AMLR
2007 Weekly Report No. 3
1. Our current position is 30 nautical miles west of Elephant
Island. On Jan. 18th,
a raucous southerly storm forced the vessel to heave to delaying our large area
survey. But the weather and sea state currently is on our side. The West Area
was finished January 19th. All major equipment is functioning.
2. Krill, salps and other
zooplankton. Postlarval
krill were present in 21 of 23 West Area samples with a slightly greater
frequency of occurrence than in the South Area (91% vs. 85% of samples). While the overall mean was a third of that in
the South (43 vs. 159 individuals per 1000 m3) the median catch
sizes in the two areas were similar (18 vs. 21 per 1000 m3). Greatest concentrations of 240-770
individuals (110-292 per 1000 m3) were located over the inner
shelves of Greenwich and King George Islands.
The krill length range of 19-58 mm was also similar to that
in the South Area however the length-frequency distributions differed greatly. Whereas in the South Area lengths were
centered around a 26 mm mode in the West they
exhibited a bimodal distribution about primary and secondary modes of 50 mm and
31 mm, respectively. Accordingly large mature forms dominated, comprising 61%
of the total catch, while juveniles made up only 29% as compared to 82% in the South. Intermediate sized immature forms made up the
same proportions (10%) in both areas.
Males outnumbered females by a ratio of 1.7:1 with 36% of
the catch represented by reproductively mature male stages. Reproductively mature females comprised 25%
of the catch, with the majority of individuals (16% of total) having recently
mated as indicated by attached spermatophore packets
with no obvious ovarian development. Individuals
with developing ovaries made up another 5% of the total. The proportion of
mature females in advanced maturity stages (29% with developing ovaries, gravid
and spent) was relatively low suggesting a slightly delayed seasonal spawning
effort. This is supported by the limited
occurrence (4 samples) and low mean abundance (1 per 1000 m3) of
larval krill in the area.
The zooplankton samples were numerically dominated by
copepods which had mean and median abundance values of 1400 and 580 individuals
per 1000 m3. Elevated copepod
concentrations were distributed across the entire West Area but with maximum
values (1000-5000 per 1000 m3) associated with oceanic water
offshore of and over the outer island shelves.
Larvae of the coastal euphausiids species Thysanoessa macrura and aggregate
stages of the salp Salpa thompsoni followed copepods in overall
mean abundance (430 and 400 per 1000 m3). Greatest concentrations of
these were both located in oceanic water offshore of Livingston
Island. While larval T. macrura
were broadly distributed across the rest of the West Area the distribution of Salpa thompsoni
demonstrated an obvious association with the ACC as salps
were virtually absent from any other water types represented here.
3. Krill biomass and dispersion. Preliminary acoustically
derived biomass estimates from the southern and western areas have been calculated
this week. Biomass in the Southern Zone, in Bransfield Strait, was calculated as more than 500 000 tons. Within the West
zone, more than 3.5 million tons of krill were estimated acoustically. Mean
densities of krill in the West area were very high, exceeding 90 g/m2.
This estimate is using the SDWBA method and the krill length delineation, a
different method than last year. This is
also using day and night data; final analysis will only include day time krill estimates
due to diurnal migration. These estimates continue to support the data
collected using nets that there has been a very large recruitment event in the South Shetland Islands.
4. Phytoplankton. As of midnight, 1/21/07, 31 more
stations were sampled and analyzed for chlorophyll (5-200 m; total of 50
stations); 23 stations were sampled for macronutrient profiles (10-200 m), plus
20 other stations at 30 m; six stations were sampled for trace elements (including
dissolved and particulate Fe); one trace metal clean incubation was initiated. Phaeopigments concentrations were ~20% those of chlorophyll
(r2 = 0.86). In the Bransfield Strait, highest chlorophyll
concentrations were found in the upper 50 meters above the pycnocline
south of the Shetland Islands (concentrations 1.0-1.5 mg CHL m-3)
and lowest along the Peninsular shelf (0.7 - 1.0 mg CHL m-3). North
of the Shetland Islands, chlorophyll concentrations were highest along the
shelf-break in the upper mixed layer of ~ 30-50 meter depth (1.0 - >2.0 mg
CHL m-3), lowest in the pelagic waters of the Antarctic Circumpolar
Current with a pycnocline of ~50 m depth (0.06 - 0.2
mg CHL m-3). In the coastal shelves on the Drake Passage
side of the Shetland Islands, chlorophyll concentrations were moderate (0.7 - 2 mg CHL
m-3). In the Elephant Island Area, only line 09 has been processed to
date. Low chlorophyll concentrations in surface waters found in pelagic waters,
and blooms >2 mg CHL m-3 in the shelf and shelf-break areas. Deep
chlorophyll maximums were found only at ~50% of stations where expected, being
Station #s 1505, 1406, 1101, 0904, 0903, and 0902. Some of these stations had
maximal concentrations at >100 m.
