Protective effect exerted by soil phosphorus on soybean subjected to arsenic and fluoride

Objetive: Arsenic (As) and fluoride (F) are found in groundwater and soils around the world, causing different problems to crops. Because these elements compete against phosphorus (P) in soils and plants, their relationship is complex. The aim of this work was to study the oxidative stress of soybean plants subjected to different concentrations of As and F, and the effect of P.

Methods: The following 10 treatments were carried out in each of two soils with different P content: three As levels (low 10?mg?As?kg^-1, medium 50?mg?As?kg^?1 and high 100?mg As kg^?1), three F levels (low 160?mg?F?kg^?1, medium 250?mg?F?kg^?1 and high 500?mg?F?kg^?1) and three As?+?F levels (same concentrations), and the control treatment (soil with the background As and F concentrations) Lipid peroxidation, chlorophyll, gluthatione contents and antioxidant enzymes activities were determination.

Results: Increased lipid peroxidation and alterations in glutathione content, catalase, superoxide dismutase and peroxidase activities as well as in chlorophyll content revealed that As causes higher oxidative stress in plants grown in soils with low P content.

Conclusion: Stress parameters in F treatments were less affected. Plants grown in soils enriched with P revealed a decrease in the toxic effects caused by As and F.     

Arsenite and arsenate impact the oxidative status and antioxidant responses in Ocimum tenuiflorum L

Physiology and Molecular Biology of Plants - Biochemical responses of Ocimum tenuiflorum plants were studied upon exposure to arsenite (AsIII) and arsenate (AsV) for 1 to 10 d. Plants...     

Transformation of Arsenobetaine and Growth of Bacteria on Zeolitic Tuffs

Arsenobetaine (AsB) is a known organoarsenical of harmless toxicity. It is formed mainly by the metabolization of arsenate in marine organisms such as fish, mollusks and crustaceans. Preliminary investigations have shown that AsB can be degraded in contact with zeolites used as feed additives. Employing high‐performance liquid chromatography (HPLC) combined with simultaneous parallel electrospray ionization (ESI) and inductively coupled plasma mass spectrometric (ICP‐MS) detection, the formation of degradation products was monitored over fifty days in batch reactors containing AsB and clinoptilolites in an aqueous solution. After a 50‐day contact with different natural Mexican zeolites, the AsB concentration decreased by 37 to 100 %. In contrast, no degradation products of AsB were detected after contact with a synthetic clinoptilolite. The formation of dimethyl (1‐carboxymethyl) arsine and arsenate proceeded with different yields in the set of four natural zeolites. To search for the presence of bacteria on the zeolites as an alternative explanation for the metabolism of AsB in our experiments, the growth of microorganisms was studied on two natural clinoptilolites from Hungary and Mexico after severe acid wash. After 10 days of cultivation in iron and sulfur media, almost a threefold increase of the microbial population was observed. In further experiments on the retention of inorganic arsenic, one sample retained, for example, 25 μg/g As(V) and 2.5 μg/g As(III) from a 400 μg/L arsenic solution.     

Bog Iron Ores and their Potential Role in Arsenic Dynamics: An Overview and a “Paleo Example”

Bog iron ores (BIOs), i.e. terrestrial accumulations of iron (Fe) minerals forming within the zone of groundwater oscillation, have been described in several regions in Germany and other countries. Since BIOs are composed of a variety of Fe minerals, primarily amorphous Fe hydroxides, they are likely to have an influence on the arsenic (As) dynamics of an area, as these minerals represent important natural As sources and sinks. In this study, mineralogical research results (XRD, microscopy) of altered BIOs of Tertiary age (“paleo” BIOs or PBIOs), occurring within Cretaceous sands in an area of North Rhine‐Westphalia, are briefly presented. Genesis and mineralogical evolution of the categorized five different types of PBIOs, along with hydrogeochemical data from the literature, are discussed and compared to studies describing Holocene BIOs from other areas. In doing so, striking similarities (depositional environment, substratum, Fe source and its transport, geochemical evolution, and mineralogy) became evident. Differences in mineralogical and chemical composition can be attributed to the longer period of oxidation that the PBIOs have undergone (Fe hydroxide “aging”). This process is still ongoing (most of the groundwaters in the area plot in the goethite stability field) and leads to a higher stability of the Fe phases and thus, a stronger As retention. The known impact of the PBIOs on the As budget of the study area (they represent the source for elevated As concentrations in soils) can be transferred to more recent environments fostering BIO formation. These are likely to be even more important As sinks – and sources – as they contain higher Fe concentrations, higher shares of potentially mobile As and highly variable redox conditions which might lead to an As output from the BIOs into groundwater, soils and plants. Therefore, BIOs and their potential role in As behaviour are not only of scientific, but also of public interest.     

