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Structural basis for catalytic and inhibitory divergence between archaeal and bacterial ammonia monooxygenases

Xiaoyun YangiD, Tieqiang Mao, Zhi-Cong He, Yan CheniD, Guoping ZhaoiD, Peng JiniD, Shengying LiiD, Hongpo DongiD, Wei PengiD, Chuanlun ZhangiD, Zongqiang LiiD

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Abstract

Ammonia oxidation initiates nitrification and is closely linked to microbial N2O production. Ammonia monooxygenase (AMO) catalyzes the first and rate-limiting step of nitrification and is widespread across evolutionarily distinct ammonia-oxidizing archaea (AOA) and bacteria (AOB). The ocean is the largest biome for AOA and AOB, which have distinct ecological niches and markedly different sensitivities to nitrification inhibitors. However, the lack of archaeal AMO structures and inhibitor-bound AMO complexes has hindered mechanistic understanding of the architectural, catalytic, and inhibitory divergence between these two enzyme systems. Here, we report high-resolution cryo-electron microscopy (cryo-EM) structures of marine archaeal AMO captured in active and inactivated states within its native membrane environment, together with inhibitor-bound structures of estuarine bacterial AMO. Archaeal AMO forms an unexpected cup-shaped homotrimer composed of eight subunits per protomer and exhibits substantial architectural divergence from bacterial AMO. Integrated structural, biochemical, kinetic, and computational analyses reveal distinct periplasmic architectures, copper-center organization, and hydrophobic channels between archaeal and bacterial AMOs for ammonium acquisition, catalysis and inhibitor response. These findings provide a structural and mechanistic framework for understanding how archaeal and bacterial AMOs have diverged to distinct ammonia-oxidizing strategies and inhibitor susceptibilities across environmentally important ammonia oxidizers.

In-depth summary

Claude Opus 5.5 · xhigh effort · 8 Nov 2026 · from the full text of version 1 (1 Sept 2026) · CC BY 4.0

Archaeal ammonia monooxygenase (AMO) is a cup-shaped homotrimer using a mononuclear CuD site; inhibitors bind bacterial AMO's dicopper center directly but apparently inactivate archaeal AMO indirectly by relocating copper.

Ammonia-oxidizing archaea (AOA) and bacteria (AOB) differ in ammonium affinity and in sensitivity to nitrification inhibitors, yet only bacterial ammonia monooxygenase (AMO) structures existed and no inhibitor-bound AMO had been solved. This work adds native-membrane cryo-EM structures of a marine archaeal AMO, active and inactivated, plus inhibitor-bound structures of an estuarine bacterial AMO, linked to kinetics, mutagenesis and quantum-chemical calculations.

Key results

  1. ShownArchaeal AMO from Nitrosopumilus maritimus SCM1 (NmAMO) forms a cup-shaped homotrimer with eight subunits per protomer. Beyond a core shared with bacterial AMO, it carries a newly identified single-helix subunit (AmoE) and an unassigned subunit (AmoH) that closes the cytoplasmic base.

    Native-membrane cryo-EM map at 2.88 Å; 51 transmembrane helices, a slightly larger assembly than bacterial AMO; NmAmoB keeps only its N-terminal cupredoxin domain, which flattens the extracellular face; AmoF/AmoG heterodimers clamp neighbouring protomers; trimers pack in hexagonal arrays in isolated membranes. · Overall structure of archaeal AMO; Image processing

  2. ShownBacterial AMO (Nitrosomonas halophila ZJB1, NhAMO) is inhibited directly: DMP (dephosphorylated DMPP) and allylthiourea (ATU) bridge the CuC-CuD dicopper center and set off a residue lid closing the hydrophobic channel entrance; the bound inhibitor also splits the channel into two isolated segments.

