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Applied and Environmental Microbiology, March 2001, p. 1351-1362, Vol. 67, No. 3
0099-2240/01/$04.00+0 DOI: 10.1128/AEM.67.3.1351-1362.2001
Copyright © 2001, American Society for Microbiology. All rights reserved.
Community Structure and Activity Dynamics
of Nitrifying Bacteria in a Phosphate-Removing Biofilm
Armin
Gieseke,1,*
Ulrike
Purkhold,2
Michael
Wagner,2
Rudolf
Amann,1 and
Andreas
Schramm1,3
Molecular Ecology Group, Max Planck Institute
for Marine Microbiology, D-28359 Bremen,1
Department of Microbiology, Technical University Munich,
D-85350 Freising,2 and Department of
Ecological Microbiology, BITOEK, University of Bayreuth,
D-95440 Bayreuth,3 Germany
Received 11 September 2000/Accepted 19 December 2000
 |
ABSTRACT |
The microbial community structure and activity dynamics
of a phosphate-removing biofilm from a sequencing batch biofilm reactor were investigated with special focus on the nitrifying community. O2, NO2
, and
NO3
profiles in the biofilm were measured
with microsensors at various times during the nonaerated-aerated
reactor cycle. In the aeration period, nitrification was oxygen limited
and restricted to the first 200 µm at the biofilm surface.
Additionally, a delayed onset of nitrification after the start of the
aeration was observed. Nitrate accumulating in the biofilm in this
period was denitrified during the nonaeration period of the next
reactor cycle. Fluorescence in situ hybridization (FISH) revealed three
distinct ammonia-oxidizing populations, related to the
Nitrosomonas europaea, Nitrosomonas oligotropha, and
Nitrosomonas communis lineages. This was confirmed by
analysis of the genes coding for 16S rRNA and for ammonia monooxygenase (amoA). Based upon these results, a new 16S
rRNA-targeted oligonucleotide probe specific for the
Nitrosomonas oligotropha lineage was designed. FISH
analysis revealed that the first 100 µm at the biofilm surface was
dominated by members of the N. europaea and the
N. oligotropha lineages, with a minor fraction related
to N. communis. In deeper biofilm layers, exclusively
members of the N. oligotropha lineage were found. This
separation in space and a potential separation of activities in time
are suggested as mechanisms that allow coexistence of the different
ammonia-oxidizing populations. Nitrite-oxidizing bacteria belonged
exclusively to the genus Nitrospira and could be
assigned to a 16S rRNA sequence cluster also found in other sequencing
batch systems.
 |
INTRODUCTION |
Modern biological treatment of
wastewater involves not only C removal, but also elimination of the
nutrients P and N (5, 20). This requires the combined or
sequential actions of various groups of microorganisms, such as
heterotrophic bacteria, phosphate-accumulating organisms (PAO), and
nitrifying and denitrifying bacteria. Consequently, purification plants
and processes have become increasingly complex to satisfy the
needs of the different microorganisms, usually in several reactor
stages (5, 27). The integration of different functions in a single reactor would save reaction space and time and
therefore is desirable from an economical point of view. However, difficulties often arise in establishing stable nitrification in such
complex systems. Nitrifying bacteria (i.e., ammonia-oxidizing bacteria [AOB] and nitrite-oxidizing bacteria [NOB]) usually
show low maximum growth rates, relatively low substrate affinities, and
high sensitivity to toxic shocks or sudden pH changes (17, 25,
41). In the presence of organic matter, they can be easily outcompeted by heterotrophs for oxygen (56) and ammonia
(19). Other problems to be solved are the inhibition of
denitrification by the presence of oxygen (5) and the need
for cyclic changes of oxic and anoxic (i.e., free of oxygen and
nitrate) conditions for biological phosphate removal (34).
Biofilm systems are an obvious option for such multifunctional
reactors. Slow-growing organisms remain in the reactor by their
attached growth; the biofilm matrix might protect bacteria from
grazing, harmful substances, or sudden pH shifts; and biofilms can be
stratified and therefore provide oxic and anoxic reaction zones
(11). During the last 5 years, several studies
have addressed nitrifying biofilms through a combination of microsensor
measurements and 16S rRNA-based methods, such as fluorescence in
situ hybridization (FISH) (39, 48, 50). This approach
revealed, e.g., the identity and spatial arrangement of AOB and NOB in
various nitrifying systems (39, 48-50) and provided a
first estimate of their in situ reaction rates and substrate
affinities (48). However, very little is known about how
and which nitrifying bacteria are adapted to competition with
heterotrophs in more complex systems and how they interact with other processes.
Recently, a biofilm system was proposed that integrates enhanced
biological phosphate removal (EBPR) and nitrification and denitrification in a single reactor (3, 18). The biofilm is subjected to a sequencing batch mode, in which an anoxic treatment period is followed by an oxic period to allow for net accumulation of
polyphosphate in the biomass, which is removed from the system by
backwashing at regular intervals. Substrate balances revealed that the
removal of organic carbon and EBPR were successfully combined with
nitrogen removal via nitrification and denitrification (3).
In the present study, the microbial ecology of this combined
nitrification-EBPR biofilm process was investigated by using microsensor analysis and various molecular techniques, i.e., FISH and
analysis of 16S ribosomal DNA (rDNA) and amoA gene
sequences. The objectives were to reveal which populations contribute
to which part of the process, which AOB and NOB persist under these highly competitive and transient conditions, and how nitrifying activity overlaps, in time and space, with heterotrophic activity, especially EBPR.
 |
MATERIALS AND METHODS |
Process description.
