Retreat of large marine-terminating glaciers may increase iron supply to surface waters

The availability of the micronutrient iron (Fe) limits primary production in large parts of the high latitude oceans. There, glacial discharge enriched in dissolved Fe may stimulate phytoplankton growth and carbon sequestration. Previous research conducted in pro-glacial environments with samples collected on land suggested that glacial dissolved Fe supply to shelf waters may scale with freshwater discharge volume. Yet, data to support this conclusion is lacking for marine-terminating glaciers where glacial freshwater is injected subsurface into subglacial cavity waters residing beneath floating ice-tongues. GEOTRACES expedition GN05 on RV Polarstern sampled immediately adjacent to Greenland’s largest floating ice-tongue. Results reveal that subglacial dissolved Fe discharge from glacier Nioghalvfjerdsbrae at 79°N is decoupled from freshwater Fe inputs, but has important benthic dissolved Fe sources. Krisch et al (2021, see reference below) show that the long residence time of waters inside the subglacial cavity results in equilibration between dissolved Fe, and sedimentary and freshwater Fe sources. As a consequence, dissolved Fe fluxes to the shelf are currently unaffected by increasing freshwater discharge, and may instead scale with the seawater circulation beneath the large floating ice-tongue. The findings demonstrate that glacial retreat and loss of ice-shelves may potentially result in increases in dissolved Fe supply to surface waters downstream of large marine terminating glaciers in future.

Figure: Iron cycling in subglacial cavity underneath the 79oN floating ice tongue. Sediment supply, particle-dissolved Fe exchange and Fe ligand binding in combination with a prolonged water residence in the cavity (~162 days) resulted in enhanced dissolved Fe concentrations in the waters exiting the cavity.


Krisch, S., Hopwood, M. J., Schaffer, J., Al-Hashem, A., Höfer, J., Rutgers van der Loeff, M. M., Conway, T. M., Summers, B. A., Lodeiro, P., Ardiningsih, I., Steffens, T., Achterberg, E. P. (2021). The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf. Nature Communications, 12(1), 3030. Access the paper:

Latest highlights

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…


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.


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.


Science Highlights

Scavenging differentiates the distribution of cadmium, nickel, zinc and copper in the North Pacific Ocean

Zheng and co-authors observed sectional distributions of cadmium, nickel, zinc, and copper in the North Pacific Ocean during three GEOTRACES related cruises…