Toxicity and bioaccumulation of chromium in some freshwater fish

Chromium (Cr) is a common pollutant of freshwater bodies in India, and is frequently detected in high concentrations in edible fish. Bioassays were carried out in the laboratory to determine acute the toxicity and pattern of accumulation of Cr in three species of freshwater fish. The 96-h LC₅₀ value of Cr for Labeo bata, Puntius sarana, and Catla catla was found respectively as 7.33, 10.37, and 31.61 mg/L. Concentrations of Cr in water, sediments, and fish, during a period of 28 d of exposure to 0, 0.73, and 2.19 mg/L of Cr, varied with exposure period, concentration of Cr, presence of weed, and species of fish exposed. Polynomial regressions obtained by drawing polynomial curves revealed that the aquatic weed Eichhornia crassipes prevented gradual decrease of Cr concentrations in water, but reduced the accumulation of Cr in L. bata and Catla catla. However, the effect of the weed on Puntius sarana was not apparent. The pattern of Cr deposition on sediments was also inconsistent. To explain interactions between environment and fish in a very precise manner, polynomial and multiple regression curves were simultaneously used. When polynomial curves were replaced by multiple regression curves, it was revealed that the aquatic weed E. crassipes could reduce Cr accumulation in Puntius sarana also.     

Toxicity and bioaccumulation of cadmium and lead in aquatic invertebrates

Cadmium toxicity and lead toxicity to four species of insects (Pteronarcys dorsata, Hydropsyche betteni, Brachycentrus sp. and Ephemerella sp.), one snail (Physa integra) and one amphipod (Gammarus pseudolimnaeus) were determined during 28-day exposures. The 28-day LC50 values for cadmium-exposed snails and lead-exposed amphipods were eleven and four times lower than the 7- and 4-day (96 h) values for these metals, respectively. Lowest effect concentrations obtained after 28 days for cadmium-exposed mayflies (Ephemerella sp.) and snails and lead-exposed amphipods were similar to those affecting fish exposed over their complete life cycle in water of similar quality. Lethal threshold concentrations were not observed for species exposed to either metal, indicating that possible effects could occur at lower concentrations during longer exposure periods. Cadmium and lead concentrations in the animals tested generally increased with increasing water concentrations and were up to 30,000 and 9000 times greater than corresponding metal concentrations in the water.     

Toxicity and bioremediation of pesticides in agricultural soil

Pesticides are one of the persistent organic pollutants which are of concern due to their occurrence in various ecosystems. In nature, the pesticide residues are subjected to physical, chemical and biochemical degradation process, but because of its high stability and water solubility, the pesticide residues persist in the environment. Moreover, the prevailing environmental conditions like the soil characteristics also contribute for their persistence. Bioremediation is one of the options for the removal of pesticides from environment. One important uncertainty associated with the implementation of bioremediation is the low bioavailability of some of the pesticides in the heterogeneous subsurface environment. Bioavailability of a compound depends on numerous factors within the cells of microorganism like the transportation of susbstrate across cell membrane, enzymatic reactions, biosurfactant production etc. as well as environment conditions such as pH, temperature, availability of electron acceptor etc. Pesticides like dichlorodiphenyltrichloroethane (DDT), hexachlorocyclohexane (HCH), Endosulfan, benzene hexa chloride (BHC), Atrazine etc. are such ubiquitous compounds which persist in soil and sediments due to less bioavailability. The half life of such less bioavailable pesticides ranges from 100 to 200 days. Most of these residues get adsorbed to soil particles and thereby becomes unavailable to microbes. In this review, an attempt has been made to present a brief idea on ‘major limitations in pesticide biodegradation in soil’ highlighting a few studies.     

