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Iron as a Limiting Factor in Oceanic Productivity

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Primary Productivity and Biogeochemical Cycles in the Sea

Part of the book series: Environmental Science Research ((ESRH,volume 43))

Abstract

Iron has been hypothesized to be a factor limiting phytoplankton standing crop in the ocean for decades. For example, in 1931, Gran suggested that, “If the productivity of the coastal waters is dependent on any factor of a chemical nature acting as a minimum factor, it must be an element which in its circulation does not follow the nitrates and phosphates accumulating in solution in the deep sea and reaching the surface again by vertical circulation of any kind. If such minimum stuffs exist, they must irreversibly go out of circulation in the sea, so that they can only be renewed from the land.” Based on growth in culture solution, Gran (1931, p.41) concluded that lack or low concentration of iron probably limited plant growth at times and in areas of the sea where it was not replenished by land drainage. Previous data, and those obtained by Braarud & Klem (1931) off the Norwegian coast at his instigation, showed the iron content of sea water to be very small, ranging from 3 to 21 mg. Fe per m3 (Harvey, 1938, p.205)

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References

  • Anderson, G. C., and Morel, F. M. M., 1982, The influence of aqueous iron chemistry on the uptake of iron by the coastal diatom Thalassiosira weissflogii, Limnol. Oceanogr., 27:789.

    Article  CAS  Google Scholar 

  • Barber, R. T., and Chavez, F. P., 1991, Regulation of primary productivity rate in the equatorial Pacific Ocean, in: “What Controls Phytoplankton Production in Nutrient-rich Areas of the Open Sea?”, ASLO Symposium, Lake San Marcos, California, February 22–24, 1991, S.W. Chisholm and F.M.M. Morel, eds., Allen Press, Lawrence, in press.

    Google Scholar 

  • Barnard, W.R., Andreae, M. O., and Iverson, R. L., 1984, Dimethyl sulphide and Phaeocystis pouchetii in the southeastern Bering Sea, Cont. Shelf Res., 3:103.

    Article  Google Scholar 

  • Barnola, J. M., Raynaud, D., Korotkevich, Y. S., and Lorius, C., 1987, Vostok ice core provides 160,000 year record of atmospheric CO2, Nature, 329:408.

    Article  CAS  Google Scholar 

  • Berger, W. H., 1991, No change down under, Nature, 351:186.

    Article  Google Scholar 

  • Braarud, T., and Klem, A., 1931, Hydrological and chemical investigations in the sea off More. Skr. Uttgift av Hvalradets ved Univ. Biol. Lab. Oslo, No. 1.

    Google Scholar 

  • Byrne, R. H., and Kester, D. R., 1975, Solubility of hydrous ferric oxide and iron speciation in seawater, Mar. Chem., 4:255.

    Article  Google Scholar 

  • Chavez, F. P., Buck, K.R., and Barber, R. T., 1990, Phytoplankton taxa in relation to primary production in the equatorial Pacific, Deep-Sea Res., 37:1733.

    Article  Google Scholar 

  • Coale, K. H., 1991, Effects of iron, managnese, copper and zinc enrichments on productivity and biomass in the subarctic Pacific, in: “What Controls Phytoplankton Production in Nutrient-rich Areas of the Open Sea?”, ASLO Symposium, Lake San Marcos, California, February 22–24, 1991, S.W. Chisholm and F.M.M. Morel, eds., Allen Press, Lawrence, in press.

    Google Scholar 

  • Crocker, K., Ondrescek, M., and Petty, R., 1991, Dimethylsulphide production from a Phaeocystis bloom in the Bellingshausen Sea, Antarctica. Abstract, in press.

    Google Scholar 

  • de Baar, H. J. W., Buma, A. G. J., Nolting, R. F., Cadee, G. C., Jaques, G., and Treguer, 1990, On iron limitation in the Southern Ocean: experimental observations in the Weddell and Scotia Seas, Mar. Ecol. Prog. Ser., 65:105.

    Article  Google Scholar 

  • De Angelis, M., Barkov, N. I., and Petrov, V.N., 1987, Aerosol concentrations over the last climatic cycle (160 kyr) from an Antarctic ice core, Nature, 325:318.

    Article  Google Scholar 

  • DiTullio, G. R., and Laws, E. A., 1991, Impact of an atmospheric-oceanic disturbance on phytoplankton community dynamics in the north Pacific central gyre, Deep-Sea Res., (in press).

    Google Scholar 

  • Duce, R. A., 1986, The impact of atmospheric nitrogen, phosphorus, and iron species on marine biological productivity, in: “The Role of Air-sea Exchange in Geochemical Cycling,” P. Buat-Menard, ed., D. Reidel Publishing Company, Dordrecht.

