Microbes and Environments
Online ISSN : 1347-4405
Print ISSN : 1342-6311
ISSN-L : 1342-6311
Regular Paper
Quantification and Phylogenetic Analysis of Ammonia Oxidizers on Biofilm Carriers in a Full-Scale Wastewater Treatment Plant
Yuki TsuchiyaTatsunori NakagawaReiji Takahashi
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Supplementary material

2020 Volume 35 Issue 2 Article ID: ME19140

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Abstract

Biofilm carriers have been used to remove ammonia in several wastewater treatment plants (WWTPs) in Japan. However, the abundance and species of ammonia oxidizers in the biofilms formed on the surface of carriers in full-scale operational WWTP tanks remain unclear. In the present study, we conducted quantitative PCR and PCR cloning of the amoA genes of ammonia-oxidizing bacteria and archaea (AOB and AOA) and a complete ammonia oxidizer (comammox) in the biofilm formed on the carriers in a full-scale WWTP. The quantification of amoA genes showed that the abundance of AOB and comammox was markedly greater in the biofilm than in the activated sludge suspended in a tank solution of the WWTP, while AOA was not detected in the biofilm or the activated sludge. A phylogenetic analysis of amoA genes revealed that as-yet-uncultivated comammox Nitrospira and uncultured AOB Nitrosomonas were predominant in the biofilm. The present results suggest that the biofilm formed on the surface of carriers enable comammox Nitrospira and AOB Nitrosomonas to co-exist and remain in the full-scale WWTP tank surveyed in this study.

Nitrification, the biological oxidation process by which ammonia is converted to nitrite then nitrate, is an important nitrogen removal step in wastewater treatment plants (WWTPs). Nitrification is considered to be driven by two phylogenetically different groups of chemolithotrophic microorganisms: ammonia-oxidizing bacteria and archaea (AOB and AOA, respectively) and nitrite-oxidizing bacteria (NOB). A complete ammonia oxidizer (comammox) that converts ammonia to nitrate in one cell was recently discovered in the NOB genus Nitrospira in enrichment cultures of biofilms that formed on the wall of a hot-water pipe (Daims et al., 2015) and on the trickling filter of an aquaculture system (van Kessel et al., 2015). AOB and AOA are key microorganisms influencing the rate of nitrogen removal in WWTPs due to their slow growth rates (Limpiyakorn et al., 2005; 2013). Moreover, comammox Nitrospira was detected in the activated sludge of several WWTPs using high-throughput sequencing (Pjevac et al., 2017; Wang et al., 2018; Roots et al., 2019) and is recognized as an important member for nitrification in WWTPs (Chao et al., 2016; Annavajhala et al., 2018). The community composition of ammonia oxidizers (AOB, AOA, and comammox Nitrospira) and their influence on nitrification in WWTPs are being highlighted worldwide.

Advanced systems using activated sludge, membrane bioreactors, or biofilm carriers are adopted by many full-scale WWTPs for nitrogen removal from wastewater. In these systems, the biofilm carrier system has potential to achieve efficient (low cost and quick) nitrification in WWTPs (Wang et al., 2005; Chung et al., 2007) because biofilm-forming AOB exhibit higher affinity for ammonium and faster recovery after ammonium starvation than planktonic cells (Batchelor et al., 1997; Bollmann et al., 2005). Moreover, other studies at a laboratory-scale reactor and pilot plant using biofilm carriers demonstrated that biofilm carriers successfully retained AOB and easily maintained nitrification activity (Welander et al., 1997; Mishima et al., 1998; Young et al., 2016). However, limited information is currently available on ammonia oxidizers (AOB, AOA, and comammox Nitrospira) on biofilm carriers in operational full-scale WWTPs. Thus, detailed investigations on the abundance and phylogeny of ammonia oxidizers on biofilm carriers will lead to a better understanding of the ecology of ammonia oxidizers in WWTPs. Furthermore, useful information will be obtained to resolve nitrification failure (Kim et al., 2006; Tang and Chen, 2015), which sometimes occurs in WWTPs.

