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Applied and Environmental Microbiology, July 2000, p. 3078-3082, Vol. 66, No. 7
Division of Microbiology, National Research
Centre for Biotechnology (GBF), D-38124 Braunschweig, Germany
Received 22 December 1999/Accepted 5 April 2000
The seasonal dynamics of river biofilm communities in two German
rivers, the Elbe and one of its tributaries, the Spittelwasser, were
investigated for the first time by using fluorescence in situ
hybridization and a standardized biofilm sampling procedure. We show
the importance of members of the In recent investigations of
microbial communities in rivers in which the 16S ribosomal DNA approach
has been used, the workers have focused on very few samples which were
analyzed in depth (3, 8) or on succession during the
development of a biofilm (13). They did not determine how
the communities were affected by the seasonal fluctuations in physical
and chemical parameters that typically occur in rivers. The dynamics of
rivers make sampling of microbial communities which are representative
of a certain geomorpholocial region and time span during the year very
difficult. Therefore, we studied sessile microbial communities which
grew on glass plates exposed at a defined depth below the river
surface. Biofilms were harvested after 1 month of growth in situ. The
microbial community composition was determined at the level of the
major phylogenetic groups present. Quantification was based on
microscopic counts of individual cells that hybridized with fluorescent
probes directed to rRNA (fluorescence in situ hybridization [FISH])
(2). The standardized way of obtaining biofilm samples used
in this study allowed us for the first time to compare seasonal
dynamics of community structure in two rivers with different levels of pollution.
Study site.
Biofilms were studied at the following two sites:
(i) the Elbe River upstream of the city of Magdeburg, at km 320 (11°40'E, 52°4'N), which is one of the big rivers in Europe and has
a catchment area of 148,268 km2 and a total length of 1,091 km (http://www.hamburg.de/Umwelt/wge/), and (ii) a massively polluted
second-order tributary of the Elbe, the Spittelwasser River, which is
close to the industrial center of Bitterfeld (12°17'E, 51°42'N).
The Spittelwasser River had high ammonia concentrations in all seasons
(average, 2.0 mg/liter, compared to 0.3 mg/liter in the Elbe), a lower
oxygen content (average, 6.3 mg/liter, compared to 10.5 mg/liter in the
Elbe), and high concentrations of heavy metals (mercury, cadmium, lead, copper, and arsenic), chlorinated aromatic compounds (hexachlorohexane, hexachlorobenzene, dichlorodiphenyl trichloroethane, polychlorinated biphenyl), adsorbable organic halogens, and organotin compounds in the
suspended particulate matter which exceeded by far the concentrations
in the Elbe. The water temperature of the Spittelwasser River was about
3 to 4°C higher than that of the Elbe from November to April due to
discharge of warm factory production wastewater (Fig.
1). Primary production in the Elbe
correlated well with the temperature, which started to increase in
April and reached low values again at the beginning of October (Fig.
1). During this time microinvertebrates were frequently found in the
biofilms.
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Biofilm Community Structure in Polluted Rivers:
Abundance of Dominant Phylogenetic Groups over a Complete Annual
Cycle
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ABSTRACT
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Abstract
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References
subclass of the class Proteobacteria, which formed the largest single group in
the massively polluted Spittelwasser at all times. Clear seasonal peaks
of abundance were observed for the planctomycetes and the
Cytophaga-Flavobacterium cluster.
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TEXT
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Abstract
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FIG. 1.
Seasonal fluctuations in the water temperatures in the
Elbe and Spittelwasser rivers and in the chlorophyll a
concentrations in the Elbe River.
Sampling device and sampling procedure.
To raise a sufficient
amount of natural biofilm in each river, a biofilm collector was
constructed (Fig. 2). This device
consisted of a Plexiglas frame carrying seven glass plates and two
holders for microscopic slides. The frame was mounted on threaded rods. The collector was submerged 20 to 30 cm below the river surface, either
by using a floating device (Elbe) or by inserting the rods into the
river bottom (Spittelwasser). Biofilms were harvested monthly from May
1994 until September 1994 in the Elbe and in both the Elbe and the
Spittelwasser from May 1997 until May 1998. After 35 ± 3 days of
exposure to the river water the biofilm collector was removed from the
river. The glass plates were taken out, and the biofilm was scraped off
with a sterile razor blade. Clean glass plates and slides were inserted
into the Plexiglas frame and exposed again in the river. Biofilm
samples could not be collected in March and April 1998 due to a period
of high water. The communities which developed on the plates can best
be compared to the epilithic biofilms described by Lock
(10). They were formed by single attached bacteria, algae,
and trapped particulate matter glued together by extracellular
polysaccharides. Thus, both free-living and particle-attached river
bacteria were represented. Subsequently, growing processes, as well as
grazing by both protozoans and macroinvertebrates, influenced the
development of the biofilms. Biofilms and slides were fixed and then
stored for FISH analysis for both gram-negative and gram-positive
bacteria as described previously (2, 18) directly on-site by
using a mobile laboratory.