A 20-liter sequencing batch biofilm
reactor (SBBR) was established as described previously
(18). The artificial wastewater was composed of
Na(CH3COO) x 3H2O (103 mg
liter
1), peptone (200 mg
liter
1),
(NH4)2SO4
(63 mg liter
1),
KH2PO4 (44 mg
liter
1), KCl (14 mg
liter
1), and yeast extract (3 mg
liter
1), leading to influent concentrations of
12 mg liter
1 for P and 38 mg
liter
1 for N and a chemical oxygen demand (COD)
of about 270 mg liter
1. Oxygen and phosphate
concentrations in the bulk water were regularly monitored by online
measurements with an oxygen electrode (Oxy 196; WTW, Weilheim, Germany)
and with a P analyzer (Phosphax Inter; Dr. Lange, Düsseldorf,
Germany). Ammonium, nitrate, and COD were determined photometrically
with standard test kits (LCK 303, 339, and 314; digital photometer ISIS
6000; Dr. Lange, Düsseldorf, Germany). The lengths of the
operation periods were as follows: 20 min of filling (min 0 to 20), 160 min of nonaerated recirculation (min 20 to 180), 260 min of
recirculation with aeration (min 180 to 440), and 40 min of draining
(min 440 to 480). The process temperature was kept at 20°C. Biofilm
was grown on substratum, Kaldnes elements (Purac, Merseburg, Germany):
i.e., plastic rings (diameter, 8 mm, height, 8 mm) designed so biofilm
could adhere to both the outer surface and the central spaces within
the ring. To remove biofilm material with incorporated polyphosphate,
the system was backwashed once a week with pressurized air and water. Removal of biomass from the central spaces of the Kaldnes elements was
not efficient, leading to complete clogging of these spaces. The
preceding FISH analysis of the biofilm structure as described below
revealed no visual difference in the composition and spatial organization of the main microbial populations in the upper parts of
biofilms originating from the external substratum surface and from the
biofilm of clogged central spaces. Therefore, elements filled
completely with biogenic material were chosen for microsensor measurements and FISH.
Microsensor measurements.
To allow measurements during
reactor operation, Kaldnes elements with biofilm were transferred
during the initial filling period from the reactor to a separate
750-cm3 flow chamber coupled to the recirculation
of the reactor. Microsensors were inserted through small holes
in the top lid that were closed with stoppers during the nonaeration
period. Vertical concentration microprofiles in the biofilm were
measured for oxygen with Clark-type microsensors (45) and
for ammonium, nitrite, and nitrate with potentiometric ion-selective
microelectrodes of the LIX type (15) as described
previously. At least 20 profiles were measured for each parameter at
different times covering the whole course of a treatment cycle.
Measurements were distributed over four cycles to check for the
similarity of conditions on different days of operation.
Rate calculations.
Due to the periodic changes in the
process conditions, the microprofiles measured in situ do not represent
a steady-state situation. Therefore, in the case of nitrate, profiles
were corrected to allow the application of a one-dimensional
diffusion-reaction model for calculation of specific volumetric rates
of net consumption or production. In each nitrate profile, the first
value measured in the bulk water was set to t = 0. Then
for each depth, the concentration change over time was calculated from
two subsequent profiles. The resulting slope was used to correct the
time-dependent change of concentration points at t > 0 in each profile by linear interpolation. In that way, every profile was
corrected for the dynamics of concentration changes leading to the
elimination of transience. The correction procedure just described
influenced the absolute values of concentration in the deeper biofilm,
but did not change the shapes of the profiles. The
correction-of-profile data were not applied to oxygen profiles, because
their appearance and the stability of bulk values throughout the oxic
period of the process indicated a clear steady-state situation with
respect to oxygen.
Volumetric nitrification rates were calculated by applying a
one-dimensional diffusion-reaction model to the corrected data. Each
profile results from a combination of production (P),
consumption (C), and diffusive transport, as described by
Fick's second law of one-dimensional diffusion, which under
steady-state conditions [
c(z, t)
t = 0)] can be written as P
C =
Ds ·
2c(z,t)/
z2,
where DS is the effective diffusion
coefficient, c is the solute concentration,
z is depth, and t is time. Assuming a zero
order reaction, volumetric net production was subsequently calculated by quadratic regression for each depth (38).
DNA extraction.
DNA was extracted from native biofilm
samples stored at
70°C with the FastDNA-Extraction kit for soil
(Bio 101, Carlsbad, Calif.), as described in the manufacturer's
instructions. The quality of DNA was checked by agarose (1%
[wt/vol]) gel electrophoresis.
16S rDNA analysis.
A 1-kb fragment of the 16S rDNA
gene was amplified with the complement of probe NOLI191
(43) as the forward primer and the unlabeled probe Nso1225
(35) as the reverse primer. The following reaction mixture
was used: 50 pmol of each primer, 2.5 µmol of each deoxynucleoside
triphosphate (dNTP), 1× PCR buffer, 1 U of SuperTaq DNA polymerase (HT
Biotechnology, Cambridge, United Kingdom), and 50 to 100 ng of template
DNA. The mixture was adjusted to 100 µl with sterile water. PCR was
performed with an Eppendorf Mastercycler (Eppendorf, Hamburg, Germany)
with 35 cycles with hot start. The annealing temperature of 56°C for
the primer set was determined in previous PCRs run at different
temperatures. After checking an aliquot of the PCR product by agarose
gel electrophoresis, the DNA was directly ligated into the pGEM-T
vector (Promega, Mannheim, Germany) according to the manufacturer's
instructions and subsequently transformed to competent high-efficiency
Escherichia coli cells (strain JM109; Promega, Mannheim,
Germany). White and blue screening was used to screen for recombinant
transformants. Inserts of positive clones were analyzed for redundancy
by amplified rDNA restriction analysis (ARDRA) (44).