In the present study, we conducted quantitative PCR (qPCR) and sequencing of the amoA genes of each ammonia oxidizer (AOB, AOA, and comammox) on biofilm carriers collected from an advanced full-scale operational WWTP in the Kanto area of Japan, and discussed the contribution of these ammonia oxidizers to nitrification in the WWTP.

Materials and Methods

Sample collection

Biofilm carrier samples were collected from an advanced WWTP in the Kanto area of Japan on 23 February, 2018. This particular WWTP serves a population of approximately 2,000,000 and treats 800,000 m3 of full-scale wastewater daily. The plant consists of an anoxic tank (AO-tank), microaerophilic tank (MA-tank), and aerobic tank (A-tank) in that order for the treatment of sewage (Fig. 1). Ring-shaped elements (approximately 4‍ ‍mm in diameter and 5‍ ‍mm in length) made of polypropylene (Bio-Tube, JFE Engineering) are suspended in the A-tank to act as a biofilm carrier (BC). Some of the treated solution from the A-tank is circulated into the AO-tank.

Fig. 1.

Schematic illustration of the full-scale WWTP in the present study. Solution containing activated sludge was collected from an anoxic (AO) tank and microaerophilic (MA) tank. A solution containing activated sludge and biofilm carriers (BC) was collected from an aerobic (A) tank.

Approximately 100‍ ‍mL of solution containing BC was collected from the A-tank. Suspended activated sludge solution samples (100‍ ‍mL each) were also collected from the AO-, MA-, and A-tanks. These samples were brought back to the laboratory inside a cooler set at ca. 4°C. Immediately after arriving at the laboratory, activated sludge solution samples were centrifuged (8,000×g, 4°C, 10‍ ‍min) and the supernatant and sediment were separated. The supernatant was filtered (0.22 μm, Millex-GV: Merck Millipore) and used to measure the concentrations of NH4+, NO2, and NO3 ions and disolved saccharides and proteins. The sediment containing activated sludge was stored at –‍80°C until used for DNA extraction; these activated sludge samples contained planktonic cells. The BC sample was gently washed 3 times with the supernatant of the A-tank solution to remove extra activated sludge, and then stored at –80°C until used in the DNA extraction process.

Sample characteristics

The concentrations of NO2 and NO3 ions in the supernatant of the tank solution collected from the AO-, MA-, and A-tanks were measured by ion chromatography (Dionex ICS-1000). The identification of NO2 and NO3 peaks was conducted using external standard methods. The concentration of NH4+ was measured by the indophenol blue method (Sagi, 1966). The concentrations of dissolved saccharides and proteins were measured by the phenol-sulfuric acid method (Kochert, 1978) and Bradford method (Bradford, 1976), respectively. Light absorbance was measured using a spectrophotometer (U-5100; HITACHI). Each measurement was conducted in triplicate.

DNA extraction

The BC samples collected from the A-tank and activated sludge samples collected from each tank (AO, MA, and A) were precisely weighed (ca. 0.2‍ ‍g and 0.1‍ ‍g for BC and activated sludge, respectively), and DNA in the samples was then extracted with the ISOIL for Beads Beating Kit (Nippon Gene) according to the manufacturer’s instructions. Four carriers (ca. 0.2‍ ‍g containing ca. 0.04‍ ‍g of the biofilm) were broken with sterilized tweezers and directly used for DNA extraction. Extracted DNA was suspended in 50‍ ‍μL of TE buffer (attached in the ISOIL for Beads Beating Kit) and stored at –20°C until qPCR. DNA extraction was conducted in triplicate.

