Aj. Ghio et al., DNA STRAND BREAKS FOLLOWING IN-VITRO EXPOSURE TO ASBESTOS INCREASE WITH SURFACE-COMPLEXED [FE3+], Archives of biochemistry and biophysics, 311(1), 1994, pp. 13-18
Surface functional groups on silicate dusts complex iron cations which
can cycle through reduction and oxidation states to generate free rad
icals. These oxidants have a capacity to produce DNA strand breaks and
mutations which are primary events in cancer induction. A differentia
l in the capacity of fibrous silicates to produce carcinoma is recogni
zed with the amphiboles demonstrating a greater biologic effect than t
he serpentine fiber chrysotile. We tested the hypothesis that the diff
erences in genotoxicity of these fibrous silicates correspond to varyi
ng concentrations of iron complexed to the surface. Relative to chryso
tile, the amphibole fibers complexed greater amounts of iron cations f
rom both inorganic and in vivo sources. Increased concentrations of su
rface-complexed iron were associated with greater oxidant generation,
measured as thiobarbituric acid-reactive products of deoxyribose, and
more covalently closed, circular DNA strand scission. These results in
dicate that genotoxic effects of these fibers may correspond to their
capacity to complex iron at the surface. (C) 1994 Academic Press, Inc.