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Preparation of samples. Prior to counting the contents of the samples had to be dispersed. An appropriate amount of each fixed biofilm sample (200 to 1,000 µl, depending on the ratio of fixative to biofilm) was centrifuged (2 min, 7,000 × g). Pellets (approximately 50 µl) were suspended in 950 µl of Na4P2O7 (0.1%, wt/vol) and homogenized by ultrasonification (30 s; 50 W; impulse, 0.6 s; Labsonic U; B. Braun). Approximately 1- to 2-µl portions of the samples were spotted onto gelatinated, Teflon-coated slides (Paul Marienfeld GmbH & Co. KG, Bad Mergentheim, Germany), dried for 20 min at 37°C, and dehydrated (2). This procedure yielded about 100 to 300 DAPI (4',6'-diamidino-2-phenylindole)-stained cells per counting grid (10 by 10 fields; magnification, ×1,000).
Probes and stringency conditions. Probes EUB338 (11), ALF1b (11), BET42a (11), GAM42a (11), CF319a (12), PLA46 (15), and HCG69a (18) were used as described previously. Nonfluorescent competitor probes were used in equal amounts with probes ALF1b, BET42a, GAM42a, and HGC69a to obtain optimal stringency conditions. BET42a and GAM42a served as competitors for each other. The competitor for HGC69a was probe NHGC (18). For probe ALF1b we obtained higher specificity by using two competitor probes, NEP (5'CGTTCAYTCTGAGCCAG3') and NLHGC (5'CGTTCGYCCTGAGCCAG3'). Nonspecific binding was checked with probe NonEUB338 (22). The 5' ends of the oligonucleotides were labeled with the indocarbocyanine dye Cy3 (TIB MOLBIOL, Berlin, Germany) except for the competitor probes. To check the stringency of hybridization directly for each slide, one well was used as a control; a mixture of easily distinguishable representative strains belonging to target and nontarget groups was applied.
Whole-cell hybridization of samples and DAPI staining. FISH of whole cells was performed as described previously (2, 11). The concentration of each probe was 5 ng/µl of hybridization solution. Ten microliters of hybridization buffer containing probes was applied to each well. The washing buffer contained concentrations of NaCl which corresponded to the formamide concentrations in the hybridization buffer. The DNA-specific dye DAPI (16) was used to determine the total numbers of cells in the samples. Ten microliters of a DAPI solution (5.5 µg/ml) was added to each well. After 2 min the DAPI was carefully rinsed off with 50 ml of MilliQ water. The slides were air dried, mounted with Citifluor AF1 against bleaching, and sealed with coverslips (24 by 50 mm) and nail polish.
Microscopy and counting. The hybridized and DAPI-stained samples were examined with an epifluorescence microscope (Axioplan; Zeiss, Oberkochen, Germany) equipped with a Plan-Neofluar objective (magnification, ×100). Excitation was carried out with a 50-W high-pressure mercury bulb (Osram HBO50) and filter sets for DAPI (filter set 01; Zeiss) and Cy3 (filter set 41007a HQ; AHF Analysentechnik, Tübingen, Germany). Two replicate samples were counted for each hybridization procedure. For each sample, 16 to 20 randomly chosen microscopic fields were counted per well by using a counting grid, the data for the two parallel counts were averaged, and the standard deviation was determined. For each grid up to 300 DAPI-stained cells were counted, and for each hybridization more than 4,000 DAPI-stained cells were counted.
Biofilm in situ hybridization.
The average staining efficiency
of the bacterial probe was 56% for the Elbe biofilms and was
consistently 10% higher for the Spittelwasser biofilms. For the Elbe,
the highest percentage of EUB338-stained cells was found in September
(70.0%) (Fig. 3A); this maximum value
corresponded to a bloom of members of the
subclass of the class
Proteobacteria (
-Proteobacteria) during this
period. The lowest percentage of EUB338-stained cells (40.8%) was
observed in January. For the Spittelwasser biofilms (Fig. 3B), a bloom
of
-Proteobacteria was observed in July. No pronounced decline in staining efficiency occurred in January. These values are
within the range of values frequently observed for aquatic habitats
(reviewed in reference 4). Since low-nutrient
(oligotrophic) environments are expected to have lower staining
efficiencies than high-nutrient (eutrophic) environments (6, 8,
23), the data might indicate that the activity of the
Spittelwasser biofilms was higher because of a higher nutrient level.
