Fe; at. no. 26; at. wt 55.845; valences 2, 3; seldom 1, 4, 6. Group VIII (8). Four naturally occurring isotopes: 54 (5.82%); 56 (91.66%); 57 (2.19%); 58 (0.33%); artificial, radioactive isotopes: 52; 53; 55; 59-61. Second most abundant metal in earth's crust after aluminum: about 5%. The earth's core is believed to consist mainly of iron. Important ores include hematite (Fe2O3), magnetite (Fe3O4), limonite [FeO(OH).nH2O] and siderite (FeCO3). Essential dietary nutrient. Study of iron and its compds by Mssbauer spectroscopy: Danon, “57Fe: Metal, Alloys and Inorganic Compounds” in Chemical Applications of Mssbauer Spectroscopy, V. I. Goldanskii, R. H. Herber, Eds. (Academic Press, New York, 1968) p 159-313. Ions involved in oxygen transport, electron transport, nitrogen fixation and a number of other biological processes: Nielands, “Evolution of Biological Iron Binding Centers” in Struct. Bonding 11, 145-170 (1972). Review of biology, pharmacology and toxicity of iron compounds: several authors, Clin. Toxicol. 4, 525-642 (1971); of metabolism and homeostasis: G. Papanikolaou, K. Pantopoulos, Toxicol. Appl. Pharmacol. 202, 199-211 (2005). Comprehensive reviews: Feldmann, Schenck in Ullmanns Encyklopdie der technischen Chemie vol. 6 (München-Berlin, 1955) pp 261-407; Nicholls in Comprehensive Inorganic Chemistry vol. 3, J. C. Bailar, Jr. et al., Eds. (Pergamon Press, Oxford, 1973) pp 979-1051; W. A. Knepper in Kirk-Othmer Encyclopedia of Chemical Technology vol. 13 (Wiley-Interscience, New York, 3rd ed., 1981) pp 735-753. Review of use in cereal flour fortification: R. Hurrell et al., Nutr. Rev. 60, 391-406 (2002).