Abstract
Nitrous oxide (N2O), a driver of global warming and climate change, has reached unprecedented concentrations in Earth’s atmosphere1. Current N2O sources outpace N2O sinks, emphasizing the need for comprehensive understanding of processes that consume N2O. Microbes that express the enzyme N2O reductase (N2OR) convert N2O to climate change-neutral dinitrogen (N2). Known N2ORs belong to the canonical clade I and clade II NosZ reductases and are considered key enzymes for N2O reduction2,3,4. Here we report a previously unrecognized protein family with a role in N2O reduction, clade III lactonase-type N2OR (L-N2OR), which diverges in sequence from canonical NosZ but conserves three-dimensional protein structural features. Integrated physiological, metagenomic, proteomic and structural modelling studies demonstrate that L-N2ORs catalyse N2O reduction. L-N2OR genes occur in several phyla, predominantly in uncultured taxa with broad geographic distribution. Our findings expand the known diversity of N2ORs and implicate previously unrecognized taxa (for example, Nitrospinota) in N2O consumption. The expansion of N2OR diversity and the identification of a novel type of catalyst for N2O reduction advances the understanding of N2O sinks, has implications for greenhouse gas emission and climate change modelling, and expands opportunities for innovative biotechnologies aimed at curbing N2O emissions5,6.
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Data availability
The Sab enrichment culture metagenomic datasets (both Illumina and PacBio data) and the resulting closed genome of D. nosdiversum strain Sab5 are deposited under NCBI BioProject ID PRJNA1176277. The Sabana microcosm metagenomes are publicly available in NCBI Bioproject ID PRJNA901179. Illumina and PacBio datasets used for construction of a circular genome of S. acidovorans strain Mol are publicly available under NCBI BioProject ID PRJNA310710. Genome bins analysed in this study are from the Genome Taxonomy Database (https://gtdb.ecogenomic.org), a global soil genome bins database (https://microbma.github.io/project/SMAG.html) and an ocean genome bins database (https://doi.org/10.6084/m9.figshare.c.5564844.v1). Other genomes and raw metagenomic sequence reads analysed in this study are publicly available in the NCBI database. Lists of the datasets are summarized in Supplementary Tables 7, 8, 10–14, 16 and 17. The mass spectrometry proteomics raw data and sequence files are available at the ProteomeXchange Consortium via the MassIVE database with the unique dataset identifier MSV000096274. The metaproteomic search results are publicly available through the MassIVE database (ftp://massive-ftp.ucsd.edu/v07/MSV000096274/).
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Acknowledgements
The authors acknowledge funding through the Dimensions of Biodiversity programme of the US National Science Foundation (awards 1831599 to F.E.L. and 1831582 to K.T.K.). G.H., W.W. and Y.X. received financial support from the China Scholarship Council. M.E.D. is recipient of a US National Science Foundation Graduate Research Fellowship. R.L.H. acknowledges support of the metaproteomics infrastructure from the Oak Ridge National Laboratory Plant-Microbe Interfaces Science Focus Area funded by the US Department of Energy Biological and Environmental Research Genome Sciences Program. J.M.P. was supported by the Laboratory Directed Research and Development programme at Oak Ridge National Laboratory, which is managed by UT-Battelle under contract DE-AC05-00OR22725 for the US Department of Energy.
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G.H. and F.E.L. conceptualized the research. F.E.L. supervised the project. F.E.L. and K.T.K. acquired funding. G.H., G.C., Y.X. and F.E.L. contributed to cultivation and analytical efforts. G.H. performed phenotypic characterizations and molecular analyses. G.H. and W.W. performed bioinformatic analyses with guidance from K.T.K., and G.H. and J.M.P. performed protein structural modelling. G.H., M.E.D. and R.L.H. performed proteomics analyses. All authors contributed to data analysis and interpretation. G.H. and F.E.L. wrote the manuscript with inputs from all authors. All authors read and approved the final version of the manuscript.
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Extended data figures and tables
Extended Data Fig. 1 Schematic of the workflow leading from Sabana forest soil to soil microcosms to solid-free Sab enrichment cultures.
Metagenome analysis of the original soil suggested tropical soils harbor diverse C-nosZ genes67. Efforts aimed at unraveling the microbiology of N2O consumption in Sabana soil microcosms experiencing different N2O feeding regimes revealed an incongruity between N2O consumption and nosZ abundance20. Twenty-five consecutive transfers starting with the Sabana soil microcosm experiencing a high N2O feeding regime yielded a Sab enrichment culture with robust N2O consumption activity. The Sab enrichment culture was incubated in 160 mL glass serum bottles containing 100 mL of basal salt medium amended with 0.02 g L−1 TSB, 5 mM fumarate, 10 mL (4.16 mM nominal; 416 µmol) H2, and 10 mL (4.16 mM nominal; 416 µmol) N2O. While the Sab enrichment culture exhibited robust N2O reduction activity, metagenomic investigations of Sab subcultures did not generate evidence for the presence of clade I or clade II C-nosZ.
