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Journal of Bacteriology, June 2004, p. 3408-3414, Vol. 186, No. 11
0021-9193/04/$08.00+0 DOI: 10.1128/JB.186.11.3408-3414.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
and Robert E. Blankenship1*
Department of Chemistry and Biochemistry, Arizona State University, Tempe, Arizona 85287-1604,1 School of Life Sciences, Arizona State University, Tempe, Arizona 85287-45012
Received 28 October 2003/ Accepted 17 February 2004
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SODs are metalloenzymes and are found in eukaryotes and aerobic and aerotolerant bacteria (10). The two primary families of these enzymes are the copper- and zinc-containing SODs (CuZnSODs) and the iron- or manganese-containing SODs (Fe/MnSODs). The CuZnSODs have little primary sequence or structural homology to the Fe/MnSODs and are thought to have evolved independently (6). Cambialistic SODs have been found in the Fe/Mn family. These enzymes are capable of using either manganese or iron catalytically. Some cambialistic SODs normally contain various amounts of both metals, while others contain either iron or manganese exclusively depending on the availability of metals in the growth medium (2, 12).
Chloroflexus aurantiacus is a thermophilic photosynthetic bacterium that lives in shallow alkaline bacterial mats that flourish at pH 8.0 in hot spring water at 52 to 60°C (3, 20). These mats are directly exposed to near-UV radiation during the day, which is a potent source of oxidative stress (13). C. aurantiacus was previously found to have relatively high resistance to damage caused by UV radiation (19). This bacterium grows rapidly as a photoheterotroph by using organic carbon, although it can also grow photoautotrophically by using either sulfide or hydrogen as an electron donor for carbon dioxide fixation (21). Chloroflexus cohabitates with various cyanobacterial Synechococcus species at and below the surface of the bacterial mats. This environment is extremely hyperoxic due to the local release of oxygen from Synechococcus photosynthesis during the day. In the top 1 mm of other cyanobacterium-containing mats, the oxygen levels are 200% of the air saturation levels (22). Oxidative stress in C. aurantiacus is also of interest because this bacterium is deeply rooted in the 16S rRNA tree of organisms and is in the earliest branch of phototrophs (26).
Here, we describe cloning, expression, and characterization of the SOD from C. aurantiacus. The SOD was expressed in Escherichia coli as an easily purified fusion construct with maltose binding protein (MBP). We show that this enzyme is cambialistic and is highly resistant to inhibition by hydrogen peroxide. Metal fidelity studies and growth medium metal enrichment experiments demonstrated that this enzyme is most efficient when manganese is incorporated, yet up to 30% of the activity is maintained with iron. Amino acid sequence analysis and phylogenetic analysis revealed that this SOD has an array of residues that are characteristic of both FeSODs and MnSODs.
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Western blotting. Antiserum was prepared by injecting polyacrylamide gel slices containing approximately 100 µg of wtSOD into rabbits. Gel slices were homogenized in 1 ml of phosphate-buffered saline and 1 ml of complete Freund's adjuvant. Three booster shots containing 100 µg of wtSOD were administered in the same manner by using incomplete Freund's adjuvant. Antibody was produced by Rockland, Inc., Gilbertsville, Pa. Antibodies were purified from the rabbit serum by first desalting it with an Econo-Pac DG-10 column, and then pure immunoglobulin G was isolated by using an Econo-Pac serum immunoglobulin G purification chromatography column (Bio-Rad). Western blotting was performed by electrophoresing 10 µg of C. aurantiacus whole-cell extract and 8 µg of pure recombinant SOD on a sodium dodecyl sulfate (SDS)-polyacrylamide gel electrophoresis gel, which was then transferred to an Immobilon-P transfer membrane (Millipore, Bedford, Mass.) for 8 h at 100 mA. The protein concentrations of SOD samples were quantified by using a Coomassie Plus protein assay reagent kit (Pierce, Rockford, Ill.). The membrane was blocked in TTBS (0.1 M Tris HCl [pH 7.5], 0.15 M NaCl, 0.01% Tween 20) containing 5.0% milk for 30 min. The membrane was then transferred to a 1:3,000 solution of SOD primary antibody in TTBS for 30 min, and this was followed by three washes with TTBS. The membrane was then soaked in a 1:10,000 dilution of alkaline phosphatase-labeled secondary anti-rabbit antibody (Novagen, Madison, Wis.) in AP buffer (10 mM Tris HCl [pH 9.5], 100 mM NaCl, 5 mM MgCl2) for 30 min. The membrane was then washed three times in TTBS and once in AP buffer. The blot was developed by mixing 66 µl of an immunopure 5-bromo-4-chloro-3-indolylphosphate p-toluidine salt (BCIP) (Pierce) solution (50 mg/ml in 100% dimethylformamide [Fisher Scientific, Pittsburgh, Pa.]) and 34 µl of a p-nitroblue tetrazolium chloride (U.S. Biochemicals, Cleveland, Ohio) stock solution (50 mg/ml in 70% dimethylformamide) with 10 ml of AP buffer. When bands appeared, the blot was removed from the solution and dried on filter paper.
