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. 2024 Mar 21;12(5):e03181-23. doi: 10.1128/spectrum.03181-23

Nitrogen source influences the interactions of comammox bacteria with aerobic nitrifiers

Katherine Jeanne Vilardi 1, Juliet Johnston 2, Zihan Dai 2, Irmarie Cotto 2, Erin Tuttle 3, Ariana Patterson 1, Aron Stubbins 1,3,4, Kelsey J Pieper 1, Ameet J Pinto 2,5,
Editor: Erik F Y Hom6
PMCID: PMC11064514  PMID: 38511951

ABSTRACT

While the co-existence of comammox Nitrospira with canonical nitrifiers is well documented in diverse ecosystems, there is still a dearth of knowledge about the mechanisms underpinning their interactions. Understanding these interaction mechanisms is important as they may play a critical role in governing nitrogen biotransformation in natural and engineered ecosystems. In this study, we tested the ability of two environmentally relevant factors (nitrogen source and availability) to shape interactions between strict ammonia and nitrite-oxidizing bacteria and comammox Nitrospira in continuous flow column reactors. The composition of inorganic nitrogen species in reactors fed either ammonia or urea was similar during the lowest input nitrogen concentration (1 mg-N/L), but higher concentrations (2 and 4 mg-N/L) promoted significant differences in nitrogen species composition and nitrifier abundances. The abundance and diversity of comammox Nitrospira were dependent on both nitrogen source and input concentrations as multiple comammox Nitrospira populations were preferentially enriched in the urea-fed system. In contrast, their abundance was reduced in response to higher nitrogen concentrations in the ammonia-fed system. The preferential enrichment of comammox Nitrospira in the urea-fed system could be associated with their ureolytic activity calibrated to their ammonia oxidation rates, thus minimizing ammonia accumulation, which may be partially inhibitory. However, an increased abundance of comammox Nitrospira was not associated with a reduced abundance of nitrite oxidizers in the urea-fed system while a negative correlation was found between them in the ammonia-fed system, the latter dynamic likely emerging from reduced availability of nitrite to strict nitrite oxidizers at low ammonia concentrations.

IMPORTANCE

Nitrification is an essential biological process in drinking water and wastewater treatment systems for treating nitrogen pollution. The discovery of comammox Nitrospira and their detection alongside canonical nitrifiers in these engineered ecosystems have made it necessary to understand the environmental conditions that regulate their abundance and activity relative to other better-studied nitrifiers. This study aimed to evaluate two important factors that could potentially influence the behavior of nitrifying bacteria and, therefore, impact nitrification processes. Column reactors fed with either ammonia or urea were systematically monitored to capture changes in nitrogen biotransformation and the nitrifying community as a function of influent nitrogen concentration, nitrogen source, and reactor depth. Our findings show that with increased ammonia availability, comammox Nitrospira decreased in abundance while nitrite oxidizers abundance increased. Yet, in systems with increasing urea availability, comammox Nitrospira abundance and diversity increased without an associated reduction in the abundance of canonical nitrifiers.

KEYWORDS: comammox, urea, nitrifiers, ammonia inhibition

INTRODUCTION

Comammox bacteria, which belong to the genus Nitrospira, are routinely detected alongside strict ammonia-oxidizing bacteria (AOB) and nitrite-oxidizing bacteria (NOB) in both drinking water and wastewater systems (19), but insights into the factors influencing their abundance, activity, and interactions in these environments are still limited. Interactions between AOB and NOB have been extensively studied including the impact of operational processes and environmental conditions such as oxygen supply, ammonia concentration, and temperature (1012). However, the presence of comammox Nitrospira within these communities requires a re-evaluation of these interactions and the collective response of nitrifying consortia to changes in environmental and/or process conditions. Our understanding of the role and ecological niche of comammox Nitrospira within complex nitrifying communities is further restricted by limited physiological insights due to the existence of only a few cultured representatives and/or enrichments, all belonging to clade A1 (1315).

Ammonia availability is likely an important factor governing interactions between strict AOB and comammox Nitrospira. For instance, comammox Nitrospira cultures and enrichments have shown a significantly higher affinity for ammonia compared to strict AOB (1416). Thus, comammox Nitrospira may outcompete strict AOB in ammonia-limited environments such as drinking water systems. Further, different comammox Nitrospira may exhibit varying preferences for ammonia concentration ranges, and these may not only be dictated by ammonia affinities but also include potential inhibition at higher concentrations. For example, ammonia oxidation by Ca. Nitrospira kreftii was partially inhibited at relatively low ammonia concentrations (25 µM) (15), which was not observed for Ca. Nitrospira inopinata (16). Comammox Nitrospira may also exhibit clade/sub-clade-dependent preferences for ammonia availability and/or environments. For example, clade A1 comammox Nitrospira associated with Ca. Nitrospira nitrosa are typically found at higher abundances than canonical nitrifiers in some wastewater systems (2, 7, 17, 18) and sometimes as the principal aerobic ammonia oxidizers in these systems (19). In the latter situation, ammonia oxidation dominated by comammox Nitrospira could also adversely impact Nitrospira-NOB by limiting nitrite availability through complete nitrification to nitrate at low ammonia concentrations; however, the relationship between the two Nitrospira groups is not well understood.

The nitrogen source could also have a significant effect on interactions between nitrifiers. For instance, ureolytic activity may enable access to ammonia derived from urea in engineered systems (e.g., wastewater treatment), as well as natural systems such as freshwater ecosystems (20). Genes for urea degradation accompanied by a diverse set of urea transporters are ubiquitously found in genomes of all comammox Nitrospira (21). Their ability to grow in urea is supported by the enrichment of multiple species of comammox Nitrospira in urine-fed membrane bioreactors (22) and the enrichment of comammox Nitrospira when supplied with urea (22, 23). Some Nitrospira-NOB are also capable of catalyzing ammonia production through urea degradation and, thus, potentially regulating nitrite availability via cross-feeding of ammonia to strict AOB (24); this could potentially influence competition between canonical nitrifiers and comammox Nitrospira.

The present work aimed to investigate the potential competitive interactions of comammox Nitrospira with canonical nitrifiers subject to different nitrogen sources and concentrations. We operated two continuous-flow laboratory-scale column reactors with granular activated carbon (GAC) containing all three nitrifying groups and supplied the reactors with either ammonia or urea at three different influent nitrogen concentrations. Our goal was to infer (i) nitrogen source (i.e., ammonia and urea), species (i.e., urea, ammonia, and nitrite), and concentration preferences of nitrifying groups and (ii) their potential interactions by quantitatively measuring their differential sorting within column reactors over time in the context of their genome-resolved metabolic capabilities.

MATERIALS AND METHODS

Reactor operation

Two laboratory-scale down-flow column reactors (diameter = 2.54 cm, height = 25.4 cm) were packed with GAC (packed height = 7.62 cm) and operated at room temperature (20°C–22°C) with an approximately 2.54 cm of water head above the GAC to ensure the media was fully saturated. The systems were each packed with 35 g of GAC from the City of Ann Arbor, Michigan Drinking Water Treatment Plant (DWTP). The two reactors were fed with synthetic groundwater media (25). Stock solution for the inorganic compounds in the media was prepared with 3.88 g/L MgCl2, 2.81 g/L CaCl2, 13.68 g/L NaCl, 6.90 g/L K2CO3, 17.75 g/L Na2SO4, and 0.88 g/L KH2PO4. The organic compound stock solution contained 3.75 g/L of glucose (C6H12O8), and a sodium bicarbonate solution was prepared with 30 g/L of NaHCO3. Influent media was then prepared in 10 L autoclaved carboys with 1 mL/L of the inorganic and organic compound stock solutions and 10 mL/L of the sodium bicarbonate stock solution. The two reactors were fed influent amended with stock solutions of ammonium chloride (NH4Cl) or urea (CH4N2O). Both reactors were fed influent at three different nitrogen concentrations over the experimental period. Column reactors were maintained in conditions 1 (1 mg-N/L) and 2 (2 mg-N/L) for 8 weeks and in condition 3 (4 mg-N/L) for 6 weeks. Influent media was pumped at 1.15 L/day with the peristaltic pump resulting in an empty bed contact time (EBCT) of approximately 48 minutes.

