Abstract

Photosynthesis-irradiance and phytoplankton absorption data from waters of the central Gulf of California, as well as data in the literature, were analyzed in order to propose working averages of the physiological parameters of phytoplankton to estimate primary productivity at large time and space scales. Since there is substantial variability within data sets, we conclude that it is not possible at this time to predict fine time- and space-scale variation in photosynthetic parameters. We recommend the following working averages for the whole Gulf of California and for "winter" conditions (surface TºC <22ºC): a surface P*max = 9.6 ± 2.4 mgC mgChl–1 h–1 (assimilation number), with a linear variation between this and 3.7 ± 0.3 at the middle of the euphotic zone (ez), and then a constant value for deeper waters; a single value of α*inc = 0.029 ± 0.004 mgC mgChl–1 h–1 (μmol quanta m–2 s–1)–1 (incubator´ s initial slope); and φmax = 0.06 ± 0.01 molC (mol quanta)–1 (quantum yield of photosynthesis). For "summer" conditions we recommend: a surface P*max = 3.7 ± 0.3, with a linear variation between this and 1.5 ± 0.2 at the middle of the ez, and another linear variation between the latter and 0.4 ± 0.1 at the bottom of the ez; a surface α*inc = 0.013 ± 0.001, with a linear variation between this and 0.001 at the bottom of the ez; and a single value φmax = 0.014 ± 0.002. A procedure is given to correct α*inc for the in situ spectral distribution of light to obtain α*in situ.

Highlights

  • La fijación fotosintética del carbono inorgánico a material orgánico es realizada casi totalmente por fitoplancton en el océano, pero la cantidad de carbono fijado es incierta (Behrenfeld et al, 1998)

  • The parameters used in these algorithms belong to three categories: environmental, ecological, and physiological (Morel, 1991)

  • November is a month of transition and, due to interannual changes, sometimes the Gulf of California has “summer” conditions during this month and sometimes it is the opposite

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Summary

Introduction

La fijación fotosintética del carbono inorgánico a material orgánico es realizada casi totalmente por fitoplancton en el océano, pero la cantidad de carbono fijado es incierta (Behrenfeld et al, 1998). The parameters used in these algorithms belong to three categories: environmental (e.g., geographic location, atmospheric conditions, irradiance profile), ecological (e.g., chlorophyll profile), and physiological (Morel, 1991). Examples of the latter are the photosynthesis-irradiance (P-E) curve parameters, the specific absorption coefficient of phytoplankton (normalized per unit chlorophyll a concentration: a*ph(λ) = aph(λ)/Chl), Valdez-Holguín et al.: Parámetros fotosintéticos del fitoplancton del Golfo de California por unidad de concentración de clorofila a: a*ph(λ) = aph(λ)/Chl), y la eficiencia cuántica de la fotosíntesis (φ(z)), donde λ es la longitud de onda de la luz y z es la profundidad

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