Gelatinous zooplankton of the Arctic Ocean: in situ observations under the ice

The gelatinous zooplankton of the Canada Basin were observed with a deep-diving remotely operated vehicle (ROV) during August–September, 2002. Taxa observed fell into four main groups: cnidarians, ctenophores, chaetognaths, and pelagic tunicates. We provide detailed data on the vertical distributions of many taxa from three sites which span the Canada Basin. The most common gelatinous organisms in the surface waters were the ctenophores Mertensia ovum and Bolinopsis infundibulum. These two species were found in very large numbers in the near-surface mixed layer. In the mesopelagic zone, below the transition from the Pacific water layer and the Atlantic water layer, the most common species was Sminthea arctica. Surprising numbers of the scyphomedusa Atolla tenella were found in the deep waters of the basin, along with an undescribed species of narcomedusae. The vertical distributions of the gelatinous zooplankton observed with the ROV show several trends related to the physical properties of the water and geographic location within the basin.     

Vertical distribution of mesozooplankton in the central and eastern Arabian Sea during the winter monsoon

The vertical distribution of mesozooplankton in the centraland eastern Arabian Sea was investigated during the winter monsoonin 1995. Samples were analysed from discrete depth zones definedaccording to oxygen and temperature profiles of the water column.Zooplankton had higher standing stock in the mixed layer comparedto the strata below. The mixed layer had 78.5% of the totalcolumn biomass, while the deepest (500–1000 m) layer accountedfor only 0.9%. The stratum between 500 and 1000 m had the lowestabundance of copepods as well as other zooplankton. A notablefeature was that zooplankton biomass and density did not showmuch variations between coastal and offshore regions. Copepodawere the dominant group. Herbivores were generally more abundantat all depths. A total of 94 species of calanoid copepods wereidentified. Based on vertical distributions, they were assignedto four groups: (i) species restricted to the upper 200 m; (ii)predominantly surface-living species with tails to deeper waters;(iii) sparser deeper-living species generally confined below300 m; (iv) species occurring throughout the water column. Diversitywas fairly high in all strata with equitability being higherin the deeper strata.     

Associations between gelatinous zooplankton and hyperiid amphipods (Crustacea: Peracarida) in the Gulf of California

Hydrobiologia - Hyperiid amphipods are pelagic crustaceans that live associated with gelatinous zooplankton including medusae, ctenophores, siphonophores, and salps. Standard plankton sampling...     

Digenea parasites of jellyfish and ctenophores of the southern Atlantic

Parasites of planktonic cnidarians and ctenophores in the southern Atlantic Ocean are little known. The aim of this study was to describe three new metacercariae from jellyfish and ctenophores, and assess the importance of the gelatinous zooplankton as intermediate hosts in the life history of digeneans. During examination of zooplankton in Argentine Sea for digeneans that mature in fishes, two species of jellyfish (Phialidium sp. and Liriope tetraphylla Chamiso & Eysenhardt, 1821), and one ctenophore (Mnemiopsis mccradyi Mayer, 1900) were analyzed for parasites. The samples were obtained in Mar del Plata. Three metacercariae belonging to Faustulidae, Lepocreadiidae and Hemiuridae are described. The prevalence (percent of hosts infected) varied from 1.4–30% and the range of intensity (number of individuals of a parasite species in a single infected host) was from 1 to 30 for the different metacercariae. Given the important position of free-swimming cnidarians and ctenophores in the marine food web, and the great number of fishes that have been found with these organisms in their digestive tracts, their importance in the life histories of digeneans should not be underrated.     

Habitat structure determines resource use by zooplankton in temperate lakes

While the importance of terrestrial linkages to aquatic ecosystems is well appreciated, the degree of terrestrial support of aquatic consumers remains debated. Estimates of terrestrial contributions to lake zooplankton have omitted a key food source, phytoplankton produced below the mixed layer. We used carbon and nitrogen stable isotope data from 25 Pacific Northwest lakes to assess the relative importance of particulate organic matter (POM) from the mixed layer, below the mixed layer and terrestrial detritus to zooplankton. Zooplankton and deep POM were depleted in 13C relative to mixed layer POM in lakes that can support deep primary production. A Bayesian stable isotope mixing model estimated that terrestrial detritus contributed <5% to zooplankton production, and confirms the role of lake optical and thermal properties; deep POM accounted for up to 80% of zooplankton production in the clearest lakes. These results suggest terrestrial support of lake zooplankton production is trivial.     

