Distribution,Abundance and population structure of the Antarctic krill (Euphausia superba Dana) in the Prydz Bay region,Antarctica

Summary This paper presents results of net sampling carried out on four marine science cruises, between 1981 and 1985, in the Prydz Bay region of Antarctica by the Australian Antarctic Division. Krill exhibited a patchy distribution and overall low abundance. The majority of sampling sites in January 1985 returned no post-larval krill or densities of <1 individual 1000 m^-3. The estimated mean abundance of E. superba in January 1985 was 6 individuals or 2 g (wet wt.) 1000 m^-3 integrated for the upper 200 m of the water column which represented 3.4% of the total zooplankton biomass. No more than five years-groups, including the larvae, were observed in Prydz Bay, with mean lengths of groups 1+, 2+, 3+ and 4+ being 24, 38, 46 and 53 mm (standard 1), respectively in the middle of January. A high proportion of naupliar stages observed in January 1985 indicated that spawning in Prydz Bay begins in January and examination of adult maturation showed that the spawning continues at least to March.     

Abundance and distribution of early life stages of krill around Iceland during spring

Abundance, distribution and development of early life stages of krill (eggs, nauplii, calyptopes and furciliae) around Iceland were studied during the latter half of May 2013. Multivariate analyses were used to examine the relationships between water mass characteristics and phytoplankton spring bloom dynamics and distribution of krill. The results show that krill eggs, nauplii and calyptopes were most abundant over the shelf edges off the southwest and east coasts, while furciliae were most abundant on the shelf off the southwest coast. Meganyctiphanes norvegica and Thysanoessa longicaudata larvae were found mainly in the southwest, while T. inermis larvae were found in highest numbers on the east coast. Redundancy analysis showed that phytoplankton biomass, temperature and bottom depth explained 41% of the distribution pattern of early ontogenetic krill stages. In areas where krill eggs and larvae were most abundant (off the southwest coast), the phytoplankton spring bloom was in an advanced state, and the phytoplankton biomass and temperature were particularly high.     

Development of eggs of Antarctic krillEuphausia superba in relation to pressure

Summary This paper focuses upon the influence of increasing hydrostatic pressure on the development of krill eggs at 2°C. This experimental study on the embryology ofEuphausia superba was conducted at the Palmer Station, Antarctica during the 1982–1983 austral summer. The gravid females were captured from Bransfield Strait aboard theR/V Hero. The various embryological stages such as early cleavage, blastula, gastrula and limb-bud nauplius larva were defined and described. The duration for these various developmental stages at 1 atm was also established at +2°C and compared with the timing of this event at negative temperature. Krill embryonic development is inhibited at 4°C. The sinking rate of eggs and embryos was also measured at various pressure. The data suggest that pressure does not significantly influence the sinking rate. There appears to be a wide variation of sinking rates of eggs within the same brood. based on a simulated model of sinking rate, egg development was studied at increasing pressure. Pressure of 5–20 atm accelerates the rate of cleavage and therefore the 32-celled stage is attained within 5–8 h, while at 1 atm it took 13 h to reach the same stage. Pressure thus seems to have some influence on the duration of the development of different developmental stages of krill embryos.     

Dominance of microflagellates over diatoms in the Antarctic areas of deep vertical mixing and krill concentrations

