Articles | Volume 23, issue 18
https://doi.org/10.5194/bg-23-6705-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-23-6705-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High nitrous oxide isotopic variability during denitrification by Pseudomonas species bearing NirK and NirS
Laboratory for Air Pollution/Environmental Technology, Empa, Überlandstrasse 129, Dübendorf, Switzerland
Aquatic and Isotope Biogeochemistry, University of Basel, Bernoullistrasse 30, Basel, Switzerland
Paul M. Magyar
Laboratory for Air Pollution/Environmental Technology, Empa, Überlandstrasse 129, Dübendorf, Switzerland
Jakob Zopfi
Aquatic and Isotope Biogeochemistry, University of Basel, Bernoullistrasse 30, Basel, Switzerland
Claudia Frey
Aquatic and Isotope Biogeochemistry, University of Basel, Bernoullistrasse 30, Basel, Switzerland
Thomas Kuhn
Aquatic and Isotope Biogeochemistry, University of Basel, Bernoullistrasse 30, Basel, Switzerland
Moritz F. Lehmann
Aquatic and Isotope Biogeochemistry, University of Basel, Bernoullistrasse 30, Basel, Switzerland
Laboratory for Air Pollution/Environmental Technology, Empa, Überlandstrasse 129, Dübendorf, Switzerland
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Cited articles
Braman, R. S. and Hendrix, S. A.: Nanogram nitrite and nitrate determination in environmental and biological materials by vanadium(III) reduction with chemiluminescence detection, Anal. Chem., 61, 2715–2718, https://doi.org/10.1021/ac00199a007, 1989.
Buchwald, C. and Casciotti, K. L.: Isotopic ratios of nitrite as tracers of the sources and age of oceanic nitrite, Nat. Geosci., 6, 308–313, https://doi.org/10.1038/ngeo1745, 2013.
Caranto, J. D., Weitz, A., Giri, N., Hendrich, M. P., and Kurtz Jr., D. M.: A Diferrous-Dinitrosyl Intermediate in the N2O-Generating Pathway of a Deflavinated Flavo-Diiron Protein, ACS Biochem., 53, 5631–5637, https://doi.org/10.1021/bi500836z, 2014a.
Caranto, J. D., Weitz, A., Hendrich, M. P., and Kurtz Jr., D. M: The Nitric Oxide Reductase Mechanism of a Flavo-Diiron Protein: Identification of Active-Site Intermediates and Products, J. Am. Chem. Soc., 136, 7981–7992, https://doi.org/10.1021/ja5022443, 2014b.
Casciotti, K. L., Sigman, D. M., Hastings, M. G., Böhlke, J. K., and Hilkert, A.: Measurement of the oxygen isotopic composition of nitrate in seawater and freshwater using the denitrifier method, Anal. Chem., 74, 4905–4912, https://doi.org/10.1021/ac020113w, 2002.
Casciotti, K. L., Böhlke, J. K., McIlvin, M., Mroczkowski, S., and Hannon, J.: Oxygen Isotopes in Nitrite: Analysis, Calibration, and Equilibration, Anal. Chem., 79, 2427–2436, https://doi.org/10.1021/ac061598h, 2007.
Chénier, N., Magyar, P. M., Zopfi, J., Frey, C., Lehmann, M. F., and Mohn, J.: High nitrous oxide isotopic variability during denitrification by Pseudomonas species bearing NirK and NirS, Zenodo [data set], https://doi.org/10.5281/zenodo.21534019, 2026.
Denk, T. R. A., Mohn, J., Decock, C., Lewicka-Szczebak, D., Harris, E., Butterbach-Bahl, K., Kiese, R., and Well, R.: The nitrogen cycle: A review of isotope effects and isotope modeling approaches, Soil Biol. Biochem., 105 121e137, https://doi.org/10.1016/j.soilbio.2016.11.015, 2016.
