Stimulation of N 2 O emission via bacterial denitrification driven by acidification in estuarine sediments

• Published in: Global Change Biology
• Main Authors: Su, Xiaoxuan, Wen, Teng, Wang, Yingmu, Xu, Junshi, Cui, Li, Zhang, Jinbo, Xue, Ximei, Ding, Kai, Tang, Yijia, Zhu, Yong‐guan
• Other Authors: National Natural Science Foundation of China, China Postdoctoral Science Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Ocean acidification
• Online Access: http://dx.doi.org/10.1111/gcb.15863; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.15863; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.15863

Abstract Ocean acidification in nitrogen‐enriched estuaries has raised global concerns. For decades, biotic and abiotic denitrification in estuarine sediments has been regarded as the major ways to remove reactive nitrogen, but they occur at the expense of releasing greenhouse gas nitrous oxide (N 2 O). However, how these pathways respond to acidification remains poorly understood. Here we performed a N 2 O isotopocules analysis coupled with respiration inhibition and molecular approaches to investigate the impacts of acidification on bacterial, fungal, and chemo‐denitrification, as well as N 2 O emission, in estuarine sediments through a series of anoxic incubations. Results showed that acidification stimulated N 2 O release from sediments, which was mainly mediated by the activity of bacterial denitrifiers, whereas in neutral environments, N 2 O production was dominated by fungi. We also found that the contribution of chemo‐denitrification to N 2 O production cannot be ignored, but was not significantly affected by acidification. The mechanistic investigation further demonstrated that acidification changed the keystone taxa of sedimentary denitrifiers from N 2 O‐reducing to N 2 O‐producing ones and reduced microbial electron‐transfer efficiency during denitrification. These findings provide novel insights into how acidification stimulates N 2 O emission and modulates its pathways in estuarine sediments, and how it may contribute to the acceleration of global climate change in the Anthropocene.