Kang Li-Juan, Xu Hai, Zou Wei, Zhu Guang-Wei, Zhu Meng-Yuan, Ji Peng-Fei, Chen Jie
State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Huan Jing Ke Xue. 2020 Sep 8;41(9):4053-4061. doi: 10.13227/j.hjkx.202002006.
The decomposition of submerged macrophytes is generally associated with dramatic changes in the water environment, such as the large release of nutrients (e.g., nitrogen and phosphorus) and organic carbon to the surrounding waters, which may result in significant changes in phytoplankton community structure. In this study, physicochemical variables, and phytoplankton samples were collected in 14 shallow lakes in the middle and lower Jianghuai Plain in spring (growing period of ) and summer (decomposition phase of ) of 2018. The effects of the decline of on water quality and phytoplankton community structure were quantified. The results showed that water transparency increased significantly in spring because the growth of inhibits sediment resuspension and macrophytes can transport the nutrients from the water column to the sediment. The values of dissolved oxygen and pH also increased significantly due the photosynthesis by macrophytes. In contrast, the decomposition of during summer months caused a significant increase in water turbidity and organic matter. There were considerable differences in phytoplankton biomass and cyanobacterial biomass in the sites with or without , and the corresponding ratios of cyanobacterial biomass to the total algal biomass were 18.96% and 34.05%, respectively. Higher values of cyanobacterial biomass were observed with the decomposition of than its counterpart in summer because ① the decomposition of macrophytes provided sufficient organic matter and nutrient (nitrogen and phosphorus) resources for cyanobacterial growth; ② decline in summer significantly increased water turbidity, which makes cyanobacteria occupy a better ecological niche and more efficiently utilize nitrogen and phosphorus.
沉水植物的分解通常与水环境的剧烈变化相关,例如大量营养物质(如氮和磷)以及有机碳释放到周围水体中,这可能导致浮游植物群落结构发生显著变化。在本研究中,于2018年春季(的生长阶段)和夏季(的分解阶段)在江淮平原中下游的14个浅水湖泊中采集了理化变量和浮游植物样本。量化了的减少对水质和浮游植物群落结构的影响。结果表明,春季水体透明度显著增加,因为的生长抑制了沉积物再悬浮,并且沉水植物能够将水柱中的营养物质输送到沉积物中。由于沉水植物的光合作用,溶解氧和pH值也显著增加。相反,夏季月份的分解导致水体浊度和有机物显著增加。在有或没有的位点,浮游植物生物量和蓝藻生物量存在相当大的差异,相应的蓝藻生物量与总藻类生物量的比例分别为18.96%和34.05%。与夏季相比,随着的分解观察到更高的蓝藻生物量值,原因如下:①沉水植物的分解为蓝藻生长提供了充足的有机物和营养(氮和磷)资源;②夏季的减少显著增加了水体浊度,这使得蓝藻占据了更好的生态位并更有效地利用氮和磷。 (注:原文中部分表述不太完整准确,翻译时尽量按照原文呈现。)