Margarida Santana

A novel scenario for the evolution of haem-copper oxygen reductases.

The increasing sequence information on oxygen reductases of the haem-copper superfamily, together with the available three-dimensional structures, allows a clear identification of their common, functionally important features. Taking into consideration both the overall amino acid sequences of the core subunits and key residues involved in proton transfer, a novel hypothesis for the molecular evolution of these enzymes is proposed. Three main families of oxygen reductases are identified on the basis of common features of the core subunits, constituting three lines of evolution: (i) type A (mitochondrial-like oxidases), (ii) type B (ba3-like oxidases) and (iii) type C (cbb3-type oxidases). The first group can be further divided into two subfamilies, according to the helix VI residues at the hydrophobic end of one of the proton pathways (the so-called D-channel): (i) type A1, comprising the enzymes with a glutamate residue in the motif -XGHPEV-, and (ii) type A2, enzymes having instead a tyrosine and a serine in the alternative motif -YSHPXV-. This second subfamily of oxidases is shown to be ancestor to the one containing the glutamate residue, which in the Bacteria domain is only present in oxidases from Gram-positive or purple bacteria. It is further proposed that the Archaea domain acquired terminal oxidases by gene transfer from the Gram-positive bacteria, implying that these enzymes were not present in the last common ancestor before the divergence between Archaea and Bacteria. In fact, most oxidases from archaea have a higher amino acid sequence identity and similarity with those from bacteria, mainly from the Gram-positive group, than with oxidases from other archaea. Finally, a possible relation between the dihaemic subunit (FixP) of the cbb3 oxidases and subunit II of caa3 oxidases is discussed. As the families of haem-copper oxidases can also be identified by their subunit II, a parallel evolution of subunits I and II is suggested.

The ‘strict’ anaerobe Desulfovibrio gigas contains a membrane‐bound oxygen‐reducing respiratory chain

Sulfate‐reducing bacteria are considered as strict anaerobic microorganisms, in spite of the fact that some strains have been shown to tolerate the transient presence of dioxygen. This report shows that membranes from Desulfovibrio gigas grown in fumarate/sulfate contain a respiratory chain fully competent to reduce dioxygen to water. In particular, a membrane‐bound terminal oxygen reductase, of the cytochrome bd family, was isolated, characterized, and shown to completely reduce oxygen to water. This oxidase has two subunits with apparent molecular masses of 40 and 29 kDa. Using NADH or succinate as electron donors, the oxygen respiratory rates of D. gigas membranes are comparable to those of aerobic organisms (3.2 and 29 nmol O2 min−1 mg protein−1, respectively). This ‘strict anaerobic’ bacterium contains all the necessary enzymatic complexes to live aerobically, showing that the relationships between oxygen and anaerobes are much more complex than originally thought.

The caa3 terminal oxidase of the thermohalophilic bacterium Rhodothermus marinus: a HiPIP:oxygen oxidoreductase lacking the key glutamate of the D-channel

The respiratory chain of the thermohalophilic bacterium Rhodothermus marinus contains a novel complex III and a high potential iron-sulfur protein (HiPIP) as the main electron shuttle (Pereira et al., Biochemistry 38 (1999) 1268-1275 and 1276-1283). In this paper, one of the terminal oxidases expressed in this bacterium is extensively characterised. It is a caa3-type oxidase, isolated with four subunits (apparent molecular masses of 42, 19 and 15 kDa and a C-haem containing subunit of 35 kDa), which has haems of the A(s) type. This oxidase is capable of using TMPD and horse heart cytochrome c as substrates, but has a higher turnover with HiPIP, being the first example of a HiPIP:oxygen oxidoreductase. The oxidase has unusually low reduction potentials of 260 (haem C), 255 (haem A) and 180 mV (haem A3). Subunit I of R. marinus caa3 oxidase has an overall significant homology with the subunits I of the COX type oxidases, namely the metal binding sites and most residues considered to be functionally important for proton uptake and pumping (K- and D-channels). However, a major difference is present: the putative essential glutamate (E278 in Paraccocus denitrificans) of the D-channel is missing in the R. marinus oxidase. Homology modelling of the R. marinus oxidase shows that the phenol group of a tyrosine residue may occupy a similar spatial position as the glutamate carboxyl, in relation to the binuclear centre. Moreover, sequence comparisons reveal that several enzymes lacking that glutamate have a conserved substitution pattern in helix VI: -YSHPXV- instead of -XGHPEV-. These observations are discussed in terms of the mechanisms for proton uptake and it is suggested that, in these enzymes, tyrosine may play the role of the glutamate in the proton channel.