One representative clone was sequenced for each distinct fragmentation
pattern by Taq Cycle sequencing with the PCR primers or
primers M13uni and M13rev on a model ABI 377 sequencer (PE Corporation,
Norwalk, Conn.). The sequences were checked for chimera formation with
the CHECK_CHIMERA software of the Ribosomal Database Project
(32). Sequences were aligned and analyzed by use of the
ARB software package (Technical University Munich, Munich, Germany)
according to the last release of the 16S rDNA sequence database of
December 1998 as well as individually added sequences of recent
publications. Trees were calculated for the clones and selected related
sequences following the suggestions of Ludwig et al. (31).
For tree calculation, maximum-parsimony, distance matrix, and
maximum-likelihood methods were used, and the results were combined in
a consensus tree.
Probe design.
Based on the newly retrieved and
published sequences of the Nitrosomonas
oligotropha lineage (40), a probe was designed by using the PROBE_DESIGN tool of ARB. The dissociation
temperature of the probe was determined by hybridization with a pure
culture of Nitrosomonas ureae isolate Nm10 at formamide
concentrations ranging from 0 to 60%. Analysis was done by confocal
laser-scanning microscopy (CLSM) and image analysis as described
elsewhere (13). The specificity of the probe was checked
against the ARB database and experimentally tested under the optimal
hybridization conditions with the strains listed in Table
1.
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TABLE 1.
Organisms used for determination of
Td, their sequence at the target region, and
hybridization results with probe Nmo218
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FISH.
Complete substratum elements with adhering biofilm
were fixed with fresh 4% paraformaldehyde solution and alternatively
with ethanol, washed with phosphate-buffered saline (PBS), and stored in PBS-ethanol (1:1) at
20°C until further processing (1, 33). After freezing and removal of the plastic material, radial biofilm sections with a thickness of 14 µm were prepared at
18°C, immobilized on gelatin-coated microscope slides, and dehydrated in an
ethanol series (50). In situ hybridizations of cells in the biofilm were performed with fluorescently labeled, rRNA-targeted oligonucleotide probes according to the method of Manz et al. (33). The probes and conditions used are listed in Table
2. Probes labeled with the
sulfoindocyanine dyes Cy3 and Cy5 were obtained from Interactiva (Ulm,
Germany) and Biometra (Göttingen, Germany). In cases in which
stringency conditions did not allow simultaneous hybridization with
several probes, multiple probe hybridization was performed in
subsequent steps by first hybridizing with the probe of higher
stringency (58). The biofilm was additionally stained with
4', 6'-diamidino-2-phenylindole (DAPI) after the hybridization step
with a solution of 1 mg liter
1 for 10 min or
100 mg liter
1 for 10 s for the purpose of
polyphosphate staining (23). Samples were analyzed by
standard epifluorescence microscopy on a Zeiss Axioplan II microscope
and by CLSM on a Zeiss LSM 510 microscope (Carl Zeiss, Jena, Germany).
Quantification of AOB and NOB.
Total AOB abundance was
quantified by microscopical counting of cells hybridized with probes
Nso1225 and Nso190 in several fields of view along a 50-µm-thick
horizontal layer up to a biofilm depth of 600 µm. Distinct
populations of AOB were counted after hybridization with probes NEU and
NOLI191. Quantification of NOB was done by CLSM as previously described
(48); i.e., optical sections with a defined thickness of
0.6 µm were scanned, and by determining the signal area and
subsequent multiplication with a volume-specific cell abundance, the
cell number for a given volume was calculated. Thorough calibration for
NOB quantification was performed by counting DAPI-stained cells in
various scanned fields of view (n = 30), leading to
volumetric indices with a 95% confidence interval of ±7%. Results
with all probes used for quantification were corrected for nonspecific
binding according to results with probe NON338 as a negative control.
For quantitative population analysis with FISH, means and medians were
calculated to describe the distribution of the AOB and NOB populations.
Analysis of amoA sequences.
To supplement
results from FISH and the specific 16S rDNA library, comparative
sequence analysis of biofilm-derived 491-bp fragments of the ammonia
monooxygenase gene (amoA) was performed as previously
described (42). Amplificates of amoA were
separated according to their GC content by agarose gel retardation as
described by Schmid et al. (47).
Nucleotide sequence accession number.
The 16S rDNA
partial sequences obtained in this study are available from the EMBL
nucleotide sequence database under accession no. AJ297415 to AJ297419.
The amoA partial sequences appear under accession no.
AF293065 to AF293075 and AY007575.
 |
RESULTS |
Functional analysis.
Concentrations of the solutes measured
by microsensors in the bulk liquid of the measuring setup
closely reflected the bulk liquid composition in the
reactor as determined independently by online monitoring (data
not shown).
During the nonaeration period, oxygen could be detected in neither the
bulk water nor the biofilm at any time. During the aeration period of
the process, the biofilm was supplied with oxygen at 227.8 ± 5.4 µM (mean ± standard deviation [SD], n = 16),
corresponding to 80.2% ± 1.9% air saturation. Oxygen penetration into the biofilm was limited to a depth of 200 µm (Fig.
1), leaving substantial parts of the
biofilm anoxic during the whole treatment. The average areal oxygen
uptake remained stable throughout the oxic period at 0.84 ± 0.05 µmol cm
2 h
1
(mean ± SD, n = 16). Neither the penetration
depth nor the slope through the diffusive boundary layer was
significantly altered during the oxic period (Fig. 1).

