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Journal of Bacteriology, November 2004, p. 7653-7658, Vol. 186, No. 22
0021-9193/04/$08.00+0 DOI: 10.1128/JB.186.22.7653-7658.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
The CorA Mg2+ Transporter Does Not Transport Fe2+
Krisztina M. Papp and
Michael E. Maguire*
Department of Pharmacology, Case School of Medicine, Case Western Reserve University, Cleveland, Ohio
Received 8 June 2004/
Accepted 13 August 2004

ABSTRACT
corA encodes the constitutively expressed primary Mg
2+ uptake
system of most eubacteria and many archaea. Recently, a mutation
in
corA was reported to make
Salmonella enterica serovar Typhimurium
markedly resistant to Fe
2+-mediated toxicity. Mechanistically,
this was hypothesized to be from an ability of CorA to mediate
the influx of Fe
2+. Consequently, we directly examined Fe
2+ transport and toxicity in wild-type versus
corA cells. As determined
by direct transport assay, CorA cannot transport Fe
2+ and Fe
2+ does not potently inhibit CorA transport of
63Ni
2+. Mg
2+ can,
relatively weakly, inhibit Fe
2+ uptake, but inhibition is not
dependent on the presence of a functional
corA allele. Although
excess Fe
2+ was slightly toxic to
S. enterica serovar Typhimurium,
we were unable to elicit a significant differential sensitivity
in a wild-type versus a
corA strain. We conclude that CorA does
not transport Fe
2+ and that the relationship, if any, between
iron toxicity and
corA is indirect.

INTRODUCTION
Mg
2+ homeostasis is poorly understood (
10,
22,
28,
30-
32). Almost
nothing is known about eukaryotic Mg
2+ transport proteins, and
relatively little is known, even with respect to bacteria, about
regulation of influx and efflux systems or intracellular buffering
of Mg
2+ (
5,
11,
12,
25,
39,
41). Three structurally distinct
systems for Mg
2+ influx have been identified in bacteria: MgtAB,
CorA, and MgtE. The MgtAB class is the least abundant, present
largely in enterobacteria and some other gram-negative species.
In contrast, both the CorA and the MgtE Mg
2+ influx systems
are present across a wide spectrum of bacteria. CorA is somewhat
less abundant than MgtE in the archaea and has only distant
homologs in the eukarya (
20,
35,
36,
38). Judging on the basis
of available genomic sequence data, CorA is a primary constitutive
Mg
2+ uptake system in about half of all eubacteria and in a
substantial minority of archaea.
Salmonella enterica serovar Typhimurium carries members of two of the three classes of Mg2+ uptake systems described above, namely, a single CorA transporter and two MgtAB transporters (21, 39). MgtA is the endogenous P-type ATPase Mg2+ transporter of S. enterica serovar Typhimurium and other enterobacteria (43, 44, 48). In contrast, S. enterica serovar Typhimurium MgtB is encoded in a pathogenicity island (2) and has close homologs in only a small number of bacterial species. Both P-type ATPase systems are repressed in cells grown in normal laboratory medium but are induced markedly in cells exposed to low extracellular Mg2+ concentrations (29, 43, 47). This induction is mediated by the PhoPQ two-component regulatory system (11, 45, 50). In contrast, the CorA Mg2+ transporter appears to be constitutively expressed (4, 43, 47). CorA is a novel transport protein in that it lacks homology to any other known transporter. It mediates Mg2+ influx with a K0.5 (ion concentration for half-maximal influx) of 10 µM. CorA also mediates influx of Ni2+ and Co2+ with K0.5 values of 200 and 20 µM, respectively. Transport is not significantly inhibited by Ca2+, Mn2+, or Zn2+ (13, 35, 41) but can be potently and selectively inhibited by several cation hexaammines that mimic the fully hydrated Mg2+ cation (23).
