Appl Environ Microbiol, June 1998, p. 1987-1990, Vol. 64, No. 6
Department of Biochemistry and Microbiology,
Cook College, Rutgers University, New Brunswick, New Jersey
08903-0231
Received 22 December 1997/Accepted 19 March 1998
Cocultures of Desulfovibrio desulfuricans and
Methanococcus maripaludis grew on sulfate-free lactate
medium while vigorously methylating Hg2+. Individually,
neither bacterium could grow or methylate mercury in this medium.
Similar synergistic growth of sulfidogens and methanogens may create
favorable conditions for Hg2+ methylation in low-sulfate
anoxic freshwater sediments.
Biomethylation of Hg2+
by sulfidogens in anoxic aquatic sediments (6) produces
highly toxic methylmercury pollutants that have a tendency to
accumulate in fish (8, 26). Somewhat paradoxically, in
high-sulfate estuarine sediments, the rate of Hg2+
methylation is far lower than the rate of Hg2+ methylation
in low-sulfate freshwater sediments (4, 7). The reason for
this appears to be the generation of H2S by the Hg2+-methylating sulfidogens, although the
exact mechanism of the H2S inhibition is uncertain at this
time. Most oligotrophic freshwater lakes show no outward evidence of
sulfidogenic activity, such as blackening or an H2S odor in
their sediments. We measured high rates of Hg2+ methylation
in oligotrophic lake sediments that were free of detectable
H2S and evolved methane vigorously (19). As
inhibition studies have consistently excluded methanogens and
implicated sulfidogens in Hg2+ methylation (6,
7), one is led to question how sulfidogens stay active and
methylate Hg2+ in environments that, because of likely
sulfate limitation, seem to be inhospitable to them. Based on these
considerations and on several reports of interspecies hydrogen
transfers between sulfidogens and methanogens (1, 5, 20), we
decided to explore the potential effect of such transfers on the
methylation of Hg2+ under sulfate-limited conditions. We
modeled the proposed interaction in vitro by using pure cultures of
sulfidogens and a methanogen.
Routine anaerobic Hungate techniques were used. Nitrogen gas was
passed through a reduced heated copper column to remove traces of
oxygen. Desulfovibrio desulfuricans LS was isolated in our laboratory (6). It was repurified by repeatedly picking
single colonies from shake tubes containing diagnostic media B and E of
Postgate (21) solidified with 1.5% agar. D. desulfuricans ND 132 was kindly donated by C. Gilmour (Academy of
Natural Sciences of Philadelphia). It was repurified similarly. The
cultures were maintained on medium C of Postgate (21) but
were pregrown for experiments in medium D (21) modified by
omitting FeSO4. Incubation was at 37°C under oxygen-free
100% N2 with slow shaking. After 24 h, 20-ml
suspensions in 50-ml serum bottles were centrifuged at 3,200 × g to pellet the cells. The modified medium D was removed from the
inverted bottles with a syringe and replaced by 10 ml of a specially
formulated coculture medium. This medium contained (per liter)
0.33 g of KCl, 2.75 g of MgCl2 · 7H2O, 0.25 g of NH4Cl, 0.14 g of
CaCl2 · 2H2O, 0.14 g of
K2HPO4, 18 g of NaCl, 5 g of NaHCO3, 0.25 g of yeast extract, 0.25 g of
cysteine, 1.0 g of resazurin, 0.1 g of sodium ascorbate,
0.1 g of thioglycolate, 6.0 g of sodium lactate, and the
trace elements in ATCC medium 1043 (2) modified by replacing
the ZnSO4 · 7H2O with 0.1 g of
ZnCl2 per liter and adding 0.5 g of ferric ammonium
citrate per liter. This coculture medium always contained a 1-µg/ml
spike of HgCl2 and was routinely incubated at 37°C under
100% N2 with slow shaking. The D. desulfuricans
cell pellets were suspended in 10 ml of this coculture medium with
shaking, and 1-ml portions were used to inoculate replicate 50-ml
bottles containing 19 ml of coculture medium.
Methanococcus maripaludis ATCC 43000 (2) was
kindly provided by W. B. Whitman, University of Georgia, Athens.