Extended Data Fig. 2 Fumarate, H2, and N2O utilization in Sab enrichment cultures following 25 sequential transfers.
Panels a-e show fumarate consumption and the formation of acetate, propionate and succinate in medium amended with (a) fumarate, (b) fumarate + H2 + N2O, (c) fumarate + H2 + N2O + TSB, (d) fumarate + H2 + TSB, and (e) fumarate + N2O + TSB. Panels f-i depict H2 and N2O consumption in medium that received (f) fumarate + H2 + N2O, (g) fumarate + H2 + N2O + TSB, (h) fumarate + H2 + TSB, (i) fumarate + N2O + TSB. Data shown represent averages and standard deviations of triplicate cultures. Error bars are not visible when smaller than the symbols.
Extended Data Fig. 3 Phylogenomic analysis revealing the taxonomic affiliation of Desulfitobacterium nosdiversum strain Sab5.
(a) The phylogenomic analysis used 120 conserved bacterial marker genes and included Desulfitobacteriaceae genomes available in the NCBI database. The scale bar indicates 0.05 nucleotide substitutions per site. Bootstrap (BP) values are divided into the categories BP < 70 (solid black circles) and BP ≥ 90 (solid grey circles). (b) Line graph showing Single Copy Protein- (SCP-) based average amino acid identity (AAI) between the strain Sab5 genome and individual genomes included in the phylogenomic analysis, with the scale displayed on the x-axis. Values for each comparison between the strain Sab5 genome and related genomes are represented by black dots, with the comparison to itself being 100%.
Extended Data Fig. 4 Growth yield of Desulfitobacterium nosdiversum strain Sab5 and protein expression during growth with N2O.
(a) Growth yields were estimated by correlating L-nosZ gene copy numbers with amounts of N2O consumed. Cell suspension samples were collected following complete consumption of N2O from triplicate vessels. Strain Sab5 cell numbers were determined with a qPCR assay targeting the L-nosZ gene. The genome of strain Sab5 contains a single L-nosZ gene, and L-nosZ gene counts equal the cell numbers. Sab enrichment cultures produced (6.8 ± 0.77) × 109 Desulfitobacterium nosdiversum strain Sab5 cells mmol N2O−1, equivalent to a growth yield (dry weight) of 4.21 ± 0.48 mg mmol N2O−1 (assuming a dry weight of 6.13 × 10−10 mg per cell27). The gray shading indicates the 95% confidence intervals around the mean values. (b) Metaproteomic analysis assigned 1,720 proteins to Desulfitobacterium nosdiversum strain Sab5 cells collected from Sab enrichment cultures grown with 5 mM fumarate, 0.02 g L−1 TSB, 4.16 mM (nominal) H2, and 4.16 mM (nominal) N2O for 3 days when >50% of the initial N2O dose had been consumed. L-NosZ, MacB type ATP-binding cassette (ABC) transporter, c-type cytochrome (K03888), b-type cytochrome (K00412), AtoC (K07714) and SasA (COG4191) were all detected (red arrows), in addition to a protein of unknown function encoded by a gene neighboring L-nosZ. The curved line shows the Log2 transformed protein abundances, and the vertical lines represent the standard deviation of triplicate cultures.
Extended Data Fig. 5 Growth and N2O reduction in cultures of Sporomusa acidovorans strain Mol.
Panels a-d show growth of Sporomusa acidovorans strain Mol and N2O consumption at different O2 partial pressures and pH conditions. (a) Growth of strain Mol at pH 7 with aqueous phase O2 concentrations of 0, 4.55 µM (355 Pa), 9.1 µM (709 Pa), 22.75 µM (1,780 Pa), and 45.5 µM (3,550 Pa). (b) N2O consumption in bottles with different O2 partial pressures at pH 7. The growth medium was prepared anoxically, and O2 was introduced by injecting 0, 1, 2, 5, 10 ml of air (i.e., 21% O2, v/v). (c) Growth of strain Mol in medium with the pH adjusted to 3.5, 4.5, 5.5, 6.5, 7.5, and 8.5. (d) N2O consumption observed at the different medium pH values. Panels e-h depict strain Mol cultures grown in basal salt medium amended with 1 g l−1 yeast extract in the presence of different amounts of N2O. (e) N2O consumption, (f) growth, and (g) acetate production in Sporomusa acidovorans cultures, with each set of triplicate cultures receiving different amounts of N2O. Acetate production was measured in samples withdrawn from cultures on day 14. (h) Correlation between N2O consumption and acetate yields. A linear regression was performed (blue line with 95% confidence interval), yielding a significant positive correlation (R² = 0.90, p = 2.07 × 10−6). No N2O consumption was observed in control vessels that received autoclaved inocula or in live cultures amended with 6 mL (v/v, 10%) acetylene. Data shown represent averages and standard deviations of triplicate cultures. Error bars are not shown when smaller than the symbols. Pairwise comparisons were performed using two-sided Student’s t-tests with p values adjusted for multiple testing using the Holm-Bonferroni method120.
