Sea-surface distribution of coccolithophores, diatoms, silicoflagellates and dinoflagellates in the South Atlantic Ocean during the late austral summer 1995
F. Eynaud et al., Sea-surface distribution of coccolithophores, diatoms, silicoflagellates and dinoflagellates in the South Atlantic Ocean during the late austral summer 1995, DEEP-SEA I, 46(3), 1999, pp. 451-482
Citations number
60
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
The sea-surface distribution of four selected fossilizable phytoplankton gr
oups (coccolithophores, diatoms, silicoflagellates and dinoflagellates) has
been studied along a transect from Cape Town (34 degrees S) to South Sandw
ich Islands (57 degrees S) during the late austral summer. The observed dis
tribution of these groups shows that their biogeographical distribution is
significantly constrained by the water masses and associated frontal system
s of the Southern Ocean. Coccolithophores are the dominant group and show c
ell abundances up to 51 x 10(3) cells/1 down to 57 degrees S. Three restric
ted areas are marked by particularly high cell densities: the continental s
helf of South Africa, the area between the Sub-Tropical Convergence and the
Sub-Antarctic Front, and the southern border of the Antarctic Polar Front,
where the highest abundances are recorded (> 650 x 10(3) cells/l). The spe
cies composition of the various assemblages representative of the four grou
ps defines distinct biogeographical zones bounded by marked sea-surface tem
perature gradients. This biogeographical distribution is confirmed by facto
r analysis of the coccolithophore (5 factors, 85% of the total variance) an
d diatom and silicoflagellate (7 factors, 87.5% of the total variance) popu
lations. When compared with the distribution pattern of siliceous fossil as
semblages in surface sediments, our data show a more accurate coupling betw
een the various water-masses of the South Atlantic Ocean and the living sil
iceous population. (C) 1999 Elsevier Science Ltd. All rights reserved.