Previous studies by Hantke and by Chamnongpol and Groisman implicated CorA in iron transport and thus in iron toxicity. Hantke reported that addition of extracellular Fe2+ to S. enterica serovar Typhimurium and Escherichia coli cultures resulted in a rapid onset of toxicity and cell death (15). Mutation of corA was reported to make the cells markedly resistant to this Fe2+-mediated toxicity. This phenotype was hypothesized to be from an ability of CorA to mediate the influx of Fe2+. Hantke also reported that a corA strain accumulated less 55Fe2+ than the wild type. Chamnongpol and Groisman (4) subsequently reported that a mutation in phoP also rendered S. enterica serovar Typhimurium extremely sensitive to Fe2+-mediated toxicity. A corA phoP double mutant was relatively resistant to Fe2+ toxicity. In contrast to Hantke's results, however, Chamnongpol and Groisman reported little or no difference in sensitivity to Fe2+ between wild-type and corA S. enterica serovar Typhimurium strains. In accord with Hantke's hypothesis, Chamnongpol and Groisman (4) also explained Fe2+-dependent phenotypes by suggesting that CorA mediates Fe2+ influx. However, neither group demonstrated directly that Fe2+ could interact with the CorA transport system. We report here that a corA strain does not exhibit alterations in Fe2+ availability or toxicity from CorA-mediated Fe2+ uptake, since, according to a direct transport assay, CorA cannot transport Fe2+.

MATERIALS AND METHODS
Bacterial strains, plasmids, and growth conditions.
Bacterial strains and plasmids used or constructed in this study
are listed in Table
1. Unless indicated otherwise, all bacterial
strains are derived from
S. enterica serovar Typhimurium SL1344.
The molecular biology methods used were those of Sambrook et
al. (
33). The high-frequency generalized transducing bacteriophage
P22 mutant HT 105/1,
int-201 was used for all transductional
crosses, and phage-free, phage-sensitive transductants were
purified as described previously (
27). The
corA mutant was constructed
by P22 transduction of a
corA::Tn
10 insertion cassette from
MM385 into MM2089 as a recipient, generating MM2242. The insertional
mutation of
corA in the SL1344 background was further confirmed
by a Co
2+ resistance assay (
17), Western blot analysis, and
PCR. To create a
corA feoB strain, the
feoB gene of MM2089 was
deleted using the technique of Datsenko and Wanner (
7) to give
MM2985. The deletion was confirmed by PCR. The
corA::Tn
10 insertion
allele was subsequently introduced by P22 transduction, giving
MM2986. Bacteria were routinely grown in Luria-Bertani (LB)
broth at 37°C with shaking and with antibiotic supplementation
when required as described previously (
16,
46).
Iron toxicity assays.
The liquid iron killing assays were adapted from the methods
of Chamnongpol and Groisman (
4) and Hantke (
15), and two different
protocols were used that were based on the adaptation. For protocol
1, strains were grown overnight at 37°C with shaking in
2 ml of N-minimal medium [13.14 g of Tris HCl, 0.196 g of Tris
Base, 0.136 g of KH
2PO
4, 0.372 g of KCl, 1.0 g of (NH
4)
2SO
4,
1.0 liters of double-distilled water] supplemented with 100
mM MgCl
2-0.1% Casamino Acids-0.4% glucose (pH 7.0). Overnight
cultures were washed twice in 1 ml of N-minimal medium containing
10 µM MgCl
2 (pH 7.0), resuspended in 200 µl of the
same medium, and used to inoculate 10 ml of N-minimal medium
with 10 µM MgCl
2-0.1% Casamino Acids-0.4% glucose (pH
5.8 or 7.0) in 125-ml flasks. Cells were incubated at 37°C
with shaking for 6 to 7 h. For toxicity assays, a 0.1 optical
density (OD) unit of cells was removed and washed three times
in 1 ml of N-minimal medium containing 10 µM MgCl
2 (pH
5.8 or pH 7.0). Cells were resuspended in 1 ml of N-minimal
medium with 10 µM MgCl
2 (pH 5.8 or 7.0). The OD at 600
nm (OD
600) was read, and cells were adjusted to the same OD
and diluted, initially at 1:100 and then twice at 1:1,000. A
total of 100 µl of each diluted cell sample was mixed
with 100 µl of 0, 10, 100, 250, or 500 µM FeCl
2 (freshly dissolved in N-minimal medium containing 10 µM
MgCl
2 [pH 5.8] preincubated at 37°C) and incubated at 37°C
with shaking for 15 min. Cells were immediately plated on N-minimal
plates containing histidine (strain SL1344 is a histidine auxotroph)
and 0.4% glucose or on LB and incubated overnight at 37°C,
and colonies were counted. All experiments were performed in
duplicate. In addition to the experiments described, other experiments
were conducted in medium lacking carbon and nitrogen sources
and in liquid medium containing 1 mM sodium ascorbate (data
not shown). In all cases, although Fe
2+ clearly killed cells,
no differences were seen between wild-type and
corA cells (data
not shown).
