E. Sakshaug et al., PARAMETERS OF PHOTOSYNTHESIS - DEFINITIONS, THEORY AND INTERPRETATIONOF RESULTS, Journal of plankton research, 19(11), 1997, pp. 1637-1670
A global assessment of carbon flux in the world ocean is one of the ma
jor undertakings of the Joint Global Ocean Flux Study (JGOFS). This ha
s to be undertaken using historical in situ data of primary productivi
ty. As required by the temporal and spatial scales involved in a globa
l study, it can be conveniently done by combining, through appropriate
models, remotely sensed information (chlorophyll a, temperature) with
basic information about the parameters related to the carbon uptake b
y phytoplanktonic algae. This requires a better understanding as well
as a more extended knowledge of these parameters which govern the radi
ative energy absorption and utilization by algae in photosynthesis. Th
e measurement of the photosynthetic response of algae [the photosynthe
sis (P) versus irradiance (E) curves], besides being less shiptime con
suming than in situ primary production experiments, allows the needed
parameters to be derived and systematically studied as a function of t
he physical, chemical and ecological conditions. The aim of the presen
t paper is to review the sig nificance of these parameters, especially
in view of their introduction into models, to analyze the causes of t
heir variations in the light of physiological considerations, and fina
lly to provide methodological recommendations for meaningful determina
tions, and interpretation, of the data resulting from P versus E deter
minations. Of main concern are the available and usable irradiance, th
e chlorophyll a-specific absorption capabilities of the algae, the max
imum light utilization coefficient (alpha), the maximum quantum yield
(phi(m)), the maximum photosynthetic rate (P-m) and the light saturati
on index (E-k) The potential of other, non-intrusive, approaches, such
as the stimulated variable fluorescence, or the sun-induced natural f
luorescence techniques is also examined.