Distributional ecology of milkfish,Chanos chanos,larvae in the Great Barrier Reef and Coral Sea near Lizard Island,Australia

Synopsis Plankton hauls captured 682 milkfish larvae (2.1–12.3 mm) in the Great Barrier Reef Lagoon and Coral Sea during 1979–1986. Larvae were present from November to March, and absent in April, July and October. We analyzed concentration, abundance and size-frequency data and concluded that spawning took place in the Coral Sea or at the outer edge of the continental shelf, apparently following an adult spawning migration of at least 50 km. Larvae then moved inshore to at least our most inshore routine sampling site near midshelf. Some larvae may have remained for a period in the lee of reefs along the shelf edge. Larvae apparently occupied the upper few metres of the water column, thereby becoming susceptible to shoreward movement in the wind-driven surface layer. Movement from spawning sites to midshelf probably required active maintenance of vertical position by larvae which enabled passive movement with favourable currents, and perhaps horizontal swimming. By the time larvae reach midshelf, continued inshore movement by horizontal swimming alone is possible.     

Early life history of Engraulicypris sardella (Cyprinidae) in Lake Malawi

Engrarulicypris sardella is the basis of an important artisanaland subsistence fishery in Lake Malawi. It is a small pelagiccyprinid growing to a maximum length of 13 cm and is the onlyfish species in the lake known to have pelagic larvae. Seasonalabundance and vertical distribution patterns of larvae wereinvestigated in the offshore pelagic zone from March 1992 toJanuary 1994. There was no evidence that E.sardella is a pelagicspawner. Growth rates were estimated by counting rings on theasteriscus otolith, and biomass and production calculated usinga length-dry weight regression relationship. Distinct seasonalpatterns were observed in the total numbers, biomass, production,and mortality, of larvae that were similar in both years ofsampling. Mortality of larvae was lowest from July to Decemberand highest from January to April. Mortality was, on average,higher in the south of the lake, and lower in the central andnorthern region. Low mortality of larvae coincided with thewindy mixed period when primary and secondary production wereat a maximum, and correlated with an increased focd supply atthis time. It is suggested that the strength of the recruitingpopulation is determined by mortality in the larval phase, ratherthan by the spawning stock biomass Larvae were found to be mostabundant in the upper 50 m of the water column during the dayand were virtually absent below 250 m. Larvae moved down byan average of 50 m at night.     

Seasonal abundance and distribution of Caridea larvae in Isafjord-deep, north-west Iceland

The abundance and distribution of Candea larvae was studiedin Ísafjord-deep, north-west Iceland, at approximatelymonthly intervals from February 1987 to February 1988 Zooplanktonsampling was made at nine stations along the length of the fjord,while temperature and chlorophyll a measurements from one ofthe stations are also presented Larvae of six species occurredin the samples, Eualus pusiolus and Pandalus borealis were mostnumerous, constituting 62 8 and 25 9% of the larvae respectively.The other species were, in declining order of abundance, Pandalusmontagui, Spirontocaris spp. (S spinus and s lilljeborgii) andSabinea septemcarinata. Eualus pusiolus was of highest abundancein the outer and middle parts of the fjord, while P.borealiswas most common in the middle and inner parts The onset of hatchingof all species in April–May appeared closely linked tothe phytoplankton spring bloom, while the temperature in thefjord was by then near the annual low (2–3°C). Exceptfor E pusiolus, of which a small part of the population produceda second brood during the summer, most of the larvae had disappearedfrom the plankton by the middle of August The monthly carapacegrowth of P.borealis larvae during the summer months was estimatedto be 1.0 mm.     

