Impact of anthropogenic forcing on the environmental controls of phytoplankton dynamics between 1974 and 2017 in the Pearl River estuary, China

• Published in: Ecological indicators 2020-09, Vol.116, p.106484, Article 106484
• Main Authors: Niu, Lixia, Luo, Xiangxin, Hu, Shuai, Liu, Feng, Cai, Huayang, Ren, Lei, Ou, Suying, Zeng, Danna, Yang, Qingshu
• Format: Article
• Language: English
• Subjects: Anthropogenic impact; Hydrological control; Nutrient limitation; Pearl River estuary; Phytoplankton chlorophyll
• ISSN: 1470-160X; 1872-7034
• DOI: 10.1016/j.ecolind.2020.106484

•Time-varying change in environmental drivers of chlorophyll investigated.•Shift in nutrient dynamics exerted from the shoal-trough instability.•Influence of riverine input on chlorophyll strong.•Role of human activity on environmental factors significant. How phytoplankton responded spatiotemporally to the co-occurrence of multiple variables is of central importance for ecosystem management. In this study, extensive investigations in the Pearl River estuary (PRE), southern China, between 1974 and 2017 revealed a strong anthropogenic effect on the environmental drivers of phytoplankton dynamics (in terms of chlorophyll a). The empirical cause-and-effect chain summarized as human activity → hydrology → nutrient → chlorophyll may constitute fundamental quantitative tools for predicting effects of coastal eutrophication. Change in subaqueous topography induced by human stress resulted in shoal-trough instability, which unexpectedly shifted nutrient dynamics across the entire regions. Over time, dissolved inorganic nitrogen (DIN) and phosphorus (PO4) increased, as did the molar N/P ratio (DIN/PO4), indicating that phytoplankton growth was potentially phosphate-limited in most PRE. The adsorption of phosphorus by sediment particles was stronger than that of nitrogen. The quantification of phytoplankton drivers demonstrated the importance of river-tide dynamics, which incorporated the interplay between environmental variables. Particularly, the influence of riverine input varied over time and site, affecting hydrological control variables and nutrient limitations. Our structural equation modelling results (p