Mercury in feral fish: distribution, accumulation and toxicity

O principal objectivo desta dissertação foi estudar a acumulação de mercúrio em vários tecidos de peixes marinhos, a sua relação com factores biológicos e as respectivas respostas bioquímicas. O trabalho realizado permitiu obter novos conhecimentos sobre a acumulação de mercúrio em peixes, possibilitando avaliar a influência da biodisponibilidade do elemento e as suas possíveis implicações no ambiente. O trabalho foi desenvolvido na Ria de Aveiro (Portugal), uma zona costeira onde existe um gradiente ambiental de mercúrio, o que oferece a oportunidade de estudar a sua acumulação e os seus efeitos tóxicos em condições realísticas. As amostragens foram efectuadas em dois locais considerados críticos em termos de contaminação por mercúrio – Largo do Laranjo (L1 e L2) e num local afastado da principal fonte de poluição, usado como termo de comparação (Referência; R); L1 e L2 corresponderam a locais moderadamente e altamente contaminados, respectivamente. Foram escolhidos juvenis de duas espécies ecologicamente diferentes e representativas da comunidade piscícola local, a tainha garrento (Liza aurata) e o robalo (Dicentrarchus labrax). Em cada local foram recolhidas amostras de água e de sedimento para determinação de mercúrio. Foram quantificadas as concentrações de mercúrio total (T-Hg) e orgânico (O-Hg) em vários tecidos dos peixes, escolhidos tendo em conta a sua função relativamente à toxicocinética e toxicodinâmica de metais. As respostas antioxidantes (Catalase- CAT, glutationa peroxidase- GPx, glutationa reductase- GR, glutationa –S-transferase- GST e conteúdo em glutationa total- GSHt), o dano peroxidativo (LPO) e o conteúdo em metalotioninas (MTs) foram também avaliados. A acumulação de T-Hg foi semelhante para as duas espécies de peixes estudadas, embora D. labrax tenha apresentado concentrações tendencialmente maiores. Ambas as espécies demonstraram capacidade de reflectir o grau de contaminação ambiental existente, indicando claramente que a acumulação depende da concentração ambiental. A acumulação revelou-se específica de cada tecido. O padrão da acumulação em L. aurata foi rim > fígado > músculo > cérebro > guelras > sangue e em D. labrax foi fígado > rim > músculo > cérebro ≈ guelras > sangue. Relativamente à acumulação de OHg, verificou-se que D. labrax exibiu concentrações mais elevadas que L. aurata. Todos os tecidos foram capazes de reflectir diferenças entre R e L2. Os níveis de O-Hg no fígado, músculo e nos conteúdos intestinais foram diferentes entre espécies, sendo mais elevados para D. labrax. As guelras e o intestino foram os tecidos onde se obtiveram os valores mais baixos de O-Hg e observaram-se valores idênticos para as duas espécies. Com excepção das guelras, as concentrações de O-Hg variaram em função do valor observado nos conteúdos intestinais, indicando que a alimentação é a via dominante da acumulação. As concentrações de O-Hg nos conteúdos intestinais revelaram ser uma informação relevante para prever a acumulação de O-Hg nos tecidos, pois verificou-se uma razão praticamente constante entre o teor de mercúrio no fígado, no músculo e nos conteúdos