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Applied and Environmental Microbiology, July 2000, p. 3037-3043, Vol. 66, No. 7
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Whole-Cell versus Total RNA Extraction for Analysis
of Microbial Community Structure with 16S rRNA-Targeted Oligonucleotide
Probes in Salt Marsh Sediments
Marc E.
Frischer,1,*
Jean M.
Danforth,1
Michele A. Newton
Healy,1,2 and
F. Michael
Saunders2
Skidaway Institute of Oceanography, Savannah,
Georgia 31411,1 and Georgia Institute of
Technology, Environmental Engineering, Atlanta, Georgia
303322
Received 28 January 2000/Accepted 28 March 2000
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ABSTRACT |
rRNA-targeted oligonucleotide probes have become powerful tools for
describing microbial communities, but their use in sediments remains
difficult. Here we describe a simple technique involving homogenization, detergents, and dispersants that allows the
quantitative extraction of cells from formalin-preserved salt marsh
sediments. Resulting cell extracts are amenable to membrane blotting
and hybridization protocols. Using this procedure, the efficiency of
cell extraction was high (95.7% ± 3.7% [mean ± standard
deviation]) relative to direct DAPI (4',6'-diamidino-2-phenylindole)
epifluorescence cell counts for a variety of salt marsh sediments. To
test the hypothesis that cells were extracted without phylogenetic
bias, the relative abundance (depth distribution) of five major
divisions of the gram-negative mesophilic sulfate-reducing delta
proteobacteria were determined in sediments maintained in a tidal
mesocosm system. A suite of six 16S rRNA-targeted oligonucleotide
probes were utilized. The apparent structure of sulfate-reducing
bacteria communities determined from whole-cell and RNA extracts were
consistent with each other (r2 = 0.60),
indicating that the whole-cell extraction and RNA extraction hybridization approaches for describing sediment microbial communities are equally robust. However, the variability associated with both methods was high and appeared to be a result of the natural
heterogeneity of sediment microbial communities and methodological
artifacts. The relative distribution of sulfate-reducing bacteria was
similar to that observed in natural marsh systems, providing
preliminary evidence that the mesocosm systems accurately simulate
native marsh systems.
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INTRODUCTION |
Over the past decade, 16S
rRNA-targeted specific oligonucleotide probes have become a powerful
tool for describing the structure of microbial communities in a variety
of natural environments (1, 35). In planktonic environments,
a number of straightforward hybridization techniques are available for
utilizing oligonucleotide probes, including whole-cell fluorescence in
situ hybridization (1, 6, 16, 28, 29) and direct whole-cell
blot hybridization (2, 5). These techniques simplify the use
of 16S rRNA-targeted probes and therefore allow processing of larger
numbers of samples required for conducting ecologically relevant
studies. However, sediment and detritus often interfere with the
enumeration of bacteria, hybridization, hybridization detection, and
the extraction and purification of RNA (34). Thus, probe
hybridization studies of sediment samples are more difficult and
time-consuming than analogous studies in planktonic environments.
Despite the difficulty involved, many studies have demonstrated the
utility of applying 16S rRNA probe hybridization strategies in sediment
environments (3, 4, 7, 9, 10, 12, 17, 23, 24, 25, 30). In
general, these studies have relied on hybridization of probes to RNA
extracted, purified, and immobilized onto charged nylon membranes or
fluorescence in situ hybridization (41). To our knowledge,
no studies have utilized more straightforward whole-cell membrane
hybridization techniques (5). One impediment to using
whole-cell hybridization protocols in association with sediments has
been the difficulty of quantitative extraction of cells from sediments.
Extraction of cells from fine-grained highly organic sediments typical
of salt marsh environments is particularly difficult.
Several problems must be overcome to facilitate the extraction of cells
from sediments. First, since cells are often tenaciously attached to
sediment particles, cells must be detached and separated from sediment
particles and organic material that might interfere with the
immobilization of cells to charged nylon or complicate microscopic
visualization of cells. Second, cells must be extracted without regard
to their phylogenetic identity or physiological status, since
extraction biases would artifactually influence the observed microbial
structure. Extraction bias is not thought to be a problem for total RNA
extraction procedures, but this assumption has not been experimentally investigated.
Several studies have investigated the quantitative extraction of cells
from sediments. Methods have typically involved ultrasonication, vigorous homogenization, and/or the addition of detergents and dispersants (13, 34, 36, 38). These methods have been successful with a variety of sediment types (11, 13, 14, 31, 32,
36, 38). In this study, we evaluated a modified protocol for
extracting cells from salt marsh sediments that involved the use of
homogenization, detergents, and dispersants, but did not require
sonication. This technique allowed the rapid and quantitative extraction of cells from sediments that had been stored in formalin, while avoiding possible cell lysis by sonication. Resulting cell extracts were substantially reduced in sediment and detritus content and were therefore amenable to membrane blotting and hybridization protocols. The intent of this study was to determine if the whole-cell and RNA extraction techniques could be used to provide equivalent information regarding the composition of salt marsh sediment microbial communities by using a 16S rRNA-targeted oligonucleotide probe hybridization approach. To test the hypothesis that cells were extracted without phylogenetic biases, the microbial community structure (depth distribution) of five major divisions of the gram-negative mesophilic sulfate-reducing bacteria (SRB) were determined using a suite of SRB group-specific
[32P]-labeled 16S rRNA-targeted oligonucleotide probes.
