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Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean

  • J. H. Martin
  • , K. H. Coale*
  • , K. S. Johnson
  • , S. E. Fitzwater
  • , R. M. Gordon
  • , S. J. Tanner
  • , C. N. Hunter
  • , V. A. Elrod
  • , J. L. Nowicki
  • , T. L. Coley
  • , R. T. Barber
  • , S. Lindley
  • , A. J. Watson
  • , K. Van Scoy
  • , C. S. Law
  • , M. I. Liddicoat
  • , R. Ling
  • , T. Stanton
  • , J. Stockel
  • , C. Collins
  • A. Anderson, R. Bidigare, M. Ondrusek, M. Latasa, F. J. Millero, K. Lee, W. Yao, J. Z. Zhang, G. Friederich, C. Sakamoto, F. Chavez, K. Buck, Z. Kolber, R. Greene, P. Falkowski, S. W. Chisholm, F. Hoge, R. Swift, J. Yungel, S. Turner, P. Nightingale, A. Hatton, P. Liss, N. W. Tindale
*Corresponding author for this work
  • Moss Landing Marine Laboratories
  • Monterey Bay Aquarium Research Institute
  • Duke University
  • Mote Marine Laboratory
  • Naval Postgraduate School
  • University of Hawaiʻi at Mānoa
  • Rosenstiel School of Marine and Atmospheric Science
  • Brookhaven National Laboratory
  • Massachusetts Institute of Technology
  • National Aeronautics and Space Administration
  • University of East Anglia
  • The University of Texas System

Research output: Contribution to journalArticlepeer-review

1229 Citations (Scopus)

Abstract

The idea that iron might limit phytoplankton growth in large regions of the ocean has been tested by enriching an area of 64 km2 in the open equatorial Pacific Ocean with iron. This resulted in a doubling of plant biomass, a threefold increase in chlorophyll and a fourfold increase in plant production. Similar increases were found in a chlorophyll-rich plume down-stream of the Galapagos Islands, which was naturally enriched in iron. These findings indicate that iron limitation can control rates of phytoplankton productivity and biomass in the ocean.

Original languageEnglish
Pages (from-to)123-129
Number of pages7
JournalNature
Volume371
Issue number6493
DOIs
Publication statusPublished - 1994
Externally publishedYes

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