Au. Bracher et al., Primary production, physiological state and composition of phytoplankton in the Atlantic Sector of the Southern Ocean, MAR ECOL-PR, 190, 1999, pp. 1-16
Phytoplankton species composition and primary production were studied in th
e Atlantic Sector of the Southern Ocean in early austral summer 1995/1996.
Results from photosynthesis-irradiance experiments (P vs E curves) were use
d to examine photosynthetic adaptation in this part of the ocean. The study
area comprised 3 different provinces: the Antarctic Polar Front (APF), the
Antarctic Circumpolar Current (ACC) beyond the influence of frontal system
s, and the marginal ice zone (MIZ). Phytoplankton composition derived from
HPLC data, P-m* (maximum biomass-specific photosynthetic production rate) v
alues and areal daily primary production (ADP) rates showed different featu
res for these zones. The central core of the APF was dominated (60 %) by a
bloom of large (>20 mu m) diatoms (Thalassiothrix spp., Pseudonitzschia cf.
lineola and Chaetoceros spp.), equal values for P-m* at the surface and 1%
light depths and ADP rates exceeding 900 mg C m(-2) d(-1). At the fringes
of the APF core, phytoplankton were smaller, diatom abundance decreased and
dinoflagellates, prymnesiophytes and chrysophytes became more important wi
thin the community. Chlorophyll a concentrations and ADP rates were low and
comparable to values for the ACC outside the front: <0.5 mg m(-3) and <300
mg C m(-2) d(-1) respectively. Beyond the frontal systems, P-m* values fro
m the 1% light depth were significantly higher than at the surface. There w
as also a bloom of large phytoplankton species within the MIZ, dominated in
contrast by Phaeocystis spp.; this province was characterised by ADP rates
of 558 mg C m(-2) d(-1). Vertical mixing processes, temperature, silicate
concentrations and zooplankton grazing seem to be the factors controlling p
roduction and growth of phytoplankton at this time.