Biochemical and Biophysical Research Communications 369 (2008) 919–923 Contents lists available at ScienceDirect Biochemical and Biophysical Research Communications journal homepage: www.elsevier.com/locate/ybbrc Crystal structure studies on sulfur oxygenase reductase from Acidianus tengchongensis Mei Li a, Zhiwei Chen b, Pingfeng Zhang a,c, Xiaowei Pan a,c, Chengying Jiang b, Xiaomin An a, Shuangjiang Liu b, Wenrui Chang a,* a National Laboratory of Biomacromolecules, Institute of Biophysics, Chinese Academy of Sciences, 15 Datun Road, Chaoyang District, Beijing 100101, PR China State Key Laboratory of Microbial Resources, Institute of Microbiology, Chinese Academy of Sciences, Beijing 100101, PR China c Graduate University of the Chinese Academy of Sciences, Beijing 100049, PR China b a r t i c l e i n f o Article history: Received 20 February 2008 Available online 7 March 2008 Keywords: Sulfur oxygenase reductase Crystal structure Non-heme iron center Channels Monomer tunnel a b s t r a c t Sulfur oxygenase reductase (SOR) simultaneously catalyzes oxidation and reduction of elemental sulfur to produce sulfite, thiosulfate, and sulfide in the presence of molecular oxygen. In this study, crystal structures of wild type and mutants of SOR from Acidianus tengchongensis (SOR-AT) in two different crystal forms were determined and it was observed that 24 identical SOR monomers form a hollow sphere. Within the icosatetramer sphere, the tetramer and trimer channels were proposed as the paths for the substrate and products, respectively. Moreover, a comparison of SOR-AT with SOR-AA (SOR from Acidianus ambivalens) structures showed that significant differences existed at the active site. Firstly, Cys31 is not persulfurated in SOR-AT structures. Secondly, the iron atom is five-coordinated rather than six-coordinated, since one of the water molecules ligated to the iron atom in the SOR-AA structure is lost. Consequently, the binding sites of substrates and a hypothetical catalytic process of SOR were proposed. Ó 2008 Elsevier Inc. All rights reserved. Biological oxidation and reduction of elemental sulfur are important reactions involved in the biogeochemical cycles of sulfur element. Members of the thermoacidophilic archaea, such as Sulfolobus and Acidianus, have been frequently isolated and detected from sulfur-containing thermal vents [1–3], suggesting that they are popular inhabitants and may play important ecological roles in those environments. Some members of the genera Sulfolobus and Acidianus oxidize sulfur for energy and their first step of sulfur oxidation was catalyzed by sulfur oxygenase reductases (SORs). SOR was first described by Emmel et al. [4]. Currently, SOR and its homologs have been identified in thermophilic and acidophilic archaea [5–8] and bacteria [9,10]. SOR simultaneously catalyzes the oxidation and reduction of elemental sulfur to produce sulfite, thiosulfate, and sulfide in the presence of molecular oxygen [4,7]. No requirements for cofactors or external electron donors/acceptors for the reaction have been reported [11,12]. The optimal catalytic temperatures for SORs from Acidianus tengchongensis and Acidianus ambilvalens were reported to be 65–85 °C. The active site of SOR is composed of a mononuclear non-heme iron site and three conserved cysteine residues. The crystal structure of the SOR-AA showed that the enzyme is a multimer containing 24 identical subunits, forming a large hollow sphere. Six * Corresponding author. Fax: +86 10 64889867. E-mail address: [email protected] (W. Chang). 