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PubMed · 11629044

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N Ercoli. [Not Available].. https://pubmed.ncbi.nlm.nih.gov/11629044/

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Reduction of pentavalent antimony by trypanothione and formation of a binary and ternary complex of antimony(III) and trypanothione.

Several pentavalent antimony compounds have been used for the treatment of leishmaniasis for decades. However, the mechanism of these antimony drugs still remains unclear. One of their targets is thought to be trypanothione, a major low molecular mass thiol inside the parasite. We show that pentavalent antimony (Sb(V)) can be rapidly reduced to its trivalent state by trypanothione at mildly acidic conditions and 310 K ( k=4.42 M(-1) x min(-1) at pH 6.4), and that Sb(III) can be bound to trypanothione to form an Sb(III)-trypanothione complex. NMR data demonstrate that Sb(III) binds to trypanothione at the two thiolates of the cysteine residues, and that the binding is pH dependent and is strongest at biological pH with a stability constant log K=23.6 at 298 K (0.1 M NaNO(3)). The addition of low molecular monothiol ligands such as glutathione and cysteine to the Sb(III)-trypanothione complex results in the formation of a ternary complex. Thiolates from both trypanothione and monothiol bind to the Sb(III) center. The formation of the ternary complex is important, as the antileishmanial properties of the drugs are probably due to a complex between of Sb(III)-trypanothione and enzymes. Although thermodynamically stable, the complex is kinetically labile and the free and bound forms of thiolates exchange on the (1)H NMR timescale. Such a facile exchange may be crucial for the transport of Sb(III) within parasites.

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Distribution and early diagenesis of antimony species in sediments and porewaters of freshwater lakes.

The study identifies the role played by different components of natural aquatic systems on the poorly known geochemistry of antimony. Different chemical forms of antimony were measured in porewaters and sediments of two Sudbury lakes characterized by contrasting redox conditions at the sediment-water interface. In porewaters, Sb(III) was present under reducing conditions where it could exist as SbS2- according to thermodynamic calculations. Sb(V) was detected mainly under oxic and mildly reducing environments where its presence was attributed to the oxidizing effect of iron and manganese oxyhydroxides or to the slow kinetics of reduction by dissolved sulfide or possible complexation by it. A third form of Sb identified as refractory was obtained after UV irradiation of the water samples, suggesting an association of Sb to low molecular weight natural organic matter. The distribution of Sb in sediments of the two lakes revealed (through the comparison of profiles and statistical correlations) the importance of iron and manganese oxyhydroxides in controlling the behavior of Sb, particularly in the lake where the interface was clearly oxic. Porewater profiles indicate that the dissolution of manganese and iron oxyhydroxides under anoxic conditions leads to the simultaneous release of dissolved Sb previously sorbed onto those compounds. In reducing sediments, the control of the solubility of Sb by iron sulfides is suggested.

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