Dynamics of inorganic carbon and pH in a large subtropical continental shelf system: Interaction between eutrophication, hypoxia, and ocean acidification

• Published in: Limnology and Oceanography
• Main Authors: Zhao, Yangyang, Liu, Jing, Uthaipan, Khanittha, Song, Xue, Xu, Yi, He, Biyan, Liu, Hongbin, Gan, Jianping, Dai, Minhan
• Other Authors: the National Key Scientific Research Project, the University Grants Committee of Hong Kong
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2020
• Subjects: Ocean acidification
• Online Access: http://dx.doi.org/10.1002/lno.11393; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.11393; https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11393; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11393; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11393

Abstract We examined the dynamics of dissolved inorganic carbon (DIC) and pH in the Pearl River Estuary (PRE) and the adjacent northern South China Sea (NSCS) shelf in summer, aiming for a better understanding of the interaction between eutrophication, hypoxia, and ocean acidification. Using a semi‐analytical diagnostic approach based on validated multiple end‐member water mass mixing models, we showed a −191 ± 54 μ mol kg −1 deficit in DIC concentrations in an extensive surface plume bulge, corresponding to a significant pH increase of ∼ 0.57 ± 0.19 units relative to conservative mixing. In contrast, DIC additions in the bottom hypoxic zone reached ∼ 139 ± 21 μ mol kg −1 , accompanied by a decrease in pH of −0.30 ± 0.04 units. In combination with stable carbon isotopic compositions, we found biological production and CO 2 outgassing to be responsible for DIC deficits in surface waters, while degradation of organic matter (OM) accounted for DIC additions in bottom waters. The PRE‐NSCS plume system as a whole served as a net source of atmospheric CO 2 from the perspective of Lagrangian observations, because strong CO 2 outgassing in the inner estuary overwhelmed the CO 2 uptake in the plume despite strong phytoplankton blooms. Using a two‐layer box model, we further estimated that at least ∼ 45 ± 13% of eutrophication‐driven OM production in the surface plume accounted for 67 ± 18% of the DIC addition and oxygen consumption in bottom waters. Eutrophication also buffered ocean acidification in surface waters while hypoxia enhanced it in bottom waters, but their effects on acid‐base buffering capacity were secondary to the amplification of coastal ocean acidification caused by freshwater inputs.