0006-291X/$ - see front matter Ó 2008 Elsevier Inc. All rights reserved. doi:10.1016/j.bbrc.2008.02.131 chimney-like protrusions, each composed of four helices that belonged to four individual monomers, were observed in the spherical structure. It was proposed that the chimney-like protrusions were the entry routes of the substrate [13]. However, there are some questions that remain unanswered, such as whether any channel that functions as the exit route for products exists within the sphere? Moreover, the detailed process of the SOR catalytic reaction remains to be accounted. In the present work, we studied enzymatic activities on wild type and mutants of SOR-AT and solved the crystal structures of recombinant SOR in two different crystal forms (I432 and R3). Although the overall folding of the SOR-AT structure is similar to that of the SOR-AA structure, the catalytic sites in the two are quite different. The detailed catalytic process and the exit routes for products were analyzed based on our structures. These results may provide new insights for understanding the catalytic process and the mechanism of SORs. Materials and methods Protein expression, purification, and enzymatic activity assays. The expression of wild type and mutants of SOR were performed as described previously [14]. Protein concentration was determined using a BCA protein assay kit (Sigma), by following the instructions of the manufacturer (BCA1, Sigma, USA). The oxygenase activity of SOR was determined as described before [15]. One unit (U) is defined as the amount of enzyme required for the formation of 1 lmol of sulfite plus thiosulfate per minute. The concentrations of SO32 and S2O32 were determined by basic fuschnin and methylene blue methods, respectively [8]. 920 M. Li et al. / Biochemical and Biophysical Research Communications 369 (2008) 919–923 Crystallization and data collection. Crystallization trials were set up using the Hampton Research Screen Kit I & II (98 conditions) by applying the hanging drop vapor diffusion technique with drops of 1 ll protein solution and 1 ll crystallization reagent, which were allowed to equilibrate against 500 ll of crystallization reagent in a well reservoir. Finally, two crystal forms of SOR suitable for diffraction studies were obtained using optimized conditions (crystal form I: 1.08 M NaCitr3, 0.1 M Hepes buffer, pH 7.5, 303 K; crystal form II: 25% PEG400, 0.1 M NaI, 0.1 M Hepes buffer, pH 7.1, 289 K). For crystal form I, a 2.7 Å resolution dataset of wild type SOR was collected at BL6B in the Photon Factory, Tsukuba, Japan. A separate dataset of a mutant SOR (C101S) was collected to 3.2 Å resolution from crystal form II, by utilizing a Rigaku R-AXIS IV image plate detector at Institute of Biophysics, CAS. Both diffraction data were collected at 100 K and were integrated and scaled with programs DENZO and SCALEPACK [16]. The results showed that crystal form I belongs to the space group I432, crystal form II belongs to the space group R3. Structure determination and refinement. The structure was solved by molecular replacement with MolRep [17] in the CCP4 suite [18]. The search model was SORAA structure (PDB code: 2CB2), which displays 88% sequence identity to SOR-AT. The initial model was manually rebuilt with the program O [19] and refined by ARP/warp [20] and refmac5 [21]/CNS [22]. The stereochemical quality of the refined structures was verified with the program PROCHECK [23]. A summary of the data collection and structure refinement statistics is provided in Table 1. The atomic coordinate of the SOR crystal structure had been deposited in the Protein Data Bank with Accession No. 3BXV. Figs. 1–4a were created using the program PyMol (DeLano Scientific, LLC). Results and discussion In the present study, crystal structures of wild type and mutant (C101S) of SOR-AT were solved in two different crystal forms: I432 and R3. It should be noted that the sequence of the SOR protein of the I432 form differs from the NCBI protein sequence AAK58572 at two positions (K174E and V238A). These changes might be due to errors introduced during PCR amplification or because of the passing of the generation in Escherichia coli. However, both sites are not conserved among SOR proteins, as shown in Supplementary Fig. 1. Further, these mutations did not affect the SOR enzymatic activity at all (Supplementary Table 1). Table 1 Data collection and refinement statistics of SOR Crystal form I II Space group Cell parameters Resolution (Å) No. of total reflections No. of unique reflections Completeness (%) I/Sigma Rmerge (on I) (%) Molecules (A. U.) No. of residues No. of Fe atoms