Toxicity of flue gas components from cement plants in microalgae CO2 mitigation systems

Microalgae-based CO₂ capture from flue gas is an attractive mitigation strategy in the cement industry. However, NO _x and SO _x components might be harmful to microalgae. We performed toxicity assays, under 2 % (v/v) CO₂ and using nitrite, sulfite, or bisulfite salts, on an environmental isolate, identified as Desmodesmus abundans (The University of Texas at Austin (UTEX), no. 2976) and Scenedesmus sp. UTEX1589. Nitrite and sulfite did not inhibit growth at the tested concentrations (0–1,067 ppm (w/v) NO₂ ^? and 0–254 ppm (w/v) SO₃ ^2?); however, bisulfite was toxic above 39 ppm. Non-toxic concentrations of both sulfur-based compounds stimulated growth, but significantly higher growth rates were only observed for HSO₃ ^?. Within a narrower range, NO _x and SO _x served as a sole nutrient source. Overall, biomass production and growth rates of the environmental isolate were greater. A novel strategy to buffer high concentrations of HSO₃ ^? (200 ppm) was developed by adding cement kiln dust (CKD), a byproduct and flue gas component. The results suggest that CKD also provided other beneficial growth components and that sulfur optimization of the culture medium significantly increased carbon assimilation, particularly in D. abundans. In additional simulations of typical flue gas conditions in a modern cement plant (320, 40, and 40 ppm (w/v) of NO₂ ^?, SO₃ ^2?, and HSO₃ ^?, respectively, and 25 % (v/v) CO₂), along with the incorporation of 300 ppm CDK, growth of D. abundans was supported. Although further studies are needed, direct utilization of flue gas might be possible with the environmental isolate, where NO _x , SO _x , and CKD are all beneficial components of the mitigation system.     

Toxicity of bisphenol A and its structural congeners to microalgae Chlorella vulgaris and Desmodesmus armatus

Journal of Applied Phycology - Bisphenol A and its structural congeners are increasingly recognized as emerging contaminants with toxic and estrogenic potential that have been widely used in many...     

Enhanced roles of biochar and organic fertilizer in microalgae for soil carbon sink

Improved soil carbon sink capability is important for the mitigation of carbon dioxide emissions and the enhancement of soil productivity. Biochar and organic fertilizer (OF) showed a significant improving effect on microalgae in soil carbon sink capacity, and the ultimate soil total organic carbons with microalgae-OF, microalgae-biochar, microalgae-OF-biochar were about 16, 67 and 58% higher than that with microalgae alone, respectively, indicating that carbon fixation efficiency of microalgae applied in soil was improved with biochar and OF whilst the soil carbon capacity was promoted, the mechanism of which is illustrated through simulative experiments. Organic fertilizer could spur algal conversion of carbon into cell molecules by increasing intracellular polysaccharide production of microalgae. Biochar could change carbon metabolism pathway of microalgae through altering the yield of intracellular saccharides, and yield and type of extracellular saccharides. There was a superimposition effect on the soil carbon sink when biochar and OF were both present with microalgae.     

Ability of marine eukaryotic red tide microalgae to utilize insoluble iron

Iron is an essential trace metal and a limiting factor for microalgal growth, but bioavailable dissolved iron concentrations in seawater are low. Microalgal blooms have frequently occurred in coastal areas under such iron limitation accompanied by mass mortalities of fish and bivalves. Their massive growth despite physiological iron-deficiency has long been an enigma, because most of them cannot grow in chemically defined artificial media. We developed a feasible artificial medium for the culture of many species of red tide microalgae modified for investigation of iron utilization. Here, we report on the ability of marine eukaryotic red tide microalgae to utilize insoluble iron. Some microalgal species could utilize particulate FePO₄ and FeS for growth. Particulate FePO₄ was available for the growth of the raphidophyte Heterosigma akashiwo, the dinoflagellate Heterocapsa triquetra and the diatom Ditylum brightwellii. The dinoflagellates Heterocapsa circularisquama and Karenia mikimotoi, and the cryptophyte Rhodomonas ovalis utilized both particulate FePO₄ and particulate FeS for growth. In contrast, particulate FeO(OH) and Fe₂O₃ did not support the growth of any of the red tide microalgae examined. Except for Chattonella species (Raphidophyceae), the growth of red tide microalgae were confirmed in the medium with very easily soluble FeCl₃ added. The order of bioavailability of tested iron-source species were Fe–EDTA > FeCl₃ > FePO₄ > FeS > FeO(OH), Fe₂O₃ for most of microalgae examined, although for H. circularisquama the utilization of FeCl₃ was higher than that of Fe–EDTA. The results suggest that red tide microalgae show different patterns of specific strategies for the utilization of various iron sources. The occurrence of red tides in coastal areas may depend on the combination of microalgal species and insoluble iron species present.     

