Total dissolvable iron in surface waters of the south Atlantic was mea
sured using a flow injection analytical system with chemiluminescent d
etection and preconcentration onto 8-hydroxyquinoline resin. Surface w
ater iron concentrations range from less than 0.5 nM to 10 nM. Results
indicate that very high iron concentrations in the surface seawater a
re possible due to high atmospheric input and upwelling. The dual inpu
t mechanism is supported by correlations with Al, particulate matter a
nd nutrients.