Extended Data Fig. 6 AlphaFold models of L-NosZ and the MacB-type ABC transporter.
Panels a-f show Cu-binding active sites in C-NosZ derived from a 1.7 Å X-ray crystal structure of Pseudomonas stutzeri (PsNosZ, PDB entry 3SBQ) and representative AlphaFold3 models of apo L-NosZ of Desulfitobacterium nosdiversum strain Sab5 and Sporomusa acidovorans strain Mol. (a) CuA site in Pseudomonas stutzeri NosZ; (b) putative CuA site in Desulfitobacterium nosdiversum strain Sab5 NosZ; (c) putative CuA site in Sporomusa acidovorans strain Mol NosZ; (d) the CuZ site in Pseudomonas stutzeri NosZ; (e) putative CuZ site in Desulfitobacterium nosdiversum strain Sab5 NosZ; (f) putative CuZ site in Sporomusa acidovorans strain Mol NosZ. The root-mean-square deviations (RMSDs) between paired H130 in 3SBQ and either H117 in Desulfitobacterium nosdiversum strain Sab5 L-NosZ or H126 in Sporomusa acidovorans strain Mol NosZ (indicated by red arrows) are higher than other paired histidine residues because H117 and H126 originate from different ß-strands in the C-NosZ and L-NosZ enzymes, respectively. Although the position and relative orientation of this histidine residue differ, it is expected to coordinate Cu3 (see panel d) in a similar manner. Specifically, H129 and H130 in the PsNosZ X-ray structure are located on the same ß-strand. In comparison, H116 and H117 in the model of NosZ from Desulfitobacterium nosdiversum strain Sab5 are located on the same ß-strand. Similarly, H125 and H126 in Sporomusa acidovorans strain Mol NosZ model come from the same ß-strand. Panels g-h show a crystal structure and AlphaFold model of MacB-type ABC transporter. (g) Homodimeric crystal structure of the ABC transporter MacB from Acinetobacter baumannii (PDB entry 5WS4). (h) AlphaFold2 model of the putative MacB transporter encoded on the Desulfitobacterium nosdiversum strain Sab5 genome generated using ColabFold with 5WS4 as a template. The model is a dimer of homodimers comprising four monomers, i.e., two copies of MacB and two copies of the ABC-type transporter. (i) Predicted aligned error (PAE) for the MacB transporter protein chains A, B, C, D, with lower PAE values (blue) indicating higher model confidence. The predicted local distance difference test (pLDDT) scores, a per-residue measure of local confidence, are indicated by colors.
Extended Data Fig. 7 Features differentiating L-NosZ from C-NosZ sequences.
(a) Maximum likelihood phylogenetic tree based on protein sequences of clade I C-NosZ (n = 105), clade II C-NosZ (n = 68) and clade III L-NosZ (n = 95). The phylogenetic analysis included 1,451 sites. The colored dots at the nodes indicate the RaxML-ng bootstrap values; bootstrap values > 90% are not shown. The tree scale bar represents the mean number of amino acid substitution per site. (b) The CuA motifs involved in electron transfer to the CuZ site are 100% conserved (CXXFCXXXHXEM) in C-NosZ and L-NosZ. (c) Independent alignments of C-NosZ and L-NosZ sequences showing differences in conserved histidine residues associated with the CuZ site. The copper binding sites, CuA and CuZ, were inferred based on analysis of X-ray crystal structure data121. The height of the symbols (i.e., the size of letter abbreviations for amino acids) reflects the relative frequency of the amino acid at that position. The multiple sequence alignment plots were created with ggmsa104.
Extended Data Fig. 8 Population genome-resolved and metagenomic read-resolved surveys of the environmental distribution of L-nosZ.
