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Applied and Environmental Microbiology, December 1999, p. 5541-5545, Vol. 65, No. 12
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Estimation of Methanogen Biomass by Quantitation of
Coenzyme M
Dwayne A.
Elias,
Lee R.
Krumholz,*
Ralph S.
Tanner, and
Joseph M.
Suflita
Institute for Energy and the Environment and
Department of Botany/Microbiology, University of Oklahoma, Norman,
Oklahoma 73019
Received 25 August 1999/Accepted 28 September 1999
 |
ABSTRACT |
Determination of the role of methanogenic bacteria in an anaerobic
ecosystem often requires quantitation of the organisms. Because of the
extreme oxygen sensitivity of these organisms and the inherent
limitations of cultural techniques, an accurate biomass value is very
difficult to obtain. We standardized a simple method for estimating
methanogen biomass in a variety of environmental matrices. In this
procedure we used the thiol biomarker coenzyme M (CoM)
(2-mercaptoethanesulfonic acid), which is known to be present in all
methanogenic bacteria. A high-performance liquid chromatography-based
method for detecting thiols in pore water (A. Vairavamurthy and M. Mopper, Anal. Chim. Acta 78:363-370, 1990) was modified in order to
quantify CoM in pure cultures, sediments, and sewage water samples. The
identity of the CoM derivative was verified by using liquid
chromatography-mass spectroscopy. The assay was linear for CoM amounts
ranging from 2 to 2,000 pmol, and the detection limit was 2 pmol of
CoM/ml of sample. CoM was not adsorbed to sediments. The methanogens
tested contained an average of 19.5 nmol of CoM/mg of protein and
0.39 ± 0.07 fmol of CoM/cell. Environmental samples contained an
average of 0.41 ± 0.17 fmol/cell based on most-probable-number
estimates. CoM was extracted by using 1%
tri-(N)-butylphosphine in isopropanol. More than 90% of
the CoM was recovered from pure cultures and environmental samples. We
observed no interference from sediments in the CoM recovery process,
and the method could be completed aerobically within 3 h. Freezing
sediment samples resulted in 46 to 83% decreases in the amounts of
detectable CoM, whereas freezing had no effect on the amounts of CoM
determined in pure cultures. The method described here provides a quick
and relatively simple way to estimate methanogenic biomass.
 |
INTRODUCTION |
Methanogenesis occurs in a wide
variety of anaerobic habitats, including wetlands, lake sediments,
animal gastrointestinal tracts, and geothermally heated environments.
The optimal temperatures for methanogenesis vary from 2°C to more
than 100°C. Most methanogens can use H2 or acetate as a
source of electrons for methanogenesis. In this respect, these
organisms carry out the terminal step in anaerobic decomposition
(41).
Thus, methanogens play an essential role in the mineralization of
organic material (9, 15) due to the energetics of electron flow (10). They are directly involved in the treatment of
wastewater, sewage, and solid wastes (19, 23, 24, 28-30,
32).
In ecological and environmental studies a quick, easy, reliable method
for accurately estimating methanogenic biomass is often necessary. Methanogens possess several potential biomarkers, including coenzyme F420, isoprenoids, and lipid ethers in the
cell membranes, as well as coenzyme M (CoM). While coenzyme
F420 has been considered a molecule which could be used for
biomass estimation, it suffers from the following two limitations: (i)
the fact that intracellular concentrations vary up to 25-fold (14,
21, 40) and (ii) the fact that it has been found in other
archaebacteria (14, 21). Quantification of unique methanogen
lipids requires labor-intensive extraction and analysis procedures.
CoM, one of the few naturally occurring sulfonic acids (38),
was discovered (22) and identified in the mid-1970s
(36). With the exception of an aerobic alkene-degrading bacterium (3), CoM is found only in methanogens; the
concentration of CoM varies only by a factor of 5 in different species
(5), and standard material is commercially available. CoM
was recently reported to be present in Xanthobacter strains
(3) participating in a highly specialized alkene oxidation
pathway. While this finding indicates that CoM is not present only in
methanogens, it is unlikely that the CoM present in
Xanthobacter strains is quantitatively important in natural
samples obtained from anaerobic environments.
The previously developed techniques for assaying CoM include a bioassay
(5) and a high-performance liquid chromatography (HPLC)-based method which measures fluorescent isoindole derivatives of
thiols (25). The latter method was not standardized for
biomass determination. Both of these methods are cumbersome and
time-consuming, require strictly anaerobic conditions, and were not
designed for use with sediments.
In this study, we modified the HPLC-based procedure (25) so
that we could quantify CoM within hours of sample collection without a
requirement for anoxic conditions. We also standardized the technique
with pure cultures so that it could be used to quantify methanogen
biomass in a variety of environmental matrices.