Toxicity of nano-zero valent iron to freshwater and marine organisms

We tested whether three commercial forms (uncoated, organic coating, and iron oxide coating) of nano zero-valent iron (nZVI) are toxic to freshwater and marine organisms, specifically three species of marine phytoplankton, one species of freshwater phytoplankton, and a freshwater zooplankton species (Daphnia magna), because these organisms may be exposed downstream of where nZVI is applied to remediate polluted soil. The aggregation and reactivity of the three types of nZVI varied considerably, which was reflected in their toxicity. Since levels of Fe(2+) and Fe(3+) increase as the nZVI react, we also evaluated their toxicity independently. All four phytoplankton species displayed decreasing population growth rates, and Daphnia magna showed increasing mortality, in response to increasing levels of nZVI, and to a lesser degree with increasing Fe(2+) and Fe(3+). All forms of nZVI aggregated in soil and water, especially in the presence of a high concentration of calcium ions in groundwater, thus reducing their transports through the environment. However, uncoated nZVI aggregated extremely rapidly, thus vastly reducing the probability of environmental transport and potential for toxicity. This information can be used to design a risk management strategy to arrest the transport of injected nZVI beyond the intended remediation area, by injecting inert calcium salts as a barrier to transport.     

Complexation of iron by microbial siderophores and effects of iron chelates on the growth of marine microalgae causing red tides

The growth rates of 13 species of abundant red tide algae in media with different iron species complexed with microbial siderophores (Ferrichrome and Ferrioxamine) and Fe‐Catechol were investigated. Our study demonstrated that the Fe‐chelates (at molar ratios = 1:1) were bioavailable to some red tide species. In Fe‐Catechol medium, growth was observed for the raphidophyte Heterosigma akashiwo, the dinoflagellates Heterocapsa circularisquama and Heterocapsa triquetra, the diatom Ditylum brightwellii, the cryptophyte Rhodomonas ovalis, the chlorophyte Oltmannsiellopsis viridis, and the haptophyte Cricosphaera roscoffensis. In Ferrioxamine medium, we found the growth of the dinoflagellate Karenia mikimotoi, the diatom Ditylum brightwellii, and the cryptophyte Rhodomonas ovalis. But, the existence of higher ligand concentrations (molar ratios ≥ 1:10) decreased the growth rates of most red tide species that were examined. Furthermore, all red tide species examined were not able to grow in Ferrichrome medium. In particular, the Chattonella species examined did not grow in the presence of Fe‐chelates. These results suggest that bioavailability of iron depends not only on ligand species, but also on the concentration of the ligands; moreover, microbial siderophores may play an important role in controlling the uptake of iron complexed with organic materials that exist in coastal water and the formation of red tides in coastal areas.     

Enhancement of total lipid yield by nitrogen,carbon, and iron supplementation in isolated microalgae

The biochemical contents and biodiesel production ability of three microalgal strains grown under different sodium nitrate, sodium carbonate, and ferric ammonium citrate (iron) levels were investigated. The highest biomass and lipid contents were found in Scenedesmus sp., Chlorella sp., and Chlamydomonas sp. when grown in normal BG‐11 containing sodium carbonate concentration at 0.03 g · L^?1, and in normal BG‐11 containing iron concentration (IC) at 0.009 or 0.012 g · L^?1. Increasing the sodium nitrate level increased the biomass content, but decreased the lipid content in all three microalgae. Among the three microalgae, Scenedesmus sp. showed the highest total lipid yield of 0.69 g · L^?1 under the IC of 0.012 g · L^?1. Palmitic and oleic acids were the major fatty acids of Scenedesmus sp. and Chlamydomonas sp. lipids. On the other hand, Chlorella sp. lipids were rich in palmitic, oleic, and linolenic acids, and henceforth contributing to poor biodiesel properties below the standard limits. The three isolated strains had a potential for biodiesel production. Nevertheless, Scenedesmus sp. from stone quarry pond water was the most suitable source for biodiesel production with tolerance toward the high concentration of sodium carbonate without the loss of its biodiesel properties.     

