Applied and Environmental Microbiology, May 2005, p. 2331-2337, Vol. 71, No. 5
0099-2240/05/$08.00+0 doi:10.1128/AEM.71.5.2331-2337.2005
Copyright © 2005, American Society for Microbiology. All Rights Reserved.
Chemical Forms of Selenium in the Metal-Resistant Bacterium Ralstonia metallidurans CH34 Exposed to Selenite and Selenate
Géraldine Sarret,1*
Laure Avoscan,2
Marie Carrière,2
Richard Collins,2
Nicolas Geoffroy,1
Francine Carrot,2
Jacques Covès,3 and
Barbara Gouget2
Environmental
Geochemistry Group, LGIT, University of Grenoble and CNRS, BP 53, 38041
Grenoble, Cedex 9, France,1
Laboratoire Pierre Süe,
CEA-CNRS UMR 9956, CEA/Saclay, 91191 Gif-sur-Yvette,
France,2
Institut de Biologie
StructuraleJ.-P. Ebel, Laboratoire des
Protéines Membranaires, 41 rue Jules Horowitz, 38027
Grenoble Cedex, France3
Received 7 October 2004/
Accepted 30 November 2004
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ABSTRACT
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Ralstonia
metallidurans CH34, a soil bacterium resistant to a
variety of metals, is known to reduce selenite to
intracellular granules of elemental selenium (Se0). We have
studied the kinetics of selenite (SeIV) and selenate
(SeVI) accumulation and used X-ray absorption spectroscopy
to identify the accumulated form of selenate, as well as possible
chemical intermediates during the transformation of these two
oxyanions. When introduced during the lag phase, the presence of
selenite increased the duration of this phase, as previously
observed. Selenite introduction was followed by a
period of slow uptake, during which the bacteria contained
Se0 and alkyl selenide in equivalent proportions. This
suggests that two reactions with similar kinetics take place:
an assimilatory pathway leading to alkyl selenide and a slow
detoxification pathway leading to Se0. Subsequently,
selenite uptake strongly increased (up to 340 mg Se per g of proteins)
and Se0 was the predominant transformation product,
suggesting an activation of selenite transport and reduction systems
after several hours of contact. Exposure to selenate did not induce an
increase in the lag phase duration, and the bacteria accumulated
approximately 25-fold less Se than when exposed to selenite.
SeIV was detected as a transient species in the first
12 h after selenate introduction, Se0 also
occurred as a minor species, and the major accumulated form was alkyl
selenide. Thus, in the present experimental conditions, selenate mostly
follows an assimilatory pathway and the reduction
pathway is not activated upon selenate exposure. These results show
that R. metallidurans CH34 may be suitable for the
remediation of selenite-, but not selenate-, contaminated
environments.
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INTRODUCTION
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Microorganisms play a major role in the biogeochemical cycle of selenium
in the environment (12).
Certain strains that are resistant to selenium oxyanions, and reduce
selenite (SeIV) and/or selenate (SeVI) to the
less available elemental selenium (Se0)
(7), could be potentially
used for the bioremediation of contaminated soils, sediments,
industrial effluents, and agricultural drainage
waters.
Ralstonia metallidurans CH34 is a soil bacterium
characteristic of metal-contaminated biotopes. It is resistant to a
variety of heavy metals and metalloids including CrVI,
CoII, NiII, CuII, ZnII,
AsV, CdII, HgII, and PbII.
The genes for metal resistance are located in two large plasmids
(pMOL28 and pMOL30). Their function and regulation are well understood
for some of these elements
(18). This bacterial
strain is also resistant to selenite, and detoxification is realized by
the incorporation of this oxyanion and its subsequent reduction to red
Se0, as shown by X-ray absorption spectroscopy
(24). This study also
revealed that the Se0 granules were localized mainly in the
cytoplasm. In contrast to previously cited metals and metalloids, the
genes involved in selenite resistance have not yet been identified, and
the exact mechanism of selenite bioreduction is still unknown. R.
metallidurans CH34 can also resist up to 16 mM selenate
(2). The capacity of
R. metallidurans CH34 to accumulate selenate and the fate of
this oxyanion following incorporation have never been investigated. We
have now studied the kinetics of selenite and selenate accumulation and
used X-ray absorption near-edge structure (XANES) spectroscopy to
determine Se speciation in order to identify the chemical
intermediates putatively appearing during reduction. For
such a purpose, XANES is the method of choice since it is
nondestructive and enables direct determination of the target element
speciation, i.e., its oxidation state and sometimes its exact chemical
form. The results obtained on speciation were combined with the total
metal content of each sample in order to deduce the concentration of
each metal species. Such quantitative information is particularly
useful to estimate the relative importance of several chemical pathways
in a particular
system.