qPCR of AOB amoA, comammox amoA, and 16S rRNA genes

AOB amoA, AOA amoA, comammox amoA, and 16S rRNA gene copies were quantified by real-time PCR with the primers amoA 1F and 2R (Rotthauwe et al., 1997), GenAOA F and -R (Meinhardt et al., 2015), Ntsp-amoA 162F and 359R (Fowler et al., 2018), and EUB 926F and 1092R (De Gregoris et al., 2011), respectively (Table 1). Triplicate DNA samples were used for real-time PCR performed with the CFX 96 Real-Time System (Bio-Rad). The PCR mixture was prepared to a total volume of 25‍ ‍μL and contained 2‍ ‍μL of 10- to 50-fold diluted DNA sample, 5 pmol of each primer, and 12.5‍ ‍μL of the SYBR Premix Ex Taq kit (Takara Bio). The PCR program for the AOB amoA gene consisted of 94°C for 5‍ ‍min followed by 35 cycles at 94°C for 30‍ ‍s, at 55°C for 30‍ ‍s, and at 72°C for 30 s. The program for the comammox amoA gene was as follows: at 95°C for 3‍ ‍min followed by 35 cycles at 95°C for 10‍ ‍s, at 57°C for 30‍ ‍s, and at 72°C for 30 s. Regarding the 16S rRNA gene, the program was as follows: at 95°C for 5‍ ‍min followed by 35 cycles at 95°C for 15‍ ‍s, at 61.5°C for 15‍ ‍s, and at 72°C for 20 s. The specificity of qPCR products was checked by a melting curves analysis and agarose gel electrophoresis. Amplification efficiency ranged between 81 and 95% with R2 values higher than 0.990 for all calibration curves.

Table 1. PCR primers used in the present study
Target gene Primer name Nucleotide sequence (5′-3′) Position Reference
AOB amoA amoA-1F GGGGTTTCTACTGGTGGT 332–349 Rotthauwe et al., 1997
amoA-2R CCCCTCKGSAAAGCCTTCTTC 802–822
COMAMMOX amoA
(clades A and B, for qPCR)
Ntsp-amoA 162F GGATTTCTGGNTSGATTGGA 162–182 Fowler et al., 2018
Ntsp-amoA 359R WAGTTNGACCACCASTACCA 339–359
COMAMMOX amoA
(clade A, for PCR cloning)
COMA F TGCGGIGACTGGGAYTTC 154–171 Yu et al., 2018
COMA R AGATCATAGTGCTRTGICC 649–667
16S rRNA gene 926F AAACTCAAAKGAATTGACGG 908–926 De Gregoris et al., 2011
1062R CTCACRRCACGAGCTGAC 1981–1064

The copy number of the gene was calculated with a standard curve generated from a series of 10-fold dilutions (101–108) of the plasmid, with each containing cloned genes (the AOB amoA gene fragment of Nitrosomonas stercoris KYUHI-ST [Nakagawa and Takahashi, 2015], and comammox amoA of the environmental clone retrieved from the present study [clone name, BC-COMA15; Accession number in DDBJ, LC503646]). Plasmid DNAs were prepared using the TA cloning method as shown previously (Nakagawa et al., 2019). Briefly, plasmids containing the target genes were constructed by cloning PCR products into the TOPO vector using the TOPO TA Cloning Kit (Invitrogen). Plasmids were extracted using the Quantum Prep Plasmid Miniprep Kit (BioRad), and DNA concentrations were measured with the Qubit dsDNA HS Assay Kit and Qubit Fluorometer (Life Technologies).

The cell numbers of AOB, comammox, and total bacteria were calculated from the gene copy numbers obtained from qPCR (AOA was not detected; see Results and Discussion). The gene copy numbers of AOB amoA and comammox amoA per genome of the bacterial cell were assumed to be 2.5 and 1.0, respectively, based on the average copy numbers of the betaproteobacterial amoA gene (Norton et al., 2002; Wang et al., 2015; Wang et al., 2018) and genomic information on the comammox amoA gene (Daims et al., 2015; Wang et al., 2018). The cell number of comammox may be overestimated because comammox species that contain 2 copies of the amoA gene in one cell were also found (e.g. Candidatus Nitrospira nitrosa) (Camejo et al., 2017). The 16S rRNA gene copy numbers per genome of the bacterial cell was assumed to be 3.6 based on the average 16S rRNA gene copies found in cultured bacteria (Klappenbach et al., 2001; Limpiyakorn et al., 2005).

