Impact of atmospheric deposition on the contrasting iron biogeochemistry of the North and South Atlantic Ocean
Open accessAbstract
Dissolved iron (dFe) distributions and atmospheric and vertical subduction fluxes of dFe were determined in the upper water column for two meridional transects of the Atlantic Ocean. The data demonstrate the disparity between the iron biogeochemistry of the North and South Atlantic Ocean and show well‐defined gradients of size fractionated iron species in surface waters between geographic provinces. The highest dFe and lowest mixed layer residence times (0.4–2.5 years) were found in the northern tropical and subtropical regions. In contrast, the South Atlantic Gyre had lower dFe concentrations (<0.4 n M) and much longer residence times (>5 years), presumably due to lower atmospheric inputs and more efficient biological recycling of iron in this region. Vertical input fluxes of dFe to surface waters ranged from 20 to 170 nmol m–2 d–1 in the North Atlantic and tropical provinces, whereas average fluxes of 6–13 nmol m–2 d–1 were estimated for the South Atlantic. Our estimates showed that the variable dFe distribution over the surface Atlantic (<0.1–2.0 n M) predominantly reflected atmospheric Fe deposition fluxes (>50% of total vertical Fe flux to surface waters) rather than upwelling or vertical mixing. This demonstrates the strength of the connection between land‐derived atmospheric Fe fluxes and the biological cycling of carbon and nitrogen in the Atlantic Ocean.
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
North Atlantic waters underlying the SAL dust plume are richer in Fe, Si, Al, Ti, Mn, P and other trace metals bio-essential for phytoplankton, in comparison with South Atlantic waters.
“Due to massive dust deposition, North Atlantic waters underlying the SAL dust plume are richer in Fe, Si, Al, Ti, Mn, P and other trace metals bio-essential for phytoplankton, in comparison with South Atlantic waters (Han et al., 2008;Ussher et al., 2013;Conway and John, 2014;Baker and Jickells, 2017).”
From African desert dust influences migrations and fisheries of the Atlantic skipjack-tuna (2023) · cites this paper as Ussher et al., 2013
Section 3.1, paragraph [14] reports higher surface-water Fe and Al in the tropical North Atlantic under the Saharan dust plume than in the central South Atlantic. The paper does not establish the claimed North–South enrichment of seawater Si, Ti, Mn, or P; the Introduction, paragraph [2], instead describes Atlantic P supply as predominantly in situ or by physical transport. Page numbers are unavailable in our copy. (LLM, conf=0.88)
Experimental — accuracy not yet measured
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Cites
No references could be resolved yet.
Research works printed but not linked: 55
- Anderson, L. A. (1995), On the hydrogen and oxygen content of marine phytoplankton, Deep Sea Res., Part I, 42(9), 1675-1680.
- Baker, A. R., T. D. Jickells, M. Witt, and K. L. Linge (2006a), Trends in the solubility of iron, aluminium, manganese and phosphorus in aerosol collected over the Atlantic Ocean, Mar. Chem., 98(1), 43-58.
- Baker, A. R., T. D. Jickells, K. F. Biswas, K. Weston, and M. French (2006b), Nutrients in atmospheric aerosol particles along the Atlantic Meridional Transect, Deep Sea Res., Part II, 53(14-16), 1706-1719, doi:10.1016/j.dsr2.2006.05.012. · DOI
- Baker, A. R., K. Weston, S. D. Kelly, M. Voss, P. Streu, and J. N. Cape (2007), Dry and wet deposition of nutrients from the tropical Atlantic atmosphere: Links to primary productivity and nitrogen fixation, Deep Sea Res. Oceanogr. Res., Part I, 54(10), 1704-1720.
- Baker, A. R., T. Lesworth, C. Adams, T. D. Jickells, and L. Ganzeveld (2010), Estimation of atmospheric nutrient inputs to the Atlantic Ocean from 50°N to 50°S based on large-scale field sampling: Fixed nitrogen and dry deposition of phosphorus, Global Biogeochem. Cycles, 24, GB3006, doi:10.1029/2009GB003634. · DOI
- Baker, A. R., C. Adams, T. G. Bell, T. D. Jickells, and L. Ganzeveld (2013), Estimation of atmospheric nutrient inputs to the Atlantic Ocean from 50°N to 50°S based on large-scale field sampling: Iron and other dust-associated elements, Global Biogeochem. Cycles, 27, 755-767, doi:10.1002/ gbc.20062. · DOI
- Bergquist, B. A., and E. A. Boyle (2006), Dissolved iron in the tropical and subtropical Atlantic Ocean, Global Biogeochem. Cycles, 20, GB1015, doi:10.1029/2005GB002505. · DOI
- Bergquist, B. A., J. Wu, and E. A. Boyle (2007), Variability in oceanic dissolved iron is dominated by the colloidal fraction, Geochim. Cosmochim. Acta, 71(12), 2960-2974.
