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Iron is a ubiquitous element in the universe. Ferrous iron (Fe(II)) was abundant in the primordial ocean until the oxygenation of the Earth's atmosphere led to its widespread oxidation and precipitation. This change of iron bioavailability likely put selective pressure on the evolution of life. This element is essential to most extant life forms and is an important cofactor in many redox-active proteins involved in a number of vital pathways. In addition, iron plays a central role in many environments as an energy source for some microorganisms. This review is focused on Fe(II) oxidation. The fact that the ability to oxidize Fe(II) is widely distributed in Bacteria and Archaea and in a number of quite different biotopes suggests that the dissimilatory Fe(II) oxidation is an ancient energy metabolism. Based on what is known today about Fe(II) oxidation pathways, we propose that they arose independently more than once in evolution and evolved convergently. The iron paleochemistry, the phylogeny, the physiology of the iron oxidizers, and the nature of the cofactors of the redox proteins involved in these pathways suggest a possible scenario for the timescale in which each type of Fe(II) oxidation pathways evolved. The nitrate dependent anoxic iron oxidizers are likely the most ancient iron oxidizers. We suggest that the phototrophic anoxic iron oxidizers arose in surface waters after the Archaea/Bacteria-split but before the Great Oxidation Event. The neutrophilic oxic iron oxidizers possibly appeared in microaerobic marine environments prior to the Great Oxidation Event while the acidophilic ones emerged likely after the advent of atmospheric O(2). This article is part of a Special Issue entitled: The evolutionary aspects of bioenergetic systems., (Copyright © 2012 Elsevier B.V. All rights reserved.)

Acidithiobacillus ferrooxidans is an acidophilic chemolithoautotrophic bacterium that can grow in the presence of either the weak reductant Fe(2+), or reducing sulfur compounds that provide more energy for growth than Fe(2+). We have previously shown that the uphill electron transfer pathway between Fe(2+) and NAD(+) involved a bc(1) complex that functions only in the reverse direction [J. Bacteriol. 182, (2000) 3602]. In the present work, we demonstrate both the existence of a bc(1) complex functioning in the forward direction, expressed when the cells are grown on sulfur, and the presence of two terminal oxidases, a bd and a ba(3) type oxidase expressed more in sulfur than in iron-grown cells, besides the cytochrome aa(3) that was found to be expressed only in iron-grown cells. Sulfur-grown cells exhibit a branching point for electron flow at the level of the quinol pool leading on the one hand to a bd type oxidase, and on the other hand to a bc(1)-->ba(3) pathway. We have also demonstrated the presence in the genome of transcriptionally active genes potentially encoding the subunits of a bo(3) type oxidase. A scheme for the electron transfer chains has been established that shows the existence of multiple respiratory routes to a single electron acceptor O(2). Possible reasons for these apparently redundant pathways are discussed.

Acidithiobacillus ferrooxidans is an acidophilic chemolithotrophic bacterium that can grow in the presence of either a weak reductant, Fe(2+), or reducing sulfur compounds that provide more energy for growth than Fe(2+). Here we first review the latest findings about the uphill electron transfer pathway established in iron-grown A. ferrooxidans, which has been found to involve a bc(1) complex. We then provide evidence that this bc(1) complex cannot function in the forward direction (exergonic reaction), even with an appropriate substrate. A search for the sequence of the three redox subunits of the A. ferrooxidans bc(1) complex (strain ATCC 19859) in the complete genome sequence of the A. ferrooxidans ATCC 23270 strain showed the existence of two different bc(1) complexes in A. ferrooxidans. Cytochrome b and Rieske protein sequence comparisons allowed us to point out some sequence particularities of these proteins in A. ferrooxidans. Lastly, we discuss the possible reasons for the existence of two different "classical" bc(1) complexes and put forward some suggestions as to what role these putative complexes may play in this acidophilic chemolithotrophic bacterium.

The periplasmic blue copper protein rusticyanin is thought to play an important role in iron oxidation by Thiobacillus ferrooxidans. We present the sequence of the gene, rus, encoding rusticyanin together with about 1.4 kb of upstream and 0.3 kb of downstream DNA. The rus gene is unique to T. ferrooxidans. Evidence is presented that it is the last gene of an operon and that it can be transcribed from its own promoter. In ATCC33020 strain, rusticyanin is synthesized in ferrous iron but also in sulfur growth conditions suggesting that it could play a role in both energetic metabolisms. The rus gene transcribed from a vector promoter in Escherichia coli leads to the production of a processed aporusticyanin in the periplasmic space, indicating that its signal sequence is correctly recognized by the secretion machinery and the signal peptidase of E. coli.