Jia Dai, Qi Fei, Xu Xia, Feng Jianxiang, Wu Hao, Guo Jiemin, Lu Weizhi, Peng Ronghao, Zhu Xiaoshan, Luo Yiqi, Lin Guanghui
Ministry of Education Key Laboratory for Earth System Modeling, Center for Earth System Science, Tsinghua University, Beijing, China.
Shenzhen Key Laboratory for Coastal Ocean Dynamic and Environment, Division of Ocean Sciences and Technology, Graduate School at Shenzhen, Tsinghua University, Shenzhen, China.
PLoS One. 2016 Jan 4;11(1):e0146199. doi: 10.1371/journal.pone.0146199. eCollection 2016.
Both plant invasion and nitrogen (N) enrichment should have significant impact on mangrove ecosystems in coastal regions around the world. However, how N2O efflux in mangrove wetlands responds to these environmental changes has not been well studied. Here, we conducted a mesocosm experiment with native mangrove species Kandelia obovata, invasive salt marsh species Spartina alterniflora, and their mixture in a simulated tide rotation system with or without nitrogen addition. In the treatments without N addition, the N2O effluxes were relatively low and there were no significant variations among the three vegetation types. A pulse loading of exogenous ammonium nitrogen increased N2O effluxes from soils but the stimulatory effect gradually diminished over time, suggesting that frequent measurements are necessary to accurately understand the behavior of N-induced response of N2O emissions. With the N addition, the N2O effluxes from the invasive S. alterniflora were lower than that from native K. obovata mesocosms. This result may be attributed to higher growth of S. alterniflora consuming most of the available nitrogen in soils, and thus inhibiting N2O production. We concluded that N loading significantly increased N2O effluxes, while the invasion of S. alterniflora reduced N2O effluxes response to N loading in this simulated mangrove ecosystem. Thus, both plant invasion and excessive N loading can co-regulate soil N2O emissions from mangrove wetlands, which should be considered when projecting future N2O effluxes from this type of coastal wetland.
植物入侵和氮(N)富集均应对全球沿海地区的红树林生态系统产生重大影响。然而,红树林湿地中的一氧化二氮(N₂O)排放如何响应这些环境变化尚未得到充分研究。在此,我们在一个模拟潮汐循环系统中,对本地红树林物种秋茄(Kandelia obovata)、入侵盐沼物种互花米草(Spartina alterniflora)及其混合物进行了中宇宙实验,实验设置添加或不添加氮。在不添加氮的处理中,N₂O排放相对较低,且三种植被类型之间无显著差异。外源铵态氮的脉冲式添加增加了土壤中的N₂O排放,但刺激作用随时间逐渐减弱,这表明需要频繁测量才能准确了解N诱导的N₂O排放响应行为。添加氮后,入侵的互花米草中的N₂O排放低于本地秋茄中宇宙的排放。这一结果可能归因于互花米草的较高生长消耗了土壤中大部分可利用的氮,从而抑制了N₂O的产生。我们得出结论,氮负荷显著增加了N₂O排放,而互花米草的入侵降低了该模拟红树林生态系统中N₂O排放对氮负荷的响应。因此,植物入侵和过量氮负荷均可共同调节红树林湿地土壤中的N₂O排放,在预测此类沿海湿地未来的N₂O排放时应予以考虑。