Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (4): 50-60.doi: 10.11978/2019101CSTR: 32234.14.2019101

• Marine Biology • Previous Articles     Next Articles

Response of phytoplankton community to atmospheric deposition along Pearl River plume front

Weiwen ZHOU1,2(), Qian LI1,2(), Zaiming GE1,2, Zijia LIU1,2, Yiping SHUAI1,2, Mengzhen MA1,2   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
  • Received:2019-10-15 Revised:2020-01-06 Online:2020-07-20 Published:2020-07-27
  • Contact: Qian LI E-mail:wwzhou@scsio.ac.cn;qianli@scsio.ac.cn
  • Supported by:
    Foundation item: National Natural Science Foundation of China(41676108);Project of State Key Laboratory of Tropical Oceanography(LTOZZ1705);Project of State Key Laboratory of Tropical Oceanography(LTOZZ1803)

Abstract:

The Pearl River plume water can form an active plume front along the coastal northern South China Sea. A higher biomass of phytoplankton could exist along the plume front affected by hydrological factors. Atmospheric deposition from land-source input has a significant impact on the ecosystem of the Pearl River Delta zone. A field survey at the western part of the Pearl River Estuary was conducted in March 2019. Substantial variations of size-fractionation phytoplankton community and picoplankton were determined along a section, which affected by the plume front. Meanwhile, atmospheric deposition amendment experiments of three stations, covering different regions of the plume front, were conducted. Results showed that the size-fractionation phytoplankton community was dominated by microphytoplankton at the shore side of the front, picophytoplankton at the sea side of the front, and evenly distributed at the frontal zone with relatively higher biomass. At the frontal zone, the total phytoplankton community was limited by Nitrogen, while the Synechococcus showed a Phosphorus-limitation. Species among the frontal zone could show different nutrients demands. Atmospheric dry or wet deposition could stimulate the growth of three size-fractionation phytoplankton community. The microphytoplankton showed higher growth rate with atmospheric dry or wet amendments at shore side or sea side of the front, while the growth of three size-fractionation phytoplankton community could be stimulated indistinguishably. The addition of atmospheric deposition significantly stimulated the growth of Picoeukaryotes in the frontal system and of Synechococcus at the shore side of the front. Inhibited effects on Synechococcus and Prochlorococcus were found at the frontal zone and sea side of the front.

Key words: plume front, phytoplankton size structure, picoplankton, atmospheric deposition

CLC Number: 

  • P735