    Cryo-EM structures at 2.15 Å (DMP) and 2.47 Å (ATU). CuC-CuD distance is 7.9 Å without inhibitor, 3.9 Å with DMP and 4.7 Å with ATU. Channel volume is 3,135 Å^3 vs 1,774 Å^3 with DMP. Mutating lid residues (R209, E218, R145) lowered ammonia oxidation by ~30%; mutating aromatic-cluster residues (F157, F161, F220, F228) also impaired activity. · Inhibition of bacterial AMO; Figure legends

  3. SuggestedArchaeal AMO appears to be inactivated indirectly. In the structure from ATU-treated cells no ATU density is seen at the active site; instead copper has moved from the CuD site to the CuC site, which the authors interpret as inhibitor-triggered copper relocation.

    2.75 Å structure of membrane-bound NmAMO from N. maritimus grown with 1000 μM ATU: same overall fold as the active state, no ATU density at the active site, copper absent at CuD and present at CuC. ICP copper content is unchanged vs the active enzyme. Across five inhibitors, AOB were strongly inhibited while AOA were suppressed only at high concentrations. · Inactivated structure of archaeal AMO; Two distinct pathways of AMO inactivation; Inhibitor activity assays; Archaeal membrane fraction extraction and…

  4. ShownThe two AMOs capture ammonium differently. NmAMO lacks the C-terminal cupredoxin domain (its structural counterpart, Nmar_1504, is a separate soluble protein) and binds less ammonium but with higher affinity. This matches higher affinity and lower maximal rates for N. maritimus than for AOB.

    Electronegative periplasmic surface ~50% smaller than NhAMO's. NmAMO cupredoxin domain bound ~30% less ammonium but with higher affinity by isothermal titration calorimetry. N. maritimus had significantly lower Km(app); AOB had higher Vmax and ammonia oxidation rates. Altering NhAMO periplasmic domains reduced activity. Seawater microcosms at 1 μM vs 10 μM NH4+ favoured AOA vs AOB. · Divergent ammonium capture in archaeal and…; Ammonium binding capacity of archaeal and…; Calculation of kinetic properties; Microcosm enrichment assay comparing the…

  5. SuggestedCalculations favour CuD as the archaeal catalytic copper and predict that a bacterial dicopper center oxidizes ammonia over lower energy barriers. Simulations give NmAMO a narrower hydrophobic channel than NhAMO.

    Active NmAMO has CuB and CuD occupied and CuC empty. Quantum-mechanical (QM) hydroxyl-amino coupling barrier is 13.6 kcal/mol from CuD vs 22.2 from CuC. On the dicopper path, NH3 hydrogen abstraction costs 9.7 and coupling 11.0 kcal/mol. Molecular dynamics minimum channel diameter is ~5.4 Å vs ~7.1 Å. Exit barrier is 34.9 vs 22.7 kcal/mol (computed for DMP per Extended Data Fig. 13). · Active center in archaeal AMO; Channel architecture and catalytic advantage of…; Umbrella sampling; Figure legends

Methods, data and reproducibility

Single-particle cryo-EM of native membranes from Nitrosopumilus maritimus SCM1 (untreated or ATU-treated) and of purified Nitrosomonas halophila ZJB1 AMO bound to DMP or ATU, plus copper ICP-MS, ammonium-binding and calorimetry assays, whole-cell kinetics, mutagenesis, lipidomics, proteomics, molecular dynamics and QM/MM calculations.