No. of water molecules Rcryst (%) Rfree (%) I432 a = b = c = 159.1 Å, a = b = c = 90° 30–2.7 (2.80–2.70) 90,202 9396 99.6 (98.7) 22.7 (3.8) 8.2 (37.7) 1 308 1 53 19.2 21.3 R3 a = b = 225.2 Å, c = 137.1 Å, c = 120° 50–3.2 (3.31–3.20) 123,519 41,173 96.2 (93.9) 6.6 (2.8) 13.9 (29.3) 8 2456 8 253 21.6 25.3 RMS deviations Bond (Å) Angle (°) 0.010 1.73 0.011 1.83 Average B-value (Å2) Main chain Side chain Fe atoms Water molecules 30.4 31.2 34.7 32.1 14.0 14.9 13.0 13.1 90.7 9.3 81.6 18.3 Ramachandran Most-favored regions (%) Additional allowed regions (%) Generously allowed regions (%) 0.1 Overall structure and the active site of SOR monomer The architectures of two independently refined structures of SOR-AT are nearly identical. The monomer consists of 308 amino acid residues and belongs to the a/b folding type. The core structure is a b-barrel composed of eight b-strands (E1–E8) surrounded by nine a-helices (H1–H9) (Fig. 1A). The active sites of the two structures in different crystal forms are also very similar. They are composed of three cysteine residues and an iron atom, which is coordinated by His86, His90, Glu114, and a water molecule (Fig. 1B). Replacements of His86 or His90 by a phenylalanine residue resulted in a dramatic reduction in SOR activity. Mutation of any cysteine residues (C31S, C101S, and C104S) at the active site also leads to complete loss of SOR catalytic ability (Supplementary Table 1). The importance of these residues is also emphasized by their 100% conservation in all SOR proteins (Supplementary Fig. 1). A comparison of the two structures showed that the conformation of Ser101 of the inactive mutant C101S, which was solved as the R3 form, is the same as that of Cys101 in the I432 form, the wild type structure (Fig. 1B), with only a c-O atom substituted for a c-S atom. This indicated that only the c-S atom contributed to the SOR function. The cysteine–cysteine and cysteine–iron distances are in the range of 5.5–12.4 Å, which is quite reasonable considering the size of elemental sulfur, one of the substrates of SOR. The two mutated residues (K174E and V238A) are located far away from the active site in the I432 form (Fig. 1A), thus having little influence on its enzymatic activity. Tetramer and trimer channels in SOR icosatetramer sphere might be routes for substrate entry and product exit, respectively In both crystal forms, 24 identical monomers are assembled into a hollow sphere according to point group symmetry 432 (Supplementary Fig. 2), which is consistent with the SOR-AA crystal structure. The distance among different active sites of neighboring monomers is greater than 37 Å, which makes it almost impossible for cooperative catalysis by individual monomers. Since the active site of each monomer is accessible to the solvent only from the inside of the sphere, it was postulated that the possible function of this packing is to form an isolated environment. Therefore, there must be passages for the entry of substrates and the exit of products. There are six protruding channels, referred to as tetramer channels, which were formed by identical a-helices (H4) of four individual monomers along the fourfold symmetry axes. Their inner surface is highly hydrophobic, formed by residues Phe133, Val137, and Phe141. The phenyl groups of Phe133 and Phe141 residues of each monomer stick out at the inner surface of the channel (Fig. 2A). Given the size and strong hydrophobic property fulfill the requirement of substrate [S0], these channels are likely to be the paths for substrate entry into the sphere; this was previously noticed by Urich et al. [13]. However, the question of how and where the products leave remains. Are the tetramer channels also the paths for products exit, or are there other channels for products? Careful examination of our structures suggested that eight channels, each composed of H3 and a loop region (H6–E7) of three individual monomers, might be the product channels (Fig. 2B), referred to as trimer channels. Unlike the tetramer channels, trimer channels are more polar, with Ser95, Arg99, Ser103, and Ser226 