Cilia and the life of ctenophores

Ctenophores, or comb jellies, are a distinct phylum of marine zooplankton with eight meridional rows of giant locomotory comb plates. Comb plates are the largest ciliary structures known, and provide unique experimental advantages for investigating the biology of cilia. Here, I review published and unpublished work on how ctenophores exploit both motile and sensory functions of cilia for much of their behavior. The long‐standing problem of ciliary coordination has been elucidated by experiments on a variety of ctenophores. The statocyst of ctenophores is an example of how mechanosensory properties of motile cilia orient animals to the direction of gravity. Excitation or inhibition of comb row beating provides adaptive locomotory responses, and global reversal of beat direction causes escape swimming. The diverse types of prey and feeding mechanisms of ctenophores are related to radiation in body form and morphology. The cydippid Pleurobrachia catches copepods on tentacles and undergoes unilateral ciliary reversal to sweep prey into its mouth. Mnemiopsis uses broad muscular lobes and ciliated auricles to capture and ingest prey. Beroë has giant smooth muscles and toothed macrocilia to rapidly engulf or bite through ctenophore prey, and uses reversible tissue adhesion to keep its mouth closed while swimming. Ciliary motor responses are calcium‐dependent, triggered by voltage‐activated calcium channels located along the length (reversed beating) or at the base (activation of beating) of ciliary membranes. Ciliary and muscular responses to stimuli are regulated by epithelial and mesogleal nerve nets with ultrastructurally identifiable synapses onto effector cells. Post‐embryonic patterns of comb row development in larval and adult stages are described and compared with regeneration of comb plates after surgical removal. Truly, cilia and ctenophores, like love and marriage, go together like a horse and carriage.     

Multilayer biological structure and mixing in the upper water column of Lake Biwa during summer 2008

We carried out a 24-h station experiment at Lake Biwa (Japan) to measure mixing events and concurrent biological signals using a free-fall microstructure profiler (TurboMAP-L), conventional hydrographic measurement device (F-probe), and the Tracker acoustic profiling system (TAPS). A clearly defined three-layer physical system was observed. Two layers were actively mixed: the surface-mixed layer and the subsurface-mixed layer. Both winds and night-time convection create the surface-mixed layer, and vertical shear due to a counterclockwise gyre maintains turbulence in the subsurface mixing layer. A strongly stratified layer between these two mixing layers is almost turbulence free, so no material flux is expected. A local oxygen maximum layer, a local oxygen minimum layer, and layers of increased chlorophyll and zooplankton abundance are all located in this strongly stratified layer. The data show the intricate influence of physical processes on the structure of biological systems and their combined influence on biogeochemical and trophic transfers in aquatic systems.     

Planktonic fauna of small salmon rivers in the Kola Peninsula

The zooplankton of 23 small salmon rivers of the White Sea and Barents Sea basins in the Kola Peninsula were studied. The species composition and quantitative indices in juvenile salmonids habitats are characterized. The maximum species diversity and abundance of planktonic fauna were recorded in lake-regulated rivers and places with large quantities of water. The quantitative development of zooplankton in rivers is low, which testifies to its minor role as a food resource for salmonid juveniles. The assessment of the ecological state of the river water is presented.     

Flounder (Platichthys flesus) in salmonid freshwater tank and cage culture

Fish farming activities result often in considerable high organic loadings to the water masses and sediments near the fishfarm. This study was carried out to evaluate the potential of flounder as food spillage feeder in salmonid freshwater culture. When transferring to fresh water, a clear tendency of an obligate need for food was discovered. Sufficient and continuous amounts of food are absolutely necessary for survival also when the flounder has been adapted for freshwater as long as 15 months. Flounder both in cages and in trays seemed to have little or no problem feeding on the bottom deposits (food and remnants of salmon) naturally occurring in salmon smolt production units. A high feeding rate in 0+ flounder preying on different cladoceran species was observed in addition to no significant size electivity. When feeding 0+ flounder and salmon in duoculture with small amounts of zooplankton, a competition effect resulting in growth inhibition in salmon was observed. Fairly good growth rates in flounder were observed in mixed culture experiments, but the flounder showed high individual variation. Fine meshed bottom net in the pen is necessary to retain enough food spillage to assure a positive growth rate in the flounder.     

A simple model of plankton population dynamics coupled with a LES of the surface mixed layer

The concentration of phytoplankton in the sea is affected by biological processes, such as growth/mortality rates, predatory zooplankton concentrations and nutrient levels. Phytoplankton concentrations are also influenced by physical processes, in particular the mixing properties of the local fluid environment. On planktonic scales (approximately 10-1000 microm) one can assume the local turbulent flow is isotropic, with no distinction between horizontal and vertical mixing. However, agglomerations of phytoplankton into patches are observed on larger scales of up to hundreds of metres, whose formation will be influenced by the anisotropic advection/mixing properties and large-eddy structures prevalent in the surface mixed layer. This paper presents the results of the coupling of a large-eddy simulation (LES) model of the mixed layer with an advection-diffusion system of coupled equations for nitrate-phytoplankton-zooplankton (NPZ) concentration, incorporating sub-grid parameterizations of the biological processes. Typically these include phytoplankton growth due to light levels and ambient nitrate concentration, offset by grazing losses due to the presence of zooplankton. The primary goal of this work is to investigate how the characteristics of the mixed layer turbulence influence the observed distribution of phytoplankton. One novel feature is the incorporation of a 'vortex-force' term in the LES code in order to generate Langmuir circulations. It has been speculated that the enhanced mixing rates associated with 'Langmuir turbulence' play a significant role in regulating planktonic activity. Results derived from the coupled LES-NPZ model, run with and without the presence of Langmuir circulations, are presented in order to investigate these ideas.     