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FIG. 1.
Representative examples of vertical concentration
microprofiles of oxygen, nitrate, and nitrite measured in biofilm at
different times of the reactor cycle. Numbers refer to the time in
minutes after start of the treatment cycle (start of aeration,
t = 180 min).
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With ammonium, nitrate, and nitrite, absolute concentrations showed a
certain variability, but the shapes and time courses of profiles
between different cycles were similar. A strong initial decrease of
ammonium directly after filling from 2,300 µM (t = 25 min) to 950 µM (t = 60 min) could be observed in the
biofilm, analogous to the decline within the bulk water in the first 60 min (profiles not shown). Later, the concentration of ammonium decreased less but continuously up to the end of the treatment cycle to
800 µM. The concentration in the biofilm followed this pattern.
Because no gradients of ammonium were observed above or within the
biofilm, ammonium uptake of the whole biofilm or of any specific layer
could not be quantified.
Production of nitrate during oxic conditions was restricted to a narrow
surface layer of about 200 µm, causing an accumulation of nitrate in
the bulk water of up to 230 µM in the final period of the treatment
(Fig. 1). The highest concentration of nitrate measured in the
productive layer was 260 µM. During the following nonaeration period
(after draining and refilling the system), the remaining nitrate was
detected up to a concentration of 200 µM in the deeper biofilm zones,
but it continuously decreased during the anoxic period. At the
beginning of the aeration (t = 180 min), no nitrate
from the previous treatment cycle was left in the biofilm (Fig. 1). The
shape of nitrate profiles supported a denitrifying activity in the
deeper biofilm layer. Nitrite accumulated during aeration up to 75 µM. In the second half of the aeration treatment period, an even
stronger local production of nitrite occurred in the deeper biofilm
layers at a depth of 600 to 700 µm, which was probably due to
denitrification, with concentrations of more than 90 µM (Fig. 1).
During the aeration period, there was a conspicuous delay in the first
occurrence of both nitrite and nitrate compared to the onset of
aeration. Detectable amounts of both solutes (>1 µM) were measured
first at t = 270 min, i.e., 90 min after onset of aeration.
A nitrogen balance based on nitrification products (300 µM),
remaining ammonium (800 µM), and an assumed stripping and
incorporation into bacterial biomass of 25% (61)
indicates an unresolved N loss of about one-third.
Calculation of nitrate production.
Volumetric nitrate
production rates were separately estimated for the productive surface
(depth of 0 to 200 µm) and the deeper biofilm (300 to 600 µm) from
profile data measured in four different batch runs. The deeper layer
showed some denitrifying activity up to about 1.0 µmol
cm
3 h
1 at
t = 360 min, evolving together with nitrifying activity
in the upper layer. The nitrate production in the surface layer during aeration reached maximum estimated rates of 1.7 µmol
cm
3 h
1 (corresponding
to 0.03 µmol cm
2 h
1)
and thus accounted for about 7% of the oxygen uptake at the end of the
process (Fig. 2).

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FIG. 2.
Volumetric net production and consumption of nitrate at
the biofilm surface (0 to 200 µm [ ]) and in the deeper biofilm
(300 to 600 µm [ ]) during the reactor cycle. Data points
originate from measurements of nitrate microprofiles of four different
batch runs. For details of calculations, see text.
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Broad-scale community structure.
Among all phylogenetic groups
tested, four groups dominated the biofilm community, as shown by FISH:
(i) members of the gram-positive bacteria with high DNA G+C content
(GPBHGC), which were mainly coccoid cells forming loose
aggregates; (ii) members of the
-proteobacteria, forming dense
layers at the very surface and dense globular aggregates mostly
located within the upper 200 µm; (iii) a population morphologically similar to the GPBHGC, with cells typically
arranged in tetrads, that hybridized with probes ALF968, ALF1b, and
GAM42a, but not with probes for subgroups of the
-proteobacteria
(Fig. 3A), leaving their phylogenetic affiliation as yet unresolved; and (iv) members of
the phylum Nitrospira (see below). Other phylogenetic groups together did not account for more than 20% of the microbial community in the biofilm (data not shown). The vast majority of all cells were
located in the upper 300 µm of the biofilm, whereas in the deeper,
permanently anoxic layers, only a few cell aggregates could be detected
occasionally.

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FIG. 3.
Confocal laser-scanning micrographs of vertical
thin sections of biofilm as hybridized with different fluorescent
oligonucleotide probes. (A) Overview of the biofilm surface hybridized
with ALF968 and HGC1351 (in green and red, respectively). (B)
Aggregates of -subclass AOB as hybridized with Nso1225 (green) and
NOB of the genus Nitrospira (Ntspa662, red). (C)
Clustered aggregates (arrows) of members of the N.
communis lineage (NmII, red) among the population -subclass
AOB (Nso1225, green). Colocalization of the two probes results in a
yellow color. (D) Aggregates of members of the N.
europaea lineage as hybridized with probe NEU (green) and of
the N. oligotropha lineage as hybridized with probe
NOLI191 (red). (E) Colocalization of signals after hybridization with
probes specific for the -subclass AOB (Nso1225, green) and the
N. oligotropha lineage (Nmo218, red); the insert
shows a big aggregate as hybridized with probes Nso1225 (green) and
NOLI191 (red). (F) Orthogonal representation of a dense
assemblage of Nitrospira sp. as hybridized with probe
Ntspa662. Scale bars are 50 µm (A, B, D, and E), 25 µm (C), and 5 µm (insert in panels E and F), respectively. Dashed lines indicate
the surface of the biofilm exposed to the wastewater.