Sample collection and processing

Influent and effluent were sampled twice weekly, while five samples spaced approximately 1.27 cm apart along the depth of the GAC column were collected weekly to capture depth-wise nitrogen species concentrations. The five sections are defined as sections 1.27 (L1), 2.54 (L2), 3.81 (L3), 5.08 (L4), and 6.35 (L5) cm (Fig. S1). All aqueous samples were filtered through 0.22-µm filters (Sartorius Minisart NML Syringe Filter—Fisher Scientific 14555269). GAC media samples were collected at week 0 followed by weeks 6, 7, and 8 for conditions 1 and 2 and week 6 for condition 3. GAC media samples (0.3 g) were collected from three locations along the reactor bed: one within the top 1.27 cm of the reactor, one mid-filter depth (3.81 cm), and another at the bottom approximately 7.62 cm from the top of the reactor location and were stored for DNA extraction in Lysing Matrix E Tubes (MP Biomedical—Fisher Scientific MP116914100). After each sampling event, the amount of GAC taken was replaced with virgin GAC, which was mixed with the remaining GAC by first fluidizing the filter media with 50 mL deionized water followed by backwashing with air for 5 minutes. A total of 42 GAC media samples were collected from seven sampling events. During each sampling event, we collected samples from three depths (top, L1; middle, L3; bottom, L5) for each of the two columns (Fig. S1). These GAC media samples were immediately stored at −80°C until further processing.

Chemical analysis

Hach TNT Vials were used to determine concentrations of ammonia (TNT832), nitrite (TNT839), nitrate (TNT835), and total alkalinity (TNT870). All samples were analyzed on a Hach DR1900 photospectrometer (Hach—DR1900-01H). Influent and effluent pH was determined using a portable pH meter (Thermo Scientific Orion Star A221 Portable pH Meter—Fisher Scientific 13-645-522). A Shimadzu TOC-L (total organic carbon analyzer) with a TNM-L attachment (total nitrogen unit) (26) was used to measure total dissolved nitrogen in influent and effluent samples using certified DOC/TDN standards [deep seawater reference: low carbon seawater, LSW, deep seawater reference material] (Batch 21 Lot 11-21, 1). Urea concentrations in samples collected from the urea-fed reactors were determined by subtracting the total inorganic nitrogen measured (i.e., sum of ammonia, nitrite, and nitrate) in each sample from influent urea concentration.

Nitrogen biotransformation rate calculations

Rates of nitrogen biotransformations were calculated from the concentration profiles of ammonia, NOx (nitrite plus nitrate), nitrate, and total inorganic nitrogen (sum of ammonia, nitrite, and nitrate) measured along the column reactor depths. Rates were calculated for six sections of the columns: 0–1.27 (In-L1), 1.28–2.54 (L1-L2), 2.55–3.81 (L2-L3), 3.82–5.08 (L3-L4), 5.09–6.35 (L4-L5), and 6.36–7.62 (L5-Eff) cms. Volumetric rates (mg-N/L packed GAC/h) were obtained by multiplying the concentration differences between the profile layers by the influent flow rate and dividing by the volume of packed GAC between the profile layers (V = 6.4 mL packed GAC in each layer).

DNA extraction and qPCR assays

DNA was extracted from all GAC samples (n = 43), which included the inoculum and samples collected at all time points and locations for each condition. Extractions were performed using Qiagen’s DNeasy PowerSoil Pro (Qiagen, Inc—Cat. No. 47014) with a few modifications. GAC in lysing matrix tubes with 800 µL of CD1 was vortexed briefly and placed in a 65°C water bath for 10 minutes. After heating, 500 µL of phenol:chloroform:isoamyl alcohol (25:24:1, vol/vol) (Invitrogen UltraPure—Fisher Scientific 15-593-031) was added to the lysing tube bead beating and processed with four 40-second rounds on the FastPrep-24 instrument (MP Biomedical—Cat. No. 116005500) with lysing tubes placed on ice for 2 minutes between rounds. Samples were then centrifuged for 1 minute, and 600 µL of the aqueous phase was used for DNA extractions on the Qiacube (Qiagen, Inc—Cat No. 9002160) protocol for PowerSoil Pro. A reagent blank was included in each round of extractions as a negative control. DNA concentrations were measured using a Qubit with the dsDNA Broad Range Assay (Invitrogen—Fisher Scientific Q32850). Extracted DNA was stored at −80°C until further processing.

Quantitative polymerase chain reaction (qPCR) assays were conducted using the Applied Biosystems 7500 Fast Real-Time PCR instrument. Primer sets listed in Table S1 were used to target the 16S rRNA gene of AOB (27), 16S rRNA gene of Nitrospira (28), amoB gene of clade A comammox Nitrospira (1), and 16S rRNA gene of total bacteria (29). The qPCR reactions were performed in 20 µL volumes, which contained 10 µL Luna Universal qPCR mastermix (New England Biolabs Inc., Fisher Scientific Cat. No. NC1276266), 5 µL of 10-fold diluted template DNA, primers at concentrations listed in Table S1, and DNA/RNAse-free water (Fisher Scientific, Cat. No. 10977015) to make the remaining volume. Each sample was subjected to qPCR in triplicate. The cycling conditions consisted of initial denaturing at 95°C for 1 minute, 40 cycles of denaturing at 95°C for 15 seconds, annealing times and temperatures listed in Table S1, and extension at 72°C for 1 minute. Three different sets of gBlock standards (Integrated DNA Technology gBlocks Gene Fragments 125–500 bp) targeting the 16S rRNA gene of total bacteria and Nitrospira, 16S rRNA gene of AOB, and amoB gene of clade A comammox Nitrospira were used to establish a seven-point standard curve for each respective assay (Table S2). The qPCR efficiencies for all assays are listed in Table S1.

16S rRNA gene amplicon sequencing and data analysis

DNA extracts (triplicate per sample) from all samples were submitted for sequencing of the V4 hypervariable region of the 16S rRNA gene at the Georgia Institute of Technology Sequencing Core. The MiSeq v2 kit was used to generate 250-bp pair-end reads using the 515F (30) and 806R (31) primers with an overhang of barcoded Illumina adapters. Removal of adapter and primer sequences from the resultant sequencing data was carried out using cutadapt v4.2. Amplicon sequencing data processing and quality filtering were performed using DADA2 v1.22.0 (32) in R v4.1.2. to infer amplicon sequence variants (ASVs) using the pipeline for paired-end Illumina MiSeq data. The SILVA nr v.138.1 database (33) was used for the taxonomic assignment of ASVs with a minimum bootstrap confidence threshold of 80. The ASV table was rarefied with the “rarefy_even_depth” function from the R package phyloseq v1.38.0 to the sample with the smallest library size. The relative abundance of ASVs in each sample was calculated by dividing ASV read counts in the sample by the total number of sample read counts.

Metagenomic sequencing, assembly, and binning

DNA extracted from samples taken at week 6 from the top layer of the ammonia- and urea-fed reactors during condition 3 were submitted for sequencing on the Illumina NovaSeq platform with a SP flow cell at the Georgia Institute of Technology Sequencing Core. Similar workflows and tools utilized in references (1, 2) were applied here to assemble and characterize metagenome-assembled genomes (MAGs). Briefly, raw paired-end reads were quality-filtered using fastp (v0.22.0) (34) and further mapped to the Univec database to remove contaminant reads. Samtools (v1.15.1) (35) was used to sort the resulting bam files, and bedtools (v2.30.0) (36) was used to convert them to fastq files. Assemblies were generated for each sample separately using metaSpades (v3.13.0) (37) with kmer sizes 21, 33, 55, and 77. The two resulting fasta assemblies were indexed with bwa index (v0.7.17), and filtered pair-ended reads were mapped back to their respective assemblies with bwa mem (v0.7.17) (38). The subsequent sam files were converted to bam files using appropriate samtools (v1.15.1) flags to retain only mapped reads.

Metabat2 (39) was used to bin contigs longer than 2,000 bp followed by CheckM (v1.1.2) (40) to determine the completeness and contamination levels of MAGs, which were then classified using the Genome Taxonomy Database Tool Kit (v1.1.1) with database release 207 (41). Open reading frames of coding regions predicted using prodigal (42) were annotated against the KEGG database (43) with kofamscan (v1.2.0) (44). The up-to-date Bacterial Core Gene pipeline (v3.0) (45) was used to construct maximum likelihood trees using a set 92 extracted and aligned single-copy genes from assembled Nitrospira-like and Nitrosomonas-like MAGs and references. A set of dereplicated MAGs was generated from MAGs recovered from the ammonia- and urea-fed systems at an average nucleotide identity (ANI) threshold of 99% using dRep (v3.4.0) (46). Reads from the ammonia- and urea-fed samples were mapped to the set of dereplicated MAGs to calculate the breadth of coverage (i.e., percent of genome covered by reads) and relative abundance using coverM (https://github.com/wwood/CoverM).

16S rRNA gene sequences of a minimum length of 500 bp were reconstructed from the metagenomes of both samples using MATAM v1.6.1 (47) to establish the linkage between ASVs generated from 16S rRNA gene amplicon sequencing and MAGs associated with nitrifying bacteria. To achieve a more comprehensive reconstruction, recursive random sub-sampling of different depths, i.e., 1%, 5%, 10%, 25%, 50%, 75%, and 100%, was performed, followed by dereplication at 99.9% identity using USEARCH v11.0.667 (48, 49). Only the longest sequence from each cluster was retained for downstream analysis. Furthermore, ASVs were aligned against the MATAM recovered 16S rRNA gene sequences and extracted 16S rRNA genes from MAGs by Barrnap v0.9 using BLASTn v2.13.0 (50), and only ASV hits of 100% identity and 100% coverage were considered as linkage candidates between ASV and MAG unless the alignment was interrupted at the end of the reference sequence.

