Hydrological connectivity controls on the dynamics of particulate organic matter in a semi-enclosed mariculture bay
ID:3668 View Protection:ATTENDEE Updated Time:2024-04-14 09:51:05 Hits:1798 Oral Presentation

Start Time:2024-05-18 14:12(Asia/Shanghai)

Duration:7min

Session: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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Abstract
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.
Keywords
Carbon and nitrogen stable isotopes; Organic matter; Isotopic mixing model; Oxygen consumption and production; Mariculture; Semi-enclosed coastal bay.
Speaker
韩爱琴
副研究员 自然资源部第三海洋研究所

Submission Author
韩爱琴 自然资源部第三海洋研究所
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    May 17

    2024

    to

    May 20

    2024

  • Mar 31 2024

    Draft paper submission deadline

  • Mar 31 2024

    Contribution Submission Deadline

  • May 20 2024

    Registration deadline

Sponsored By
青年地学论坛理事会
Organized By
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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