Long distance dissolved iron transport in the North-East Pacific revealed by multiple tracers and an ocean circulation model

Science Highlights

15 October 2024

GEOTRACES strategy is to combine the information provided by different geochemical tracers to identify and quantify oceanic processes. Sieber and co-authors (2024, see reference below) have made extensive use of this multi-tracer approach, coupled to an oceanic circulation model. By measuring sediment‐source tracers including dissolved iron isotope composition (δ56Fe), manganese (Mn), radium-228 (228Ra), and particulate iron (Fe), they revealed the dissolved Fe provenance of three dissolved iron plumes identified close to the Alaskan continental margin: surprisingly, while two originate from local shelf and abyss sedimentary sources, the intermediate depth dissolved Fe plume results not from the local margin but instead from long‐distance transport of dissolved iron from Asian marginal sediment sources. This finding extends work that already has shown the large eastward transport of Fe from Asian marginal seas into the North Pacific.

Figure 1. Cruise track and stations of the 2018 US GEOTRACES GP15 Meridional Transect off Alaska, as well as major surface currents in the region. AS = Alaskan Stream, ACC = Alaskan Coastal Current, NPC = North Pacific Current.
Figure 2. Iron concentrations at ~1300 m depth across the North Pacific Ocean, compiled from various cruises, and arrows showing the direction of flow and how Fe from Asian marginal seas is transported to Alaska. GPc06 and GP15 show the location of Japanese and US GEOTRACES cruises.

Reference:

Sieber, M., Lanning, N. T., Steffen, J. M., Bian, X., Yang, S.-C., Lee, J. M., Weiss, G., Hunt, H. R., Charette, M. A., Moore, W. S., Hautala, S. L., Hatta, M., Lam, P. J., John, S. G., Fitzsimmons, J. N., & Conway, T. M. (2024). Long Distance Transport of Subsurface Sediment‐Derived Iron From Asian to Alaskan Margins in the North Pacific Ocean. Geophysical Research Letters, 51. Access the paper: 10.1029/2024gl110836

Latest highlights

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…

To Ba or not to Ba: Evaluating water column excess particulate barium as a proxy for water column respiration

Rahman and co-workers examine the relationship between excess particulate barium and organic matter respiration in the water column…

Assessment of the Solomon Sea’s dissolved iron contribution to the Equatorial Under Current

Sarthou and co-workers analysed 11 vertical profiles of dissolved iron at the entrance, within, and at the exit of the Solomon Sea…

Major controls on the fate of dissolved manganese in the northeastern Indian Ocean

Malla and Singh investigated the key factors controlling dissolved manganese in the northeastern Indian Ocean.

Rechercher