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A century-scale, human-induced ecohydrological evolution of wetlands of two large river basins in Australia (Murray) and China (Yangtze)

机译:澳大利亚(墨累)和中国(长江)两个大型流域的湿地百年尺度人为生态水文演变

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Recently, the provision of food and water resources of two of the world's largest river basins, the Murray and the Yangtze, has been significantly altered through widespread landscape modification. Long-term sedimentary archives, dating back for some centuries from wetlands of these river basins, reveal that rapid, basin-wide development has reduced the resilience of biological communities, resulting in considerable decline in ecosystem services, including water quality. Large-scale human disturbance to river systems, due to river regulation during the mid-20th century, has transformed the hydrology of rivers and wetlands, causing widespread modification of aquatic biological communities. Changes to cladoceran zooplankton (water fleas) were used to assess the historical hydrology and ecology of three Murray and Yangtze river wetlands over the past century. Subfossil assemblages of cladocerans retrieved from sediment cores (94, 45, and 65?cm) of three wetlands: Kings Billabong (Murray), Zhangdu, and Liangzi lakes (Yangtze), showed strong responses to hydrological changes in the river after the mid-20th century. In particular, river regulation caused by construction of dams and weirs together with river channel modifications, has led to significant hydrological alterations. These hydrological disturbances were either (1) a prolonged inundation of wetlands or (2) reduced river flow, both of which caused variability in wetland depth. Inevitably, these phenomena have subsequently transformed the natural wetland habitats, leading to a switch in cladoceran assemblages to species preferring poor water quality, and in some cases to eutrophication. The quantitative and qualitative decline of wetland water conditions is indicative of reduced ecosystem services, and requires effective restoration measures for both river basins which have been impacted by recent socioeconomic development and climate change.
机译:最近,通过广泛的景观改造,世界上最大的两个流域墨累和扬子江的粮食和水资源供应已大大改变。这些河流流域的湿地可追溯到几个世纪以来的长期沉积档案显示,流域范围内的快速发展降低了生物群落的复原力,导致包括水质在内的生态系统服务大幅下降。由于20世纪中叶的河流管制,人类对河流系统的大规模干扰已经改变了河流和湿地的水文状况,导致了水生生物群落的广泛改变。使用锁骨浮游动物(水蚤)的变化来评估过去一个世纪的三个墨累和长江湿地的历史水文学和生态学。从三个湿地的沉积物核心(94、45和65?cm)取回的锁骨亚化石组合:国王比拉蓬(墨累),张渡和良子湖(长江)对中游后的水文变化表现出强烈的反应。 20世纪。特别是,由于修建水坝和堰坝而引起的河道整治以及河道的改造导致了重大的水文变化。这些水文干扰要么是(1)湿地的长期淹没,要么是(2)河流流量的减少,这两者都导致了湿地深度的变化。不可避免地,这些现象随后改变了自然湿地的栖息地,导致锁骨的组合转变为偏爱水质较差的物种,并在某些情况下转向富营养化。湿地水质的数量和质量下降表明生态系统服务减少,并且需要受最近社会经济发展和气候变化影响的两个流域的有效恢复措施。

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