Denman, K. L., Brasseur, G., Chidthaisong, A., Ciais, P., Cox, P. M., Dickinson, R. E., Hauglustaine, D., Heinze, C., Holland, E., Jacob, D., Lohmann, U., Ramachandran, S., da Silva Dias, P. L., Wofsy, S. C., and Zhang, X.: Couplings Between Changes in the Climate System and Biogeochemistry, Climate Change: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, https://www.ipcc.ch/site/assets/uploads/2018/02/ar4-wg1-chapter7-1.pdf (last access: 22 September 2026), 2007.
Frame, C. H. and Casciotti, K. L.: Biogeochemical controls and isotopic signatures of nitrous oxide production by a marine ammonia-oxidizing bacterium, Biogeosciences, 7, 2695–2709, https://doi.org/10.5194/bg-7-2695-2010, 2010.
Gruber, W., Magyar, P.M., Mitrovic, I., Zeyer, K., Vogel, M., von Känel, L., Biolley, L., Werner, R. A., Morgenroth, E., Lehmann, M. F., and Braun, D.: Tracing N2O formation in full-scale wastewater treatment with natural abundance isotopes indicates control by organic substrate and process settings, Water Research X, 15, 100130, https://doi.org/10.1016/j.wroa.2022.100130, 2022.
Hansen, H. P. and Koroleff, F.: Determination of nutrients, Methods of Seawater Analysis, 159–228, https://doi.org/10.1002/9783527613984, 1999.
Haslun, J. A., Ostrom, N. E., Hegg, E. L., and Ostrom, P. H.: Estimation of isotope variation of N2O during denitrification by Pseudomonas aureofaciens and Pseudomonas chlororaphis: implications for N2O source apportionment, Biogeosciences, 15, 3873–3882, https://doi.org/10.5194/bg-15-3873-2018, 2018.
Ibraim, E., Harris, E., Eyer, S., Tuzson, B., Emmenegger, L., Six, J., and Mohn, J.: Development of a field-deployable method for simultaneous, real-time measurements of the four most abundant N2O isotopocules, Isot. Environ. Healt. S., 54, https://doi.org/10.1080/10256016.2017.1345902, 2018.
IPCC: Climate Change 2023: Synthesis Report. Contribution of Working Groups I, II and III to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change, IPCC, Geneva, Switzerland, https://doi.org/10.59327/IPCC/AR6-9789291691647, 2023.
Jones, L. C., Peters, B., Lezama Pacheco, J. S., Casciotti, K. L., and Fendorf, S.: Stable isotopes and iron oxide mineral products as markers of chemodenitrification, Environ. Sci. Technol., 49, 3444–3452, https://doi.org/10.1021/es504862x, 2015.
Kelly, C. L., Manning, C., Frey, C., Kaiser, J., Gluschankoff, N., and Casciotti, L. L.: Pyisotopomer: A Python package for obtaining intramolecular isotope ratio differences from mass spectrometric analysis of nitrous oxide isotopocules, Rapid Commun. Mass Spectrom., 1097–0231, https://doi.org/10.1002/rcm.9513, 2023.
Kool, D. M., Wrage, N., Oenema, O., Dolfing, J., and Van Groenigen, J. W.: Oxygen exchange between (de) nitrification intermediates and H2O and its implications for source determination of NO and N2O: a review, Rapid Commun. Mass Sp., 21, 3569–3578, https://doi.org/10.1002/rcm.3249, 2007.
Lewicka-Szczebak, D., Dyckmans, J., Kaiser, J., Marca, A., Augustin, J., and Well, R.: Oxygen isotope fractionation during N2O production by soil denitrification, Biogeosciences, 13, 1129–1144, https://doi.org/10.5194/bg-13-1129-2016, 2016.
Mariotti, A., Leclerc, A., and Germon, J. C.: Nitrogen isotope fractionation associated with the NO → N2O step of denitrification in soils, Can. J. Soil Sci., 62, 227–241, https://doi.org/10.1007/BF02374138, 1981.
