Mercury stable isotopes constrain atmospheric pathways to the ocean


Mercury is one of the least concentrated trace elements in the ocean. Yet, the small seawater Hg levels biomagnify million times along the marine food chain, to reach harmful levels in predatory fish and their human consumers. Natural and anthropogenic Hg sources to the ocean remain ill-constrained. It took 10 years of development to come up with a method to measure Hg stable isotopes of seawater at subpicomolar levels. The Hg isotopic signatures in the ocean suggest the gas uptake (Hg0) and ionic deposition (HgII) are equally important (1:1), which is contrary than our current understanding (1:3)[1].  HgII deposition is likely overestimated by 2 to 3-fold, and the ocean receives less Hg overall. The study’s results hold promise that the implementation of anti-pollution measures under the Minamata Convention[2] will likely result in a faster decrease of oceanic Hg levels than previously thought.  

Figure: Summary of marine HgII deposition and Hg0 air-sea exchange fluxes. Gross fluxes (solid arrows, Mg y-1) are based on published model estimates. Hg0exchange is bidirectional. Marine Δ200Hg signatures of 0.04‰ indicate a relatively more important contribution of the atmospheric Hg0 end-member to marine Hg than current 3D models suggest. This indicates that either 3D model HgII deposition is likely overestimated (black dotted arrows, indicating 2–3 times lower, required to fit Δ200Hg data).

Reference:

Jiskra, M., Heimbürger-Boavida, L., Desgranges, M., Petrova, M., Dufour, A., Ferreira-Araujo, B., Masbou, J., Chmeleff, J., Thyssen, M., Point, D., Sonke, J. E. Mercury stable isotopes constrain atmospheric sources to the ocean. Nature, https://doi.org/10.1038/s41586-021-03859-8


[1] https://www.unep.org/resources/publication/global-mercury-assessment-2018

[2] https://www.mercuryconvention.org/en

Latest highlights

Dissolved nickel sources: transformation and sinks in the Arabian Sea

Malla and co-authors present an extensive study of the distribution of dissolved nickel in the Arabian Sea.

Linking cadmium cycling to phosphate dynamics in the Indian Ocean: Evidence from GEOTRACES transects

Mishra and Singh determined cadmium and phosphate concentrations along 34 complete vertical profiles in the Indian Ocean.

New software enables global ocean biogeochemical modeling in Python

The newly designed tmm4py software makes biogeochemical modelling more widely accessible.

Aerosol dissolution and iron isotope fractionation during atmospheric transport

Camin and co-authors present the iron concentrations and isotopic compositions of aerosols in previously undocumented areas of the Pacific Ocean.

Rechercher