Diet fluorescence patterns were discovered in phytoplankton sampled over 70
00 kilometers of the South Pacific Ocean that appear indicative of iron-lim
iting growth conditions. These patterns were rapidly Lost after in situ iro
n enrichment and were not observed during a 15,000-kilometer transect in th
e Atlantic Ocean where iron concentrations are relatively high. Laboratory
studies of marine Synechococcus sp, indicated that the patterns in the Sout
h Pacific are a unique manifestation of iron limitation on the fluorescence
signature of state transitions. Results suggest that primary productivity
is iron limited not only throughout the equatorial Pacific but also over mu
ch of the vast South Pacific gyre.