Environmental Microbiology | Biodegradation and Bioremediation
Microbiol. Biotechnol. Lett. 2023; 51(1): 1-9
https://doi.org/10.48022/mbl.2212.12003
Shamayita Basu, Samir Kumar Mukherjee, and Sk Tofajjen Hossain*
Department of Microbiology, University of Kalyani, Kalyani 741235, India
Correspondence to :
Sk Tofajjen Hossain, sktofajjen.hossain@gmail.com
Arsenic (As), which is ubiquitous throughout the environment, represents a major environmental threat at higher concentration and poses a global public health concern in certain geographic areas. Most of the conventional arsenic remediation techniques that are currently in use have certain limitations. This situation necessitates a potential remediation strategy, and in this regard bioremediation technology is increasingly important. Being the oldest representativse of life on Earth, microbes have developed various strategies to cope with hostile environments containing different toxic metals or metalloids including As. Such conditions prompted the evolution of numerous genetic systems that have enabled many microbes to utilize this metalloid in their metabolic activities. Therefore, within a certain scope bacterial isolates could be helpful for sustainable management of As-contamination. Research interest in microbial As(III) oxidation has increased recently, as oxidation of As(III) to less hazardous As(V) is viewed as a strategy to ameliorate its adverse impact. In this review, the novelty of As(III) oxidation is highlighted and the implication of As(III)-oxidizing microbes in environmental management and their prospects are also discussed. Moreover, future exploitation of As(III)-oxidizing bacteria, as potential plant growth-promoting bacteria, may add agronomic importance to their widespread utilization in managing soil quality and yield output of major field crops, in addition to reducing As accumulation and toxicity in crops.
Keywords: Arsenic, environmental pollution, arsenic detoxification, microbial arsenite oxidation, bioremediation
Decontamination of hazardous substances is a challenge both in technological and scientific reality [1]. Arsenic (As) is considered as global threat among such hazardous soil and water pollutants, which has a negative impact on human health [2]. Since the beginning of geological time, As is ubiquitous to earth's crusts, soil, sediments, aquifers, and living things. It has become a significant global environmental issue during last few decades. Geographical area of 0.173 million Km2 in West Bengal, India, where several million people are under the threat due to continuous As exposure [3]. Drinking water is the primary source of dietary exposure to inorganic As in humans, due to its natural occurrence in aquifers. Besides soil contamination with As due to various anthropogenic activities, irrigation with As-contaminated groundwater results in the accumulation in crops, eventually which enter the food chain and cause widespread exposure to As [4]. Therefore, for the general population, consumption of As containing food and As-contaminated groundwater are the major reasons for hazardous impact of As on human health. Environmentalists are facing a huge challenge for a sustainable approach to detoxify the environment contaminated with As, the most common methods rely on various physico-chemical techniques, however, currently As-resistant microorganisms have been shown to be both economically and environmentally sustainable [5]. Since As has been present on earth since the beginning of time and Asresistant genes have been found in microbiota, a variety of resistance mechanisms have been common, which could be a better option for developing As detoxification method. This review gives an insight of prevalent As bioremediation applications with an emphasis on perspectives of applying indigenous As(III) oxidizing bacteria for possible As detoxification.
Arsenic (As), a metalloid, ranked as the 20th most plentiful element in the earth's crust, is toxic to most living organisms. The continental crusts typically contain 2 to 3 mg/kg of As on an average [6]. As-contaminations either from geogenic or anthropogenic sources are badly jeopardizing public health globally, especially it is a huge concern in the Bengal delta of south Asia [4, 7]. The alluvial soil tract of Bangladesh and Gangetic plain of India are the main geogenic sources of As, where reports of arsenic availability in soil or water are above the recommended level [4]. Out of several mineral forms of As, the principal forms can be classified into arsenates, and arseno-pyritic salts. As(III) and As(V) are the most prevalent oxidation states of As in soil and water. Generally, in an oxidative environment, As(V) predominates, whereas in a reducing environment, As(III) is abundant.
Globally, millions of people consume As above the permissible level through drinking water due to the existence of As-rich geological formation in aquifers and/ or anthropogenic behaviours in certain geographical areas [2, 5, 7]. Several crops like rice accumulate high amount of As easily from contaminated soil, so regular consumption of As accumulated food grains creates huge health concern among the people dwelling in such area. Arsenic is classified as an established carcinogen by the WHO-IARC, an arm of the World Health Organization [2]. Various health ailments were reported as the major consequences upon prolonged consumption of Ascontaminated water or food, collectively called arsenicosis [7]. Higher amounts of As accumulation in body can produce severe intoxication, leading to gastrointestinal problems, cardiovascular problems, dysfunction of neuronal system, and even may results fatality. According to the most recent WHO assessment, As exposure to humans from drinking water is the main cause of kidney, skin, and bladder malignancies [2].