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Additional staining with DAPI in high concentrations, indicating
polyanionic inclusions by yellow fluorescence (23), was exclusively colocalized with hybridization signals for
GPBHGC. However, only a fraction of the GPBHGC
population was stained yellow with DAPI.
AOB community structure.
A common problem for the
quantification of nitrifying bacteria is the formation of dense
aggregates resulting in a typical patchy distribution of AOB and NOB
(Fig. 3). Therefore, neither normal distribution of values nor
homogeneity of variances is given throughout the biofilm. For that
reason, the median may be a better representative of cell densities
than the mean and will be given in the following sections. To allow
comparison with other studies, however, both means and medians are
displayed in Fig. 4.

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FIG. 4.
Depth distribution of -subclass AOB (A), of
populations affiliated with different lineages of the genus
Nitrosomonas (B), and of the NOB
Nitrospira spp. (C) in the biofilm investigated. Numbers
are given as volume-specific abundances. Cumul, cumulative. Note the
different scales of the ordinates.
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The globular aggregates hybridizing with probe BET42a were shown to
belong to the AOB of
-proteobacteria by FISH with probes Nso1225 and
Nso190 (Fig. 3B). The abundance of AOB was highest at the biofilm
surface (Nso1225, 2.9 × 109
cm
3; Nso190, 2.0 × 109 cm
3) and declined
below 1 × 108 cm
3
within the first 200 µm. A cumulative mean of 95% of all AOB could
be detected within the first 200 µm (Fig. 4A). A few single aggregates of
-ammonia oxidizers occurred in the deeper biofilm as
well, but the abundance in these layers on average was very low.
Hybridization with probes Nsm156 and Nsv443 revealed that the complete
AOB community consisted of members of the genus
Nitrosomonas. Within this genus, three different subgroups
of AOB were detected. The smallest fraction (which was not further
quantified) belonged to the Nitrosomonas communis lineage
(40) of
-subclass AOB, as identified by hybridization
with probes Nso1225 and NmII (Fig. 3C). They formed small aggregates
and were restricted to the upper 100 µm. The two dominant
subpopulations showed distinct distribution patterns. One population
belonged to the Nitrosomonas europaea lineage of
-subclass AOB (40), as identified by hybridization with
probes Nso1225, Nsm156, and NEU (Fig. 3D). Hybridization with Nse1472
or NmV resulted in no signals, indicating that the population is not
identical to N. europaea or Nitrosococcus
mobilis. The second population hybridized with Nso1225 and NOLI191
(Fig. 3D and E), a probe that had been designed for the N. oligotropha lineage (40) based solely on the sequence
of N. ureae (43). Both groups together
accounted for from 55 to 100% of
-subclass AOB hybridizing with
probe Nso1225 in the upper 200 µm of the biofilm. At the surface, 22 and 33% of Nso1225-positive cells hybridized with probes NEU and
NOLI191, respectively. At a depth of 200 µm, about 90% of
Nso1225-positive cells hybridized with probe NOLI191, whereas the
abundance of the N. europaea lineage declined to
less than 10% (Fig. 4B). No signals were detected after hybridizations
with probe NmIV specific for Nitrosomonas cryotolerans.
AOB-specific PCR.
Because hybridization with a single
probe is sometimes not sufficient to prove the identity of a given cell
(2), a specific PCR and cloning strategy was applied
to support the occurrence of populations affiliated with the
N. oligotropha lineage within the biofilm. From the 26 clones analyzed by ARDRA, 10 different restriction patterns were
obtained. Three of the patterns, representing a total of 13 clones,
were indicative of sequences most similar to
Nitrosomonas isolate JL21 (55), a member
of the N. oligotropha lineage (Fig.
5). Two patterns, representing a total of
eight clones, belonged to sequences most similar to Nitrosomonas
communis Nm2. The remaining five clones with different ARDRA
patterns represented single sequences not related to the genus
Nitrosomonas. The amplification of these sequences and of
the ones similar to Nitrosomonas communis was due to
insufficient primer discrimination under the conditions chosen.

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FIG. 5.
Phylogenetic tree of the genus
Nitrosomonas inferred from comparative analysis of 16S
rDNA sequence data. The accession numbers of the published
sequences used are given in the tree. Sequences with accession no.
AB000701, AB000702, AJ005546, M96399, M96402, M96403, and Z46987
represent the N. europaea lineage, and sequences with
accession no. AJ003777, M96400, Z46990, Z69091, and Z69097 represent
the N. marina lineage. The numbers of clones with
identical ARDRA patterns for each sequence are given in parentheses.
Phylogenetic reconstruction is based on a maximum-likelihood tree
calculated from 950 informative positions with a genus-specific 50%
positional variability filter. Tree topology was tested by distance
matrix and maximum-parsimony methods, and a consensus tree was drawn.
Multifurcations connect branches for which a relative order could not
unambiguously be determined by the different treeing methods used.
Bootstrap values (100 cycles) refer to the maximum-parsimony tree.
Values smaller than 80% were omitted. The sequence of N.
oligotropha isolate Nm45 was added to the consensus tree by the
ARB maximum-parsimony method without changing the tree topology. The
bar represents 10% estimated sequence divergence.
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Design and application of probe Nmo218.