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MATERIALS AND METHODS
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Bacterial strain and growth media.
R.
metallidurans CH34 provided by Max Mergeay (SCK/CEN, Mol, Belgium)
was grown aerobically at 29°C in Tris salt mineral medium with
2% gluconate as a carbon source
(18,
19).
One-contaminant (SeIV or SeVI) exposure.
A preculture was obtained by growing
the cells until mid-exponential phase (absorbance at 600 nm
[A600] of 1.5). Cells were then
appropriately diluted to inoculate 300 ml Tris salt mineral medium at
an initial A600 of 0.3. The cultures were monitored
by recording the A600 as a function of time. A
first series of experiments was run by adding selenite or selenate at a
final concentration of 2 mM at time zero (A600
= 0.3). In a second set of experiments, the selenium oxyanion
was added during the first half of the exponential phase
(A600 = 1). Finally, a third series was run
by adding the selenium oxyanion at the beginning of the stationary
phase (A600 = 3). Sodium selenite and
sodium selenate were prepared as a 1 M stock solution in ultrapure
water and sterilized by filtration. Control cultures were grown under
identical conditions in the absence of the selenium oxyanions. Anywhere
from 5 to 15 ml, depending on the turbidity of the cell suspension, was
sampled at various time intervals over 6 days and centrifuged, and the
pellets were freeze-dried and stored for further use. Cell yield was
determined by recording the A600 and assaying the
protein content (bicinchoninic acid method with bovine serum albumin as
standard).
Two-contaminant (SeIV and SeVI) exposure.
Cultures of R. metallidurans
CH34 were inoculated to an absorbance at 600 nm of 3 (stationary phase)
and exposed to two different mixtures of selenite and selenate (2 mM
selenite and 2 mM selenate or 1 mM selenite and 10 mM selenate). Three
cases were tested: (i) selenite and selenate were both added
immediately after inoculation, (ii) selenite was added immediately
after inoculation and selenate 3 h later, or (iii) selenate
was introduced immediately after inoculation and selenite 3 h
later. A control culture, under identical conditions, was grown in the
presence of selenite alone added immediately after inoculation. The
appearance of the red color, a sign of the reduction of selenite to
Se0, was checked after 24 h of
exposure.
Inductively coupled plasma-mass spectrometry (ICP-MS) analyses.
Bacteria and culture medium were
separated by centrifugation at 6,000 x g for 10 min.
Cell pellets were washed twice with ultrapure water at
4°C and resuspended in a minimum volume of ultrapure water. A
fraction of the pellet was digested in a mixture of 1 M
NaOH-20% sodium dodecyl sulfate. In order to fully
solubilize elemental selenium, H2O2 was added to
the digested sample until the characteristic red color disappeared.
These samples were used to determine total Se
accumulation.
Selenium concentrations were measured by ICP-MS
using an X7 series quadrupole instrument (Thermo Electron Corporation,
Cergy-Pontoise, France). Calibration curves were obtained by analysis
of a range of SPEX certiPrep selenium standards (Metuchen, NJ).
Selenium concentrations were determined with the isotopes 79 and 82,
and yttrium was used as an internal standard (1 µg
liter1). For digested bacteria analyses, samples
were acidified with ultrapure 65% nitric acid (Normatom quality
grade; Prolabo, Fontenay sous Bois, France) and diluted in ultrapure
water.
X-ray absorption spectroscopy.
Selenium
K-edge X-ray absorption experiments were performed on beamline FAME
(BM30B) of the European Synchrotron Radiation Facility. The Se model
compounds (all in solid state unless
otherwise noted) used for this study were as
follows: hexagonal (gray) elemental selenium, sodium
selenate (solid and in solution), sodium selenite (solid and in
solution), selenium sulfide, selenium dioxide, dimethyl selenide in
solution, selenomethionine,
S-methyl seleno L-cysteine,
seleno-DL-cystine, selenocystamine, selenodiglutathione
(RSSeSR) in solution, selenourea, and selenoguanosine.
Selenodiglutathione was prepared by mixing sodium selenite and
glutathione with a molar ratio of 1:4 in a dilute HCl solution (pH 1.3)
(10). A bacterial pellet
of R. metallidurans CH34 exposed to selenite over 10
days, and which was shown to contain monoclinic (red)
Se0
(24), was used
as a reference for this compound. The
other compounds were purchased from Sigma-Aldrich.
Freeze-dried bacteria were ground in an agate mortar and
diluted with glucose when necessary. The mixture was pressed into
5-mm-diameter pellets prior to determining XANES
measurements.