intestinais. A percentagem de O-Hg no músculo e no fígado variou de acordo com o grau de contaminação ambiental e com o tipo de assimilação preferencial do elemento (alimentação vs. água), sugerindo que o fígado exerce um papel protector em relação à acumulação de mercúrio nos outros órgãos. Ambas as espécies de peixes demonstraram ser boas sentinelas da contaminação ambiental com mercúrio (T-Hg e O-Hg), sendo o cérebro e o músculo os tecidos que melhor reflectiram o grau de acumulação com o elemento. A análise conjunta dos dados de bioacumulação e de respostas ao stress oxidativo permitiram estabelecer uma relação entre as concentrações de mercúrio nas guelras, fígado, rim e cérebro e a sua toxicidade. As respostas do cérebro aos efeitos tóxicos do mercúrio revelaram ser específicas de cada espécie. Enquanto que para o cérebro de L. aurata se verificou um decréscimo de todos os parâmetros antioxidantes estudados nos locais contaminados, sem haver evidência de qualquer mecanismo compensatório, no D. labrax observaram-se respostas ambivalentes, que indicam por um lado a activação de mecanismos adaptativos e, por outro, o decréscimo das respostas antioxidantes, ou seja, sinais de toxicidade. Embora em ambas as espécies de peixe fosse evidente uma condição pró-oxidante, o cérebro parece possuir mecanismos compensatórios eficientes, uma vez que não se verificou peroxidação lipídica. As respostas antioxidantes do cérebro de D. labrax foram comparadas em diferentes períodos do ano - quente vs. frio. O período quente mostrou ser mais crítico, uma vez que no período frio não se verificaram diferenças nas respostas entre locais, ou seja, a capacidade antioxidante do cérebro parece ser influenciada pelos factores ambientais. As guelras revelaram susceptibilidade à contaminação por mercúrio, uma vez que se verificou uma tendência para o decréscimo da actividade de CAT em L2 e ausência de indução em L1. O fígado e o rim demonstraram mecanismos adaptativos face ao grau de contaminação moderada (L1), evidenciados pelo aumento de CAT. O rim também demonstrou adaptabilidade face ao grau elevado de contaminação (L2), uma vez que se verificou um aumento GST. Embora o grau de susceptibilidade tenha sido diferente entre os órgãos, não se verificou peroxidação lipídica em nenhum. A determinação do conteúdo em MTs em D. labrax e em L. aurata revelou que este parâmetro depende não só da espécie, mas também do tecido em causa. Assim, em D. labrax foi observado um decréscimo de MTs no cérebro, bem como a incapacidade de síntese de MTs no sangue, guelras, fígado, rim e músculo. Em L. aurata observou-se um aumento do conteúdo em MTs no fígado e no músculo. Estes resultados indicam que a aplicabilidade das MTs como biomarcador de exposição ao mercúrio parece ser incerta, revelando limitações na capacidade de reflectir os níveis de exposição ao metal e por consequência o grau de acumulação. Este trabalho comprova a necessidade de se integrarem estudos de bioacumulação com biomarcadores de efeitos, de modo a reduzir os riscos de interpretações erróneas, uma vez que as respostas nem sempre ocorrem para os níveis mais altos de contaminação ambiental com mercúrio.