For protocol 2, strains were grown overnight at 37°C with shaking in tryptone yeast extract (TY) medium (8.0 g of tryptone, 5.0 g of yeast extract, and 5.0 g of NaCl per liter). Overnight cultures were centrifuged, and the cell pellets were resuspended in a HEPES-salts buffer (30.0 g of HEPES, 4.65 g of NaCl, 1.5 g of KCl, 1.0 g of NH4Cl, and 0.425 g of Na2SO4 per liter at pH 7.2) supplemented with 0.2% glucose and 10 µM MgSO4. Then
109 cells were incubated with 30 µM FeSO4 for 0, 5, 20, 40, and 60 min. At each time point, cells were diluted and plated on TY plates and incubated overnight at 37°C, and colonies were counted. All assays were conducted in the presence of 1 mM sodium ascorbate and in duplicate. For plate iron killing assays, a lawn of cells was plated on LB plates. A 6-mm-diameter filter paper disk in the center of the dish received 15 µl of freshly made 1 mM FeCl2 with 1 mM sodium ascorbate. After overnight incubation, the diameter of the ring around the disk devoid of cells was evaluated (data not shown).
Transport assays.
The uptake of 63Ni2+ (NEN, Boston, Mass.) was assayed instead of Mg2+ uptake, as 28Mg2+ is prohibitively expensive and not readily available. Methods for transport have been described in detail previously (13, 40, 42). Briefly, cells were grown aerobically overnight in LB with appropriate antibiotics, washed twice in cold cell wash buffer (N-minimal medium with 0.4% glucose and 0.2% Casamino Acids at either pH 5.8 or 7.0), resuspended to an OD600 between 1.0 and 2.0, and placed on ice. Cells were added to tubes containing various concentrations of inhibitor cation plus 200 µM NiCl2 and 0.3 to 1 µCi 63Ni2+ in a final volume of 1 ml. The reaction mixtures were incubated for 15 min at 37°C, stopped by the addition of 5 ml of ice-cold N-minimal medium containing 10 mM MgSO4 and 0.5 mM EDTA, filtered immediately on nitrocellulose filters (Schleicher & Schuell, Keene, N.H.) and washed once with 5 ml of the same solution. The filters were placed in 3 ml of Biosafe II scintillation cocktail (Research Products International Corp, Mount Prospect, Ill.), and radioactivity was measured by scintillation counting.
All solutions containing iron were made fresh immediately before use. Fe2+ solutions always contained 1 mM ascorbate unless noted, and 55Fe2+ transport assays were always conducted in solutions containing 1 mM freshly made sodium ascorbate. The final Fe2+ concentration was 1 µM when 55Fe2+ transport was measured, but the transport assay was otherwise similar to that for 63Ni2+ transport assays. When Fe3+ was tested, ascorbate was not used to make stock solutions and no ascorbate was added to the incubation or wash buffers. In all cases, the concentration of sodium ascorbate used was chosen based on methods previously described; most likely some sodium ascorbate was consumed during the experiment. However, throughout the duration of all experiments up to 12 h postexperiment, oxidation of ferrous iron or precipitation of ferric iron in stock solutions was not observed.
While our transport assays were very similar to those used by Hantke (15), there were some differences. Hantke analyzed S. enterica serovar Typhimurium LT2, whereas we studied S. enterica serovar Typhimurium SL1344 and 14028s. However, CorA-mediated transport was initially characterized by this laboratory using S. enterica serovar Typhimurium LT2 as a strain background (13, 16, 17). corA expression and CorA-mediated transport results appear to be identical for the LT2, 14028s and SL1344 strain backgrounds. corA is a single gene locus, and both the promoter and coding sequences are identical for the different S. enterica serovar Typhimurium strains. In addition, Hantke grew cells overnight in TY medium and resuspended in a medium buffered with HEPES and containing NaCl, KCl, NH4Cl, and Na2SO4 and no added magnesium. In our hands and with our methods, cells can be grown overnight in LB or N-minimal medium with or without various monovalent cations and resuspended in several buffers containing any monovalent cation without altering transport properties (13). Thus, these minor differences should not alter interpretation of the transport data.

RESULTS
Effect of mutation of corA on survival after exposure to iron.
