Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China.
Sci Total Environ. 2019 Dec 1;694:133702. doi: 10.1016/j.scitotenv.2019.133702. Epub 2019 Jul 31.
Coastal wetlands accumulate enormous quantities of nitrogen due to their position at the interface between land and sea and high trapping capacity. Fortunately, they have high nitrogen (N) purifying (removal) capacity, which means that they likely play an important role in mitigating against coastal eutrophication. However studies that empirically measure the degree to which wetlands purify nitrogen and their removal pathways (e.g. denitrification, anammox, plant uptake, microbial immobilization, etc.) are rare. In this study, the N purification potential (denitrification and anammox) and enzyme activities related to denitrification in different subtropical wetlands types were conducted in nitrogen-enriched wetlands of Daya Bay, Southern China. We found the average N purification rate was 11.4 μmol N·kg·h, with denitrification accounting for 84.2%-100% of the total N production in the wetlands of Daya Bay. The N purification potential in the wet season, subtidal areas and mangrove forests were generally observed to be higher than that in the dry season, high and low tidal areas, barren and estuary habitats, respectively. Correspondingly, these differences were mainly driven by the temperature, Eh and NH-N, respectively. Additionally, the nitrate reductase (Nar) and nitrite reductase (Nir) activities tended to be similar among different seasons and tidal areas, however, Nir activity in mangrove forest was 1.5-fold and 2-fold of the estuarine and barren areas, respectively. Meanwhile, Nir showed a positive correlation with denitrification rate. These results indicate that NO-N reduction, the key control mechanism for N purification, should be the rate-limiting step of the denitrification process in Daya Bay wetlands. Notably, mangroves could improve N removal rates by 48.0% compared to other wetlands. Therefore, protecting and restoring mangrove ecosystems could be an effective way to reduce the risk of coastal eutrophication.
由于位于陆海交界处和具有较高的截留能力,滨海湿地积累了大量的氮。幸运的是,它们具有很高的氮(N)净化(去除)能力,这意味着它们可能在减轻沿海富营养化方面发挥着重要作用。然而,实证测量湿地净化氮的程度及其去除途径(例如反硝化、厌氧氨氧化、植物吸收、微生物固定化等)的研究很少。在这项研究中,对中国南部大亚湾富营养化湿地的不同亚热带湿地类型的氮净化潜力(反硝化和厌氧氨氧化)和与反硝化相关的酶活性进行了研究。我们发现,氮净化率平均为 11.4μmol N·kg·h,反硝化作用占大亚湾湿地总氮产生量的 84.2%-100%。湿地在湿季、潮下带和红树林中的氮净化潜力通常高于干季、高潮带和低潮带、贫瘠和河口生境。相应地,这些差异主要由温度、Eh 和 NH-N 分别驱动。此外,硝酸盐还原酶(Nar)和亚硝酸盐还原酶(Nir)活性在不同季节和潮区之间趋于相似,但红树林中的 Nir 活性分别是河口和贫瘠地区的 1.5 倍和 2 倍。同时,Nir 与反硝化速率呈正相关。这些结果表明,NO-N 还原,即氮净化的关键控制机制,应该是大亚湾湿地反硝化过程的限速步骤。值得注意的是,与其他湿地相比,红树林可以将氮去除率提高 48.0%。因此,保护和恢复红树林生态系统可能是减少沿海富营养化风险的有效途径。