SummaryThe cell walls of Sulfolobales species consist of proteinaceous S-layers assembled from two polypeptides, SlaA and SlaB. We isolated the large S-layer protein of Acidianus ambivalens and both S-layer subunits of Sulfolobus solfataricus and Metallosphaera sedula, respectively. The slaAB genes, lying adjacently in the chromosomes, are constitutively transcribed as bicistronic operons in A. ambivalens and S. solfataricus. A smaller slaA transcript appeared in Northern hybridizations of A. ambivalens RNA. PCRs experiments showed that 80-85% of the transcripts stop at an oligo-T terminator downstream of slaA while 15-20% are read through to a second terminator downstream of slaB. The bicistronic operons including promoter and terminator regions are conserved in the Sulfolobales. While no SlaA homologue is found outside the Sulfolobales, SlaB is distantly similar to S-layer proteins of other Crenarchaeota, e.g. the Staphylothermus marinus tetrabrachion. Molecular modelling suggests SlaBs to be composed of 2-3 consecutive beta sandwich domains, a coiled-coil domain of 15-17 nm in length and a C-terminal transmembrane helix. Electron microscopy shows crystalline protein arrays with triangular and hexagonal pores. We propose that the mushroom-shaped 'unit cells' of the Sulfolobales' S-layers consist of three SlaBs anchoring the complex in the membrane and six SlaAs forming the detergent-resistant outer sacculus.

Background: The sulfur oxygenase reductase (SOR) is the initial enzyme of the sulfur oxidation pathway in the thermoacidophilic Archaeon Acidianus ambivalens. The SOR catalyzes an oxygen-dependent sulfur disproportionation to H2S, sulfite and thiosulfate. The spherical, hollow, cytoplasmic enzyme is composed of 24 identical subunits with an active site pocket each comprising a mononuclear non-heme iron site and a cysteine persulfide. Substrate access and product exit occur via apolar chimney-like protrusions at the fourfold symmetry axes, via narrow polar pores at the threefold symmetry axes and via narrow apolar pores within in each subunit. In order to investigate the function of the pores we performed site-directed mutagenesis and inhibitor studies. Results: Truncation of the chimney-like protrusions resulted in an up to sevenfold increase in specific enzyme activity compared to the wild type. Replacement of the salt bridge-forming Arg99 residue by Ala at the threefold symmetry axes doubled the activity and introduced a bias toward reduced reaction products. Replacement of Met296 and Met297, which form the active site pore, lowered the specific activities by 25–55% with the exception of an M296V mutant. X-ray crystallography of SOR wild type crystals soaked with inhibitors showed that Hg2+ and iodoacetamide (IAA) bind to cysteines within the active site, whereas Zn2+ binds to a histidine in a side channel of the enzyme. The Zn2+ inhibition was partially alleviated by mutation of the His residue. Conclusions: The expansion of the pores in the outer shell led to an increased enzyme activity while the integrity of the active site pore seems to be important. Hg2+ and IAA block cysteines in the active site pocket, while Zn2+ interferes over a distance, possibly by restriction of protein flexibility or substrate access or product exit.

A biochemical, biophysical, and phylogenetic study of the sulfur oxygenase reductase (SOR) from the mesophilic gammaproteobacterium Halothiobacillus neapolitanus (HnSOR) was performed in order to determine the structural and biochemical properties of the enzyme. SOR proteins from 14 predominantly chemolithoautotrophic bacterial and archaeal species are currently available in public databases. Sequence alignment and phylogenetic analysis showed that they form a coherent protein family. The HnSOR purified from Escherichia coli after heterologous gene expression had a temperature range of activity of 10 to 99°C with an optimum at 80°C (42 U/mg protein). Sulfite, thiosulfate, and hydrogen sulfide were formed at various stoichiometries in a range between pH 5.4 and 11 (optimum pH 8.4). Circular dichroism (CD) spectroscopy and dynamic light scattering showed that the HnSOR adopts secondary and quaternary structures similar to those of the 24-subunit enzyme from the hyperthermophile Acidianus ambivalens (AaSOR). The melting point of the HnSOR was ≈20°C lower than that of the AaSOR, when analyzed with CD-monitored thermal unfolding. Homology modeling showed that the secondary structure elements of single subunits are conserved. Subtle changes in the pores of the outer shell and increased flexibility might contribute to activity at low temperature. We concluded that the thermostability was the result of a rigid protein core together with the stabilizing effect of the 24-subunit hollow sphere.

Rieske proteins and Rieske ferredoxins are present in the three domains of life and are involved in a variety of cellular processes. Despite their functional diversity, these small Fe-S proteins contain a highly conserved all-b fold, which harbors a [2Fe-2S] Rieske center. We have identified a novel subtype of Rieske ferredoxins present in hyperthermophilic archaea, in which a twocysteine conserved SKTPCX (2-3) C motif is found at the C-terminus. We establish that in the Acidianus ambivalens representative, Rieske ferredoxin 2 (RFd2), these cysteines form a novel disulfide bond within the Rieske fold, which can be selectively broken under mild reducing conditions insufficient to reduce the [2Fe-2S] cluster or affect the secondary structure of the protein, as shown by visible circular dichroism, absorption, and attenuated total reflection Fourier transform IR spectroscopies. RFd2 presents all the EPR, visible absorption, and visible circular dichroism spectroscopic features of the [2Fe-2S] Rieske center. The cluster has a redox potential of ?48 mV (25°C and pH 7) and a pK a of 10.1 ± 0.2. These shift to ?77 mV and 8.9 ± 0.3, respectively, upon reduction of the disulfide. RFd2 has a melting temperature near the boiling point of water (T m = 99°C, pH 7.0), but it becomes destabilized upon disulfide reduction (DT m = -9°C, DC m = -0.7 M guanidinium hydrochloride). This example illustrates how the incorporation of an additional structural element such as a disulfide bond in a highly conserved fold such as that of the Rieske domain may fine-tune the protein for a particular function or for increased stability.

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