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Quantification of dissolved iron sources to the North Atlantic Ocean

Nature volume 511, pages 212215 (10 July 2014) | Download Citation



Dissolved iron is an essential micronutrient for marine phytoplankton, and its availability controls patterns of primary productivity and carbon cycling throughout the oceans1,2. The relative importance of different sources of iron to the oceans is not well known, however, and flux estimates from atmospheric dust, hydrothermal vents and oceanic sediments vary by orders of magnitude. Here we present a high-resolution transect of dissolved stable iron isotope ratios (δ56Fe) and iron concentrations ([Fe]) along a section of the North Atlantic Ocean. The different iron sources can be identified by their unique δ56Fe signatures, which persist throughout the water column. This allows us to calculate the relative contribution from dust, hydrothermal venting and reductive and non-reductive sedimentary release to the dissolved phase. We find that Saharan dust aerosol is the dominant source of dissolved iron along the section, contributing 71–87 per cent of dissolved iron. Additional sources of iron are non-reductive release from oxygenated sediments on the North American margin (10–19 per cent), reductive sedimentary dissolution on the African margin (1–4 per cent) and hydrothermal venting at the Mid-Atlantic Ridge (2–6 per cent). Our data also indicate that hydrothermal vents in the North Atlantic are a source of isotopically light iron, which travels thousands of kilometres from vent sites, potentially influencing surface productivity. Changes in the relative importance of the different iron sources through time may affect interactions between the carbon cycle and climate.

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We thank the Captain, crew and GEOTRACES sampling team on RV Knorr on both USGT10 and USGT11; A. Rosenberg for technical assistance; J. Wu, R. Middag, K. Bruland and P. Sedwick for supplying concentration data that informed double-spike calculations; and C. Hayes for calibrating transmissometry data. We thank W. Jenkins, W. Smethie, E. Boyle and G. Cutter for water mass observations. The Ocean Data Facility supplied temperature, PSS-78 salinity, fluorescence, transmissometry, dissolved oxygen and nutrient data from both cruises. Figures were created with Matlab and Adobe Illustrator. This study was funded by National Science Foundation grant OCE-1131387.

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    • Tim M. Conway

    Present address: Institute of Geochemistry and Petrology, Eidgenössische Technische Hochschule Zürich, NW D81.4, Clausiusstrasse 25, 8092 Zürich, Switzerland.


  1. Department of Earth and Ocean Sciences, University of South Carolina, Columbia, South Carolina 29208, USA

    • Tim M. Conway
    •  & Seth G. John


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The paper was written by T.M.C. and S.G.J. Samples were processed and analysed by T.M.C.

Competing interests

The authors declare no competing financial interests.

Corresponding author

Correspondence to Tim M. Conway.

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  1. 1.

    Supplementary Data

    This file contains dataset of 0.2 μm filtered dissolved iron concentration and dissolved iron stable isotope ratios (δ56Fe) for the North Atlantic Zonal Transect (legs USGT10 and USGT11). Values were averaged from two ICPMS analyses. All δ56Fe are expressed relative to isotope standard IRMM-014. See Methods for more details.

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