Seasonal behavior of mercury species in waters and sediments from the Negro River Basin, Amazon, Brazil

Total (HgT), reactive (HgR) and organic (Hg ORG) mercury species have been quantified in non-filtered waters collected from the Negro River Basin, Amazon (from January/2002 through January/2004), in both black and white water bodies. Black waters presented the highest HgT, HgORG and HgR concentration (29.1 ng L-1, 1.63 ng L-1 and 3.9 ng L-1, respectively), while, white waters presented the lowest HgT, Hg ORG and HgR concentration (8.8 ng L-1, 0.49 ng L-1 and 1.2 ng L-1, respectively). An inverse correlation between HgT and the water level over the basin was obtained, although the HgORG concentration has increased in the first rainy months and then decreased as the water level rose. Total mercury in surface sediments (0-10 cm) ranged from 70 to 271 mg kg-1 being the methylmercury 0.47-1.79 % of this stock. The results indicate that HgR and the labile dissolved organic matter were introduced into the aquatic environment during the flooding season, especially in the earlier stages, thus contributing to mercury methylation. ©2007 Sociedade Brasileira de Química.

Cytotoxicity and genotoxicity of low doses of mercury chloride and methylmercury chloride on human lymphocytes in vitro

Mercury is a xenobiotic metal that is a highly deleterious environmental pollutant. The biotransformation of mercury chloride (HgCl2) into methylmercury chloride (CH3HgCl) in aquatic environments is well-known and humans are exposed by consumption of contaminated fish, shellfish and algae. The objective of the present study was to determine the changes induced in vitro by two mercury compounds (HgCl2 and CH3HgCl) in cultured human lymphocytes. Short-term human leukocyte cultures from 10 healthy donors (5 females and 5 males) were set-up by adding drops of whole blood in complete medium. Cultures were separately and simultaneously treated with low doses (0.1 to 1000 µg/l) of HgCl2 and CH3HgCl and incubated at 37ºC for 48 h. Genotoxicity was assessed by chromosome aberrations and polyploid cells. Mitotic index was used as a measure of cytotoxicity. A significant increase (P < 0.05) in the relative frequency of chromosome aberrations was observed for all concentrations of CH3HgCl when compared to control, whether alone or in an evident sinergistic combination with HgCl2. The frequency of polyploid cells was also significantly increased (P < 0.05) when compared to control after exposure to all concentrations of CH3HgCl alone or in combination with HgCl2. CH3HgCl significantly decreased (P < 0.05) the mitotic index at 100 and 1000 µg/l alone, and at 1, 10, 100, and 1000 µg/l when combined with HgCl2, showing a synergistic cytotoxic effect. Our data showed that low concentrations of CH3HgCl might be cytotoxic/genotoxic. Such effects may indicate early cellular changes with possible biological consequences and should be considered in the preliminary evaluation of the risks of populations exposed in vivo to low doses of mercury.

Bixin and norbixin protect against DNA-damage and alterations of redox status induced by methylmercury exposure in vivo

Populations in the Amazon are exposed to organic mercury via consumption of contaminated foods. These ethnic groups consume a specific plant seed annatto which contains certain carotenoids. The aim of this study was to find out if these compounds (bixin, BIX and norbixin, NOR), protect against DNA-damage caused by the metal. Therefore, rats were treated orally with methylmercury (MeHg) and with the carotenoids under conditions that are relevant to humans. The animals were treated either with MeHg (30 mu g/kg/bw/day), BIX (0.110 mg/kg/bw/day), NOR (0.011.0 mg/kg/bw/day) or combinations of the metal compound and the carotenoids consecutively for 45 days. Subsequently, the glutathione levels (GSH) and the activity of catalase were determined, and DNA-damage was measured in hepatocytes and leukocytes using single cell gel electrophoresis assays. Treatment with the metal alone caused a decrease in the GSH levels (35%) and induced DNA damage, which resulted in increased DNA migration after electrophoresis in liver and blood cells, whereas no effects were seen with the carotenoids alone. When BIX or NOR were given in combination with organic mercury, the intermediate and the highest concentrations of the carotenoids (1.0 and 10.0 mg/kg/bw/day BIX and 0.1 and 1.0 mg/kg/bw/day NOR) protected against DNA-damage. Furthermore, we found with both carotenoids, a moderate increase in the GSH levels in both metal-treated and untreated animals, while the activities of catalase remained unchanged. Our results indicate that consumption of BIX and NOR may protect humans against the adverse health effects caused by exposure to organic mercury. Environ. Mol. Mutagen., 2012. (c) 2012 Wiley Periodicals, Inc.

Measurement of nonmethane organic carbon

The present dissertation focuses on the measurement of nonmethane organic carbon compounds (NMOC) and their exchange by biosphere-atmosphere interactions. To access the accuracy, precision, and reproducibility of NMOC analysis, two intercomparison experiments were carried out during the present study. These experiments comprised the sampling of NMOCs on graphitised carbon blacks, followed by gas-chromatographic analysis. Furthermore, they comprised the sampling of short chain carbonyl compounds on solid phase extraction cartridges and their analysis by high pressure liquid chromatography. To investigate the exchange of NMOCs between vegetation and the atmosphere, plant enclosure studies were performed on two European deciduous tree species. These measurements were conducted during two consecutive summer seasons by utilisation of the above specified techniques on sunlit and shaded leaves of European beech (Fagus sylvatica L., monoterpene emitter) and sunlit leaves of English oak (Quercus robur L., isoprene emitter). According to its broad geographical distribution, the impact of European beech on the European monoterpene budget was characterized by a model simulation. Complementary an instrument was developed, that is capable of measuring the amount of total NMOC that is exchanged by biosphere-atmosphere interactions. The instrument was tested under laboratory conditions and was evaluated versus an independent method performing branch enclosure measurements.

