Modeling the speciation and biogeochemistry of iron at the Bermuda Atlantic Time-series Study site

Global Biogeochemical Cycles

Volumn 19, Issue 1, 2005, Pages 1-23

  Weber, L ^a,b   Volker C ^c   Schartau, M ^c,d   Wolf Gladrow, D A ^c  

^a GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^b NATIONAL OCEANOGRAPHY CENTRE   (United Kingdom)

^c ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^d STONY BROOK UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

BIOGEOCHEMISTRY; IRON; PHYTOPLANKTON; SPECIATION (CHEMISTRY); TIME SERIES ANALYSIS;

ATLANTIC ISLANDS; ATLANTIC OCEAN; BERMUDA; OCEANIC REGIONS; WORLD;

ALGAE;

EID: 20444366233     PISSN: 08866236     EISSN: None     Source Type: Journal    
DOI: 10.1029/2004GB002340     Document Type: Review

References (112)

1. Anderson, M., and F. Morel (1982), The influence of aqueous iron chemistry on the uptake of iron by the coastal diatom Thalassiosira weissflogii, Limnol. Oceanogr., 27, 789-831.
2. Archer, D., and K. Johnson (1999), A model of the iron cycle in the ocean, Global Biogeochem. Cycles, 13, 269-279.
3. Arimoto, R. (2001), Eolian dust and climate: Relationships to sources, tropospheric chemistry, transport, and deposition, Earth Sci. Rev., 54, 29-42.
4. Armstrong, R. (1999), An optimization-based model of iron-light-ammonium colimitation of nitrate uptake and phytoplankton growth, Limnol. Oceanogr., 44, 1436-1446.
5. Aumont, O., E. Maier-Reimer, S. Blain, and P. Monfray (2003), An ecosystem model of the global ocean including Fe, Si, P colimitations, Global Biogeochem. Cycles, 17(2), 1060, doi:10.1029/2001GB001745.
6. Balistieri, L., P. Brewer, and J. Murray (1981), Scavenging residence times of trace metals and surface chemistry of sinking particles in the deep ocean, Deep Sea Res., Part A, 28, 101-121.
7. Barbeau, K., and J. Moffett (2000), Laboratory and field studies of colloidal iron oxide dissolution as mediated by phagotrophy and photolysis, Limnol. Oceanogr., 45, 827-835.
8. Barbeau, K., J. Moffett, D. Caron, P. Croot, and D. Erdner (1996), Role of protozoan grazing in relieving iron limitation of phytoplankton, Nature, 380, 61-64.
9. Barbeau, K., E. Rue, K. Bruland, and A. Butler (2001), Photochemical cycling of iron in the surface ocean mediated by microbial iron (III)-binding ligands, Nature, 413, 409-413.
10. Barbeau, K., E. Rue, C. Trick, K. Bruland, and A. Butler (2003), Photochemical reactivity of siderophores produced by marine heterotrophic bacteria and cyanobacteria based on characteristic Fe(III) binding groups, Limnol. Oceanogr., 48, 1069-1078.
11. Baskaran, M., P. Santschi, G. Benoit, and B. Honeyman (1992), Scavenging of thorium isotopes by colloids in seawater of the Gulf of Mexico, Geochim. Cosmochim. Acta, 56(9), 3375-3388.
12. Bissett, W. P., J. J. Walsh, D. A. Dieterle, and K. L. Carder (1999), Carbon cycling in the upper waters of the Sargasso Sea: I. Numerical simulation of differential carbon and nitrogen fluxes, Deep Sea Res., Part I, 46, 205-269.
13. Bowie, A., M. Maldonado, R. Frew, P. Croot, E. Achterberg, R. Mantoura, P. Worsfold, C. Law, and P. Boyd (2001), The fate of added iron during a mesoscale fertilisation experiment in the Southern Ocean, Deep Sea Res., Part II, 48, 2703-2743.
14. Boyd, P., and C. Law (2001), The Southern Ocean Iron Release Experiment (SOIREE) - Introduction and summary, Deep Sea Res., Part II, 48, 2425-2438.
15. Brock, T. D. (1981), Calculating solar radiation for ecological studies, Ecol. Modell., 14, 1-19.
16. Bruland, K., J. Donat, and D. Hutchins (1991), Interactive influences of bioactive trace metals on biological production in natural waters, Limnol. Oceanogr., 36, 1555-1577.
17. Byrne, R., and D. Kester (1976), Solubility of hydrous ferric oxide and iron speciation in seawater, Mar. Chem., 4, 255-274.