- Blain, S., U. Guieu, H. Claustre, K. Leblanc, T. Moutin, B. Queguiner, J. Ras, and G. Sarthou (2004), Availability of iron and major nutrients for phyto- plankton in the northeast Atlantic Ocean, Limnol. Oceanogr., 49(6), 2095-2104.
- Bowie, A. R., E. P. Achterberg, R. F. C. Mantoura, and P. J. Worsfold (1998), Determination of sub-nanomolar levels of iron in seawater using flow injection with chemiluminescence detection, Anal. Chim. Acta, 361(3), 189-200.
- Bowie, A. R., D. J. Whitworth, E. P. Achterberg, R. F. C. Mantoura, and P. J. Worsfold (2002), Biogeochemistry of Fe and other trace elements (Al, Co, Ni) in the upper Atlantic Ocean, Deep Sea Res., Part I, 49(4), 605-636.
- Bowie, A. R., E. P. Achterberg, P. L. Croot, H. J. W. de Baar, P. Laan, J. W. Moffett, S. Ussher, and P. J. Worsfold (2006), A community-wide intercomparison exercise for the determination of dissolved iron in seawa- ter, Mar. Chem., 98(1), 81-99.
- Bowie, A. R., S. J. Ussher, W. M. Landing, and P. J. Worsfold (2007), Intercomparison between FI-CL and ICP-MS for the determination of dissolved iron in Atlantic seawater, Environ. Chem., 4(1), 1-4.
- Boyd, P. W., E. Ibisanmi, S. G. Sander, K. A. Hunter, and G. A. Jackson (2010), Remineralization of upper ocean particles: Implications for iron biogeochemistry, Limnol. Oceanogr., 55(3), 1271-1288.
- Buck, C. S., W. M. Landing, J. A. Resing, and C. I. Measures (2010a), The solubility and deposition of aerosol Fe and other trace elements in the North Atlantic Ocean: Observations from the A16N CLIVAR/CO2 repeat hydrography section, Mar. Chem., 120(1-4), 57-70.
- Buck, C. S., W. M. Landing, and J. A. Resing (2010b), Particle size and aero- sol iron solubility: A high-resolution analysis of Atlantic aerosols, Mar. Chem., 120(1-4), 14-24.
- Charette, M. A., and S. B. Moran (1999), Rates of particle scavenging and particulate organic carbon export estimated using 234Th as a tracer in the subtropical and equatorial Atlantic Ocean, Deep Sea Res., Part II, 46(5), 885-906.
- Doi, T., T. Tozuka, and T. Yamagata (2010), The Atlantic Meridional Mode and its coupled variability with the Guinea Dome, J. Clim., 23(2), 455-475.
- Duce, R. A., and N. W. Tindale (1991), Atmospheric transport of iron and its deposition in the ocean, Limnol. Oceanogr., 36(8), 1715-1726.
- Elrod, V. A., W. M. Berelson, K. H. Coale, and K. S. Johnson (2004), The flux of iron from continental shelf sediments: A missing source for global budgets, Geophys. Res. Lett., 31, L12307, doi:10.1029/ 2004GL020216. · DOI
- Helmers, E., and O. Schrems (1995), Wet deposition of metals to the tropical North and the South Atlantic Ocean, Atmos. Environ., 29(18), 2475-2484.
- Hsieh, Y.-T., G. M. Henderson, and A. L. Thomas (2011), Combining seawater 232Th and 230Th concentrations to determine dust fluxes to the surface ocean, Earth Planet. Sci. Lett., 312(3-4), 280-290.
- Hydes, D. J., and P. S. Liss (1976), Fluorimetric method for determination of low concentrations of dissolved aluminum in natural-waters, Analyst, 101(1209), 922-931.
- Jickells, T. D. (1999), The inputs of dust derived elements to the Sargasso Sea; a synthesis, Mar. Chem., 68(1-2), 5-14.
- Johnson, K. S., et al. (2007), Developing standards for dissolved iron in seawater, Eos. Trans. AGU, 88(11), 131.
- Johnson, M. S., N. Meskhidze, F. Solmon, S. Gassó, P. Y. Chuang, D. M. Gaiero, R. M. Yantosca, S. Wu, Y. Wang, and C. Carouge (2010), Modeling dust and soluble iron deposition to the South Atlantic Ocean, J. Geophys. Res., 115, D15202, doi:10.1029/2009JD013311. · DOI
- Kaufman, Y. J., I. Koren, L. A. Remer, D. Tanre, P. Ginoux, and S. Fan (2005), Dust transport and deposition observed from the Terra-Moderate Resolution Imaging Spectroradiometer (MODIS) spacecraft over the Atlantic Ocean, J. Geophys. Res., 110, D10S12, doi:10.1029/ 2003JD004436. · DOI
- Kistler, R., et al. (2001), The NCEP-NCAR 50 year reanalysis: Monthly means CD-ROM and documentation, Bull. Am. Meteorol. Soc., 82(2), 247-267.
