Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; University of Chinese Academy of Sciences, Beijing 100049, China.
Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; Laboratory of Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China.
Harmful Algae. 2017 Feb;62:60-72. doi: 10.1016/j.hal.2016.12.006. Epub 2017 Jan 4.
The sea area adjacent to the Changjiang River estuary is the most notable region for harmful algal blooms (HABs) in China as both diatom and dinoflagellate blooms have been recorded in this region. Affected by the Changjiang diluted water (CDW) and currents from the open ocean (i.e., Taiwan warm current, TWC), the environmental conditions in the coastal waters adjacent to the Changjiang River estuary are quite complex. To obtain a better understanding of the mechanisms of HABs in this region, analyses based on field investigation data collected by the National Basic Research Priority Program (CEOHAB I) were performed using principle component analysis (PCA), multiple regression analysis (MRA) and path analysis (PA). The results suggested that phosphate and silicate are the major factors that directly affect the diatom bloom, while dissolved inorganic nitrogen (DIN), temperature and turbidity are the factors that influence the dinoflagellate bloom. CDW and the TWC have different roles in affecting the two types of algal blooms. CDW, which has a high concentration of nitrate and silicate, is essential for the diatom bloom, while the intrusion of the TWC (mainly Kuroshio subsurface water that is rich in phosphate at the bottom) is critical for the maintenance of the dinoflagellate bloom. The results of this study offer a better understanding of the mechanisms of HABs in the East China Sea.
毗邻长江口的海域是中国赤潮最显著的区域,该区域既有硅藻赤潮又有甲藻赤潮的记录。受长江淡水(CDW)和来自外海的海流(即台湾暖流,TWC)的影响,毗邻长江口的沿海海域的环境条件非常复杂。为了更好地了解该区域赤潮的机制,利用国家重点基础研究发展计划(CEOHAB I)收集的现场调查数据进行了主成分分析(PCA)、多元回归分析(MRA)和路径分析(PA)。结果表明,磷酸盐和硅酸盐是直接影响硅藻赤潮的主要因素,而溶解无机氮(DIN)、温度和浊度是影响甲藻赤潮的因素。CDW 和 TWC 对两种藻类赤潮的影响作用不同。CDW 具有高浓度的硝酸盐和硅酸盐,对硅藻赤潮至关重要,而 TWC 的入侵(主要是富含磷酸盐的底层黑潮次表层水)对甲藻赤潮的维持至关重要。本研究结果更好地了解了东海赤潮的机制。