Metamorphic Competence, a Major Adaptive Convergence in Marine Invertebrate Larvae

Larvae from diverse marine-invertebrate phyla are able to respondrapidly to environmental cues to settlement and to undergo veryrapid metamorphic morphogenesis because they share the developmentaltrait of metamorphic competence. The competent state, characteristicof larvae as diverse as those of cnidarian planulae, molluscanveligers, and barnacle cyprids, is one in which nearly all requisitejuvenile characters are present in the larva prior to settlement.Thus metamorphosis, in response to more or less specific environmentalcues (inducers), is mainly restricted to loss of larva-specificstructures and physiological processes. Competent larvae oftwo "model marine invertebrates" studied in the authors' laboratory,the serpulid polychaete Hydroides elegans and the nudibranchPhestilla sibogae, complete metamorphosis in about 12 and 20hr, respectively. Furthermore, little or no de novo gene actionappears to be required during the metamorphic induction processin these species. Contrasting greatly with the slow, hormonallyregulated metamorphic transitions of vertebrates and insects,competence and consequent rapid metamorphosis in marine invertebratelarvae are conjectured to have arisen in diverse phylogeneticclades because they allow larvae to continue to swim and feedin the planktonic realm while simultaneously permitting extremelyfast morphological transition from larval locomotory and feedingmodes to a different set of such modes that are adaptive tolife on the sea bottom.     

Plankton distribution across a slope current-induced front in the southern Bay of Biscay

Relatively warm (12.50–12.75°C) and high-salinity[<35.640 practical salinity units (PSU)] water flowing eastwardwas detected at the shelf-break during a cruise carried Outin the southern Bay of Biscay in Spring 1987. The slope currentinduced the formation of a convergent front separating well-mixedoceanic waters from haline-stratified coastal waters. Very highconcentrations of dissolved oxygen (295 µmol kg^–1)and chlorophyll a(>4.5 mg m^–3) were found at the outeredge of the frontal boundary. Small autotrophic flagellatesdominated the phytoplankton community. Primary production peakedat the boundary region. Estimated phytoplankton growth ratesindicated that active growth was taking place, with lower turnovertimes integrated over the water column at the frontal station(2.5–5 days) than at coastal (1.5–2.8 days) or oceanic(1.5–3.5 days) stations. The lowest doubling times (1–2days) were calculated for surface frontal populations. Accumulationof zooplankton was also observed associated with the convergentphysical structure, although this relationship was less markedthan for phytoplankton. Copepods, mainly Paracalanus parvus,Acartia clausi and Oithona helgolandica, formed the bulk ofthe mesozooplankton biomass. Compatibility between the sizeof phytoplankton cells and copepod size spectra indicate highfood availability for these animals, particularly in the vicinityof the front. The distribution of fish eggs and fish larvaewas also coupled with the slope current-induced front. Sardinelarvae were more abundant at the coastal side of the front,whereas larval stages of blue whiting reached the highest densitiesat off-shelf stations. Larvae of lamellibranch molluscs andbryozoa were restricted to nearshore waters, as the frontalboundary prevented larval dispersion to the open ocean. Theresults presented in this paper suggest that the Iberian slopecurrent and its associated shelf-break frontal structure werecrucial in controlling phytoplankton primary production, activityof grazers, distribution of larvae of fishes and benthic invertebrates,and ultimately in determining the structure of the pelagic foodweb in the southern Bay of Biscay during the seasonal periodof vertical mixing.     

Pyrosoma atlanticum (Tunicata, Thaliacea): diel migration and vertical distribution as a function of colony size

A large population of the colonial pelagic tunicate Pyrosomaatlanticum occurred in April 1991 in offshore waters of theLigurian Sea (Northwestern Mediterranean). The high numbersof colonies caught allowed their vertical distribution and dielmigration in the 0–965 m water column to be describedas a function of their size. Daytime depths and amplitudes ofthe migration were correlated with colony size. The amplitudeof the migration ranged from 90 m for 3-mm-length colonies to760 m for 51-mm-length colonies, with a mean amplitude of 410m for the whole population, all sizes pooled. The results ofhorizontal hauls at a given depth around sunrise and sunsetshowed a marked diurnal symmetry of the migratory cycle relativeto noon, and that migration of the population was not cohesive.For example, the larger the colonies, the later after sunsetthey reached the upper layers during their upward migration.     

