechanisms to abort cell injury and tissue dysfunction (Benekos et al., 2010; Ruan et al., 2011) which operate indivdually or together in plants. The capability of plant defense mechanisms depends upon plant species, plant maturity and the continuation and degree of exposure. Specific plant parts are involved in heavy metal sequestration or detoxification, like trichomes (Küpper et al., 2000), epidermis (Freeman et al., 2006), cuticle (Robinson et al., 2003), and if not detoxified causes disruption of the photosynthetic apparatus. Furthermore, plant root cells are the main centers for sequestering heavy metals absorbed by the plants.
Root cells detoxify heavy metal by making complexes with amino acids, organic acids, or in vacuoles (Rascio and Navari-Izzo, 2011). These complexes check the mobility of heavy metal and consequently help in leaf tissue protection along with metabolically dynamic photosynthetic cells from heavy metal injury (Rascio and Navari-Izzo, 2011). When plants are subjected to increased concentration of heavy metal then toxicity can only be minimized through strong defense mechanisms and adequate sinks for accumulating toxic metals (Wojas et al., 2010; Hassan and Aarts, 2011; Ali et al., 2013; Sharma et al., 2016). If plants comprise these sinks, they can remove the deleterious effects of these metals. Plant metal homeostasis and metal detoxification occur mainly during vacuolar sequestration (Ali et al., 2013; Sharma et al., 2016). Various pathways have been adopted during metal sequestration in vacuoles. Metal homeostasis in plants is operated by a range of families of transporters identified by genome sequencing (Klatte et al., 2009). These families of transporters are heavy metal ATPases (HMAs), ATP-binding cassettes (ABC), Zrt/Irt-like protein (ZIP), cation exchangers (CAXs), cation diffusion facilitators (CDF), and natural resistance-associated macrophage (NRAMP) (Hall and Williams, 2003; Grotz and Guerinot, 2006; Ovečka and Takác, 2014; Thakur et al., 2016). Amongst these transporters, NRAMP, CDF, and ABC have been recognized as decisive for heavy metal tolerance (Hanikenne et al., 2005; Chaffai and Koyama, 2011; Ovečka and Takác, 2014). Moreover, Phytochelatins (PCs) and metallothioneins (MTs) are the most vital metal-binding ligands found in plant cells (Rea, 2012; Ovečka and Takác, 2014; Inouhe et al., 2015). Phytochelatins are tiny HM binding polypeptides having structure of (γ-Glu-Cys)nGly (n = 2–11). Phytochelatins fits in various classes of cysteine-rich HM-binding protein molecules. Heavy metals activate phytochelatin synthase (PCS), further stimulating PCs (Jiang and Liu, 2010; Ovečka and Takác, 2014). Metal ions such as Pb, Cd, Cu, and Zn activates the synthesis of PCs which gets catalyzed non-translationally by phytochelatin synthase (Ogawa et al., 2011; Ovečka and Takác, 2014). These natural chelators in plants bind and translocate heavy metals toward cell vacuole (Israr et al., 2011; Inouhe et al., 2015). It is presumed that the translocation of metal-PC complex is assisted by ABC transporters (Prévéral et al., 2009). Usually, in cytosol PCs binds heavy metal and this resultant complex is sequestered in vacuoles (Ogawa et al., 2011; Sharma et al., 2016). As a result, concentration of free metal ions are reduced in the cytosol. In such a way, ROS generation gets inhibited by natural ligands which are the outcome of HM interaction with redox system of the plant.
A sulfur containing tri-peptide, glutathione (GSH; γ-glutamatecysteine-glycine) is amongst the most significant low molecular weight biological thiols. Glutathione defends plants against metal toxicity by extinguishing metal-induced ROS (Noctor et al., 2012; Viehweger, 2014). A series of ROS react non-enzymatically with glutathione and the resultant formation is thiyl radicals (Mahmood et al., 2016). These radicals might produce , which gets counter balanced by SOD/CAT enzymes. It is noteworthy that GSH also reacts with LPO (lipid peroxidation) metabolite 4-hydroxy-2-nonenal (Wonisch et al., 1997), and exhibit a major role in the preliminary resistance against malondialdehyde (a highly lethal LPO product) (Turton et al., 1997). Elevated level of proline accumulation in heavily HM stressed plants is documented in several reports, which is due to glutathione production, which is also in correlation with less damage to plant protein and membranes (Liu et al., 2009). Likewise, thiol group of cysteine is tremendously susceptible to ROS because of its hypersensitivity toward oxidation. Another tolerance mechanism that has been developed by plants in order to protect proteins from oxidation is glutathionylation, whose outcome is reversible post-translational alteration of protein thiols (Michelet et al., 2006; Zaffagnini et al., 2012; Asgher et al., 2017). Additionally, plants have another mechanism to detoxify any free radical which is achieved by triggering antioxidant enzymes such as CAT, GR, APX, POD, SOD, dehydroascorbate reductase (DHAR), and mono-dehydroascorbate reductase (MDHAR) (Vanhoudt et al., 2011; Cestone et al., 2012; Shahid et al., 2014; Nahar et al., 2016; Rajewska et al., 2016). Previously, many researchers have proved that elevated level of antioxidant enzymes can boost stress tolerance. The antioxidant enzymes get triggered in various plant parts in order to scavenge the ROS species which are generated during HM toxicity (He et al., 2011; Cestone et al., 2012; Shahid et al., 2014). In addition to this, the bacteria that can produce siderophores, 1-aminocyclopropane- 1-carboxylate (AAC) deaminase and auxin (IAA) play a significant role in plant growth promotion, lowering the level of ethylene by cleaving AAC (precursor of ethylene that level increase in the presence of heavy metal) to ammonia and α- ketobutyrate, and in supplying iron to the plants for optimal growth (Wang et al., 2000; Glick, 2014). Siderophores are small organic molecules produced by microorganisms under iron limiting environment which promote the uptake of iron to the microorganisms (Saha et al., 2016). Though, the main role of siderophores is the chelation of ferric ion, but they also play a significant role in neutralizing toxic metals such as Cr, Cu, Al, and Pb in contaminated soil (Rajkumar et al., 2010; O'Brien et al., 2014). The mobility of siderophore bound heavy metals other than iron in the cell is not efficient while iron moves into the cells efficiently (Braud et al., 2009; Noinaj et al., 2010). For example, siderophore producing Pseudomonas azotoformans helps in removing As from contaminated sites (Nair et al., 2007). Likewise, siderophores also play an important role in mobilizing metals from mine waste (Edberg et al., 2010). Therefore, siderophores could be used as bioremediating agent for metals.