During encounter with host cells,
S. enterica serovar Typhimurium
encounters significant stress due to exposure to increased reactive
oxygen and nitrogen species (
9,
18). In addition, stress due
to iron limitation is well known to affect virulence. A reported
phenotype of a
corA strain is its lack of sensitivity to Fe
2+ toxicity (
15). Therefore, the survival rates of wild-type (strains
SL1344, LT2, and 14028s) and
corA and
phoP strains were determined
by challenge with different concentrations of Fe
2+ in liquid
medium and protocols adapted both from Hantke and from Chamnongpol
and Groisman (Fig.
1 and Table
2). A marked increase in Fe
2+ sensitivity in three different
phoP strains, as had been reported
by Chamnongpol and Groisman (
4), was observed; however, altered
sensitivity to iron as a function of
corA allele status, as
reported by Hantke (
15), could not be demonstrated (Fig.
1 and
Table
2). Only a slight effect of a 20 to 30% difference in
survival could be observed for wild-type compared to
corA cells.
A similar lack of effect of a
corA mutation on iron sensitivity
was also noted by Chamnongpol and Groisman (
4). Iron toxicity
was independent of
S. enterica serovar Typhimurium strain background,
whether LT2, SL1344, or 14028s (Table
2). Similar results were
also obtained from plate diffusion assays used to detect iron
toxicity (data not shown). Reported changes in Fe
2+ sensitivity
were attributed to an ability of the CorA transporter to mediate
influx of Fe
2+. However, these interpretations were inferred
from indirect assays rather than from direct demonstration of
Fe
2+ interaction with CorA. We therefore examined the effect
of expression of CorA on Fe
2+ accumulation.
CorA and iron accumulation.
The only characterized primary Fe
2+ uptake system in
S. enterica serovar Typhimurium,
E. coli, and
Helicobacter pylori is FeoB
(
14,
19,
49). Although other transport systems such as MntH
and SitABCD transport Fe
2+ when it is present at very high concentrations,
Fe
2+ is not their primary substrate cation. We therefore measured
the ability of wild-type,
corA,
feoB, and
corA feoB strains
to accumulate iron.
If CorA provided any significant amount of Fe2+ uptake, its mutation should have diminished total Fe2+ accumulation after growth on typical laboratory medium. While iron uptake results differed between experiments, the average amount (n = 11) of 55Fe2+ accumulation did not differ significantly between a wild-type versus a corA strain or between a wild-type and an feoB strain (Fig. 2). While Hantke observed no difference in Fe2+ uptake between wild-type and feoB strains, he did report a difference between wild-type and corA strains. We suggest that this difference in results can be attributed to the very high variability in iron accumulation from experiment to experiment, as indicated by the error bars in Fig. 2. We examined several parameters to reduce variability in an attempt to determine whether there was a real difference in iron accumulation, including type of buffer, presence or absence of Mg2+, iron concentration, use of EDTA in wash buffers, and time of incubation, but could never detect consistent differences or markedly reduce variability, most likely because iron binds tightly to many biological molecules and cannot be readily removed without more severe (and likely deleterious) means. Similar issues arise in measurement of 45Ca2+ uptake, as we have previously noted (13). Regardless, under the growth and assay conditions used, the presence or absence of CorA had no effect on Fe2+ accumulation, an indication that CorA cannot mediate the uptake of iron. Interestingly, by an unknown mechanism, the corA feoB strain accumulated more Fe2+ than the wild type or the single mutants (Fig. 2).
Effect of iron on CorA-mediated transport.
We next determined the ability of Fe
2+ and Fe
3+ to interact
with CorA. If CorA is capable of transporting iron, then iron
must inhibit the uptake of other CorA substrates.
63Ni
2+ has
been used as a surrogate due to the high cost and poor availability
of
28Mg
2+ (
13,
17,
41). The apparent
K0.5 of Mg
2+ for CorA is
10 to 20 µM, while that of Ni
2+ is 200 µM. If the
total [
63Ni
2+] in the assay solution is equal to the
K0.5, then
the concentration of a cation required to inhibit 50% of control
63Ni
2+ uptake (IC
50) is exactly double the true
Ki for that
cation by simple Mass Action Law consideration. The ability
of Mg
2+ with and without 1 mM ascorbate, Fe
2+ with 1 mM ascorbate,
and Fe
3+ to inhibit
63Ni
2+ uptake was measured for MM2089, a
wild-type SL1344
S. enterica serovar Typhimurium strain. Although
this strain carries functional
mgtA and
mgtCB alleles in addition
to
corA,
corA is constitutively expressed, and cells for assay
were grown overnight in LB, which contains sufficient Mg
2+ to
completely repress transcription of
mgtA and
mgtCB (
37,
47).