The apparent structure of SRB communities was compared between RNA and
whole-cell extracts from replicate salt marsh sediment samples.
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MATERIALS AND METHODS |
Collection of sediments.
Sediments used for developing the
cell extraction protocol were collected from a pristine Spartina
alterniflora-dominated salt marsh located adjacent to the Skidaway
River, Savannah, Ga., on the campus of the Skidaway Institute of
Oceanography. Intact sediment cores were collected using a custom
manufactured surface-sterilized polycarbonate corer with a diameter of
5 cm and total length of 40 cm. Sediment from 2- to 4-cm intervals were
extruded using a Teflon-tipped plunger into sterile disposable 50-ml
tubes. Sediment (up to 4 g) was aliquoted into fresh sterile
tubes, and an amount of 10 ml of artificial seawater (ASW) g of
sediment
1 (27) that was 3.7% formalin (Sigma
Chemical Co., St. Louis, Mo.) was added to the sediment and slurried by
vortexing. Preserved sediments were stored at 4°C until use.
Salt marsh sediments used in probe hybridization studies were
originally collected from an Environmental Protection Agency (EPA)
Superfund site (LCP chemical site) located in Brunswick, Ga. These
sediments were contaminated with mercury and polychlorinated biphenyls
(ca. 10 ppt each) as a result of the operation of a chlor-alkali plant
(18, 37). Contaminated sediments planted with S. alterniflora and unplanted are maintained in a salt marsh mesocosm
system operated by the Skidaway Institute of Oceanography (21). These mesocosms consist of 2.88- by 1.44- by 1.44-m
cells filled to a depth of 0.91 m (3.8 m3) with marsh
sediments and operated on a 6.5-h tidal cycle that approximates the
natural tidal cycle in coastal south Georgia. Replicate sediment cores
(10-cm depth) were collected from randomly selected locations in the
mesocosms by using a 50-ml custom-manufactured syringe coring device.
For these studies, sediment cores were collected in June 1999, 6 months
after sediments were initially placed in the mesocosm systems.
Sediments were collected, extruded, and preserved frozen at
80°C
until use.
Whole-cell extraction.
Formalin-fixed sediments (generally
1 g in 10 ml of ASW plus 3.7% formalin) were made 0.01 M (final
concentration) with respect to sodium pyrophosphate (stock solution at
0.1 M; Sigma Chemical Co.) and 0.09% Tween 80 (stock solution at
100%; Sigma Chemical Co.) and were vigorously vortexed for 1 min.
Sediments were incubated for 30 min at room temperature and were again
vortexed for 15 s. The bulk of sediment particles were removed by
centrifugation at 700 × g for 2 min. The supernatant
containing the bacteria was removed to a fresh tube by aspiration. The
sediment was washed two times with 10 ml of sterile ASW by vortexing
for 1 min, and the wash supernatant was collected after centrifugation
as described above. Both the original extract and wash supernatant
(approximately 30 ml) were combined. Cells were collected by
centrifugation at 12,000 × g for 10 min at 4°C and
resuspended in 3 ml of fresh sterile ASW. In some cases, remaining fine
sediment particles were removed by centrifugation (200 × g) for 1 min. Total cell abundance was determined by
epifluorescence microscopy after staining cells with DAPI
(4',6'-diamidino-2-phenylindole) (40).
RNA extraction.
Total RNA was extracted and purified from
salt marsh sediments essentially by following the procedure described
by Moran et al. (25). The yield and quality of extracted RNA
was improved when sediments were frozen prior to extraction (data not
shown), and thus RNA was routinely extracted from sediment samples (5 g) that had been stored frozen
80°C for at least 2 days. Sediments were thawed on ice and equilibrated in 20 ml of ice-cold 120 mM sodium
phosphate (pH 5.2) for 15 min with shaking. Following equilibration, the sediment was collected by centrifugation at 6,000 × g for 10 min at 4°C. The supernatant was discarded, and the
sediment pellet was washed with another 20 ml of phosphate buffer.
Following centrifugation at 6,000 × g for 10 min, the
resulting pellet was resuspended in 7 ml of lysing buffer (50 mM Tris
[pH 8.0], 0.25 mM EDTA [pH 8.0], 25% sucrose), to which 5 mg of
lysozyme (Sigma Chemical Co.) ml
1 was freshly added. The
sediment was incubated at room temperature for 15 min and centrifuged
at 6,000 × g for 10 min at 4°C. The resulting
supernatant was decanted, and the pellet was equilibrated with 7 ml of
ACE buffer (10 mM sodium acetate, 10 mM NaCl, 3 mM EDTA [pH 5.1]).
The pellet was again collected by centrifugation (6,000 × g, 10 min) and warmed to 60°C in a heated water bath for 10 to
15 min. ACE-buffered phenol (250 µl) and 20% sarcosyl (500 µl
warmed to 60°C) were added to the pellet. The sediment was vortexed
briefly and was incubated at room temperature. After 5 min, the
solution was made 0.075 M NaCl by the addition of 300 µl of a 2 M
NaCl solution that had been warmed to 60°C. The resulting sediment
was extracted once with 6 ml of ACE-buffered phenol-chlorform-isoamyl alcohol (pH 5.1; 75:24:1). The aqueous extract (ca. 8 to 13 ml) was
made 0.3 M sodium acetate by the addition of 1/10 volume of a 3 M
sodium acetate solution. Following nucleic acid concentration, DNA was
digested with 100 U of RNase-free DNase I (Sigma Chemical Co.) and
purified using ACE-buffered phenol chlorform as previously described
(25). Generally, the RNA-containing aqueous phase remained
dark brown at this stage. Contaminating humic substances were removed
by size filtration in 2.5-ml Sephadex G-75-120 spun columns constructed
in standard 3-ml disposable syringes as described by Moran et al.