Statistical analysis

All statistical analysis was performed in R v4.1.2 (51). A significant difference in effluent concentrations of ammonia, nitrite, and nitrate in the ammonia- and urea-fed systems was tested using the non-parametric Wilcox rank sum test. Ratios of effluent NOx to influent nitrogen concentrations as a proxy for ammonia consumption in both systems were compared with Student’s t-test for conditions 2 and 3 while condition 1 required the systems to be compared with Welch’s t-test due to unequal variance between the ammonia- and urea-fed systems. The data distribution and variance for all tests were checked with the Shapiro–Wilks and Levene tests, respectively. We tested if the microbial community in GAC samples clustered significantly by nitrogen source, concentration, and reactor depth using the Bray–Curtis dissimilarities calculated from the ASV abundance table and applying a PERMANOVA test using the adonis function in the R package vegan v2.6-4 (52). Correlations between microbial community composition and concentrations of ammonia, nitrite, and nitrate measured in the biofiltrations were calculated with the Mantels test. The mean relative abundances of nitrifier ASVs and qPCR-based relative abundances of comammox Nitrospira, strict AOB, and Nitrospira-NOB were compared in both systems across the nitrogen concentrations using ANOVA. Pearson correlation was used to statistically quantify and test the significance of the relationship between the abundance of comammox Nitrospira and Nitrospira-NOB in both systems.

RESULTS

Nitrogen biotransformation in ammonia- and urea-fed systems

Urea- and ammonia-fed systems had similar concentrations of ammonia, nitrite, and nitrate in the effluent [sample size (n) = 16, Wilcoxon P > 0.05] (Fig. S2) and similar depth-wise distributions of inorganic nitrogen species (Fig. 1A) at the lowest influent concentration (condition 1: 1 mg-N/L). The majority of the influent nitrogen (~70%) was completely oxidized to nitrate in the topmost portion of the reactors (0–1.27 cm section) (Fig. 1A and B). Rates of ammonia oxidation (4.99 ± 1.95 mg-N/L packed GAC/h) and urea degradation (5.13 ± 0.70 mg-N/L packed GAC/h) were highest in the 0–1.27 cm section and were nearly equal to the rate of nitrate production (5.31 ± 1.55 and 4.79 ± 0.83 mg-N/L packed GAC/h, respectively) (Fig. 1B). Increasing the influent nitrogen concentrations to 2 mg-N/L (i.e., condition 2) led to significantly higher nitrite accumulation in the ammonia-fed reactor compared to the urea-fed reactor (n = 16, Wilcoxon P < 0.05) due to an imbalance between ammonia oxidation (10.91 ± 1.49 mg-N/L packed GAC/h) and nitrate production (8.51 ± 2.03 mg-N/L packed GAC/h) rates in the In-1.27 cm section of the ammonia-fed system (Fig. 1B). In contrast, the average urea degradation rate (8.25 ± 2.21 mg-N/L packed GAC/h) was nearly equal to the nitrate production rate (6.85 ± 1.67 mg-N/L packed GAC/h) in the top section of the urea-fed reactor. Nitrite accumulation was exacerbated at the higher influent nitrogen concentration (condition 3: 4 mg-N/L) with significantly higher effluent nitrite concentrations in the ammonia-fed system (1.00 mg-N/L) compared to the urea-fed system (0.10 ± 0.04 mg-N/L). The average ammonia oxidation rate (15.02 ± 2.67 mg-N/L packed GAC/h) in the top section of the ammonia-fed system was 1.8 times higher than the nitrate production rate (8.50 ± 2.03 mg-N/L packed GAC/h). The rates of nitrate production in the 0–1.27 cm section were similar between conditions 2 and 3 (8.56 ± 1.47 and 8.50 ± 2.03 mg-N/L packed GAC/h, respectively) in the ammonia-fed system, indicating that maximum rates of nitrate production had been reached. Interestingly, ammonia accumulation in the urea-fed systems resulted in similar effluent ammonia concentrations as observed in the ammonia-fed systems for conditions 1 and 2, suggesting that both reactors had reached their ammonia oxidation capacity across the entire depth of the reactors.

Fig 1.

Fig 1

(A) Concentrations of ammonia, nitrite, and nitrate measured at five depths along the reactors. Measurements were taken at 1.27 (L1), 2.54 (L2), 3.81 (L3), 5.08 (L4), and 6.35 (L5) cm from the top of GAC in the reactors. Data points represent the average concentration obtained from the different reactor depths along with error bars for standard deviation. (B) Rates of nitrogen biotransformation along the depths of the reactors. Rates are colored by the type of nitrogen biotransformation (purple, ammonia oxidation; green, nitrate production; orange, NOx production; gray, urea degradation). Data points represent the average rates obtained from the different reactor depths along with error bars for standard deviation.

GAC microbial community composition

Rarefaction to the smallest library size (70,354 reads) resulted in the retention of 1,738 ASVs out of 2,400 constructed from the V4 hypervariable region of the 16S rRNA gene. ASVs with the highest relative abundance belonged to the class Gammaproteobacteria (5.09% ± 1.96%: ASV 1 and 4.62% ± 2.96%: ASV 2), Vicinamibacteria (3.70% ± 1.49%: ASV 3), Nitrospira (3.50% ± 1.63%: ASV 4 and 2.72% ± 1.40%: ASV 6), and Alphaproteobacteria (3.40% ± 1.56%: ASV 5). Microbial community composition was shaped significantly by nitrogen concentration (n = 42, PERMANOVA R = 0.628, P < 0.05), nitrogen source (PERMANOVA R = 0.134, P < 0.05), and reactor section [i.e., GAC sampling point, top (L1), middle (L3), and bottom (L5)] (PERMANOVA R = 0.163, P < 0.05) (Fig. 2A). Nitrogen source (i.e., ammonia-fed vs urea-fed) played a more significant role in shaping the overall microbial community for condition 2 (n = 18, PERMANOVA R = 0.224, P < 0.05) as compared to condition 1 (n = 18, PERMANOVA R = 0.104, P > 0.05) or condition 3 (n = 6, PERMANOVA R = 0.412, P > 0.05). Community composition of the two reactors may not exhibit a strong difference for condition 1 due to very similar depth-wise nitrogen species profiles (Fig. 1A and B), while differences during condition 3 may not be flagged as significant due to the limited data points. In the ammonia-fed system (Fig. 2A), the microbial community separated into distinct clusters based on nitrogen concentration (n = 21, PERMANOVA R = 0.614, P < 0.05) but not by reactor depth (n = 21, PERMANOVA R = 0.077, P > 0.05). In contrast, both nitrogen concentration (n = 21, PERMANOVA R = 0.665, P < 0.05) and reactor depth (n = 21, PERMANOVA R = 0.204, P < 0.05) were significantly associated with differences in microbial community composition for the urea-fed system (Fig. 2B).

Fig 2.

Fig 2

Non-metric multidimensional scaling (NMDS) plots constructed with the abundance tables of all ASVs in the (A) ammonia-fed system and (B) urea-fed system and nitrifier ASVs in the (C) ammonia-fed and (D) urea-fed systems. Blue-, purple-, and orange-colored points are GAC samples collected during conditions 1, 2, and 4, respectively. Shape symbolizes the reactor depth the GAC samples were taken from [L1, top (circle); L3, middle (triangle); L5, bottom (square)]. The outline color of shapes represents the system the GAC was collected from (gray, urea-fed; black, ammonia-fed).

Compositional differences in nitrifier communities were evaluated with ASVs classified as Nitrospira-like (nine ASVs) and Nitrosomonas-like (five ASVs) bacteria; this is in line with our previous work, which found nitrifiers belonged to only these genera in GAC samples from the same biofiltration system (1), and these were the only nitrifying genera identified in the inoculum used for this study (Table S3). Nitrifier communities in the ammonia- and urea-fed systems were significantly dissimilar during conditions 1 (n = 18, ANOSIM R = 0.319, P < 0.05) and 2 (n = 18, ANOSIM R = 0.368, P < 0.05) (Fig. S2B). Nitrogen source explained a greater variance between communities in condition 3 (n = 6, PERMANOVA R = 0.406) but was found to be insignificant potentially due to fewer data points. In both the ammonia- and urea-fed systems, nitrifier community composition was most dissimilar between conditions 1 and 3 (n = 42, ANOSIM R = 0.607 and 0.536, P < 0.05) (Fig. 2C and D). Collectively, our results show that the composition of both the whole community and nitrifiers was significantly shaped by nitrogen source and availability. The largest impacts were consistently observed when comparing the lowest and highest nitrogen concentration conditions.

