The xanthophyll cycle has been implicated as a possible photoprotectiv
e mechanism in higher plants and algae by dissipating excess excitatio
n energy via non-photochemical quenching. To examine whether colonial
Phaeocystis antarctica Karsten displays xanthophyll cycling, nutrient-
replete cultures were initially grown under limiting (40 mu mol quanta
m(-2) s(-1)) and saturating (280 mu mol quanta m(-2) s(-1)) irradianc
es for photosynthesis and their responses to irradiance transitions we
re examined for 1 h under 4 treatments. The in vivo chl-specific absor
ption coefficient [a(ph)(lambda), m(2) (mg chl a)(-1)] for the Light-
limited cultures was initially lower than the light-saturated cultures
while chlorophyll (chl) a-normalized fluorescence yields were similar
for both treatments. Increases in irradiance induced increases in the
diatoxanthin to diadinoxanthin ratio (DT:DD, w:w) up to 9-fold wherea
s parallel decreases in irradiance similarly decreased the DT:DD ratio
. Light-induced increases in DT concentration were reduced in cultures
exposed to dithiothreitol (DTT), an inhibitor of DD to DT conversion.
Short-term changes in DD and DT concentrations were attributed solely
to xanthophyll cycling; no de novo synthesis of DD or DT was evident
based on a constant sum of DD and DT in the 1 h experimental perturbat
ions. It was found that DD and DT de novo synthesis required long-term
acclimation; the mass ratio at steady state of (DD+DT)/chl a was 0.1
and 0.4 for the low and high light treatments, respectively. Pooled re
sults from treatment and control cultures showed a linear relationship
between light-induced changes in DT/chl a concentration and F/chl a (
fluorescence to chi a ratio) and the slopes depended on the initial ph
otoacclimated state of the culture. Cellular fluorescence changes appe
ared to be physiologically based; a(ph)(lambda) did not change in res
ponse to abrupt irradiance changes. Xanthophyll cycling may enable P.
antarctica to tolerate both high light environments and sudden changes
in irradiance, which occur during austral spring due to shallow mixed
layers and intermittent shading by ice or clouds.