AMLR 2002 Weekly
Report No. 4
3 February 2002
1. Current position is just off the east end of Elephant
Island at Cape
Valentine. The survey of
bio-oceanographic conditions in the South Shetland Islands
was finished this week with completion of the Joinville Island
and South Areas. Personnel from the Copacabana field camp (W. Trivelpiece) and the Cape Shirreff
field camp (R. Holt, M. Goebel and V. Vallejos) were
brought aboard to conduct a census of Antarctic fur seal pups throughout the
South Shetland Islands (see item 7).
2. Krill, salps and other
zooplankton. Post-larval krill were present in 75% of 95 survey samples. The largest catch, from the South area, contained
nearly 4000 individuals (1477 krill per 1000 m3). Other large catches (i.e., >1000 krill,
estimated 400-700 per 1000 m3) were taken in all areas. These concentrations were located north of Livingston
and King George
Islands (Drake Passage),
north of Joinville
Island (Bransfield
Strait) and northeast of Elephant
Island area. Abundance differences among the four areas
were not significant (ANOVA, P>>0.05 in all cases). Mean and median abundance in the Elephant
Island area (39 and 8 per 1000 m3,
respectively) were slightly higher than during the January 2001 survey (19 and
6 per 1000 m3). Juveniles, representing successful recruitment of
the 2000/2001 year class, dominated the krill catches in all four areas. Krill >32 mm were rare in the South and Joinville areas where juveniles constituted 88-93% of
individuals. Broader size ranges (16-60
mm) and more heterogeneous length-maturity stage compositions were represented
in the West and Elephant Island
areas. In the West area length distribution
was polymodal with peaks around 22, 25, 31, 36 and
53-55 mm modes; 57% were juveniles, 17% immature and 26% mature stages. Reproductively mature males (M3b) constituted
6% and females 20% of the total; 84% of these females were in advanced stages,
predominantly gravid (F3d). Small
juveniles (20-30 mm) made up 46% of the Elephant
Island catch. Older krill had lengths centered about a
41-42 mm mode and 20% of were >45 mm (i.e., >4 years old). Immature and mature stages comprised 9% and
45%, respectively. Females outnumbered
males by 60%; most of these females (92%) were in advanced stages indicating active
spawning in the area. The overall abundance
and size/maturity composition indicated:
extremely good proportional recruitment of the 2000/2001 year class;
essential absence of recruits from the 1999/2000 year class (2 year-old krill);
and markedly reduced numbers of krill from the highly successful 1995/1996 year
class. Krill larvae were present in 23% of the samples. Greatest concentrations were in the Elephant
Island area. The mean 36 per 1000 m3 was
essentially the same as observed during January 2001. Calyptopis stages
dominated, and resulted from spawning 30-45 days earlier (i.e., early to mid
December). These observations, along
with the adult spawning condition, indicate a normal spawning season and bode
well for recruitment success of the 2001/2002 year class.
Salpa thompsoni was
present in 88% of survey samples.
Abundance was greatest in the Elephant
Island (410 and 86 per 1000 m3)
and South (201 and 71 per 1000 m3) areas and lowest in the Joinville Island
area (184 and 2 per 1000 m3).
Aggregate (chain) forms constituted 98% of the overall catch. Presence of extremely large
aggregates indicate a particularly early onset of seasonal chain
production. Despite a prolonged
production period salp abundance in the Elephant
Island was relatively low,
suggesting that they were not being retained within the area during summer
2002.
Copepods numerically dominated the zooplankton in all four
areas. The primary constituents, in
order of abundance, were Calanoides acutus, Calanus propinquus and Metridia gerlachei. Greatest concentrations were in the West area
(25400 per 1000 m3 mean, 12500 per 1000 m3 median) associated
with the Oceanic influence. Mean and
median copepod abundance values in the Elephant
Island area were 1 to 2 orders of magnitude
larger than observed during previous January surveys. Larvae of the euphausiid
Thysanoessa macrura
comprised the second most abundant taxon
overall. Due to their predominantly
offshore distribution they also ranked second in abundance to copepods in West
and Elephant Island
areas. Postlarval T. macrura, having a predominantly
coastal distribution, ranked second in abundance to copepods in the South area.
The overall impression is of high
secondary production over much of the January 2002 survey area.
3. Krill biomass and dispersion. Upon completion of Survey
A, krill biomass densities were estimated as 10 to 28 g m-2, 19 to
40 g m-2, 7 g m-2, and 15 g m-2 for the West, Elephant
Island, Joinville Island,
and South areas, respectively. In comparison, biomass densities for the West, Elephant
Island, and South areas of 17 g m-2,
16 g m-2, and 13 g m-2 were estimated during Survey A of
2001. Greatest krill biomass densities are located halfway between King
George Island
and Elephant Island,
and north of Elephant Island. Other areas of high densities were the
regions northwest of King George
Island, north of Livingston
Island, and northwest of Snow
Island. These areas were consistently located along
the 500 m isobath.