The sequence of probe
NOLI191 differs from the target sites of most of the recently reported
16S rRNA sequences of the N. oligotropha lineage (42,
52, 55). Furthermore, the probe hybridizes to organisms (e.g.,
Pseudomonas lemoignei) not belonging to the intended target
group. Therefore, we designed probe Nmo218 encompassing the
whole N. oligotropha lineage (Fig. 5). The probe sequence
and binding sites of target and nontarget organisms are displayed in
Table 1. The dissociation temperature of the probe was 40.1 ± 1.7°C, and the optimal formamide concentration in the hybridization
buffer was 35%. When applied under these conditions, probe Nmo218 did
not hybridize with any negative controls, except for Nitrosomonas
cryotolerans and Nitrosomonas aestuarii (Table 1). (The
sequences of five clones with identical binding sites to N. cryotolerans or N. aestuarii might also not be
discriminated.) The occurrence of N. cryotolerans can,
however, be ruled out by parallel use of probe NmIV. Hybridization of
probe Nmo218 to the biofilm resulted in a picture similar to that with
probe NOLI191 (Fig. 3D and E). However, simultaneous hybridization with
both probes revealed a certain number of organisms only hybridizing with either of the two probes. Cells of N. aestuarii
hybridized with probe Nmo218 (Table 1), but not with probe NOLI191.
Consequently, cells showing this hybridization pattern might be related
to N. aestuarii.
AOB diversity assessed by comparative amoA sequence
analysis.
Specific amplification of the amoA gene
fragments from extracted biofilm DNA and subsequent separation by gel
retardation resulted in three clearly visible amoA bands.
All bands were excised and separately cloned and sequenced. A total of
12 amoA clones (4 from each band) were analyzed, which
represented five phylogenetically distinct
-subclass AOB (Fig.
6). Two clusters (representing two different bands), each containing four amoA sequences, were
found within the Nitrosomonas marina-N.
oligotropha lineages (which cannot clearly be distinguished by
using amoA sequences) (42). The third band
contained a higher diversity of amoA sequences. One
amoA clone was closely related to Nitrosomonas
communis. Another clone was affiliated with Nitrosococcus
mobilis, which could not be detected in the biofilm by FISH. The
two remaining amoA clones obtained from the third band
clustered together and formed an independent lineage not closely
related to any described AOB.

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|
FIG. 6.
Phylogenetic FITCH-Margoliash amoA tree
(using global rearrangement and randomized input order [7 jumbles])
showing the position of the 12 recovered biofilm sequences in relation
to described -subclass AOB (42). The bar indicates 10%
estimated sequence divergence. The root was determined with the
amoA sequences of the -subclass ammonia-oxidizing
bacteria (42). Cloned amoA sequences with
amino acid similarities >99% are represented by a single clone: the
number in parentheses indicates the number of clones for each
representative. Clones labeled with the prefixes B2, B3, and B4 were
obtained from different gel retardation bands.
|
|
NOB community structure.
The only NOB detected in the system
were of the genus Nitrospira, as identified by hybridization
with probes Ntspa712, Ntspa662, and NSR826 (Fig. 3B and F). Low numbers
of cells also hybridized with probe NSR1156. The abundance of
Nitrospira spp. in the upper 100 µm of the biofilm was
1.1 × 1011 cm
3 and
therefore was about 30 times higher than the abundance of
-subclass
AOB, as quantified with probe Nso1225. In comparison to the AOB, the
vertical distribution was broadened towards depth. Within the section
investigated, a 95% limit in cumulative (mean) abundance was reached,
although not before a depth of 400 µm, and the numbers were high even
in deeper layers of the biofilm (Fig. 4C).
Cell-specific nitrification rates.
The average cell density of
NOB in the upper 200 µm of the biofilm where nitrification was mainly
performed was 6.6 × 1010
cm
3. Because nitrate production in this layer
during aeration on average was 0.7 µmol cm
3
h
1, conversion rates were about 0.01 fmol of
nitrite cell
1 h
1 for
the final aeration period. Maximum rates were 0.025 fmol of nitrite
cell
1 h
1. Cell-specific
ammonia oxidation rates can only be roughly estimated based on nitrate
production rates. With the average abundance of AOB of 1.09 × 109 cm
3 in the upper 200 µm, mean conversion rates were at least 0.65 fmol of ammonium
cell
1 h
1 (maximum of
1.5 fmol of ammonium cell
1
h
1). However, because of the accumulation of
nitrite within the nitrification zone, this number is clearly an underestimate.
 |
DISCUSSION |
Biofilm activity and community structure.
In the biofilm
studied, biological phosphorus removal is combined with nitrogen
removal via nitrification and denitrification. Nitrification is
typically performed by distinct phylogenetic groups and will be
discussed later. For biological P removal, involvement of various
groups has been suggested: e.g., GPBHGC (12,
59), members of the genus Rhodocyclus (7, 8,
21), or a mixture of multiple species (34). The
high abundance of GPBHGC and the detection of DAPI-stainable
inclusions indicative of polyphosphate (23) in part of
this population strongly promote the first hypothesis for our system.
However, the fixation procedure used might have led to the
disappearance of polyphosphate granules (21), and
therefore PAO, especially among gram-negative bacteria, might
have been overlooked.
Denitrification cannot at all be assigned to a certain microbial
population, nor is it restricted to a certain zone of the biofilm.
During the anoxic period, the surface layers denitrify nitrate that has
been accumulated during the oxic period of the preceding cycle (Fig. 1
and 2) and by that contribute about 20% to the total N loss. During
the oxic period, the deeper parts of the biofilm remain anoxic and are
provided with nitrate via nitrification (Fig. 1). The contribution of
denitrification in the 300- to 600-µm-deep biofilm during the oxic
period to total N loss is about 15%. Because there are reports of
denitrifying PAO (28, 57) and because GPBHCG as
potential PAO were found in close proximity to nitrifying bacteria, the
source of nitrate, involvement of PAO in denitrification appears to be
possible. However, this cannot be proven based upon our data.
