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A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization


Boyd, PW and Watson, AJ and Law, CS and Abraham, ER and Trull, T and Murdoch, R and Bakker, DCE and Bowie, AR and Buesseler, KO and Chang, H and Charette, M and Croot, P and Downing, K and Frew, R and Gall, M and Hadfield, M and Hall, J and Harvey, M and Jameson, G and LaRoche, J and Liddicoat, M and Ling, R and Maldonada, MT and McKay, RM and Nodder, S and Pickmere, S and Pridmore, R and Rintoul, SR and Safi, K and Sutton, P and Strzepek, R and Tanneberger, K and Turner, S and Waite, A and Zeldis, J, A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization, Nature, 407 pp. 695-702. ISSN 0028-0836 (2000) [Refereed Article]

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Copyright Statement

Copyright 2000 Macmillan Magazines Ltd.

DOI: doi:10.1038/35037500


Changes in iron supply to oceanic plankton are thought to have a significant effect on concentrations of atmospheric carbon dioxide by altering rates of carbon sequestration, a theory known as the 'iron hypothesis'. For this reason, it is important to understand the response of pelagic biota to increased iron supply. Here we report the results of a mesoscale iron fertilization experiment in the polar Southern Ocean, where the potential to sequester iron-elevated algal carbon is probably greatest. Increased iron supply led to elevated phytoplankton biomass and rates of photosynthesis in surface waters, causing a large drawdown of carbon dioxide and macronutrients, and elevated dimethyl sulphide levels after 13 days. This drawdown was mostly due to the proliferation of diatom stocks. But downward export of biogenic carbon was not increased. Moreover, satellite observations of this massive bloom 30 days later, suggest that a sufficient proportion of the added iron was retained in surface waters. Our findings demonstrate that iron supply controls phytoplankton growth and community composition during summer in these polar Southern Ocean waters, but the fate of algal carbon remains unknown and depends on the interplay between the processes controlling export, remineralisation and timescales of water mass subduction.

Item Details

Item Type:Refereed Article
Keywords:phytoplankton bloom, iron fertilization, Southern Ocean
Research Division:Earth Sciences
Research Group:Oceanography
Research Field:Chemical oceanography
Objective Division:Environmental Management
Objective Group:Marine systems and management
Objective Field:Measurement and assessment of marine water quality and condition
UTAS Author:Trull, T (Professor Thomas Trull)
UTAS Author:Bowie, AR (Professor Andrew Bowie)
UTAS Author:Rintoul, SR (Dr Steve Rintoul)
UTAS Author:Strzepek, R (Dr Robert Strzepek)
ID Code:76851
Year Published:2000
Web of Science® Times Cited:1140
Deposited By:CRC-Antarctic Climate & Ecosystems
Deposited On:2012-03-14
Last Modified:2021-11-15
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