Hydrological connectivity controls on the dynamics of particulate organic matter in a semi-enclosed mariculture bay
编号:3668 访问权限:仅限参会人 更新:2024-04-14 09:51:05 浏览:845次 口头报告

报告开始:2024年05月18日 14:12(Asia/Shanghai)

报告时间:7min

所在会场:[S20] 主题20、城市海岸带与陆海统筹 [S20-1] 主题20、城市海岸带与陆海统筹 专题20.1、专题20.2、专题20.5(18日下午,402)

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摘要
Semi-enclosed bay provides favorable conditions for mariculture, however, mariculture activities can disrupt hydrological connectivity of river-coastal continuum and create a bioreactor for particulate organic matter (POM). The impacts of increasing mariculture activities on POM dynamics, including sources, transportation, and transformation, associated dissolved oxygen and nutrients in semi-enclosed bays remain unclear. This study investigated carbon and nitrogen contents, as well as the stable isotopic compositions of POM (d13CPOC and d15NPN) in a semi-enclosed bay, Sansha Bay, which is the largest mariculture bay for large yellow croaker in China and is influenced by riverine input and nearshore coastal waters. Our findings revealed that, spatially, riverine POM dominated along main channel that connects river inlet and bay outlet under the influence of water mixing (C:N ratios ~5.7-15.8, d13CPOC ~-21‰--24‰, and d15NPN ~13‰-17‰). On top of water mixing, autochthonous POM dominates in off-main channel (C:N ratio 5-9, d13CPOC -21‰--17‰, and d15NPN 7.0‰-8.5‰). Using a three end-member isotopic mixing model, our data shows that the POM in main channel comprises ~90% of riverine POM and ~10% of phytoplankton production, while in off-main channel, ~59% of POM was contributed by autochthonous phytoplankton production and the rest ~41% was sourced from main channel. Furthermore, riverine POM degradation consumes oxygen along main channel, forming consistent with the classic Redfield stoichiometry of aerobic respiration (N:O2, ~0.13±0.02). In contrast, in off-main channel where water exchange is slower, the degradation of fish feed regenerates dissolved inorganic nitrogen, which subsequently stimulates phytoplankton production, leading to oxygen production following the canonical Redfield stoichiometry of phytoplankton photosynthesis (N:O2, ~0.10±0.01). Our results highlight the influence of hydrological connectivity, superimposed by mariculture activity, in shaping POM biogeochemistry and dissolved oxygen dynamics in semi-enclosed bays. These findings provide important insights for the remediation of risks of hypoxia and harmful algal blooms in coastal mariculture ecosystems.
关键词
Carbon and nitrogen stable isotopes; Organic matter; Isotopic mixing model; Oxygen consumption and production; Mariculture; Semi-enclosed coastal bay.
报告人
韩爱琴
副研究员 自然资源部第三海洋研究所

稿件作者
韩爱琴 自然资源部第三海洋研究所
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重要日期
  • 会议日期

    05月17日

    2024

    05月20日

    2024

  • 03月31日 2024

    初稿截稿日期

  • 03月31日 2024

    报告提交截止日期

  • 05月20日 2024

    注册截止日期

主办单位
青年地学论坛理事会
承办单位
厦门大学近海海洋环境科学国家重点实验室
中国科学院城市环境研究所
自然资源部第三海洋研究所
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