Chlorophyll maxima layer in a large subtropical reservoir (Xinanjiang Reservoir): Spatial development process and limitation by CO2 and phosphorus

• Published in: Water research (Oxford) 2022-08, Vol.222, p.118912-118912, Article 118912
• Main Authors: Luo, Jiajie, Hu, Zhehui, Chen, Xueping, Li, Xiaoying, Liu, Liu, Yang, Meilin, Miao, Haocheng, Chu, Yongsheng, Xu, Peifan, Wang, Fushun
• Format: Article
• Language: English
• Subjects: Dissolved CO2 limitation; Large subtropical reservoir; Seasonal thermal stratification; Subsurface chlorophyll-a maxima
• ISSN: 0043-1354; 1879-2448
• DOI: 10.1016/j.watres.2022.118912

•Seasonal and spatial heterogeneity of subsurface chlorophyll maxima in a reservoir.•Thermal stratification of water column is the basis for SCM development.•DCO2 limitation shift to phosphorus limitation downward across the SCM layer.•Incoming water supply nutrient for middle water layer during thermal stratification. In marine investigations, the maximum chlorophyll-a (Chla) concentration is often reported to occur at a specific depth below the ocean surface, a phenomenon known as subsurface Chla maxima (SCM). However, SCM has long been overlooked in artificial reservoirs, which may lead to a serious underestimation of the primary productivity level and trophic status of reservoirs. To better understand the temporal and spatial variability of SCM and the mechanisms leading to SCM development, this study conducted a detailed survey in a large subtropical reservoir (Xinanjiang Reservoir, XAJR) from September 2020 to August 2021. The seasonal thermal stratification, in situ variables (WT, pH, DO and Chla), nutrient concentrations (DSi, NO3−, DIP and DCO2), Chla maxima depth and magnitude of the riverine region (S1), transition region (S2) and the central part of the XAJR (S3 and S4) were all thoroughly investigated. Thermal stratification and SCM in XAJR exhibited significant seasonal and spatial heterogeneity. Phytoplankton biomass in the epilimnion was limited by dissolved CO2 from June to October in the warm seasons, while it was primarily limited by phosphorus in the other seasons, according to the nutrient limitation analysis. Along the water column, dissolved CO2 limitation occurred mainly above the SCM layer, and the water column below the SCM layer gradually transitioned from dissolved CO2 limitation to phosphorus limitation. Furthermore, as the thermal stratification developed, the upstream water mass moves along the middle of the water column as density flow toward the reservoir, providing nutrients for the development of the SCM. This research contributes to a better understanding of the temporal and spatial variation of SCM and nutrient supply in deep and large stratified reservoirs. [Display omitted]