The spectra were recorded at room temperature in
fluorescence mode, using a 30-element solid-state Ge detector
(Canberra), for the most diluted bacterial samples and in transmission
mode, using a diode, for the more concentrated samples. The
monochromator was a Si(220) double crystal. Two to four scans of 10 min
were summed, depending on Se concentration. The position of the beam on
the pellet was changed between each scan in order to limit radiation
damage. Hexagonal Se (0) was recorded simultaneously, and the spectra
were energy calibrated by setting the energy of the maximum of the
white line for this reference spectrum at 12.6592 keV. XANES spectra
were normalized using polynomial functions of degrees 1 and 3 for the
pre-and postedge parts, respectively. Each set of spectra for a given
kinetics experiment was treated by using principal component analysis
(PCA) (17,
30). This approach allows
the determination of the number of Se species present in a set of
samples and to identify these species, using a library of reference
spectra. The number of principal components was determined based on the
eigenvalue of each component and on the quality of the reconstructed
spectra by using one, two, three, or more components with the total
normalized sum-squares residual (total
NSS):
 | (1) |
where
µexp. is the experimental normalized
absorbance and µrec. is the reconstructed
normalized absorbance. The principal components were identified by
target transformation using the NSS criterion as
follows:
 | (2) |
The
percentage of each species, in molar fraction of Se, was then
determined by linear combination fitting of each spectrum with the
spectra of the identified reference materials. The precision was
estimated at ±5% of total Se. The percentages were then
multiplied by total Se content, as determined by ICP-MS, in order to
obtain the concentrations of each species (mg of Se per g of
proteins).
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RESULTS
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The sensitivity of Se
K-edge XANES spectroscopy for probing the oxidation state of Se is well
established (20,
21). Figure
1 displays some of the reference spectra used in this study. The main
peak of SeIV and SeVI is shifted by +4.5
eV and +7.5 eV, respectively, relative to that of
Se0. The energy shift is much smaller for organoselenium
compounds (+0.4 to +1.5 eV relative to that of
Se0, depending on the type of compound). The position of the
main peak is identical for compounds with similar Se environments, for
instance, S-methyl selenocysteine and selenomethionine for
alkyl selenide (RSeR), seleno-DL-cystine and selenocystamine
for alkyl diselenide (RSeSeR), and selenourea and selenoguanosine for
the Se-C double bond (not shown). The energy shift between two types of
Se local structures, for instance, RSeSeR and RSSeSR, can be as small
as 0.5 eV. The sensitivity of XANES is probably not sufficient to
determine the distribution of several types of organic Se in a complex
mixture, but it certainly enables the identification of the major
organoselenium species.

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FIG. 1. XANES
spectra for some reference compounds (in solid state unless otherwise
specified). From top to bottom: sodium selenate, sodium selenite,
selenourea, S-methyl seleno L-cysteine,
seleno-DL-cystine, selenodiglutathione (in solution), red
and gray elemental selenium. The position of the maximum of the white
line is indicated in
parentheses.
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Selenite exposure.
In the
first experiment, a culture of R.
metallidurans CH34 was exposed to 2 mM selenite added at the
beginning of growth (A600 = 0.3). As
described previously
(24), the presence of
selenite induced an increase in the lag phase duration (approximately
48 h compared to 10 h in the absence of selenite).
The accumulation of selenite was minimal during this phase (<40
mg Se per g of protein). However, at the end of the exponential phase,
and during the stationary phase, selenium was strongly accumulated: at
t = 144 h, Se accounted for one-third of the
protein weight (Fig.
2).

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FIG. 2. Concentration
of Se species in R. metallidurans CH34 exposed to selenite as
determined by XANES linear combination fitting and ICP-MS analyses and
time course of growth for the bacteria exposed to selenite (open
circles). Error bars correspond to ±5% of total
Se.
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Selected XANES spectra for the bacteria at various exposure times
are shown in Fig.
3. The position of the main peak for t = 0 h at
12.6637 keV and the presence of a shoulder on the left-hand part of the
peak suggested that the bacteria contain selenite and a minor
proportion of organoselenium. At higher exposure times (t
= 1 h to 48 h), the spectra were identical
and the maximum of the main peak was intermediate between RSeR and
Se0 (12.6599 keV). The main peak was then slightly shifted
to the left at t = 96 h (12.6596 keV) and
matched the position of Se0 at t = 120 and
144 h (12.6592 keV). PCA showed that this set of spectra
could be described by three components (eigenvalues of 80.0, 4.1, and
1.1). As expected, selenite and red Se0 were positively
identified as principal components (NSS values of 4.7
103 and 2.9 104, respectively).
