Elevated methylmercury level in Arctic rain and aerosol linked to oceanic dimethylmercury emissions

He and colleagues (2025, see reference below) conducted a research cruise from coastal Alaska through the Bering and Chukchi Seas in May-June 2021, and made high-resolution measurements of dimethylmercury (DMHg) in surface seawater. Their study revealed that DMHg released from the ocean surface is converted in the atmosphere into methylmercury (MeHg), the most toxic and bioaccumulative form of mercury. The study showed that MeHg can be transported over long distances in the atmosphere before returning to the surface ocean via precipitation and aerosol deposition, potentially contaminating fish and marine mammals in ecosystems far from the original DMHg source. The team observed a 5-fold increase in the MeHg-to-total Hg fraction in rain and a 10-fold increase in aerosols, both closely linked to atmospheric inputs from the elevated surface DMHg concentrations. By quantifying the various fluxes involved, the study highlights a previously underappreciated pathway of Hg transport, underscoring its significance to human health and ecological risk in the rapidly changing Arctic environment.

Figure: This diagram shows how a toxic form of Hg builds up in Arctic rain and aerosols. In coastal Alaska, seawater releases DMHg into the air, where it transforms into MeHg. That MeHg then travels through the atmosphere and returns to the ocean with rain and aerosols, reaching areas like the Chukchi Sea over 1,700 km away from the DMHg source. The chart also shows that this ocean-to-air-to-land/ice/ocean pathway adds a significant amount of toxic Hg to remote Arctic ecosystems.

Reference:

He, Y., Inman, H., Kadko, D. C., Stephens, M. P., Hammond, D. E., Landing, W. M., & Mason, R. P. (2025). Elevated methylmercury in Arctic rain and aerosol linked to air-sea exchange of dimethylmercury. Science Advances11. Access the paper:10.1126/sciadv.adr3805

Latest highlights

23 million years of productivity reconstructed in the Central Pacific Ocean using past and modern proxies

Using diverse geochemical proxies, Chu and colleagues analysed an iron–manganese crust to reconstruct central Pacific productivity over the past 23 million years.

Lead isotopes reveal that hydrothermal variability is driven by Sea‐Level change and transient magmatism

De and colleagues present the first millennial-scale reconstruction of hydrothermal variability at a mid-ocean ridge using lead isotopes from iron-manganese coatings…

Long-range transport of iron via the Agulhas Current and counter-current: a boon for the phytoplankton

Authors establish that significant iron fertilisation via the Agulhas current explains the Indian Subantarctic blooms…

Hydrothermal activity detected above the ultra-slow South West Indian Ridge, using a multi-proxy approach

Baudet and colleagues demonstrate the occurrence of hydrothermal venting on the Southwest Indian Ridge…

Rechercher