Studies on {partial}-amino levulinic acid deydratase in radish cotyledons during chloroplast development

The subcellular localization and biosynthetic site of 8-aminolevulinic acid dehydratase [EC 4.2.1.24 [EC] , ALAD] were investigatedin relation to chloroplast development in radish cotyledons. ALAD was mainly located in the chloroplasts and cytoplasm. Mostof the ALAD in the chloroplasts was readily released by hypotonicshock. The enzyme was also found in the proplastids of etiolatedcotyledons. The normal increase in the activity of ALAD in the chloroplastsas well as the cytoplasm was inhibited by cycloheximide butunaffected by D-threo chloramphenicol and kanamycin during thegreening of radish cotyledons. We concluded that the ALAD inboth the cytoplasm and chloroplasts was synthesized on the cytoplasmic80S-ribosomes. This suggests that the ALAD formed on the 80S-ribosomesmight be incorporated into chloroplasts during their development. When etiolated radish seedlings were illuminated, ALAD in boththe cytoplasm and chloroplasts increased up to the point ofthe full development of the chloroplasts, and thereafter itdecreased. (Received August 20, 1975; )     

Short-term temporal variation in coastal zooplankton communities: the relative importance of physical and biological mechanisms

Drogues were deployed off the coast of Northumberland (north-eastEngland), as they were tracked zooplankton were collected, byfour vertical hauls of a UNESCO WP-2 net (200 µm), adjacentto the drogue at hourly intervals Sampling covered a full tidalcycle, at least once each month from February to April, andin July and August 1993. Short-term changes in the communitystructure (in terms of species composition and abundance) wereinvestigated with respect to the local wind field and tidaladvection. It was observed, from a cluster analysis that duringhorizontal transport, the zooplankton maintained the same communitystructure for at least three consecutive hours on each samplingoccasion [Pearson correlation (r) 0.70; P0.01] even during periodsof high turbulent mixing, driven by wind stress Multiple regressionmodels including parameters of the wind field and the rate ofhorizontal transport only accounted for a maximum of 52% ofthe temporal variation in zooplankton community structure. Theunaccounted for variation provides the basis for the considerationof the zooplankton as ‘active drifters’ rather than‘passive particles’, this is discussed.     

Morphological and Physiological Responses of Echinoderm Larvae to Nutritive Signals

SYNOPSIS. Echinoid larvae have been found previously to developshorter arms as phytoplankton concentrations increase. In thepresent study, the skeletal dimensions of larvae of the seaurchins Lytechinus pictus and Strongylocentrotus purpuratuswere measured after exposure to dissolved organic compoundsin seawater. The presence of glucose or individual amino acids(at 1 or 2 µM), a mixture of 16 different amino acids(100 nM each), or algal exudate resulted in larvae with shorterarms (by 12 to 88%), relative to larvae in seawater with noadditions. Larvae exposed to mixtures of amino acids also hadchanges in the constituents of their internal free amino acidpools (as determined by HPLC). For another echinoid, Dendrasterexcentricus, amino acid transport (T, from 500 nM) by individuallarvae (n = 47) scaled to arm length (L) as follows: T = 2.06L^0.81(0.81 ± 0.26,95% confidence intervals). Mass (M) andmetabolic rate (MR) did not scale in the same manner (as transport)to arm length for larvae of the echinoid Centrostephanus coronatus(MR = 148L^1.51; M = 1.7L^2.01). These characteristics may scaleto arm length independently from transport rate under certainconditions. Larvae of echinoderms respond morphologically to"signals" in their environment that may indicate the availabilityof dissolved and paniculate nutrients. This in turn will haveconsequences for their ability to take up and metabolize thesenutrients. The response may be mediated by surface receptorsfor dissolved organic compounds, or by changes in the sizesof intracellular substrate pools.     

