Hypoxia, acidification and nutrient accumulation in the Yellow Sea Cold Water of the South Yellow Sea

2020 ◽  
Vol 745 ◽  
pp. 141050
Author(s):  
Jinqiang Guo ◽  
Huamao Yuan ◽  
Jinming Song ◽  
Xuegang Li ◽  
Liqin Duan
2020 ◽  
Vol 428 ◽  
pp. 106244 ◽  
Author(s):  
Yi Zhong ◽  
Lulu Qiao ◽  
Dehai Song ◽  
Yang Ding ◽  
Jishang Xu ◽  
...  

2020 ◽  
Vol 7 ◽  
Author(s):  
Qian Zhang ◽  
Min Su ◽  
Peng Yao ◽  
Yongping Chen ◽  
Marcel J. F. Stive ◽  
...  

Tidal currents belong to the main driving forces shaping the bathymetry of marginal seas. A globally unique radial sand ridge field exists in the South Yellow Sea off the central Jiangsu coast, China. Its formation is related to the distinctive “radial tidal current” pattern at that location. A generally accepted hypothesis is that the “radial tidal current” is a consequence of the interference between the northern amphidromic tidal wave system and the southern incoming tidal wave. In this study, a schematized numerical tidal model was designed to investigate the tidal current system and the factors of influence in the South Yellow Sea. Concepts of the tidal current amphidromic point (CAP) and the tidal current inclination angle are utilized to analyze the inherent structure of the tidal current system. By conducting a series of numerical experiments, it is found that the Poincaré modes are necessary for the existence of “radial tidal current,” and the e-folding decay length should be smaller than the basin length. In the Yellow Sea, cross-basin phase differences due to lateral depth differences as well as open boundary conditions favor the emergence of the “radial tidal current.” Further analyses indicate that the CAP system (i.e., the co-inclination lines, the CAPs, and the tidal ellipticity) deepens the understanding on the dynamic structure of a tidal current system, and therefore, it deserves more attention in future studies.


Diversity ◽  
2021 ◽  
Vol 13 (1) ◽  
pp. 21
Author(s):  
Yanfeng Sun ◽  
Yang Liu ◽  
Chao Wu ◽  
Xiaoting Fu ◽  
Congcong Guo ◽  
...  

Eukaryotic plankton are important parts of the marine biome and play an important role in maintaining the stability of marine ecosystems. In order to characterize the eukaryotic plankton communities in the South Yellow Sea Cold Water Mass (CWM) and the South Yellow Sea nearshore waters (NW) in October 2019, Illumina high–throughput sequencing was performed using the 18S rDNA V9 region as the target gene. Environmental factors (depth, pH, salinity, temperature, Chl a, nitrate, nitrite, ammonium, silicate, phosphate) in two sea areas were measured, and their correlations with abundance and diversity of eukaryotic plankton were analyzed. A total of 807 species of plankton were identified, of which 663 species in 24 categories were from the CWM area, and 614 species in 26 categories were from NW. The total phytoplankton abundance in CWM waters was higher than that in NW. Dinophyta and Bacillariophyta were the most abundant phyla of phytoplankton in the two areas. Arthropoda and Cnidaria were the major zooplankton taxa. The dominant fungal population was mainly Basidiomycota. Both the CWM and NW have effects on dissolved inorganic nutrient concentrations and plankton abundance. Environmental factor correlation analysis showed that the concentration of dissolved inorganic nutrients within the CWM increased with water depth and the abundance of plankton gradually increased. Ammonium salts, nitrates, phosphates, silicates and water depth were important factors affecting phytoplankton growth. Phytoplankton abundance increased with increasing concentrations of inorganic nutrients. Bacillariophyta showed a strong positive correlation with silicates and depth. Depth and microscopic phytoplankton abundance were important factors influencing the structure of the zooplankton community.


2012 ◽  
Vol 32 (2) ◽  
pp. 85-92 ◽  
Author(s):  
Fanghui HOU ◽  
Xunhua ZHANG ◽  
Zhixun ZHANG ◽  
Zhenhe WEN ◽  
Rihui LI ◽  
...  

1999 ◽  
Vol 42 (1) ◽  
pp. 97-112 ◽  
Author(s):  
Ying Wang ◽  
Dakui Zhu ◽  
Kunyuan You ◽  
Shaoming Pan ◽  
Xiaodong Zhu ◽  
...  

Author(s):  
Ye Chen ◽  
Siqi Li ◽  
Xiaoqing Xu ◽  
Manman Ma ◽  
Tiezhu Mi ◽  
...  

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.


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