Yang Ping, Tang Kam W, Tong Chuan, Lai Derrick Y F, Zhang Linhai, Lin Xiao, Yang Hong, Tan Lishan, Zhang Yifei, Hong Yan, Tang Chen, Lin Yongxin
School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; Key Laboratory of Humid Subtropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007, China.
Department of Biosciences, Swansea University, Swansea SA2 8PP, United Kingdom.
Water Res. 2022 Dec 1;227:119326. doi: 10.1016/j.watres.2022.119326. Epub 2022 Nov 6.
Land reclamation is a major threat to the world's coastal wetlands, and it may influence the biogeochemical cycling of nitrogen in coastal regions. Conversion of coastal marshes into aquaculture ponds is common in the Asian Pacific region, but its impacts on the production and emission of nitrogen greenhouse gases remain poorly understood. In this study, we compared NO emission from a brackish marsh and converted shrimp aquaculture ponds in the Shanyutan wetland, the Min River Estuary in Southeast China over a three-year period. We also measured sediment and porewater properties, relevant functional gene abundance, sediment NO production potential and denitrification potential in the two habitats. Results indicated that the pond sediment had lower N-substrate availability, lower ammonia oxidation (AOA and comammox Nitrospira amoA), nitrite reduction (nirK and nirS) and nitrous oxide reduction (nosZ Ⅰ and nosZ Ⅱ) gene abundance and lower NO production and denitrification potentials than in marsh sediments. Consequently, NO emission fluxes from the aquaculture ponds (range 5.4-251.8 μg m h) were significantly lower than those from the marsh (12.6-570.7 μg m h). Overall, our results show that conversion from marsh to shrimp aquaculture ponds in the Shanyutan wetland may have diminished nutrient input from the catchment, impacted the N-cycling microbial community and lowered NO production capacity of the sediment, leading to lower NO emissions. Better post-harvesting management of pond water and sediment may further mitigate NO emissions caused by the aquaculture operation.
填海造地是对世界沿海湿地的一大威胁,可能会影响沿海地区氮的生物地球化学循环。在亚太地区,将沿海沼泽地转变为水产养殖池塘的情况很常见,但其对氮温室气体产生和排放的影响仍知之甚少。在本研究中,我们比较了中国东南部闽江口鳝鱼滩湿地一片咸淡水沼泽地和改造后的对虾养殖池塘在三年期间的一氧化氮排放情况。我们还测量了这两种生境中的沉积物和孔隙水特性、相关功能基因丰度、沉积物一氧化氮产生潜力和反硝化潜力。结果表明,与沼泽沉积物相比,池塘沉积物的氮底物可用性较低,氨氧化(氨氧化古菌和完全氨氧化硝化螺菌amoA基因)、亚硝酸盐还原(nirK和nirS基因)和一氧化二氮还原(nosZⅠ和nosZⅡ基因)基因丰度较低,一氧化氮产生和反硝化潜力也较低。因此,水产养殖池塘的一氧化氮排放通量(范围为5.4 - 251.8微克·米⁻²·小时⁻¹)显著低于沼泽地(12.6 - 570.7微克·米⁻²·小时⁻¹)。总体而言,我们的结果表明,鳝鱼滩湿地从沼泽地转变为对虾养殖池塘可能减少了流域的养分输入,影响了氮循环微生物群落,降低了沉积物的一氧化氮产生能力,导致一氧化氮排放量降低。对池塘水和沉积物进行更好的收获后管理可能会进一步减少水产养殖作业造成的一氧化氮排放。