Why is the deep ocean zinc isotopic signature so heavy?

The oceanic balance of the micronutrient zinc (Zn) is getting more puzzling –although better documented- while the Zn isotope data set increases. Presenting the first high resolution section of seawater dissolved Zn concentration and Zn isotope ratios (δ66Zn) from the North Atlantic, Conway and John (2014, see reference below) confirm that the deep ocean is fairly homogeneous for δ66Zn, close to +0.5‰, except near local North Atlantic sources of Zn (margins, the Mediterranean Sea, hydrothermal vents) where it is isotopically lighter.

Balancing the Zn isotopic budget raises questions. Indeed, the known inputs of this element (continental, riverine, and aerosol) display δ66Zn ranging between 0 and +0.3‰ while the known outputs (carbonates, ferromanganese nodules, and ferromanganese crusts) are isotopically heavier (+0.9 to +1‰). As previously suggested by Little et al. (2014, see also highlight about it), an isotopically light sink is therefore missing. The authors suggest that burial of biogenic Zn in sediments might be this important sink. They also suggest a potential role for zinc sulfide (ZnS) precipitation in low-oxygen open-ocean waters as a possible light sink, analogous to recent studies on Cd (Janssen et al., 2014, see also highlight about it).

14 Conway2 l
Figure. Distribution of dissolved stable Zn isotope ratios (δ66Zn) for the US GEOTRACES North Atlantic GA03 and GA03_e sections. δ66Zn is expressed relative to JMC Lyon standard. Station numbers are shown for 2010 (USGT10, red) and 2011 (USGT11, blue). The black vertical line denotes the crossover between the cruises at USGT10-12 and USGT11-24. Click here to view the figure larger.

 

References:

Conway, T. M., & John, S. G. (2014). The biogeochemical cycling of zinc and zinc isotopes in the North Atlantic Ocean. Global Biogeochemical Cycles, 28, 1111-1128 doi: 10.1002/2014GB004862. Click here to view the paper.

Little, S.H., Vance, D., Walker-Brown, C., Landing, W.M., 2014. The oceanic mass balance of copper and zinc isotopes, investigated by analysis of their inputs, and outputs to ferromanganese oxide sediments. Geochimica et Cosmochimica Acta 125, 673–693. doi:10.1016/j.gca.2013.07.046. Click here to view the paper.

Janssen, D.J., Conway, T.M., John, S.G., Christian, J., Kramer, D.I., Pederson, T.F., Cullen, J.T., 2014. An undocumented water column sink for cadmium in open ocean oxygen deficient zones. Proceedings of the National Academy of Sciences USA 111, 6888–6893. doi: 10.1073/pnas.1402388111. Click here to access the paper.

Latest highlights

Science Highlights

Volcanic emissions in the Southern Ocean: an efficient and unexpected source of iron for this remote area

This study suggests that volcanic emission can represent a significant source of bioavailable Fe to open ocean anaemic ecosystems.

20.09.2021

Science Highlights

Surprisingly heavy silicon isotopes in the surface and deep Arctic Ocean

Brzezinski and his colleagues report on a comprehensive study of the Arctic Ocean silicic acid concentrations and silicon isotopic composition…

14.09.2021

Science Highlights

Unique winter dataset of particulate and dissolved cadmium in the Indian sector of the Southern Ocean

Cloete and collaborators analysed particulate and dissolved cadmium at 7 stations in austral winter along a North South section off South Africa.

06.09.2021

Science Highlights

A new proxy for ocean iron bioavailability

The approach established and verified in this study, opens a new way for determining dissolved iron bioavailability in samples across the ocean.

23.07.2021

Rechercher