(25). Sephadex was equilibrated in diethyl
pyrocarbonate-treated distilled water prior to use. The quantity,
purity, and quality of the extracted RNA were routinely determined by
spectroscopy and visualization after agarose gel electrophoresis,
respectively (33). Purified RNA was stored at
80°C until use.
Determination of microbial community structure.
The relative
abundance of the total eubacteria community and five phylogenetically
distinct groups of SRB (Desulfobulbus, Desulfobacterium, Desulfobacter,
Desulfovibrio, and Desulfococcus) was determined
by hybridization of phylogenetic group-specific, 32P-labeled 16S rRNA-targeted oligonucleotide probes
previously developed (8, 15). The Desulfovibrio
group probe (SRB 687) also hybridizes with a number of the
iron-reducing geobacters which are not SRB (22). All probes
used in this study are shown in Table 1.
The specificity of each of these probes was confirmed empirically at
the indicated hybridization temperature by using purified RNA from
cultured SRB strains (Fig. 1a). The
sensitivity of each probe was also determined by dilution series
studies using representative SRB cultures (Fig. 1b). Probe
hybridization was conducted in a slot blot format using charged nylon
(Zeta Probe, catalog no. 162-0165; Bio-Rad Laboratories, Hercules,
Calif.). Initially, hybridization of concentration dilution series of
RNA and sediment whole-cell extracts were performed to determine the optimal RNA and cell concentrations most appropriate for quantification by scanning densitometry. These studies indicated that under the conditions of this study, 2 to 5 ng of purified RNA/slot or ca. 106 cells/slot yielded hybridization densities well within
the dynamic range of the scanning densitometer for quantification (data
not shown). Therefore, in all studies reported here, RNA (ca. 2 to 5 ng/slot) and whole-cell extracts containing ca. 3 × 106 cells in 100 µl were immobilized on nylon membranes
using a slot blot apparatus (Schleicher & Schuell, Inc., Keene, N.H.).
Following blotting, RNA was cross-linked to the membrane by baking in
vacuo at 80°C for 2 h or by UV cross-linking for 30 s at
the 120,000-microjoule setting using a UV cross-linker (UV Stratalinker
model 1800; Stratagene Cloning Systems, La Jolla, Calif.). Membranes
were stored desiccated at
20°C until use.

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FIG. 1.
Specificity of 16S rRNA-targeted probes used in this
study and the detection sensitivity of a typical probe (UNIV 342)
applied for the detection of membrane blotted cells. (A) The
specificity of each of the probes used in this study was determined by
hybridization at 37°C for the universal eubacterium-targeted probe
UNIV and at 55°C for the SRB group-specific probes (SRB 687, 660, 814, 129, 221). RNA (2 ng/slot) purified from cultures of
Desulfovibrio desulfuricans ATCC 13541 (DSV),
Desulfobulbus propionicus ATCC 33891 (DSB),
Desulfococcus multivorans ATCC 33890 (DSC),
Desulfobacter sp. strain BG-8 (DBACTER
[30]), and Desulfobacterium sp. strain
BG-33 (DSBM [30]) were immobilized on replicate
charged nylon membranes and hybridized with each probe used in this
study. (B) Hybridization sensitivity of a 16S rRNA-targeted probe (UNIV
342) for the detection of immbolized D. desulfuricans cells.
Hybridization signal was proportional (r2 = 0.90) to the number of cells. Hybridization detection is expressed
in relative optical density (OD) units. Autoradiograph of replicate
whole-cell hybridization used to construct the regression line is shown
below the regression line.
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Oligonucleotides were synthesized using an ABI DNA/RNA synthesizer
(model 394) by the Molecular Genetics Facility at the University of
Georgia. Oligonucleotides were end labeled with 60 µCi of
[
-32P]ATP (6,000 Ci/mmol; Du Pont/NEN, Boston, Mass.)
using T4 polynucleotide kinase (Promega Corp., Madison, Wis.) as
described previously (15).
Prehybridization, hybridization, and washes were performed by following
published methods (15) at 55°C. Hybridization and wash
temperatures were previously empirically determined for each probe
(8, 19, 20; Table 1). The blots were prehybridized in a filter-sterilized (0.2 µm) hybridization solution containing 6×
SSPE (1× SSPE is 180 mM NaCl, 10 mM NaH2PO4,
and 1 mM Na2EDTA [pH 7.7]), 0.1% sodium dodecyl sulfate,
and 1× Denhardt's solution (0.2% Ficoll, 0.02%
polyvinylpyrrolidone, 0.02% bovine serum albumin). After 3 h, the
prehybridization solution was replaced with fresh hybridization
solution containing 20 pmol of 32P-labeled probe and was
incubated overnight. Prehybridization and hybridization were conducted
in 50- or 100-ml hybridization tubes (Bockel Scientific, Feasterville,
Pa.) in a rotary hybridization oven (Robbins Scientific Model 2000 microhybridization incubator; Robbins Scientific, Corp., Sunnvale,
Calif.). To avoid excessive nonspecific background hybridization,
especially with the RNA blots, it was critical to perform
prehybridization and hybridization of cell and RNA blots separately
(data not shown). Following hybridization, the blots were washed for
1 h in three changes of 6× SSPE plus 0.1% SDS at the
hybridization temperature. The blots were dried briefly under an
infrared lamp and were attached to filter paper, and hybridization was
detected by autoradiography using medical X-ray film (Fuji Medical
Systems, USA, Inc., Stamford, Conn.). Generally, a clear hybridization
signal was detected after 3 to 24 h for whole-cell blots and 24 to
72 h for RNA blots, depending on the probe used and the sample.
