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Volume 38 Issue 4
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Article Navigation >  Haiyang Xuebao  > 2016  >  38(4): 1-21
Sun Jun, Li Xiaoqian, Chen Jianfang, Guo Shujin. Progress in oceanic biological pump[J]. Haiyang Xuebao, 2016, 38(4): 1-21. doi: 10.3969/j.issn.0253-4193.2016.04.001
Citation: Sun Jun, Li Xiaoqian, Chen Jianfang, Guo Shujin. Progress in oceanic biological pump[J]. Haiyang Xuebao, 2016, 38(4): 1-21. doi: 10.3969/j.issn.0253-4193.2016.04.001
shu

Progress in oceanic biological pump

doi: 10.3969/j.issn.0253-4193.2016.04.001
  • 1.

    College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China

  • 2.

    State Oceanic Administration Key Laboratory of Marine Ecosystems and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration Hangzhou 310012, China

  • Received Date: 2016-01-20
  • Rev Recd Date: 2016-03-31
    Abstract
  • Oceanic biological pump, as an important component of oceanic carbon cycle, transfers the atmospheric carbon into the deep ocean. In this paper, the processes in oceanic carbon sink and biological pump are discussed, including sinking of phytoplankton cells, zooplankton fecal pellet package effects, transparent exopolymer particles (TEP) sinking, marine snow sinking and carbonate counter pump. Meanwhile, the present paper attempts to state the progress and perspectives of the biological pump in the South China Sea, which contributes to the carbon cycle in China Seas.
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    • References(172)
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