Several organoselenium species including RSeR, RSeSeR, and RSSeSR were
also correctly reconstructed (NSS values of 1.2 104
to 4.3 104). Among these five compounds retained,
the most likely triplet of primary components should provide the best
simulation of the whole set of bacterial spectra by linear combinations
of these three spectra. Thus, all possible triplets were tested and
selenite, red Se0, and RSeR provided the best results. Fits
using RSeSeR, or RSSeSR instead of RSeR, were poorer, as shown by
increases of the residual by 27%, 34%, and 47%,
respectively. The fact that these species were correctly reconstructed
by PCA is due to their intermediate position betweeen Se0
and RSeR (Fig. 1). The
occurrence of selenocysteine (RSeH) was not tested since this compound
reoxidized to selenocystine during the experiment. However, preliminary
results obtained by high-performance liquid chromatography support the
predominance of the RSeR form (L. Avoscan, R. Collins, G. Sarret, M.
Carrière, J. Covès, and B. Gouget, Abstr. 227th ACS Natl.
Meet., abstr. 016, p. U1107, 2004). In conclusion, alkyl
selenide is believed to be the dominant organic form of Se in the
bacteria exposed to selenite.

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FIG. 3. Selected
Se K-edge XANES spectra for R. metallidurans CH34 at various
incubation times after introduction of selenite into the culture medium
at A600s (optical densities [O.D.]) of
0.3, 1, and 3 and the distribution of Se species determined by linear
combination
fitting.
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Figure
2 shows the evolution in
the concentration of Se species in the bacteria during growth.
Immediately after the introduction of selenite, Se was distributed as
60% SeIV and 40% RSeR in the bacteria. This
latter species is likely to be a reaction product of selenite rather
than constitutive selenium contained in amino acids and/or
proteins since control bacteria, not exposed to selenite, did not yield
a detectable Se XANES signal. Subsequently, until the end of the lag
phase (t = 1 h to
48 h), a mixture of RSeR and Se0 in equivalent
proportions was observed. The concentration of RSeR was almost stable
from 48 to 96 h (18 and 15 mg Se g1 of
proteins, respectively), whereas the Se0 concentration
strongly increased (20 and 140 mg Se g1 of
proteins, respectively). At 120 and 144 h, Se0 was
the only species detected. The amount of organoselenium species
identified at 96 h might still be present in these two
samples but was masked by the dominant Se0 form (estimated
error of ±5% of total Se, i.e., 13 mg
g1 at 120 h and 17 mg
g1 at 144 h).
In parallel
experiments, selenite was added at approximately mid-exponential phase
(A600 = 1) and at the beginning of the
stationary phase (A600 = 3). Similar
evolutions of Se accumulation and speciation were observed: Se uptake
was limited for several hours and then increased. RSeR and
Se0 were observed during the slow uptake period, followed by
Se0 only (Fig.
3). However, the
production of Se0 was faster at higher
A600 values. For instance, after 48-h exposure, the
bacteria contained 99.4 mg g1 Se0
compared to 19.8 mg g1 Se0 when selenite
was added at A600s of 1 and 0.3,
respectively.
Selenate exposure.
In this experiment, the bacteria were
exposed to 2 mM selenate at the beginning of the growth
(A600 = 0.3) (Fig.
4). The highest accumulation also occurred during the exponential phase,
but this oxyanion was much less accumulated than selenite (the maximum
concentration is 14 compared to 340 mg of Se g1 of
proteins for selenite). In contrast with the selenite experiment, the
presence of selenate did not increase the lag phase duration. During
the exponential phase, bacteria in selenate-complemented media grew at
rates comparable to those of bacteria grown in selenite-free media and
maximal densities were very similar whether or not selenate was present
in the culture medium (Fig.
4). The experiment was
stopped after 72 h since the bacterial population started to
decrease, probably due to the depletion of nutrients in the medium (the
same decrease was observed for the control culture). This was indicated
by the decrease in absorbance and verified by the numeration of cells
forming colonies on Luria broth agar (data not shown).

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FIG. 4. Concentration
of Se species in R. metallidurans CH34 exposed to selenate as
determined by XANES linear combination fitting and ICP-MS analyses and
time course of growth for the bacteria exposed to selenate (open
circles) and for the control culture in the absence of added selenium
oxyanion (filled circles). Error bars correspond to ±5%
of total
Se.
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XANES
spectra for the bacteria at various selenate exposure times are shown
in Fig.
5. The PCA of this set of spectra showed that three Se species were
present (eigenvalues of 73, 4.9, and 1.9): SeVI,
SeIV, and organoselenium (NSS values of 3.7
103, 3.3 103, and 2.7
104 to 6.6 104, respectively).
Se0 could not be considered a principal component (NSS value
of 1.2 102). Using the same procedure as for the
selenite experiment, we found that RSeR was the most likely
organoselenium species. SeVI was detected in the bacterial
pellets immediately after its introduction to the culture medium
(t = 0 h) and at t =
12 h (Fig. 5).