It was maintained and pregrown for experiments in ATCC medium 1439 (2) under 80% H2-20% CO2 with
slow shaking at 37°C. After 24 h, the cells were pelleted and
ATCC medium 1439 was replaced with 10 ml of coculture medium, as
described above for D. desulfuricans LS. One-milliliter
portions of the resuspended cells were used to inoculate a series of
50-ml bottles containing 19 ml of coculture medium. In addition, a
series of bottles containing 18 ml of coculture medium were each
inoculated with 1 ml of D. desulfuricans and 1 ml of
M. maripaludis. All of the bottles were incubated at 37°C under 100% N2 with slow shaking. At appropriate times,
bottles were removed from the incubator, 2.0 ml of a 1.0 M
CuSO4 solution was added to each bottle to stop the
reaction, and the vials were kept at For experiments performed with resting cells, the D. desulfuricans strains were pregrown in modified (sulfate-free)
medium D (21) as described above for the coculture
experiments. The cells were sedimented in the serum bottles by
centrifugation, washed once with coculture medium, and suspended to the
original volume in coculture medium containing 1.0 µg of
HgCl2 per ml.
Prior to analysis, the bottles were thawed and mixed by shaking. Five
milliliters was removed from each of the bottles, and the cells were
centrifuged and used for protein determination (17). The
remaining 15 ml was analyzed for methylmercury by the procedure of
Longbottom et al. (13) by using a Hewlett-Packard model 5890 gas chromatograph equipped with a macrobore capillary column (inside
diameter, 0.53 mm; length, 15 m: type AT-35; Alltech, Deerfield,
Ill.). The operating conditions were as follows: the carrier gas was
Ar-CH4 (95:5, vol/vol; ultrapure grade; Matheson Gas
Products, East Rutherford, N.J.) at a flow rate of 35 ml/min, the
injector temperature was 150°C, and the electron capture detector temperature was 250°C. Monomethylmercury peak (retention time, 1.25 min) areas were recorded with a Hewlett-Packard model 3392A integrator
that was calibrated by using monomethylmercury (CH3HgI) standards (American Tokyo Kasei, Inc., Portland, Oreg.). The detection limit for monomethylmercury was 1 ng/ml. The procedure of
Longbottom et al. (13) analyzes all methylmercury as
monomethylmercury, and the synthesis of CH3Hg2+
was plotted over time. In order to make comparisons between experiments easier, the rates of methylmercury synthesis were normalized to the
initial protein concentrations of the inocula. The data for time points
given below represent single determinations.
Methane determinations in the headspaces of bottles were made with a
model 1200 gas partitioner (Fisher Co., Springfield, N.J.) operated at
50°C with helium as the carrier gas at a flow rate of 30 ml/min. The
sample volume analyzed was 250 µl, and the instrument was calibrated
with methane standards (Fisher). Microscopic observations were made
with a Reichert Zetopan microscope at a magnification of ×1,000.
As shown in Fig. 1A, neither
D. desulfuricans LS nor M. maripaludis was able
to grow individually in the coculture medium, since the organic
substrate (lactate) could be used only by the former bacterium and the
electron acceptor (carbonate) could be used only by the latter
bacterium. However, in the coculture of the two bacteria, the protein
level increased 15-fold in 8 days, from 3 to 45 µg/ml.
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Mercury Methylation by Interspecies Hydrogen and
Acetate Transfer between Sulfidogens and Methanogens
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ABSTRACT
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Abstract
Introduction
Materials & Methods
Results & Discussion
References
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INTRODUCTION
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Abstract
Introduction
Materials & Methods
Results & Discussion
References
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MATERIALS AND METHODS
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Abstract
Introduction
Materials & Methods
Results & Discussion
References
20°C until analysis.
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RESULTS AND DISCUSSION
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Abstract
Introduction
Materials & Methods
Results & Discussion
References

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FIG. 1.
(A and B) Protein contents of D. desulfuricans LS and M. maripaludis cultures and a
coculture in lactate-carbonate coculture medium (A) and synthesis of
CH3Hg+ (per microgram of initial protein) from
a 1-µg/ml HgCl2 spike in the same experiment (B). (C)
Protein contents of D. desulfuricans ND 132 and M. maripaludis cultures and a coculture in lactate-carbonate
coculture medium (C) and synthesis of CH3Hg+
(per microgram of initial protein) from a 1-µg/ml HgCl2
spike in the same experiment (D). Symbols:
, D. desulfuricans culture;
, M. maripaludis culture;
, coculture.
The morphologies of the two bacteria are quite distinct. M. maripaludis cells are large cocci that are of 2 to 2.5 µm in diameter, while D. desulfuricans cells are motile curved rods that are 1.0 to 1.5 µm long. Microscopic observations of the coculture showed that the two types of cells multiplied proportionally and roughly equal numbers of the two types were produced (results not shown).