Long-term variations of biotic and abiotic conditions in the ecosystem of the Barents Sea

Synchronism of year-class strength was noted for the majority of commercial fish in the Barents Sea. The reason for this is probably connected with a common factor, namely the intensity of water inflow which influences spawning efficiency, zooplankton food production, fish larval drift to the feeding grounds, and consequent survival of juvenile fish. Consequently, the established regular relationships of hydrological and weather processes in the ecosystem can serve as basis for long-term fishing forecasts. The overall pattern of the Barents Sea water circulation, long-term climatic changes in this region, and their effect on the fish stock reproduction are considered, using Arctic cod as an example.     

Phytoplankton and zooplankton of the Westport River Estuary,Massachusetts (USA)

Zooplankton and phytoplankton samples were simultaneously collected at approximately biweekly intervals over most of an annual cycle in the Westport River Estuary, Massachusetts. Phytoplankton numbers were overwhelmingly dominated throughout the study by athecate nanoplankton <5 µm in diameter. The zooplankton was primarily composed of copepod nauplii. Periods of occurrence of other zooplankters such as adult copepods, marine cladocerans, meroplankters and ctenophores were similar to those recorded for adjacent estuaries. Our results emphasize the abundance of smaller plankters that have been historically undersampled.     

大鹏湾生态因子灰关联分析

研究大鹏湾夜光藻、反曲原甲藻、浮游动物种群增殖与浮游动物和海水理化因子之间的关系,采用的方法是根据它们的种群增殖态势与浮游动物和理化因子的比较,依据空间理论的数学基础,按照规范性、偶对称性、整体性和接近性这四条原则,确定参考数列（母序列：夜光藻和反曲原甲藻、浮游动物）和若干比较数列（子序列：浮游动物和海水理化因子）之间的关联度．给出各因子对母序列影响的排列次序．其结果是,对大鹏湾生态环境起主要影响的因子有浮游动物、锰、铁和溶解氧     

Bacterial communities associated with the ctenophores Mnemiopsis leidyi and Beroe ovata

Residing in a phylum of their own, ctenophores are gelatinous zooplankton that drift through the ocean's water column. Although ctenophores are known to be parasitized by a variety of eukaryotes, no studies have examined their bacterial associates. This study describes the bacterial communities associated with the lobate ctenophore Mnemiopsis leidyi and its natural predator Beroe ovata in Tampa Bay, Florida, USA. Investigations using terminal restriction fragment length polymorphism (T-RFLP) and cloning and sequencing of 16S rRNA genes demonstrated that ctenophore bacterial communities were distinct from the surrounding water. In addition, each ctenophore genus contained a unique microbiota. Ctenophore samples contained fewer bacterial operational taxonomic units (OTUs) by T-RFLP and lower diversity communities by 16S rRNA gene sequencing than the water column. Both ctenophore genera contained sequences related to bacteria previously described in marine invertebrates, and sequences similar to a sea anemone pathogen were abundant in B.?ovata. Temporal sampling revealed that the ctenophore-associated bacterial communities varied over time, with no single OTU detected at all time points. This is the first report of distinct and dynamic bacterial communities associated with ctenophores, suggesting that these microbial consortia may play important roles in ctenophore ecology. Future work needs to elucidate the functional roles and mode of acquisition of these bacteria.     

Seasonal strengths of the abiotic and biotic drivers of a zooplankton community

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Predator-prey interactions in Lake Michigan: model predictions and recent dynamics

Synopsis Several years ago, we used a bioenergetics model to evaluate the impact of increasing salmonid stocking on the highly variable alewife forage base in Lake Michigan. At that time, we forecast an alewife population decline and the following system-wide effects: increased abundances of large zooplankton, decreased salmonid growth rates, increased diet breadth of salmonids, niche shifts among competitors of the alewife, increased alewife growth rates and increased densities of fishes suppressed by alewife. Alewives have continued to decline steadily since 1981 and are now reduced to a density similar to early outbreak levels in the early 1960s. Recent reports on fish growth rates, zooplankton size and fish community structure support our projections regarding system-wide responses to the alewife decline.     

