The Xiamen Symposium on Marine Environmental Sciences

2027 Xiamen Symposium on Marine Environmental Sciences

January 12-15, 2027

Plankton Mediated Carbon Sink Processes in the Eastern Indian Ocean
ID:604 Invited Oral Presentation

2027-01-14 13:30 (China Standard Time)

Session:Session 49 - Biological Carbon Pump: New Insights from Field Observations and Model Constraints

Abstract
The Eastern Indian Ocean is a climatically sensitive region characterized by strong monsoon forcing, persistent upper ocean stratification, complex circulation, and extensive oxygen deficient waters. Despite relatively low primary productivity, this region can exhibit high carbon export efficiency, highlighting the importance of plankton community structure, particle formation, and sinking processes in regulating ocean carbon sequestration. Based on multidisciplinary observations collected during a series of Indian Ocean expeditions from 2010 to 2024, we investigated major plankton mediated carbon fixation and export pathways, including primary production, nitrogen fixation, transparent exopolymer particles, phytoplankton sinking, zooplankton fecal pellet production, calcification, silicification, and greenhouse gas production.
Depth integrated primary production in the euphotic zone ranged from 113 to 817 mg C m-2 d-1, with an average of 522 mg C m-2 d-1. Nitrogen fixation contributed approximately 0.3 to 1.3 percent of primary production, with small diazotrophs contributing most strongly throughout the water column. Phytoplankton sinking rates ranged from minus 0.291 to 2.188 m d-1 and were jointly regulated by community composition, nutrient availability, temperature, and water column stratification. Transparent exopolymer particles represented an important component of particle aggregation, with an integrated carbon inventory of 2136.36 ± 929.94 mg C m-2 and sinking rates ranging from minus 0.3 to 1.9 m d⁻¹. Zooplankton fecal pellets provided an additional pathway for rapid carbon export, with estimated production rates of 4.033 to 68.19 mg C m-2 d-1.
Regional synthesis suggests an annual primary production of approximately 718 Tg C, of which transparent exopolymer particles, fecal pellets, particulate organic carbon export, and calcification account for substantial fractions. However, microbial degradation of sinking organic matter also produces CO2, CH4, and N2O, partially offsetting the climatic benefits of biological carbon sequestration. These findings emphasize that assessments of the Indian Ocean biological carbon pump should integrate carbon fixation, particle export, remineralization, and associated greenhouse gas emissions within a unified framework.
 
Speaker
Jun Sun Tianjin University of Science and Technology

Author
Jun Sun Tianjin University of Science and Technology

    Important Dates

    • Jan 30

      2026

      Session / Event proposals open

    • Mar 31

      2026

      Session / Event proposals close
      (Extended to April 7)

    • Apr 30

      2026

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    • Apr 30

      2026

      Abstract submissions & registration open

    • Jun 30

      2026

      Abstract submissions close
      (Extended to July 21)

    • Aug 31

      2026

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    • Sep 15

      2026

      Scientific program released

    • Oct 15

      2026

      Early bird registration closes

    • Jan 12–15

      2027

      XMAS 2027