A Possible Connectivity among Estuarine Tapertail Anchovy (Coilia nasus) Populations in the Yangtze River, Yellow Sea, and Poyang Lake

2016 ◽  
Vol 39 (6) ◽  
pp. 1762-1768 ◽  
Author(s):  
Tao Jiang ◽  
Hongbo Liu ◽  
Mingjie Lu ◽  
Tingting Chen ◽  
Jian Yang
2013 ◽  
Vol 37 (7) ◽  
pp. 1081
Author(s):  
Gangchun XU ◽  
Zhijuan NIE ◽  
Shouling ZHANG ◽  
Yong ZHANG ◽  
Wu JIN ◽  
...  

2020 ◽  
Vol 32 (2) ◽  
pp. 506-517
Author(s):  
LIU Yi ◽  
◽  
REN Peng ◽  
YANG Xiwen ◽  
LI Xingfeng ◽  
...  

2013 ◽  
Vol 664 ◽  
pp. 27-31
Author(s):  
Zhao Jun Song ◽  
Jin Zhou ◽  
Qiao Chen ◽  
Zhen Kui Gu

research of submarine paleochannels has not only a great significance in exploring the evolution of palaeoenvironment of continental shelf but also a practical application value in solving problems on disaster geology and environmental geology in the continental shelf development. Yellow River and Yangtze River both were concentrated in the northern Jiangsu to enter the South Yellow Sea Basin in the Last Glacial, playing an important role in the palaeoenvironment evolution of the South Yellow Sea. On the basis of integrating previous research results and researching a large number of shallow stratigraphic sections of paleochannels in the South Yellow Sea Shelf in detail, identification and research of Yangtze River and Yellow River paleochannels in the South Yellow Sea Shelf are carried out in this paper. Research results show that: the Yangtze River and Yellow River paleochannels in the South Yellow Sea continental shelf are significantly different in the river section, river pattern, major elements, as well as trace elements, clay minerals, carbonate content and heavy mineral assemblages in the river sediments and other aspects. These differences can be used as the evidence for identification of the Yangtze River and Yellow River paleochannels.


2020 ◽  
Vol 36 (3) ◽  
pp. 315-325
Author(s):  
Jin Ma ◽  
Bai Li ◽  
Jing Zhao ◽  
Xuefang Wang ◽  
Cameron T. Hodgdon ◽  
...  

2014 ◽  
Vol 54 ◽  
pp. 103-112 ◽  
Author(s):  
Dong Liu ◽  
Yingying Li ◽  
Wenqiao Tang ◽  
Jinquan Yang ◽  
Hongyi Guo ◽  
...  

2011 ◽  
Vol 10 ◽  
pp. 2256-2264 ◽  
Author(s):  
Junkai Zhao ◽  
Jiufa Li ◽  
Hong Yan ◽  
Lin Zheng ◽  
Zhijun Dai

2016 ◽  
Vol 47 (S1) ◽  
pp. 102-119 ◽  
Author(s):  
Xianghu Li ◽  
Jing Yao ◽  
Yunliang Li ◽  
Qi Zhang ◽  
Chong-Yu Xu

Poyang Lake, one of the most frequently flooded regions in China, connects with the Yangtze River and the five sub-tributaries in the local catchment. The lake's hydrological regime is complicated by a complex hydraulic connection and strong river–lake interaction, especially for the extreme hydrological regime. This study analyzes the relationships between the lake level changes and the flow regimes of Yangtze River and local catchment during the flood season and employs a physically based hydrodynamic model to quantify their relative contributions to the development of floods. The study found that the large catchment runoff and Yangtze River discharge were both significant contributors to flood development but that their contributions were unevenly distributed in time and space. The local catchment imposed more influence during the period of April–May and at the middle parts of the lake, and its influence decreased toward the north and south; in contrast, the most remarkable lake level changes were observed in July–August and at the northern lake for the Yangtze River cases, and these changes reduced from north to south. Moreover, Yangtze River imposed far stronger influences on the lake level changes than the catchment runoff and dominated the duration of floods to a great extent.


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