State Key Laboratory of Estuarine and Coastal Research, Yangtze Delta Estuarine Wetland Ecosystem Observation and Research Station, Ministry of Education & Shanghai, East China Normal University, Shanghai200241, China.
Key Laboratory of Geographic Information Science of the Ministry of Education, School of Geographic Sciences, East China Normal University, Shanghai200241, China.
Environ Sci Technol. 2023 Feb 14;57(6):2660-2671. doi: 10.1021/acs.est.2c06602. Epub 2023 Feb 3.
Estuarine and coastal environments are assumed to contribute to nitrous oxide (NO) emissions under increasing nitrogen loading. However, isotopic and molecular mechanisms underlying NO production pathways under elevated nitrogen concentration remain poorly understood. Here we used microbial inhibition, isotope mass balance, and molecular approaches to investigate NO production mechanisms in estuarine and coastal sediments through a series of anoxic incubations. Site preference of the NO molecule increased due to increasing nitrate concentration, suggesting the changes in NO production pathways. Enhanced NO production under high nitrate concentration was not mediated by bacterial denitrification, but instead was mainly regulated by fungal denitrification. Elevated nitrate concentration increased the contribution of fungal denitrification to NO production by 11-25%, whereas it decreased bacterial NO production by 16-33%. Chemodenitrification was also enhanced by high nitrate concentration, contributing to 13-28% of NO production. Elevated nitrate concentration significantly mediated -type denitrifiers structure and abundance, which are the keystone taxa driving NO production. Collectively, these results suggest that increasing nitrate concentration can shift NO production pathways from bacterial to fungal and chemodenitrification, which are mainly responsible for the enhanced NO production and have widespread implications for NO projections under ongoing nitrogen pollution in estuarine and coastal ecosystems.
沿海河口环境被认为在氮负荷增加的情况下会促进氧化亚氮(NO)的排放。然而,在高浓度氮条件下,NO 产生途径的同位素和分子机制仍知之甚少。在这里,我们通过一系列缺氧培养实验,利用微生物抑制、同位素质量平衡和分子方法,研究了沿海河口沉积物中 NO 的产生机制。由于硝酸盐浓度的增加,NO 分子的位置偏好增加,这表明 NO 产生途径发生了变化。高硝酸盐浓度下的增强的 NO 产生不是由细菌反硝化作用介导的,而是主要由真菌反硝化作用调控的。高硝酸盐浓度增加了真菌反硝化作用对 NO 产生的贡献,增加了 11-25%,而降低了细菌的 NO 产生,降低了 16-33%。化学反硝化作用也因高硝酸盐浓度而增强,对 13-28%的 NO 产生做出贡献。高硝酸盐浓度显著调节了 -型反硝化细菌的结构和丰度,这些是驱动 NO 产生的关键类群。总的来说,这些结果表明,增加硝酸盐浓度可以将 NO 产生途径从细菌反硝化作用转变为真菌反硝化作用和化学反硝化作用,这主要是增强 NO 产生的原因,并对沿海河口生态系统中氮污染持续下的 NO 预测有广泛的影响。