University of KwaZulu-Natal, School of Life Sciences, Durban, South Africa.
University of KwaZulu-Natal, School of Life Sciences, Durban, South Africa.
Sci Total Environ. 2018 Jun 1;626:915-926. doi: 10.1016/j.scitotenv.2018.01.166. Epub 2018 Feb 19.
Estuarine carbon fluxes constitute a significant component of coastal CO emissions and nutrients recycling, but high uncertainty is still present due to the heterogeneity of these areas. Although South Africa has nearly 300 estuaries, very little is known about their contribution to carbon emissions or sequestration. This study aims to provide a first estimation of the carbon emissions and nutrient fluxes of South African sub-tropical estuaries through a direct quantification of respiration, primary production and nutrient regeneration of benthic and planktonic communities. In order to account for the extreme variability in subtropical estuarine areas, due to seasonality in rainfall, two estuaries with opposite characteristics were studied; the temporarily open/closed Mdloti Estuary subjected to strong anthropic pressure, and the permanently open Mlalazi Estuary located in a natural reserve. Field deployment of benthic chambers and clear/dark bottles assessed oxygen, ammonia and phosphate fluxes of both benthic and planktonic communities. An inverse pattern between benthic and pelagic primary production was found in both estuaries. Different drivers related to mouth status and sediment characteristics were identified in the two estuaries. The annual average carbon emission indicates that the two systems are heterotrophic over the year releasing substantial CO emissions into the atmosphere. Results show that carbon fluxes in subtropical estuaries are extremely variable in space and time. Future up-scaling carbon estimations need to account for those small scale and regional dynamics.
河口碳通量是沿海 CO 排放和营养物质循环的重要组成部分,但由于这些地区的异质性,仍然存在很大的不确定性。尽管南非拥有近 300 个河口,但对它们对碳排放或封存的贡献知之甚少。本研究旨在通过直接量化底栖和浮游生物群落的呼吸、初级生产和营养再生,对南非亚热带河口的碳排放量和营养通量进行首次估算。为了说明由于降雨量季节性导致亚热带河口地区的极端可变性,研究了两个具有相反特征的河口;受强烈人为压力影响的暂时开放/封闭的 Mdloti 河口,以及位于自然保护区内的永久性开放的 Mlalazi 河口。现场部署底栖室和透明/黑暗瓶评估了底栖和浮游生物群落的氧气、氨和磷酸盐通量。在两个河口都发现了底栖和浮游初级生产之间的相反模式。在两个河口,确定了与河口状态和沉积物特征相关的不同驱动因素。年平均碳排放量表明,这两个系统全年都是异养的,向大气中释放大量的 CO 排放。结果表明,亚热带河口的碳通量在空间和时间上变化极大。未来的碳估算需要考虑到这些小规模和区域性的动态变化。