Influence of Arsenic from Anthropogenic Loaded Soils on the Mine Water Quality in the Tin District Ehrenfriedersdorf,Erzgebirge (Germany)

The central part of the tin ore deposit Ehrenfriedersdorf/Erzgebirge, which was exploited from the 13^th century to 1990, was flooded from 1994 to 1996. Since that time mine waters have flown through the gallery “Tiefer Sauberger Stolln” to the creek Wilisch in the Elbe river catchment area. The water at the mine portal shows high concentrations of arsenic and heavy metals. The average arsenic concentration is about 0.5 mg/L. Approximately two thirds of arsenic are transported dissolved. Where the mine water ascends from deeper levels, arsenic concentrations of about 0.4 mg/L were found. Here arsenic occurs predominantly particular. The mining gallery “Tiefer Sauberger Stolln” provides the unique opportunity of subsurface sampling for the identification of the arsenic sources under different hydrological conditions (normal and high water level). The sources of dissolved arsenic in the gallery part between the raise and the portal were determined and analyzed. Between these two monitoring points, many inflows of infiltration water were detected. The concentration of As in the infiltration water reaches up to 1.8 mg/L, which varies depending on the location in the gallery and the hydrological situation. The first part of the gallery was straightened, heightened and partly concreted with modern mining technique. The arsenic concentrations can decrease owing to high precipitation rates and snow melt events. The last part of the gallery was preserved due to low coverage. Here the arsenic concentrations in the infiltration waters increase with the surface water inflow. At a normal water level, 1 kg arsenic per day leaves the raise and 2.1 kg the gallery portal, which means that 50 % of the arsenic load comes from the infiltration water. At a high water level, 2.5 kg arsenic per day are transported through the raise and 8.2 kg per day through the gallery portal, which means that about 70 % of the arsenic load comes from infiltration water. The area of Ehrenfriedersdorf is characterized by a superposition of anthropogenic soil pollution over the geogenic inventory. There is a close connection between ancient soil contaminations by high amounts of water‐soluble arsenic compounds, e.g. arsenic trioxide formed by roasting the ores during ancient tin smelting, and high concentrations of dissolved arsenic in the infiltration water. The contamination of surface water and river sediments by arsenic is originating from an anthropogenic pollution of soils by ancient tailings via infiltration of water rich in arsenic into the mine gallery.     

Characterization of polycyclic aromatic hydrocarbons degradation and arsenate reduction by a versatile Pseudomonas isolate

A Pseudomonas isolate, designated PAHAs-1, was found capable of reducing arsenate and degrading polycyclic aromatic hydrocarbons (PAHs) independently and simultaneously. This isolate completely reduced 1.5 mM arsenate within 48 h and removed approximately 100% and 50% of 60 mg l⁻¹ phenanthrene and 20 mg l⁻¹ pyrene within 60 h, respectively. Using PAHs as the sole carbon source, however, this isolate showed a slow arsenate reduction rate (4.62 μM h⁻¹). The presence of arsenic affected cell growth and concurrent PAHs removal, depending on PAH species and arsenic concentration. Adding sodium lactate to the medium greatly enhanced the arsenate reduction and pyrene metabolism. The presence of the alpha subunit of the aromatic ring-hydroxylating dioxygenase (ARHD) gene, arsenate reductase (arsC) and arsenite transporter (ACR3(2)) genes supported the dual function of the isolate. The finding of latter two genes indicated that PAHAs-1 possibly reduced arsenate via the known detoxification mechanism. Preliminary data from hydroponic experiment showed that PAHAs-1 degraded the majority of phenanthrene (>60%) and enhanced arsenic uptake by Pteris vittata L. (from 246.7 to 1187.4 mg kg⁻¹ As in the fronds). The versatile isolate PAHAs-1 may have potentials in improving the bioremediation of PAHs and arsenic co-contamination using the plant-microbe integrated strategy.     