Mass spectrometry. Mass spectrometry data were collected with a 10 µM sample of recombinant SOD cleaved from MBP in 20 mM Tris (pH 8.0). The instrument used was a DE STR mass spectrometer from Applied Biosystems. Mass spectra were acquired in the linear, positive-ion mode by using delayed extraction. Protein samples were mixed with an equal volume of a saturated solution of sinapinic acid dissolved in a mixture of 1% trifluoroacetic acid in water and acetonitrile (2:1), and 1 µl of the mixture was dried on a stainless steel sample plate. The spectrum was the average of 100 laser shots.
Subunit determination. The molecular weight of native SOD was determined by gel filtration on a Sepharose 100 high-resolution column (1.5 by 100 cm). The column was equilibrated with 20 mM Tris-150 mM NaCl (pH 8.0). The column was calibrated with a molecular mass marker kit (12 to 200 kDa; Sigma) containing blue dextran (2,000 kDa), alcohol dehydrogenase (150 kDa), albumin (66 kDa), carbonic anhydrase (29 kDa), and cytochrome c (12.4 kDa). FeSOD from E. coli (37 kDa; Sigma) was also used as a column standard.
Phylogenetic analysis. SOD sequences of various bacteria were obtained from the National Center for Biotechnology Information website. Only sequences of SODs whose metal contents have been experimentally characterized were used. Protein sequences were aligned with the program Clustal W. A phylogenetic tree was inferred by using Mega (version 2) and the neighbor-joining tree method with 500 bootstrap replicates (16).
Metal analysis.
Metal analysis and quantification were performed by using a Varian SpectrAA-400 Zeeman graphite furnace atomic absorption spectrometer. Iron and manganese standard solutions were obtained from VHG Labs, Manchester, N.H. A manganese standard curve was obtained by using 0.1% nitric acid in 18-M
water and Mn3+ concentrations of 0.5, 5.0, 10, 12.5, and 15 µg/liter. Similarly, an iron standard curve was obtained by using 0.1% nitric acid and Fe2+ concentrations of 1, 5, 10, 20, and 25 µg/liter. The absorbance of manganese and the absorbance of iron were measured at 297.5 and 248.3 nm, respectively. SOD samples were diluted in nanopure water with 0.1% nitric acid until the absorbance fell in the range on the standard curves. Protein concentrations of SOD samples were determined by using a Coomassie Plus protein assay reagent kit (Pierce).
Purified catalytically active MBP-SOD fusion protein was used in metal analysis and electron paramagnetic resonance (EPR) assays. The fusion protein was in 20 mM Tris (pH 8.0). The fusion protein was also concentrated with a Centricon-3 concentrator (Amicon, Beverly, Mass.), and its flowthrough was used as a control for both the atomic absorption and EPR analyses. MBP cleaved from SOD and purified during the IEF step was also used as a control in the atomic absorption measurements.
EPR spectroscopy. EPR measurements were obtained at about 8 K by using a Bruker EPR E580 ELEXSYS spectrometer with an Oxford Instruments ESR900 liquid helium flow cryostat (Bruker, Billerica, Mass.). The instrument conditions were as follows: microwave frequency, 9.42 GHz; magnetic field modulation frequency, 100 kHz; modulation amplitude, 15 G; sweep range, 2,250 ± 2,000 G; sweep time, 336 s; time constant, 0.082 s; microwave power, 5.0 mW; and horizontal resolution, 2,048 points. Each spectrum was the average of four scans.
Spectrophotometrry-based activity assays. The specific activities of SOD samples were determined by the xanthine-xanthine oxidase-based method as previously described (11). All reagents were purchased from Sigma. Samples were thoroughly dialyzed in 20 mM Tris (pH 8.0) prior to the assay.