At t = 12 h, the bacteria contained
SeIV, SeVI, and RSeR. The simulation of the
spectrum for t = 24 h was significantly
improved by adding Se0 to the simulation (NSS value
decreased by 27%), although this species was not a principal
component of the system. The occurrence of only 8%
Se0 in one particular sample explains why it was not
detected as principal component of the system. At longer exposure
times, RSeR was the only species detected.

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FIG. 5. Selected
Se K-edge XANES spectra for R. metallidurans CH34
at various incubation times after the introduction of selenate
into the culture medium at A600s
(optical densities [O.D.]) of 0.3 and 1 and the
distribution of Se species determined by linear combination
fitting.
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In another experiment,
selenate was added at mid-exponential phase (A600
= 1). The same evolution in the speciation of selenium was
observed, although Se0 was more represented (up to
27% of total Se) (Fig.
5). The slight shift of
the main peak for the spectrum at t = 6 h
compared to at t = 168 h was indicative of
this higher Se0 content (Fig.
5).
The composition
of headspace gas was not investigated during the selenite and selenate
experiments, but the formation of volatile methylated Se species is
believed to be limited since >90% of the Se initially in
solution could be accounted for upon ICP-MS analyses of the bacterial
samples and solutions.
Two-contaminant (SeIV and SeVI) exposure.
As selenite is completely reduced to
Se0, whereas selenate is not, although some selenite is
produced, we have checked the hypothesis of the inhibition of the
selenite reduction to Se0 by selenate. The bacteria were
thus exposed to both selenite and selenate introduced at the same time
or to one of these species first with the addition of the second one
3 h later. The day after exposure, the characteristic red
color of Se0 was observed in the three experiments, both at
equivalent selenite and selenate concentrations (2 mM) and with a
10-fold excess in selenate (1 mM selenite and 10 mM selenate)
regardless of the order of introduction. Thus, the possible inhibition
of selenite reduction by selenate could be ruled
out.
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DISCUSSION
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The fast selenite uptake
following several hours of slow uptake cannot be ascribed to the high
metabolism of the cells during the exponential phase since the same
profiles were observed when this oxyanion was added during
the lag phase, during the exponential phase, or at
the beginning of the stationary phase. This behavior might suggest the
slow activation of some selenite transport system. To our knowledge, no
specific selenite transporter has been characterized in microorganisms.
In Escherichia coli, selenite can enter the cell through the
sulfate transporter, but the repression of this carrier does not
inhibit selenite uptake completely
(28). In Rhodobacter
sphaeroides, a polyol transporter is suggested as the transporting
agent of selenite into the cytoplasm
(4).
Could the
organoselenium species observed during the period of slow uptake be an
intermediate product of the formation of elemental selenium? For E.
coli, selenite reduction can follow a nonenzymatic pathway
involving glutathione, and organoselenium intermediates include RSSeSR
and glutathioselenol
(28). The fact that
RSSeSR was not detected as transient species does not necessarily imply
that this nonenzymatic reduction pathway does not exist in R.
metallidurans CH34 (the occurrence of glutathioselenol was not
tested since this compound was absent from our model compounds
library). The nonenzymatic reduction of selenite is accompanied by the
production of O2·
(14) and generates an
oxidative stress. In the case of R. metallidurans CH34, the
overexpression of an enzyme associated with oxidative stress, an
iron-containing superoxide dismutase, has been recently observed in the
presence of selenite
(23). This might support
the hypothesis that nonenzymatic reduction takes place in these
bacteria. Alternatively, the RSeR species observed after selenite
introduction might result from an assimilatory pathway. Such a pathway
is thought to exist in bacteria since Se is a composite of some
bacterial enzymes such as formate dehydrogenase
(27). The most commonly
(nonvolatile) alkyl selenide species found in microorganisms is
selenomethionine (6).
High-performance liquid chromatography analyses are under way to
determine the exact nature of the RSeR species present in R.
metallidurans CH34. To summarize, the presence of RSeR and
Se0 species in equivalent amounts during the period of slow
uptake suggests that selenite is accumulated through two competing
pathways, an assimilatory pathway and a slow detoxification pathway,
with both having similar kinetics.
During the period of fast
selenite uptake, the reduction pathway becomes predominant. These
contrasting behaviors between the period of slow and fast uptake mirror
what has been previously observed for R. sphaeroides at low
and high selenite exposure: this bacterium metabolized selenite into
approximately 60% RSeR and 40% Se0 after
exposure to 1.6 mg liter1 of selenite and produced
almost 100% Se0 after exposure to 160 mg
liter1 selenite
(29). For some bacteria,
selenite reduction is mediated by a single enzyme: a periplasmic
nitrite reductase (16) in
Thauera selenatis and a nitrite or a nitrate reductase (NR) in
Enterobacter cloacae
(9,
15). The proteome
analysis of R. sphaeroides exposed to selenite did not reveal
the overexpression of a single enzyme capable of reducing selenite but
did confirm the presence of some chaperones, an elongation factor, and
some enzymes associated with oxidative stress
(4). Garbisu et al.