Hybridization was quantified by scanning densitometry using the
Quantity One version 4 software package and a GS-710 Calibrated Imaging
Densitometer system (Bio-Rad Laboratories).
Statistics.
The observed relative distribution of SRB groups
with respect to depth were compared between the whole-cell extraction
and RNA extraction techniques for each sample and at each depth by two-way analysis of variance. The relative abundance of the five SRB
groups in each sample was estimated by normalizing against the
abundance of total eubacteria determined using the universal eubacterial probe UNIV 342 in the same sample. The overall comparison of the hybridization results between the whole-cell extraction technique and hybridization of purified RNA was made by linear regression. Cell concentrations of extracted sediments were compared to
cell concentrations of unextracted samples by simple t
tests. All comparisons were performed at the 95% confidence level.
Statistical analyses were facilitated using the SigmaStat version 2.01 software package (SPSS, Inc., Chicago, Ill.).
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RESULTS |
Whole-cell extraction from salt marsh sediments.
The
efficiency of cell extraction from sediment was determined by comparing
the concentrations of cells in sediment-free extracts to cell
concentrations determined in the same sediments prior to extraction.
Cell recoveries from salt marsh sediments sampled from various depths
ranged from 91 to 102% relative to those from unextracted cell counts
(Table 2). The average extraction
recovery was 95.7% ± 3.7% (mean ± standard deviation) and was
not significantly different from unextracted cell counts at the 95%
confidence limit (P = 0.118). The amount of detrital
material in sediment extracts appeared to be substantially reduced
compared to that in unextracted samples (Fig.
2). In these micrographs, the irregularly
shaped yellow stained material is believed to be detritus and sediment, while bacteria appear blue-white after DAPI staining (26).
Cell extracts were sufficiently free of sediments so that
106 to 108 cells could be quantitatively
blotted and cross-linked to charged nylon membranes and hybridized
without interference from sediment particles. The cell extraction
procedure typically required only 2 h, compared to nearly 2 days
required for extraction and purification of RNA from sediments.

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FIG. 2.
Photomicrographs of DAPI-stained bacteria before (A and
B) and after (C and D) extraction using the whole-cell extraction
procedure.
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Blot hybridization; whole-cell versus RNA.
Slot blot
hybridization with 32P-labeled oligonucleotide probes of
whole cells and purified RNA are shown in Fig.
3. On average, 105 to
107 cells that originated from 0.015 to 0.03 g of
sediment and 2 to 4 ng of RNA were blotted per individual slot.
Generally, significantly stronger hybridization signals were obtained
from whole-cell blots versus purified RNA relative to the amount of
sediment initially extracted. Thus, in addition to the whole-cell
extraction procedure being considerably simpler and less time-consuming
than the RNA extraction procedure, hybridization sensitivity appears
also to be greater using the whole-cell technique. These observations suggest that a greater fraction of the total sediment bacterial RNA is
recovered when cells are extracted from the sediment prior to lysis
rather than lysing cells in situ as is done when total RNA is
extracted. Because stronger hybridization signals were routinely
obtained from the whole-cell blots than from the RNA blots, the time
required for autoradiographic quantification was also shorter for
whole-cell blots relative to that for RNA blots. Typically, whole-cell
blots with 105 to 107 cells · slot
1 rarely required more than 24 h of exposure,
while RNA blots with 3 to 5 ng of RNA · slot
1
typically required several days of exposure for adequate
quantification.

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FIG. 3.
Hybridization of whole-cell (A) and RNA-extracted (B)
sediments with 32P-labeled universal eubacterial 16S
rRNA-targeted oligonucleotide probe UNIV 342. Fifty microliters of the
whole-cell extract (ca. 105 to 106 cells) and 3 ng of extracted RNA was immobilized on the membrane for each depth
sample (slot). Sediment depth and average relative hybridization
density (optical density) for each depth is shown. Average
hybridization signal is the result of replicate blots from replicate
core samples indicated as REP 1 and REP 2.
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Estimating phylogenetic diversity.
The distribution of total
eubacteria and of five groups of gram-negative mesophilic SRB
populations in salt marsh sediments that had recently been placed in a
tidal mesocosm system was determined by hybridization with a suite of
phylogenetic group-specific probes. The distribution in the top 10 cm
of the sediment was determined using purified RNA and whole-cell
extracts simultaneously. The relative distribution of each group is
reported after normalization to the total eubacterial rRNA signal that
was determined by quantifying the hybridization signal of replicate
blots hybridized with the universal eubacterium-targeted
oligonucleotide probe UNIV 342 (Table 1). With the exception of one
group of the SRB (Desulfobulbus, probe SRB 660), the
distribution of SRB populations and of total eubacteria was
statistically identical whether the distribution was determined using
the whole-cell or RNA extraction technique (Fig.