- Kramer, J., P. Laan, G. Sarthou, K. R. Timmermans, and H. J. W. de Baar (2004), Distribution of dissolved aluminium in the high atmospheric input region of the subtropical waters of the North Atlantic Ocean, Mar. Chem., 88(3-4), 85-101.
- Mahaffey, C., R. G. Williams, G. A. Wolff, and W. T. Anderson (2004), Physical supply of nitrogen to phytoplankton in the Atlantic Ocean, Global Biogeochem. Cycles, 18, GB1034, doi:10.1029/ 2003GB002129. · DOI
- Marshall, J. C., A. J. G. Nurser, and R. G. Williams (1993), Inferring the sub- duction rate and period over the North Atlantic, J. Phys. Oceanogr., 23(7), 1315-1329.
- Martin, J. H., S. E. Fitzwater, R. M. Gordon, C. N. Hunter, and S. J. Tanner (1993), Iron, primary production and carbon-nitrogen flux studies during the JGOFS North Atlantic Bloom Experiment, Deep Sea Res., Part II, 40(1-2), 115-134.
- Measures, C. I., W. M. Landing, M. T. Brown, and C. S. Buck (2008), High- resolution Al and Fe data from the Atlantic Ocean CLIVAR-CO(2) repeat hydrography A16N transect: Extensive linkages between atmospheric dust and upper ocean geochemistry, Global Biogeochem. Cycles, 22, GB1005, doi:10.1029/2007GB003042. · DOI
- Mills, M. M., C. Ridame, M. Davey, J. La Roche, and R. J. Geider (2004), Iron and phosphorus co-limit nitrogen fixation in the eastern tropical North Atlantic, Nature, 429(6989), 292-294.
- Moore, J. K., S. C. Doney, D. M. Glover, and I. Y. Fung (2002), Iron cycling and nutrient-limitation patterns in surface waters of the World Ocean, Deep Sea Res., Part II, 49(1-3), 463-507.
- Moore, C. M., M. M. Mills, A. Milne, R. Langlois, E. P. Achterberg, K. Lochte, R. J. Geider, and J. La Roche (2006), Iron limits primary productivity during spring bloom development in the central North Atlantic, Global Change Biol., 12(4), 626-634.
- Moore, C. M., et al. (2009), Large-scale distribution of Atlantic nitrogen fixation controlled by iron availability, Nat. Geosci., 2(12), 867-871.
- Moran, S. B., and R. M. Moore (1988), Evidence from mesocosm studies for biological removal of dissolved aluminium from sea water, Nature, 335(6192), 706-708.
- Orians, K. J., and K. W. Bruland (1986), The biogeochemistry of aluminum in the Pacific Ocean, Earth Planet. Sci. Lett., 78(4), 397-410.
- Parekh, P., M. J. Follows, and E. Boyle (2004), Modeling the global ocean iron cycle, Global Biogeochem. Cycles, 18, GB1002, doi:10.1029/ 2003GB002061. · DOI
- Powell, C. (2010), Atmospheric inputs of iron and other key nutrients to the Tropical North Atlantic, PhD Thesis, Univ. of East Anglia, Norwich, Norfolk, U. K.
- Rijkenberg, M., S. Steigenberger, C. Powell, H. van Haren, M. D. Patey, A. R. Baker, and E. P. Achterberg (2012), Fluxes and distribution of dissolved iron in the eastern (sub-) tropical North Atlantic Ocean, Global Biogeochem. Cycles, 26, GB3004, doi:10.1029/2011GB004264. · DOI
- Sarthou, G., et al. (2003), Atmospheric iron deposition and sea-surface dissolved iron concentrations in the eastern Atlantic Ocean, Deep Sea Res., Part I, 50(10-11), 1339-1352.
- Schlosser, C., and P. L. Croot (2009), Controls on seawater Fe(III) solubility in the Mauritanian upwelling zone, Geophys. Res. Lett., 36, L18606, doi:10.1029/2009GL038963. · DOI
- Sedwick, P. N., E. R. Sholkovitz, and T. M. Church (2007), Impact of an- thropogenic combustion emissions on the fractional solubility of aerosol iron: Evidence from the Sargasso Sea, Geochem. Geophys. Geosyst., 8, Q10Q06, doi:10.1029/2007GC001586. · DOI
- Shelley, R. U., et al. (2012), Controls on dissolved cobalt in surface waters of the Sargasso Sea: Comparisons with iron and aluminum, Global Biogeochem. Cycles, 26, GB2020, doi:10.1029/2011GB004155. · DOI
- Stramma, L., G. C. Johnson, J. Sprintall, and V. Mohrholz (2008), Expanding oxygen-minimum zones in the tropical oceans, Science, 320(5876), 655-658.