18. Carlson, C., H. W. Ducklow, and A. F. Michaels (1994), Annual flux of dissolved organic-carbon from the euphotic zone in the northwestern Sargasso Sea, Nature, 371, 405-408.
19. Carroll, D. (1996), Chemical laser modeling with genetic algorithms, AIAA J., 34, 338-346.
20. Chen, M., R. Dei, W.-X. Wang, and L. Guo (2003), Marine diatom uptake of iron bound with natural colloids of different orgins, Mar. Chem., 81, 177-189.
21. Christian, J., M. Verschell, R. Murtigudde, A. Busalacchi, and C. McClain (2002), Biogeochemical modelling of the tropical Pacific Ocean: II. Iron biogeochemistry, Deep Sea Res., Part II, 49, 509-543.
22. Cloern, J. (1995), An empirical model of the phytoplankton chlorophyll: Carbon ratio - The conversion factor between productivity and growth rate, Limnol. Oceanogr., 40, 1313-1321.
23. Coale, K., et al. (1996), A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean, Nature, 383, 495-501.
24. 2 in natural waters exposed to sunlight, Environ. Sci. Technol., 22, 1156-1160.
25. II in an iron-induced Southern Ocean phytoplankton bloom, Geophys. Res. Lett., 28, 3425-3428.
26. Doney, S. (1996), A synoptic atmospheric surface forcing data set and physical upper ocean model for the U.S. JGOFS Bermuda Atlantic Time-Series Study site, J. Geophys. Res., 101, 25,615-25,634.
27. Doney, S., R. Najjar, and S. Stewart (1995), Photochemistry, mixing and diurnal cycles in the upper ocean, J. Mar. Res., 53, 341-369.
28. Duce, R., and N. Tindale (1991), Atmospheric transport of iron and its deposition in the ocean, Limnol. Oceanogr., 36, 1715-1726.
29. Emmenegger, L., R. Schönberger, L. Sigg, and B. Sulzberger (2001), Light-induced redox cycling of iron in circumneutral lakes, Limnol. Oceanogr., 46, 49-61.
30. Evans, G., and J. Parslow (1985), A model of annual plankton cycles, Biol. Oceanogr., 3, 327-347.
31. Farley, K., and F. Morel (1986), Role of coagulation in the kinetics of sedimentation, Environ. Sci. Technol., 20, 187-195.
32. Fasham, M. (1993), Modelling the marine biota, in The Global Carbon Cycle, edited by M. Heimann, pp. 457-504, Springer, New York.
33. Fennel, K., M. Losch, J. Schroeter, and M. Wenzel (2001), Testing a marine ecosystem model: Sensitivity analysis and parameter optimization, J. Mar. Syst., 28, 45-63.
34. Fung, I., S. Meyn, I. Tegen, S. Doney, J. John, and J. Bishop (2000), Iron supply and demand in the upper ocean, Global Biogeochem. Cycles, 14, 281-301.
35. Geider, R., and J. La Roche (1994), The role of iron in phytoplankton photosynthesis and the potential for iron-limitation of primary productivity in the sea, Photosynth. Res., 39, 275-301.
36. Geider, R., H. MacIntyre, and T. Kana (1998), A dynamic regulatory model of phytoplankton acclimation to light, nutrients and temperature, Limnol. Oceanogr., 43, 679-694.
37. Gledhill, M., and C. van den Berg (1994), Determination of complexation of iron(III) with natural organic complexing ligands in seawater using cathodic stripping voltammetry, Mar. Chem., 47, 41-54.
38. Honeyman, B., and P. Santschi (1989), A Brownian-pumping model for trace metal scavenging: Evidence from Th isotopes, J. Mar. Res., 47, 951-992.
39. Hudson, R., and F. Morel (1990), Iron transport in marine phytoplankton: Kinetics of cellular and medium coordination reactions, Limnol. Oceanogr., 35, 1002-1020.
40. Hurtt, G. C., and R. A. Armstrong (1996), A pelagic ecosystem model calibrated with BATS data, Deep Sea Res., Part II, 43, 653-683.
41. Hutchins, D., W.-X. Wang, and N. Fisher (1995), Copepod grazing and the biogeochemical fate of diatom iron, Limnol. Oceanogr., 40, 989-994.
42. Hutchins, D., A. Witter, A. Butler, and G. Luther III (1999), Competition among marine phytoplankton for different chelated iron species, Nature, 400, 858-861.