Heavy metals usually have low mobility in the soil and therefore are not easily absorbed by the plant roots. Thus, the interaction between plant roots and soil microbes could improve the bioavailability of heavy metals in rhizosphere (Saravanan et al., 2007; Sheng et al., 2008). Although, there are many literatures available for soil-bacteria assisted phytoremediation but our knowledge about potential of endophytic bacteria in phytoremediation of heavy- metal contaminated soils is still in their infancy (Sheng et al., 2008). Li et al. (2012) tested an endophytic fungus in rice (O. sativa L.) subjected to different concentration of lead (Pb) stress. The results showed significantly higher chlorophyll and carotenoid content in the endophyte infected seedlings compared to non-infected seedlings. Likewise, net photosynthetic rate, transpiration rate, and water use efficiency were significantly higher in endophyte infected seedlings compared to non-infected seedlings under higher concentrations of Pb.
Concluding Remarks and Future Perspective
Heavy metal pollution poses serious environmental threat on a global scale. When plants are introduced to the elevated toxic level of heavy metal/ metalloid they demonstrate significantly reduced growth accompanied with poor productivity and yields. Heavy metal pollution destroys plants' cellular structures and membranes due to elevated ROS species production. ROS species also inhibit basic metabolism of plants and transport processes within the plant. However, abiotic stresses (like drought and salinity) can also cause these adverse effects. But, plants combating heavy metal stress have some exceptional features. Plants alleviate the effects of heavy metal toxicity by limiting the uptake of metal/metalloids ions, complexing and chelating them either in extracellular space or in the cytoplasm, and possibly sequestration in the vacuole. To achieve this, the plant must be proficient enough to trigger defense responses like activation and expression of antioxidative enzymes. In addition to this, plants must regulate their mechanisms for averting or fixing secondary defects produced during oxidative stress. However, diverse plant species develop different strategies to combat the problem of heavy metal toxicity. Increased uptake of metal ions by plants also demonstrates elevated level of metals in the soil (esp. metals which are mobile). Beyond a certain critical concentrations of heavy metals, plants' yield and quality are severely affected which can influence animal and human health. Careful monitoring is required to evaluate the concentrations of toxic heavy metals in plants as they may potentially reach the danger level in animal or human being via the food chain without having any deleterious effect on plants. Heavy metals are frequently associated with other major nutrients that have synergistic, additive, or antagonistic effects. Hence, the sustenance and vigor of our future generation requires that the soil resources must be preserved from slow and insidious poisoning of heavy metals. This proves to be the biggest challenge for our scientific investigators, advisors, and legislators. Another important challenge to be faced by the scientist is a long-term prediction of possible hazards in soils arising from different soil conditions. Therefore, scientists from all over the globe can and should continue to cooperate in investigations and development of stringent guidelines for disposal and use of toxic metals in agricultural soil.
Author Contributions
RS, VS, and AS proposed and structured the review. VS, AS, and PS wrote the manuscript. AS made the figure. SS and AdA reviewed and improved English of the manuscript. All the authors participated in discussion of the research.
Conflict of Interest Statement
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Acknowledgments
Authors are thankful to the Director, Dean, and Head, Institute of Environment and Sustainable Development, Banaras Hindu University for providing the necessary facilities. RS is thankful to Department of Science and Technology, India, University of Nebraska–Lincoln, Indo-US Science and Technology Forum (IUSSTF) and Robert Daugherty Water for Food Institute (DWFI)—University of Nebraska for support. AS is thankful to the HoD, Department of Botany, University of Gour Banga, for this collaborative work. The authors extend their sincere thanks to Dr. Shannon L. Bartelt-Hunt, Department of Civil Engineering, University of Nebraska-Lincoln, USA for improving the English and grammar of the manuscript.
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Keywords: heavy metal, contamination, toxicity, soil health, plant metabolism, soil microflora
Citation: Srivastava V, Sarkar A, Singh S, Singh P, de Araujo ASF and Singh RP (2017) Agroecological Responses of Heavy Metal Pollution with Special Emphasis on Soil Health and Plant Performances. Front. Environ. Sci. 5:64. doi: 10.3389/fenvs.2017.00064
Received: 08 April 2017; Accepted: 29 September 2017;
Published: 16 October 2017.
Edited by:
Tripti Agarwal, National Institute of Food Technology Entrepreneurship and Management, IndiaReviewed by:
Srinivasan Balachandran, Visva-Bharati University, IndiaNaveen Kumar Singh, Manipal University Jaipur, India
Copyright © 2017 Srivastava, Sarkar, Singh, Singh, de Araujo and Singh. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Rajeev P. Singh, rajeevprataps@gmail.com
Abhijit Sarkar, abhijitbhu@gmail.com