上升流
原绿藻
透光带
海洋学
联合球菌
海底管道
水团
盐度
浮游植物
海面温度
地质学
温盐度图
环境科学
生态学
蓝藻
生物
营养物
古生物学
细菌
作者
Mei‐Lin Wu,You‐Shao Wang,Dongxiao Wang,Junde Dong
标识
DOI:10.2478/s13545-014-0143-x
摘要
Abstract Coastal upwelling occurred along the west coast of Guangdong in the northern South China Sea during the summer of 2006. The effects of upwelling on the vertical and horizontal distributions of Prochlorococcus and Synechococcus were investigated. A distinct vertical temperature difference between the surface water and water at a depth of 30 m was observed in the coastal upwelling region. There was a clear spatial variability of temperature, and an increasingly obvious horizontal gradient was created from the coast to offshore waters. Picophytoplankton communities observed from the coast to offshore waters were significantly different. In the coastal upwelling waters, the picophytoplankton community was dominated by Synechococcus within the euphotic zone. Prochlorococcus dominated the picophytoplankton community in the euphotic zone in the non-upwelling region. This difference in the picophytoplankton community structure was due to different hydrodynamics. The results of canonical correspondence analysis demonstrate that temperature, salinity, and phosphate concentration may be important factors affecting the distribution of Prochlorococcus and Synechococcus.
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