Cloning, sequencing, and phylogenetic analysis of AOB and comammox amoA genes

The amoA genes of AOB and comammox in the biofilm formed on BC samples were amplified by PCR using primer sets (as shown in Table 1) and Go Taq G2 Hot Start Master Mix (Promega) following the manufacturer’s instructions. PCR was performed at 95°C for 2‍ ‍min (for a hot start), then at 94°C for 2‍ ‍min followed by 33 cycles at 94°C for 30‍ ‍s, at 55°C for 30‍ ‍s, and at 72°C for 30‍ ‍s, and then at 72°C for 10‍ ‍min for the final extension. After agarose electrophoresis, amplified DNA fragments were cloned into the vector pCR2.1-TOPO with a TOPO TA PCR Cloning Kit (Life Technologies) following the manufacturer’s instructions. Positive colonies were directly amplified with the vector-specific primers M13F and M13R (Life Technologies). After checking the length of DNA using agarose gel electrophoresis, amplicons were purified with a QIA quick PCR purification kit (Qiagen) prior to sequencing. Both strands of PCR products amplified using the M13F and M13R primers were sequenced with a BigDye Terminator version 3.1 (Life Technologies) on a 3130xl Genetic Analyzer (Life Technologies), and connected into one sequence using MEGA7 (Kumar et al., 2016). The sequences obtained were compared with reference sequences in the NCBI database by the BLAST program. Sequences with 97% similarity were grouped into an operational taxonomic unit (OTU). Each representative OTU (ca. 400 bp) was aligned with CLUSTALW and used to construct a neighbor-joining (NJ) tree with MEGA7. Bootstrap values were assessed from 1,000 replications. To compare the richness of the AOB and comammox community, a rarefaction analysis was performed with Analytic Rarefaction v1.3 software (https://strata.uga.edu/software/index.html), and Good’s coverage value (Good, 1953) was calculated.

The amoA sequences of AOB and comammox in the present study were deposited in the DDBJ under accession numbers LC503692 to LC503740 (AOB) and LC503632 to LC503691 (comammox) (Table S1 and S2).

Statistical analysis

Differences in the concentrations of N-related ions and the abundance of the amoA and 16S rRNA genes among samples were verified using a one-way analysis of variance (ANOVA); multiple comparisons were performed using the Tukey-Kramer test in JMP v1.4 software (SAS Institute).

Results and Discussion

Characteristics of tanks in WWTP

The WWTP in the present study consisted of AO-, MA-, and A-tanks with suspended BC (in that order) for the treatment of full-scale sewage (Fig. 1). The water temperature of all tanks was 19.2–19.3°C. The pH of all tanks was 6.8–7.0. The dissolved oxygen (DO) concentrations in the AO-, MA-, and A-tanks were ca. 0, 1.3, and 6.0‍ ‍mg L–1, respectively. The dissolved saccharide concentration was ca. 4‍ ‍mg glucose equivalent L–1 for all tanks. Dissolved protein was not detected in any tank. The AO-tank had the highest NH4+ concentration, followed by the MA-tank, and then the A-tank (Fig. 2). NO2 and NO3 concentrations significantly increased (P<0.01) in the MA-tank and markedly in the A-tank (Fig. 2). These results suggest that nitrification occurred in the MA- and A-tanks. The dissolved inorganic nitrogen (DIN) concentration (NH4+, NO2, and NO3 concentrations combined) in the AO-tank (ca. 830‍ ‍μM) decreased in the MA- and A-tanks (ca. 570 and 270‍ ‍μM, respectively), suggesting that the (aerobic) denitrification process (Liu et al., 2018) and/or utilization of nitrogen also occurred in these two tanks.

Fig. 2.

Average concentrations of NH4+, NO2, and NO3 in anoxic (AO), microaerophilic (MA), and aerobic (A) tanks. Different letters above the columns indicate significant differences (P<0.05). SE represents the standard error.

Abundance of ammonia oxidizers and total bacteria

We quantified the copy numbers of the amoA genes and 16S rRNA gene in the biofilm formed on the surface of BC of the A-tank and in the suspended activated sludge of the AO-, MA-, and A-tanks using the qPCR method with specific primer sets (Table 1) and estimated the cell numbers of ammonia oxidizers and total bacteria (Fig. 3).

Fig. 3.

Average abundance of AOB (A), comammox (B), and total bacteria (C) in the unit wet weight of the activated sludge in AO-, MA-, and A-tanks and the biofilm on BC. Different letters above the columns indicate significant differences (P<0.05). The comammox in the activated sludge of the tanks was below the detection limit (shown as ND). SE represents the standard error.