(Some of the results have been presented previously
[14a].)
 |
MATERIALS AND METHODS |
Growth of methanogens.
Methanococcus
thermolithotrophicus DSM 2095 and Methanococcus voltae
DSM 1537 were grown as previously described (34, 39). Methanobacterium thermoautotrophicum Marburg (= DSM 2133),
Methanospirillum hungatei GP1 (= DSM 1101), and
Methanosarcina barkeri Fusaro (= DSM 804) were cultured as
described by Daniels et al. (13). Methanosarcina
barkeri was grown on N2-CO2-methanol,
H2-CO2, and N2-CO2-acetate. Methanolobus
tindarius DSM 2278 was grown as previously described
(20) by using 0.4% methanol added from a sterile stock solution. Methanosaeta concilli DSM 3671 was grown as
described by Patel (30). The most-probable-number (MPN)
assays used were three-tube assays to a 10
8 dilution. The
media used for MPN assays performed with pure methanogenic cultures
were the media described above for the organisms. For MPN assays
performed with sediment samples (1), the medium used was
medium 1 prepared as previously described (4). Direct cell
counts were obtained by using a hemocytometer. All experiments were
performed twice in duplicate. The data are presented as averages with
standard deviations where appropriate.
Methanogen cultures (100 ml) were grown to the late log phase,
harvested by centrifugation at 2,700 × g for 20 min at
5 to 10°C, and resuspended in 10 ml of sterile medium. To determine levels of CoM over time, organisms were grown in 2-liter batch cultures, and 100-ml portions of the cultures were harvested at intervals. The protein contents of pure cultures were determined by
using the bicinchoninic acid protein assay (Pierce Chemical Co.).
HPLC equipment and solvent system.
A Beckman model 157 fluorescence detector (equipped with a 338-nm excitation filter and a
450-nm emission filter) was used to quantitate CoM. The HPLC analysis
was performed by using an Econosphere C18 column. The
mobile phase was 50 mM sodium acetate buffer (pH 5.7)-acetonitrile
(70:30) flowing at a rate of 1 ml/min with a 20-µl injection loop.
The isoindole derivative of CoM (calculated mass, 301 Da) was
identified by using a liquid chromatograph-mass spectrophotometer
(LC-MS) (Hewlett-Packard Series 1100) equipped with an Econosphere
C18 column. The mobile phase was 10 mM ammonium acetate
buffer (pH 5.7)-acetonitrile (70:30) flowing at a rate of 1 ml/min.
Both a standard containing 100 µM CoM and an extract of
hydrocarbon-contaminated sediment were tested and analyzed in the
electrospray-negative mode for the mass spectrophotometer and scanned
from 100 to 500 mass units. The retention times for CoM with both
solvent systems were determined by using synthetic CoM.
Analysis of CoM and samples.
All reagents were purchased
from Sigma, and standards and stock solutions were prepared fresh
daily. A 1 mM CoM stock solution was prepared by dissolving CoM in 50 mM acetate-1 mM EDTA buffer (pH 4.5). All dilutions were prepared with
1% tri-(N)-butylphosphine in 2-propanol (1% TBP). The
reagents used for derivatization of CoM were 20 µl of
o-phthalaldehyde (20 mg/ml of methanol) per ml of sample and
20 µl of ethanolamine (20 µl/ml of boric acid buffer [pH 9.0])
per ml of sample. Standards were allowed to derivatize aerobically for
5 min at room temperature.
A variety of thiols were tested to determine whether common thiols
interfered with quantification of CoM. Each thiol was prepared
as a 1 mM stock solution and diluted with 1% TBP prior to
derivatization.
The linearity of the assay was determined by diluting the 1 mM CoM
stock solution with 1% TBP. The concentrations of the resulting
standards ranged from 0.1 to 100 µM, which corresponded to 2 to
2,000 pmol of CoM
injected.
To extract CoM from cells, 0.5 ml of cells was mixed with 1 ml of 1%
TBP, and the preparation was incubated in Eppendorf tubes
for 1 h
at room temperature. Samples were then centrifuged at
12,000 ×
g for 2 min. The supernatant (1 ml) was derivatized as
described above and was analyzed by
HPLC.
The effect of freezing on the extractability of CoM was determined by
using cultures of
Methanosarcina barkeri (acetate grown),
Methanococcus thermolithotrophicus,
Methanococcus
voltae, and
Methanobacterium thermoautotrophicum
Marburg. Cultures were harvested,
and aliquots were immediately assayed
to determine their CoM contents
as described above or were stored
frozen at

60°C for 3 days in
Eppendorf tubes. After 3 days, samples
were thawed at room temperature
and assayed as described
above.