(11) showed that selenite
reduction by Bacillus subtilis was not affected by an excess
of nitrate, nitrite, sulfate, or sulfite in the medium and suggested
that selenite was reduced by an inducible detoxification system
different from N- and S-related reductases. The kinetics of selenite
accumulation and transformation by R. metallidurans CH34
suggest the induction of some selenite uptake and reduction systems
whose nature remains unknown. The putative induction of selenite
transport and reduction, which takes several hours, can be qualified as
slow compared to the induction of the mer operon by
Hg2+, which takes a few seconds
(3).
The
uptake of selenate by R. metallidurans CH34 was
strongly limited, and the bacterial growth was not
affected by this oxyanion. This behavior is consistent with the general
idea that selenate is slowly transported inside the cells via the
sulfate permease system
(13). Selenite was
detected during the first 12 h after selenate introduction.
Several types of enzymes have been shown to reduce selenate to
selenite. In T. selenatis, this is done by a specific selenate
reductase (16,
26). In E. coli,
reduction is catalyzed by a molybdenum enzyme distinct from a nitrate
reductase (5). Evidence
for the role of a molybdo-enzyme in selenate reduction was also shown
for Enterobacter cloacae
(31). In vitro studies
showed that several NR, including some membrane-bound NR of E.
coli (1) and some
membrane-bound and periplasmic NR of R. sphaeroides,
Paracoccus denitrificans, Paracoccus pantotrophus,
and Ralstonia eutropha DSM 428
(25), were able to reduce
selenate under anaerobic conditions. Selenate might also be reduced by
the enzymes of the sulfate assimilation pathway. Such a process is
known to occur in higher plants
(22), but there is no
direct evidence for the role of sulfate-reducing enzymes in bacterial
selenate reduction. For the moment, we have no indication of
the selenate-reducing agent in R.
metallidurans CH34. The occurrence of selenite is followed by a
mixture of Se0 and RSeR and then by RSeR only. The absence
of Se0 at t = 72 h can be
explained by the high RSeR content, which may mask Se0 (see
the error bar in Fig.
4).
In summary, our
results show that selenate is partly reduced to Se0 but that
the main process is the transformation and accumulation of an RSeR-like
organoselenium compound. A similar fate for selenate was observed in
R. sphaeroides at both low and high selenate concentrations
(29). de Souza et al.
(8) found that
selenate-treated Halomonas bacteria accumulate selenate and a
minor selenomethionine-like species and suggested that selenate follows
the sulfate assimilation pathway.
These results raise the
question of why selenite and selenate follow different pathways,
provided that selenate is first reduced to selenite. This study shows
that reduction and assimilation pathways are taken by both oxyanions
and that the former pathway seems to be activated upon selenite
exposure only. The possible inhibition of the reduction of selenite to
Se0 by selenate can be ruled out since the bacteria exposed
to both oxyanions still produced the red color indicative of
Se0. The nonactivation of the reduction pathway upon
selenate exposure could be related to the much smaller uptake of
selenate relative to selenite, supposing that this pathway is activated
above a threshold concentration of selenite or any chemical agent
derived from selenite. In this study, maximum measured selenite
concentrations were comparable upon selenite and selenate exposure
(around 3 mg Se per g of proteins) (Fig.
2 and
4), but these values are
only snapshot images, rather than a direct monitoring of the selenite
content.
In conclusion, this study showed that both selenite and
selenate follow an assimilatory and a detoxification pathway in R.
metallidurans CH34 and that transport and reduction are activated
upon selenite exposure. The capacity of this bacterium to accumulate
and reduce large amounts of selenite may qualify this strain as
suitable for the bioremediation of selenite-contaminated soils,
sediments, and waters. However, the same is not true for selenate,
since the organoselenium species produced may represent some mobile and
bioavailable forms of selenium. This study illustrates the potential of
XANES spectroscopy combined with elemental analyses, which enable the
quantification of Se species. This spectroscopic approach
is complementary to analytical speciation techniques such as
liquid or ionic chromatography or electrospray mass spectrometry
(6), which are better
suited to identify individual
molecules.
 |
ACKNOWLEDGMENTS
|
|---|
We
acknowledge J. L. Hazemann and O. Proux for their assistance
during XANES measurements and the ESRF for the provision of beam
time.