contributing to their inner surface. The side chains of Arg99 and Ser226 stick out, forming a narrow gorge of the trimer channel (Fig. 2B). Considering the smaller size and the positively charged nature, it was assumed that trimer channels might be used for products exit. M. Li et al. / Biochemical and Biophysical Research Communications 369 (2008) 919–923 921 Fig. 1. (A) Superposition of the overall structures of SOR-AT between the two crystal forms. The core structure is composed of nine a-helices and eight b-strands. The secondary structure is labeled as H1–H9 for helices and E1–E8 for strands. The structure of the I432 form is shown in blue and that of the R3 form, in green. The iron atom is represented as a large sphere and the ligated water molecule as a small sphere. Two mutated residues in the I432 form are represented as sticks and labeled in red italic fonts. (B) Superposition of the active site of SOR-AT structures between the two crystal forms. The color designation is the same as that in (A). The iron atom and water molecule are represented as spheres. The residues constituting the active site are shown as sticks. The conformation of C101 in the I432 form and that of S101 in the R3 form are similar. The residue is labeled by a letter within parentheses; the letters refer to the amino acid type in the R3 form. (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.) Fig. 2. Ribbon representation of the tetramer channel and trimer channel in SOR-AT structure. (A) Tetramer channel. Four individual monomers are shown in red, orange, green, and purple. The side chains of residues Phe133, Val137, and Phe 141 at each monomer, which contributed to the inner surface of the tetramer channel, are shown as sticks. View along the crystallographic fourfold axis. (B) Trimer channel. Three individual monomers are shown in red, blue, and pink. The side chains of residues Arg99 and Ser 226 at each monomer, which contributed to the inner surface of the trimer channel, are shown as sticks. View along the crystallographic threefold axis. (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.) Monomer tunnel in SOR structure Besides tetramer and trimer channels, monomer tunnels were also observed in our structures. The iron atom is buried inside the SOR molecule and is accessible to the solvent only through the monomer tunnel, which can also be described as the joining of two differently orientated pockets. One pocket is wider; its opening at the SOR surface is formed by Phe20, Phe23, Ser24, Gly27, Val47, Val296, and Met297 (Fig. 3A). The other is relatively narrow, the opening being made up of Ala105, Met108, Pro112, and Phe210 (Fig. 3B). The observation of the monomer tunnel in the whole icosatetramer sphere structure revealed that the wider opening lies near the tetramer channel, while the narrower one lies close to the tri- mer channel. However, the narrow opening is covered by a loop from another monomer, with Glu560 , Arg570 , Phe580 , and Gly590 in its vicinity. Interestingly, the side chains of all these residues swing away, maintaining this pocket in the open state (Supplementary Fig. 3). Moreover, the side chain of Arg570 swings back and is just located near the narrow opening of the monomer tunnel, which may facilitate the movement of negatively charged products toward it. Thus, it was proposed that the wider opening of the tunnel is the entrance, which is used by the substrate to access the active site, while the narrower one is the exit. At the active site, the iron atom and its binding residues are located close by, while the three cysteine residues are located far from them. Relative to the iron atom, Cys31 is located on the entrance side of the monomer tunnel, while Cys101 and 104 are 922 M. Li et al. / Biochemical and Biophysical Research Communications 369 (2008) 919–923 Fig. 3. Surface representations of SOR monomer. Red represents a negative charge, and blue represents a positive charge. The monomer surface is shown as a transparent layer. There are two openings of the monomer tunnel at the SOR surface. The residues constituting the