Trace metals including iron (Fe), cobalt (Co), manganese (Mn), cadmium (Cd), nickel (Ni) and copper (Cu) can regulate phytoplankton growth, marine primary productivity, ultimately carbon export in the ocean. Sources and fluxes of trace metals are therefore crucial to identify the ocean state and how ocean reacts to climate change.
Liu and her colleagues (2022, reference below) investigated dissolved trace metals distributions within the Benguela Upwelling System sampled from GEOTRACES GA08 cruise. Results reveal shelf sediments are a major redox-sensitive trace metals (Fe, Co and Mn) to the shelf and eastern South Atlantic Ocean, whereas distributions of nutrient-type trace metals (Cd, Ni and Cu) are shaped by regeneration and water masses on the shelf and in the open ocean, respectively. Estimated off-shelf fluxes of Fe and Co from 200-500m are larger than those from upper 200m, indicating an important role of shelf edge as a source of trace metals. These findings demonstrate that supplies of Fe, Co and Mn from the shelf could increase and potentially result in a more extensive regional limitation of primary production by fixed nitrogen availability in the future of ocean deoxygenation.
Liu, T., Krisch, S., Xie, R. C., Hopwood, M. J., Dengler, M., & Achterberg, E. P. Sediment release in the Benguela Upwelling System dominates trace metal input to the shelf and eastern South Atlantic Ocean. Global Biogeochemical Cycles, e2022GB007466. Access the paper: https://doi.org/10.1029/2022GB007466