However, some investigators have observed unexpectedly high staining
efficiencies for low-nutrient and/or cold habitats, such as an
oligotrophic river (13), drinking water biofilms
(7), and the winter cover and pelagic layers of an
oligotrophic mountain lake (1).
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Effect of pollution on river biofilm community structure.
The
two rivers which we compared differed with respect to pollution
(extreme pollution in the Spittelwasser, medium pollution in the Elbe)
and with respect to size and the parameters correlated with it (e.g.,
flow velocity). However, the major phylogenetic groups of bacteria were
present in both rivers at similar abundances (Fig. 3). One significant
difference was the large proportion of
-Proteobacteria in
the Spittelwasser biofilms; in these biofilms they were the most
abundant organisms at all times, accounting for on average 31% of all
of the cells (compared to 18% in the Elbe biofilms). The ammonia
concentrations were significantly higher in the Spittelwasser River
than in the Elbe throughout the year and might have supported a large
population of ammonia-oxidizing bacteria, which are a monophyletic
assemblage in the
-Proteobacteria (20). The
-Proteobacteria did not constitute a major component of
the community, based on numerical abundance, neither in the Spittelwasser nor in the Elbe biofilms. In the past many biodegrading strains were assigned to the genus Pseudomonas, which forms
a tight cluster within the
-Proteobacteria
(14). However, since then several former
Pseudomonas species have been redescribed and assigned to
members of the
-Proteobacteria (9), and
several new biodegrading strains belonging to the
-Proteobacteria have been isolated (21). Thus,
some of the diversity of the
-Proteobacteria in the Elbe
and particularly in the Spittelwasser River may be due to
pollutant-degrading bacteria.
Seasonal fluctuations in the planctomycetes and the
Cytophaga-Flavobacterium cluster.
For the
Proteobacteria and gram-positive bacteria with high G+C
contents, no seasonal pattern was observed, probably because of the
great diversity of physiologically different microorganisms in these
groups. Another reason might be that despite the open character and
dynamics of rivers, there is a certain uniformity in the microbial
community. A seasonal cycle of abundance was observed for the
planctomycetes and the Cytophaga-Flavobacterium (CF) cluster
(Fig. 4). The maximum level of
planctomycetes occurred in July, and the abundance decreased during
autumn; the densities were especially low in December, January, and
February both in the Elbe and in the Spittelwasser River. The July
maximum was confirmed by analyzing biofilms which were collected in the
Elbe River in 1994. Less pronounced but still significant was the
bimodal distribution of the abundance of members of the CF cluster; a maximum occurred in July, and a second maximum occurred in the winter
(in February for the Elbe and in January for the Spittelwasser). Thus,
in the cold season (Fig. 1), low levels of planctomycetes and high
levels of members of the CF cluster were present. These general
patterns occurred in both rivers and thus must have been caused by
factors common to both. Maximum levels of members of the CF cluster
have been observed frequently in the winter in aquatic environments, as
determined by both culturing and culture-independent methods (8,
17). Planctomycetes are widespread in aquatic habitats
(15) and have been shown to follow or accompany algal or
cyanobacterial blooms (for a review, see reference
5). However, as-yet-uncultured members of the
planctomycetes might have completely different physiological properties
(19).
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-Proteobacteria and the degree of pollution. Moreover,
the observed stability of the overall river biofilm community structure in spite of significant variations in chemical and biological parameters during the year was an interesting finding which needs to be
confirmed by analyses that provide higher resolution.
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ACKNOWLEDGMENTS |
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We are grateful to S. Wolff and H. Reincke of the ARGE (Cooperative for the Protection of the Elbe), E. Becker of the STAU (Federal Bureau of Environment Protection, Magdeburg, Germany), and D. Spott and H. Guhr of UFZ (Center for Environmental Research Leipzig-Hallebranch Magdeburg) for access to sampling sites, data, and site maps. We thank F. Walkow of the Landratsamt Bitterfeld, V. Harms of the Regierungspräsidium Dessau, H. Meye and A. Schlicht of the STAU Dessau/Wittenberg for providing Spittelwasser data. We especially thank S. Thieme of the measuring station in Magdeburg, Germany, who was always ready to help. Critical comments on the manuscript by Andreas Felske are gratefully acknowledged.
This work was funded by a grant from the Studienstiftung des Deutschen Volkes to Ingrid Brümmer and by a grant from the Niedersächsischer Schwerpunkt Meeresbiotechnologie to Wanda Fehr.
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FOOTNOTES |
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* Corresponding author. Mailing address: GBF, Mascheroder Weg 1, D-38124 Braunschweig, Germany. Phone: 49-531-6181 408. Fax: 49-531-6181 411. E-mail: iwd{at}gbf.de.
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