[口头报告]Hydrological connectivity controls on the dynamics of particulate organic matter in a semi-enclosed mariculture bay

Hydrological connectivity controls on the dynamics of particulate organic matter in a semi-enclosed mariculture bay
编号:3668 稿件编号:353 访问权限:仅限参会人 更新:2024-04-14 09:51:05 浏览:41次 口头报告

报告开始:2024年05月18日 14:12 (Asia/Shanghai)

报告时间:7min

所在会议:[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.
关键字
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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