  • Nitrosopumilus maritimus SCM1 cultures (marine AOA) for native-membrane cryo-EM, kinetics, inhibitor assays, lipidomics and proteomics · Nitrosopumilus maritimus SCM1 (archaeon) · n = 70 L culture harvested for membranes
  • Nitrosomonas halophila ZJB1 (estuarine AOB isolated by the authors) expressing Flag-tagged AmoA, for AMO-inhibitor complexes; plus site-directed mutant strains · Nitrosomonas halophila ZJB1 · n = 120 L culture; seven kanamycin-resistant mutant strains
  • Nitrosomonas europaea cultures for kinetic, activity and proteomic comparisons · Nitrosomonas europaea
  • Cryo-EM datasets: NhAMO-DMP, NhAMO-ATU, active NmAMO, inactivated NmAMO · Nitrosomonas halophila; Nitrosopumilus maritimus · n = 15,310, 10,073, 16,914 and 15,382 micrographs · EMD-66948, EMD-66954, EMD-66926, EMD-66857; PDB 9XK5, 9XKB, 9XJ2, 9XGS
  • Surface seawater microcosms from Shenzhen Bay site SZB1 amended to 1 μM or 10 μM NH4+ for three weeks, with amoA qPCR · natural AOA and β-AOB community · n = three biological replicates per treatment
  • Representative AOA and AOB genomes for concatenated marker-gene phylogenies (122 archaeal, 120 bacterial markers) and amo gene synteny · ammonia-oxidizing archaea and bacteria · n = 10 AOA and 6 AOB taxa
  • Previously determined bacterial AMO structures used as a model-building template (NhAMO, PDB 9LEG, the authors' recent structure) or for comparison (NeAMO, PDB 9CL6) · Nitrosomonas halophila; Nitrosomonas europaea · PDB 9LEG; PDB 9CL6
Methods & tools
cryoSPARC 4.3.2, AlphaFold3, Coot, Phenix, Amber 22, Gaussian 16, CP2K 2024.1, ChemShell, GROMACS 2024.1, DIA-NN 2.2.0, MS-DIAL, GTDB-Tk / IQ-TREE
Reagents & environment
cryoSPARC 4.3.2; Amber 22 with AmberTools23 (ff14SB, Lipid21, GAFF, MCPB.py); Gaussian 16; CP2K 2024.1; GROMACS 2024.1; DIA-NN 2.2.0; Waters2mzML 1.2.0; VMD 1.9.3a; Origin 7.0; GraphPad Prism 10.0
Experimental conditions
Computation at the SUSTech Center for Computational Science and Engineering; hardware and run times not reported (simulation lengths: 200 ns MD, 50 ps QM/MM-MD, 800 RAMD trajectories).
Reproducibility gaps
No analysis code released (a custom Python script was used for lipidomics features). Maps and models are deposited; other data are said to be in the article and supplementary files, with no repository stated for raw proteomics or lipidomics. Availability of strains and plasmids is not stated.
Limitations (6)
  • Structures of AMOs from soil-associated archaeal and bacterial lineages are still needed to capture the enzyme's full environmental diversity. · stated by the authors
  • The proposed ranking of catalytic capacity (expanded cupredoxin surface plus dicopper center highest) is a conceptual framework, because copper occupancy may vary with species, redox state, substrate supply, metal homeostasis and membrane environment. · stated by the authors
  • Roles of the GDGT tetraether lipids and the lipid-like density near the hydrophobic channel are inferential; reconstitution in defined lipids or in vivo lipid perturbation was not done. · stated by the authors
  • How ammonium enrichment couples to NH3 delivery is unresolved. More catalytic intermediates, copper-occupancy states and inhibitor-bound archaeal structures are needed to complete the catalytic and inhibitory cycle. · stated by the authors
  • Copper stoichiometry is described inconsistently: about 1.1 Cu per protomer in the active-site section but two per protomer in the inactivation section, where the counts are cited as support for the copper-relocation model. · noted in this summary
  • The 34.9 vs 22.7 kcal/mol exit barriers used to argue substrate retention are, per the Methods and the Extended Data Fig. 13 legend, umbrella-sampling profiles for the inhibitor DMP leaving the active site, not for ammonia or hydroxylamine. · noted in this summary

Read this if you study nitrification, copper monooxygenases or why nitrification inhibitors act differently on archaea and bacteria, and want native-membrane archaeal AMO structures and inhibitor-bound bacterial AMO models.

Citations
1

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