Mj. Whitehouse et al., SUBSTANTIAL OPEN-OCEAN PHYTOPLANKTON BLOOMS TO THE NORTH OF SOUTH GEORGIA, SOUTH-ATLANTIC, DURING SUMMER 1994, Marine ecology. Progress series, 140(1-3), 1996, pp. 187-197
Substantial open-ocean phytoplankton blooms in the Antarctic Zone to t
he northwest of South Georgia, South Atlantic are described. Chlorophy
ll a, nutrient and physical oceanography data, collected between 2 and
5 January 1994 and again 1 mo later between 2 and 4 February along a
450 km transect comprising 14 stations, are presented. The transect cr
ossed the Subantarctic and the Polar Front. During the January transec
t survey, in 2 locations to the south of the Polar Front, average surf
ace mixed-layer chlorophyll a concentrations were >8 and >13 mg m(-3),
and were associated with silicate, nitrate and phosphate depletions (
<2.0, <11.0 and 1.0 mmol m(-3) respectively), and nitrite and ammonium
enhancement (>0.3 and >1.4 mmol m(-3) respectively). One of the phyto
plankton blooms was associated with the nearby Polar Front, but the or
igin of a bloom further south, well within the Antarctic Zone, was not
clear. Phytoplankton production predicted by nutrient drawdown was fa
r greater than the observed biomass on both surveys. If a common Antar
ctic Zone origin is accepted for the southern bloom, a decline in biom
ass of similar to 2.7 mol C m(-2) occurred in the upper 50 m of the wa
ter column between the 2 surveys, which cannot be accounted for by zoo
plankton grazing. If the bloom had originated in Subantarctic water ad
vected to the south of the Polar Front, initial nutrient concentration
s would have been lower and consequently predicted production was clos
er to the observed biomass values. Nevertheless, the area may be one o
f intense but local carbon export.