Stand scale variability of topsoil organic matter composition in a high-elevation Norway spruce forest ecosystem

Our knowledge about the effect of single-tree influence areas on the physicochemical properties of the underlying mineral soil in forest ecosystems is still limited. This restricts our ability to adequately estimate future changes in soil functioning due to forest management practices. We studied the stand scale spatial variation of different soil organic matter species investigated by 13C NMR spectroscopy, lignin phenol and neutral sugar analysis under an unmanaged mountainous high-elevation Norway spruce (Picea abies L.) forest in central Europe. Multivariate geostatistical approaches were applied to relate the spatial patterns of the different soil organic matter species to topographic parameters, bulk density, oxalate- and dithionite-extractable iron, pH, and the impact of tree distribution. Soil samples were taken from the mineral top soil. Generally, the stand scale distribution patterns of different soil organic matter compounds could be divided into two groups: Those compounds, which were significantly spatially correlated with topography/altitude and those with small scale spatial pattern (range ≤ 10 m) that was closely related to tree distribution. The concentration of plant-derived soil organic matter components, such as lignin, at a given sampling point was significantly spatially related to the distance of the nearest tree (p ≤ 0.05). In contrast, the spatial distribution of mainly microbial-derived compounds (e.g. galactose and mannose) could be attributed to the dominating impact of small-scale topography and the contribution of poorly crystalline iron oxides that were significantly larger in the central depression of the study site compared to crest and slope positions. Our results demonstrate that topographic parameters dominate the distribution of overall topsoil organic carbon (OC) stocks at temperate high-elevation forest ecosystems, particularly in sloped terrain. However, trees superimpose topography-controlled OC biogeochemistry beneath their crown by releasing litter and changing soil conditions in comparison to open areas. This may lead to distinct zones with different mechanisms of soil organic matter degradation and also stabilization in forest stands.

Total organic carbon, lithology and alkylthiophenes in immature sediments (Table 1)

A series of novel long-chain 3,4-dialkylthiophenes (C36-C54) was identified in a number of sediments ranging from Pleistocene to Cretaceous. The identifications were based on mass spectral characterisation, desulphurisation and mass spectral data of synthesised model compounds. These organic sulphur compounds are probably formed by sulphur incorporation into mid-chain dimethylalkadienes with two methylenic double bonds. These putative precursor lipids are unprecedented and may be considered rather unusual. The distribution of 3,4-dialkylthiophenes in sediments varies considerably with the depositional palaeoenvironment, indicating that these compounds have a potential as molecular markers reflecting changes in palaeoenvironment.

Organic geochemistry of interstitial waters at DSDP Holes 64-474 and 64-479

Studies of the nature and amount of dissolved organic matter (DOM) in pore-water solutions have been confined mostly to recent sediments (Henrichs and Farrington, 1979; Krom and Sholkovitz, 1977; Nissenbaum et al., 1972). The analyses of organic constituents in interstitial waters have not been extended to sediment depths of more than 15 meters (Starikova, 1970). Large fluctuations in organic contents of near-bottom interstitial fluids suggest that organic compounds may provide insight into the chemical and biological processes occurring in the sedimentary column. Gradients in inorganic ion concentrations have been used as indicators of diagenesis of organic matter in deep sediments and interstitial waters. Shishkina (1978) attributed the occurrence of iodine and Cl/Br ratios that deviated from the value of seawater to the breakdown of organic matter and the liberation of bromide during mineralization. Sulfate depletion and maxima in ammonia concentrations were interpreted to be a consequence of sulfate reduction reactions in pore fluids, even at depths of more than 400 meters (Miller et al., 1979; Manheim and Schug, 1978).The purpose of this chapter is to study organic carbon compounds dissolved in interstitial waters of deep sediments at Sites 474 and 479.