Neither Fe2+ nor Fe3+ could inhibit 63Ni2+ uptake via CorA at pH 7.0. At concentrations up to 20 µM Fe3+ (data not shown) or 100 µM Fe2+ (Fig. 3), neither iron species had any effect on 63Ni2+ uptake. At the assay pH of 7.0, higher concentrations of Fe2+ and Fe3+ precipitated during filtering; they did not precipitate in stock solutions (Fig. 3). Thus, it could not be determined whether very high concentrations of iron could inhibit CorA at pH 7.0. Nonetheless, biological systems are highly unlikely to have free iron concentrations of this magnitude; therefore, for practical purposes, iron is not an effective inhibitor of the CorA Mg2+ transporter. We also performed the same experiment at pH 5.8, since S. enterica serovar Typhimurium can encounter acid conditions in some growth situations. Acid pH increases the apparent Vmax of CorA about twofold (40, 46) and slightly decreases the K0.5 for Ni2+ to about 100 µM. Again, neither Fe2+ nor Fe3+ had any effect on uptake via CorA at concentrations of up to 300 µM Fe2+ (Fig. 3) or Fe3+ (data not shown). Since we have previously shown that S. enterica serovar Typhimurium LT2, 14028s, and SL1344 strains have identical CorA transport properties and since coding and promoter sequences are identical for all three strains, these results are strain independent.
Effect of Mg2+, Co(III)hexaammine, and CorA on 55Fe2+ uptake.
Mg
2+ inhibited uptake of
55Fe
2+ (1 µM) in wild-type cells
with a
K0.5 of 50 to 100 µM, a result severalfold higher
than the
K0.5 of Mg
2+ for CorA. However, Mg
2+ inhibition of
55Fe
2+ uptake was identical in a
corA strain (Fig.
4), an indication
that the ability of Mg
2+ to inhibit
55Fe
2+ uptake was not due
to interaction with the CorA transporter. The ability of Mg
2+ to inhibit
55Fe
2+ uptake presumably reflects a low-affinity
interaction of Mg
2+ with one or more iron transporters. Finally,
Co(III)hexaammine is a selective inhibitor of CorA, with a
Ki of 1 µM. However, its half-maximal inhibitory concentration
for
55Fe
2+ uptake was around 1 mM, about 3 logs higher than
its
Ki for CorA (Fig.
4). These data clearly indicate that binding
of these compounds to CorA is not involved in any effect they
may have on Fe
2+ toxicity.

DISCUSSION
Chemistry of Fe2+ and Mg2+.
A cation that is a substrate for a transport system must in
turn inhibit the transport of any other substrate cation. However,
from the viewpoint of the respective chemical properties of
Fe
2+ and Mg
2+, it is highly unlikely that Fe
2+ would be transported
by a system capable of selectively interacting with and transporting
Mg
2+. Mg
2+ has a far larger hydration shell than does Fe
2+.
Mg
2+ is a very hard Lewis acid, whereas Fe
2+ is an intermediate-to-soft
Lewis acid. While Mg
2+ readily interacts with carboxylate and
phosphate anions in solution or on proteins (
1,
26), its transport
by CorA (
40,
46) or by MgtB (D.G. Kehres and M. E. Maguire,
unpublished observations) does not require electrostatic interactions,
in apparent contrast to transport of iron (
3,
24,
34,
52). Mg
2+ is invariably hexacoordinate, with resulting Mg
2+-ligand bond
angles of 90 ± 5° in the octahedron (
6). In contrast,
Fe
2+ can be tetra- or hexacoordinate, with far more flexibility
in bond angles (
6). Iron prefers in many cases to bind to sulfur-containing
ligands, whereas Mg
2+ binds almost exclusively to oxygen-containing
ligands (
6,
26). Finally, although Mg
2+ does not possess
d orbital
electrons, the other two known substrates of CorA, Co
2+ and
Ni
2+, are high-spin
d7 and
d8 coordinate ligands whereas Fe
2+ is usually a low spin
d6 ligand in biological complexes (
6,
8,
26). Overall, this combination of properties makes Fe
2+ a
very unlikely substrate for CorA. We note, however, that this
does not preclude simple inhibition of transport by a nonsubstrate
cation, since an inhibitory cation need only interact with a
part of the transport protein.