Gene cluster of Rhodothermus marinus high-potential iron-sulfur Protein: oxygen oxidoreductase, a caa(3)-type oxidase belonging to the superfamily of heme-copper oxidases.

The respiratory chain of the thermohalophilic bacterium Rhodothermus marinus contains an oxygen reductase, which uses HiPIP (high potential iron-sulfur protein) as an electron donor. The structural genes encoding the four subunits of this HiPIP:oxygen oxidoreductase were cloned and sequenced. The genes for subunits II, I, III, and IV (named rcoxA to rcoxD) are found in this order and seemed to be organized in an operon of at least five genes with a terminator structure a few nucleotides downstream of rcoxD. Examination of the amino acid sequence of the Rcox subunits shows that the subunits of the R. marinus enzyme have homology to the corresponding subunits of oxidases belonging to the superfamily of heme-copper oxidases. RcoxB has the conserved histidines involved in binding the binuclear center and the low-spin heme. All of the residues proposed to be involved in proton transfer channels are conserved, with the exception of the key glutamate residue of the D-channel (E(278), Paracoccus denitrificans numbering). Analysis of the homology-derived structural model of subunit I shows that the phenol group of a tyrosine (Y) residue and the hydroxyl group of the following serine (S) may functionally substitute the glutamate carboxyl in proton transfer. RcoxA has an additional sequence for heme C binding, after the Cu(A) domain, that is characteristic of caa(3) oxidases belonging to the superfamily. Homology modeling of the structure of this cytochrome domain of subunit II shows no marked electrostatic character, especially around the heme edge region, suggesting that the interaction with a redox partner is not of an electrostatic nature. This observation is analyzed in relation to the electron donor for this caa(3) oxidase, the HiPIP. In conclusion, it is shown that an oxidase, which uses an iron-sulfur protein as an electron donor, is structurally related to the caa(3) class of heme-copper cytochrome c oxidases. The data are discussed in the framework of the evolution of oxidases within the superfamily of heme-copper oxidases.

Presence and expression of terminal oxygen reductases in strictly anaerobic sulfate-reducing bacteria isolated from salt-marsh sediments

In the anaerobic sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough genes were found encoding membrane terminal oxygen reductases of two types: a cytochrome c oxidase and a cytochrome bd oxidase, both enzymes are terminal oxidases typical of facultative or aerobic microorganisms (Heidelberg JF, et al., The genome sequence of the anaerobic, sulfate-reducing bacterium D. vulgaris Hildenborough. Nat Biotechnol 2004; 22: 554-9). To apprehend the presence of both oxidases in other sulfate-reducing bacteria (SRB), several assays were performed on isolates recovered from salt-marsh sediments in Portugal, representative of the different phylogenetic groups identified. Hybridization and PCR experiments for DNA sequencing were performed on the chosen isolates. Primers were selected to amplify conserved regions of cytochrome c oxidases and cytochrome bd oxidases taking into consideration alignment of corresponding subunit I sequences. The results showed that both oxidase genes are present on the chromosome of several isolates characterized as Desulfovibrio. These genes were shown to be transcribed, as demonstrated by Reverse Transcriptase-PCR experiments on total RNA. In order to assess the relative contribution of each oxidase to oxygen consumption, oxygen uptake was measured for each isolate and further characterized by the effect of cyanide on oxygen consumption. It was concluded that cytochrome bd oxidase was the terminal membrane oxygen reductase allowing oxygen consumption. In addition, it was observed that isolates containing cytochrome bd oxidase had higher resistance to air exposure, suggesting an important role of this enzyme in survival to air exposure. The pattern for the presence of oxygen reductase genes was compared to the physiological pattern of substrate use, which was determined for each isolate. Salinity tolerance, pH and temperature growth of each isolate were also analyzed.