The average abundance of AOB in the biofilm formed on the surface of BC was 3.4±2.2×107 cells wet-g–1, which was significantly (P<0.05) greater than that in the activated sludge of all tanks (ca. 0.5–1.3×106 cells wet-g–1) (Fig. 3A). The A-tank solution is continuously mixed and partially flows away. Under this condition, it is probably difficult for AOB in activated sludge to grow and remain in the tank due to slow growth. Biofilm formation on BC may be advantageous for AOB to remain in the tank, as reported in other studies (Chung et al., 2007; Chao et al., 2016).

Comammox with an average abundance of 8.2±0.79×107 cells wet-g–1 was detected in the biofilm on BC (Fig. 3B). This number was higher than that of AOB in the biofilm. Based on genomic and physiological analyses, comammox appeared to adapt to low concentrations of NH4+ (ca. 1‍ ‍mg or less NH4+-N L–1) and DO (ca. 1‍ ‍mg L–1) (Daims et al., 2015; Kits et al., 2017; Palomo et al., 2018). Therefore, comammox generally finds it challenging to compete with AOB when WWTP tanks are under eutrophic and/or aerobic conditions (Gonzalez-Martinez et al., 2016; Annavajhala et al., 2018; Roots et al., 2019). In the A-tank of the present study, the DO concentration (ca. 6‍ ‍mg L–1) was too high for comammox, whereas the NH4+ concentration was sufficiently low (ca. 1‍ ‍mg NH4+-N L–1). In the biofilm on carriers, an environment that is suitable for comammox (low concentrations of O2 and NH4+) may be formed, as suggested in other studies (Lawson and Lücker, 2018; Koch et al., 2019). Gradients of DO and NH4+ concentrations have been identified inside biofilms (Flemming et al., 2016; Satoh et al., 2006; Wang et al., 2016). Biofilms may generate a niche for comammox, leading to the co-existence of comammox with AOB under the tank condition. Further analyses of 1) the spatial distribution of comammox and AOB inside the biofilm on BC and 2) the profiles of DO and ion concentrations inside the biofilm are needed in order to obtain a more detailed understanding of the relationship between comammox and AOB in biofilms.

Comammox numbers in the activated sludge of all tanks were below the detection limit (Fig. 3B). Tank solution conditions were probably inadequate for comammox, as described above. In the A-tank, an excessive DO concentration (ca. 6‍ ‍mg L–1) was observed, whereas the NH4+ concentration was sufficiently low. In the AO and MA-tanks, an excessive NH4+-N (more than 1‍ ‍mg L–1) concentration was detected, whereas the DO concentration was sufficiently low. These conditions may negatively affect the growth of comammox outside the biofilm, resulting in the absence of comammox (or only a small number) in the activated sludge of the tanks.

The primer set of comammox amoA for qPCR used in the present study was designed to detect total comammox (clades A and B) (Fowler et al., 2018). A recent study reported that the comammox number might be overestimated using this primer set; extra bands in agarose gel electrophoresis and broad peaks in a melting curve analysis after qPCR were observed in some activated sludge samples (Beach and Noguera, 2019). In the present study, although weak extra bands were observed in agarose electrophoresis from BC samples, broad peaks were not detected in the melting curve analysis (Fig. S1). Thus, the primer-related overestimation of the comammox number was not significant, at least for BC samples in the present study.

The amoA gene of AOA was not amplified by PCR from any samples in the present study (data not shown). This result suggests no or few AOA in the biofilm and the activated sludge in the WWTP. AOA adapts to a much lower NH4+ concentration than AOB and comammox (Martens-Habbena et al., 2009; Zhang et al., 2015). In the present study, the NH4+ concentrations in each tank solution and in the biofilm on BC may be inadequate for AOA. Several studies also reported that AOA in WWTPs were difficult to detect using the qPCR method with the present primer sets due to their small numbers (Park et al., 2006; Gao et al., 2014).