Phytoplankton data obtained during six summer Polish expeditionsto the Antarctic Peninsula area, are compared with concurrentlyrecorded data on water column stabilities and krill abundance.The results show that flagellates (1.5–20 µm) arenumerically dominant over diatoms in the areas of deep verticalmixing and/or extensive krill concentrations. Of 102 stationsdominated by flagellates, 85 (83.3%) are located in a well mixedwater column (>100 m) and correspond to a mean krill densityof 15–346 t Nm^–2. In the same areas, estimated flagellatecarbon biomass exceeds diatom carbon. On the other hand, ofthe 40 stations dominated by diatoms, 36 (90%) are located inareas of increased water column stability (upper mixed layerof 10–50 m) and correspond to a low mean krill biomassof 0.34–4.6 t Nm^–2. Positive correlations of flagellateto diatom (F:D) cell number ratios with the depth of the uppermixed layer suggest light limitation of diatom growth and anincreased sinking rate of diatoms relative to flagellates inthe areas of deep vertical mixing. The relationship of the F:Dratio with krill abundance suggests that krill prefer feedingon diatoms and are less efficient in grazing particles of thesize of microflagellates (<20 µm). Flagellates exceeddiatoms in an unstable water column when the phytoplankton populationsare low; both algal groups increase in numbers with growingstability. The results provide field evidence that deep verticalmixing and krill grazing create conditions for the dominanceof flagellates over diatoms. Both factors acting together arelikely to suppress diatom blooms in the Antarctic.     

Production and supply of larvae as determinants of zonation in a brooding tropical coral

Production and settlement of planktonic larvae of the coral Favia fragum (Esper) were studied. The species is restricted to shallow back- and fore-reef habitats throughout the Caribbean Sea. Adults are in their greatest abundance on the reef-crest and shallow reef slope (<3 m) at Tague Bay, St. Croix, in the US Virgin Islands. Because F. fragum broods larvae that are capable of immediate settlement, this distribution pattern may be due to variation in fecundity among depths. Corals were collected from shallow (1.0 m) and deep depths (10-13 m) and cultured in individual containers exposed to shaded ambient light. Corals from shallow depths had greater fecundity (polyp⁻¹ lunar cycle⁻¹) and were larger than deep corals. To test the hypothesis that fecundity was related to successful fertilization, corals were kept in different densities in an area with sea-grass, where there were no natural adults. Production of larvae 6 months later was not affected by density of adults, possibly due to self-fertilization. Larval choice of habitat was also examined. In the laboratory, twice as many larvae settled on coral rubble fragments collected from depths where adults were common (1.5 and 3 m) than on those from depths where adults were rare (10 m). Larval supply may establish the vertical distribution of adults on St. Croix.     

The parachute function of the hull in eggs of Mopalia kennerleyi (Chitonida: Mopaliidae), and swimming of its larvae through ontogeny

Free‐spawning species of chitons produce eggs enclosed in a coating known as the hull. In Chitonida, several studies have shown that the hull helps to direct sperm to specific areas of the egg surface, facilitating fertilization. One study has found evidence that this structure also serves to reduce the sinking rates of the eggs. To clarify how the presence of the hull modifies sinking rates in chiton eggs, here we compare sinking speeds and densities of eggs of Mopalia kennerleyi with and without the hull. Sinking rates of eggs with the hull were approximately one‐third of those without it. This structure acts as a flotation device because it has a density very close to that of seawater, and it increases the effective diameter and therefore the drag on the negatively buoyant egg. Since there is limited knowledge about morphology and behavior of chiton larvae, we also analyzed changes during ontogeny in behavior, swimming speeds, and body shape of larvae of M. kennerleyi. Over time, the larvae decreased their upward swimming tendency and preferred to stay near the bottom, and their bodies became elongated and dorso‐ventrally compressed. These changes may be related to preparation for settlement and metamorphosis. Further studies of these subjects are required in chitons, since movement of early stages, as eggs/embryos sinking or larvae swimming in the water column, may affect their survival.     

Recolonisation of four small streams in central Scotland following drought conditions in 1984

Four streams in the Loch Ard Forest in central Scotland dried out almost completely during a drought in the summer of 1984. The recovery of the invertebrate populations in the streams was studied from September 1984 until March 1985 when most of the insect larvae and nymphs were almost full-grown.The appearance of very small larvae belonging to several insect orders within a month of the streams' filling up suggests that they had survived the drought as eggs, or eggs had been laid by adults soon after the drought ended.Statistical analysis showed that with the exception of 3 taxa there was no significant difference between the numbers of animals in November 1984 samples and in samples collected in March 1985.Comparison of samples from March 1984 and March 1985 showed significant difference in population size for a few species; with 2 exceptions the 1984 samples (ie before drought) were larger. In the long term the overall effect of the drought on the invertebrate communities seems to have been limited.     