Bars show metagenomic reads (%) recruited to the clade III L-NosZ-encoding genomes. The x-axis displays the metagenome accession IDs. Relevant information on metagenomes and genome bins is summarized in Supplementary Tables 13 and 14, respectively. The numbers above each bar indicate the MAGs used as reference genomes in metagenome recruitment analysis. The 16 MAGs detected along with the highest taxonomic classification are represented by numbers. (1) GCA009782775 (Desulfovibrionaceae); (2) GCA015231995 (Nitrospinota); (3) GCA016223025 (Gallionellaceae); (4) GCA015232395 (Magnetococcales); (5) GCA008933335 (Casimicrobiaceae); (6) GCA001804905 (Nitrospinota); (7) GCA011052055 (Nitrospinota); (8) GCA016214995 (Desulfobacterota); (9) GCA016200645 (Desulfobacterota); (10) GCA024244705 (Alphaproteobacteria); (11) GCA011051655 (Chromatiales); (12) GCA016218475 (Gallionella); (13) GCA031269345 (Frigididesulfovibrio); (14) GCA030739775 (Alphaproteobacteria); (15) GCA003450795 (Desulfobacterota); (16) GCA016191995 (Rubrivivax). Individual genome bins are distinguished by colors. The world map inset shows the geographic distribution of 1,053 metagenomes representing 12 distinct biomes from six continents. The pie charts indicate the normalized clade I (red), clade II (green), and clade III (blue) nosZ counts relative to the total nosZ counts in each metagenome, with the radii indicating the total nosZ counts per metagenome. A nosZ phylotype was inferred based on the phylogenetic placement on the GraftM NosZ reference tree (Extended Data Fig. 7).
Extended Data Fig. 9 nosZ transcripts detected in the Tara Oceans metatranscriptome (Ocean metaT) dataset53.
To explore nosZ expression, an HMM was built from 173 C-NosZ and 95 L-NosZ sequences to search the protein sequences provided in the Ocean metaT dataset. Transcripts with expression levels higher than 1 RPKM were considered expressed and are represented in the graphs. The search and filtering criteria resulted in a total of four clade I-type sequences (NosZ transcripts 1-4), three clade II-type sequences (NosZ transcripts 5-7), and one clade III-type sequence (NosZ transcript 8). Relevant metadata (e.g., dissolved O2 concentrations) corresponding to the metatranscriptomes were obtained from the Ocean metaT dataset. The taxonomic assignments of each NosZ transcript are: NosZ_1 (Gammaproteobacteria); NosZ_2 (Gammaproteobacteria); NosZ_3 (Unclassified bacteria); NosZ_4 (Unclassified bacteria); NosZ_5 (Flavobacteriaceae); NosZ_6 (Bacteroides); NosZ_7 (Unclassified bacteria); NosZ_8 (Nitrospinota). The dissolved O2 concentrations varied in the Tara Oceans sampling locations: Arctic Ocean (200 µM <c[O2] <400 µM); Indian Ocean (c[O2] <4 µM); North Pacific Ocean (c[O2] <3 µM); South Pacific Ocean (3 µM <c[O2] <250 µM). The transcriptome accession IDs correspond to the Ocean metaT dataset.
Extended Data Fig. 10 Potential utilization of electron acceptors by bacteria represented by genome bins harboring clade III L-nosZ and their predicted O2 preference.
The tree was constructed using the GTDB-TK workflow79. The scale bar represents the mean number of amino acid substitution per site. Terminal reductases investigated include nitrate reductase (encoded by napAB or narGHIJ), NO-forming nitrite reductase (nirK or nirS), ammonium-forming nitrite reductase (nrfAH), sulfate adenylytransferase (sat), and dissimilatory sulfite reductase (dsrAB) based on the annotations derived from eggNOG database v5122. Seven curated HMMs, comprising genes encoding nitric oxide reductases (NOR, NO → N2O)123, were queried against the protein sequences. The resulting NOR sequences were then filtered by conserved motif sequences in the different NOR families (i.e., cNOR, qNOR, gNOR, nNOR, sNOR, bNOR and eNOR). Genes encoding bacterial high affinity (ccoNOP and cydAB) and low affinity (ctaABCDE) oxidases catalyzing the reduction of O2 reduction were also investigated58. Bacteria represented by genome bins were classified as facultative and strict anaerobes with genome-based computational models using GenomeSpot v1.0.159, and the red squares indicate strict anaerobes. About two-thirds (n = 70) of the genome bins harbor NOR genes. Seventeen genome bins contain all genes required for complete denitrification (\({{\rm{NO}}}_{3}^{-}\) → \({{\rm{NO}}}_{2}^{-}\) → NO → N2O → N2).
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He, G., Wang, W., Chen, G. et al. A novel bacterial protein family that catalyses nitrous oxide reduction. Nature 646, 152–160 (2025). https://doi.org/10.1038/s41586-025-09401-4
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DOI: https://doi.org/10.1038/s41586-025-09401-4
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