4.7 Article

Massive shellfish farming might accelerate coastal acidification: A case study on carbonate system dynamics in a bay scallop (Argopecten irradians) farming area, North Yellow Sea

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 798, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.149214

Keywords

Carbonate system; Scallop fanning; Photosynthesis; Respiration; Calcification; Coastal acidification

Funding

  1. Strategic Priority Research Program of the Chinese Academy of Sciences [XDA23050303]

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The study found that bay scallop farming significantly impacts the carbonate system of seawater, mainly by reducing the carbonate concentration to increase the DIC/TAlk ratio. This may accelerate the acidification process of coastal waters.
Seven cruises were carried out in a bay scallop (Argopecten irradians) farming area and its surrounding waters. North Yellow Sea, from March to November 2017 to study the dynamics of the carbonate system and its controlling factors. Results indicated that the studied parameters were highly variability over a range of spatiotemporal scales, comprehensively forced by various physical and biological processes. Mixing effect and scallop calcification played the most important role in the seasonal variation of total alkalinity (TAlk). For dissolved inorganic carbon (DIC), in addition to mixing, air-sea exchange and microbial activity, e.g. photosynthesis and microbial respiration processes, had more important effects on its dynamics. Different from the former, the changes of water pH(T), partial pressure of CO2 (pCO(2)) and aragonite saturation state (Omega(A)) were mainly controlled by the combining of the temperature, air-sea exchange, microbial activity and scallop metabolic activities. In addition, the results indicated that massive scallop farming can significantly increase the DIC/TAlk ratio by reducing the TAlk concentration in seawater, thereby reducing the buffering capacity of the carbonate system in seawater especially for Omega(A). Preliminary calculated, similar to 75.7 and similar to 45.5 mu mol kg(-1) of TAlk were removed from the surface and bottom waters respectively in one scallop cultivating cycle. If these carbonates cannot be replenished in time, it is likely to accelerate the acidification process of coastal waters. This study highlighted the control mechanism of the carbonate system under the influence of bay scallop farming, and provided useful information for revealing the potential link between human activities (shelled-mollusc mariculture) and coastal acidification. (C) 2021 Elsevier B.V. All rights reserved.

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