Gf. Blanchard et V. Carioulegall, PHOTOSYNTHETIC CHARACTERISTICS OF MICROPHYTOBENTHOS IN MARENNES-OLERON BAY, FRANCE - PRELIMINARY-RESULTS, Journal of experimental marine biology and ecology, 182(1), 1994, pp. 1-14
The photosynthetic characteristics of microphytobenthos inhabiting an
intertidal mudflat in Marennes-Oleron Bay (France) have been studied o
n samples collected at the air-sediment interface during low tide, Pho
tosynthesis-Irradiance (P-I) parameters were estimated at different ti
mes of low tide in March and in July. In summer, two different sedimen
t depths were also compared. The results point out different kinds of
changes in the photophysiological characteristics of microphytobenthos
, according to the time scale under consideration. At a seasonal scale
, there was an increase of I-k from March to July, thus indicating pho
toacclimation of microphytobenthos. At an hourly scale there was no ch
ange in I-k. In March, there was no change in P-I parameters, but ther
e was a significant change of alpha(B) and P-m(B) in July with the hig
hest values at T-3 (middle of low tide) at the surface of the sediment
. It is speculated that this change could be due to an endogenous phot
osynthetic rhythm. There was no difference in the photosynthetic chara
cteristics of microphytobenthos from the photic and the aphotic layers
, suggesting sediment mixing by physical and/or biological processes (
or microalgal migration) at a rate compatible with the persistence of
the photosynthetic response in the aphotic layer. Although benthic mic
roalgae did experience photoinhibition in experimental conditions, the
re was no indication of a photoinhibitory effect in situ. This suggest
s that microalgae were not exposed to strong illumination for extended
periods of time during low tide in spite of the direct exposure of th
e mudflat to incident irradiance, We suggest that the strong attenuati
on of light within the sediment, self-shading within algal mats, the m
otility of microalgae, and bioturbation can explain this apparent para
dox.