Impact of nitrogen source and concentrations on nitrifying bacteria

In the ammonia- and urea-fed systems, four Nitrospira-like (ASVs 4, 6, 46, and 236) and three Nitrosomonas-like (ASVs 17, 54, and 62) ASVs were detected. Mapping ASVs 4, 6, and 46 against Nitrospira reference genomes and full-length 16S rRNA sequences indicated that ASV 4 was a Nitrospira lenta-like strict NOB (100% ID to NCBI accession number KF724505) and ASVs 6 and 46 were Nitrospira nitrosa-like comammox Nitrospira (both 100% ID to NZ_CZQA00000000). All Nitrosomonas-like ASVs shared high sequence similarity (>98% ID) with 16S rRNA gene sequences within Nitrosomonas cluster 6a [Nitrosomonas ureae (NZ_FOFX01000070) and Is79 (NC_015731)].

In the ammonia-fed system, the relative abundance of Nitrospira lenta-like ASV 4 averaged across the reactor (i.e., samples from top, middle, and bottom combined) increased with increasing nitrogen concentrations (1 mg-N/L: 2.63% ±0.45%, 2 mg-N/L: 3.89% ± 1.23%, and 4 mg-N/L: 5.40% ± 1.75%) with its abundance significantly higher in condition 3 compared to condition 1 (n = 21, ANOVA/Tukey, P < 0.05) (Fig. S3). In contrast, the average relative abundance of comammox-like ASV 6 across the column decreased with increased nitrogen concentrations (1 mg-N/L: 2.67% ±0.70%, 2 mg-N/L: 1.16% ± 0.38%, and 4 mg-N/L: 0.67% ± 0.22%) with its the abundance significantly higher during condition 1 compared to both conditions 2 and 4 (n = 21, ANOVA/Tukey, P < 0.05). Furthermore, the abundance of ASV 6 did not change with depth in the ammonia-fed reactor during all conditions whereas the abundance distribution of ASV 4 appeared to be dependent on nitrogen availability (Fig. 3A). The abundance of ASV 4 was positively associated with concentrations of ammonia (n = 21, Pearson R = 0.344, P < 0.05) and nitrite (n = 21, Pearson R = 0.304, P < 0.05), but the opposite was observed for the abundance of ASV 6, which had a negative association with both ammonia (n = 21, Pearson R = 0.367, P < 0.05) and nitrite (n = 21, Pearson R = 0.346, P < 0.05) (Fig. S4A and B). The relative abundance of Nitrosomonas-like ASV 17 across the column remained consistent between conditions (1 mg-N/L: 1.23% ± 0.31%, 2 mg-N/L: 1.44% ± 0.39%, and 4 mg-N/L: 0.97% ± 0.28%) (P < 0.05) (Fig. S3) with similar relative abundances found in each section of the reactor regardless of nitrogen concentration (Fig. 3A). ASV 54 replaced ASV 17 as the dominant Nitrosomonas-like ASV as its average relative abundance across the column increased 27-fold between conditions 1 (0.12% ± 0.19%) and 4 (3.23% ± 3.88%). The abundance of both ASVs 54 and 62 was positively correlated with the concentration of ammonia (n = 21, Pearson R = 0.503 and Pearson R = 0.474, P < 0.05) (Fig. S4A), indicating their abundance increased in response to higher ammonia concentrations in the ammonia-fed system.

Fig 3.

Fig 3

Relative abundance of nitrifier ASVs and qPCR-based relative abundance of comammox Nitrospira, strict AOB, and Nitrospira-NOB in the (A) ammonia-fed and (B) urea-fed systems at 1 (top panels), 2 (middle panels), and 4 (bottom panels) mg-N/L. Nitrosomonas- and Nitrospira-like populations are represented by circles and triangles, respectively. Data points for ASVs are the average relative abundance of nitrifier ASVs calculated in the top, middle, and bottom sections of the reactors during each nitrogen concentration with error bars for standard deviation. Data points for qPCR assays are the average relative abundances of comammox Nitrospira, strict AOB, and Nitrospira-NOB in the top, middle, and bottom sections of the reactors during each nitrogen concentration with error bars for standard deviation.

While the abundance of Nitrosomonas-like ASV 54 increased 40-fold with increased influent nitrogen concentration in the urea-fed system, ASV 17 remained the dominant ASV with its relative abundance increasing from 0.88% ± 0.31% in condition 1 to 2.45% ± 1.92% in condition 3 across the column. In contrast, Nitrosomonas-like ASV 62, which increased in abundance proportional to ammonia concentration in the ammonia-fed system, demonstrated no significant change between any of the urea conditions (n = 21, ANOVA/Tukey, P > 0.05) and remained at low relative abundance, suggesting it was outcompeted in the urea-fed system. While ASVs 4 and 6 were still dominant Nitrospira-like ASVs in the urea-fed system, another Nitrospira-like ASV (48) increased in abundance across the column from 0.18% ± 0.14% to 1.41% ± 1.36% to 1.93% ± 1.76% for conditions 1, 2, and 3, respectively; ASV 46 was only detected in conditions 1 and 2 in the ammonia-fed system at extremely low abundance (<0.006%), thus showing a clear enrichment in the urea-fed systems (Fig. S3). Its abundance also changed with reactor depth during conditions 2 and 4 in the urea-fed system where its abundance was higher in the top section compared to lower portions (Fig. 3B). Consistent with the ammonia-fed system, the abundance of Nitrospira lenta-like ASV 4 was positively associated with ammonia concentrations (n = 21, Pearson R = 0.289, P < 0.05) (Fig. S4C), and that of ASV 6 was negatively associated with nitrite concentrations (n = 21, Pearson R = 0.398, P < 0.05) in the urea-fed system (Fig. S4D).

Comammox Nitrospira abundance averaged across the columns based on qPCR assays was significantly lower in conditions 2 (1.06% ± 0.35%) and 3 (0.56% ± 0.13%) compared to its abundance during condition 1 (2.08% ± 0.71%) (ANOVA/Tukey, P < 0.05) in the ammonia-fed system (Fig. 3A). Additionally, the relative abundance of comammox Nitrospira displayed minimal change along sections of the ammonia-fed reactor during all conditions, which aligns with the trends observed for ASV 6. The relative abundance of Nitrospira-NOB averaged across the column assessed by qPCR increased with each nitrogen concentration (1 mg-N/L: 1.14% ± 0.88%, 2 mg-N/L: 1.76% ± 0.73%, and 4 mg-N/L: 2.37% ± 0.84%) though its abundance was not significantly different between each of them (n = 42, ANOVA/Tukey, P > 0.05). However, its relative abundance was highest overall (3.32%) during condition 3 in the top section where ammonia and nitrite availability was considerably higher compared to the other two nitrogen concentrations. Thus, Nitrospira-NOB likely benefited from increased availability of ammonia and nitrite during higher nitrogen concentrations whereas comammox Nitrospira preferred the lowest nitrogen condition with limited ammonia availability in the ammonia-fed system. The overall highest abundance of strict AOB and Nitrospira-NOB occurred in the top section of the reactor during condition 3.

qPCR-based abundance of comammox Nitrospira was significantly higher in all urea-fed conditions compared to its abundance in any of the ammonia-fed conditions (Fig. 3A and B), which was also observed for comammox-like ASVs. The combined abundance of comammox-like ASVs was strongly correlated with the qPCR-based abundance of comammox Nitrospira (n = 42, Pearson R = 0.92, P < 0.05) (Fig. S5). Furthermore, qPCR- and ASV-based abundances agreed that comammox Nitrospira were the dominant ammonia oxidizers regardless of nitrogen concentration in the urea-fed system. The qPCR-based abundance of Nitrospira-NOB in the urea-fed system was lower than that of comammox Nitrospira during each condition (Fig. 3B). However, the increased abundance of comammox Nitrospira did not result in decreased abundance of Nitrospira-NOB (n = 21, Pearson R = 0.10, P > 0.05) (Fig. 4A). This is in contrast to the ammonia-fed system where comammox Nitrospira and Nitrospira-NOB populations demonstrated a significant negative association (n = 21, Pearson R = −0.48, P < 0.05) (Fig. 4B). There are no significant associations between the abundance of comammox Nitrospira and strict AOB, and Nitrospira-NOB and strict AOB in either the ammonia- or urea-fed systems (data not shown).

Fig 4.

Fig 4

(A) Lack of any relationship between the abundance of comammox Nitrospira and Nitrospira-NOB in the urea-fed system contrasts with (B) significant negative association between the abundance of comammox Nitrospira and Nitrospira-NOB in the ammonia-fed system.