    Google Scholar 

  • Dunbar, R. B., Leventer, A. R., and Stockton, W. L., 1989, Biogenic sedimentation in McMurdo Sound, Antarctica, Mar Geol., 85:155.

    Article  CAS  Google Scholar 

  • Elrod, V. A., Johnson, K.S., and Coale, K. H., 1991, Determination of subnanomolar levels of iron(II) and total dissolved iron in seawater by flow injection analysis with chemiluminescence detection, Anal. Chem., 63:893.

    Article  CAS  Google Scholar 

  • El-Sayed, S. Z., 1988, Productivity of the Southern Ocean: A closer look, Compar. Biochem. Physiol., 90B:489.

    Google Scholar 

  • Feldman, G. C., 1986, Patterns of phytoplankton production around the Galapagos Islands, in: “Tidal Mixing and Plankton Dynamics; Lecture Notes on Coastal and Estraurine Studies, Vol. 17, J. Bowman, M. Yentsch, and W.T. Peterson, eds., Springer-Verlag, Berlin.

    Google Scholar 

  • Gran, H. H., 1931, On the conditions for the production of plankton in the sea, Rapp. Proc. Verb. Cons. Int. Explor. Mer., 75:37.

    Google Scholar 

  • Hart, T. J., 1934, On the phytoplankton of the south-west Atlantic and the Bellingshausen Sea, 1929–31, Discovery Reports, Vol. VIII.

    Google Scholar 

  • Harvey, H. W., 1938, The supply of iron to diatoms. J. Mar. Biol. Assoc., U.K., 22:205.

    Google Scholar 

  • Helbling, E. W., Villafane, V., and Holm-Hansen, O., 1991, Effect of Fe on productivity and size distribution of Antarctic phytoplankton, in: “What Controls Phytoplankton Production in Nutrient-rich Areas of the Open Sea?”, ASLO Symposium, Lake San Marcos, California, February 22–24, 1991, S.W. Chisholm and F.M.M. Morel, eds., Allen Press, Lawrence, in press.

    Google Scholar 

  • Hudson, J. M., and Morel, F. M. M., 1990, Iron transport in marine phytoplankton: Kinetics of cellular and medium coordination reactions, Limnol. Oceanogr., 35:1002.

    Article  CAS  Google Scholar 

  • Knox, F., and McElroy, M. B., 1984, Changes in atmospheric carbon dioxide: Influence of the marine biota at high latitude, J. Geophys. Res., 89:4629.

    Article  CAS  Google Scholar 

  • Legrand, M., Feniet-Saigne, C., Saltzman, E. S., Germain, C., Barkov, N.I., and Petrov, V.N., 1991, Ice-core record of oceanic emissions of dimethylsulphide during the last climate cycle, Nature, 350:144.

    Article  CAS  Google Scholar 

  • Lloyd, P., 1991, Iron determinations, Nature, 350:19.

    Article  Google Scholar 

  • Martin, J. H., 1990, Glacial-Interglacial CO2 change: The iron hypothesis, Paleoceanogr, 5:1.

    Article  Google Scholar 

  • Martin, J. H., and Gordon, R. M., 1988, Northeast Pacific iron distributions in relation to phytoplankton productivity, Deep-Sea Res., 35:177.

    Article  CAS  Google Scholar 

  • Martin, J. H., Gordon, R. M., Fitzwater, S., and Broenkow, W. W., 1989, VERTEX: Phytoplankton/iron studies in the Gulf of Alaska, Deep-Sea Res., 36:649.

    Article  CAS  Google Scholar 

  • Martin, J. H., Gordon, R. M., and Fitzwater, S.E., 1990, Iron in Antarctic waters, Nature, 345:156.

    Article  CAS  Google Scholar 

  • Martin, J. H., Gordon, R. M., and Fitzwater, S. E., 1991, The case for iron, in: “What Controls Phytoplankton Production in Nutrient-rich Areas of the Open Sea?”, ASLO Symposium, Lake San Marcos, California, February 22–24, 1991, S.W. Chisholm and F.M.M. Morel, eds., Allen Press, Lawrence, in press.

    Google Scholar 

  • McTaggert, A., 1991, The biogeochemistry of dimethylsulphide in Antarctic coastal seawater, Abstract, this volume.

    Google Scholar 

  • Minas, H. J., Coste, B., Minas, M., and Raimbault, P., 1990, Conditions hydrologiques, chimiques et production primaire dans les upwellings du Perou et des iles Galapagos, en regime d’hiver austral (campagne Paciprod), Oceanologia Acta, 10:383.

    Google Scholar 

  • Morel, F. M. M., and Hudson, R. J. M., 1985, The cycle of trace elements in aquatic systems: Redfield revisited, in: “Chemical Processes in Lakes,” W. Stumm, ed., Wiley, New York.

