The biodegradation of iron-citrate complexes depends on the structure of the complex formed between the metal and citric acid. Ferric iron formed a bidentate complex with citric acid, [Fe(III) (OH)(2) cit] involving two carboxylic acid groups, and was degraded at the rate of 86 muM h. In contrast, ferrous iron formed a tridentate complex with citric acid, [Fe(II) cit], involving two carboxylic ...

Most organisms depend on iron as a co-factor for proteins catalyzing redox reactions. Iron is, however, a difficult element for cells to deal with, as it is insoluble in its ferric (Fe3+) form and potentially toxic in its ferrous (Fe2+) form. Thus, in vertebrates iron is transported through the circulation bound to transferrin (Tf) and delivered to cells through an endocytotic cycle involving t...

After total dose infusion of iron dextran to 14 pregnant women the saturation of transferrin and the concentration of ferritin were increased in the cord blood at birth, compared with untreated cases. These changes suggest that the fetal iron stores may be increased by such treatment.

It was most unfortunate that, because of the minimal risk of producing a tumour at the site of injection, the use of intramuscular iron-dextran complex, used for some time as an effective prophylactic against late anaemia of prematurity, had to be discontinued. A single injection had a long term effect and avoided the need for daily oral iron. Thus it became necessary to determine if oral treat...

The Biwabik Iron Formation is a approximately 1.9 billion year-old sequence of iron-rich sedimentary rocks that was metamorphosed at its eastern-most extent by approximately 1.1 billion year-old intrusions of the Duluth Complex. The metamorphic recrystallization of iron-formation locally produced iron-rich amphiboles and other fibrous iron-silicate minerals. The presence of these minerals in ir...