Competition for oxygen.
Both nitrification and phosphate
uptake require oxygen. Therefore, competition for oxygen between the
respective microbial populations during the aeration period is to be
expected. Microsensor data indicate that the nitrifying bacteria were
oxygen limited. Oxygen penetration was low, whereas ammonium was
present in excess during the whole process. The distribution of AOB and
NOB in general corresponds to the oxygen penetration depth, supporting
the findings of earlier studies (39, 50). The delayed
onset of nitrification after the start of the aeration and the
accumulation of nitrite despite the high abundance of NOB very likely
reflect the limited supply of oxygen. Due to their high
Km for oxygen, AOB and NOB are poor
competitors compared to heterotrophic bacteria (17, 41,
56). Thus, during the initial aeration period, oxygen is
taken up preferentially by heterotrophs as the PAO. As the phosphate
uptake rate declines with the ongoing aeration period (data not shown),
the stoichiometric oxygen demand of PAO metabolism decreases as well
(51). Consequently, during the course of the aeration
period, phosphate accumulation is most likely replaced by nitrification
in terms of oxygen consumption.
Nitrification rates.
The handling of concentration data to
estimate volumetric nitrate production rates (see Materials and
Methods) is based on two assumptions: (i) low lateral
heterogeneity of the concentration in the biofilm at a certain time and
(ii) slow dynamics of the concentration changes due to activity
compared to those due to diffusion (i.e., a pseudo-steady-state
situation). Structural analysis showed a certain lateral inhomogeneity
based mostly on the clustering of nitrifiers (Fig. 3B), but
inhomogeneity is low in the horizontal direction, and the resolution of
the measurements was not in the range of the cluster size. Therefore,
the first assumption is not violated. For a similar system
(36), it was shown that the time required to reach
equilibrium was 1.8 min in a biofilm with a thickness of 500 µm.
This is quite short compared to the overall cycle dynamics observed
here. Nevertheless, the second assumption may introduce some error,
especially in highly dynamic layers. The rates determined here should
therefore be regarded as best estimates.
The rates of both estimated cell-specific in situ ammonia oxidation and
nitrate production are on the order of magnitude of those calculated
for aggregates of a nitrifying fluidized bed reactor based on
microsensor measurements (48) and the ammonia oxidation
rate estimated by a process mass balance of a sewage treatment plant
(60). Unfortunately, the resolution of our measurements was too low to distinguish between the ammonia oxidation rate of the
surface layer (with the mixed nitrifying community) and that of the
deeper layer (with the N. oligotropha-like population). Also, the different activities of each of the individual AOB
populations in the surface layer or of individual cells within a
monospecies cluster cannot be resolved. Therefore, it has to be noted
that the cell-specific ammonia oxidation rate calculated here
represents an average value for a diverse assemblage of AOB consisting
of at least three different populations.
Community structure of AOB.
The combined approach of FISH, 16S
rDNA, and amoA analyses led to the unexpected but
consistent finding that there were several different AOB populations
occurring in close spatial vicinity. In contrast, previous studies in
biofilms and activated sludge usually reported a single population
dominating the system, e.g., populations related to N. europaea (39, 50), Nitrosococcus mobilis
(22), or members of the genus Nitrosospira
(39, 49). This raises the question of what mechanisms
allow for the coexistence of the different AOB populations in the
biofilm studied here.
N. communis-like AOB were found only within the first 100 µm at the biofilm surface and only in low abundance. Isolates of this
lineage originally were obtained from soils (24) and were recently also detected in activated sludge and biofilm systems (42). Unfortunately, the lack of ecophysiological data
about N. communis and its exclusive occurrence in the same
zone with both members of the N. europaea- and N. oligotropha-like AOB leave the specific adaptation of N. communis-like AOB to our system unresolved.
The second population was identified as members of the N. europaea lineage, although these bacteria were not identical to N. europaea itself. The low number of amoA
sequences analyzed allows for some hidden diversity, because several
clones might be represented by one band in the gel retardation. The
N. europaea-like population detected by FISH thus might be
unrepresented by any amoA clone. Members of this
phylogenetic cluster, like, e.g., N. europaea and N. eutropha, are typically isolated from activated sludge systems
(24), and the maximum substrate conversion rates for
N. europaea are high compared to those of other strains of AOB (41). Pure culture and chemostat experiments revealed
low substrate affinities for N. europaea with
Km
(NH4+) values in the range of
0.4 to 7 mM (41) and 0.88 to 1.96 mM (29),
respectively. The same is true for oxygen affinity, with Km (O2) values
between 6.9 and 17.4 µM (29). While ammonium concentrations in the biofilm exceeded most of the reported
Km values, oxygen limitation for N. europaea-like AOB is obvious. Between a depth of 100 and 200 µm,
the oxygen concentration decreases from 33.8 ± 5.45 µM to
7.0 ± 1.01 µM (mean ± SD, n = 15).
