4.7 Article

Dissimilatory nitrate reduction and functional genes in two subtropical rivers, China

Journal

ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
Volume 28, Issue 48, Pages 68155-68173

Publisher

SPRINGER HEIDELBERG
DOI: 10.1007/s11356-021-15197-3

Keywords

River; Sediment; Denitrification; Anammox; DNRA; Functional gene

Funding

  1. National Natural Science Foundation of China [32030069, 31720103905]

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The study investigated dissimilatory nitrate reduction rates in sediments of two subtropical rivers in China, revealing varying contributions of denitrification, anammox, and DNRA in different seasons and under different levels of human disturbance. The rates were correlated with environmental factors, highlighting the importance of understanding these processes for sustaining the ecohealth of river ecosystems.
Dissimilatory nitrate reduction processes, including denitrification, anaerobic ammonium oxidation (anammox), and dissimilatory nitrate reduction to ammonium (DNRA), are important pathways of nitrate transformation in the aquatic environments. In this study, we investigated potential rates of denitrification, anammox, and DNRA in the sediments of two subtropical rivers, Jinshui River and Qi River, with different intensities of human activities in their respective catchment, China. Our objectives were to assess the seasonality of dissimilatory nitrate reduction rates, quantify their respective contributions to nitrate reduction, and reveal the relationship between dissimilatory nitrate reduction rates, functional gene abundances, and physicochemicals in the river ecosystems. Our results showed higher rates of denitrification and anammox in the intensively disturbed areas in autumn and spring, and higher potential DNRA in the slightly disturbed areas in summer. Generally, denitrification, anammox, and DNRA were higher in summer, autumn, and spring, respectively. Relative contributions of nitrate reduction from denitrification, anammox, and DNRA were quite different in different seasons. Dissimilatory nitrate reduction rates and gene abundances correlated significantly with water temperature, dissolved organic carbon (DOC), sediment total organic carbon (SOC), NO3-, NH4+, DOC/NO3-, iron ions, and sulfide. Understanding dissimilatory nitrate reduction is essential for restoring nitrate reduction capacity and improving and sustaining ecohealth of the river ecosystems.

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