Dissimilatory nitrate reduction pathways drive high nitrous oxide emissions and nitrogen retention under the flash drought in the largest freshwater lake in China

被引:1
作者
Su, Rui [1 ,2 ]
Zhao, Dayong [1 ]
Zhang, Xiaomin [1 ,2 ]
Zhang, Hongjie [1 ]
Cheng, Junxiang [2 ,5 ]
Xu, Ligang [2 ,5 ]
Wu, Qinglong L. [2 ,3 ,4 ]
Zeng, Jin [2 ,3 ,5 ]
机构
[1] Hohai Univ, Joint Int Res Lab Global Change & Water Cycle, Natl Key Lab Water Disaster Prevent, Nanjing 210098, Peoples R China
[2] Nanjing Inst Geog & Limnol, Chinese Acad Sci, Key Lab Lake & Watershed Sci Water Secur, Nanjing 211135, Peoples R China
[3] Univ Chinese Acad Sci, Sino Danish Ctr Educ & Res, Beijing 100039, Peoples R China
[4] Ctr Evolut & Conservat Biol, Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China
[5] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Poyang Lake Wetland Res Stn, Jiujiang 332899, Peoples R China
基金
中国国家自然科学基金;
关键词
Flash drought; Nitrous oxide; Denitrification; DNRA; Metabolic mechanism; Climate feedback; ENVIRONMENTAL CONTROLS; N2O EMISSIONS; EXTREME HEAT; NITRIC-OXIDE; SOIL; DENITRIFICATION; ESTUARINE; QUANTIFICATION; COMMUNITIES; MECHANISMS;
D O I
10.1016/j.watres.2024.123075
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Flash drought (FD) events induced by climate change may disrupt the normal hydrological regimes of floodplain lakes and affect the plant-microbe mediated dissimilatory nitrate reduction (DNR), i.e., denitrification, anammox and dissimilatory nitrate reduction to ammonium (DNRA), thus having important consequences for nitrous oxide (N2O) emissions and nitrogen (N) retention. However, the responses of the DNR pathways in the floodplain lake to the record-breaking FD in 2022 in Yangtze River of China, as well as the underlying microbial mechanisms and feedbacks to climate change remain poorly understood. Here, we collected exposed sediments and Carex cinerascens-associated soils in the littoral wetlands of Poyang Lake during 2022 FD and the dry seasons prior to and after this event. The potential DNR rates and the synergistic metabolism of microbial guilds involved in DNR were investigated using 15N isotope pairing technique, high-throughput and metagenomic sequencing. We found that the in situ N2O fluxes in the littoral wetlands were highest during the flash drought, especially in the exposed sediments. The potential DNRA rates were highest under flash drought conditions, and DNRA dominated the DNR for both exposed sediments (80.4 %) and Carex cinerascens-associated soils (57.5 %). Nutrients (i.e., N and P) and DNRA bacterial communities played a key role in producing the extremely high N2O fluxes from exposed sediments, which could be explained by the synergistic metabolism of DNRA bacteria and denitrifiers through the exchange of the key intermediates in DNR. Therefore, the climate change-induced flash drought promoted greater nitrous oxide emissions and N retention in the littoral wetlands of Poyang Lake, producing a greater flux of greenhouse gas emissions and elevating the risk of lake eutrophication. Hence, flash droughts reinforce a positive feedback between climate change and nitrous oxide emission from these aquatic ecosystems.
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页数:13
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