A variety of environmental matrices were sampled and assayed to
determine their CoM contents. These matrices included sediments
from a
landfill leachate-contaminated aquifer (
2,
7,
8)
a
hydrocarbon-contaminated aquifer (
6,
11,
12,
35), and
a
campus pond, as well as sewage sludge. To analyze environmental
samples, 5 g was mixed with 2 ml of 1% TBP and incubated for
1
h at room temperature to extract the
CoM.
To maximize solvent recovery, the sediment was weighed and placed into
a 10-ml syringe with its plunger removed and a piece
of Whatman filter
paper placed in the bottom of the syringe barrel.
The syringe was set
into a hole cut in the lid of a capped 50-ml
centrifuge tube (Nalgene).
After centrifugation (27,000 ×
g),
the syringe and
sediment were discarded, and 1 ml of the supernatant
in the centrifuge
tube was assayed as described
above.
Adsorption of CoM to sediments was tested by adding 100 µl of a 0.1 to 50 µM CoM solution to 2 g of sediment that previously
had been
determined to contain no detectable CoM. The CoM-spiked
sediment was
incubated aerobically at room temperature for 3 h,
and this was
followed by extraction and derivatization as described
above.
To determine the completeness of CoM extraction, environmental samples
were subjected to an additional extraction procedure.
Sediment samples
from the leachate-contaminated aquifer and pond
sediment were assayed
to determine their CoM contents, and then
they were reextracted and
assayed
again.
The effect of freezing on CoM extractability in environmental samples
was determined. Landfill aquifer sediment, hydrocarbon-contaminated
sediment, pond sediment, and sewage sludge (5 g each) were all
analyzed, and an additional 5 g of each was set aside and frozen
at

60°C for 3 days in a stoppered 10-ml syringe. After 3 days,
samples were thawed at room temperature, and the amount of CoM
was
determined.
 |
RESULTS |
Assay development and validation.
Using the HPLC method
resulted in an isolated peak at approximately 3.6 min when the sample
was dissolved in water and at 2.9 min when the sample was dissolved in
isopropanol. The peak was confirmed to be the isoindole derivative of
CoM by mass spectroscopy (Fig. 1). The
detection limit was 2 pmol, as determined by an analysis of standards.
With both pure methanogen cultures and environmental samples several
other peaks were produced. However, it was not difficult to resolve the
CoM peak. All of the other thiols tested eluted at different times than
CoM (Table 1). The assay proved to be
linear with synthetic CoM (2 to 2,000 pmol of CoM), pure methanogen
cultures (0.5 to 5.0 ml), and environmental samples (0.5 to 5.0 g). Synthetic CoM added to environmental samples was almost completely
recovered, and the amount of CoM mirrored the synthetic CoM regression
line, indicating that there was no interference from sediments and that
extracellular CoM did not adsorb to sediments.

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FIG. 1.
HPLC chromatogram of derivatized CoM (retention time,
2.9 min) from the hydrocarbon-contaminated aquifer. The buffer system
used for both HPLC and LC-MS was ammonium acetate-acetonitrile (70:30).
(Inset) LC-MS profile of the isoindole derivative of standard CoM (left
panel) and the corresponding profile of the environmental sample (right
panel). Both spectra show that the ionic molecular weight was 300, which is consistent with the structure of the fluorescent CoM
derivative shown.
|
|
Methanobacterium thermoautotrophicum Marburg and
Methanospirillum hungatei were both analyzed during growth.
With
Methanobacterium thermoautotrophicum Marburg, the
amount of total CoM (CoM per
milliliter of culture) increased with time
from 0.03 to 0.31 nmol
of CoM as the absorbance at 600 nm increased
from 0.02 to 0.17.
However, when the values were normalized for protein
content,
there was not a significant change in the amount of CoM per
milligram
of protein over time (Fig.
2).
Similar results were obtained with
Methanospirillum hungatei
(data not shown). This indicated that
the amounts of CoM per milligram
of protein were stable, and consequently,
the growth phase of the cells
may not substantially influence
CoM levels in natural samples.

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FIG. 2.
Absorbance ( ), CoM content per milliliter of culture
( ), and CoM content normalized for culture protein content ( ) in
a Methanobacterium thermoautotrophicum Marburg culture
growing on hydrogen.
|
|
CoM contents of cultures and sediments.