4). Within the top 10 cm of sediment the
distribution of eubacteria was approximately homogeneous (Fig. 4A),
while four of the five SRB groups examined exhibited a relative maximum
between the depths of 4 and 6 cm (Fig. 4B to E). In the one instance in which the results from the whole-cell and RNA extraction techniques did
not yield the same results (Desulfobulbus; P = 0.037), the whole-cell technique indicated a relative maximum of
Desulfobulbus at 4 to 6 cm (Fig. 4F). Results obtained from
RNA blots suggested that there were no differences in the relative
abundance of this group with depth. Overall, the relative hybridization
signals obtained with the whole-cell and RNA extraction techniques were similar. Relative hybridization of RNA blots could be reasonably predicted from relative whole-cell hybridization intensities by a
simple first-order linear regression model (r2 = 0.60) when the results from the hybridization with the
Desulfobulbus-specific probe were omitted (Fig.
5). The slope (0.96) and intercept (0.03) were not significantly different from 1 and 0, respectively, indicating a quantitatively direct relationship between the techniques.

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FIG. 4.
Relative depth distribution of total eubacteria and five
groups of gram-negative mesophilic SRB in mercury- and PCB (Aroclor
1268)-contaminated salt marsh sediment equilibrated in the BERM
mesocosm system for 6 months. Relative normalized hybridization is
reported as a fraction of the strongest hybridization signal at any
depth in a given core. Profiles of sulfate-reducing groups were
normalized to the total eubacterial signal. Distribution was determined
after whole-cell extraction ( ) and direct RNA extraction ( ).
Depth profiles of total eubacteria (probe UNIV 342) (A),
Desulfobacterium (probe SRB 221) (B),
Desulfobacter (probe SRB 129) (C), Desulfovibrio
(probe SRB 687) (D),
Desulfococcus/Desulfosarcina/Desulfobotulus group (probe SRB
814) (E), and Desulfobulbus (probe SRB 660) (F) are shown.
Error bars indicate standard deviation of the mean from four
independent hybridizations. Depth distributions for each probe
determined after whole-cell and RNA extractions were compared by
two-way analysis of variance.
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FIG. 5.
Linear regression of relative hybridization of all
16S rRNA-targeted oligonucleotide probes used in this study determined
after whole-cell extraction and RNA extraction in paired samples from
the same cores and depths. Comparisons include all phylogenetic groups
except the Desulfobulbus group (probe SRB 660). The
regression coefficient is 0.60, the slope is 0.96, and the intercept is
0.03.
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DISCUSSION |
The objectives of this study were to develop a whole-cell
extraction technique suitable for use with salt marsh sediments and to
determine whether cell extracts were suitable for microbial diversity
studies utilizing phylogenetic group-specific 16S rRNA-targeted oligonucleotide probes.
Direct comparisons of cell counts obtained from a variety of salt marsh
sediments before and after the whole-cell extraction indicated that
cells could be quantitatively recovered from salt marsh sediments by
using the cell extraction procedure developed in this study.
Furthermore, it was not possible to extract sufficient RNA for
additional hybridization analysis from extracted sediments, strengthening the conclusion that cells were quantitatively removed from marsh sediments using the procedure described here (data not
shown). Sonication, which in some studies has been shown to be required
for dislodging sediment-attached bacteria but also to reduce cell
recoveries (13), was not required to achieve quantitative
cell recoveries using the technique developed in this study with salt
marsh sediments. The cell extraction technique required substantially
less time compared to the relatively laborious RNA extraction and
purification techniques previously used in conjunction with molecular
probe hybridization studies. Therefore, the whole-cell extraction
technique is more amenable to the analysis of larger ecologically
significant numbers of samples. Furthermore, because hybridization
signals were consistently stronger when whole-cell blots were
hybridized relative to blotted RNA, it can be speculated that the
efficiency of RNA extraction was greater when the cells are extracted
prior to cell lysis. Therefore, the sensitivity of the whole-cell
extraction technique is greater than that achieved by RNA extraction.
Thus, smaller sample sizes are required, further improving the ability
to conduct ecologically relevant studies that typically can require the
analysis of hundreds to thousands of individual samples. The greater
efficiency of RNA extraction in the whole-cell extraction procedure is
most likely due to a number of factors associated with lysing cells in
the presence of native sediments. For example, it is likely that the
degradation rate of free RNA is greater than cellular RNA in sediments
and that sediments more readily bind free RNA rather than cellular RNA.
Alternatively, if the specificity of the probes when hybridized to
whole-cell extracts is different from that achieved when purified RNA
was hybridized, the inferred greater hybridization sensitivity detected
with whole-cell blots might be due to nonspecific probe hybridization.
However, several reports in the literature suggest that the specificity
of 16S rRNA-targeted oligonucleotide probes are maintained when used in
whole-cell formats (1, 5) although the sensitivity of probes
may be reduced in whole cells due to ribosomal higher order structure
(15).