The total bacterial numbers in the biofilm on BC and in the activated sludge of all tanks were in the order of 1010–1011 cells wet-g–1, with no significant differences being observed among samples (Fig. 3C). These numbers were similar to those in the activated sludge of other WWTPs (ca. 1010–1011 cells g–1 of MLVSS [mixed liquor volatile suspended solids]) (Harms et al., 2003), which suggests similar bacterial densities on carrier biofilms and activated sludge among WWTPs.

Relative abundance of comammox and AOB in total bacterial number

The percentages of the number of comammox and AOB out of the total number of bacteria were calculated (Fig. 4). The AOB number in the biofilm on BC accounted for ca. 3×10–2% of total bacteria. This percentage was significantly (P<0.05) higher than that in the activated sludge of the tanks (ca. 2–5×10–3%). Including comammox, the percentage of the ammonia oxidizers in the biofilm on BC increased to approximately 100-fold (ca. 3.5×10–1%) that in the activated sludge. This result suggests that comammox and AOB attach and grow on BC more easily than other bacteria. A similar percentage was reported for the activated sludge samples of other WWTPs (Wang et al., 2018). Although the percentage of comammox and AOB in total bacteria was no more than 3.5×10–1% in the present study, ammonia oxidizers on BC may have similar nitrification potential as ammonia oxidizers in activated sludge.

Fig. 4.

Percentages of AOB and comammox numbers in total bacterial numbers in the activated sludge of AO-, MA-, and A-tanks and the biofilm on BC. Different letters above the columns indicate significant differences (P<0.05). SE represents the standard error.

Comparison of the abundance of AOB, comammox, and total bacteria among tanks

The activated sludge (and biofilm) volume in the collected tank solution differed among tanks (Table S3). To compare the abundance of bacteria among the tanks, we calculated the numbers of comammox, AOB, and total bacteria in a unit volume of the tank solution (cells L–1) (Fig. 5). The A-tank solution had the greatest abundance of AOB per litter among the three tank solutions (Fig. 5A). As shown in Fig. 2, decreased NH4+ and increased NO2 and NO3 concentrations were observed in the A-tank, in which aerobic conditions were maintained by aeration (DO was ca. 6‍ ‍mg L–1). AOB in the A-tank may make a major contribution to the nitrification of the WWTP. In particular, AOB in the biofilm on BC (accounting for more than 90% of AOB in the A-tank) may play an important role in tank nitrification.

Fig. 5.

Average abundance of AOB (A), comammox (B), and total bacteria (C) in the unit volume (L) of solutions in AO-, MA-, and A-tanks, calculated based on numbers shown in Fig. 3. There were no significant differences among the samples (P>0.05). SE shows the standard error.

In the MA-tank (in which the second greatest AOB abundance was observed) decreased NH4+ and increased NO2 and NO3 concentrations under microaerophilic conditions were observed (DO was ca. 3‍ ‍mg L–1), suggesting less activity and smaller contribution of nitrification by AOB than that in the A-tank. On the other hand, AOB in the AO-tank was probably inhibited by anaerobic conditions (DO was ca. 0‍ ‍mg L–1). The detection of AOB in the AO-tank may have been due to the recycling of the A-tank solution. Otherwise, the AOB may have originated from the influent.

The abundance of comammox per litter of A-tank solution was similar to (or higher than) AOB abundance (Fig. 5B). In addition to AOB, comammox may make a considerable contribution to nitrification in the WWTP. In contrast to AOB, comammox was only detected in the biofilm on BC. BC appears to be important for the accumulation of comammox and achieving efficient nitrification in the WWTP. As described above, the environment inside the biofilm may be adequate for comammox (low concentrations of O2 and NH4+). Several studies reported that the genus Nitrospira, containing comammox as well as canonical NOB, was located in the inner part of biofilms in order to avoid being exposed to excessive oxygen, while AOB, such as Nitrosomonas, was located in the outer part of biofilms due to low affinity to oxygen and NH4+ (Okabe et al., 1999; Schramm et al., 2000; Suarez et al., 2019). This may also be the case for comammox and AOB in the biofilm on BC.

