 | FAO/SIDP Species Identification Sheets |
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| Euphausia superba Dana, 1852 |
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| FAO Names |
EN - Antarctic krill; FR - Krill antarctique; SP - Krill antártico.
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| Diagnostic Features |
| Eyes spherical, somewhat larger in
males than in females. Rostrum short, triangular and
truncated, a little shorter in males than in females. Distal
segment of mandibular palp long and slender, seven times as
long as broad. First segment of antennular peduncle bearing
a wide lappet with a sinuous distal margin which is stouter,
narrower and smaller in males than females second segment
bearing a dorsal lappet which is wider and larger in
females. Abdominal segments without mid-dorsal spines; sixth
segment clearly as long as high. Proximal process of petasma
without keel, terminal process curved and pointed, not cleft
in two; lateral process without secondary tooth. |
| Geographical Distribution |
E. superba occurs in a wide
circumpolar belt between the Antarctic Continent and the
Polar Front. Areas of highest abundance as determined
with plankton nets an trawls are found within or next to
the East Wind Drift, and in other northern sectors such
as the Scotia Sea, Weddell Drift and off the Antarctic
Peninsula and the Kerguelen-Gaussberg Ridge.
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| Habitat and Biology |
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The distribution pattern of
populations may be a result of the effect of currents,
eddies and other hydrographic processes, of the bottom
topography, or of the food and predator distribution.
The existence of more or less independent populations of
this species around the Antarctic Continent has been
proposed. Overall densities of krill show considerable
variability in space and time throughout the
distributional range of the species, due to its
gregarious behaviour. Recent observations showed krill
swarms swimming at 90° to currents for about 180 miles,
but as E. superba seems
generally incapable of swimming against most Antarctic
surface currents, it can form patches, shoals, schools,
swarms or superswarms. These groups extend in space from
a few square metres to more than 100 km, with densities
ranging from 0.5 to several kg/m3;
they are located at the surface or
at various depth ranges, either migrating vertically or
remaining stationary within the upper 100 m water layer.
These groups may be transient
(hours-days) or persist for weeks to a life-time and
their components vary considerably in shape, size and
gonad development. Swarming and schooling behaviour of
krill is explained as an adaptive strategy to avoid
selective predators (fishes, birds, etc.), and to
increase efficiency in food-searching and food-patch
utilization. The groups are usually associated with
islands, continental shelves and slopes, or zones of
water mixing. Although krill is commonly found in dense
aggregations, a significant (perhaps a major) part of
the population occurs in a solitary or dispersed stage.
Spawning probably occurs over most
of the distributional range of the species, either near
the continent or in the open ocean during late spring
and summer, peaking from early January to mid-February.
Several thousands of eggs per female are laid in the
upper 100 m of water. The eggs sink for about 10 days
and hatch as nauplii
several hundreds to 2,000 m deep.
The nauplii ascend and develop
into metanauplii continuing to rise to shallower layers
and developing into calyptopes. These surface dwellers
pass through three stages to become furcilia (5 stages),
the duration of every larval stage being between 8 and
15 days. Thereafter, the furcilia develop into juveniles
which begin gonad development during the second
spring-summer season of life. Individuals mature and
begin mating at two years of age. Some individuals delay
maturity and spawning until the third year, while others
may spawn a second time in this third year.
A major part of the population has
a two-year lifespan, but recent research suggests a
7-year lifespan. A typical summer size-class
distribution of E. superba in
the Scotia Sea shows 3 modes: calyptopes and furcilia
peak at about 7 mm, juveniles at 34 mm and adults at 50 mm.
Calyptopes and early furcilia stages
perform pronounced vertical diel migrations, while
juveniles and adults are commonly found in the upper 30
m at flight, and may migrate within the upper 100 m
layer in daytime or remain stationary throughout day and
night. No definite diel pattern of vertical distribution
is established for juveniles or adults.
Krill feed preferentially on phytoplankton
from large diatoms to nanno-plankton. They are also
adapted to feed on a wide spectrum of items including
their own eggs, larvae, molts and phaeces, live or dead
krill specimens, other zooplankters, or ice-attached
diatoms. Raptorial feeding rather than filter-feeding
seems the main mode of food intake of E.
superba. During the winter months, krill
may depend upon alternative food sources rather than on
phytoplankton, or may survive by consuming its body
tissues which will be accompanied by body shrinkage and
reversal of gonad development.
E. superba is considered a
key species of the Antarctic ecosystem. As a dominant
herbivore, it channels the organic matter produced by
the phytoplankton to a greater variety of dominant
components of the Antarctic biota. Baleen whales, seals,
fishes, birds and cephalopods are among the largest
krill predators.
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| Size |
| Maximum: 6.2 cm total length. |
| Interest to Fisheries |
| Total production for Euphausia superba. | Total capture for Euphausia superba. |
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Estimates (1985) of total krill biomass
range between 125 and 750 t. These estimates present
great variation due to spatial and temporal variation in
krill distribution and methods used. However, data
analysis of krill biomass using acoustics during a
recent multiship survey in the Indian Ocean and Western
Atlantic sectors of the Southern Ocean indicate a
standing stock of only about 7 million mt for the area
surveyed, a figure much lower than expected. Estimates
of annual krill production are also widely variable,
ranging between 13 million to several billion t.
Exploratory fishing began in 1961-62 with a catch of 4 t
by the Former USSR. The total catch reached about 477
184 t in 1980, have had two falls in 1984 (128,218 t)
and 1994 (83 962 t) but has partially recovered in 1995
(118,714 t). Most commercial krill fishing is carried on
by Japan, Ukraine and Poland in area 48. The
krill-fishing operations are carried out with large
stern trawlers using successfully midwater trawls, side
trawls and conical nets. The maximum reported (up to
1985) catch rate was 35 t in 8 minutes by a German
trawler and daily catches of 200 to 300 t are reported
practicable. One of the factors limiting the increase of
catch rates is the rapid enzymatic breakdown and
tainting of the meat by the gut and liver, which
requires processing of the entire catch within 1 to 3
hours after capture. Protein in krill meat amounts to 8
to 20% of wet weight (40 to 80% of dry weight). When
fresh, krill has too strong a taste for direct
consumption and when dehydrated it is bland with a
characteristic after-taste and odour. The total catch
reported for this species to FAO for 1999 was 103 318 t.
The countries with the largest catches were Japan (71
318 t) and Poland (18 554 t).
Krill is mainly processed into a variety
of products for direct human consumption (paste, frozen
tails, sticks, etc.), and for animal feeds, or used as
bait for sports fishermen (dehydrated or frozen). Many
economic factors constraining this new fishery are
expected to be solved, assuming a permissible catch of
several million tons a year. It is nevertheless accepted
that the scientific basis for management of this fishery
is weak and further information on the behaviour of this
species and fishing statistics are badly needed.
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| Source of Information |
| D.Lloris, Recursos Marinos Renovables, ICM. |
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