Ea. Pakhomov et al., Zooplankton structure and grazing in the Atlantic sector of the Southern Ocean in late austral summer 1993 - Part 1. Ecological zonation, DEEP-SEA I, 47(9), 2000, pp. 1663-1686
Citations number
73
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
The composition, distribution, abundance, biomass and size structure of mes
ozooplankton, collected using Bongo nets in the top 300 m layer along a tra
nsect between the Antarctic continent and Cape Town, were investigated duri
ng the second South African Antarctic Marine Ecosystem Study (SAAMES II) in
Jan.-Feb. 1993. Small (<10 mm) and medium (20-50 mm) size groups of zoopla
nkton consistently dominated across the Southern Ocean. The highest zooplan
kton densities were recorded at the Antarctic Polar Front (APF) and at the
Subtropical Convergence (STC). Minor peaks in zooplankton densities were ob
served in the southern vicinity of the Subantarctic Front (SAF) and APF. El
evated zooplankton stocks were also found within the Marginal Ice Zone (MIZ
) and the Polar Frontal Zone. The lowest densities were recorded in the per
manently open zone (MIZ-APF) and in the Subantarctic zone (SAF-STC). Copepo
ds were generally important along the entire transect and formed the bulk o
f zooplankton stock within the MIZ and in the Polar Frontal Zone (APF-SAF),
accounting for at least 40-95% of total abundance and biomass. Euphausiids
were also a prominent group along the transect. Their contribution was hig
hest (up to 80% of total biomass) between the MIZ and the APF, mainly becau
se of the occurrence of swarms of the Antarctic krill Euphausia superba. Tu
nicates, Pyrosoma sp. and Salpa fusiformis, were found in great numbers onl
y in the region of the STC and further north, while Salpa thompsoni was abu
ndant at the southern boundary of the APF. Chaetognaths dominated samples n
umerically and by mass in the Subantarctic Zone. Results obtained from clus
ter and ordination analyses show that zooplankton community structure was w
ell correlated with the position of various biogeographical zones separated
by the main frontal systems of the Southern Ocean. Two major groupings of
stations, separated by the SAF, were identified in these analyses. This fro
nt separated the Antarctic and the subantarctic/subtropical assemblages, co
nfirming its important role as a biogeographical boundary. (C) 2000 Elsevie
r Science Ltd. All rights reserved.