A priori there is reason to believe that the extraction of cells from
sediments may lead to extraction bias in cell recovery. For example,
some cell types may be more fastidiously attached to sediment particles
and therefore may be less efficiently extracted. However, in the
studies described here, the differences observed in the relative
distribution of cell types in sediment cores between the RNA and
whole-cell extraction methods were not significant. This observation
was true whether essentially all eubacterial cells or specific groups
of the delta proteobacteria were studied. Of six comparisons made (120 individual hybridization blots), in only one case
(Desulfobulbus probe) were the relative hybridization signals different between the RNA and whole-cell extracts. These results suggest that the whole-cell extraction and RNA extraction hybridization approaches for describing sediment microbial communities are equally robust. Although the relative results obtained with the two
techniques could be compared directly, since the absolute quantities of
specific RNA targets or cell types were not determined, it was not
possible to infer the diversity (species richness and abundance) of the
sediment microbial communities from these studies.
Although the relative hybridization results obtained with the two
methods were similar, the variability associated with replicates was
high. In some cases, variability between replicate samples exceeded 2 standard deviations from the mean. This variability appears to stem
both from natural heterogeneity of sediment microbial communities and
from methodological artifacts, since there was an equally high degree
of variability between replicate cores and between replicate extracts
of single core samples (data not shown). Although the source of this
variability remains largely unknown, it seems unlikely that the bulk of
variability was associated with the inherent complexity of the target
microbial consortia. If this were the case, we would have expected that
the magnitude of hybridization variability associated with a particular
probe would be inversely proportional to its phylogenetic specificity, since the broader the phylogenetic specificity the more complex the
target community. This was not the case. For example, the average
precision (standard deviation) associated with the mean relative
hybridization of whole-cell extracts using the universal eubacterium-targeted probe (UNIV 342) was similar to the average precision associated with the five delta proteobacterium-specific probes. The standard deviation associated with the eubacterial probe
was 0.2 compared with an average standard deviation of 0.2 ± 0.1 associated with the delta proteobacterial group-specific probes.
However, the source of this variability remains unclear. No obvious
correlation between sediment characteristics, such as density,
porosity, or organic content, was noted in these studies, although the
variability associated with sediments that were obtained from a 6- to
8-cm depth generally seemed to be the highest (Fig. 4). The high
variability associated with direct RNA hybridization, regardless of
whether the whole-cell extraction or RNA extraction technique is used,
limits the resolution of these techniques to discern differences in the
composition of sediment microbial community structures. Therefore,
methodological and sampling variability should be an important
consideration in the generation and interpretation of sediment rRNA
hybridization data. Furthermore, these studies suggest that continued
research is required to determine the source and nature of the
variability associated with rRNA phylogenetic specific probe
hybridization of sediment microbial communities.
Although only relative abundances of bacteria were determined in this
study, the overall distribution pattern of gram-negative mesophilic SRB
was similar to those reported in other studies (17, 30). SRB
consortia were observed at all depths sampled, but were maximal between
4 and 6 cm. Similar distribution patterns have also been observed in
natural S. alterniflora-dominated salt marshes in Georgia by
using the same suite of rRNA-targeted oligonucleotide probes (19,
20).
Because the sediments used in this study originated from an
experimental mesocosm system that had been established for 6 months, an
evaluation of the distribution patterns of different microbial groups
provides an opportunity to evaluate how accurately the mesocosm
reflects native salt marsh sediments. Although the observations that
are reported here must still be considered preliminary from this
perspective, these results suggest that the mesocosm systems do
accurately simulate the distribution of microbial consortia after a
6-month period of equilibration. The equilibration process of these
mesocosms with respect to other parameters, including sediment physical
characteristics, porewater chemistry, microbial activity, and plant
growth, will be reported elsewhere. To our knowledge, the structure of
microbial consortia has not been previously evaluated in these types of
mesocosm systems and suggests that salt marsh mesocosm systems can be
established that accurately simulate a native S. alterniflora salt marsh environment typical of southeastern United
States coastal systems.
 |
ACKNOWLEDGMENTS |
This work was supported by grants from the National Science
Foundation (grant number DEB-9706317), the Office of Naval Research (grant number N00014-97-1-0955), and the U.S. EPA (Hazardous Substance Research Council) (grant number R825513-01).
We thank J. K. King for technical assistance and the Skidaway
Institute of Oceanography physical operations staff for construction and operation of the BERM tidal mesocosm facility. Anna Boyette helped
prepare the figures and Dee Peterson prepared the manuscript.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Skidaway
Institute of Oceanography, 10 Ocean Science Circle, Savannah, GA 31411. Phone: (912) 598-2308. Fax: (912) 598-2310. E-mail:
frischer{at}skio.peachnet.edu.
 |
REFERENCES |
| 1.
|
Amann, R. I.,
W. Ludwig, and K.-H. Schleifer.
1995.
Phylogenetic identification and in situ detection of individual microbial cells without cultivation.
Microbiol. Rev.
59:143-169[Abstract/Free Full Text].
|
| 2.
|
Betzl, D.,
W. Ludwig, and K.-H. Schleifer.
1990.
Identification of lactococci and enterococci by colony hybridization with 23S rRNA-targeted oligonucleotide probes.
Appl. Environ. Microbiol.
56:2927-2929[Abstract/Free Full Text].
|
| 3.
|
Boivin-Jahns, V.,
D. Ruimy,
A. Bianchi,
S. Daumas, and R. Christen.
1996.
Bacterial diversity in a deep-subsurface clay environment.
Appl. Environ. Microbiol.
63:3405-3412[Abstract].
|
| 4.
|
Borneman, J.,
P. W. Skroch,
K. M. O'Sullivan,
J. A. Palus,
N. G. Rumjanek,
J. L. Janse,
J. Nienhuis, and E. W. Triplett.
1996.