Native polyacrylamide gel-based SOD activity assays. Electrophoresis was performed by using a Bio-Rad Mini-Protean 3 cell with 25 mM Tris-0.192 M glycine-0.1% SDS (pH 8.3) as the electrode buffer. Analytical gels with 5% acrylamide stacking gels and 15% acrylamide resolving gels were used. The protein reference was the Benchmark prestained protein ladder (Invitrogen, Carlsbad, Calif.). Denatured samples were boiled for 15 min after addition of 0.1% SDS, 2-mercaptoethanol, 0.5 M Tris (pH 6.8), and 0.5% bromophenol blue. Native samples were prepared in sample buffer without 2-mercaptoethanol and were not boiled. Native gel-based activity assays were performed by the p-nitroblue tetrazolium chloride-based photochemical method (5).
Reconstitution of MBP-SOD in the presence of MnSO4 and FeSO4. MBP-SOD was denatured by dialysis into 8 M urea-10 mM EDTA-50 mM Tris (pH 8.0) for 24 h at 25°C. The sample was then dialyzed into 50 mM Tris (pH 8.0) for 24 h at 4°C, which resulted in catalytically inactive SOD apoprotein. Neutral pH was used because this protein readily precipitated when it was exposed to acidic pH. The SOD sample was then divided and placed into five different dialysis bags with molecular mass cutoffs of 6 to 8 kDa (Spectrum, Gardena, Calif.), and it was dialyzed into 8 M urea-50 mM Tris (pH 8.0) with the following metals added for 4 h at 4°C: (i) 10 mM FeSO4, (ii) 10 mM FeSO4 and 1 mM MnSO4, (iii) 10 mM FeSO4 and 10 mM MnSO4, (iv) 1 mM FeSO4 and 10 mM MnSO4, and (v) 10 mM MnSO4. Using the same concentrations of metals and Tris buffer, the urea concentration was stepped down from 8 M to 6, 4, and 2 M for 4 h each at 4°C. Then, for 4 h at 4°C, each sample was placed in 50 mM Tris (pH 8.0) with 0.5 mM EDTA, and each metal concentration was reduced 10-fold. Finally, each sample was placed in 50 mM Tris (pH 8.0) with 0.5 mM EDTA for 24 h at 4°C. The specific activity of each sample was measured by the xanthine-xanthine oxidase SOD assay as described above.
Nucleotide sequence accession number. The GenBank accession number for the complete nucleotide sequence of the SOD gene of C. aurantiacus is AY289213.
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FIG. 1. SDS-polyacrylamide gel electrophoresis and Western blotting of purified recombinant C. aurantiacus SOD. (A) The protein fraction was isolated from E. coli ER2508 expressing C. aurantiacus SOD as the MBP-SOD fusion protein. MBP-SOD was isolated by using an amylose column. Lane 1, protein ladder; lane 2, E. coli whole-cell extract with MBP-SOD; lane 3, amylose column flowthrough; lane 4, pure MBP-SOD eluted from the amylose column. (B) Pure SOD was obtained by factor Xa cleavage of MBP-SOD and was isolated by IEF. Lane 1, protein ladder; lane 2, pure recombinant SOD. (C) Western blot with anti-wtSOD antibodies. Lane 1, prestained protein ladder; lane 2, C. aurantiacus whole-cell extract; lane 3, pure recombinant SOD.
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FIG. 2. Mass spectrum of SOD and MBP cleaved by factor Xa. The SOD peak is at 23,153.01 Da, and there is a second peak at 22,963.33 Da. This second peak is most likely a secondary cleavage product produced by factor Xa. MBP is at 42,491.32 Da, with the doubly charged peak at 21,236.06 Da.
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FIG. 3. Deduced amino acid sequence of C. aurantiacus SOD. This sequence is available from GenBank under accession number AY289213. The N-terminal factor Xa cleavage site and putative secondary structure regions are indicated, and metal-coordinating residues are indicated by boldface type.
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FIG. 4. Neighbor-joining tree of experimentally characterized SODs from bacteria and archaea. The GenBank accession numbers for the protein sequences used are AAL26890, A38461, P00448, CAA44556, CAA11227, P09738, AAC64207, AAA72217, NP_341862, AAF36989, BAA00489, 1BT8_B, P17670, CAA50266, AAA91964, and NP_743076.