Effects of environmental factors on ichthyoplankton communities in the Miramichi estuary, Gulf of St Lawrence

Ichthyoplankton in 20 taxa (17 identified to species, threeto genus) representing 14 families were collected in 10 surveysof the Miramichi estuary between May and September 1992. Thetaxonomic composition was typical of other estuaries in theGulf of St Lawrence and Gulf of Maine. Larvae of three anadromousspecies [rainbow smelt (Osmerus mordax), alewife (Alosa pseudoharengus)and blueback herring (Alosa aestivalis)] were several ordersof magnitude more abundant than any other taxon. The upper estuary(Miramichi River and its tributaries) probably serves as a nurseryground for larvae of these species and others such as Atlantictomcod (Microgadus tomcod). The species composition of the lowerestuary (Miramichi Bay) was dominated by typically marine formsand probably serves as a nursery ground for winter flounder(Pleuronectes americanus), smooth flounder (Pleuronectes putnami).sculpin (Myoxocephalus sp ) and sand lance (Ammodytes sp) Ofthe environmental factors investigated, salinity was the mostuseful predictor of larval distribution in the estuary.     

Observations on the distribution of meroplankton during an upwelling event

The distribution of the larvae of benthic invertebrates wasinvestigated relative to hydrographic structures as a test ofthe hypothesis that larvae behave as if they are passive particles.Observations of larval and oceanographic distributions weremade off Duck, North Carolina, USA in August 1994. Conditionswere characterized by wind-driven coastal upwelling; flow wasgenerally offshore near the surface and onshore below the pycnocline.Within 5 km of the shore the pycnocline was bent upward by theupwelling and it intersected the surface along most of the transects.In zooplankton samples, 20 taxa of larvae were counted (10 bivalveveligers, nine gastropod veligers and one polychaete larvae).Using cluster analysis, larvae were separated into groups withsimilar patterns of distribution and similar affinities to waterproperties. The larvae in Cluster 3 did not display a consistentdistribution pattern beyond that they tended to be found inwarmer surface waters. An earlier paper described the distributionof larvae in the same location during a downwelling event [A.Shanks et al. (2002) J. Plankton Res., 24, 391–416]. Twoof the clusters identified during this previous study were quitesimilar in composition to Clusters 1 and 2 in this study. Inboth studies, Cluster 1 larvae were found below the pycnocline,but during the upwelling event they were transported shorewardwith the advection of the subpycnocline waters by the upwellingcirculation. Within 5 km of the shore, Cluster 1 larvae werefound at depths shallower than the base of the pycnocline andwere often found in patches of high larval concentration. Thepatches were located where the waters were upwelling. Cluster2 larvae were found within 5 km of the shore in both studiesand tended to be highly concentrated in convergences or divergences.Larvae in Cluster 1 generally appeared to be dispersing as passiveparticles, except within the zone of upwelling where they mayhave been swimming against the upwelling flow leading to higherlarval concentrations. Cluster 2 larvae appeared to be consistentlyconcentrated in areas of vertical currents, suggesting thatthey may be attempting to maintain a preferred depth in theface of the vertical flow which would lead to high larval concentrationand nearshore larval distributions despite extensive cross-shelfmovement of water. Despite their slow swimming speeds, the larvaein Clusters 1 and 2 were not swept offshore by the upwellingevent.     

Hydrocarbon accumulation and lipid biosynthesis during larval development in the cabbage looper,Trichoplusia ni

Larvae of the cabbage looper, Trichoplusia ni, were analyzed for the accumulation and biosynthesis of cuticular and internal hydrocarbon at closely spaced and accurately timed intervals during the fourth and fifth stadia. Large differences in the incorporation of [1-¹⁴C]acetate into hydrocarbon were observed at different times during larval development. Much higher incorporation was observed during feeding stages as compared to wandering stages, while lowest rates of biosynthesis occurred just prior to ecdysis. Fourth stadia wanderers accumulated increased amounts of internal hydrocarbon, which is apparently used to cover the newly forming cuticle. During the fourth to fifth stadium moult insects lost all cuticular hydrocarbon that was present on the old cuticle (about 8 μg/insect) and had about 8 μg/insect on the surface of the newly exposed cuticle. During the fourth stadium incorporation of [1-¹⁴C]acetate into total lipid declined between feeding and wandering stages from 24% of injected radiolabel to 7%. Similar decreases in lipid biosynthesis were observed between feeders and wanderers in fifth stadium larvae with the greatest decrease found in the triacylglycerol fraction. These results document dramatic changes in the accumulation and biosynthesis of hydrocarbon and other lipids during larval development.     