Mohn, J., Biasi, C., Bodé, S., Boeckx, P., Brewer, P. J., Eggleston, S., Geilmann, H., Guillevic, M., Kaiser, J., Kantnerová, K., and Moossen, H.: Isotopically characterised N2O reference materials for use as community standards, Rapid Commun. Mass Specrom., 36, 13, e9296, https://doi.org/10.1002/rcm.9296, 2022.
Opdyke, M. R., Ostrom, N. E., and Ostrom, P. H.: Evidence for the predominance of denitrification as a source of N2O in temperate agricultural soils based on isotopologue measurements, Global Biogeochem. Cy., 23, 4, https://doi.org/10.1029/2009GB003523, 2008.
Ostrom, N. E. and Ostrom, P. H.: The isotopomers of nitrous oxide: analytical considerations and application to resolution of microbial production pathways, Handbook of Environmental Isotope Geochemistry, Vol. I, Berlin, Heidelberg: Springer Berlin Heidelberg, 453–476, https://doi.org/10.1007/978-3-642-10637-8_23, 2011.
R Core Team: R: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria, https://www.R-project.org/ (last access: 21 September 2026), 2020.
Reay, D. S., Davidson, E. A., Smith, K. A., Smith, P., Melillo, J. M., Dentener, F., and Crutzen, P. J.: Global agriculture and nitrous oxide emissions, Nat. Clim. Change, 2, 410–416, https://doi.org/10.1038/nclimate1458, 2012.
Rivett, E. D., Finders, C. M., Haslun, J. A., Gandhi, H., Kahle, M., Ädelroth, P., Ostrom, P. H., Ostrom, N. E., and Hegg E. L.: Isotopic Fractionation and Kinetic Isotope Effects of a Purified Bacterial Nitric Oxide Reductase (NOR), Biochemistry, 64, 4327–4340, https://doi.org/10.1021/acs.biochem.5c00417, 2025.
Rohe, L., Well, R., and Lewicka‐Szczebak, D.: Use of oxygen isotopes to differentiate between nitrous oxide produced by fungi or bacteria during denitrification, Rapid Commun. Mass Spectrom., 31, 1297–1312, https://doi.org/10.1002/rcm.7909, 2017.
Sigman, D. M., Casciotti, K. L., Andreani, M., Barford, C., Galanter, M., and Böhlke, J. K.: A bacterial method for the nitrogen isotopic analysis of nitrate in seawater and freshwater, Anal. Chem., 73, 4145–4153, https://doi.org/10.1021/ac010088e, 2001.
Snider, D. M., Schiff, S. L., and Spoelstra, J.: and stable isotope ratios of nitrous oxide produced during denitrification in temperate forest soils, Geochim. Cosmochim. Ac., 73, 877–888, 2009.
Strubbe, L., Keck, H., Magyar, P. M., Mohn, J., Joss, A., and Froemelt, A.: Activating specific N2O production pathways to understand emission dynamics in wastewater treatment, Water Res., 296, 125580, https://doi.org/10.1016/j.watres.2026.125580, 2026.
Sutka, R. L., Ostrom, N. E., Ostrom, P. H., Breznak, J. A., Gandhi, H., Pitt, A. J., and Li, F.: Distinguishing nitrous oxide production from nitrification and denitrification using N2O isotopomers, Appl. Environ. Microbiol., 72, 638–644, https://doi.org/10.1128/AEM.72.1.638-644.2006, 2006.
Toyoda, S., Mutobe, H., Yamagishi, H., Yoshida, N., and Tanji, Y.: Fractionation of N2O isotopomers during production by denitrifier bacteria, Soil Biol. Biochem., 37, 1535–1545, https://doi.org/10.1016/j.soilbio.2005.01.009, 2005.
Visser, A.-N., Wankel, S. D., Niklaus, P. A., Byrne, J. M., Kappler, A. A., and Lehmann, M. F.: Impact of reactive surfaces on the abiotic reaction between nitrite and ferrous iron and associated nitrogen and oxygen isotope dynamics, Biogeosciences, 17, 4355–4374, https://doi.org/10.5194/bg-17-4355-2020, 2020.
