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Effects of dam construction and increasing pollutants on the ecohydrological evolution of a shallow freshwater lake in the Yangtze floodplain

机译:大坝施工及污染物对长江洪泛区浅淡水湖泊生态学演变的影响

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摘要

Large river-floodplain systems which provide a variety of societal, economic and biological benefits are undergoing extensive and intensive human disturbance. However, floodplain lakes responses to multiple stressors are poorly understood. The Yangtze River and its floodplain which provide water and food resources for more than 300 million people are an important region in China. Hydrological regulation as well as socio-economic development have brought profound negative influence on this ecologically important area. To improve understanding of decadal-scale responses of floodplain lakes to multiple stressors, lake sediment proxies including particle size, geochemical elements, diatoms and chironomids were analysed in a lead-210 dated core from Futou Lake. The analyses show that dams constructed in 1935 and the early 1970s stabilized hydrological conditions in Futou Lake and impeded the interaction with the Yangtze River, resulting in a decrease in major elements (e.g., Mg, Al, Fe) transported into the lake and an increase of macrophyte-related chironomids (C. sylvestris-type, P. penicillatus-type and Paratanytarsus sp.). After the late 1990s, further decreases in major elements and increases in median grain size are attributed to the erosion of the Yangtze riverbed and declining supply of major elements-enriched sediments from the upper Yangtze caused by the impoundment of the Three Gorges Dam. Chironomid and diatom assemblages indicate that hydrological stabilization caused by dam constructions stimulated the growth of macrophytes, which may be important in buffering against an ecosystem state change towards a phytoplankton-dominated and turbid state with ongoing eutrophication. However, a recent increase in Zn, TP and the emergence of eutrophic diatom and chironomid species indicate initial signs of water quality deterioration which may be related to the combined effects of hydrological stabilization and aquaculture. Over all, the sediment record from Futou Lake emphasizes the importance of interactions between hydrological change and pollutant loads in determining floodplain lake ecosystem state.
机译:提供各种社会,经济和生物效益的大型河流 - 洪泛区正在进行广泛和密集的人类障碍。然而,洪泛区湖泊对多次压力源的反应很差。长江及其洪泛区提供了3亿以上人们的水和粮食资源是中国的重要地区。水文调节以及社会经济发展对这一生态重要地区带来了深刻的负面影响。为了改善对多重压力源的洪泛区湖泊的二等程度响应的理解,在Futou湖的引线210日期核心中分析了包括粒度,地球化学元素,硅藻和依湿式体的湖泊沉积物代理。该分析表明,1935年建造的水坝和20世纪70年代初期稳定在福堡湖中的水文条件,并阻碍了与长江的互动,导致主要元素(例如,Mg,Al,Fe)减少到湖中并增加宏观物质相关的甲基化型(C.Sylvestris型,P.Penicillatus型和ParatanyTarsus SP。)。 20世纪90年代末期后,主要要素进一步减少,中位数粒度的增加归因于长江河床的侵蚀,并从三峡大坝蓄积造成的上扬子引起的主要元素富含沉积物的侵蚀。依甲酰静脉和硅藻组件表明,由坝结构引起的水文稳定刺激了宏观物质的生长,这对于缓冲生态系统状态的变化可能是朝向较富营养的浮游植物的植物主导和混浊状态的变化。然而,近期Zn,TP和富营养基硅藻和挥之不良含量的出现表明水质恶化的初始迹象,这可能与水文稳定和水产养殖的综合影响有关。过度所有的是Futou湖的沉积物记录强调了在确定洪泛区湖生态系统状态时水文变化与污染物负荷之间的相互作用的重要性。

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