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1. Key Laboratory of Marine Bio-Resources Sustainable Utilization South China Sea Institute of Oceanology Chinese Academy of Sciences
2. State Key Laboratory of Tropical Oceanography South China Sea Institute of Oceanology Chinese Academy of Sciences
网络首发:2013-03-07,
纸质出版:2013
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Spatio-temporal variations in the siphonophore community of the northern South China Sea[J]. 海洋湖沼学报(英文), 2013,31(2):312-326.
Li, K., Yin, J., Huang, L. et al. Spatio-temporal variations in the siphonophore community of the northern South China Sea., Chin. J. Ocean. Limnol. 31, 312–326 (2013). https://doi.org/10.1007/s00343-013-2058-6
Spatio-temporal variations in the siphonophore community of the northern South China Sea[J]. 海洋湖沼学报(英文), 2013,31(2):312-326. DOI: 10.1007/s00343-013-2058-6.
Li, K., Yin, J., Huang, L. et al. Spatio-temporal variations in the siphonophore community of the northern South China Sea., Chin. J. Ocean. Limnol. 31, 312–326 (2013). https://doi.org/10.1007/s00343-013-2058-6 DOI:
To understand how hydrological and biological factors affect near- to off-shore variations in the siphonophore community
we sampled zooplankton at 82 stations in the northern South China Sea during summer
winter
and spring. Forty-one species of siphonophore were collected by vertical trawling. The species richness of siphonophores increased from the nearshore to offshore regions in all three seasons of investigation
with maximum richness in summer and minimum richness in winter. The abundance of siphonophores was also higher in summer than in spring and winter
concentrated in the nearshore region in the warm season and scattered in the offshore region in the cold season. Four siphonophore groups were classified according to the frequency of occurrence: nearshore
near-offshore
offshore
and tropical pelagic. Among them
the nearshore group had higher abundance nearshore compared with the offshore. The tropical pelagic group had higher species number offshore than nearshore. Spatial and temporal fluctuations in taxonomic composition and abundance of siphonophores were due to the influence of the coastal upwelling and surface ocean currents of the South China Sea
driven by the East Asia monsoonal system.
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