Distribution of decapod larvae in the surface layer of an isolated equatorial oceanic archipelago: the cases of benthic Grapsus grapsus (Brachyura: Grapsidae) and pelagic Sergestes edwardsi (Dendrobranchiata: Sergestidae)

Two different decapod larval assemblages inhabit the marine environment of Saint Paul’s Rocks, differentiating the inlet from the surrounding oceanic waters. Larvae of the crab Grapsus grapsus and of the holopelagic shrimp Sergestes edwardsi are abundant in superficial waters of the archipelago and have previously been shown to be good indicators of the inlet and adjacent oceanic waters, respectively. We investigated the horizontal, diel and temporal distribution of these species at Saint Paul’s Rocks. Horizontal surface hauls were conducted from 2003 to 2005, in the inlet and at four increasing distances from the archipelago, in the morning and at night, using a 200-μm mesh net. Larvae of G. grapsus were identified in samples from all expeditions and abundance was found significantly higher at night in the inlet site. Only larvae in the first zoeal stage were found in samples, highlighting the importance of the area for this species reproduction. On the contrary, the distribution of larvae of S. edwardsi was typical of a holopelagic species, which are permanent residents of the water column and spawn in oceanic areas, indicating that the islands are of little influence to them.     

Description of Rhynchoteuthion larvae of Illex argentinus from the summer spawning subpopulation

The Rhynchoteuthion larvae of Illex argentinus resulting fromsummer spawning in North Patagonic shelf waters, its distributionand abundance, are described in this paper. The material wascollected in the Argentine Sea (35–55°S) by meansof plankton nets. The research cruises were made by the R/VShinkai Maru and the R/V Walther Herwig during the period April1978 to April 1979. The most important spawning ground of thesummer spawning subpopulation is found in continental-shelfwaters (between 43 and 46°S) during the period December-February.This area was established on the basis of both ripe (December)and spent females (February). The larvae which were caught duringthe same period, especially in March, confirmed the spawningarea of this demographic unit. The larvae showed the lengthof the mantle (ML) to be from 1.2 to 6.5 mm. Tentacles weresplitting in specimens from 5.0 to 6.5 mm ML (transition stage).When 7.0 mm ML or more, all specimens were juveniles and hadtheir tentacles completely separated. Larvae were characterizedas type C, following the proposal of Sato (1973) and Sato andSawada (1974) in the Bulletin of the Shizuoka Prefectural FisheriesExperimental Station.     

Structure and swimming behavior of the larva of Halichondria melanadocia (Porifera: Demospongiae)

Larvae of the sponge Halichondria melanadocia are of the parenchymella type and, during swimming, can change shape rapidly from cigar-like to ovoid. Larvae collected in Hawaii displayed neither qualitative nor quantitative differences in behavior or structure from those collected in Florida. Floridian larvae were examined at 2, 28, 48, and 72 hr after release to assess anatomical changes correlated with duration of the free-swimming period. Although 2 hr larvae were significantly longer than 48 or 72 hr larvae, other differences were not observed. Positively phototactic throughout the free-swimming period, the larvae eventually begin to swim on or near the bottom of dishes, settle temporarily, but can resume swimming before permanent settlement is achieved. The larva is extensively flagellated and a band of long flagella separates the lateral and posterior regions. The epidermis is a tall, simple columnar epithelium composed of highly polarized, monoflagellated cells. The interior contains at least two distinct amoeboid cell types that intermesh with the basal ends of epidermal cells within a loosely defined cavity. No spicules are present. Choanocyte chambers, found within 3 of the 50 larvae that were serially sectioned, varied in size and complexity, but were not associated with canals. This report is the-first of such chambers in Halichondria larvae. Spicules and choanocyte chambers are somatic structures associated with adults, and their appearance in larvae is presumably a consequence of a heterochronic event, most likely acceleration. The evolutionary significance of the occurrence of these traits in Halichondria larvae awaits further developmental analysis and greater phylogenetic resolution.     