Cadmium uptake and bioaccumulation in selected cultivars of durum wheat and flax as affected by soil type

Accumulation of cadmium (Cd) in crop plants is of great concern due to the potential for food chain contamination through the soil-root interface. Although Cd uptake varies considerably with plant species, the processes which determine the accumulation of Cd in plant tissues are affected by soil factors. The influence of soil type on Cd uptake by durum wheat (Triticum turgidum var. durum L.) and flax (Linum usitatissimum L.) was studied in a pot experiment under environmentally controlled growth chamber conditions. Four cultivars/lines of durum wheat (Kyle, Sceptre, DT 627, and DT 637) and three cultivars/lines of flax (Flanders, AC Emerson, and YSED 2) were grown in two Saskatchewan soils: an Orthic Gray Luvisol (low background Cd concentration; total/ABDTPA extractable Cd: 0.12/0.03 mg kg^-1, respectively) and a Dark Brown Chernozem (relatively high background Cd concentration; total/ABDTPA Cd: 0.34/0.17 mg kg^-1 respectively). Plant roots, stems, newly developed heads, and grain/seeds were analyzed for Cd concentration at three stages of plant growth: two and seven weeks after germination, and at plant maturity. The results showed that Cd bioaccumulation and distribution within the plants were strongly affected by both soil type and plant cultivar/line. The Cd concentration in roots leaves and stems varied at different stages of plant growth. However, all cultivars of both plant species grown in the Chernozemic soil accumulated more Cd in grain/seeds than plants grown in the Orthic Gray Luvisol soil. The different Cd accumulation pattern also corresponded to the levels of ABDTPA extractable and metal-organic complex bound soil Cd found in both soils. Large differences were found in grain Cd among the durum wheat cultivars grown in the same soil type, suggesting the importance of rhizosphere processes in Cd bioaccumulation and/or Cd transport processes within the plant. Distribution of Cd in parts of mature plants showed that durum grain contained up to 21 and 36% of the total amount of Cd taken up by the plants for the Orthic Gray Luvisol and Chernozemic soils, respectively. These results indicate the importance of studying Cd speciation, bioaccumulation and cycling in the environment for the management of agricultural soils and crops.     

Prediction of reducible soil iron content from iron extraction data

Soils contain various iron compounds that differ in solubility, reducibility and extractability. Moreover, the contribution of the various iron compounds to total iron (Fe) and total Fe concentrations differs highly among soils. As a result, the total reducible Fe content can also differ among soils, and so does the dynamics of iron reduction. These factors complicate the prediction of reducible Fe based on Fe extraction data and hamper the application of process-based models for reduced or waterlogged soils where redox processes play a key-role. This paper presents a theoretical analysis relating reducible to extractable Fe reported in the literature. Predictions made from this theoretical analysis were evaluated in soil incubations using 18 rice paddy soils from all over the world. The incubation studies and the literature study both show that reducible Fe can be related to Fe from some selected, but not all, iron extractions. The combination of measurements for labile Fe(III)oxides (derived from oxalate-extractable Fe) and stabile Fe(III)oxides (derived from dithionite-citrate-extractable Fe) shows highly significant correlations with reducible Fe with high coefficients of determination (r² = 0.92–0.95 depending on the definition of stabile Fe(III)oxides). Given the high diversity in rice soils used for the incubations, these regression equations will have general applicability. Application of these regression equations in combination with soil database information may improve the predictive ability of process-based models where soil redox processes are important, such as CH₄ emission models derived for rice paddies or wetlands.     

Soil microalgae and cyanobacteria: the biotechnological potential in the maintenance of soil fertility and health

Abstract

The soil microbiota plays a major role in maintaining the nutrient balance, carbon sink, and soil health. Numerous studies reported on the function of microbiota such as plant growth-promoting bacteria and fungi in soil. Although microalgae and cyanobacteria are ubiquitous in soil, very less attention has been paid on the potential of these microorganisms. The indiscriminate use of various chemicals to enhance agricultural productivity led to serious consequences like structure instability, accumulation of toxic contaminants, etc., leading to an ecological imbalance between soil, plant, and microbiota. However, the significant role of microalgae and cyanobacteria in crop productivity and other potential options has been so far undermined. The intent of the present critical review is to highlight the significance of this unique group of microorganisms in terms of maintaining soil fertility and soil health. Beneficial soil ecological applications of these two groups in enhancing plant growth, establishing interrelationships among other microbes, and detoxifying chemical agents such as insecticides, herbicides, etc. through mutualistic cooperation by synthesizing enzymes and phytohormones are presented. Since recombinant technology involving genomic integration favors the development of useful traits in microalgae and cyanobacteria for their potential application in improvement of soil fertility and health, the merits and demerits of various such advanced methodologies associated in harnessing the biotechnological potential of these photosynthetic microorganisms for sustainable agriculture were also discussed.     