Molecular microbial diversity of an agricultural soil in Wisconsin.
Appl. Environ. Microbiol.
62:1935-1943[Abstract].
|
| 5.
|
Braun-Howland, E. B.,
P. A. Vescio, and S. A. Nierzwicki-Bauer.
1993.
Use of a simplified cell blot technique and 16S rRNA-directed probes for identification of common environmental isolates.
Appl. Environ. Microbiol.
59:3219-3224[Abstract/Free Full Text].
|
| 6.
|
DeLong, E. F.,
G. S. Wickham, and N. R. Pace.
1989.
Phylogenetic stains: ribosomal RNA-based probes for the identification of single cells.
Science
243:1360-1363[Abstract/Free Full Text].
|
| 7.
|
Devereux, R.,
M. Delaney,
F. Widdel, and D. A. Stahl.
1989.
Natural relationships among sulfate-reducing bacteria.
J. Bacteriol.
171:6689-6695[Abstract/Free Full Text].
|
| 8.
|
Devereux, R.,
M. D. Kane,
J. Winfrey, and D. A. Stahl.
1992.
Genus- and group-specific hybridization probes for determinative and environmental studies of sulfate-reducing bacteria.
Syst. Appl. Microbiol.
15:601-609.
|
| 9.
|
Devereux, R., and G. W. Mundfrom.
1994.
A phylogenetic tree of 16S rRNA sequences from sulfate-reducing bacteria in a sandy marine sediment.
Appl. Environ. Microbiol.
60:3437-3439[Abstract/Free Full Text].
|
| 10.
|
Devereux, R.,
M. E. Hines, and D. A. Stahl.
1996.
S cycling: characterization of natural communities of sulfate-reducing bacteria by 16S rRNA sequence comparisons.
Microb. Ecol.
32:283-292[Medline].
|
| 11.
|
Dye, A. H.
1983.
A method for the quantitative estimation of bacteria from mangrove sediments.
Estuar. Coast. Shelf Sci.
17:207-212.
|
| 12.
|
Edgcomb, V. P.,
J. H. McDonald,
R. Devereux, and D. W. Smith.
1999.
Estimation of bacterial cell numbers in humic acid-rich salt marsh sediments with probes directed to 16S ribosomal DNA.
Appl. Environ. Microbiol.
65:1516-1523[Abstract/Free Full Text].
|
| 13.
|
Ellery, W. N., and M. H. Schleyer.
1984.
Comparison of homogenization and ultrasonication as techniques in extracting attached sedimentary bacteria.
Mar. Ecol. Prog. Ser.
15:247-250.
|
| 14.
|
Epstein, S. S., and J. Rossel.
1995.
Enumeration of sandy sediment bacteria: search for optimal protocol.
Mar. Ecol. Prog. Ser.
117:289-298.
|
| 15.
|
Frischer, M. E.,
P. J. Floriani, and S. A. Nierzwicki-Bauer.
1996.
Differential sensitivity of 16S rRNA targeted oligonucleotide probes used for fluorescence in situ hybridization is a result of ribosomal higher order structure.
Can. J. Microbiol.
42:1061-1071[Medline].
|
| 16.
|
Giovannoni, S. J.,
E. F. DeLong,
G. J. Olsen, and N. R. Pace.
1988.
Phylogenetic group-specific oligodeoxynucleotide probes for identification of single microbial cells.
J. Bacteriol.
170:720-726[Abstract/Free Full Text].
|
| 17.
|
Hines, M. E.,
R. S. Evans,
B. R. Sharak Genthner,
S. G. Willis,
S. Friedman,
J. N. Rooney-Varga, and R. Devereux.
1999.
Molecular phylogenetic and biogeochemical studies of sulfate-reducing bacteria in the rhizosphere of Spartina alterniflora.
Appl. Environ. Microbiol.
65:2209-2216[Abstract/Free Full Text].
|
| 18.
|
Kannan, K.,
K. A. Maruya, and S. Tanabe.
1997.
Distribution and characterization of polychlorinated biphenyl congeners in soil and sediment from a Superfund site contaminated with Aroclor 1268.
Environ. Sci. Technol.
31:1483-1488[CrossRef].
|
| 19.
|
King, J. K.
1999.
Quantitative assessment of mercury methylation by phylogenetically diverse consortia of sulfate-reducing bacteria in salt marsh systems. Ph.D. thesis.
Georgia Institute of Technology, Atlanta.
|
| 20.
|
King, J. K.,
J. E. Kostka,
M. E. Frischer, and F. M. Saunders.
2000.
Sulfate-reducing bacteria methylate mercury at variable rates in pure culture and in marine sediments.
Appl. Environ. Microbiol.
66:2430-2437[Abstract/Free Full Text].
|
| 21.
|
Lee, R. F.
1997.
Bioremediation studies at the Skidaway Institute of Oceanography. Skidaway Scenes: Newsl.
Skidaway Mar. Sci. Found.
13:2-4.
|
| 22.
|
Lonergan, D. J.,
H. L. Jenter,
J. D. Coates,
E. J. Phillips,
T. M. Schmidt, and D. R. Lovely.
1996.
Phylogenetic analysis of dissimilatory Fe(III)-reducing bacteria.
J. Bacteriol.
178:2402-2408[Abstract/Free Full Text].
|
| 23.
|
MacGregor, B. J.,
D. P. Moser,
E. W. Alm,
K. H. Nealson, and D. A. Stahl.
1997.
