The response of zooplankton communities to the 2016 extreme hydrological cycle in floodplain lakes connected to the Yangtze River in China

2018 ◽  
Vol 25 (23) ◽  
pp. 23286-23293 ◽  
Author(s):  
Kun Zhang ◽  
Mei Xu ◽  
Qili Wu ◽  
Zhi Lin ◽  
Fangyuan Jiang ◽  
...  
Water ◽  
2020 ◽  
Vol 12 (3) ◽  
pp. 842 ◽  
Author(s):  
Naveed Ahmed ◽  
Genxu Wang ◽  
Martijn J. Booij ◽  
Adeyeri Oluwafemi ◽  
Muhammad Zia-ur-Rahman Hashmi ◽  
...  

The headwaters of the Yangtze River are located on the Qinghai Tibetan Plateau, which is affected by climate change. Here, treamflow trends for Tuotuohe and Zhimenda sub-basins and relations to temperature and precipitation trends during 1961–2015 were investigated. The modified Mann–Kendall trend test, Pettitt test, wavelet analysis, and multivariate correlation analysis was deployed for this purpose. The temperature and precipitation significantly increased for each sub-basin, and the temperature increase was more significant in Tuotuohe sub-basin as compared to the Zhimenda sub-basin. A statistically significant periodicity of 2–4 years was observed for both sub-basins in different time spans. Higher flow periodicities for Tuotuohe and Zhimenda sub-basin were found after 1991 and 2004, respectively, which indicates that these are the change years of trends in streamflows. The influence of temperature on streamflow is more substantial in Tuotuohe sub-basin, which will ultimately impact the melting of glaciers and snowmelt runoff in this sub-basin. Precipitation plays a more critical role in the Zhimenda streamflow. Precipitation and temperature changes in the headwaters of the Yangtze River will change the streamflow variability, which will ultimately impact the hydropower supply and water resources of the Yangtze Basin. This study contributes to the understanding of the dynamics of the hydrological cycle and may lead to better hydrologic system modeling for downstream water resource developments.


<em>Abstract</em>.—The Yangtze (Changjiang) River floodplain is one of the most important ecosystems in China, as well as in the world, but is seriously threatened by multiple factors. Thus, it is crucial and urgent to rehabilitate the river floodplain. This paper reviews ecological studies conducted on the Yangtze River floodplain and presents suggestions for conservation and rehabilitation. First, the Yangtze River system is briefly introduced. Formed 23 million years ago, the Yangtze River is ca. 6,300 km in length with a mean annual runoff of 9.6 × 10<sup>11</sup> m<sup>3</sup>. Thousands of floodplain lakes are distributed along the mid-lower Yangtze River, and the total area remains 15,770 km<sup>2</sup> at present. Such a river-lake complex ecosystem holds a unique and diverse biota, with ca. 400 hydrophytes and hygrophytes, ca. 170 mollusks, ca. 200 fishes, ca. 400 water birds, and endangered dolphins and porpoises. Second, main threats to the Yangtze River floodplain ecosystem are identified: (1) habitat loss, including river channelization, sharp shrinkage of lake area (ca. 10,000 km<sup>2</sup> since the 1950s), degradation of lakeshore zones, and sand overmining; (2) alternations of hydrological regimes, including construction of ca. 47,000 reservoirs in the whole basin and disconnection of most floodplain lakes from the main stem; (3) water pollution, including eutrophication, heavy metals, and organic pollutants; and (4) overexploitation of biological resources, including overfishing and intensive pen culture. Third, effects of river–lake disconnection on lake ecosystems are summarized on the basis of our studies in the past 20 years. It was found that (1) disconnection is one of the main causes of lake eutrophication; (2) species diversity, biomass, and production of macrophytes and macrobenthos reach maxima at some levels of intermediate river connectivity; (3) disconnection greatly reduces fish species richness of each habitat guild, and natural fish larvae is severely depleted; and (4) disconnection simplifies macroinvertebrate food web structure, and the trophic basis of the simplified food web is more heavily dependent on detritus in disconnected lakes. Last, conservation strategies are proposed. Since the Yangtze River floodplain is a huge integrated system, the biodiversity conservation must be conducted on the whole basin scale. By establishing species–area models of fishes, the minimum protected area of Yangtze-connected lakes is estimated to be ca. 14,400 km<sup>2</sup>. It means that at least 8,900 km<sup>2</sup> of disconnected lakes should be reconnected with the Yangtze main stem, and ecohydrological operation of dams and sluices is the feasible approach. Based upon our preliminary studies on environmental flow requirements, the following measures are suggested: (1) lower water levels during spring to improve germination of macrophytes, and control rising rates of water levels during spring–summer to ensure development of macrophytes; and (2) open sluice gates to restore migration routes for juveniles migrating into lakes during April–September and for adults migrating back to the Yangtze main stem during November–December.


2004 ◽  
Vol 88 (8) ◽  
pp. 59-64
Author(s):  
Changyu Shao ◽  
Qinger Deng

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