This research was supported by the CNRS and CEA through the
Programme National Toxicologie Nucléaire
Environnementale.
 |
FOOTNOTES
|
|---|
* Corresponding
author. Mailing address: Environmental Geochemistry Group,
LGIT, University of Grenoble and CNRS, BP 53, 38041 Grenoble, Cedex 9,
France. Phone: 33 (0)4 76 82 80 21. Fax: 33 (0)4 76 82 81 01. E-mail:
gsarret{at}ujf-grenoble.fr. 
 |
REFERENCES
|
|---|
- Avazéri,
C., R. Turner, J. Pommier, J. Weiner, G. Giordano, and A.
Verméglio. 1997. Tellurite reductase activity of
nitrate reductase is responsible for the basal resistance of
Escherichia coli to tellurite. Microbiology
143:1181-1189.[Abstract]
- Avoscan,
L., M. Carrière, F. Jehanneuf, R. Collins, F. Carrot, J.
Covès, and B. Gouget. 2004. Ralstonia
metallidurans CH34 resistance to selenium oxyanions:
growth kinetics, bioaccumulation and reduction, p.267
-271. In J. A.
Centeno, P. Collery, and G. Vernet (ed.), Metal ions in biology
and medicine, vol. 8. John Libbey Eurotext, Montrouge,
France.
- Barkay,
T., S. Miller, and A. Summers. 2003. Bacterial mercury
resistance from atoms to ecosystems. FEMS Microbiol.
Rev.
27:355-384.[CrossRef][Medline]
- Bebien,
M., J.-P. Chauvin, J.-M. Adriano, S. Grosse, and A.
Verméglio. 2001. Effect of selenite on growth
and protein synthesis in the phototrophic bacterium Rhodobacter
sphaeroides. Appl. Environ. Microbiol.
67:4440-4447.[Abstract/Free Full Text]
- Bébien,
M., J. Kirsch, V. Méjean, and A. Verméglio.2002
. Involvement of a putative molybdenum enzyme in the
reduction of selenate by Escherichia coli.Microbiology
148:3865-3872.[Abstract/Free Full Text]
- Chasteen,
T., and R. Bentley. 2003. Biomethylation of selenium
and tellurium: microorganisms and plants. Chem. Rev.
103:1-25.[CrossRef][Medline]
- Combs,
G. F., Jr., C. Garbisu, B. C. Yee, A. Yee,
D. E. Carlson, N. R. Smith, A. C.
Magyarosy, T. Leighton, and B. B. Buchanan.1996
. Bioavailability of selenium accumulated by
selenite-reducing bacteria. Biol. Trace Elem. Res.
52:209-225.[Medline]
- de
Souza, M. P., A. Amini, M. A. Dojka, I.
J. Pickering, S. C. Dawson, N. R. Pace, and N.
Terry. 2001. Identification and characterization of
bacteria in a selenium-contaminated hypersaline evaporation pond.Appl. Environ. Microbiol.
67:3785-3794.[Abstract/Free Full Text]
- Dungan,
R. S., and W. T. Frankenberger.1998
. Reduction of selenite to elemental selenium by
Enterobacter cloacae SLD1a-1. J. Environ. Qual.
27:1301-1306.[Abstract/Free Full Text]
- Ganther,
H. 1968. Selenotrisulfides. Formation by the reaction
of thiols with selenious acid. Biochemistry
7:2898-2905.[CrossRef][Medline]
- Garbisu,
C., S. Gonzalez, W. H. Yang, B. C. Yee,
D. L. Carlson, A. Yee, N. R. Smith, R. Otero,
B. B. Buchanan, and T. Leighton. 1995.
Physiological mechanisms regulating the conversion of selenite to
elemental selenium by Bacillus subtilis.Biofactors
5:29-37.[Medline]
- Haygarth,
P. 1994. Global importance and global cycling of
selenium, p. 1-27. In
W. T. Frankenberger, Jr., and S. Benson (ed.),Selenium in the environment
. Marcel Dekker, New York,
N.Y.
- Heider,
J., and A. Böck. 1993. Selenium metabolism in
micro-organisms. Adv. Microb. Physiol.
35:71-109.[Medline]
- Kramer,
G., and B. Ames. 1988. Mechanisms of mutagenicity and
toxicity of sodium selenite (Na2SeO3) in
Salmonella typhimurium. Mutat. Res.
201:169-180.[Medline]
- Losi,
M. E., and W. T. Frankenberger.1998
. Reduction of selenium oxyanions by Enterobacter
cloacae strain SLDIa-I, p.515
-544. In W. T.
Frankenberger and R. A. Engberg (ed.), Environmental
chemistry of selenium, vol. 64. Marcel Dekker, New York,
N.Y.
- Macy,
J. M. 1994. Biochemistry of selenium
metabolism by Thauera selenatis gen. nov. sp. nov. and use of
the organism for bioremediation of selenium oxyanions in San Joaquin
Valley drainage water, p. 421-444.