43. Jickells, T. (1995), Atmospheric input of metals and nutrients to the oceans: Their magnitude and effects, Mar. Chem., 48, 199-214.
44. Jickells, T. (1999), The input of dust-derived elements to the Sargasso Sea: A synthesis, Mar. Chem., 68, 5-14.
45. Jickells, T., and L. Spokes (2001), Atmospheric iron inputs to the oceans, in The Biogeochemistry of Iron in Seawater, edited by D. Turner and K. Hunter, pp. 85-121, John Wiley, Hoboken, N. J.
46. Jickells, T., W. Denser, and R. Belastock (1990), Temporal variations in the concentrations of some particulate elements in the surface waters of the sargasso sea and their relationship to deep-sea fluxes, Mar. Chem., 29, 203-219.
47. Johnson, K., K. Coale, V. Elrod, and N. Tindale (1994), Iron photochemistry in seawater from the equatorial Pacific, Mar. Chem., 46, 319-334.
48. Johnson, K., R. Gordon, and K. Coale (1997), What controls dissolved iron concentrations in the world ocean?, Mar. Chem., 57, 137-161.
49. Kieber, R., W. Cooper, J. Wiley, and G. B. Avery Jr. (2001), Hydrogen peroxide at the Bermauda Atlantic Timeseries Station: 1. Temporal variability of atmospheric hydrogen peroxide and its influence on seawater concentrations, J. Atmos. Chem., 39, 1-13.
50. 210Po in the upper Sargasso Sea: Influence from atmospheric iron deposition, Global Biogeochem. Cycles, 15, 651-661.
51. 7Be to the Sargasso Sea, Global Biogeochem. Cycles, 13, 1183-1192.
52. King, D., H. Lounsbury, and F. Millero (1995), Rates and mechanism of Fe(II) oxidation at nanomolar total iron concentrations, Environ. Sci. Technol., 29, 818-824.
53. Kuma, K., S. Nakabayashi, Y. Suzuki, I. Kudo, and K. Matsunaga (1992), Photo-reduction of Fe(III) by dissolved organic substances and existence of Fe(II) in seawater during spring blooms, Mar. Chem., 37, 15-27.
54. Lancelot, C., E. Hannon, S. Becquevort, C. Veth, and H. De Baar (2000), Modeling phytoplankton blooms and carbon export production in the Southern Ocean: Dominant controls by light and iron in the Atlantic sector in Austral spring 1992, Deep Sea Res., Part I, 47, 1621-1662.
55. 2 concentrations, Global Biogeochem. Cycles, 13, 727-736.
56. Mahowald, N., K. Kohfeld, M. Hansson, Y. Balkanski, S. Harrison, I. Prentice, M. Schulz, and H. Rodhe (1999), Dust sources and deposition during the Last Glacial Maximum and current climate: A comparison of model results with paleodata from ice cores and marine sediments, J. Geophys. Res., 104, 15,895-15,916.
57. Maldonado, M., and N. Price (1999), Utilization of iron bound to strong organic ligands by plankton communities in the subarctic North Pacific, Deep Sea Res., Part II, 46, 2447-2473.
58. Maldonado, M., and N. Price (2001), Reduction and transport of organically bound iron by Thalassiosira oceanica (Bacillariophyceae), J. Phycol., 37, 298-309.
59. 2 change: The iron hypothesis, Paleoceanography, 5, 1-13.
60. Martin, J., and S. Fitzwater (1988), Iron deficiency limits phytoplankton growth in the northeast Pacific subarctic, Nature, 331, 341-343.
61. Martin, J., et al. (1994), Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean, Nature, 371, 123-129.
62. Michaels, A., and A. Knap (1996), Overview of the U.S. JGOFS Bermuda Atlantic Timeseries Study and Hydrostation S program, Deep Sea Res., Part II, 43, 157-198.
63. Miller, W., D. King, J. Lin, and D. Kester (1995), Photochemical redox cycling of iron in coastal seawater, Mar. Chem., 50, 63-77.
64. 2 in seawater, Geochim. Cosmochim. Acta, 53, 1867-1873.
65. Millero, F., S. Sotolongo, and M. Izaguirre (1987), The oxidation kinetics of Fe(II) in seawater, Geochim. Cosmochim. Acta, 51, 793-801.
66. Moffett, J. (1995), Temporal and spatial variability of copper complexation by strong chelators in the Sargasso Sea, Deep Sea Res., Part I, 42, 1273-1295.