Wang, R. Z., Lonergan, Z. R., Wilbert, S. A., Eiler, J. M., and Newman, D. K.: Widespread detoxifying NO reductases impart a distinct isotopic fingerprint on N2O under anoxia, P. Natl. Acad. Sci. USA, 121, 25 e2319960121, https://doi.org/10.1073/pnas.2319960121, 2024.
Wei, J., Ibraim, E., Brüggemann, N., Vereecken, H., and Mohn, J.: First real-time isotopic characterisation of N2O from chemodenitrification, Geochim. Cosmochim. Ac., 267, https://doi.org/10.1016/j.gca.2019.09.018, 2019.
Weigand, M. A., Foriel, J., Barnett, B., Oleynik, S., and Sigman, D. M.: Updates to instrumentation and protocols for isotopic analysis of nitrate by the denitrifier method, Rapid Commun. Mass Sp., 30, 1365–1383, https://doi.org/10.1002/rcm.7570, 2016.
WMO: Greenhouse Gas Bulletin, World Meteorological Organization, https://library.wmo.int/idurl/4/69057 (last access: 7 September 2026), 2024.
Wunderlin, P., Mohn, J., Joss, A., Emmenegger, L., and Siegrist, H.: Mechanisms of N2O production in biological wastewater treatment under nitrifying and denitrifying conditions, Water Res., 46, 1027–1037, https://doi.org/10.1016/j.watres.2011.11.080, 2012.
Wunderlin, P., Lehmann, M. F., Siegrist, H., Tuzson, B., Joss, A., Emmenegger, L., and Mohn, J.: Isotope signatures of N2O in a mixed microbial population system: constraints on N2O producing pathways in wastewater treatment, Environ. Sci Technol., 47, 1339–1348, https://doi.org/10.1021/es303174x, 2013.
Xu, Z., Hattori, S., Masuda, Y., Toyoda, S., Koba, K., Yu, P., and Senoo, K.: Unprecedented N2O production by nitrate-ammonifying Geobacteraceae with distinctive N2O isotopocule signatures, mBio, 15, e02540-24, https://doi.org/10.1128/mbio.02540-24, 2024.
Yamazaki, T., Hozuki, T., Arai, K., Toyoda, S., Koba, K., Fujiwara, T., and Yoshida, N.: Isotopomeric characterization of nitrous oxide produced by reaction of enzymes extracted from nitrifying and denitrifying bacteria, Biogeosciences, 11, 2679–2689, https://doi.org/10.5194/bg-11-2679-2014, 2014.
Ye, R. W., Averill, B. A., and Tiedje, J. M.: Denitrification: production and consumption of nitric oxide, Appl. Environ. Microb., 60, 1053–1058, https://doi.org/10.1128/aem.60.4.1053-1058.1994, 1991.
Yoshida, N. and Toyoda, S.: Constraining the atmospheric N2O budget from intramolecular site preference, Nature, 405, 330–334, https://doi.org/10.1038/35012558, 2000.
Yu, L., Harris, E., Lewicka-Szczebak, D., Barthel, M., Blomberg, M. R. A., Harris, S. J., Johnson, M. S., Lehmann, M. F., Liisberg, J., Müller, C., Ostrom, N. E., Six, J., Toyoda, S., Yoshida, N., and Mohn, J.: What can we learn from N2O isotope data? – Analytics, processes and modelling, Rapid Commun. Mass Sp., 34, e8858, https://doi.org/10.1002/rcm.8858, 2020.
Zumft, W. G.: Cell biology and molecular basis of denitrification, Microbiol. Mol. Biol. Rev., 61, 533–616, 1997.
Short summary
N₂O is a greenhouse gas produced by microbes during nitrogen cycling. We studied two bacterial species and found that the isotope signatures of the N₂O they produced changed strongly depending on growth conditions and cell activity. Early during growth, the distribution of N isotopes within the N₂O molecule also changed unexpectedly. These results show that N₂O isotope signatures are more variable than previously assumed and depend strongly on physiology.
N₂O is a greenhouse gas produced by microbes during nitrogen cycling. We studied two bacterial...
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