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EPR spectroscopy confirmed the presence of coordinated iron and some manganese in the SOD (Fig. 5A and B). Iron was the primary metal present in this SOD. The EPR-active form of iron (as determined by using standard EPR methodology) is Fe(III), and the features near 1,570 G (about g = 4.3) in Fig. 5A and B are characteristic of high spin (S = 5/2 ferric iron in a strongly rhombic environment) (24). Adventitiously bound Fe(III) can produce similar spectra. However, the fact that SOD activity was retained in the presence of diethylenetriaminepentaacetic acid (Sigma), an effective chelator of iron, along with the enzyme's ability to replace Fe(III) with Mn(III) in manganese-enriched growth media (see below), indicates that the absorption at g = 4.3 was not due solely to nonspecifically bound iron. Less intense peaks extending below 1,000 G in Fig. 5A were associated with the iron signal at g = 4.3 (24). Since Mn(III) was incorporated into the active site, it was EPR silent and therefore was not found in the spectra of the native samples (Fig. 5A and C). The characteristic hydrated Mn(II) spectrum was obtained only when Mn(III) was released from the protein active site upon acidification of the sample (Fig. 5B and D). Thus, the complex set of features in the range from 3,000 to 4,000 G was due to Mn(II). There were six lines, spaced 90 to 100 G apart, with nearly the same amplitudes. This so-called hyperfine structure arose from the magnetic interaction of the electron spin (S = 5/2) on Mn(II) and the nuclear spin (I = 5/2) of 55Mn. In the general case of nuclear spin I, 2I + 1 hyperfine lines are observed. The origin of the sharp step near 3,400 G in the spectrum in Fig. 5B is not known, but it was probably an artifact arising from a radical contaminant.
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FIG. 5. EPR spectra of MBP-SOD isolated from E. coli grown under two conditions. (A and B) Normal LB growth medium, with production of native MBP-SOD (A) and acidified MBP-SOD (B). (C and D) LB medium supplemented with 1 mM MnSO4, with production of native MBP-SOD (C) and acidified MBP-SOD (D). Iron and, to a lesser extent, manganese were present in MBP-SOD, and manganese was the only metal detected when E. coli was grown in the presence of 1 mM MnSO4.
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The specific activities of various SOD samples were measured by using the xanthine-xanthine oxidase-based SOD activity assay, as described above (Table 1). The iron- and manganese-containing MBP-SOD purified from the E. coli culture enriched with 1 mM MnSO4 was found to have an activity of 683.5 U/mg of protein. This is about threefold higher than the activity of the primarily iron-containing MBP-SOD from E. coli grown in LB broth alone. The iron-containing sample of SOD was enzymatically separated from MBP and purified by IEF and was found to have a specific activity of 421 U/mg of protein. Since there was approximately threefold less SOD present per milligram of protein in the fusion protein sample than in the purified cleaved SOD sample and since the pure cleaved SOD had been subjected to significantly more purification procedures, the presence of MBP does not seem to significantly hinder the activity of SOD.
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TABLE 1. Specific activities of SOD samplesa
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It is interesting that this enzyme also resisted thermal inactivation. The enzymatic activity of SOD reconstituted with manganese was not significantly affected by boiling for 5 min. Furthermore, addition of 2-mercaptoethanol did not affect the activity of a sample, which was probably due to the absence of any cysteine residues in the SOD.
Native gel activity assays were done to visualize the hydrogen peroxide sensitivity of the purified recombinant SOD (Fig. 6). The SOD remained active, and the activity was not significantly changed by exposure to H2O2 at concentrations up to 80 mM, which is consistent with the properties of MnSODs. E. coli MnSOD and FeSOD were included in the experiment as controls to illustrate the inactivation of FeSODs by peroxide and the natural resistance of MnSODs to peroxide (8).
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FIG. 6. Native polyacrylamide gel electrophoresis activity assays of pure recombinant SOD and the effects of H2O2 exposure. SOD samples were electrophoresed on polyacrylamide gels under native conditions. The gels were identical except for pretreatment with H2O2. Lane 1, 20 µg of E. coli MnSOD; lane 2, 25 µg of E. coli FeSOD; lane 3, 5.4 µg of recombinant C. aurantiacus SOD. (A) Buffer control; (B) pretreatment with 10 mM H2O2; (C) pretreatment with 20 mM H2O2; (D) pretreatment with 80 mM H2O2.
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A partially purified sample of wtSOD from C. aurantiacus was also analyzed by atomic absorption spectrometry to determine its metal content. This SOD sample contained twofold more manganese than iron. This is consistent with the fact that the medium used to grow laboratory cultures of C. aurantiacus contains 3.75-fold more manganese than iron (4).
