Premium
Iron in evolution
Author(s) -
Williams R.J.P.
Publication year - 2012
Publication title -
febs letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.593
H-Index - 257
eISSN - 1873-3468
pISSN - 0014-5793
DOI - 10.1016/j.febslet.2011.05.068
Subject(s) - ferrous , ferric , ferric iron , chemistry , oxidation state , redox , environmental chemistry , chemical evolution , ferric ion , oxygen , electron transfer , atmospheric oxygen , inorganic chemistry , biochemistry , photochemistry , organic chemistry , catalysis , stars , physics , astronomy
Iron chemistry in the environment and in organisms is entwined. The iron surface minerals in solution for the first billion years of the planet were ferrous compounds. This ion became and has remained a major participant in organisms. The evolution of iron was due to its oxidation to insoluble ferric ions by oxygen released from organisms. The evolution of cellular iron chemistry then required uptake from this oxidised state. Use was expanded from the mainly electron transfer properties in the original reductive cell interior to employment in external oxidative chemistry. The environment/organisms evolution is that of one predictable chemical system.