The physico-chemical treatment techniques make up the majority of the traditional arsenic removal methods to date. Coagulation-precipitation, adsorption, ion exchange, membrane filtration etc. are examples of physico-chemical technologies. In the coagulation-precipitation process, coagulants convert soluble As forms into insoluble solids [8]. Physical adsorption of As on the surface of appropriate adsorbent results immobilization of As in water. When treating contaminated water through an ion exchange column, synthetic resins are utilized as the solid phase because they are effective at adsorbing As ions [9]. This metalloid can be eliminated from a water system via membrane-filtration, that involves a number of distinct processes, including electrodialysis, reverse osmosis, ultrafiltration, and nano-filtration [9].
All of these conventional procedures are not always environment friendlyor cost-effective, often resultrelease of hazardous chemicals, and are often tedious and time consuming. Hence, as an alternative, biological treatment processes like phytoremediation and microbial remediation might be good options and are getting huge attention currently. Phytoremediation or microbeassisted phytoremediation is now being considered as potential tools to get rid of hazardous chemicals including toxic metals/metalloids from the environment [10]. Plants those having high As resistance, hyperaccumulation ability, high propagating ability, potential biomass productivity, and widespread dispersion are reported to be useful for As phytoremediation [10]. Microbial remediation is the deployment of microorganisms to remove, and to change harmful substances into less hazardous forms in the ecosystem [11].
Microorganisms have a variety of ways to interact with different toxic metals, making their use in heavy metal disposal and environmental remediation unique. The success of the microorganism-based remediation method mostly depends on the exploitation of microorganisms' ability to survive under toxic metal contaminated habitat [11]. Microbial transformation is a key component of the biogeochemical cycle of As (Fig. 1), which has an impact on the solubility and distribution of various As forms in nature [7, 12]. As a part of survival strategy in the As-contaminated habitat, bacteria have developed a number of As-resistance mechanisms that use incredibly precise metabolic pathways to guard against As toxicity [13, 14]. The principles of the mechanisms are briefly presented in Fig. 2.
Mobilization and immobilization — Fe+3-reducing microbes produce energy by combining the reduction of Fe+3 with the oxidation of As(V)-containing electron sources. Arsenic is thus, mobilized into the environment, as a result of dissolution of minerals containing Fe+3 [15]. On the other hand, iron-oxidizing bacteria oxidizes Fe+2 to Fe+3 and the resulted electron oxidizes As(III) to immobilized As(V) [15]. Thus, both iron-oxidizing and iron-reducing bacterial community contribute in mobilization and immobilization of As species and play crucial role in geochemical cycle of As.
Adsorption — The most effective methods for employing microbes to detoxify different hazardous metals are adsorption approaches [16]. Since As(V) is present in neutral aqueous solutions as oxide anions, while As(III) behaves neutrally so far the charge is concern and thus both do not adsorb on microbial cell surface. Therefore, in order for As to be adsorbed, the microbes' surfaces either need to be altered through pre-processing [16], or it could happen naturally as a result of cell surface components- extracellular substances [17].
Methylation and volatilization — There are several publications on the methylation of As by fungus and other eukaryotes; conversely, there are few reports on the methylation of As by bacteria [18, 19]. It is seen to be a difficult possibility to use arsenic methylation to potentially bioremediate a polluted environment by volatilization. As(V) is converted to volatilized arsines through a series of reactions that begins with its reduction, and ends with inclusion of -CH3 group by oxidation [19]. The resulted methylated arsenicals may vary conditionally on the nature of the -CH3 group donor and the reaction process [18, 19]. Arsenic volatilization has been attributed by the function of
Oxidation and reduction — A variety of microbiological metabolic processes contribute in As cycling, including both reduction and oxidation, in soil, sediment, and natural water systems [12, 13, 23]. As(III) and As(V) are the only ecologically significant inorganic As species, however, the biological processes contributing in As biorecycling are rather multifaceted. In major cases, As(III) is more hazardous than As(V). Numerous chemolithoautotrophic and heterotrophic bacteria participate in the transformation of As(III) to comparatively non-hazardous compound As(V) known as arsenate [24]. As(V) can be reduced by two separate physiological groups, each serving a different function. As(V) can be used as a terminal acceptor of electrons by various chemolithoautotrophic bacteria, including
Green first reported on As(III) oxidizing bacteria [27], and thereafter many environmental microbiologists documented As(III) oxidation by various bacterial communities [28, 29]. Majority of such bacterial strains were cultivated as lithotrophs and continued to be able to employ As(III) as the specific electron donor [30]. As(III)- oxidizing heterotrophic bacteria can receive energy through As(III) oxidation and as a result, arsenic detoxification occurred [31].
