Volume 39 Issue 6
Jun.  2020
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Dawei Chen, Congcong Guo, Linhui Yu, Yuanzhen Lu, Jun Sun. Phytoplankton growth and microzooplankton grazing in the central and northern South China Sea in the spring intermonsoon season of 2017[J]. Acta Oceanologica Sinica, 2020, 39(6): 84-95. doi: 10.1007/s13131-020-1593-1
Citation: Dawei Chen, Congcong Guo, Linhui Yu, Yuanzhen Lu, Jun Sun. Phytoplankton growth and microzooplankton grazing in the central and northern South China Sea in the spring intermonsoon season of 2017[J]. Acta Oceanologica Sinica, 2020, 39(6): 84-95. doi: 10.1007/s13131-020-1593-1

Phytoplankton growth and microzooplankton grazing in the central and northern South China Sea in the spring intermonsoon season of 2017

doi: 10.1007/s13131-020-1593-1
Funds:  The National Key Research and Development Program of China under contract No. 2019YFC1407805; the National Natural Science Foundation of China under contract Nos 41876134 and 41676112; the University Innovation Team Training Program for Tianjin under contract No. TD12-5003; the Tianjin 131 Innovation Team Program under contract No. 20180314; the Changjiang Scholar Program of Chinese Ministry of Education to Jun Sun under contract No. T2014253.
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  • Corresponding author: E-mail: phytoplankton@163.com
  • Received Date: 2019-05-15
  • Accepted Date: 2019-06-17
  • Available Online: 2020-12-28
  • Publish Date: 2020-06-25
  • Phytoplankton growth rates and mortality rates were experimentally examined at 21 stations during the 2017 spring intermonsoon (April to early May) in the northern and central South China Sea (SCS) using the dilution technique, with emphasis on a comparison between the northern and central SCS areas which had different environmental factors. There had been higher temperature but lower nutrients and chlorophyll a concentrations in the central SCS than those in the northern SCS. The mean rates of phytoplankton growth (μ0) and microzooplankton grazing (m) were (0.88±0.33) d–1 and (0.55±0.22) d–1 in the central SCS, and both higher than those in the northern SCS with the values of μ0 ((0.81±0.16) d–1) and m ((0.30±0.09) d–1), respectively. Phytoplankton growth and microzooplankton grazing rates were significantly coupled in both areas. The microzooplankton grazing impact (m/μ0) on phytoplankton was also higher in the central SCS (0.63±0.12) than that in the northern SCS (0.37±0.06). The microzooplankton abundance was significantly correlated with temperature in the surface. Temperature might more effectively promote the microzooplankton grazing rate than phytoplankton growth rate, which might contribute to higher m and m/μ0 in the central SCS. Compared with temperature, nutrients mainly affected the growth rate of phytoplankton. In the nutrient enrichment treatment, the phytoplankton growth rate (μn) was higher than μ0 in the central SCS, suggesting phytoplankton growth in the central SCS was nutrient limited. The ratio of μ0/μn was significantly correlated with nutrients concentrations in the both areas, indicating the limitation of nutrients was related to the concentrations of background nutrients in the study stations.
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