Pure cultures of
methanogens were compared to determine the variation in CoM levels
among different organisms, and the data suggest that CoM levels may
vary up to sevenfold (Table 2). Based on
the environmental samples tested, all of the samples contained measurable amounts of CoM (Table 3), and
sewage sludge had the highest CoM content (on a per-gram basis), 0.09 nmol of CoM/g.
Extraction efficiency of CoM assay.
Several cultures and
anoxic sediments were examined to determine whether a second extraction
increased the recovery of CoM. For pure cultures, 87.8 to 96.8% of the
total CoM detectable was recovered during the first extraction, while
the values for environmental samples ranged from 91.8 to 100% during
the first extraction. The results suggest that only a single extraction
is necessary to recover the majority of the CoM present.
Cell lysis with a French press.
Methanosarcina barkeri
(N2-CO2-methanol), Methanospirillum
hungatei, Methanobacterium thermoautotrophicum Marburg,
Methanococcus thermolithotrophicus, and Methanococcus
voltae were examined to determine if cell lysis increased the
total recovery of CoM. Cells were lysed by using a French pressure cell
at 38,000 lb/in2. CoM was extracted from cells and cell
extracts in the usual manner. For all four methanogens tested the
results were similar (data not shown).
Effect of freezing on CoM.
Pure cultures and anoxic sediments
were examined to determine if freezing had an effect on the recovery of
CoM. With all of the pure cultures tested there was not a significant
loss of CoM after freezing (Fig. 3A). In
contrast to the pure cultures, with all of the sediments there was a
significant decrease in the amount of detectable CoM after samples were
frozen and thawed (Fig. 3B).

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FIG. 3.
(A) Cultures of methanogens tested before and after
freezing at 60°C. There was no decrease in the amount of CoM
detected in cells due to freezing. (B) Environmental samples tested
before and after freezing at 60°C. There were 46 to 83% decreases
in the amount of detectable CoM depending on the matrix. Bars indicate
standard errors. Abbreviations: Ms., Methanosarcina; Mb.
therm, Methanobacterium thermoautotrophicum; Mc. therm.,
Methanococcus thermolithotrophicus; Mc.,
Methanococcus.
|
|
Amount of CoM per cell.
The amount of CoM per cell was
determined by both an MPN assay and a direct cell counting procedure.
The amounts of CoM per cell were comparable, and the overall values for
the organisms were similar (Table 2). The amounts determined by the
direct cell count procedure ranged from 0.14 fmol of CoM/cell in
Methanobacterium thermoautotrophicum to 0.70 fmol of
CoM/cell in Methanospirillum hungatei, and the average was
0.40 ± 0.20 fmol of CoM/cell. The corresponding MPN-based values
ranged from 0.34 fmol of CoM/cell in Methanococcus
thermolithotrophicus to 0.47 fmol of CoM/cell in
Methanospirillum hungatei, and the average was 0.39 ± 0.07 fmol of CoM/cell.
The amounts of CoM per cell were calculated for sediment from a campus
pond, a landfill leachate-contaminated aquifer, sewage
sludge, and six
different depths in a sediment core obtained from
the
hydrocarbon-contaminated site (Table
3). In the sediment
core obtained
from the hydrocarbon-contaminated site, the values
ranged from 0.43 to
0.74 fmol of CoM/cell. The values for the
other three samples ranged
from 0.18 to 0.48 fmol of CoM/cell.
An overall average of 0.41 ± 0.17 fmol of CoM/cell was calculated
by using the average for the
hydrocarbon-contaminated site (0.59
fmol of CoM/cell) and the values
for the other three
samples.
 |
DISCUSSION |
For many applications in environmental microbiology, accurate
estimates of microbial population size are beneficial. Methanogens are
important in many anoxic environments and carry out the terminal electron-accepting process in a variety of ecosystems. Because of this,
an accurate estimate of methanogen biomass is often desirable.
Previously, several marine thiols, including CoM, were quantified by
using an HPLC-based technique involving precolumn derivatization (25). In a more recent study, this technique was used to
quantitate thiols in pore water but not in sediments (37).
This is not the first report of the use of HPLC for thiol detection.
Two forms of CoM, mesna (sodium 2-mercaptoethanesulfonate) and dimesna
(2-mercaptoethanesulfonate disulfate), were quantitated by using
HPLC-based methods with postcolumn derivatization and colorimetry
(18, 33). The difference between the postcolumn methods used
previously and the detection procedure used in this study is that two
steps were involved in the former methods; to separate the thiol of
interest from others compounds, derivatization and quantitation
were performed separately, which required additional labor. More
recently, CoM was detected by using a fluorescent precolumn
derivatization procedure, followed by reverse-phase HPLC
(16). This procedure is similar to the procedure which we
used but differs in that synthesis of the derivatizing reagents is
difficult and time-consuming, whereas the reagents required for our
procedure are readily available.
