D. Karentz et Hj. Spero, RESPONSE OF A NATURAL PHAEOCYSTIS POPULATION TO AMBIENT FLUCTUATIONS OF UVB RADIATION CAUSED BY ANTARCTIC OZONE DEPLETION, Journal of plankton research, 17(9), 1995, pp. 1771-1789
During the austral spring of 1990, rotation of the Antarctic polar vor
tex resulted in a 2-fold change in ozone concentrations (170-380 Dobso
n units) over regions of the marginal ice zone of the Bellingshausen S
ea. The changes in ozone caused significant variations in incident and
in-water UVB fluences. Phytoplankton cell densities, nutrient concent
rations, DNA concentrations and stable carbon isotope ratios (delta(13
)C) of particulate organic and dissolved inorganic carbon were monitor
ed for a 5-week period during the ozone fluctuations. Phaeocystis was
the dominant phytoplankton taxon and cell numbers were positively corr
elated to ozone and the delta(13)C of seawater Sigma CO2, and negative
ly correlated to nutrient concentrations. The densities of co-occurrin
g diatoms were not related to changes in ozone, delta(13)C or nutrient
s. These observations suggest that Phaeocystis sp. responds very rapid
ly and adversely to increased UVB exposure, and that seawater delta(13
)C data may be a useful tool for assessing the physiological state of
high-latitude marine communities relative to increased UVB levels.