AMLR 2004 Weekly Report No. 3
1. Our current position is approximately 30 miles south of
2. Krill, salps and other
zooplankton. Over 4000 krill (Euphausia
superba) have been collected in 31 of 49 total Elephant Island Area samples.
Overall abundance so far is ca. 4 times greater than that in the West Area. The
overwhelming majority of krill (90%) are longer than 35 mm and represent the
highly successful 2000-2001 and 2001-2002 year classes. Males and females are
equally represented. About half of the mature females have mated and
demonstrate ovarian development (stage 3C). This, in conjunction with
relatively small concentrations of early larval stages, indicates that peak
seasonal spawning has not yet occurred. As in the West Area, the paucity of
small juvenile and immature sizes suggests minimal recruitment success from
last year's (2002-2003) spawn. As in the West Area, copepods and the salp, Salpa Thompsoni, have similar abundance and numerically
dominate the zooplankton assemblage. Metridia gerlachei, a coastal species, represents about half of
the copepods so far collected in this area. Post larvae of the euphausiid,
Thysanoessa macrura,
follow copepods and salps in overall abundance. The
high latitude salp, Ihlea racovitzai, is regularly collected near
the island shelf break zones and may indicate the presence of westward flowing
slope water.
3. Krill biomass and dispersion. Mean krill biomass
density in the West Area was 26 g m-2, similar to last year's
estimate for this stratum of 27 g m-2. Krill were not as evenly
distributed as last year with highest densities in the western portion of the
West Area along the shelf break near
4. Phytoplankton. Phytoplankton concentrations in the
West area averaged 0.3 +/- 0.4 mg chl-a m-3 for 5 m samples (31 +/- 20 mg m-2
for chl-a concentrations integrated through the water
column to 100 m). Chl-a concentrations
were higher within the shelf and shelf-break region (0.5 +/- 0.5 mg m-3
and 42 +/- 24 mg m-2) compared with pelagic stations (0.2 +/- 0.3 mg
m-3 and 25 +/- 15 mg m-2) for 5 meter and integrated values,
respectively. These concentrations are slightly lower than historical
(1997-2003) values of 1.1 +/- 0.9 and 0.4 +/- 0.5 mg chl-a
m-3 for 5 m concentrations (50 +/- 36 and 30 +/- 25 mg m-2
for chl-a integrated to 100 m) for shelf/shelf break
and pelagic waters, respectively. Satellite imagery (Modis
Aqua) revealed bloom development along the northwestern coasts of the
5. Oceanography and meteorology. 45 CTD stations were
occupied in the West and Elephant Island Areas. According to the Water Zone Classification
table, there was a less clearly defined distinction of the classical Water Zone
1 (ACW) type waters on the offshore stations in the West Area, than in previous
years. Many stations in this area displayed a mixing of Water Zone 1 and 2
waters. This mixing was also evident in many of the shallower inshore stations,
to the north of the islands, where the distinctions between Water Zones 2, 3
and 4 were not as distinct as in previous years. The 200 m horizontal
temperature plot showed the intrusion of <0ēC water between King George and
6. The instrument buoy moored off
7. Predator diet studies. 35 milk samples have been
processed for lipid extraction. Transterification
will be performed at the SWFSC in March. To date, 5 Gymnoscopalus braui and 15 Electrona
8. Bird and marine mammal observations. As of January
25, We have conducted 57 transits between stations. 18
species of seabirds were recorded in the West Area,
and 24 in the Elephant Island Area. Blue Petrels and Antarctic Prions were very common during transits over the South
Shetland Trough and in offshore waters over the Shackleton
Fracture Zone. These species, which are usually more abundant in proximity to
the convergence zone in the
Submitted by Roger
Hewitt