The Joinville
Island area was relatively low in
krill abundance with respect to the West, Elephant
Island and South areas.
4. Phytoplankton. The pattern for surface chlorophyll
concentrations in the Bransfield Strait
and Joinville Island Area closely follows the types
of water, with low values found for Weddell Sea water
and high values for Bransfield Strait
water. 5m chlorophyll averages 0.84 +\- 0.78
mg m-3, and integrated (100 meters) averages 47 +\- 28 mg m-2
for the entire area (31 stations). The Bransfield Strait region closest to the
Shetland Islands (7 stations) averaged 1.89 +\- 1.00 mg chl
m-3 as compared to 0.36 +\- 0.27 mg chl m-3
for those stations closest to the peninsula (10 stations). The most phytoplankton rich area of the
entire first leg were for stations 11-11, 09-09 and 12-12 having highest 5 meter
chlorophyll concentrations of 3.2, 2.8 and 2.4 mg m-3, respectively.
The lowest chlorophyll concentrations of the first leg were found near the Weddell
Sea (Stations 02-13, 04-11, and 04-13), having 0.08 +\- 0.01 mg chl m-3. Upon completion of the survey grid, 100
high pressure liquid chromotography, 31 particulate
organic carbon, 101 particulate absorbance, and miscellaneous particulate
fluorescence and particulate size distribution samples of the water column were
collected for analysis at Scripps Institution of Oceanography. These samples
were in addition to 7 deployments of an integrated optics package, 31 casts of
a free-fall profiling radiometer, and 92 CTD casts that incorporated a fluorometer and both a blue and a red transmissometer.
5. Oceanography and meterology:
Overall, as in previous years, the southern part of the survey is mainly type
IV (Bransfield water) with an intrusion of type V (Weddell water) from the
south-east. The north-east axis through
the center of the survey (including the island chain) is dominated by
transition water (types 2 & 3 identified) meandering into the north. The
north-western area is influenced by Drake Passage water and
the southern boundary of the Antarctic Circumpolar Current (ACC). The presence of type I water is less clearly
defined with the characteristic winter water (WW) subsurface temperature
minimum not as pronounced nor as cold as the previous
season and at a slightly higher salinity.
Although the 1.8°C isotherm marking the southern boundary of the ACC
cuts through the survey area from west to north-east, meandering in the area NW
of Elephant island, the temperature-salinity (TS) curves from CTD casts north
of this are not conclusively type I and the tentative conclusion is that the
area surveyed north of the island archipelago is mainly transition water.
Moderate North Westerly to Westerly winds
(<20knts) for most of the week with some periods of stronger Easterlies (up
to 30 knts). Air temperatures were mostly
above 1°C, with a minimum of 0.5°C and a brief peak of 7°C. Overcast and foggy
days were interspersed by four partly cloudy days. The highest barometer
reading for trip so far was recorded this week, being 1007mbars.
6. Predator diet studies. Scats from weeks 1-4 have been
processed (38 scats and 3 regurgitations). In the regurgitation sample
processed this week, whole undigested krill were measured according to CCAMLR
Standard Length Measurement in addition to carapace measurements in order to ground-truth
the regression used to relate carapace size to body length. Prey samples of myctophid fish have been identified by species, measured for
Standard Length, weighed, and sex has been determined as well as stomach
fullness and contents. Each myctophid had their otoliths removed as a future identification guide. Samples
were then homogenized and frozen for further studies.
7. The 2002 Survey of South Shetlands
fur seal colonies began on 30 January.
The first census was of San Telmo Island, the
largest single colony in the survey, begun with the best of weather conditions.
Our weather held for two days and we were able to census Window
Island, Start Point and Cape
Smith (last surveyed in 1986/87), Desolation
Island, and the Fildes Peninsula,
King George
Island. On 1 Feb we landed at Stigant Point and tried to make a landing later in the day
at Turret Point on the south coast of King
George Island.
We chose to investigate Turret Point because of an anecdotal report of fur seal
pups there. If confirmed, Turret Point, King
George Island,
would be the first re-colonization of a south coast site in the South
Shetlands. Unfortunately,
our visit was cancelled due to high winds. Yesterday and today we surveyed the Seal
Island and Cape
Valentine group of colonies. Thus
far, most sites appear to be stable and have similar numbers of pups when
compared to previous surveys. The exceptions have been North Cove, Seal
Island and Cape
Lindsey, Elephant
Island, both of which had significant
reductions in total pups. However, two other satellite colonies at Seal
Island had modest increases.