Variability of Euphausia superba populations near Elephant Island and the South Shetlands: 1981 vs. 1984

Summary March 1981 and 1984 Euphausia superba populations were compared using acoustics and net catches near Elephant Island, the South Shetlands, and in the Bransfield Strait. In 1981, krill tended to form large, thick swarms and in 1984, smaller, more dispersed, shallower patches. March body lengths of juvenile-adult krill were 22–59 mm in 1981 and 13–59 mm in 1984. Near Elephant I. in 1981, krill >45 mm were most numerous; in 1984 sizes <45 mm were dominant. In March 1984, the larger (>45 mm) body-size group was prereproductive and occurred from just west of Elephant I. westward into waters north of the South Shetlands; in 1981 the larger krill were postreproductive and more widely distributed in the Elephant I. area. Overall, netted postlarval krill, 1981 vs. 1984, averaged 73 vs. 48 individuals/m², or 54 vs. 16 g/m²; acoustic biomass estimates were 229 vs. 134–201 g/m². Larvae near Elephant I. averaged >2000/m² in 1981 vs. <1/m² in 1984—compatible with respective March reproductive states. Net-type comparisons revealed short-term (15 min to 6h) variability of a similar scale in both MOCNESS and bongo net catches, but bongo abundances averaged greater. Variation in maturity composition across 1981 swarms, patches, and random transects was like variation among the random 1984 tows; spatial distributions were more heterogeneous in 1984. The March 1984 krill of 20–44 mm (Year-2, mode 34 mm) relate to November 1983 krill of 9–30 mm (mode 21 mm), indicating growth averaging 12 mm during the season. Body-lengths and size-frequency modes of Year-2 and combined Years-3,3+ krill from comparable Feb-Mar data collected since 1968 suggest trends between times when (1) Year-2 krill average small and peak reproduction seems to be late in the season and/or weak (1979, 1982–1984), and (2) Year-2 krill are larger, and reproduction is possibly earlier and more successful (1976, 1980, 1981).     

Developmental defects in pelagic fish embryos from the western Baltic

In February/March 1983 and 1984 a survey of pelagic fish eggs was conducted in the western Baltic (Kiel Bight), employing a horizontally towed plankton net (1 m Ø and 300 μm mesh). Maximum egg numbers in the upper meter of the S=21×10^?3 salinity layer were 200·100 m^?3. The most abundant eggs were cod (up to 142 eggs·100 m^?3), followed by plaice (up to 74 eggs·100 m^?3) and flounder (20 eggs·100 m^?3). A considerable percentage of embryos of all species displayed aberrant development. In 1983 18% of cod, 22% of flounder and 24% of plaice eggs caught contained defective embryos; in 1984 this number was larger, ranging from 28% in plaice over 32% in cod to 44% in flounder. Early developmental stages showed the highest malformation rates (up to 51% in the case of early flounder embryos). With progressive development, malformations decreased in numbers, being lowest prior to hatching. Highest rates of malformations were recorded in the Mecklenburg Bight in 1983. A second area with high incidence of malformation rates was located south and east of the island of Langeland. Several reasons, including environmental and anthropogenic factors, for the occurrence of malformed embryos in pelagic fish eggs are discussed. The potential of malformation rates in embryos of pelagic fish eggs as a tool for monitoring is considered.     