For the detoxification of waste or ground water contaminated with As, the biological oxidation of As(III) using bacteria is of special importance. By turning more harmful As(III) into less mobile and less toxic As(V) molecules, microbial oxidation of As is a crucial link in the global As cycle [31]. To date numerous As(III)-oxidizing bacteria from various aquatic and soil habitats have been isolated, and were reported to be phylogenetically diverse (Table 1) [5, 28, 32−57].
Table 1 . As(III) oxidizing bacterial diversity and their environmental sources.
As(III) oxidizing bacteria | Source environment | References |
---|---|---|
Soil | 32 | |
Gold tailings soil | 33 | |
Anaeromyxobacter spp. | Soils and sediments | 34 |
Soil | 35 | |
Shallow aquifer | 6 | |
Ground water | 37 | |
Mine soil | 38 | |
Mine slag | 39 | |
Contaminated soil | 40 | |
Shallow aquifers | 41 | |
High Andean watershed | 42 | |
Fly Ash Pond | 43 | |
Industrial waste | 44 | |
Soil | 45 | |
Contaminated soil | 46 | |
Contaminated soil | 47 | |
Contaminated soil | 48 | |
Rhizosphere | 49 | |
Contaminated soil | 50 | |
Shallow aquifer | 51 | |
Contaminated soil | 5 | |
Industrial sludge | 52 | |
Soil | 53 | |
Sewage sample | 54 | |
Aquatic macrophyte | 28 | |
Terrestrial geothermal habitat | 55 | |
Hot spring | 56 | |
α-Proteobacteria NT-26 | Gold mine | 57 |
Since As(III) can operate as an electron donor during this process, As(III) oxidation is an energy-producing reaction [13, 23, 25]. To date diverse microbial community have been reported to obtain energy by redox processes of As oxyanions [14]. The rapid oxidation of As(III) in a hot spring habitat has been attributed to microbial mats made primarily of filamentous microorganisms [56]. Evidence for As(III)-assisted anoxygenic photosynthesis was reported among the mat-forming photosynthetic bacteria in lentic ecosystem [58]. Additionally, they offered proof of purple bacteria growing photoautotrophically, assisted by As(III) oxidation to As(V). As(III) is used as an energy source in chemolithoautotrophic microbes [57]. As(III) was also reported to be oxidized outside the cells As(III) oxidase [56] and is currently gaining importance for enzymatic oxidation under cellfree conditions.
Oxidation by As(III) Oxidase — As(III) is converted to As(V) through the process of oxidation, which is carried out by the enzyme As(III) oxidase, a product of
As(III) Oxidase Genes — The As(III) oxidase is a heterotetramer AioBA catalytic protein, which is made of a large (AioA) and a small subunit (AioB) encoded by
Capacity of enzymatic oxidation of As(III) by various As(III)-oxidizing bacteria are considered to be the prospective candidates for detoxification of areas having higher level of arsenic [72]. As(III)-oxidizing bacteria can directly alter the redox states of arsenicals, though they can also facilitate the accumulation of As by plants. For instance, alfalfa showed increased growth and arsenicuptake efficiency when inoculated with
Due to its toxicity, endurance, and bioaccumulation, As is a hazardous metalloid, just like other toxic metals. In nature, bacteria contribute a huge role in chemical cycling of As owing to their acquired resistance, and thus could be the potential tools in As decontamination, especially in the affected area. Oxidation of As(III) to As(V) is generally perform by As(III)-oxidizing microbes, leading to higher rate of immobilization of arsenic on solid surfaces. Additionally, immobilized As(V) could easily be separated from the ambient condition, especially for the detoxification of drinking water by ecofriendly physico-chemical methods. Further exploitation of this ability of As(III)-oxidizing bacteria by utilizing them as Plant Growth Promoting Rhizobacteria, may result in reduction of As accumulation and toxicity in plants, thereby avoiding human As exposure via crops. It is another aspect of the novelty of As(III)-oxidizing bacteria in environmental As remediation. Thus, it can be concluded that As(III)-oxidizing bacteria are probably one of the most preferable tools for As bioremediation in the present scenario for environmental sustainability.
The authors have no financial conflicts of interest to declare.
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