openings are labeled. The iron atom is represented as a sphere. (A) The entrance of the monomer tunnel. (B) The exit of the monomer tunnel. (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.) Fig. 4. (A) Superposition of the active site between the SOR-AT (I432 form) and SOR-AA structures. The iron atom is represented as a large sphere and water molecules as small spheres. The residues constituting the active site are shown as sticks. The SOR-AA structure is shown in green, while the color of the SOR-AT structure is represented by the atom type: yellow, carbon atom; red, oxygen atom (water molecule is included); blue, nitrogen atom; orange, sulfur atom; magenta, iron atom. (B) The stereo view of electron density maps at the active site of SOR. The color designation is the same as that in (A). The structures are shown by a ball and stick model. The 2 Fo–Fc electron density map countered at 1r is shown in blue, the Fo–Fc electron density map countered at 2.5r is shown in red. (For interpretation of the references to color in this figure legend, the reader is referred to the web version of this article.) M. Li et al. / Biochemical and Biophysical Research Communications 369 (2008) 919–923 923 located on the exit side, implying that the function of these cysteine residues might be different during the catalytic reaction process. Since the whole catalytic reaction of SOR could be split into sulfur oxidation and sulfur disproportionation reactions, it was postulated that Cys31 is involved in the oxidation reaction, while Cys101 and 104 are involved in the latter reaction. Appendix A. Supplementary data Comparison of SOR-AT and SOR-AA structures [1] T.D. Brock, K.M. Brock, R.T. Belly, R.L. Weiss, Sulfolobus: a new genus of sulfuroxidizing bacteria living at low pH and high temperature, Arch. Microbiol. 84 (1972) 54–68. [2] N.P. Burton, P.R. Norris, Microbiology of acidic, geothermal springs of Montserrat: environmental rDNA analysis, Extremophiles 4 (2000) 315–320. [3] S. Simmons, R. Norris, Acidophiles of saline water at thermal vents of Vulcano, Italy, Extremophiles 6 (2002) 201–207. [4] T. Emmel, W. Sand, W.A. Konig, E. Bock, Evidence for the existence of a sulfur oxygenase in Sulfolobus-brierleyi, J. Gen. Microbiol. 132 (1986) 3415– 3420. [5] Z. He, Y. Li, P. Zhou, S. Liu, Cloning and heterologous expression of a sulfur oxygenase/reductase gene from the thermoacidophilic archaeon Acidianus sp. S5 in Escherichia coli, FEMS Microbiol. Lett. 193 (2000) 217–221. [6] Z.G. He, H. Zhong, Y. Li, Acidianus tengchongensis sp. nov., a new species of acidothermophilic archaeon isolated from an acidothermal spring, Curr. Microbiol. 48 (2004) 159–163. [7] A. Kletzin, Coupled enzymatic production of sulfite, thiosulfate, and hydrogen sulfide from sulfur: purification and properties of a sulfur oxygenase reductase from the facultatively anaerobic archaebacterium Desulfurolobus ambivalens, J. Bacteriol. 171 (1989) 1638–1643. [8] A. Kletzin, Molecular characterization of the sor gene, which encodes the sulfur oxygenase/reductase of the thermoacidophilic Archaeum Desulfurolobus ambivalens, J. Bacteriol. 174 (1992) 5854–5859. [9] Z.W. Chen, Y.Y. Liu, J.F. Wu, Q. She, C.Y. Jiang, S.J. Liu, Novel bacterial sulfur oxygenase reductases from bioreactors treating gold-bearing concentrates, Appl. Microbiol. Biotechnol. 74 (2007) 688–698. [10] G. Deckert, P.V. Warren, T. Gaasterland, W.G. Young, A.L. Lenox, D.E. Graham, R. Overbeek, M.A. Snead, M. Keller, M. Aujay, R. Huber, R.A. Feldman, J.M. Short, G.J. Olsen, R.V. Swanson, The complete genome of the hyperthermophilic bacterium Aquifex aeolicus, Nature 392 (1998) 353–358. [11] T. Urich, T.M. Bandeiras, S.S. Leal, R. Rachel, T. Albrecht, P. Zimmermann, C. Scholz, M. Teixeira, C.M. Gomes, A. Kletzin, The sulphur oxygenase reductase from Acidianus ambivalens is a multimeric protein containing a low-potential mononuclear non-haem iron centre, Biochem. J. 381 (2004) 137–146. [12] T. Urich, A. Kroke, C. Bauer, K. Seyfarth, M. Reuff, A. Kletzin, Identification of core active site residues of the sulfur oxygenase reductase from Acidianus ambivalens by site-directed mutagenesis, FEMS Microbiol. Lett. 248 (2005) 171–176. [13] T. Urich, C.M. Gomes, A. Kletzin, C. Frazao, X-ray structure of a selfcompartmentalizing sulfur cycle metalloenzyme, Science 311 (2006) 996– 1000. [14] C.W. Sun, Z.W. Chen, Z.G. He, P.J. Zhou, S.J. Liu, Purification and properties of the sulfur oxygenase/reductase from the acidothermophilic archaeon, Acidianus strain S5, Extremophiles 7 (2003) 131–134. [15] Z.W. Chen, C.Y. Jiang, Q. She, S.J. Liu, P.J. 