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

Mercury content and isotopes in bird’s guano: a window to reconstruct past climates

By analysing peat cores, Chuxian Li and her colleagues have shown how populations of nesting seabirds have fluctuated on a sub-Antarctic Island over the last 8,000 years.

Contraction of North Atlantic Deep Water during glacial times: a paradigm called into question

Blaser and co-authors propose a new distribution of deep-water masses in the Atlantic Ocean during the Last Glacial Maximum and the Heinrich Stadial..

Authigenic radiogenic neodymium isotope composition traces millennial-scale overturning circulation variability in the Arabian Sea

The neodymium isotopic signature of the sediment authigenic fraction is, a priori, a valuable proxy for reconstructing deep-water mass trajectories…

Magmatic activity at the Carlsberg Ridge in the Indian Ocean triggered by glacial sea-level variation

De and colleagues provide a high-resolution record of magmatic input and associated hydrothermal activity over the past 49 kyr from a core recovered from a magmatic segment of the slow-spreading Carlsberg Ridge in the Indian Ocean.

Rechercher