In W. T. Frankenberger, Jr., and S. Benson (ed.),Selenium in the environment
. Marcel Dekker, New York,
N.Y.
- Manceau,
A., M. A. Marcus, and N. Tamura. 2002.
Quantitative speciation of heavy metals in soils and sediments by
synchrotron X-ray techniques, p.341
-428. In P. Fenter, M.
Rivers, N. Sturchio, and S. Sutton (ed.), Applications of
synchrotron radiation in low-temperature geochemistry and environmental
science, vol. 49. Reviews in mineralogy and geochemistry,
Mineralogical Society of America, Washington,
D.C.
- Mergeay,
M., S. Monchy, T. Vallaeys, V. Auquier, A. Benotmane, P. Bertin, S.
Taghavi, J. Dunn, D. van der Lelie, and R. Wattiez.2003
. Ralstonia metallidurans, a bacterium
specifically adapted to toxic metals: towards a catalogue of
metal-responsive genes. FEMS Microbiol. Rev.
27:385-410.[CrossRef][Medline]
- Mergeay,
M., D. Nies, H. G. Schlegel, J. Gerits, P. Charles, and F.
Van Gijsegem. 1985. Alcaligenes eutrophus
CH34 is a facultative chemolithotroph with plasmid-bound resistance to
heavy metals. J. Bacteriol.
162:328-334.[Abstract/Free Full Text]
- Pickering,
I., G. George, V. Van Fleet-Stalder, T. Chasteen, and R. Prince.1999
. X-ray absorption spectroscopy of selenium-containing
amino acids. J. Biol. Inorg. Chem.
4:791-794.[CrossRef][Medline]
- Pickering,
I. J., G. E. Brown, and T. K.
Tokunaga. 1995. Quantitative speciation of selenium in
soils using X-ray absorption spectroscopy. Environ. Sci.
Technol.
29:2456-2459.
- Pilon-Smits,
E. A. H., S. B. Hwang, C. M.
Lytle, Y. L. Zhu, J. C. Tai, R. C. Bravo,
Y. C. Chen, T. Leustek, and N. Terry. 1999.
Overexpression of ATP sulfurylase in Indian mustard leads to increased
selenate uptake, reduction, and tolerance. Plant
Physiol.
119:123-132.[Abstract/Free Full Text]
- Roux,
M., and J. Covès. 2002. The iron-containing
superoxide dismutase of Ralstonia metallidurans CH34.FEMS Microbiol. Lett.
210:129-133.[CrossRef][Medline]
- Roux,
M., G. Sarret, I. Pignot-Paintrand, M. Fontecave, and J.
Covès. 2001. Mobilization of selenite by
Ralstonia metallidurans CH34. Appl. Environ.
Microbiol.
67:769-773.[Abstract/Free Full Text]
- Sabaty,
M., C. Avazeri, D. Pignol, and A. Vermeglio. 2001.
Characterization of the reduction of selenate and tellurite by nitrate
reductases. Appl. Environ. Microbiol.
67:5122-5126.[Abstract/Free Full Text]
- Schröder,
I., S. Rech, T. Krafft, and J. M. Macy.1997
. Purification and characterization of the selenate
reductase from Thauera selenatis. J. Biol.
Chem.
272:23765-23768.[Abstract/Free Full Text]
- Stadtman,
T. 1996. Selenocysteine. Annu. Rev.
Biochem.
65:83-100.[CrossRef][Medline]
- Turner,
R. J., J. H. Weiner, and D. E.
Taylor. 1998. Selenium metabolism in Escherichia
coli. Biometals
11:223-227.[CrossRef][Medline]
- Van
Fleet-Stalder, V., T. G. Chasteen, I. J. Pickering,
G. N. George, and R. C. Prince.2000
. Fate of selenate and selenite metabolized by
Rhodobacter sphaeroides. Appl. Environ.
Microbiol.
66:4849-4853.[Abstract/Free Full Text]
- Wasserman,
S. R., P. G. Allen, D. K. Shuh,
J. J. Bucher, and N. M. Edelstein.1999
. EXAFS and principal component analysis: a new shell
game. J. Synchrotron Rad.
6:284-286.[CrossRef][Medline]
- Watts,
C., H. Ridley, K. Condie, J. Leaver, D. Richardson, and C. Butler.2003
. Selenate reduction by Enterobacter
cloacae SLD1a-1 is catalysed by a molybdenum-dependent
membrane-bound enzyme that is distinct from the membrane-bound nitrate
reductase. FEMS Microbiol. Lett.
228:273-279.[CrossRef][Medline]
Applied and Environmental Microbiology, May 2005, p. 2331-2337, Vol. 71, No. 5
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