Sediment and organic matter properties, and molecular formula from sampling locations in the Northern Black Sea

Remineralization of organic matter in reactive marine sediments releases nutrients and dissolved organic matter (DOM) into the ocean. Here we focused on the molecular-level characterization of DOM by high-resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS) in sediment pore waters and bottom waters from contrasting redox regimes in the northern Black Sea with particular emphasis on nitrogen-bearing compounds to derive an improved understanding of the molecular transformations involved in nitrogen release. The number of nitrogen-bearing molecules is generally higher in pore waters than in bottom waters. This suggests intensified degradation of nitrogen-bearing precursor molecules such as proteins in anoxic sediments: No significant difference was observed between sediments deposited under oxic vs anoxic conditions (average O/C ratios of 0.55) suggesting that the different organic matter quality induced by contrasting redox conditions does not impact protein diagenesis in the subseafloor. Compounds in the pore waters were on average larger, less oxygenated, and had a higher number of unsaturations. Applying a mathematical model, we could show that the assemblages of nitrogen-bearing molecular formulas are potential products of proteinaceous material that was transformed by the following reactions: (a) hydrolysis and deamination, both reducing the molecular size and nitrogen content of the products and intermediates; (b) oxidation and hydration of the intermediates; and (c) methylation and dehydration.

Competitive sorption reactions between phosphorus and organic matter in soil: a review

The incorporation of organic matter ( OM) in soils that are able to rapidly sorb applied phosphorus ( P) fertiliser reportedly increases P availability to plants. This effect has commonly been ascribed to competition between the decomposition products of OM and P for soil sorption sites resulting in increased soil solution P concentrations. The evidence for competitive inhibition of P sorption by dissolved organic carbon compounds, derived from the breakdown of OM, includes studies on the competition between P and (i) low molecular weight organic acids (LOAs), (ii) humic and fulvic acids, and (iii) OM leachates in soils with a high P sorption capacity. These studies, however, have often used LOAs at 1 - 100 mM, concentrations much higher than those in soils ( generally < 0.05 mM). The transience of LOAs in biologically active soils further suggests that neither their concentration nor their persistence would have a practical benefit in increasing P phytoavailability. Higher molecular weight compounds such as humic and fulvic acids also competitively inhibit P sorption; however, little consideration has been given to the potential of these compounds to increase the amount of P sorbed through metal - chelate linkages. We suggest that the magnitude of the inhibition of P sorption by the decomposition products of OM leachate is negligible at rates equivalent to those of OM applied in the field. Incubation of OM in soil has also commonly been reported as reducing P sorption in soil. However, we consider that the reported decreases in P sorption ( as measured by P in the soil solution) are not related to competition from the decomposition products of OM breakdown, but are the result of P release from the OM that was not accounted for when calculating the reduction in P sorption.

Source/receptor reconciliation of ambient organic fine particulate matter in Palm Beach County

Airborne particulate matter (PM) is of environmental concern not only in urban but also rural areas that are easily inhalable and have been considered responsible, together with gaseous pollutants, for possible health effects. The objectives of this research study is to generate an extensive data set for ambient PM collected at Belle Glade and Delray Beach that ultimately was used together with published source profiles to predict the contributions of major sources to the overall airborne particle burden in Belle Glade and Delray Beach. ^ The size segregated particle sampling was conducted for one entire year. The samples collected during the months of January and May were further subjected to chemical analysis for organic compounds by Gas Chromatography-Mass Spectrometry. Additional, PM10 sampling was conducted simultaneously with size segregated particle sampling during January and May to analyze for trace elements using Instrumental Neutron Activation Analysis technique. Elements and organic marker compounds were used in Chemical Mass Balance modeling to determine the major source contribution to the ambient fine particle matter burden. ^ Size segregated particle distribution results show bimodal in both sampling sites. Sugarcane pre-harvest burning in the rural site elevated PM10 concentration by about 30% during the sugarcane harvest season compared to sugarcane growing season. Sea salt particles and Saharan dust particles accounted for the external sources. ^ The results of trace element analysis show that Al, Ca, Cs, Eu, Lu, Nd, Sc, Sm, Th, and Yb are more abundant at the rural sampling site. The trace elements Ba, Br, Ce, Cl, Cr, Fe, Gd, Hf, Na, Sb, Ta, V, and W show high abundance at the urban site due to anthropogenic activities except for Na and Cl, which are from sea salt spray. On the other hand, size segregated trace organic compounds measurements show that organic compounds mainly from combustion process were accumulated in PM0.95. ^ In conclusion, major particle sources were determined by the CMB8.2 software as follows: road dust, sugarcane leaf burning, diesel-powered and gasoline powered vehicle exhaust, leaf surface abrasion particles, and a very small fraction of meat cooking. ^