Proteins of hyperthermophilic bacteria have previously been found to contain a larger portion of charged residues for the purpose of forming stabilizing ion pairs (17, 18). C. aurantiacus SOD actually contains 35% fewer charged residues than the mesophilic MnSOD from E. coli. This may indicate that C. aurantiacus, which grows at temperatures up to 62°C, does not live at high enough temperatures to require the stabilizing properties of ion pairs in its proteins.
The protein sequence of SOD from C. aurantiacus has characteristics of both FeSODs and MnSODs, as well as some unique features. The tertiary structure of each monomer in dimeric Fe/Mn-type SODs consists of two domains. The secondary structure of the first domain is
-helical, and the second domain is an
-ß fold. The four conserved residues of C. aurantiacus that ligate the metal atom are most likely His27 and His79 in the first domain and Asp165 and His169 in the second domain, based on alignment with SODs whose crystal structures are known, such as the SOD of P. shermanii (data not shown).
An analysis of the primary amino acid sequence revealed features of the C. aurantiacus SOD that are common to both FeSODs and MnSODs of bacteria. An extensive review of the primary sequences and structures of FeSODs, MnSODs, and cambialistic SODs was perfromed by Jackson and Cooper in 1998 (14), and the results will be compared to our data for C. aurantiacus SOD. There are some unusual features of the C. aurantiacus SOD in the first helix starting at His25 with the sequence H-Y-H-H-D-N-H-H. The first two residues, His25 and Tyr26, are basic and aromatic residues, respectively. Other FeSODs and MnSODs normally have an acidic Glu residue and a neutral Leu residue or similar residues at these positions. Asn30 is similar to the normally conserved Lys at this position, which has been found to be involved in guiding the O2 substrate into the active site (25). Interestingly, His32 is not typically conserved in cambialistic SODs.
The other helix in the first domain starts with Arg73, and its sequence is R-N-N-G-G-G-H-W-N-H-T-F-F-W; His82 is the second metal ligand. This sequence is more representative of MnSODs; the only exception is the Asn residue at position 74, at which there is usually an aromatic residue, such as Phe, while Asn is found in FeSODs at this position. Also, the cambialistic SODs of Bacteriodes fragilis and B. gingivalis contain Phe at position 86, whereas C. aurantiacus cambialistic SOD has the conserved Trp residue at this position.
In the second domain, the first ß-strand begins with Gly128, and its sequence is G-S-G-W-A-W-L; the G-W is typical of MnSODs, and the last Leu is conserved in FeSODs. The second ß-strand of SODs does not exhibit high homology, but this strand may begin at Leu142 and extend for about seven residues. The sequence between the second and third ß-strands is N-Q-D, which is also conservatively changed in MnSODs. The third ß-strand contains the other two metal ligands, Asp165 and His169.
A neighbor-joining tree was constructed with the SOD protein sequence from C. aurantiacus by using bacterial and archaeal SOD protein sequences. It is interesting that the archaeal clade (Methanothermobacter thermautotrophicus, Halobacterium cutirubrum, Sulfolobus solfataricus, and Acidianus ambivalens) grouped with the host-dependent pathogenic mycobacteria (P. shermanii, Mycobacterium tuberculosis, Mycobacterium fortuitum, and Nocardia asteroides). Also, the monophyletic proteobacterial group (Pseudomonas putida, Rhodobacter capsulatus, E. coli, Methylomonas sp., and Aeromonas hydrophila) is interrupted by a gram-positive bacterium (Bacillus caldotenax) and by C. aurantiacus, which is a photosynthetic green nonsulfur bacterium. This phylogenetic tree is not consistent with 16S rRNA data and may be evidence that there was horizontal gene transfer.
The SOD from the filamentous anoxygenic photosynthetic bacterium C. aurantiacus was found to be cambialistic. This was the only SOD found in the soluble protein fraction and therefore fulfills the vital need in C. aurantiacus for an efficient and flexible defense against the accumulation of the toxic superoxide anion. In future experiments we will focus on the inducibility of the SOD in C. aurantiacus under oxidative stress conditions, such as high UV radiation and high levels of hydrogen peroxide.
This work was supported by NASA GSRP grant NGT2-52284. An Applied Biosystems Voyager mass spectrometer was purchased with NSF grant CHE-0131222.
Present address: Ribomed, Phoenix, AZ 85040. ![]()
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