Shelf sediments in the Benguela Upwelling System as a major source of trace metals to the shelf and eastern South Atlantic Ocean

Science Highlights

21 October 2022

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.

Figure. Schematic of different trace metal (TM) fluxes in the Benguela Upwelling System. Grey shading indicates OMZ over the Namibian shelf. Arrows (a – e) indicate different processes, a. upward transfer, b. lateral off-shelf transfer within the surface layer, c. precipitation/scavenging to the shelf edge, d. lateral transfer within the bottom shelf layer, e. off-shelf transfer from the shelf edge. The thickness of arrows (a, b, c and e) are scaled up to the magnitude of the associated flux. The dashed arrows indicate changes of different TM fluxes following ocean deoxygenation.   

Reference:

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

Latest highlights

Continuous record of the Antarctic Circumpolar Current latitude over the last glacial-interglacial cycles

The meridional positions of the oceanic fronts separating subtropical and Antarctic waters are key to constraining the mechanisms that drive the degassing of deeply-stored CO2 at the end of the glacial periods…

23 Million Years of iron sources reconstructed in the Northwest Pacific Ocean using iron isotopes in a ferromanganese crust

Using iron isotopes and elemental records, Chu and co-workers analysed an iron-manganese crust recovered from the Hongyan Seamount, and reconstructed the sources of dissolved Fe to the Northwest Pacific Ocean…

Variability of the past deep-water masses in the Arabian Sea over the last 41ka

Shukla and colleagues propose a high-resolution authigenic ƐNd record measured from a sediment core located in the eastern Arabian Sea…

Arctic outflows to Davis Strait and the Labrador Sea traced by radionuclide distributions

This study demonstrates that Arctic outflows through the Canadian Arctic Archipelago play a much more significant role than previously recognised.

Rechercher