Reactions of iron chelates in calcareous soil and their relative efficiency in iron nutrition of corn

Summary Laboratory incubation studies on the reactions of Fe-DTPA, Fe-EDTA, Fe-citrate and Fe-fulvate with a calcareous soil indicated that Fe³⁺ was very rapidly displaced by Ca²⁺, Mg²⁺, Zn²⁺ and Cu²⁺ ions. The displacement of iron was in the reverse order of the stability of the Fe-chelates. The activity of Fe³⁺, Ca²⁺, Mg²⁺, Zn²⁺ and Cu²⁺ tended to attain a constant value with time. Application of chelating agents to a calcareous soil mobilized different amounts of iron as defined by their relative stability and cation competition. The degree of mobilization increased with increasing levels of applied chelating agents. A significant negative correlation (r = –0.77)^* was observed between pH and DTPA-extractable iron. Results of greenhouse experiment showed significant increase in the dry matter yield and iron uptake by corn plants upon application of iron-chelates. The chelates enhance the uptake of both native and applied sources. The effectiveness of the chelates used was in the order of their capacity to maintain iron in soluble form in the soil solution. These results suggest that iron nutrition of plants in calcareous soils can be effectively regulated by the application of iron chelated by natural or synthetic water-soluble chelating agents.     

Chemical forms of plant and soil iron as influenced by soil moisture

Summary Experiments were conducted to determine whether soil moisture content has an effect on the chemical forms of plant and soil iron. Soybean plants, variety Lee, were grown on Adelanto loam soil under greenhouse conditions. Two different moisture levels, 75 per cent and 120 per cent of the moisture equivalent, were maintained in soil samples placed in individual containers. The same moisture treatments were used for separate soil samples on which the test plants were grown.Soil iron forms were determined in the moisture-treated soil by using different extracting agents. A significant decrease in soil iron extracted with 10^–4 M EDTA from soil at the high moisture level was attributed to a relative increase in the free calcium ion.Soybean plants grown under the high moisture level were chlorotic while those under the low moisture level were green in appearance. Plant samples were taken at two stages of growth for subsequent analysis.The chemical analysis of the leaf tissues have shown the presence of equal amounts of total iron and less amounts of water-soluble and active iron in chlorotic tissues as compared to non-chlorotic tissues. The difference found between chlorotic and non-chlorotic plants in the amount of iron in the water extract was in the trichloroacetic acid-soluble fraction. The water- and salt-soluble protein nitrogen was approximately the same in chlorotic and non-chlorotic leaves.     

Lead bioaccumulation,subcellular distribution and chemical form in sugarcane and its potential for phytoremediation of lead-contaminated soil

Abstract

Sugarcane is a promising species for lead (Pb) phytoextraction due to its large biomass and high tolerance toward Pb content. To understand the mechanisms involved in Pb tolerance and detoxification and its potential for phytoremediation in sugarcane, the bioaccumulation, subcellular distribution, and chemical forms of Pb in different tissues were investigated through pot cultivation sugarcane with increasing Pb concentrations in the present study. Results showed that sugarcane could tolerate high concentrations of Pb (up to 1250.0–1750.0?mg/kg); the Pb content in roots and shoots increased with increasing Pb concentration. A large amount of Pb content was stored in roots. The subcellular distribution of Pb in sugarcane revealed that the majority of Pb was bound to the cell wall. Meanwhile, the greatest amount of Pb was extracted by 2.0% acetic acid and 0.6?mol/L HCl, which indicated that most of Pb was combined with undissolved phosphate and oxalate. These results implied that the Pb formation of undissolved salts and compartmentalization in the cell wall may be a key strategy for Pb detoxicity and tolerance in sugarcane.