67. Mongin, M., D. M. Nelson, P. Pondaven, M. A. Brzezinski, and P. Tréguer (2003), Simulation of upper-ocean biogeochemistry with a flexible-composition phytoplankton model: C, N and Si cycling in the western Sargasso Sea, Deep Sea Res., Part I, 50, 1445-1480.
68. Moore, J., S. Doney, D. Glover, and I. Fung (2001), Iron cycling and nutrient-limitation patterns in surface waters of the world ocean, Deep Sea Res., Part II, 49, 463-507.
69. Moran, S. B., and K. O. Buesseler (1992), Short residence time of colloids in the upper ocean off Bermuda, Nature, 359, 221-223.
70. Muggli, D., M. Lecourt, and P. Harrison (1996), Effects of iron and nitrogen source on the sinking rate, physiology and elemental composition of an oceanic diatom from the subarctic Pacific, Mar. Ecol. Prog. Ser., 132, 215-227.
71. Nodwell, L., and N. Price (2001), Direct use of inorganic colloidal iron by marine mixotrophic phytoplankton, Limnol. Oceanogr., 46, 765-777.
72. Nyffeler, U., Y.-H. Li, and P. Santschi (1984), A kinetic approach to describe trace-element distribution between particles and solution in natural aquatic systems, Geochim. Cosmochim. Acta, 48, 1513-1522.
73. 2 and the photochemical demand of surface water DOM across the subtropical Atlantic Ocean, Limnol. Oceanogr., 46, 632-643.
74. O'Sullivan, D., A. Hanson, W. Miller, and D. Kester (1991), Measurement of Fe(II) in surface water of the equatorial Pacific, Limnol. Oceanogr., 36, 1727-1741.
75. Parekh, P., M. Follows, and E. Boyle (2004), Modeling the global ocean iron cycle, Global Biogeochem. Cycles, 18, GB1002, doi:10.1029/ 2003GB002061.
76. Rose, A., and T. Waite (2003a), Predicting iron speciation in coastal waters from the kinetics of sunlight-mediated iron redox cycling, Aquat. Sci., 65, 375-383.
77. Rose, A., and T. Waite (2003b), Kinetics of hydrolysis and precipitation of ferric iron in seawater, Environ. Sci. Technol., 37, 3897-3903.
78. Rose, A., and T. Waite (2003c), Kinetics of iron complexation by dissolved natural organic matter in coastal waters, Mar. Chem., 84, 85-103.
79. Rue, E., and K. Bruland (1995), Complexation of iron(III) by natural organic ligands in the Central North Pacific as determined by a new competitive ligand equilibration/adsorptive cathodic stripping voltammetric method, Mar. Chem., 50, 117-138.
80. Schartau, M., and A. Oschlies (2003a), Simultaneous data-based optimization of a 1D-ecosystem model at three locations in the North Atlantic Ocean: I. Method and parameter estimates, J. Mar. Res., 61, 765-793.
81. Schartau, M., and A. Oschlies (2003b), Simultaneous data-based optimization of a 1D-ecosystem model at three locations in the North Atlantic Ocean: II. Standing stocks and nitrogen fluxes, J. Mar. Res., 61, 795-821.
82. Schartau, M., A. Oschlies, and J. Willebrand (2001), Parameter estimates of a zero-dimensional ecosystem model applying the adjoint method, Deep Sea Res., Part II, 48, 1769-1800.
83. Soria-Dengg, S., and U. Horstmann (1995), Ferrioxamines B and E as iron sources for the marine diatom Phaeodactylum tricornutum, Mar. Ecol. Prog. Ser., 127, 269-277.
84. Spitz, Y. H., J. R. Moisan, and M. R. Abbott (2001), Configuring an ecosystem model using data from the Bermuda Atlantic Time Series (BATS), Deep Sea Res., Part II, 48, 1733-1768.
85. Spokes, L., and T. Jickells (1996), Factors controlling the solubility of aerosol trace metals in the atmosphere and on mixing into seawater, Aquat. Geochem., 1, 355-374.
86. Stumm, W. (1992), Chemistry of the Solid-Water Interface, Wiley-Interscience, Hoboken, N. J.
87. Sunda, W., and S. Huntsman (1995), Iron uptake and growth limitation in oceanic and coastal phytoplankton, Mar. Chem., 50, 189-206.
88. Sunda, W., and S. Huntsman (1997), Interrelated influence of iron, light and cell size on marine phytoplankton growth, Nature, 390, 389-392.