Abundance and daytime vertical distribution of planktonic fish larvae in an oligotrophic South Island lake

The vertical distribution of common bully (Gobiomorphus cotidianus) and koaro (Galaxias brevipinnis) larvae in the limnetic zone of Lake Coleridge were determined using a high-frequency (200 KHz) echosounder. Planktonic bully larvae first appeared in appreciable numbers in January. By February, they formed a scattering layer between depths of 12 to 24 m during the day, where they achieved a maximum density of 0.59 fish m^-3. Larger (> 18mm) fish migrated to the littoral zone and densities declined to < 0.01 fish m^-3 by July, when remaining larval fish occupied greater daytime depths. Their vertical distribution during the day appeared to be influenced mainly by light levels and water temperatures. Larvae grew more slowly (0.12 mm d^-1) than in more productive North Island lakes, and were also present in lower densities for a more restricted period of time. Koaro larvae first appeared in November and December and were found in low numbers (< 0.01 fish m^-3) in summer at depths of 10 to 26 m. Salmonid production in the limnetic zone is probably limited by the small size and relative scarcity of forage fish present.     

Postembryonic development of Nymphon unguiculatum Hodgson 1915 (Pycnogonida, Nymphonidae) from the South Shetland Islands (Antarctica)

Male specimens of the sea spider species Nymphon unguiculatum, carrying eggs, larvae and postlarvae in various stages of development, were collected off the South Shetland Island at water depths between 112 and 472 m in austral summer 2006/2007. Here, we describe the external morphology of four postembryonic stages (protonymphon, instar 1, instar 2, and instar 3) carried by these specimens. We found that (1) protonymphon larvae hatch from the eggs; (2) larvae and postlarval stages have yolk reserves and are characterized by a relatively large size (average body lengths of 0.46, 0.55, 0.65 and 0.73 mm in the successive stages); (3) postlarvae remain on the ovigerous legs of males during several moults; (4) a spinning apparatus is present; (5) the development of walking legs is sequential. The larval and postlarval development of N. unguiculatum is compared with that known from other pycnogonid species.     

Size and stage composition of age class 0 Antarctic krill (<Emphasis Type="Italic">Euphausia superba</Emphasis>) in the ice–water interface layer during winter/early spring

The condition and survival of Antarctic krill (Euphausia superba) strongly depends on sea ice conditions during winter. How krill utilize sea ice depends on several factors such as region and developmental stage. A comprehensive understanding of sea ice habitat use by krill, however, remains largely unknown. The aim of this study was to improve the understanding of the krill’s interaction with the sea ice habitat during winter/early spring by conducting large-scale sampling of the ice–water interface (0–2 m) and comparing the size and developmental stage composition of krill with the pelagic population (0–500 m). Results show that the population in the northern Weddell Sea consisted mainly of krill that were <1 year old (age class 0; AC0), and that it was comprised of multiple cohorts. Size per developmental stage differed spatially, indicating that the krill likely were advected from various origins. The size distribution of krill differed between the two depth strata sampled. Larval stages with a relatively small size (mean 7–8 mm) dominated the upper two metre layer of the water column, while larger larvae and AC0 juveniles (mean 14–15 mm) were proportionally more abundant in the 0- to 500-m stratum. Our results show that, as krill mature, their vertical distribution and utilization of the sea ice appear to change gradually. This could be the result of changes in physiology and/or behaviour, as, e.g., the krill’s energy demand and swimming capacity increase with size and age. The degree of sea ice association will have an effect on large-scale spatial distribution patterns of AC0 krill and on predictions of the consequences of sea ice decline on their survival over winter.     

Structural Changes of Yolk Platelets and Related Organelles during Development of the Newt Embryo

Structural changes in yolk platelets and related organelles in the cytoplasm of the presumptive ectodermal region up to the stage of gastrulation were studied by light and electron microscopies using full-grown oocytes, mature eggs descending the oviduct and embryos of the newt, Cynops pyrrhogaster . Yolk platelets with a superficial layer are first observed in mature eggs descending the oviduct. During the cleavage and early morula stages, the superficial layer increases in thickness and the main bodies become more slender. The superficial layer decreases in thickness in the blastula stage, and many yolk platelets lose this layer in the gastrula stage.
The amount of rough-surfaced endoplasmic reticulum (r-ER) increases rapidly in the morula stage, while Golgi complexes gradually increase in number between the cleavage and gastrula stages. In the cleavage and early morula stages, most of the r-ER is closely adherent to yolk platelets and is associated with several mitochondria. Two types of free vesicles, large (0.5–4.0 μm diameter) and small (0.15–0.3 μm diameter), were seen in abundance from the early morula stage to the early gastrula stages.
Changes in the structure of yolk platelets are discussed in relation to changes in other cytoplsmic organelles.     