Our results differ from those of Hantke (15), who reported that mutation of corA made E. coli and S. enterica serovar Typhimurium relatively resistant to Fe2+-mediated killing. Neither we (this report) nor Chamnongpol and Groisman (4) observed any difference in Fe2+ toxicity between a wild-type and a corA strain of S. enterica serovar Typhimurium. We have no explanation for this discrepancy. We (this report) and previously Chamnongpol and Groisman (4) also observed a difference in iron toxicity between phoP and wild-type strains. (Those authors also reported that introduction of a corA mutation into a phoP strain restored wild-type Fe2+ resistance, a phenotype we did not investigate.) However, an interpretation from such experiments that corA cells were transporting iron because they were resistant to iron toxicity is premature without direct transport assays. Furthermore, our data do not show that a corA strain accumulates less iron than a wild-type strain, again differing from Hantke's results. We attribute this latter difference to the highly variable nature of iron transport (see error bars in Fig. 2). During preliminary experiments, transport assay conditions were adjusted considerably in an effort to minimize such variability with 55Fe2+, with incomplete success. Subsequently, of 11 independent experiments in which we evaluated 55Fe2+ uptake, a corA strain accumulated slightly more iron than wild-type in 5 experiments, slightly less iron in 4 experiments, and an approximately equivalent amount in 2 experiments. Thus, it would be possible to observe a decrease (or an increase) in iron uptake in a corA strain if only a few experiments were performed. These results are in contrast to those comparing wild-type or corA strains with a corA feoB strain, for which 10 or 11 experiments showed a marked increase in iron uptake in the corA feoB strain compared to the results seen with the others.
Regardless of these accumulation experiments, the K0.5 of Mg2+ inhibition of 55Fe2+ uptake is severalfold greater than would be expected if Mg2+ were interacting with CorA, the dose response curve for Mg2+ inhibition of 55Fe2+ uptake is independent of the presence of the CorA transporter, and the ability of the CorA-selective inhibitor Co(III)hexaammine to inhibit 55Fe2+ uptake does not correlate with its Ki for inhibition of CorA (Fig. 4). Thus, even with the experimental limitations noted, mutation of corA has no significant effect on 55Fe2+ uptake. These conclusions are emphasized by the demonstration, by direct transport assay, that Fe2+ does not affect CorA-mediated transport of a known substrate, 63Ni2+ (Fig. 3). One substrate of a transporter must inhibit flux of another substrate. Fe2+ does not inhibit CorA-mediated transport of 63Ni2+ even at high nonphysiological iron concentrations (Fig. 3). Thus, we conclude that CorA cannot transport Fe2+.
Despite the reasonable presumptions that CorA might be considered a "housekeeping" system and, further, that its mutation leads to no significant Mg2+-dependent growth phenotype, loss of corA gives a surprising array of phenotypes. These include altered transcription of PhoPQ-regulated genes, altered expression of genes encoded by Salmonella pathogenicity island I, increased sensitivity to heat shock and peroxide, and diminished virulence (J. Lin, D. G. Kehres, and M. E. Maguire, unpublished data). Thus, while it is possible that loss of corA may be a cause of one or more phenotypes related to iron (4, 15), the association is indirect and does not arise from an ability of CorA to transport iron.

ACKNOWLEDGMENTS
This work was supported by National Institutes of Health grant
GM39447 to M.E.M. K.P. was supported by National Institutes
of Health training grant T32 GM08803.
We thank E.A. Groisman and M. Mahan for strains.

FOOTNOTES
* Corresponding author. Mailing address: Department of Pharmacology, School of Medicine, Case Western Reserve University, 10900 Euclid Ave., Cleveland, OH 44106-4965. Phone: (216) 368-6186. Fax: (216) 368-3395. E-mail:
mem6{at}po.cwru.edu.


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Journal of Bacteriology, November 2004, p. 7653-7658, Vol. 186, No. 22
0021-9193/04/$08.00+0 DOI: 10.1128/JB.186.22.7653-7658.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
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