Phylogeny and metabolism of nitrifier MAGs

Two hundred and one hundred seventy-two MAGs were recovered from the metagenomic assemblies from the ammonia- and urea-fed systems, respectively. The nitrifier community in the ammonia-fed system was comprised of three Nitrosomonas-like MAGs and two Nitrospira-like MAGs (one classified as Nitrospira_F and one classified as Nitrospira_D), which aligns with the number of dominant nitrifier ASVs in the ammonia-fed system (Table 1). Nitrifier MAGs assembled from the urea-fed system also mirrored the number of dominant nitrifier ASVs with three Nitrospira-like (two Nitrospira_F and one Nitrospira_D) and three Nitrosomonas-like MAGs. While an additional Nitrosomonas-like MAG was assembled from the urea-fed GAC sample, it was extremely of low quality (completeness <10%).

TABLE 1.

Quality statistics for nitrifier MAGs assembled from GAC taken from the ammonia- and urea-fed reactors

MAG name Classification Reactor Completeness (%) Redundancy (%)
Nitrospira_D1_A Nitrospira_D sp002083555 Ammonia 92.27 3.91
Nitrospira_F1_A Nitrospira_F Ammonia 88.88 3.69
Nitrosomonas_1_A Nitrosomonas Ammonia 80.3 0.48
Nitrosomonas_2_A Nitrosomonas sp016708955 Ammonia 97.38 0.51
Nitrosomonas_3_A Nitrosomonas Ammonia 92.34 0.03
Nitrospira_F1_U Nitrospira_F Urea 92.11 71.93
Nitrospira_D1_U Nitrospira_D sp002083555 Urea 94.09 4.82
Nitrospira_F2_U Nitrospira_F sp002083565 Urea 84.65 6.41
Nitrosomonas_1_U Nitrosomonas Urea 98.72 0.48
Nitrosomonas_2_U Nitrosomonas sp016708955 Urea 93.38 0.51
Nitrosomonas_3_U Nitrosomonas Urea 93.54 0.03
Nitrosomonas_4_U Nitrosomonas Urea 6.22 0

Phylogenetic analysis with 92 single-copy core genes clustered Nitrospira_F1_A with clade A comammox Nitrospira (Fig. 5A), and it showed high sequence similarity (~94% ANI) with Nitrospira sp. Ga0074138, which is a comammox Nitrospira MAG previously assembled by Pinto et al. (9) from GAC obtained from the same reactor. Nitrospira_F1_A shared extremely high sequence similarity (>99% ANI) with Nitrospira_F1_U assembled from the urea-fed system, suggesting that the two MAGs were likely the same population (Fig. S6A). Another Nitrospira MAG (Nitrospira_F2_U) assembled from the urea-fed system sample was placed within comammox clade A but clustered separately with other drinking water-related comammox MAGs (Nitrospira sp. ST-bin4 and SG-bin2). This MAG shared less than 80% ANI with all other Nitrospira MAGs in this study. Phylogenetic placement of hydroxylamine dehydrogenase (hao) gene sequences present in all comammox MAGs in this study was grouped into clade A2 comammox Nitrospira (data not shown). The remaining two Nitrospira MAGs (Nitrospira_D1_A and Nitrospira_D1_U) clustered with Nitrospira-NOB belonging to lineage II (Fig. 5A) with Nitrospira lenta and other Nitrospira-NOB obtained from a drinking water system (Nitrospira sp. ST-bin5) and rapid sand filter (RSF 13 and CG24D). Nitrospira_D1_A and Nitrospira_D1_U from this study shared over 99% sequence similarity, indicating that they are the same population (Fig. S6A).

Fig 5.

Fig 5

Maximum likelihood trees for (A) Nitrospira and (B) Nitrosomonas based on a set of bacterial single-copy core genes. MAGs assembled in this study are labeled in red, and reference genomes and MAGs are in black.

ANI comparisons between the Nitrosomonas-like MAGs assembled from the ammonia-fed (Nitrosomonas_1_A, Nitrosomonas_2_A, and Nitrosomonas_3_A) and urea-fed (Nitrosomonas_1_U, Nitrosomonas_2_U, and Nitrosomonas_3_U) systems revealed that the same set of three Nitrosomonas-like MAGs were assembled from both samples (Fig. S6B). Within-sample ANI comparisons showed that the three Nitrosomonas-like MAGs shared less than 95% ANI, suggesting they were separate species. The phylogenomic placement of Nitrosomonas MAGs in this study affiliated them with Nitrosomonas cluster 6a, which are known for their oligotrophic physiologies (53). Nitrosomonas_1_A and Nitrosomonas_1_U (ANI > 99%) clustered with Nitrosomonas ureae while Nitrosomonas_2_A and Nitrosomonas_2_U (ANI > 99%) grouped with Nitrosomonas Is79A3 (Fig. 5B). Nitrosomonas_3_A and Nitrosomonas_3_U (ANI > 99%) clustered with uncultured Nitrosomonas MAGs that were still within the cluster 6a grouping. Out of all reference comparisons, Nitrosomonas MAGs from this study shared the highest similarity to Nitrosomonas ureae strain Nm5 Ga0181075 101 (ANI = 83%, Nitrosomonas_1_A and Nitrosomonas_1_U), Nitrosomonas Is79 (ANI = 89%, Nitrosomonas_2_A and Nitrosomonas_2_U), and Nitrosomonas sp. Nm141 Ga0181066 101 (ANI = 79%, Nitrosomonas_3_A and Nitrosomonas_3_U).

Dereplication of MAGs from urea- and ammonia-fed systems resulted in three Nitrosomonas-like MAGs, one Nitrospira-NOB MAG, and two comammox Nitrospira-like MAGs. Filtered reads from the ammonia-fed system were mapped to the set of dereplicated MAGs, revealing that all nitrifier MAGs had 99% breadth of coverage (i.e., percent of genome covered by reads) in both systems. However, the comammox MAG that was assembled only from the urea-fed sample (Nitrospira_F2_U) had very low relative abundance (0.065%) in the ammonia-fed system, which could explain why it was not assembled. Comparably, relative abundances of comammox Nitrospira MAGs, Nitrospira_F1_A/Nitrospira_F1_U and Nitrospira_F2_U, were approximately 12- and 5-fold higher in the urea-fed system (~7.81% Nitrospira_F1_A/Nitrospira_F1_U, 0.30% Nitrospira_F2_U) than in the ammonia-fed system (~0.66 Nitrospira_F1_A/ Nitrospira_F1_U, 0.065% Nitrospira_F2_U). These results align with both the qPCR-based abundance of comammox Nitrospira and abundance of comammox-like ASVs 6 and 46 in the urea-fed system being substantially higher than their abundance in the ammonia-fed system. Thus, based on abundance trends of the comammox-like ASVs 6 and 46 and comammox MAGs, we associate ASV 6 with the comammox Nitrospira population belonging to Nitrospira_F1_A/Nitrospira_F1_U while ASV 46 is associated with Nitrospira_F2_U.

Similar to our previous study, comammox MAGs (Nitrospira_F1_A, Nitrospira_F1_U, and Nitrospira_F2_U) contained genes for urea degradation (ureCAB) and transportation (urtACBCDE). Strict AOB MAGs Nitrosomonas_1_A and Nitrosomonas_1_U also possessed these genes for ureolytic activity, which aligns with their sequence similarity to and clustering with Nitrosomonas ureae. The other Nitrosomonas MAGs (Nitrosomonas_2_A, Nitrosomonas_2_U, Nitrosomonas_3_A, and Nitrosomonas_3_U) only encoded a single urea accessory gene (ureJ) and gene encoding for urea carboxylase. An unbinned Nitrosomonas-associated ureC gene was found in the metagenome assembly from the urea-fed system, suggesting that another urease-positive strict AOB MAGs could have been present in the system. Nitrospira MAGs (Nitrospira_D1_A and Nitrospira_D1_U) did not contain urease genes; however, unbinned genes for ureA with 100% sequence ID match to strict NOB Nitrospira lenta were detected in the metagenome assembly for both samples, suggesting that Nitrospira-NOB were urease-positive.