Distribution of Japanese temperate bass, <Emphasis Type="Italic">Lateolabrax japonicus</Emphasis>, eggs and pelagic larvae in Ariake Bay

We collected eggs and larvae of the Japanese temperate bass, Lateolabrax japonicus, and present horizontal and temporal changes of distribution relative to development and growth during the species pelagic life history in Ariake Bay. Sampling was conducted from the inner to central region (11 sampling stations) of Ariake Bay using a plankton net (80 cm diameter, 0.5-mm mesh) from November 2000 to February 2001. Both eggs and larvae were collected most abundantly in mid-December. The CPUE of eggs in the surface layer was higher than the middle layer, which is in contrast to that at the larval stage. Most eggs were collected around the central and western regions of the bay. The distribution of eggs shifted vertically to the middle layer with development. Yolk-sac larvae were collected in the central region of the bay, and preflexion and flexion larvae were more abundantly collected in the inner region of the bay. The body length of larvae around the inner bay was larger than in the central region. The pelagic life history can be summarized as follows: eggs are distributed around the central region of the bay and eggs and larvae expand their distribution to the inner and shallower waters with growth. We conclude that the shift of vertical distribution in pelagic stages and the hydrographic features of the middle layer form one of the mechanisms enabling the inshore migration of L. japonicus.     

Nutritional condition and vertical distribution of Baltic cod larvae

Newly hatched Baltic cod Gadus morhua larvae are typically found at depths >60 m. This is a region of low light and prey availability, hence generating the hypothesis that larvae have to migrate from hatching depth to the surface layer to avoid starvation and improve their nutritional condition. To test this hypothesis, Baltic cod larvae were sampled during the spawning seasons of 1994 and 1995 with depth-resolving multiple opening/closing nets. Each larva was aged by otolith readings and its RNA/DNA ratio was determined as a measure of nutritional condition. The RNA/DNA ratios of these larvae aged 2-25 days (median 10 days) ranged from 0.4 to 6.2, corresponding to levels exhibited by starving and fast-growing larvae in laboratory calibration studies (starvation, protein growth rate, G_pi= -12.2% day⁻¹; fastgrowing larvae, G_pi=14.1%day⁻¹) respectively. Seventy per cent of the field caught larvae had RNA/DNA ratios between the mean values found for starving and fed laboratory larvae. Only larvae aged 8-11 days had higher mean RNA/DNA ratios above 45 m than below ( t -test, P<0.05). However, the instantaneous protein growth rates were significantly higher for all larval age groups in the surface layers ( t -test, P<0.05). Starving larvae were found in all depths sampled (10-85 m), whereas growing larvae (positive G_pi) were restricted to samples taken shallower than 45 m. These superior growth rates above 45 m corroborate the hypothesis and imply that migration to the shallow water layers is a prerequisite for good nutritional condition, growth and survival of Baltic cod larvae. The frequent occurrence of cod larvae older than 8 days in the deep water in poor condition suggests that a proportion of the larvae will die from Starvation in the deep layers of the Baltic Sea.     

Ontogenic phototactic behaviors of larval stages in intertidal barnacles

Hydrobiologia - During larval development of the intertidal barnacle Fistulobalanus albicostatus, larvae in the naupliar stages I and II (NI&amp;II) possess a single naupliar eye, and later...     