Growth, development and condition of Dendraster excentricus (Eschscholtz) larvae reared on natural and laboratory diets

Feeding invertebrate larvae may be food limited while developingin the ocean. If they are, then their time in the plankton isprolonged, which likely increases mortality. Food limitationcould be due to the quantity and/or quality of the food available.In an effort to answer how food type influences larval nutrition,we compared growth, development and lipid deposition for Dendrasterexcentricus larvae reared in natural seawater from two depths(1 and 20 m) and in filtered seawater on a monoculture laboratorydiet of 6 cells µL^–1 of the green alga Dunaliellatertiolecta (Butcher). Five days post-fertilization, larvaereared on the laboratory diet had developed to the latest stage,were the largest and had lipid deposits. Larvae reared on naturalsurface water were intermediate in size and developmental stage,and larvae reared in the water from 20 m depth were the smallestand developed the slowest. This trend continued at 8 days post-fertilizationwhen surface water diet larvae were similar in size to laboratorydiet larvae, but their juvenile rudiments were significantlysmaller. To assess food availability in each food treatment,we compared the concentration of chlorophyll (Chl) a, b andc in natural seawater from each depth and in D. tertiolectaculture in filtered seawater. Natural seawater collected fromthe surface had the highest concentration of Chl a and c, whereasChl b was not significantly different between treatments. IncreasedChl concentrations in the surface water are likely due to higherconcentrations of diatoms and dinoflagellates, which are typicallynot high-quality food items for echinoid larvae. Our resultssupport a hypothesis that echinoid larvae in the water columnmay be limited by food quality.     

Vertical migrations of herring,Clupea harengus,larvae in relation to light and prey distribution

Synopsis The influence of light and prey abundance on the vertical distribution of herring larvae was evaluated by three investigations made under calm weather conditions in the North Sea off the Scottish coast. The investigations took place at different time after hatching and the vertical distributions of three size groups of larvae (mean sizes 8,15 and 19 mm) were related to time of day and the vertical distribution of copepods. No migratory behaviour of copepods was observed but their vertical distribution differed between investigations. In the investigation on intermediate sized larvae, copepod density peaked at the pycnocline (40 m). Larvae concentrated at this depth at noon. At dawn and dusk larvae migrated towards the surface and the vertical distributions fluctuated semidielly. In the two other investigations, copepods were homogeneously distributed in the water column and after migration towards the surface at dawn larvae stayed in the upper water column during the day. The observations suggest that the daytime vertical distribution of larvae in calm weather is mainly determined by feeding conditions: the larvae move to depths were light is sufficient for feeding, and refinement within that zone is made according to a compromise between optimal light conditions for feeding and optimal prey densities.     

Distribution pattern of decapod larvae off the north-western Iberian Peninsula coast (NE Atlantic)

In October 1977 the model of general circulation of the watermasses off the coast of Galicia, and the presence of a coastalupwelling, led to a high primary productivity. This high productivityin turn favoured the development of a rich population of decapodlarvae. The abundance and distribution pattern of these organismswere closely linked (i) to the abundant presence of the correspondingadult species in the area, (ii) with the spatial distributionof phytoplanktonic populations concurrently studied by Estrada[J. Plankton Res ., 6, 417–434 (1984)] and (iii) withthe hydrodynamic pattern in the area. Fifty-two decapod larvaetaxa were identified and Solenocera membranacea, Pisidia longicornis,Pilumnushirtellus and Goneplax rhomboides were the most representativespecies It was observed that the greatest concentrations oflarvae (3387 larvae 10^–2 m^–3) were to be found nearthe mouth of the Rfas Baixas (situated in the south-west ofthe coastal area) and in some zones further out to sea (863larvae 10^–2 m^–3) (due to a process of hydrodynamictransport)