We modified the previously described method (25) by adding
1% TBP. The 1% TBP acts as a reducing agent which prevents oxidation of CoM-SH to a homodisulfide of CoM-S-S-CoM or a heterodisulfide of
CoM-S-S-HTP (7-mercaptoheptanoylthreonine phosphate) (26, 27) as the cells are lysed in isopropanol. This means that the assay can be conducted without stringent anoxic conditions. The CoM in
several pure cultures of methanogens and environmental samples was
quantified. The protocol can be accomplished within 3 h of sample
collection. With this technique, an accurate estimate of the
methanogenic population at a given site may be obtained. This
conclusion is based on several findings, including the detection limit
(2 pmol of CoM) and the linear response of the assay for both the
synthetic cofactor and CoM obtained from pure cultures. The assay was
found to be applicable to environmental samples. An HPLC-based method
for CoA quantitation (17) produced similar results,
suggesting that a similar technique may be developed for other organisms.
Although our technique has many advantages over direct quantitation of
methanogens with the culturing technique, it clearly has some
limitations. The major limitation is the fact that the technique cannot
distinguish between viable and nonviable cells. Oxic samples involved
in oxidation of alkenes could also contain significant numbers of
nonmethanogenic organisms which contain CoM used in the degradation
reactions. We do not believe that these issues should restrict the
utility of this procedure for the quantitation of methanogens.
Our experiments revealed that the CoM concentration increased as the
absorbance of pure cultures increased over time but that the amount of
CoM per milligram of protein was constant. Thus, the CoM content per
cell varied little with the growth phase. The same trend was found for
coenzyme F420 in methanogens (31). We observed
that the amount of CoM per milligram of protein varied by up to a
factor of 7 among organisms, which was comparable to the factor of 5 associated with the previously described CoM bioassay (5).
The amounts of CoM per milligram of protein were consistent in the
current study compared to the bioassay (5).
Methanosarcina barkeri (grown on methanol) contained 41.1 nmol of CoM/mg of protein, compared to the 44.4 nmol of CoM/mg of
protein found with the bioassay, while Methanobacterium
thermoautotrophicum contained 7.5 nmol of CoM/mg of protein,
compared to the 6.7 nmol of CoM/mg of protein found with the bioassay.
The Methanospirillum hungatei data were not as consistent;
this organism contained 19.4 nmol of CoM/mg of protein, compared to the
3.9 nmol of CoM/mg of protein reported previously (5).
While there was no decrease in the ability to detect CoM in pure
cultures due to freezing, there were 46 to 83% decreases in the
environmental samples. While the reasons for this are not clear, the
data suggest that it is not advisable to store environmental samples in
the freezer prior to the assay.
The CoM biomass determined by the HPLC-based assay and the CoM biomass
determined by the direct cell count or MPN assay agreed well. The
average values obtained were as follows: 0.40 ± 0.20 fmol of
CoM/cell with the direct cell count procedure and 0.39 ± 0.07 fmol of CoM/cell with the MPN method for pure cultures and 0.41 ± 0.17 fmol of CoM/cell for environmental samples. The similarity of the
values obtained by using MPN data for environmental samples indicates
that a reference value for methanogens is possible. This would allow
quick and accurate estimation of methanogen populations directly from
the HPLC-based CoM values.
Based on the data obtained in this study, there is at most a threefold
difference in the amount of CoM per cell in environmental samples.
Also, if a reference value of 0.41 fmol of CoM/cell were used, the
laborious MPN assay would no longer be required; this would allow
reasonably accurate estimation of a methanogen population in the time
required to complete the assay.
The inherent advantage of the procedure described here over previously
described procedures is that the CoM content per cell has been
determined for a variety of environmental matrices. This procedure
provides a quick and simple aerobic method for detecting the cofactor
as a biomarker and thus quantifying methanogen biomass.
 |
ACKNOWLEDGMENTS |
This work was supported by grants from DOE and EPA Epscor.
We thank Melanie Mormile for her initial investigations during this
study, Kevin Kropp for his invaluable assistance in confirming the
identity of the CoM derivative with the LC-MS, and Richard Sparling for
his gift of Methanococcus thermolithotrophicus and Methanococcus voltae.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Institute for
Energy and the Environment and Department of Botany/Microbiology,
University of Oklahoma, Norman, OK 73019. Phone: (405) 325-0437. Fax:
(405) 325-7619. E-mail: krumholz{at}ou.edu.
 |
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Applied and Environmental Microbiology, December 1999, p. 5541-5545, Vol. 65, No. 12
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