PHYSIOLOGICAL LIMITATION OF PHYTOPLANKTON PHOTOSYNTHESIS IN THE EASTERN EQUATORIAL PACIFIC DETERMINED FROM VARIABILITY IN THE QUANTUM YIELDOF FLUORESCENCE
Rm. Greene et al., PHYSIOLOGICAL LIMITATION OF PHYTOPLANKTON PHOTOSYNTHESIS IN THE EASTERN EQUATORIAL PACIFIC DETERMINED FROM VARIABILITY IN THE QUANTUM YIELDOF FLUORESCENCE, Limnology and oceanography, 39(5), 1994, pp. 1061-1074
On a transect study in the eastern equatorial Pacific, from the high-n
utrient, low-chlorophyll tropical waters to the oligotrophic subtropic
al waters, we determined the variability in the maximum change in the
quantum yield of chlorophyll fluorescence (DELTAphi(m)) by means of a
fast repetition rate fluorometer. DELTAphi(m) is a quantitative measur
e of photochemical energy conversion efficiency in photosystem 2, the
variability of which is determined by the functional organization of t
he photosynthetic apparatus. The results revealed that DELTAphi(m) was
relatively low throughout the nutrient-rich equatorial waters, provid
ing unequivocal evidence for physiological limitation of photochemical
energy conversion efficiency in the natural phytoplankton populations
. Shipboard enrichment studies showed that DELTAphi(m) increased follo
wing addition of nanomolar concentrations of inorganic iron as well as
aerosol dust added at similar iron concentrations. This response refl
ects an iron-induced repair of photosystem 2 function in the enclosed
bottle community. Low DELTAphi(m) at the top of the Equatorial Undercu
rrent indicated that the amount of iron upwelled to the surface was in
sufficient to repair photosystem 2 function. Our results strongly sugg
est that iron availability limits photochemical energy conversion effi
ciency and is the principal mechanism controlling rates of photosynthe
sis and growth in the nutrient-rich equatorial Pacific.