- Sunda, W. G. (1997), Control of dissolved iron concentrations in the world ocean, a comment, Mar. Chem., 57(3-4), 169-172.
- Tagliabue, A., et al. (2010), Hydrothermal contribution to the oceanic dissolved iron inventory, Nat. Geosci., 3(4), 252-256.
- Tian, Z., P. Olliver, A. Véron, and T. M. Church (2008), Atmospheric Fe deposition modes at Bermuda and the adjacent Sargasso Sea, Geochem. Geophys. Geosyst., 9, Q08007, doi:10.1029/2007GC001868. · DOI
- Ussher, S. J., P. J. Worsfold, E. P. Achterberg, A. Laës, S. Blain, P. Laan, and H. J. W. de Baar (2007), Distribution and redox speciation of dissolved iron on the European continental margin, Limnol. Oceanogr., 52(6), 2530-2539.
- Ussher, S. J., I. Petrov, C. R. Quétel, and P. J. Worsfold (2010), Validation of a portable flow injection-chemiluminescence (FI-CL) method for the determination of dissolved iron in Atlantic open ocean and shelf waters by comparison with isotope dilution-inductively coupled plasma mass spectrometry (ID-ICPMS), Environ. Chem., 7(2), 139-145.
- Vink, S., and C. I. Measures (2001), The role of dust deposition in determin- ing surface water distributions of Al and Fe in the South West Atlantic, Deep Sea Res., Part II, 48(13), 2787-2809.
- Wilcox, E. M., K. M. Lau, and K. M. Kim (2010), A northward shift of the North Atlantic Ocean Intertropical Convergence Zone in response to summertime Saharan dust outbreaks, Geophys. Res. Lett., 37, L04804, doi:10.1029/2009GL041774. · DOI
- Xie, S.-P., and J. A. Carton (2004), Tropical Atlantic variability: Patterns, mech- anisms, and impacts, in Earth's Climate: The Ocean-Atmosphere Interaction, Geophys. Monogr. Ser., vol. 147, pp. 121-142, AGU, Washington, D. C.
Cited by
Sorted by citations
African desert dust influences migrations and fisheries of the Atlantic skipjack-tuna
Rodríguez, S., Riera, R., Fonteneau, A., Alonso-Pérez, S., & López-Darias, J. (2023) · Atmospheric Environment · doi:10.1016/j.atmosenv.2023.120022 · Cited by 23 · see citing works
“…massive dust deposition, North Atlantic waters underlying the SAL dust plume are richer in Fe, Si, Al, Ti, Mn, P and other trace metals bio-essential for phytoplankton, in comparison with South Atlantic waters (Han et al., 2008; Ussher et al., 2013; Conway and John, 2014; Baker and Jickells, 2017).”
- Authors
- Ussher, S. J., Achterberg, E. P., Powell, C., Baker, A. R., Jickells, T. D., Torres, R., & Worsfold, P. J.
- Affiliations
- Bermuda Institute of Ocean Sciences (BM)
- National Oceanography Centre (GB)
- University of East Anglia (GB)
- Plymouth Marine Laboratory (GB)
- University of Plymouth (GB)
- Corresponding author
- Ussher, Simon J.
- ORCID
- Venue
- Global Biogeochemical Cycles
- Publisher
- American Geophysical Union (AGU)
- Published
- 2013-11-13
- Volume
- 27
- Issue
- 4
- Pages
- 1096-1107
- ISSN
- 0886-6236 (ISSN-L)
- 1944-9224
- OpenAlex
- W1930487100
- Cited by
- 53
- References
- 0
- Citations by year
- 2026: 1 · 2025: 4 · 2024: 1 · 2023: 5 · 2022: 2 · 2021: 1 · 2020: 2 · 2019: 3 · 2018: 4 · 2017: 8 · 2016: 5 · 2015: 9 · 2014: 8
- FWCI
- 5.20
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Global Biogeochemical Cycles (publishedVersion)
- Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
- UEA Digital Repository (University of East Anglia) (acceptedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- Marine Biological Association (submittedVersion)
- Funders
- NERC (NER/A/S/2003/00489)
- AMT Consortium (NER/O/S2001/00680, NE/c001737/1)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric chemistry and aerosols
- Keywords
- dissolved iron, atmospheric iron deposition, iron biogeochemistry, North Atlantic, South Atlantic, iron recycling, meridional transect, South Atlantic gyre
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review