DISCUSSION

Nitrite accumulation in ammonia-fed but not urea-fed system may be associated with NOB inhibition and the rate of ammonia production from urea

Strict AOB and Nitrospira-NOB were the dominant nitrifiers in the ammonia-fed systems and particularly at higher ammonia concentrations with the ammonia oxidation rates being consistently higher than the nitrite oxidation rates leading to nitrite accumulation. While nitrite accumulation occurred in the ammonia-fed reactor for condition 3, Nitrospira-NOB were more abundant than both AOB and comammox Nitrospira. It could be possible that despite their high abundance, Nitrospira-NOB were impacted by higher ammonia concentrations of conditions 2 and 3. Fujitani et al. (54) observed that the average Km value for nitrite (0.037 mg/L) attributed to a Nitrospira-NOB strain originating from a drinking water treatment plant increased fivefold to approximately 0.18 mg-N/L NO2 in the presence of free ammonia concentrations around 0.85 mg NH3-N/L (54). Thus, decreased nitrite affinity could have impacted the ability of this Nitrospira strain to oxidize low nitrite concentrations depending on the concentration of free ammonia. Further, in wastewater systems, suppression of strict NOB activity can be achieved at ammonia concentrations higher than 5 mg-N/L (55). Here, in the ammonia-fed system, average ammonia concentrations observed in the top section of the reactor during conditions 2 (0.89 mg NH3/L) and 4 (2.64 mg NH3/L) were in line with free ammonia concentrations shown to impact nitrite affinity of Nitrospira-NOB strain KM1 in Fujitani et al. (54), thus explaining nitrite accumulation. In the urea-fed system, urease-positive nitrifiers, including comammox Nitrospira and Nitrospira-NOB, regulated ammonia production and, thus, potentially controlled ammonia availability. While ammonia did accumulate during the highest nitrogen concentration in the urea-fed reactor, unlike the ammonia-fed reactors, comammox Nitrospira abundance did not decrease, and there was no nitrite accumulation. This is likely because the highest ammonia concentrations in the urea-fed reactor were consistently lower than the highest concentrations in the ammonia-fed reactors, and thus, comammox Nitrospira were not outcompeted by AOB and both comammox and Nitrospira-NOB were likely not inhibited.

Increased ammonia availability in ammonia-fed reactor detrimentally impacted comammox populations

Consistent with the reported higher ammonia affinity (i.e., lower Km(app)) of comammox Nitrospira compared to strict AOB (1416), comammox Nitrospira did indeed dominate over AOB only during the lowest nitrogen concentration in the ammonia-fed system. Though strict AOB were affiliated with Nitrosomonas cluster 6a characterized with higher ammonia affinities (Km(app) = 0.24–3.6 µM) (53) compared to other AOB, the reported ammonia affinity for comammox Nitrospira is still substantially higher for comammox Nitrospira (Km(app) = 63 nM). In addition to ammonia affinity, it is very likely that ammonia tolerance played a role as the partial inhibition of ammonia oxidation activity by Ca. Nitrospira kreftii has been reported at ammonia concentrations as low as 0.425 mg/L, which is within the range of ammonia concentrations observed in the ammonia-fed reactor (0.25–2 mg-N/L) during conditions 2 and 3. However, ammonia sensitivity resulting in the partial inhibition of ammonia oxidation has not been observed for Ca. Nitrospira inopinata (16) and Ca. Nitrospira nitrosa-like comammox Nitrospira in wastewater systems where ammonia concentrations are higher (2, 3, 19). Comammox Nitrospira in this study may be adapted to low ammonia concentrations and were most similar to other clade A1 comammox Nitrospira obtained from low ammonia environments. Thus, continuous exposure to elevated ammonia concentrations could play a role in the observed reduction in the abundance of comammox Nitrospira via inhibition.

Increase in urea concentration favored Nitrospira bacteria including comammox Nitrospira

Comammox Nitrospira were the dominant nitrifier across all conditions in the urea-fed system with their overall abundance significantly higher in the urea-fed system compared to their abundance in the ammonia-fed system. Favorable conditions under urea-fed conditions for comammox Nitrospira were also supported by the highest abundances of comammox Nitrospira consistently observed in the top of the urea-fed reactor where urea was most available and the emergence of a second low abundance comammox population in the urea-fed reactor. Our observation is similar to other reports of enrichment of very different comammox populations at much higher urea concentrations (22, 23). Though we are unable to identify the exact reason for comammox Nitrospira enrichment on urea, it could be a combination of metabolic traits associated with urea uptake and utilization. Specifically, comammox Nitrospira may balance the rate of ammonia production from urea with its ammonia oxidation rate, thus maximizing ammonia availability while also maintaining ammonia concentrations at non-inhibitory levels. Further, additional urea transporters are found in comammox genomes that are absent in other Nitrospira including an outer-membrane porin (fmdC) for uptake of short-chain amides and urea at low concentrations and a urea carboxylase-related transport (uctT) (21). Thus, the enhanced ability to uptake urea and regulate its conversion to ammonia balanced with its ammonia oxidation rates may underpin comammox Nitrospira preference for urea. Estimating the kinetic parameters such as comammox Nitrospira’s affinity for urea and uptake rate relative to other nitrifiers and ammonia production relative to its own ammonia oxidation rates would be extremely useful for assessing their overall preference for urea.

Nitrogen source drives potential competitive and co-operative dynamics between aerobic nitrifiers

In these continuous flow reactors and our previous batch microcosm experiments (1), we observed nitrogen source-dependent dynamics between the abundance of comammox Nitrospira and Nitrospira-NOB. We hypothesized that tight metabolic coupling exists between strict AOB and Nitrospira-NOB when urea is supplied due to reciprocal feeding between the two groups. Here, the production of nitrite can be controlled by urease-positive Nitrospira-NOB via cross-feeding ammonia to strict AOB, which in turn provide nitrite at a rate at which Nitrospira-NOB can consume it. This dynamic between canonical nitrifiers substantially contrasts with their relationship when only ammonia is provided as Nitrospira-NOB are fully dependent on strict AOB to provide them nitrite. Therefore, a negative relationship between comammox and canonical NOB Nitrospira when only ammonia is available may reflect comammox Nitrospira limiting Nitrospira-NOB access to nitrite (produced by AOB) by performing complete ammonia oxidation to nitrate. In contrast, at high ammonia concentrations, comammox Nitrospira may in fact be a source of nitrite for Nitrospira-NOB as their ammonia oxidation rates are faster than their nitrite oxidation rates, and their affinities for nitrite are lower than that of Nitrospira-NOB (13, 56). Supplementation with urea eliminates this potential comammox-NOB negative association as both nitrifiers are urease-positive and potentially produce ammonia themselves for different purposes (i.e., comammox produce their own ammonia; strict NOB provide ammonia to strict AOB). Competition for urea would then be determined by the urea affinity and uptake rates, which are currently unknown. However, in this study, we show that the increased abundance of comammox Nitrospira did not result in the decreased abundance of Nitrospira-NOB in the urea-fed system. This suggests that the apparent competitive dynamics between these nitrifiers is reduced when an alternative nitrogen source is available compared to ammonia which induced a competitive relationship.

In this study, the impact of nitrogen source and availability on nitrifying communities was evaluated in continuous flow column reactors, supplied with either ammonia or urea and operated over three different nitrogen concentrations. Consistent with our previous batch microcosm experiments (1), we show that different nitrogen sources and concentrations distinctly shape the nitrifying community. Direct supply of ammonia favored a combination of AOB and NOB particularly as the nitrogen concentrations were increased, with a decrease in comammox Nitrospira abundance likely associated with ammonia-based inhibition. Ammonia availability has been considered an important niche differentiating factor between comammox Nitrospira and strict AOB, and here, we show that it may also be a significant factor in shaping populations of comammox Nitrospira. In contrast, the urea provision promoted the abundance of multiple comammox populations along with strict AOB and Nitrospira-NOB. With urea as a nitrogen source, nitrification can be initiated by urease-positive nitrifiers controlling ammonia production and its availability, which in turn significantly impacted nitrification process performance.

ACKNOWLEDGMENTS

This work was supported by the NSF Graduate Research Fellowship and Cochrane Fellowship to K.V. and by NSF Award number 2203731.

Contributor Information

Ameet J. Pinto, Email: ameet.pinto@ce.gatech.edu.

Erik F. Y. Hom, University of Mississippi, University, Mississippi, USA

DATA AVAILABILITY

Raw fastq files for amplicon sequencing and metagenomic sequencing data, metagenomic assembly, and curated MAGs are available via NCBI bioproject submission number PRJNA1027363.

SUPPLEMENTAL MATERIAL

The following material is available online at https://doi.org/10.1128/spectrum.03181-23.

Supplemental information. spectrum.03181-23-s0001.docx.

Supplemental tables and figures.

DOI: 10.1128/spectrum.03181-23.SuF1

ASM does not own the copyrights to Supplemental Material that may be linked to, or accessed through, an article. The authors have granted ASM a non-exclusive, world-wide license to publish the Supplemental Material files. Please contact the corresponding author directly for reuse.