    Google Scholar 

  • Mortlock, R. A., Charles, C. D., Froelich, P. N., Zibello, M. A., Saltzman, J., Hays, J.D., and Burckle, L. H., 1991, Evidence for lower productivity in the Antarctic Ocean during the last glaciation, Nature, 351:220.

    Article  Google Scholar 

  • Nelson, D. M., and Smith, W. O., Jr., 1986, Phytoplankton bloom dynamics of the western Ross Sea ice edge — II. Mesoscale cycling of nitrogen and silicon, Deep-Sea Res., 33:1389.

    Article  CAS  Google Scholar 

  • Petit, J. R., Briat, M., and Royer, A., 1981, Ice age aerosol content from East Antarctic ice core samples and past wind strength, Nature, 293:391.

    Article  CAS  Google Scholar 

  • Price, N. M., Andersen, L.F., and Morel, F. M. M., 1991, Iron and nitrogen nutrition of equatorial Pacific plankton, Deep-Sea Res., (in press).

    Google Scholar 

  • Prospero, J. M., 1981, Eolian transport to the world ocean, in: “The Sea,” Vol. 7, C. Emiliani, ed., Wiley, N.Y.

    Google Scholar 

  • Raven, J. A., 1988, The iron and molybdenum use efficiencies of plant growth with different energy, carbon and nitrogen sources, New Phytol., 109:279.

    Article  CAS  Google Scholar 

  • Sarmiento, J. L., 1991, Slowing the buildup of fossil CO2 in the atmosphere by iron fertilization: A comment, Global Biogeochem. Cycles, 5:1.

    Article  CAS  Google Scholar 

  • Sarmiento, J. L., and Toggweiler, L. R., 1984, A new model for the role of the oceans in determining atmospheric carbon dioxide levels, Nature, 308:621.

    Article  CAS  Google Scholar 

  • Sarnthein, M., 1978, Sand deserts during glacial maximum and climatic optimum, Nature, 272:43.

    Article  Google Scholar 

  • Siegenthaler, U., and Wenk, T. H., 1984, Rapid atmospheric CO2 variations and ocean circulation, Nature, 308:624.

    Article  CAS  Google Scholar 

  • Sunda, W. G., Swift, D. G., and Huntsman, S. A., 1991, Low iron requirement in oceanic phytoplankton, Nature, 351:55.

    Article  CAS  Google Scholar 

  • Uematsu, M., 1987, Study of the continental material transported through the atmosphere to the ocean, J. Oceanogr. Soc. Japan, 43:395.

    Article  Google Scholar 

  • Uematsu, M., Duce, R. A., Prospero, J. M., Chen, L., Merrill, J. T., and McDonald, R. L., 1983, Transport of mineral aerosol from Asia over the North Pacific Ocean, J. Geophys. Res., 88:5343.

    Article  CAS  Google Scholar 

  • Wanninkhof, R., Ledwell, J. R., and Watson, A. J., 1991, Analysis of sulphur hexaflouride in seawater, J. Geophys. Res., 96:8733.

    Article  Google Scholar 

  • Wassmann, P., Vernet, M., Mitchell, B. G., and Rey, F., 1990, Mass sedimentation of Phaeocystis pouchetii in the Barents Sea, Mar. Ecol. Prog. Series, 66:183.

    Article  CAS  Google Scholar 

  • Young, R. W., Carder, K. L., Betzer, P. R., Costello, D. K., Duce, R. A., DiTullio, G. R., Tindale, N. W., Laws, E. A., Uematsu, M., Merrill, J. T., and Feely, R. A., 1991, Atmospheric iron inputs and primary productivity: Phytoplankton responses in the north Pacific, Global Biogeochem. Cycles (in press).

    Google Scholar 

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Authors and Affiliations

  1. Moss Landing Marine Laboratories, Moss Landing, CA, 95039, USA

    John H. Martin

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  1. John H. Martin
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Editors and Affiliations

  1. Oceanographic and Atmospheric, Sciences Division, Brookhaven National Laboratory, Upton, NY, 11973, USA

    Paul G. Falkowski

  2. Biology Department, Brookhaven National Laboratory, Upton, NY, 11973, USA

    Avril D. Woodhead

  3. Brookhaven National Laboratory, Upton, NY, USA

    Katherine Vivirito

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© 1992 Springer Science+Business Media New York

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Martin, J.H. (1992). Iron as a Limiting Factor in Oceanic Productivity. In: Falkowski, P.G., Woodhead, A.D., Vivirito, K. (eds) Primary Productivity and Biogeochemical Cycles in the Sea. Environmental Science Research, vol 43. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-0762-2_8

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  • DOI: https://doi.org/10.1007/978-1-4899-0762-2_8

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