Crenarchaeota in Lake Michigan sediment.
Appl. Environ. Microbiol.
63:1178-1181[Abstract].
|
| 24.
|
Manz, W.,
M. Eisenbrecher,
T. R. Neu, and U. Szewzyk.
1998.
Abundance and spatial organization of Gram-negative sulfate-reducing bacteria in activated sludge investigated by in situ probing with specific 16S rRNA targeted oligonucleotides.
FEMS Microbiol. Ecol.
25:43-61[CrossRef].
|
| 25.
|
Moran, M. A.,
V. L. Torsvic,
T. Torsvick, and R. E. Hodson.
1993.
Direct extraction and purification of rRNA for ecological studies.
Appl. Environ. Microbiol.
59:915-918[Abstract/Free Full Text].
|
| 26.
|
Mostajir, B.,
J. R. Dolan, and F. Rassoulzadegan.
1995.
A simple method for the quantification of a class of labile marine pico-sized and nano-sized detritus DAPI yellow particles (DYP).
Aquat. Microbiol. Ecol.
9:259-266.
|
| 27.
|
Paul, J. H.
1982.
The use of Hoechst dyes 33258 and 33342 for enumeration of attached and planktonic bacteria.
Appl. Environ. Microbiol.
43:939-944[Abstract/Free Full Text].
|
| 28.
|
Ramsing, N. G.,
M. Kuhl, and B. B. Jorgensen.
1993.
Distribution of sulfate-reducing bacteria, O2, and H2S in photosynthetic biofilms determined by oligonucleotide probes and microelectrodes.
Appl. Environ. Microbiol.
59:3840-3849[Abstract/Free Full Text].
|
| 29.
|
Ramsing, N. B.,
H. Fossing,
T. G. Ferdelman,
F. Andersen, and B. Thamdrup.
1996.
Distribution of bacterial populations in a stratified fjord (Mariager fjord, Denmark) quantified by in situ hybridization and related to chemical gradients in the water column.
Appl. Environ. Microbiol.
62:1391-1404[Abstract].
|
| 30.
|
Rooney-Varga, J. N.,
R. Devereux,
R. S. Evans, and M. E. Hines.
1997.
Seasonal changes in the relative abundance of uncultivated sulfate-reducing bacteria in a salt marsh sediment and in the rhizosphere of Spartina alterniflora.
Appl. Environ. Microbiol.
63:3895-3901[Abstract].
|
| 31.
|
Rublee, P., and B. E. Dornseif.
1978.
Direct counts of bacteria in the sediments of North Carolina saltmarsh.
Estuaries
1:188-191[CrossRef].
|
| 32.
|
Rublee, P. A.
1982.
Bacteria and microbial distribution in estuarine sediments, p. 159-182.
In
V. S. Dennedy (ed.), Estuarine comparisons. Academic Press, Inc., New York, N.Y.
|
| 33.
|
Sambrook, J.,
E. F. Fritsch, and T. Maniatis.
1989.
Molecular cloning: a laboratory manual, 2nd ed.
Cold Spring Harbor Laboratory Press, Cold Spring Harbor, N.Y.
|
| 34.
|
Schallenberg, M.,
J. Kalff, and J. B. Rasmussen.
1989.
Solutions to problems in enumerating sediment bacteria by direct counts.
Appl. Environ. Microbiol.
55:1214-1219[Abstract/Free Full Text].
|
| 35.
|
Stahl, D. A.
1995.
Application of phylogenetically based hybridization probes to microbial ecology.
Mol. Ecol.
4:535-542.
|
| 36.
|
Tao, S. F., and G. L. Taghon.
1997.
Enumeration of protozoa and bacteria in muddy sediment.
Microbial Ecol.
33:144-148[CrossRef][Medline].
|
| 37.
|
U.S. Environmental Protection Agency.
1995.
Phase I site characterization sampling map and chemical analysis supplement, LCP Chemicals.
U.S. Environmental Protection Agency, Washington, D.C.
|
| 38.
|
Velji, M. I., and L. J. Albright.
1986.
Microscopic enumeration of attached marine bacteria of seawater, marine sediment, fecal matter, and kelp blade samples following pyrophosphate and ultrasound treatments.
Can. J. Microbiol.
32:121-126.
|
| 39.
|
Vescio, P. A., and S. A. Nierzwicki-Bauer.
1995.
Extraction and purification of CR amplifiable DNA from lacustrine subsurface sediments.
J. Microbiol. Methods
21:225-233.
|
| 40.
|
Williams, S. C.,
Y. Hong,
D. C. A. Danavall,
M. H. Howard-Jones,
D. Gibson,
M. E. Frischer, and P. G. Verity.
1998.
Distinguishing between living and nonliving bacteria: evaluation of the vital stain propidium iodide and the combined use with molecular probes in aquatic samples.
J. Microbiol. Methods
32:225-236.
|
| 41.
| Zepp Falz, K., C. Holliger, R. Großkopt, W. Liesack,
A. N. Nozhevnikova, B. Müller, B. Wehrli, and D. Hahn.
Vertical distribution of methanogens in the anoxic sediment of Rotsee
(Switzerland). Appl. Environ. Microbiol. 65:2402-2408.
|
Applied and Environmental Microbiology, July 2000, p. 3037-3043, Vol. 66, No. 7
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