REFERENCES

  • 1. Vilardi KJ, Cotto I, Sevillano M, Dai Z, Anderson CL, Pinto A. 2022. Comammox Nitrospira bacteria outnumber canonical nitrifiers irrespective of electron donor mode and availability in biofiltration systems. FEMS Microbiol Ecol 98:fiac032. doi: 10.1093/femsec/fiac032 [DOI] [PubMed] [Google Scholar]
  • 2. Cotto I, Vilardi KJ, Huo L, Fogarty EC, Khunjar W, Wilson C, De Clippeleir H, Gilmore K, Bailey E, Lücker S, Pinto AJ. 2023. Low diversity and microdiversity of comammox bacteria in wastewater systems suggest specific adaptations within the Ca. Water Res 229:119497. doi: 10.1016/j.watres.2022.119497 [DOI] [PubMed] [Google Scholar]
  • 3. Cotto I, Dai Z, Huo L, Anderson CL, Vilardi KJ, Ijaz U, Khunjar W, Wilson C, De Clippeleir H, Gilmore K, Bailey E, Pinto AJ. 2020. Long solids retention times and attached growth phase favor prevalence of comammox bacteria in nitrogen removal systems. Water Res 169:115268. doi: 10.1016/j.watres.2019.115268 [DOI] [PubMed] [Google Scholar]
  • 4. Fowler SJ, Palomo A, Dechesne A, Mines PD, Smets BF. 2018. Comammox Nitrospira are abundant ammonia oxidizers in diverse groundwater-fed rapid sand filter communities. Environ Microbiol 20:1002–1015. doi: 10.1111/1462-2920.14033 [DOI] [PubMed] [Google Scholar]
  • 5. Palomo A, Jane Fowler S, Gülay A, Rasmussen S, Sicheritz-Ponten T, Smets BF. 2016. Metagenomic analysis of rapid gravity sand filter microbial communities suggests novel physiology of Nitrospira spp. ISME J 10:2569–2581. doi: 10.1038/ismej.2016.63 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 6. Poghosyan L, Koch H, Lavy A, Frank J, van Kessel M, Jetten MSM, Banfield JF, Lücker S. 2019. Metagenomic recovery of two distinct comammox Nitrospira from the terrestrial subsurface. Environ Microbiol 21:3627–3637. doi: 10.1111/1462-2920.14691 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 7. Zheng M, Tian Z, Chai Z, Zhang A, Gu A, Mu G, Wu D, Guo J. 2023. Ubiquitous occurrence and functional dominance of comammox Nitrospira in full-scale wastewater treatment plants. Water Res 236:119931. doi: 10.1016/j.watres.2023.119931 [DOI] [PubMed] [Google Scholar]
  • 8. Wang Y, Ma L, Mao Y, Jiang X, Xia Y, Yu K, Li B, Zhang T. 2017. Comammox in drinking water systems. Water Res 116:332–341. doi: 10.1016/j.watres.2017.03.042 [DOI] [PubMed] [Google Scholar]
  • 9. Pinto AJ, Marcus DN, Ijaz UZ, Bautista-de Lose Santos QM, Dick GJ, Raskin L. 2016. Metagenomic evidence for the presence of comammox Nitrospira-like bacteria in a drinking water system. mSphere 1:e00054-15. doi: 10.1128/mSphere.00054-15 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 10. Pérez J, Lotti T, Kleerebezem R, Picioreanu C, van Loosdrecht MCM. 2014. Outcompeting nitrite-oxidizing bacteria in single-stage nitrogen removal in sewage treatment plants: a model-based study. Water Res 66:208–218. doi: 10.1016/j.watres.2014.08.028 [DOI] [PubMed] [Google Scholar]
  • 11. Seuntjens D, Han M, Kerckhof F-M, Boon N, Al-Omari A, Takacs I, Meerburg F, De Mulder C, Wett B, Bott C, Murthy S, Carvajal Arroyo JM, De Clippeleir H, Vlaeminck SE. 2018. Pinpointing wastewater and process parameters controlling the AOB to NOB activity ratio in sewage treatment plants. Water Res 138:37–46. doi: 10.1016/j.watres.2017.11.044 [DOI] [PubMed] [Google Scholar]
  • 12. Sliekers AO, Haaijer SCM, Stafsnes MH, Kuenen JG, Jetten MSM. 2005. Competition and coexistence of aerobic ammonium- and nitrite-oxidizing bacteria at low oxygen concentrations. Appl Microbiol Biotechnol 68:808–817. doi: 10.1007/s00253-005-1974-6 [DOI] [PubMed] [Google Scholar]
  • 13. Daims H, Lebedeva EV, Pjevac P, Han P, Herbold C, Albertsen M, Jehmlich N, Palatinszky M, Vierheilig J, Bulaev A, Kirkegaard RH, von Bergen M, Rattei T, Bendinger B, Nielsen PH, Wagner M. 2015. Complete nitrification by Nitrospira bacteria. Nature 528:504–509. doi: 10.1038/nature16461 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 14. Ghimire-Kafle S, Weaver ME, Bollmann A. 2023. Ecophysiological and genomic characterization of the freshwater complete ammonia oxidizer Nitrospira sp. strain BO4. Appl Environ Microbiol 89:e0196522. doi: 10.1128/aem.01965-22 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 15. Sakoula D, Koch H, Frank J, Jetten MSM, van Kessel M, Lücker S. 2021. Enrichment and physiological characterization of a novel comammox Nitrospira indicates ammonium inhibition of complete nitrification. ISME J 15:1010–1024. doi: 10.1038/s41396-020-00827-4 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 16. Kits KD, Sedlacek CJ, Lebedeva EV, Han P, Bulaev A, Pjevac P, Daebeler A, Romano S, Albertsen M, Stein LY, Daims H, Wagner M. 2017. Kinetic analysis of a complete nitrifier reveals an oligotrophic lifestyle. Nature 549:269–272. doi: 10.1038/nature23679 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 17. Roots P, Wang Y, Rosenthal AF, Griffin JS, Sabba F, Petrovich M, Yang F, Kozak JA, Zhang H, Wells GF. 2019. Comammox Nitrospira are the dominant ammonia oxidizers in a mainstream low dissolved oxygen nitrification reactor. Water Res 157:396–405. doi: 10.1016/j.watres.2019.03.060 [DOI] [PubMed] [Google Scholar]
  • 18. Camejo PY, Santo Domingo J, McMahon KD, Noguera DR. 2017. Genome-enabled insights into the ecophysiology of the comammox bacterium Candidatus Nitrospira nitrosa. mSystems 2:e00059-17. doi: 10.1128/mSystems.00059-17 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 19. Vilardi K, Cotto I, Bachmann M, Parsons M, Klaus S, Wilson C, Bott CB, Pieper KJ, Pinto AJ. 2023. Co-occurrence and cooperation between comammox and anammox bacteria in a full-scale attached growth municipal wastewater treatment process. Environ Sci Technol 57:5013–5023. doi: 10.1021/acs.est.2c09223 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 20. Solomon C, Collier J, Berg G, Glibert P. 2010. Role of urea in microbial metabolism in aquatic systems: a biochemical and molecular review. Aquat. Microb. Ecol 59:67–88. doi: 10.3354/ame01390 [DOI] [Google Scholar]
  • 21. Palomo A, Pedersen AG, Fowler SJ, Dechesne A, Sicheritz-Pontén T, Smets BF. 2018. Comparative genomics sheds light on niche differentiation and the evolutionary history of comammox Nitrospira. ISME J 12:1779–1793. doi: 10.1038/s41396-018-0083-3 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 22. Li J, Hua Z-S, Liu T, Wang C, Li J, Bai G, Lücker S, Jetten MSM, Zheng M, Guo J. 2021. Selective enrichment and metagenomic analysis of three novel comammox Nitrospira in a urine-fed membrane bioreactor. ISME Commun 1:7. doi: 10.1038/s43705-021-00005-3 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 23. Zhao Y, Hu J, Yang W, Wang J, Jia Z, Zheng P, Hu B. 2021. The long-term effects of using nitrite and urea on the enrichment of comammox bacteria. Sci Total Environ 755:142580. doi: 10.1016/j.scitotenv.2020.142580 [DOI] [PubMed] [Google Scholar]
  • 24. Koch H, Lücker S, Albertsen M, Kitzinger K, Herbold C, Spieck E, Nielsen PH, Wagner M, Daims H. 2015. Expanded metabolic versatility of ubiquitous nitrite-oxidizing bacteria from the genus Nitrospira. Proc Natl Acad Sci U S A 112:11371–11376. doi: 10.1073/pnas.1506533112 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 25. Smith EJ, Davison W, Hamilton-Taylor J. 2002. Methods for preparing synthetic freshwaters. Water Res 36:1286–1296. doi: 10.1016/s0043-1354(01)00341-4 [DOI] [PubMed] [Google Scholar]
  • 26. Stubbins A, Dittmar T. 2012. Low volume quantification of dissolved organic carbon and dissolved nitrogen. Limnol Ocean Methods 10:347–352. doi: 10.4319/lom.2012.10.347 [DOI] [Google Scholar]
  • 27. Hermansson A, Lindgren P-E. 2001. Quantification of ammonia-oxidizing bacteria in arable soil by real-time PCR. Appl Environ Microbiol 67:972–976. doi: 10.1128/AEM.67.2.972-976.2001 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 28. Graham DW, Knapp CW, Van Vleck ES, Bloor K, Lane TB, Graham CE. 2007. Experimental demonstration of chaotic instability in biological nitrification. ISME J 1:385–393. doi: 10.1038/ismej.2007.45 [DOI] [PubMed] [Google Scholar]