The methylmercury synthesis pattern was similar to the protein production pattern (Fig. 1B). M. maripaludis alone failed to form any methylmercury, and D. desulfuricans LS alone formed only a trace amount, but the coculture synthesized 22 ng of methylmercury per µg of initial protein in 8 days, methylating 2.6% of the available Hg2+. This rate was very similar to the rate of synthesis of methylmercury by D. desulfuricans LS in a sulfate-free pyruvate medium in which this sulfidogen can grow fermentatively without an electron acceptor (6, 19, 21). In this medium the typical D. desulfuricans LS protein yield was 30 µg/ml. M. maripaludis was unable to synthesize any methylmercury even in a complete methanogen medium (2) in which the typical M. maripaludis protein yield is 38 µg/ml (19).
The coculture experiment was also performed with D. desulfuricans ND 132, and the results were only slightly different. This strain was selected for its exceptional ability to methylate mercury. It also appeared to have a limited ability to use lactate fermentatively in the absence of sulfate or to grow on the amino acids in yeast extract, since the protein concentration of the D. desulfuricans ND 132 culture approximately doubled (Fig. 1C). As in the experiment described above, the protein concentration in the coculture increased to about 50 µg/ml. The coculture methylated large amounts of mercury, but, in contrast to D. desulfuricans LS, D. desulfuricans ND 132 alone methylated as much as two-thirds of the mercury methylated by the coculture (Fig. 1D). These experiments were repeated several times to ascertain that the difference observed was strain specific and reproducible.
D. desulfuricans LS and ND-132 belong to the "incomplete
oxidizer" subgroup of sulfidogens (21, 25). In the
presence of sulfate, they oxidize lactate to pyruvate, and the latter
yields CO2, acetate, and reducing equivalents for
SO42
reduction. D. desulfuricans
strains are unable to use acetate (6), but M. maripaludis, like many other methanogens, can use acetate as a
substrate for methanogenesis and growth (2). Thus, D. desulfuricans strains, in addition to transferring lactate hydrogens to M. maripaludis for CO2 reduction,
also benefited the methanogen by producing acetate as a methanogenic
substrate. In turn, the removal of H2 and acetate by the
methanogen allowed D. desulfuricans strains to utilize
lactate even in the absence of SO42
.
The experiments described above were performed with a 5% inoculum, and mercury methylation occurred during growth. To determine whether preformed D. desulfuricans biomass could methylate mercury under nongrowth conditions, we repeated the control experiments with the two D. desulfuricans strains in coculture medium but with a 100% inoculum. As shown in Fig. 2, D. desulfuricans LS failed to grow or to form any methylmercury under these conditions. The protein content of D. desulfuricans ND 132, which showed a limited ability to grow in the absence of sulfate, doubled, but this organism synthesized only a trace amount of methylmercury. It may be concluded that growth conditions are necessary for mercury methylation.
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The effects of selective inhibitors of methanogenesis and sulfate reduction (18) on the coculture of D. desulfuricans LS and M. maripaludis are shown in Fig. 3. Bromoethanesulfonic acid (BESA) at a concentration of 0.5 mM allowed only marginal protein synthesis by the coculture (Fig. 3A), but it allowed almost normal mercury methylation by the coculture (Fig. 3B). Molybdate (2 mM) prevented both growth of and mercury methylation by the coculture (Fig. 3A and B). The methylation of mercury observed in the BESA-inhibited coculture was unexpected, since M. maripaludis was completely inhibited by 0.2 mM BESA when it was grown alone in methanogen medium (results not shown). A possible explanation for this apparent paradox is that under sulfate-limited conditions, some sulfidogens are capable of using BESA as alternate electron acceptor (18), making cooperation with the methanogen unnecessary. That M. maripaludis was in fact inhibited by BESA in the coculture was evident from the effect of BESA on methanogenesis (Fig. 3C). Methane evolution was completely suppressed by the inhibitor, while in 7 days the control coculture produced 1,200 µl of methane per µg of initial protein in the inoculum. The results of an experiment to determine whether BESA in fact serves as an electron acceptor for D. desulfuricans LS are shown in Fig. 4. Inoculated alone into coculture medium, this strain failed to grow or to methylate mercury. In the presence of BESA, however, it methylated one-half as much mercury as it methylated when it was grown fermentatively on pyruvate without an electron acceptor. However, the rate of protein synthesis was low when BESA served as an electron acceptor compared to the rate when the organism was grown in medium D. D. desulfuricans ND 132 behaved in a similar manner (results not shown).
