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

Bucciarelli, Penven et al. (2025, see reference below) combined float trajectories with high-resolution model diagnostics, thus could establish that a significant iron fertilisation was explaining the huge phytoplankton bloom recurrently observed in the western Indian Subantarctic Zone. They show that the energetic Agulhas current is leaching sedimented iron over the African margin, crossing the Subtropical Front via the region’s intense mesoscale eddy variability with the Agulhas Return Current (ARC), eventually transporting iron through the Sub Tropical Front (STF) and extending into the Sub Antarctic Zone (SAZ). So far, it was established that aeolian inputs to this area support only about half of the biological iron demand in the SAZ. The results of Bucciarelli, Penven et al. contribute to balance the dissolved iron budget for this region, which productivity represents 20–40% of Southern Ocean carbon export to the deep ocean. Beyond the present fertilisation, the authors also hypothesised that the past ARC variability could have influenced past productivity across much of the western Indian SAZ, providing a convincing reconstruction over the past 350 ka.

Figure: Satellite chlorophyll-a for the 25/12/2017 mapped on ocean surface topography shows the Agulhas Front (AF), Subtropical Front (STF) and Subantarctic Front (SAF). Purple lines trace floats passing near the East African margin (black triangles), about half of which cross the STF. These waters carry Fe from the African margin into the SAZ, supplying half of the phytoplankton’s iron needs. The inset indicates that past changes in the strength of the Agulhas Return Current over the last 350 kyr (a) may have influenced productivity in the western Indian SAZ (c-e), alongside variations in dust inputs (b).

Reference:

Bucciarelli, E., Penven, P., Pous, S., & Tagliabue, A. (2025). Western Indian subantarctic phytoplankton blooms fertilized by iron-enriched Agulhas water. Nature Geoscience, 18, 1152–1158. Access the paper:10.1038/s41561-025-01823-z

Read also the “Behind the paper” post: https://communities.springernature.com/posts/the-southern-agulhas-leakage-a-source-of-iron-for-the-southern-ocean?channel_id=behind-the-paper

Latest highlights

Sedimentary controls on seawater nickel distributions and nickel isotope compositions: a two steps study

Nickel isotopic mass balance in the ocean stands among the less understood so far…

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…

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