No abstract

The atmospheric transport of

No abstract

No abstract

On a transect study in the eastern equatorial Pacific, from the high-nutrient, low-chlorophyll tropical waters to the oligotrophic subtropical waters, we determined the variability in the maximum change in the quantum yield of chlorophyll fluorescence (A&,) by means of a fast repetition rate fluorometer. A& is a quantitative measure of photochemical energy conversion efficiency in photosystem 2, the variability of which is determined by the functional organization of the photosynthetic apparatus. The results revealed that A&,, was relatively low throughout the nutrient-rich equatorial waters, providing unequivocal evidence for physiological limitation of photochemical energy conversion efficiency in the natural phytoplankton populations. Shipboard enrichment studies showed that A&, increased following addition of nanomolar concentrations of inorganic iron as well as aerosol dust added at similar iron concentrations. This response reflects an iron-induced repair of photosystem 2 function in the enclosed bottle community. Low A&, at the top of the Equatorial Undercurrent indicated that the amount of iron upwelled to the surface was insufficient .t,o repair photosystem 2 function. Our results strongly suggest that iron availability limits photochemrcal energy conversion efficiency and is the principal mechanism controlling rates of photosynthesis and growth in the nutrient-rich equatorial Pacific.Unused nutrients (inorganic N and P) persist throughout the surface waters of the equatorial Pacific despite light and stratification conditions favorable for rapid nutrient utilization. Fueled by the upwelling of nutrient-rich waters, equatorial primary productivity and phy-* Present address: Department of Biology, Brookhaven National Laboratory, Upton, New York 11973. AcknowledgmentsWe thank the captain and crew of the RV Wecoma for their assistance during the preparation and conduct of the field program. We are grateful to S. Tanner for conducting nutrient and chlorophyll analyses and to J. Martin and A. Hanson for providing dissolved Fe data. We also extend our appreciation to J. Cullen and an anonymous reviewer for critical comments on the manuscript.