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Dissimilatory nitrate reduction to ammonium increased with rising temperature

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Abstract

Although recent studies have explored dissimilatory nitrate reduction to ammonium (DNRA), little is known about the dependence of this process on temperature. A laboratory experiment was conducted to investigate if temperature regulates nitrate (NO3ˉ) reduction by DNRA and denitrification. Soil samples were incubated at 10 to 40 °C for 28 days, and 15N tracer methods were applied to estimate the reduction of 15NO3ˉ to 15NH4+ by DNRA organisms and to 15N2O or 15N2 by denitrifiers. Raising the temperature from 10 to 40 °C increased DNRA, which contributed to enrichment of the NH4+ pool, particularly at 40 °C. The percentage of 15NO3ˉ reduced by DNRA was from 4 to 30% of that reduced by denitrification, and decreased with increasing temperature. DNRA and denitrification were positively correlated with the abundance of nrfA and nosZ genes, respectively. The accumulation of 15NH4+ slowed in the final 12 h of sampling times, which may be due to a re-conversion of 15NH4+ to 15NO3ˉ by nitrification. High temperatures (30 to 40 °C) enhanced 15N2 production, which suggests that temperature plays an important role in regulating complete denitrification from NO3ˉ to N2.

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Acknowledgments

We acknowledge the assistance of Yi Zhou (University of Adelaide) for soil collection and the Australian Centre for Plant Functional Genomics for the analysis of qPCR data.

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This study was funded by the Yitpi Foundation (UA0006005964).

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Correspondence to Matthew D. Denton.

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Lai, T.V., Ryder, M.H., Rathjen, J.R. et al. Dissimilatory nitrate reduction to ammonium increased with rising temperature. Biol Fertil Soils 57, 363–372 (2021). https://doi.org/10.1007/s00374-020-01529-x

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