Informative zinc isotopic fractionation in the Southern Ocean

Science Highlights

9 March 2020

Ellwood and co-workers (2020, see reference below) established the distribution of dissolved and particulate zinc (dZn and pZn respectively) and its isotopes in the Subantarctic Zone South of Tasmania.

Concentration profiles show that zinc has a longer regeneration length scale than phosphorus and of cadmium, but shorter than copper. Modelling of the particulate profiles produced variable vertical attenuation factors of 0.82, 2.04, 2.41 and 0.28 for zinc, phosphorus, cadmium and copper respectively.

Interestingly, concentrations and isotopic Zn distributions were established inside cold-core eddy (CCE) and compared to the same parameter distributions outside the eddy.

The isotope composition of surface dZn (δ66Zndissolved) from the CCE station is ~ twice its deep water value. This is likely due to the isolated nature of the cold-core, which retains the signals of isotope fractionation, while they are likely lost by mixing outside the core.

The authors then apply a 1D-simulation to their data and show that the isotopic structure of the dissolved and particulate zinc from this specific station are determined by the interplay of processes like uptake by phytoplankton, complexation of zinc with natural organic ligands and the regeneration of zinc from particulate matter.

2020 Ellwood
Figure: Model results highlighting seasonal variations in the isotope composition dissolved zinc (top middle panel) particulate zinc (central middle panel) and the difference between dissolved and particulate (bottom middle panel). These model results suggest in the upper ocean that the zinc isotope composition of seawater should vary seasonally with changes and in phytoplankton production. This is highlighted in the simulated dissolved and particulate profiles for late summer/autumn (top right panel) and winter (bottom right panel). The map (left panel) shows the locations of Southern Ocean stations sampled in this study. Click on the figure to view it larger.

Reference:

Ellwood, M. J., Strzepek, R., Chen, X., Trull, T. W., & Boyd, P. W. (2020). Some observations on the biogeochemical cycling of zinc in the Australian sector of the Southern Ocean: a dedication to Keith Hunter. Marine and Freshwater Research, 71(3), 355. Access the paper: https://doi.org/10.1071/MF19200

Latest highlights

Deep-sea mining, dewatering waste, accidental plumes and their potential consequences on trace metal fates in the North Pacific Ocean

Xiang and his colleagues conducted laboratory incubation experiments that simulate mining discharge into anoxic waters.

Biogeochemical behaviours of barium and radium-226 in the Pacific Ocean

Barium and radium-226 are not just proxies for nutrients and ocean circulation but are themselves marine biogeochemical tracers…

Intrigued by Rare Earth Elements and neodymium isotopes? A review for the curious

Vanessa Hatje and a group of Rare Earth Element (REE) specialists propose an exhaustive review on the behaviour of REE.

North-South section of bioactive cadmium, nickel, zinc, copper and iron along GEOTRACES transect GP19 in the Pacific Ocean

Zheng and his colleagues propose the first full sections of the simultaneous dissolved distributions of five nutrient-type trace metals in the western South Pacific Ocean.

Rechercher