Changes in specific photosynthetic rate of oceanic phytoplankton from the northeast Pacific Ocean

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Abstract

The study is based on data (n=244) from light-saturation experiments utilizing artificial incubation under fluorescent light. Values of maximum photosynthetic rate, Pmax, and the light intensity at which it takes place, Imax, are estimated by non-linear regression using stepwise Gauss-Newton iterations. Estimated values of Pmax ranged from 0.85 to 5.48 mg C (mg Chl a·h)-1;Imax varied from 2.35 to 5.52 cal (cm2·h)-1. The effects of time (months) and depth (illumination levels) and their interaction are evaluated by analysis of covariance using a linear model. A significant time-depth interaction is noted: The maximum specific primary productivity occurred in the surface layers during March, at the 50% light level during April, and at 1% level during May. Estimates of Pmax from simulated in situ primary productivity experiments for the same period are lower than those from light-saturation experiments. A comparison of data from light-saturation and simulated in situ experiments indicated that effects of duration of experiments and the quality of available light may affect primary productivity data considerably. © 1977 Biologische Anstalt Helgoland.

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Hameedi, M. J. (1977). Changes in specific photosynthetic rate of oceanic phytoplankton from the northeast Pacific Ocean. Helgoländer Wissenschaftliche Meeresuntersuchungen, 30(1–4), 62–75. https://doi.org/10.1007/BF02207825

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