Plankton Mediated Carbon Sink Processes in the Eastern Indian Ocean
编号:604 访问权限:仅限参会人 更新:2026-08-31 17:36:14 浏览:0次 特邀报告

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摘要
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.
 
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报告人
Jun Sun
Tianjin University of Science and Technology

稿件作者
Jun Sun Tianjin University of Science and Technology
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重要日期
  • 会议日期

    01月12日

    2027

    01月15日

    2027

  • 07月21日 2026

    初稿截稿日期

  • 01月15日 2027

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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