Structure at 1.3 Å Resolution of Rhodothermus marinus caa3 Cytochrome c Domain

The cytochrome c domain of subunit II from the Rhodothermus marinus caa(3) HiPIP:oxygen oxidoreductase, a member of the superfamily of heme-copper-containing terminal oxidases, was produced in Escherichia coli and characterised. The recombinant protein, which shows the same optical absorption and redox properties as the corresponding domain in the holo enzyme, was crystallized and its structure was determined to a resolution of 1.3 A by the multiwavelength anomalous dispersion (MAD) technique using the anomalous dispersion of the heme iron atom. The model was refined to final R(cryst) and R(free) values of 13.9% and 16.7%, respectively. The structure reveals the insertion of two short antiparallel beta-strands forming a small beta-sheet, an interesting variation of the classical all alpha-helical cytochrome c fold. This modification appears to be common to all known caa(3)-type terminal oxidases, as judged by comparative modelling and by analyses of the available amino acid sequences for these enzymes. This is the first high-resolution crystal structure reported for a cytochrome c domain of a caa(3)-type terminal oxidase. The R.marinus caa(3) uses HiPIP as the redox partner. The calculation of the electrostatic potential at the molecular surface of this extra C-terminal domain provides insights into the binding to its redox partner on one side and its interaction with the remaining subunit II on the other side.

Inferring pathways leading to organic-sulfur mineralization in the Bacillales

Abstract Microbial organic sulfur mineralization to sulfate in terrestrial systems is poorly understood. The process is often missing in published sulfur cycle models. Studies on microbial sulfur cycling have been mostly centered on transformations of inorganic sulfur, mainly on sulfate-reducing and inorganic sulfur-oxidizing bacteria. Nevertheless, organic sulfur constitutes most sulfur in soils. Recent reports demonstrate that the mobilization of organic-bound-sulfur as sulfate in terrestrial environments occurs preferentially under high temperatures and thermophilic Firmicutes bacteria play a major role in the process, carrying out dissimilative organic-sulfur oxidation. So far, the determinant metabolic reactions of such activity have not been evaluated. Here, in silico analysis was performed on the genomes of sulfate-producing thermophilic genera and mesophilic low-sulfate producers, revealing that highest sulfate production is related to the simultaneous presence of metabolic pathways leading to sulfite synthesis, similar to the ones found in mammalian cells. Those pathways include reverse transsulfuration reactions (tightly associated with methionine cycling), and the presence of aspartate aminotransferases (ATs) with the potential of 3-sulfinoalanine AT and cysteine AT activity, which ultimately leads to sulfite production. Sulfite is oxidized to sulfate by sulfite oxidase, this enzyme is determinant in sulfate synthesis, and it is absent in many mesophiles.

Structure at 1.3A Resolution of Rhodothermus Marinus Caa(3) Cytochrome C Domain

The cytochrome c domain of subunit II from the Rhodothermus marinus caa(3) HiPIP:oxygen oxidoreductase, a member of the superfamily of heme-copper-containing terminal oxidases, was produced in Escherichia coli and characterised. The recombinant protein, which shows the same optical absorption and redox properties as the corresponding domain in the holo enzyme, was crystallized and its structure was determined to a resolution of 1.3 A by the multiwavelength anomalous dispersion (MAD) technique using the anomalous dispersion of the heme iron atom. The model was refined to final R(cryst) and R(free) values of 13.9% and 16.7%, respectively. The structure reveals the insertion of two short antiparallel beta-strands forming a small beta-sheet, an interesting variation of the classical all alpha-helical cytochrome c fold. This modification appears to be common to all known caa(3)-type terminal oxidases, as judged by comparative modelling and by analyses of the available amino acid sequences for these enzymes. This is the first high-resolution crystal structure reported for a cytochrome c domain of a caa(3)-type terminal oxidase. The R.marinus caa(3) uses HiPIP as the redox partner. The calculation of the electrostatic potential at the molecular surface of this extra C-terminal domain provides insights into the binding to its redox partner on one side and its interaction with the remaining subunit II on the other side.

High temperature microbial activity in upper soil layers.

Biomineralization at high temperatures in upper soil layers has been largely ignored, although desertification and global warming have led to increasing areas of soils exposed to high temperatures. Recent publications evidenced thermophilic bacteria ubiquity in soils as viable cells, and their role in nutrient cycling and seedling development. High temperature events, frequently observed at medium and low latitudes, locate temporal niches for thermophiles to grow in soils. There, at temperatures inhibitory for common mesophiles, thermophilic bacteria could perform biogeochemical reactions important to the soil food web. Nutrient cycling analyses in soils at medium and low latitudes would benefit from considering the potential role of thermophiles.

Desulfovibrio vulgaris Hildenborough transcriptomic analysis by restriction fragment functional display (RFFD)

Comunicacion presentada a la citada conferencia, celebrada del 28 noviembre-1 diciembre, 2007, Sevilla, Espana.