Spatial and Temporal Variations of Chlorophyll a and Primary Productivity in the Hangzhou Bay

Journal of Marine Science and Engineering

Wei Zhang¹  Jianfang Chen¹  Qiang Hao¹  Yiheng Wang¹  Feng Zhou² 

[1] Key Laboratory of Marine Ecosystem Dynamics, Ministry of Natural Resources, Hangzhou 310012, China;Ocean College, Zhejiang University, Zhoushan 316021, China;

关键词: Hangzhou Bay;    chlorophyll a;    primary productivity;    light exposure;    total suspended matters;   

DOI  :  10.3390/jmse10030356

来源: DOAJ

【 摘 要 】

The Hangzhou Bay (HZB) is an important part of the Zhoushan fishing ground, the most productive region in the Eastern China Seas. Although HZB remains eutrophication all year round, its chlorophyll a (Chl) and primary productivity (PP) are usually significantly lower than those in the adjacent waters. In the present study, we presented the Chl and PP distributions in the HZB and analyzed their correlations with environmental factors in four seasons. The field observation showed that Chl and PP had significant seasonal variations, and was highest in the summer (1.66 ± 0.61 mg·m⁻³ and 12.11 ± 12.25 mg C·m⁻³·h⁻¹, respectively). Total suspended matters (TSM) concentration was the key environmental factor that constrains PP in the study area. High concentration of TSM reduced light exposure (LE, the annual mean value was 0.92 ± 0.81 Einstein·m⁻²·day⁻¹) in the mixed layer of the HZB, which was much lower than the saturated light intensity of phytoplankton growth, and thus caused a strong light limitation in the HZB. However, the seasonal variations in the photosynthesis rates (P^B) and Chl did not coincide. This fact suggested that the growth rate was not the only factor controlling seasonal variations of phytoplankton biomass. In winter, the very high TSM and strong mixing might reduce the zooplankton grazing rate, and lead to a relatively high concentration of Chl during the very low LE and P^B period. These results implied that, in the HZB, the extremely turbid water could affect both phytoplankton growth and loss, which was probably the major mechanism responsible for the complex phytoplankton spatial and temporal variations.

【 授权许可】

Unknown