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The utilization of BESA as an alternate electron acceptor by sulfidogens presents a future methodological challenge for demonstrating interspecies electron transfer-mediated mercury methylation in sulfate-limited sediments. A straightforward approach would be to inhibit methanogens in such sediments by using BESA, expecting this to inhibit mercury methylation. However, since BESA serves as an alternate electron acceptor for sulfidogens, mercury methylation is likely to remain unaffected, even when the methanogens are inhibited.
In anoxic sediments, the microbial community preferentially uses the
electron acceptor that maximizes the energy yield from the available
electron donors (3). Thus, there is usually little methanogenesis from substrates utilizable by both groups until sulfate
becomes limiting to sulfidogenic activity. There is no agreement in the
literature concerning the sulfate concentration at which sulfate
becomes limiting for the activity of sulfate reducers. On the high end,
Ingvorsen et al. (10) described 300 µM as the limiting
concentration, while other workers (16, 22, 24) have claimed
that levels as low as 20 to 30 µM are limiting. Several authors have
reported values between these extremes (23, 27). The way
that sulfate reduction is measured (i.e., by spiking sediments with
35SO42
) is relevant to this
controversy. In sulfate-rich marine and estuarine sediments, the spike
adds an insignificant amount to the total sulfate concentration, but
when the sulfate concentration is near the limiting concentration, the
spike can significantly alter the sulfate pool (11). If this
is the case, the measurement does not reflect the in situ rate
accurately but instead gives a value between the actual in situ rate
and the in situ potential. In addition to this methodological
difficulty, obviously the quantity and quality of the available organic
substrates, the temperature, the pH, and other environmental factors
may influence the sulfate concentration at which sulfate becomes
limiting.
Regardless of the exact inhibitory limit, it may be assumed that at least partial sulfate limitation occurs when anoxic sediments evolve methane vigorously, indicating that much of the energy flow passes through the methanogens. This is typical of many oligotrophic freshwater lakes. Most methanogens can use CO2 as an electron acceptor, but their substrate ranges are extremely limited and they have higher Ks values for H2 and acetate than sulfidogens have (12, 14-16, 27). In sulfate-limited situations, sulfidogens may still have primary access to the organic substrates but can gain energy from them only by passing on hydrogen and acetate to methanogens and in this manner utilize the only remaining electron sink (CO2). Such interspecies hydrogen transfer has been demonstrated previously in several sulfidogen-methanogen cocultures (1, 5, 20). Our contribution explores the potential significance of this phenomenon with respect to mercury methylation.
Hg2+ is methylated principally by sulfidogens (6), yet at sulfate levels above 200 µM the product of the normal metabolism of these organisms (H2S) inhibits mercury methylation (4, 7, 9). Therefore, situations that allow sulfidogens to be active without sulfate reduction are very favorable for Hg2+ methylation. One such situation is the growth of sulfidogens on a fermentable substrate like pyruvate (6, 21). Another one, which has potentially broader ecological and environmental significance, may be the interspecies transfer of hydrogen and acetate from sulfidogens to methanogens.
We do not wish to imply that interspecies hydrogen transfer is an
exclusive mechanism for Hg2+ methylation; it merely
represents a very favorable opportunity. It has been demonstrated that
at concentrations just above the limiting concentration, sulfate
additions to a lake sediment increase Hg2+ methylation
(9). However, at SO42
concentrations of more than 200 µM, accumulating H2S
apparently starts to interfere with CH3Hg+
synthesis. As the window for sulfate-reducing activity without inhibition of Hg2+ methylation by H2S seems to
be narrow, there is reason to believe that Hg2+ methylation
via interspecies hydrogen and acetate transfer has environmental
significance.
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ACKNOWLEDGMENTS |
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This work was supported by grant 14-08-0000162034 from the U.S. Geological Survey and by New Jersey state funds.
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FOOTNOTES |
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* Corresponding author. Mailing address: Department of Biochemistry and Microbiology, R-322, Lipman Hall, Cook College, Rutgers University, P.O. Box 231, New Brunswick, NJ 08903-0231. Phone: (732) 932-9763, ext. 322. Fax: (732) 932-8965.
New Jersey Agricultural Experiment Station Publication no.
D-01408-02-97.
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