1. Unprecedented N 2 O production by nitrate-ammonifying Geobacteraceae with distinctive N 2 O isotopocule signatures.
- Author
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Xu Z, Hattori S, Masuda Y, Toyoda S, Koba K, Yu P, Yoshida N, Du Z-J, and Senoo K
- Subjects
- Soil Microbiology, Ammonium Compounds metabolism, Nitrate Reductase metabolism, Nitrate Reductase genetics, Oxidation-Reduction, Bacterial Proteins metabolism, Bacterial Proteins genetics, Nitrates metabolism, Nitrous Oxide metabolism
- Abstract
Dissimilatory nitrate reduction to ammonium (DNRA), driven by nitrate-ammonifying bacteria, is an increasingly appreciated nitrogen-cycling pathway in terrestrial ecosystems. This process reportedly generates nitrous oxide (N
2 O), a strong greenhouse gas with ozone-depleting effects. However, it remains poorly understood how N2 O is produced by environmental nitrate-ammonifiers and how to identify DNRA-derived N2 O. In this study, we characterize two novel enzymatic pathways responsible for N2 O production in Geobacteraceae strains, which are predominant nitrate-ammonifying bacteria in paddy soils. The first pathway involves a membrane-bound nitrate reductase (Nar) and a hybrid cluster protein complex (Hcp-Hcr) that catalyzes the conversion of NO2 - to NO and subsequently to N2 O. The second pathway is observed in Nar-deficient bacteria, where the nitrite reductase (NrfA) generates NO, which is then reduced to N2 O by Hcp-Hcr. These enzyme combinations are prevalent across the domain Bacteria. Moreover, we observe distinctive isotopocule signatures of DNRA-derived N2 O from other established N2 O production pathways, especially through the highest15 N-site preference (SP) values (43.0‰-49.9‰) reported so far, indicating a robust means for N2 O source partitioning. Our findings demonstrate two novel N2 O production pathways in DNRA that can be isotopically distinguished from other pathways.IMPORTANCEStimulation of DNRA is a promising strategy to improve fertilizer efficiency and reduce N2 O emission in agriculture soils. This process converts water-leachable NO3 - and NO2 - into soil-adsorbable NH4 + , thereby alleviating nitrogen loss and N2 O emission resulting from denitrification. However, several studies have noted that DNRA can also be a source of N2 O, contributing to global warming. This contribution is often masked by other N2 O generation processes, leading to a limited understanding of DNRA as an N2 O source. Our study reveals two widespread yet overlooked N2 O production pathways in Geobacteraceae , the predominant DNRA bacteria in paddy soils, along with their distinctive isotopocule signatures. These findings offer novel insights into the role of the DNRA bacteria in N2 O production and underscore the significance of N2 O isotopocule signatures in microbial N2 O source tracking., Competing Interests: The authors declare no conflict of interest.- Published
- 2024
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