Vertical distribution of eggs and larvae of the Baltic Sprat <Emphasis Type="Italic">Sprattus sprattus balticus</Emphasis> (Clupeidae) in relation to seasonal and diurnal variation

Vertical distribution of eggs and larvae of the Baltic sprat Sprattus sprattus balticus was studied. Diurnal variation was revealed in the distribution of eggs of the first stage of development and larvae with a length of more than 5 mm, which is related to dynamics of spawning and vertical migrations of sprat larvae. Seasonal variation in the distribution of eggs manifested itself in: (1) widening of the range of occurrence from the zone of halocline at the beginning of spawning (winter) to the entire water column in spring-summer and (2) emergence in the surface layer in July of all stages of egg development unlike the presence from May to June mainly of the first stage of development. It is suggested that the ability of early ontogenetic stages of sprat to maintain in the surface layer depended on the extent of development of vertical gradients of density in the thermocline.     

Krill diet affects faecal string settling

Summary Free-floating sediment traps used on a transect from Scotia Sea to Weddell Sea collected larger, more degraded, krill faecal strings in the deeper (150 m) than in the 50 or 75 m traps. The smallest faecal strings were only present in the shallower traps. Sinking velocity of smaller faecal strings was — as expected — much lower than for larger ones, with a total range of 50 to 800 m · day ^–1 for faecal string volumes of 0.007 to 0.53 mm³. Krill feeding largely on diatoms produced faeces with higher settling velocity than those feeding on non-diatom phytoplankton. Smaller krill faecal strings do not leave the upper mixed layer. Potential settling velocities as measured in settling tubes (without turbulence), may in this respect be misleading. Small oval faecal pellets of unknown origin showed relatively high settling velocities (80 to 250 m·day^–1 for 0.002 to 0.013 mm³) due to higher compaction and lower form resistance to sinking.Data presented here were collected during the European Polarstern Study (EPOS) sponsored by the European Science Foundation     

Seabird and fur seal responses to vertically migrating winter krill swarms in Antarctica

Summary The foraging behaviour of fur seals and two species of surface feeding seabirds was observed over swarms of vertically migrating krill along the Antarctic Peninsula in July 1987. Fur Seal haul out patterns were correlated with krill in the upper 30 m of the water column. Krill moved to the surface at night; seals subsequently foraged from 1400-0700 hours before returning to floes. Foraging was continuous through the night. Dive duration decreased as krill moved up to the surface; shorter dives may have been more successful than longer ones. It is possible that very deep dives, which occur early in a foraging bout, represent more of an attempt to assess krill depth and distribution rather than being a genuine foraging effort. Seabirds responded to the presence of a surface krill swarm by circling over it and foraging; krill at depths greater than 30 m elicited directional flight and low frequencies of prey capture attempts. Both Snow Petrels and Antarctic Terns preyed on krill, but each species approached the swarms from different habitats. Snow Petrels primarily overflew areas covered by ice; terns preferred open water. This suggested that prey encounters are essentially opportunistic, although the search for prey is limited to rather specific marine habitats. This feature may be important to our understanding of the factors that determine the pelagic distribution of seabirds.     

Working with living krill – the people and the places

The fascination of Antarctic scientists with Antarctic krill and their capabilities has a long and varied history, and prompted many scientists to maintain and manipulate krill under laboratory conditions. Starting in the Discovery era with Mackintosh at the King Edward Point labs on South Georgia, 1930, scientists have collected krill from sailing vessels, small boats, inflatable zodiacs and large ice-breaking vessels. Krill have been maintained in small and large jars, deep rectangular tanks, large round tanks and in flow-through and recycling systems. They have been maintained both on board research vessels and in laboratories, in flowing seawater systems at ambient conditions and in temperature-controlled environmental rooms. A few researchers have transported living krill back to their home laboratories, for example tropical laboratories in Japan (Murano) and Australia (Ikeda), temperate laboratories (Nicol) in Australia, a northern European laboratory in Germany (Marschall) and a sunny maritime laboratory in California (Ross and Quetin). The goals have been varied: short-term experiments to understand in situ physiological rates, long-term experiments to test the effects of manipulations or controlled changes in environmental conditions, and behavioral responses. We take you on a brief historical tour as we trace the lineage of modern day research on living Antarctic krill.