In rivers and other freshwater bodies, the presence of mercury can be due to direct contamination by anthropic activities such as gold mining. However, it can also be attributed to atmospheric deposition and erosion, runoff, or lixiviation from surrounding soils. In the case of the Amazon rainforest, high mercury contents have been reported for litter and topsoil, which could affect the mercury concentrations in water bodies. Samples of suspended particulate matter were obtained from a transect of the Itenez River, associated lakes, and some of its tributaries. The aim was to obtain information on particulate mercury’s origin in the study area and determine the relationship between particulate mercury and particulate organic carbon. The concentration of mercury, organic matter, and the C:N ratio of the suspended matter was determined. The concentration of particulate mercury by water volume depended on changes in suspended matter loads, which in turn were mostly affected by the nature of the watershed or sediment resuspension. The observed values for the percentage of organic matter and the C:N ratio suggest that most of the mercury content in rivers and lakes originated from soils. A positive correlation was found between mercury concentration by weight of particulate matter and organic carbon content in particles. This correlation might be due to the direct binding of mercury to organic matter through functional groups like thiols or to an indirect effect of oxyhydroxides that can adsorb mercury and are associated with organic matter.
In order to determine the effect of various soil components on the activity of proteins, we monitored the fluorescence and the enzymatic activity of, respectively, green fluorescent protein (GFP) and β-glucosidase adsorbed on fine soil particles. We also monitored the activity of these proteins in the presence of components that are representative of soil colloids: a montmorillonite clay, goethite and organic matter extracted from soil. Upon adsorption on clay and goethite, GFP lost its fluorescence properties while β-glucosidase suffered only a partial loss of its catalytic activity. Extractable organic matter had an inactivating role on GFP while it did not cause inactivation of β-glucosidase. When GFP and β-glucosidase adsorbed on particles from natural soil samples, their behaviour was consistent with the behaviour observed for these proteins in the presence of the separate components, suggesting that the macroscopic activity of proteins adsorbed on soil particles corresponds to an average of the activities of proteins adsorbed on a mixture of surfaces. The monitoring of the proteins on soil particles with different organic matter contents has also shown that organic matter can have different effects (protecting or inactivating) on different proteins.
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