Spatial distribution and behavior of dissolved selenium speciation in the South China Sea and Malacca Straits during spring inter-monsoon period

2021 ◽  
Vol 40 (8) ◽  
pp. 1-13
Author(s):  
Wanwan Cao ◽  
Yan Chang ◽  
Shan Jiang ◽  
Jian Li ◽  
Zhenqiu Zhang ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
Selenium Speciation ◽  
The South ◽  
Monsoon Period ◽  
China Sea ◽  
Dissolved Selenium ◽  
And Behavior

Archaeal Diversity and Spatial Distribution in the Surface Sediment of the South China Sea

2013 ◽  
Vol 31 (1) ◽  
pp. 1-11 ◽  
Author(s):  
Peng Wang ◽  
Yuli Wei ◽  
Tao Li ◽  
Fuyan Li ◽  
Jun Meng ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
South China ◽  
Surface Sediment ◽  
The South China Sea ◽  
Archaeal Diversity ◽  
The South ◽  
China Sea

Research progress on the Zhongnan-Liyue Fault Zone in the South China Sea Basin

2020 ◽  
Author(s):  
Ziying Xu ◽  
Jun Wang ◽  
Hongfang Gao ◽  
Yongjian Yao
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
Fault Zone ◽  
South China ◽  
The South China Sea ◽  
Magnetic Data ◽  
Tectonic Deformation ◽  
The South ◽  
China Sea ◽  
The North

<p>We give a review of the up-to-date research situation about The Zhongnan-Liyue Fault Zone (ZLFZ), than analyze the spatial distribution and tectonic deformation feature of the ZLFZ based on the geophysical data including topographic, seismic, gravity and magnetic data. The results show that the ZLFZ has obvious north-south segmentation characteristics in in the South China Sea Basin. The north section, which is between northwest sub-basin and east sub-basin, is a narrow zone with the width of ~16 km, and is NNW trend from 18°N,115.5°E to 17.5°N,116°E. Meanwhile ,the south section, which is between southwest sub-basin and east sub-basin, is a wide zone with the width of 60-80 km, and is NNW trend from the east of ZhongshaBank to the west of LiyueBank. The main fault of the ZLFZ is NNW trend along the seamounts ridge of Zhongnan. the ZLFZ of transition region is NNE trend from the north section to the south section. According the sub-basin’s sedimentary thickness and oceanic crust thickness exist obvious difference, on both sides of the ZLFZ, we speculate that the ZLFZ play an important role on geological structure of sub-basin. According to the chang of crustal structure, We speculate that the ZLFZ is at least a crustal fracture zone.</p><p><strong>Key words: </strong>South China Sea Basin; Zhongnan-Liyue Fault Zone; Spatial distribution; Tectonic deformation<strong> </strong></p><p><strong>Foundation item:</strong> National Natural Science Foundation of China (41606080, 41576068); The China Geological Survey Program (GZH201400202, 1212011220117, DD20160138, 1212011220116).</p>

Influence of mesoscale eddies on primary production in the South China Sea during spring inter-monsoon period

2014 ◽  
Vol 33 (3) ◽  
pp. 118-128 ◽  
Author(s):  
Zifeng Hu ◽  
Yehui Tan ◽  
Xingyu Song ◽  
Linbin Zhou ◽  
Xiping Lian ◽  
...  
Keyword(s):  
South China Sea ◽  
Primary Production ◽  
South China ◽  
Mesoscale Eddies ◽  
The South China Sea ◽  
The South ◽  
Monsoon Period ◽  
China Sea

Occurrence and spatial distribution of legacy and novel brominated flame retardants in seawater and sediment of the South China sea

2021 ◽  
Vol 271 ◽  
pp. 116324
Author(s):  
Hongru Feng ◽  
Yixue Cheng ◽  
Yuefei Ruan ◽  
Mirabelle M.P. Tsui ◽  
Qi Wang ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
South China ◽  
Flame Retardants ◽  
Brominated Flame Retardants ◽  
The South China Sea ◽  
The South ◽  
China Sea

Spatial distribution and source of biotoxins in phytoplankton from the South China Sea, China

2021 ◽  
pp. 126285
Author(s):  
Chao Liu ◽  
Ying Ji ◽  
Lei Zhang ◽  
Jiangbing Qiu ◽  
Zhaohui Wang ◽  
...  
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea

Seasonal and spatial distribution of chaetognaths on the north-west continental shelf of the South China Sea

2014 ◽  
Vol 94 (4) ◽  
pp. 837-846 ◽  
Author(s):  
X. Wu ◽  
K. Li ◽  
L. Huang ◽  
J. Yin ◽  
Y. Tan
Keyword(s):  
Spatial Distribution ◽  
South China Sea ◽  
Continental Shelf ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
North West ◽  
China Sea ◽  
The North ◽  
Region I

The seasonal variation and spatial distribution of chaetognaths were studied based on samples collected from July to August 2006 (summer), December 2006 to January 2007 (winter), and in April 2007 (spring) on the north-west continental shelf of the South China Sea. A total of 19 species of chaetognaths were identified. The average chaetognath abundances (mean ±SD) were 54.0 ± 44.5, 36.8 ±16.7 and 48.9 ± 95.5 ind. m−3 in summer, winter and spring, respectively. Flaccisagitta enflata and Serratosagitta pacifica were the dominant species during the whole sampling period, and F. enflata determined the spatial distribution of total chaetognath abundance. According to the topography and hydrological conditions, the survey area was divided into three sub-regions: inshore waters of the western Guangdong (Region I), inshore waters to the east of Hainan Island (Region II) and offshore waters from the western Guangdong to Hainan Island (Region III). The community structure and abundance distribution of chaetognaths varied significantly between the three sub-regions. The species richness was significantly different among the three sub-regions, with the lowest in Region I and the highest in Region III. The species richness was correlated positively with temperature and salinity. The abundance of chaetognaths was significantly higher in Region I than in both Regions II and III in summer and spring. The increasing food availability caused by the cold eddy, coastal upwelling and the western Guangdong coastal current was able support a greater abundance of chaetognaths during warm seasons on the north-west continental shelf of the South China Sea.

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