Pseudomonas arsenicoxydans sp nov., an arsenite-oxidizing strain isolated from the Atacama desert

A Gram-negative, arsenite-oxidizing bacterial strain, designated VC-1, was isolated from sediment samples from the Camarones Valley in the Atacama Desert, Chile. Strain VC-1 was strictly aerobic, oxidase and catalase positive, rod shaped, of about 5.5 μm in length and 0.5–1.0 μm in diameter. It was motile by means of multiple polar flagella. The phylogenetic reconstruction of the 16S rRNA gene sequence, an MLSA study by concatenating six genes, and DDH studies indicated that the strain differed genotypically from its closest relatives and was therefore recognized as a new species within the genus Pseudomonas. Phenotypic analysis combining metabolic tests, fatty acid profiles and MALDI-TOF profiles of total cell extracts supported the classification of the new species for which we propose the designation Pseudomonas arsenicoxydans sp. nov. The type strain is accessible under the culture collection numbers CCUG 58201^T and CECT 7543^T.     

Brevibacterium sp. strain CS2: A potential candidate for arsenic bioremediation from industrial wastewater

A multiple metal-resistant Brevibacterium sp. strain CS2, isolated from an industrial wastewater, resisted arsenate and arsenate upto 280 and 40 mM. The order of resistance against multiple metals was Arsenate > Arsenite > Selenium = Cobalt > Lead = Nickel > Cadmium = Chromium = Mercury. The bacterium was characterized as per morphological and biochemical characteristics at optimum conditions (37 ℃ and 7 pH). The appearance of brownish color precipitation was due to the interaction of silver nitrate confirming its oxidizing ability against arsenic. The strain showed arsenic processing ability at different temperatures, pH, and initial arsenic concentration which was 37% after 72 h and 48% after 96 h of incubation at optimum conditions with arsenite 250 mM/L (initial arsenic concentration). The maximum arsenic removal ability of strain CS2 was determined for 8 days, which was 32 and 46% in wastewater and distilled water, respectively. The heat-inactivated cells of the isolated strain showed a bioremediation efficiency (E) of 96% after 10 h. Genes cluster (9.6 kb) related to arsenite oxidation was found in Brevibacterium sp. strain CS2 after the genome analysis of isolated bacteria through illumine and nanopore sequencing technology. The arsenite oxidizing gene smaller subunit (aioB) on chromosomal DNA locus (Prokka_01508) was identified which plays a role in arsenite oxidation for energy metabolism. The presence of arsenic oxidizing genes and an efficient arsenic oxidizing potential of Brevibacterium sp. strain CS2 make it a potential candidate for green chemistry to eradicate arsenic from arsenic-contaminated wastewater.     

Arsenite‐induced changes in hepatic protein abundance in cynomolgus monkeys (Macaca fascicularis)

Arsenic is an environmental pollutant, and its liver toxicity has long been recognized. The effect of arsenic on liver protein expression was analyzed using a proteomic approach in monkeys. Monkeys were orally administered sodium arsenite (SA) for 28 days. As shown by 2D‐PAGE in combination with MS, the expression levels of 16 proteins were quantitatively changed in SA‐treated monkey livers compared to control‐treated monkey livers. Specifically, the levels of two proteins, mortalin and tubulin beta chain, were increased, and 14 were decreased, including plastin‐3, cystathionine‐beta‐synthase, selenium‐binding protein 1, annexin A6, alpha‐enolase, phosphoenolpyruvate carboxykinase‐M, erlin‐2, and arginase‐1. In view of their functional roles, differential expression of these proteins may contribute to arsenic‐induced liver toxicity, including cell death and carcinogenesis. Among the 16 identified proteins, four were selected for validation by Western blot and immunohistochemistry. Additional Western blot analyses indicated arsenic‐induced dysregulation of oxidative stress related, genotoxicity‐related, and glucose metabolism related proteins in livers from SA‐treated animals. Many changes in the abundance of toxicity‐related proteins were also demonstrated in SA‐treated human hepatoma cells. These data on the arsenic‐induced regulation of proteins with critical roles may help elucidate the specific mechanisms underlying arsenic‐induced liver toxicity.