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was released by brucite or olivine dissolution and was subsequently oxidized and precipitated as ferric hydroxide. Thermodynamic computations show that this process may be a potential source of catabolic
Bereich: Sites
sequestering important quantities of Fe as FeS2. The in situ oxidation of ferrous Fe and precipitation of ferric hydroxides at the olivine surface commonly observed in oxic environments were obviously impeded.
Pichler, T. and Lamarche, G., 2001, Mineralogical characterization of a natural very As-rich hydrous ferric oxide coprecipitate formed by mixing of hydrothermal fluid and sea water. American Mineralogist,
Bereich: FB5
altered levels of ferritin and transferrin receptor in cultured astrocytes during incubation with ferric ammonium citrate. J. Neurochem. 88, 1194-1202. J.R. Liddell, S.R. Robinson, R. Dringen (2004) Endogenous
Bereich: FB2