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Biol. 298 (2000) 691–704. The superposition of SOR-AT (I432 form) and SOR-AA structures showed that their overall architectures are quite similar; however, significant differences were found with regard to the active site. A very special residue, Css31 (cysteine persulfide), was refined in the SOR-AA structure. Previous reports showed that the sulfane sulfur atoms are labile species, usually generated in the catalytic cycles of the synthesis of sulfur-containing biomolecules [24,25]. In contrast, the residue in SOR-AT structures is a cysteine, and no extra Fo–Fc electron density around the c-S atom of Cys31 was found (Fig. 4). Another difference is that the iron atom is five-coordinated, and only one of the two water molecules (Wat1 and Wat2) that coordinate the iron atom in the SOR-AA structure was found in the SOR-AT structures (Fig. 4A). As Fig. 4B shows, the Fo–Fc density countered at 2.5r was clearly present at the positions of Wat1 and the adjacent solvent molecule, while no Fo–Fc density exists at the positions of Wat2 and the d-S atom of Css31. Postulated catalytic reaction process of SOR Since Cys31 is located at the entrance of the monomer tunnel, we proposed that it might be the real residue that binds the substrate [S0] at the initial step of the catalytic reaction; the binding site should be the position of the d-S atom of Css31 in the SORAA structure. Accordingly, the position of Wat2 in the SOR-AA structure was suggested to be the binding site of molecular oxygen. The two crystal structures might represent two different statuses in the catalytic reaction process of SOR, which is probably due to the different characteristics, different resources and/or the different crystallization conditions of the two proteins. Based on our structures, on combining the SOR-AA structure, a preliminary and hypothetical process of catalytic reaction of SOR can be proposed. The substrate sulfur initially entered the inner part of the icosatetramer sphere through the hydrophobic tetramer channel. It then moved toward the entrance of the monomer tunnel to access the active site by binding to the c-S atom of Cys31. Simultaneously, the oxygen molecule settled near the iron atom at the position of Wat2, thereby trigger the oxidation reaction. Cys101 and 104 might assist in sulfur binding, or they might probably be involved later in the disproportionation reaction. After the reaction was completed, the products moved via the exit of the monomer tunnel and then out of the sphere through the trimer channel. In this study, we observed trimer channels and monomer tunnels in SOR-AT structures for the first time. Besides, the structural comparison of SOR-AT and SOR-AA revealed the remarkable differences in their active sites, leading to the assumption that they might represent different statuses of SOR. Thus, a detailed process of the SOR catalytic reaction was suggested, which may provide new insights for better understanding SOR proteins. Acknowledgments This work was supported by the National Natural Science Foundation of China (Grant Nos. 30500094, 10490193, and 30621005), the 973 Project (Grant No. 2006CB911001). We are grateful to Drs. N. and K. Sakabe at Photon Factory, Japan, Dr. Yu-hui Dong and Dr. Peng Liu at the Institute of High Energy Physics, CAS, Mr. Yi Han at the Institute of Biophysics, CAS for data collection. Supplementary data associated with this article can be found, in the online version, at doi:10.1016/j.bbrc.2008.02.131. References
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