The abundance of total bacteria per liter of tank solution was in the order of 1012 cells L–1 for all tanks, with no significant differences being observed among the tanks (Fig. 5C), suggesting that the concentrations of N-related ions and DO that differed among tanks did not affect the number of total bacteria. Relatively greater abundance was observed in the MA-tank (4.6×1012 cells L–1). The dissolved saccharide concentration in the tank solution slightly decreased from the AO-tank to MA-tank (from ca. 4.3±0.4 to 3.8±0.2‍ ‍mg glucose equivalent L–1). Organic substances in the tank solution might affect the abundance of bacteria. However, further analyses of the relationship between bacterial abundance and the concentrations of organic and inorganic substances in each tank are necessary.

The abundance and activities of AOB and AOA are generally known to be influenced by many factors such as water characteristics (including ammonia concentrations and organic loading), environmental parameters (such as temperature, pH, DO concentrations, and retention times) (Almstrand et al., 2011), and the type of wastewater treatment system (activated sludge, moving-bed, etc) (Koops and Pommerening-Röser, 2001; Sinthusith et al., 2015; Wang et al., 2018). Although the present study showed sample data collected from a WWTP at one time point, future studies need to examine the time course of the abundance of ammonia oxidizers in the WWTP and compare the contribution that each ammonia oxidizer makes to nitrification in several plants.

Community compositions of AOB and comammox on biofilm carriers

qPCR revealed that biofilm carriers hold markedly greater numbers of AOB and comammox than activated sludge, and, thus, probably contribute more to nitrification in the WWTP. In the present study, the community composition of AOB and comammox in the biofilm was analyzed using TA cloning. Good’s coverages (Good, 1953) of AOB and comammox clone libraries were 91 and 83%, respectively.

Forty-nine clones of the AOB amoA gene retrieved from BC samples were randomly selected and sequenced (Table S1), then a NJ phylogenetic tree was constructed using amino acid sequences (Fig. 6). A similar tree was obtained when the nucleotide sequences of the amoA gene were used for the phylogenetic calculation (Fig. S2). The tree demonstrated that all of the clones in the present study fell into the genus Nitrosomonas, characterized by tolerance to ammonia, which is often detected in the activated sludge of WWTPs (Stehr et al., 1995; Suwa et al., 1997; Koops and Pommerening-Röser, 2001). Higher NH4+ concentrations in WWTP tanks than in natural environments, such as soils and rivers, may lead to the enrichment of Nitrosomonas spp. The sequences of most clones (47/49, OTU1, and OTU2) were not closely affiliated with any lineages of the genus Nitrosomonas (i.e., N. europaea/mobilis lineage, N. oligotropha lineage, N. communis lineage, N. marina lineage, N. cryotorelans, and N. sp. Nm143 lineage) (Purkhold et al., 2003; Koops et al., 2006), and formed individual clusters together with uncultured bacterium clones retrieved from freshwater or wastewater samples. The cluster was relatively associated with the N. europaea/mobilis lineage. The organisms of this lineage have been found in biofilms in other wastewater treatment systems (Egli et al., 2003; Okabe et al., 2004; Satoh et al., 2006). Moreover, several isolates of this lineage are known to form biofilms with other heterotrophic bacteria (Tsuneda et al., 2001; Petrovich et al., 2017). AOB, which has the ability to form biofilms, may accumulate on BC.

Fig. 6.

Neighbor-joining phylogenetic tree of betaproteobacterial AmoA amino acid sequences of clones retrieved from BC samples. AmoA of Nitrosomonas species and environmental clones detected as the best BLASTx hits were used as reference sequences. Nitrosospira multiformis ATCC 25196 was used for the outgroup. The numbers at nodes represent bootstrap values (%, 1,000 resampling); only values greater than 50% are indicated.