Juvenile chum salmon consumption of zooplankton in marine waters of southeastern Alaska: a bioenergetics approach to implications of hatchery stock interactions

Bioenergetics modeling was used to estimate zooplankton prey consumption of hatchery and unmarked stocks of juvenile chum salmon (Oncorhynchus keta) migrating seaward in littoral (nearshore) and neritic (epipelagic offshore) marine habitats of southeastern Alaska. A series of model runs were completed using biophysical data collected in Icy Strait, a regional salmon migration corridor, in May, June, July, August, and September of 2001. These data included a temperature (1-m surface versus surface to 20-m average), zooplankton standing crop (surface to 20-m depth versus entire water column), chum salmon diet (percent weight of prey type consumed), energy densities, and weight. Known numbers of hatchery releases were used in a cohort reconstruction model to estimate total abundance of hatchery and wild chum salmon in the northern region of southeastern Alaska, given average survival to adults and for two different (low and high) early marine littoral mortality rate assumptions. Total prey consumption was relatively insensitive to temperature differences associated with the depths potentially utilized by juvenile chum salmon. However, the magnitudes and temporal patterns of total prey consumed differed dramatically between the low and high mortality rate assumptions. Daily consumption rates from the bioenergetics model and CPUE abundance from sampling in Icy Strait were used to estimate amount and percentage of zooplankton standing crop consumed by mixed stocks of chum salmon. We estimated that only a small percentage of the available zooplankton was consumed by juvenile chum salmon, even during peak abundances of marked hatchery and unmarked mixed stocks in July. Total daily consumption of zooplankton by all stock groups of juvenile chum salmon was estimated to be between 330 and 1764 g/km²d¹ from June to September in the neritic habitat of Icy Strait. As with any modeling exercise, model outputs can be misleading if input parameters and underlying assumptions are not valid; therefore, additional studies are warranted, especially to determine physiological input parameters, and to improve abundance and mortality estimates specific to juvenile chum salmon. Future bioenergetics modeling is also needed to evaluate consumption by the highly abundant, vertically migrating planktivorous that co-occurred in our study; we suggest that these fishes have a greater impact on the zooplankton standing crop in Icy Strait than do hatchery stock groups of juvenile chum salmon.     

Activation of brine shrimp nauplii photoresponses involved in diel vertical migration by chemical cues from visual and non-visual planktivores

The effects of exposure to visual and non-visual planktivoreson the photoresponses involved in the descent phase of nocturnaldiel vertical migration (DVM) of bnne shrimp (Anemia franciscana)naupliar larvae were measured in a laboratory system that mimickedthe underwater angular light distribution. This species wasused as a model for testing the general effects of differentplanktivores because a previous study demonstrated that naupliarphotoresponses were activated by exposure to one fish speciesthat was a visual planktivore, but did not co-exist with brineshrimp. The present study tested other fish and non-visual planktivores(ctenophores, chaetognaths, blue crab postlarvae). Photoresponseswere activated by 1 day exposure to: (i) three species of fish(Atlantic menhaden larvae, mummichog and pinfish) and (ii) waterthat had previously contained the fish or ctenophores. Thus,chemical cues from both visually and non-visually hunting planktivoresactivated photoresponses, contrary to the hypothesis that nocturnalDVM functions for avoidance of visual planktivores. Activationoccurred within 5 min, indicating that brine shrimp naupliihave a phenotypic response to zooplankton planktivores. Photoresponsesensitivity decreased with decreasing concentration of chemicalcue, indicating that activation of DVM should vary with planktivoreabundance. In contrast, photoresponse activation was very weakafter exposure to the physical presence of two non-visual, verticallymigrating planktivores (blue crab postlarvae and chaetognaths).The results support the predictions that zoo-plankton DVM patternshould vary with exposure to different planktivore types andthat migration amplitude should increase with increasing planktivoreabundance.     

A comparison of carbon-specific respiration rates in gelatinous and non-gelatinous zooplankton: A search for general rules in zooplankton metabolism

Using 470 data from the literature the dry weight-specific respiration rates of gelatinous zooplankton (cnidarians, ctenophores and salps) and non-gelatinous zooplankton (mainly crustacea) were converted to carbon-specific values. The resulting carbon-specific respiration rates showed no significant differences between the two groups of zooplankton, indicating similar oxygen requirements per gram of carbon biomass. From this finding, it can be suggested that the differences in the rates of oxygen consumption measured in the two types of zooplankton in the sea can be explained by the carbon biomass ratio between gelatinous and non-gelatinous zooplankton. Furthermore, the low rate of metabolism of gelatinous species compared with that of non-gelatinous animals of the same volume can be attributed predominantly to the relatively low organic matter content in the former. It is recommended that all weight-specific metabolism rates be expressed using carbon as body mass unit (e.g. mg O₂ gC⁻¹ d⁻¹) which enables more accurate comparisons between individuals exhibiting different dry weight/carbon ratios.