Acidithiobacillus ferrooxidans is an acidophilic, chemolithoautotrophic γ-proteobacterium that uses energy and electrons derived from the oxidation of ferrous iron (Fe(II)) and reduced inorganic sulfur compounds (RISCs) for carbon dioxide and nitrogen fixation and other anabolic processes. It is a member of a consortium of microorganisms used for industrial copper recovery (bioleaching or biomining) and gold recovery (biooxidation) and contributes to the geobiochemical recycling of metals and nutrients in pristine and contaminated acid-rich environments.
When
A. ferrooxidans requires reducing power it is confronted by a particularly challenging bioenergetic problem because the standard reduction half-potential of the Fe(II)/Fe(III) couple (+0.77 V at pH 2, the pH of the medium) is much more positive than that of the NAD(P)/NAD(P)H couple (-0.32 V at the cytoplasmic pH 7). This means that electrons have to be "pushed uphill" from Fe(II) to NAD(P) against the redox potential gradient (uphill pathway). The energy to accomplish this was proposed to come from the proton motive force that naturally occurs across the periplasmic membrane of
A. ferrooxidans (outside = pH 2, inside = pH 7). It was further suggested that protons, entering the cell through a membrane associated ATP synthetase, could be consumed during the reduction of oxygen to water (2e
- + 1/2 O
2 + 2H
+ → H
2O) in which electrons for this reaction come from the oxidation of Fe(II) in a pathway that is thermodynamically favorable (downhill pathway). These ideas were first promulgated based upon theoretical considerations by Ingledew [
1] but the model has been extended more recently and major parts of it are now supported by experimental evidence (reviewed in [
2]).
According to the model (see Figure ), components involved in the downhill electron pathway from Fe(II) to oxygen include: an outer membrane high molecular-weight cytochrome
c encoded by
cyc2, a gene of unknown function (ORF1), a periplasmic soluble blue copper protein rusticyanin encoded by
rus, a periplasmic membrane-bound dihemic cytochrome
c4 encoded by
cyc1 and a terminal cytochrome oxidase of the
aa3-type encoded by the
coxBACD gene cluster [
3-
6]. In
A. ferrooxidans ATCC 33020 these genes are cotranscribed in an eight gene transcriptional unit, termed the
rus operon that is upregulated in Fe(II)-grown cells [
5,
7]. Gene context analysis of the recently annotated genomic sequence of
A. ferrooxidans type strain ATCC 23270 demonstrates that the
rus operon is similarly organized in this strain [
8].
The uphill components include: a cytochrome
bc1 complex (complex III, ubiquinol-cytochrome
c reductase), the quinone pool and a NADH1 dehydrogenase complex (hereafter abbreviated to NADH complex) functioning in reverse [
9-
11]. Genetic and biophysical evidence obtained for
A. ferrooxidans ATCC 19859 and ATCC 33020 support this view [
11-
13]. In these two strains, the genes encoding the
bc1 complex have been shown to be part of a five-gene operon, termed the
petI operon, mainly transcribed in Fe(II) conditions and organized as following: a diheme cytochrome
c4 (
cycA1), a short-chain dehydrogenase (
sdrA1) of unknown function, a cytochrome
b (
petA1), an iron-sulfur protein Rieske (
petB1), and a cytochrome
c1 (
petC1) [
2,
12,
13]. Based on the cotranscription of the diheme cytochrome
c4 gene (
cycA1) with those encoding the
bc1 complex, it was proposed that electrons from the diheme cytochrome
c4 take a thermodynamically uphill pathway via the
bc1 complex to a NADH complex driven energetically by proton motive force [
2,
12-
14] (see Figure ). Adjacent to the
petI operon, is a three gene (
resBC and a hypothetical gene) operon in which ResBC are predicted to be chaperones involved in heme insertion in
c-type cytochromes, possibly those involved in the maturation of the
c1 cytochrome of the
bc1 complex [
12]. The
petI operon is similarly organized and transcribed in
A. ferrooxidans ATCC 23270 [
14] supporting this model.
The bifurcation in the flow of electrons from Fe(II) to reduce either NAD (uphill) or O
2 (downhill) has been proposed to occur at the level of rusticyanin, a small periplasmic blue copper protein [
2,
13,
14] (see Figure ). By adjusting the flow of electrons at this branch point, it was suggested that
A. ferrooxidans could balance its requirements for NADH and ATP [
9].
The components involved in both the uphill and downhill electron flow have been shown to form a Fe-oxidizing/O
2-reducing supercomplex spanning both inner and outer membranes in an unnamed strain of
A. ferrooxidans [
15] supporting previous models. The supercomplex has also been suggested to include a copper containing protein (ORF1) physically associated with the periplasmic Cyc1 that is proposed to be involved in downhill electron flow. In addition,
in vitro reconstitution of the iron oxidation system of the
A. ferrooxidans type strain with rusticyanin,
aa3-type cytochrome oxidase, the cytochromes
c Cyc2 and Cyc1 has been reported recently [
16].
Despite progress in understanding iron oxidation in the Acidithiobacillus genus, several lacunae in our knowledge persist, such as the identification of components involved in the proposed connection between the bc1/quinone complex and the NADH complex, the identification of the chaperones used for cofactor insertion into the relevant redox proteins, and the mechanisms and components regulating the electron flux via the downhill pathway to O2 versus the uphill pathway to the NADH complex.
Reduced inorganic sulfur oxidation is widespread in prokaryotes (reviewed in [
17,
18]. However, in contrast to iron that occurs in only two oxidation states, sulfur exists in multiple states from -2 to +6, complicating identification of intermediates and relevant enzymes in sulfur oxidation. Also, some sulfur compounds can be oxidized abiotically adding further difficulties in resolving enzymatic steps from chemical changes. Despite these difficulties, several biological pathways for RISCs oxidation have been identified including the phylogenetically widespread sulfur oxidizing (
sox) gene pathway (reviewed in [
17]) and the archaeal type sulfur oxygenase reductase (
sor) gene system (reviewed in [
19]). However, neither
sox, nor
sor have been detected in the genome of
A. ferrooxidans [
2,
8], raising the question as to how this organism oxidizes RISCs.
Much of our knowledge of RISCs oxidation in
A. ferrooxidans comes from enzyme assays performed many years ago on different strains, some of which await phylogenetic characterization or, in some cases, have not yet even been isolated as pure cultures [
2]. Those that have been characterized form genetically diverse clusters with at least three phylogenetic groups [
20-
23]. This raises the possibility that current models of RISCs oxidation reflect a patchwork assemblage of predicted pathways and activities that may not exist
in toto in any one
A. ferrooxidans strains and perhaps more accurately reflect the pangenomic capacity of the genus
Acidithiobacillus for RISCs oxidation.
Thus the current investigation was prompted by the need to generate a more comprehensive picture of iron and sulfur bioenergetics by searching for missing steps and predicting novel enzymatic and electron transfer components and to provide a coherent picture of these processes in one strain of A. ferrooxidans (type strain, ATCC 23270), facilitating the recognition of species variation in bioenergetic pathways.