PCR cloning of the comammox amoA gene retrieved from BC samples was conducted using the primer set for qPCR (Ntsp-amoA 162F and 359R), and the results obtained confirmed that all clone sequences (30 clones) were affiliated with the comammox clade A (data not shown). In order to construct a phylogenic tree using sufficient lengths of the sequences, we used the primer set targeting comammox clade A (COMA-F and -R). Sixty clones of the comammox amoA gene (clade A) were sequenced (Table S2), and a NJ phylogenetic tree was constructed using amino acid sequences (Fig. 7). A similar tree was obtained when nucleotide sequences were used for the phylogenetic calculation (Fig S3). The results of the phylogenetic analysis demonstrated that all comammox detected in the present study were classified into the genus Nitrospira. The majority of clones (40/60 clones, OTU1) formed individual clusters, which were relatively close to the branch of the AmoA of Candidatus Nitrospira inopinata enriched from the biofilms obtained from the walls of deep oil well pipes (Daims et al., 2015) (Fig. 7). This result indicates that as-yet-cultivated comammox Nitrospira were predominant in the biofilm. OTU2, OTU3, and OTU5–OTU10 (in total, 18/60 clones) were related to the AmoA of Candidatus Nitrospira nitrosa discovered from tap water (van Kessel et al., 2015; Wang et al., 2017) and of uncultured Nitrospira sp. clones retrieved from river sediments (Yu et al., 2018). The rest of the clones (2/60 clones, OTU4) were related to Nitrospira cf. moscoviensis and the environmental clones of an uncultured bacterium retrieved from river sediments (Xia et al., 2018; Yu et al., 2018). Comammox Nitrospira in the biofilm on BC may originate from oligotrophic environments.

Fig. 7.

Neighbor-joining phylogenetic tree of comammox AmoA amino acid sequences of clones retrieved from BC samples. AmoA of Comammox Nitrospira species and environmental clones detected as the best BLASTx hits were used as reference sequences. Nitrosospira multiformis ATCC 25196 was used for the outgroup. The numbers at nodes represent bootstrap values (%, 1,000 resampling); only values greater than 50% are indicated.

As shown in Fig. 7 and Table S2, the particulate methane monooxygenase A (PmoA) of uncultured bacteria were detected as the related sequences of OTUs in the present study. Other studies suggested that the sequences of some of the pmoA genes were erroneously classified in databases (van Kessel et al., 2015; Chao et al., 2016; Wang et al., 2018), and should be included in comammox amoA based on the findings of phylogenetic analyses (Pinto et al., 2015; Yu et al., 2018). Considering this point, we added the canonical PmoA (alphaproteobacterial, gammaproteobacterial, and verrucomicrobial PmoA) sequences to the tree. As a result, they clustered differently from the comammox AmoA cluster. Therefore, PmoAs detected as relatives of the OTUs of the present study appear to be comammox AmoA.

The rarefaction analysis indicated that the number of species in comammox Nitrospira was greater than AOB Nitrosomonas in the biofilm (Fig. S4). Various comammox Nitrospira species appear to accumulate on BC. To clarify the characteristics of comammox Nitrospira on BC, isolation and physiological analyses of comammox Nitrospira in natural environments as well as in the biofilm on BC are needed.

Conclusion

The present study demonstrated the existence of comammox Nitrospira in the biofilm formed on carriers suspended in the aerobic tank of a full-scale operational WWTP in Japan. qPCR of amoA genes revealed that the abundance of comammox Nitrospira in the biofilm was similar to that of AOB Nitrosomonas. On the other hand, only AOB Nitrosomonas was detected in the activated sludge in the tank, with less abundance than that in the biofilm. Phylogenetic analyses of the amoA gene in the biofilm confirmed that as-yet-cultivated comammox Nitrospira and uncultured AOB Nitrosomonas are predominant in the biofilm. Biofilm formation on carriers appears to be important for the co-existence of comammox and AOB. Further studies are needed to clarify the spatial distribution and activity of ammonia oxidizers inside biofilms on carriers.

Acknowledgements

We wish to thank the staff of the Sewerage Works Division at Saitama prefecture for their support with sampling, and Takuya Idenuma, Hayato Kokubu, Shingo Saruhashi, and Yuya Motegi for their microbiological analyses. We are grateful to the staff of the General Research Institute of Nihon University for their support with sequencing.

References
 
© 2020 by Japanese Society of Microbial Ecology / Japanese Society of Soil Microbiology / Taiwan Society of Microbial Ecology / Japanese Society of Plant Microbe Interactions / Japanese Society for Extremophiles.

This article is licensed under a Creative Commons [Attribution 4.0 International] license.
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