Consequently, N. europaea-like AOB virtually disappear
within these layers (Fig. 4B). Here, the biofilm is dominated by
N. oligotropha-like AOB with an abundance of 1 × 108 to 2 × 108 cells
cm
3 down to a depth of 400 µm. Based on 16S
rDNA sequence analysis, members of the N. oligotropha lineage (also referred to as
Nitrosomonas cluster 6a [26, 54]) have
recently been detected in freshwater and brackish environments
(52, 53), terrestrial habitats (26, 54), and
activated sludge (42, 55). This suggests high
physiological versatility and ecological importance. Isolates of this
lineage are sensitive to ammonium concentrations exceeding 10 to 60 mM (24, 53, 55), show low Km
(NH4+ plus
NH3) values, and possess urease activity
(53). These features support adaptation of the N. oligotropha lineage to low substrate concentrations. Although no
kinetic data with respect to oxygen are available, this might also
imply high affinity towards oxygen. Lower
Km (O2) values of
the N. oligotropha-like AOB than the values reported for
N. europaea-related AOB could be responsible for the
outcompetition of the latter at the oxic-anoxic transition zone in the
biofilm. At the biofilm surface, however, both populations were found
to coexist in almost equal abundance. Assuming higher maximum substrate
conversion rates for N. europaea-like AOB (41), they should be able to outcompete other AOB in this zone. For explanation of the co-occurrence, the dynamics of the system have to be
taken into account (i.e., the metabolic activity of the populations
might be separated in time). In the initial aeration period, N. oligotropha-like AOB in particular might be active, because, as
suggested above, their higher oxygen affinity allows competition for
oxygen with the highly active heterotrophic PAO. In the late oxic
period, when oxygen uptake of the heterotrophic PAO decreases, N. europaea-like AOB could become more active. Their relatively high
maximum substrate conversion rate might compensate for their
time-limited activity and contribute to the successful establishment of
this population in the biofilm. It has been shown for biofilm
populations of AOB that the abundance is likely not to be affected by
short starvation periods (i.e., a few days). Furthermore, recovery for
both growth and activity of AOB from starvation is very rapid. This
effect is likely to be coupled to high densities of AOB, as found in
biofilms, and is probably due to cell-cell signaling (4).
The high cell density and occurrence in dense clusters we found are in
agreement with this hypothesis. Based on this strategy, it can be
argued that even merely short-term activity would allow AOB to persist
in the biofilm.
In addition, there are reports about an anoxic type of metabolism in
N. europaea and N. eutropha when electron
acceptors other than oxygen are used (6). The ability to
survive or even thrive during anoxic conditions is, however, likely to
differ among the three AOB populations. Therefore, the nonaeration
period of the reactor cycle might be another factor to support a mixed
community of AOB. However, alternative hypotheses explaining the
coexistence are possible. Detection of AOB populations in situ does not
prove their recent activity (60). It can be speculated
that the ability to maintain the ribosome content during inactive
periods might be stronger in the N. oligotropha lineage than
in the N. europaea lineage. This would cause N. europaea-like AOB to become more rapidly undetectable by FISH in
deeper layers of the biofilm compared to the results with N. oligotropha. Currently, we have no evidence in favor of this
hypothesis, but future studies including the detection of local
activity (e.g., by use of microautoradiography) (30) might
help to support or reject this hypothesis. By amoA analysis,
three more clones could be identified, related to Nitrosococcus mobilis (B3-5) and not closely affiliated with any isolated
Nitrosomonas strain (B3-3). Because neither population
could be identified by FISH, we assume the populations were either low
in numbers or were in a dormant state.
NOB population.
Using different probes for NOB, the existence
of a certain population of Nitrospira spp. could be proven,
whereas Nitrobacter spp. were not detected. This is in
agreement with several other culture-independent studies of engineered
systems (10, 22, 39, 48, 49, 61). Analysis of the probe
match pattern in the current data set by the software package ARB
(Technical University Munich, Munich, Germany) showed that it fits a
cluster of closely related sequences in the genus Nitrospira
(strains with accession no. Y14636 to Y14643) retrieved from a
nitrite-oxidizing sequencing batch reactor by Burrell et al.
(10). The NOB population in our system is thus likely to
be affiliated with this particular cluster of the genus
Nitrospira. It might be speculated whether this cluster
possesses common functional features leading to a competitive advantage
under the periodically changing conditions typical for sequencing batch
reactors. The cell densities of Nitrospira spp. found in
this study are on the order of magnitude of those reported from a
purely nitrifying fluidized bed reactor (48). However, the
abundance is 1 order of magnitude higher than that of the AOB. The
question remains of how such a high abundance is supported, when the
substrate turnover is speculated to be low (48).
Conclusions.
Through the combination of microsensor
measurements and molecular methods, it was possible to resolve the
structure and activity of the nitrifying community in a complex,
P-removing biofilm. Some first insights were obtained into the
mechanism that allows for the coexistence of different populations of
AOB in the same biofilm, i.e., separation of their distributions in
space and separation of their activities in time. The design of probe
Nmo218 specific for the N. oligotropha lineage will enable
in situ detection and quantification of N. oligotropha-like
AOB in future studies to collect more information about their natural
abundance and ecology.
 |
ACKNOWLEDGMENTS |
This study was supported by the German Research Foundation (SFB
411, Project A1
Research Center for Fundamental Studies of Aerobic
Biological Wastewater Treatment, Munich, Germany) and by the
Max-Planck-Society.
We are indebted to Patrik Arnz for the maintenance of the reactor and
Jakob Pernthaler for image analysis for melting temperature determination. Gabriele Eickert, Anja Eggers, and Vera Hübner are
acknowledged for the preparation of oxygen microeletrodes, and Dirk de
Beer and Olivier Pringault are acknowledged for valuable comments on
the handling of microsensor data. Harold L. Drake is acknowledged for support.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Molecular
Ecology Group, Max Planck Institute for Marine Microbiology,
Celsiusstraße 1, D-28359 Bremen, Germany. Phone: 49 421 2028 836. Fax: 49 421 2028 690. E-mail: agieseke{at}mpi-bremen.de.
 |
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