OCCURRENCE OF ANTARCTIC KRILL (EUPHAUSIA-SUPERBA) CONCENTRATIONS IN THE VICINITY OF THE SOUTH SHETLAND ISLANDS - RELATIONSHIP TO ENVIRONMENTAL PARAMETERS
T. Ichii et al., OCCURRENCE OF ANTARCTIC KRILL (EUPHAUSIA-SUPERBA) CONCENTRATIONS IN THE VICINITY OF THE SOUTH SHETLAND ISLANDS - RELATIONSHIP TO ENVIRONMENTAL PARAMETERS, Deep-sea research. Part 1. Oceanographic research papers, 45(8), 1998, pp. 1235-1262
The influences of abiotic and biotic parameters on the occurrence of A
ntarctic krill (Euphausia superba) concentrations were studied in the
waters north of the South Shetland Islands, a major krill fishing grou
nd in the Antarctic, during the 1990/1991 austral summer. From early t
o mid-summer krill density increased and showed distinct offshore-insh
ore differences in abundance and maturity stages. In mid-summer, krill
density was low in the oceanic zone (8 gm(-2)) and higher in the slop
e frontal zone (36 gm(-2)), being highest along the shelf break (131 g
m(-2)) in the inshore zone. Krill were in the reproductive stage in th
e oceanic and frontal zones, but non-reproductive in the inshore zone.
Water circulation, food and frontal features were considered importan
t environmental factors determining the occurrence of high krill conce
ntrations in these waters. Drifting buoys indicated that the surface w
ater circulation in areas of krill concentrations was characterized by
a sluggish current with eddies along the shelf break in the inshore z
one and a shear current in the frontal zone, thus enhancing the reside
nce time for krill. Diatom abundance in both the frontal and inshore z
ones increased from early to mid-summer, improving krill feeding condi
tions. Gravid females were closely associated with the frontal zone, s
howing that the latter may also be a favored spawning area because of
the higher probability of survival for embryos and larvae, in addition
to enhanced opportunities for their transport to nursery grounds by p
revailing currents. In the waters north of the South Shetland Islands,
krill appeared to be highly adapted for exploitation of the rich food
resources of the frontal/inshore zone, taking advantage of oceanograp
hic features that led to their retention in these zones. (C) 1998 Else
vier Science Ltd. All rights reserved.