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Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean
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Permanent Link:
http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15052517/00001
Material Information
Title:
Testing the iron hypothesis in ecosystems of the equatorial Pacific Ocean
Series Title:
Nature Magazine Volume 371
Creator:
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. 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
Publication Date:
1994-09-08
Language:
English
Subjects
Subjects / Keywords:
climate change
Pacific Ocean
iron
phytoplankton
Notes
Abstract:
The idea that iron might limit phytoplankton growth in large regions of the ocean has been tested by enriching an area of 64 km 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.
Record Information
Source Institution:
Florida International University
Rights Management:
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