89. van den Berg, C. (1995), Evidence for organic complexation of iron in seawater, Mar. Chem., 50, 139-157.
90. Voelker, B., and D. Sedlak (1995), Iron reduction by photoproduced superoxide in seawater, Mar. Chem., 50, 93-102.
91. Völker, C., and D. Wolf-Gladrow (1999), Physical limits on iron uptake mediated by siderophores or surface reductases, Mar. Chem., 65, 227-244.
92. Waite, T., R. Szymczak, Q. Espey, and M. Furnas (1995), Diel variations in iron speciation in northern Australian shelf waters, Mar. Chem., 50, 79-91.
93. Watson, A. (2003), Iron limitation in the ocean, in The Biogeochemistry of Iron in Seawater, edited by D. R. Turner and K. A. Hunter, pp. 9-39, John Wiley, Hoboken, N. J.
94. Wells, M. (2003), The level of iron enrichment required to initiate diatom blooms in HNLC waters, Mar. Chem., 82, 101-114.
95. Wells, M., and E. Goldberg (1992), Marine submicron particles, Mar. Chem., 40, 5-18.
96. Wells, M., and E. Goldberg (1993), Colloid aggregation in seawater, Mar. Chem., 41, 353-358.
97. Wells, M., and L. Mayer (1991), The photoconversion of colloidal iron oxyhydroxides in seawater, Deep Sea Res., 38, 1379-1395.
98. Wen, L.-S., P. Santschi, and D. Tang (1997), Interactions between radioactively labeled colloids and natural particles: Evidence for colloidal pumping, Geochim. Cosmochim. Acta, 61, 2867-2878.
99. Wilhelm, S., and C. Trick (1994), Iron-limited growth of cyanobacteria: Multiple siderophore production is a common response, Limnol. Oceanogr., 39, 1979-1984.
100. Wilhelm, S., D. Maxwell, and C. Trick (1996), Growth, iron requirements, and siderophore production in iron-limited Synechococcus PCC 7002, Limnol. Oceanogr., 41, 89-97.
101. Wilhelm, S., K. MacAuley, and C. Trick (1998), Evidence for the importance of catechol-type siderophores in the iron-limited growth of a cyanobacterium, Limnol. Oceanogr., 43, 992-997.
102. Witter, A., and G. Luther III (1998), Variation in Fe-organic complexation with depth in the northwestern Atlantic Ocean as determined using a kinetic approach, Mar. Chem., 62, 241-258.
103. Witter, A., D. Hutchins, A. Butler, and G. Luther III (2000), Determination of conditional stability constants and kinetic constants for strong model Fe-binding ligands in seawater, Mar. Chem., 69, 1-17.
104. 2 coprecipitation, Anal. Chim. Acta, 367, 183-191.
105. Wu, J., and E. Boyle (2002), Iron in the Sargasso Sea: Implications for the processes controlling dissolved Fe distribution in the ocean, Global Biogeochem. Cycles, 16(4), 1086, doi:10.1029/2001GB001453.
106. Wu, J., and G. Luther III (1994), Size-fractionated iron concentrations in the water column of the western North Atlantic Ocean, Limnol. Oceanogr., 39, 1119-1129.
107. Wu, J., and G. Luther III (1995), Complexation of Fe(III) by natural organic ligands in the Northwest Atlantic Ocean by a competitive ligand equilibration method and a kinetic approach, Mar. Chem., 50, 159-177.
108. Wu, J., E. Boyle, W. Sunda, and L.-S. Wen (2001), Soluble and colloidal iron in the oligotrophic North Atlantic and North Pacific, Science, 293, 847-849.
109. Yuan, J., and A. Shiller (2001), The distribution of hydrogen peroxide in the southern and central Atlantic Ocean, Deep Sea Res., Part II, 48, 2947-2970.
110. Zhu, X., J. Prospero, and F. Millero, (1997), Diel variability of soluble Fe(II) and soluble total Fe in North African dust in the trade winds at Barbados, J. Geophys. Res., 102, 21,297-21,305.
111. Zhuang, G., R. Duce, and D. Kester (1990), The dissolution of atmospheric iron in the surface seawater of the open ocean, J. Geophys. Res., 95, 16,207-16,216.
112. Zhuang, G., Z. Yi, R. Duce, and P. Brown (1992), Chemistry of iron in marine aerosols, Global Biogeochem. Cycles, 6, 161-173.