Bio-Optical Sampling. The Integrated Optics Package (IOP) and the Profiling
Reflectance Radiometer system (PRR) have been deployed at 9 mid day CTD
stations; complementary water samples were also taken at the mid day
stations. HPLC pigment samples have been
collected at a total of 24 stations at surface and 75 m. 18 photosynthesis vs. irradiance
(PvsE) experiments have been run and analyzed,
45 particulate absorption (ap/ad) and dissolved
material absorption (as) samples have been analyzed, 49 HPLC pigment samples
and 45 particulate CHN samples have been collected.
So far, 84 samples were collected from 11 stations for
determination of total and dissolved Fe. Besides iron, samples were collected
at the same stations for determination of bacterial number and diversities, phytoplankton
(fixed in formalin), DOC, POC and nitrate reductase.
A deck incubation experiment was started in order to test the effect of Fe and
light on the water collected from a DCM depth in two different light regimes
(50% and 5% of incident light).
5. Oceanography and meteorology. A Southeaster, averaging 30 knots and peaking
at 50 knots, accompanied rough seas from Wednesday to Friday. A swing to a 25
to 30 knot Northwester on Friday saw a continuation of the rough seas until
Sunday. 39 CTD stations were completed across the West and Elephant Island Area
with 2 stations having to be abandoned due to rough seas. The CTD hardware was
swapped with the spare system while faultfinding intermittent communications
and bottle triggering problems. The problem was traced to an earth leakage in
the braid of the new coaxial sea cable being used. The braid was disconnected
and the CTD grounded on the cable’s outer steel armor. Dissolved oxygen data
was lost on Station A07-02 when a connector leaked. The predominant water type
in the West Area was well defined Water Zone 1 (ACW) zones at the deep offshore
stations, Water Zone 2 stations along the shelf break, and on the shelf itself,
north of the islands.
6. Ocean acidification. We have collected water for the determination
of dissolved inorganic carbon along several transects on the west area, and
will continue to collect samples within the Elephant Island area. The storm
that occurred over the last week required a change in deployment strategy, as
several stations along one transect were not sampled. Seven casts have been
made on the shelf and in ACC waters and we will collect water from two more ACC
like and two more shelf locations around Elephant
Island. Ten percent of the bottles will be used as replicates. We
have preserved pteropods from all areas of the Bransfield Strait and we will continue to collect and preserve samples from Elephant
7. Predator diet studies. Lipids have been extracted
from 44 Antarctic fur seal milk samples. At the commencement of the nearshore survey, more milk samples will be arriving
onboard on
8. Seabird and mammal observations. Data on the distribution, abundance and
behavior of seabirds and mammals was collected during underway ship operations
in the West Area. Twenty-four transects were collected totaling approximately
530 nautical miles of survey effort. Seabird
community composition was concordant with previous AMLR surveys. The community consisted primarily of Cape Petrels, Black- browed Albatrosses, Gray-headed Albatrosses, Giant
Petrels, Blue Petrels, Antarctic Prions,
Black-bellied Storm Petrels, Wandering Albatrosses, Light-mantled Sooty
Albatrosses and Chinstrap Penguins.
Cape Petrels were the most conspicuous avian predator and were observed
feeding throughout the West Area. The
numbers of Cape Petrels observed in West Area are the highest ever recorded during
an AMLR survey. However, the majority of
Cape Petrels were observed on 2 transits in a few dense
aggregations. On transit to stations
12.08 and 11.07, there were numerous feeding frenzies, which coincided with large
densities of krill collected during net sampling. At these locations, krill were actively
mating and spawning (Per. Comms. V. Loeb). To determine what feeding petrels were
probably consuming, a Manta net was towed along side the vessel to sample
surface plankton. Krill, pteropods, amphipods and
copepods were present in net samples.
Other interesting bird sightings include 1 Arctic Tern and
1 Antarctic Petrel.
Humpback Whales were the most common cetaceans in the West
Area. We collected 38 sightings of
Humpback Whales. Group size was
typically 2 to 3 whales. In addition, Minke Whales, Fin Whales and Southern Bottlenose Whales
were observed.
A. Jenkins sends.