  • 29. Caporaso JG, Lauber CL, Walters WA, Berg-Lyons D, Lozupone CA, Turnbaugh PJ, Fierer N, Knight R. 2011. Global patterns of 16S rRNA diversity at a depth of millions of sequences per sample. Proc Natl Acad Sci U S A 108 Suppl 1:4516–4522. doi: 10.1073/pnas.1000080107 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 30. Parada AE, Needham DM, Fuhrman JA. 2016. Every base matters: assessing small subunit rRNA primers for marine microbiomes with mock communities, time series and global field samples. Environ Microbiol 18:1403–1414. doi: 10.1111/1462-2920.13023 [DOI] [PubMed] [Google Scholar]
  • 31. Apprill A, McNally S, Parsons R, Weber L. 2015. Minor revision to V4 region SSU rRNA 806R gene primer greatly increases detection of SAR11 bacterioplankton. Aquat Microb Ecol 75:129–137. doi: 10.3354/ame01753 [DOI] [Google Scholar]
  • 32. Callahan BJ, McMurdie PJ, Rosen MJ, Han AW, Johnson AJA, Holmes SP. 2016. DADA2: High-resolution sample inference from Illumina amplicon data. Nat Methods 13:581–583. doi: 10.1038/nmeth.3869 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 33. Quast C, Pruesse E, Yilmaz P, Gerken J, Schweer T, Yarza P, Peplies J, Glöckner FO. 2013. The SILVA ribosomal RNA gene database project: improved data processing and web-based tools. Nucleic Acids Res 41:D590–D596. doi: 10.1093/nar/gks1219 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 34. Chen S, Zhou Y, Chen Y, Gu J. 2018. fastp: an ultra-fast all-in-one FASTQ preprocessor. Bioinformatics 34:i884–i890. doi: 10.1093/bioinformatics/bty560 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 35. Danecek P, Bonfield JK, Liddle J, Marshall J, Ohan V, Pollard MO, Whitwham A, Keane T, McCarthy SA, Davies RM, Li H. 2021. Twelve years of SAMtools and BCFtools. Gigascience 10:giab008. doi: 10.1093/gigascience/giab008 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 36. Quinlan AR, Hall IM. 2010. BEDTools: a flexible suite of utilities for comparing genomic features. Bioinformatics 26:841–842. doi: 10.1093/bioinformatics/btq033 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 37. Nurk S, Meleshko D, Korobeynikov A, Pevzner PA. 2017. metaSPAdes: a new versatile metagenomic assembler. Genome Res 27:824–834. doi: 10.1101/gr.213959.116 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 38. Li H, Durbin R. 2009. Fast and accurate short read alignment with Burrows–Wheeler transform. Bioinformatics 25:1754–1760. doi: 10.1093/bioinformatics/btp324 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 39. Kang DD, Li F, Kirton E, Thomas A, Egan R, An H, Wang Z. 2019. MetaBAT 2: an adaptive binning algorithm for robust and efficient genome reconstruction from metagenome assemblies. PeerJ 7:e7359. doi: 10.7717/peerj.7359 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 40. Parks DH, Imelfort M, Skennerton CT, Hugenholtz P, Tyson GW. 2015. CheckM: assessing the quality of microbial genomes recovered from isolates, single cells, and metagenomes. Genome Res 25:1043–1055. doi: 10.1101/gr.186072.114 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 41. Parks DH, Chuvochina M, Waite DW, Rinke C, Skarshewski A, Chaumeil P-A, Hugenholtz P. 2018. A standardized bacterial taxonomy based on genome phylogeny substantially revises the tree of life. Nat Biotechnol 36:996–1004. doi: 10.1038/nbt.4229 [DOI] [PubMed] [Google Scholar]
  • 42. Hyatt D, Chen G-L, Locascio PF, Land ML, Larimer FW, Hauser LJ. 2010. Prodigal: prokaryotic gene recognition and translation initiation site identification. BMC Bioinformatics 11:119. doi: 10.1186/1471-2105-11-119 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 43. Kanehisa M, Sato Y, Kawashima M, Furumichi M, Tanabe M. 2016. KEGG as a reference resource for gene and protein annotation. Nucleic Acids Res 44:D457–D462. doi: 10.1093/nar/gkv1070 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 44. Aramaki T, Blanc-Mathieu R, Endo H, Ohkubo K, Kanehisa M, Goto S, Ogata H. 2020. KofamKOALA: KEGG Ortholog assignment based on profile HMM and adaptive score threshold. Bioinformatics 36:2251–2252. doi: 10.1093/bioinformatics/btz859 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 45. Na S-I, Kim YO, Yoon S-H, Ha S-M, Baek I, Chun J. 2018. UBCG: up-to-date bacterial core gene set and pipeline for phylogenomic tree reconstruction. J Microbiol 56:280–285. doi: 10.1007/s12275-018-8014-6 [DOI] [PubMed] [Google Scholar]
  • 46. Olm MR, Brown CT, Brooks B, Banfield JF. 2017. dRep: a tool for fast and accurate genomic comparisons that enables improved genome recovery from metagenomes through de-replication. ISME J 11:2864–2868. doi: 10.1038/ismej.2017.126 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 47. Pericard P, Dufresne Y, Couderc L, Blanquart S, Touzet H. 2018. MATAM: reconstruction of phylogenetic marker genes from short sequencing reads in metagenomes. Bioinformatics 34:585–591. doi: 10.1093/bioinformatics/btx644 [DOI] [PubMed] [Google Scholar]
  • 48. Edgar RC. 2010. Search and clustering orders of magnitude faster than BLAST. Bioinformatics 26:2460–2461. doi: 10.1093/bioinformatics/btq461 [DOI] [PubMed] [Google Scholar]
  • 49. Song W, Zhang S, Thomas T. 2022. MarkerMAG: linking metagenome-assembled genomes (MAGs) with 16S rRNA marker genes using paired-end short reads. Bioinformatics 38:3684–3688. doi: 10.1093/bioinformatics/btac398 [DOI] [PubMed] [Google Scholar]
  • 50. Camacho C, Coulouris G, Avagyan V, Ma N, Papadopoulos J, Bealer K, Madden TL. 2009. BLAST+: architecture and applications. BMC Bioinformatics 10:421. doi: 10.1186/1471-2105-10-421 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 51. RCoreTeam . 2014. R: a language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria. [Google Scholar]
  • 52. Oksanen Blanchet Kindt R, Legendre P, Minchin PR, O’Hara RB, Simpson GL, Solymos P, Stevens MHH, Wagner HJF. 2013. Vegan: community ecology package [Google Scholar]
  • 53. Koops H-P, Purkhold U, Pommerening-Röser A, Timmermann G, Wagner M. 2006. The Lithoautotrophic ammonia-oxidizing bacteria, p 778–811. In Dworkin M, Falkow S, Rosenberg E, Schleifer KH, Stackebrandt E (ed), The prokaryotes. Springer New York. [Google Scholar]
  • 54. Fujitani H, Momiuchi K, Ishii K, Nomachi M, Kikuchi S, Ushiki N, Sekiguchi Y, Tsuneda S. 2020. Genomic and physiological characteristics of a novel nitrite-oxidizing Nitrospira strain isolated from a drinking water treatment plant. Front Microbiol 11:545190. doi: 10.3389/fmicb.2020.545190 [DOI] [PMC free article] [PubMed] [Google Scholar]
  • 55. Poot V, Hoekstra M, Geleijnse MAA, van Loosdrecht MCM, Pérez J. 2016. Effects of the residual ammonium concentration on NOB repression during partial nitritation with granular sludge. Water Res 106:518–530. doi: 10.1016/j.watres.2016.10.028 [DOI] [PubMed] [Google Scholar]
  • 56. van Kessel M, Speth DR, Albertsen M, Nielsen PH, Op den Camp HJM, Kartal B, Jetten MSM, Lücker S. 2015. Complete nitrification by a single microorganism. Nature 528:555–559. doi: 10.1038/nature16459 [DOI] [PMC free article] [PubMed] [Google Scholar]

Associated Data

This section collects any data citations, data availability statements, or supplementary materials included in this article.

Supplementary Materials

Supplemental information. spectrum.03181-23-s0001.docx.

Supplemental tables and figures.

DOI: 10.1128/spectrum.03181-23.SuF1

Data Availability Statement

Raw fastq files for amplicon sequencing and metagenomic sequencing data, metagenomic assembly, and curated MAGs are available via NCBI bioproject submission number PRJNA1027363.


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