ALBERT

Notes: Abstract The seasonal variations in distribution and abundance of the common zooplankton species in the Bristol Channel and Severn Estuary were related to the salinity regimes observed over the period November 1973 to February 1975. The dominant constituents in all regions were the calanoid copepods, which reached maximum densities in July: approximately 100 times their winter levels. Four zooplankton assemblages were recognised using an objective classification program which computed similarity coefficients and used group-average sorting. The assemblages existed along the salinity gradient observed from the Severn Estuary to the Celtic Sea. The assemblages were classified as true estuarine, estuarine and marine, euryhaline marine and stenohaline marine and were characterized by the copepods Eurytemora affinis (Poppe) (〈30‰S), Acartia bifilosa var. inermis (rose) (27 to 33.5‰S), Centropages hamatus (Lilljeborg) (31 to 35‰S) and Calanus helgolandicus (Claus) (〉33‰S), respectively.

Notes: Abstract Mysids are important components of the zooplankton biomass of estuaries and coastal regions. Twelve species were identified from the Bristol Channel and Severn Estuary (British Isles). The most abundant species wasSchistomysis spiritus (Norman), the majority of which occurred in the Channel within a salinity range of 27 to 34‰ S. The seasonal distribution and numerical abundance of this species are described over the period November 1973 to February 1975. The peak of abundance ofS. spiritus occurred in the Inner Channel in September (mean of 14 individuals m-3, ca. 250 individuals m-2 for this sub-region) when it represented 76% of the omnivore biomass (μg C m-3); for the 364 d from 4 November 1973, the species contributed 43% of the total integrated omnivore standing stock. This peak of biomass was the product of the development of the juveniles from the reproductive period in the spring. Correlation analyses were carried out betweenS. spiritus biomass and 10 physical and biotic variables for 2 mo, November 1973 and September 1974. Temperature and salinity, which are simple indices of seasonal change, exhibited significant correlations with the mysid's abundance in both months. These correlations do not necessarily imply causal relationships or mechanisms between the distribution and abundance of the species and these variables. Clearly, in such a complex environment as an estuarine ecosystem a single variable is unlikely to control the abundance of a species, it is more the result of the combined influence of a number of variables acting in concert.

Notes: Abstract A decreasing gradation in the plankton standing stock of the Bristol Channel was observed from the seaward section to the inner, less saline, reaches. Two sub-regions of our survey, the North Outer Channel (NOC) and the Inner Channel (IC), represented the extremes of this gradient and were selected for detailed comparison. The integrated zooplankton biomass, over the 307 d sampling period (4 November 1973 to 6 September 1974), was 2 475 mg C m-3 (≡266 mg C m-2 d-1) in the NOC and 335 mg C m-3 (≡20 mg C m-2 d-1) in the IC. The omnivorous plankton accounted for 76% of the standing stock in the NOC and 89% in the IC, of which 58 and 23% were meroplankton and 39 and 71% were holoplankton, respectively; the remainder was unassigned. The majority of the meroplankton in both subregions was decapod larvae and adults, whereas the holoplankton biomass was dominated in the NOC by copepods (89%) and in the IC by mysids (57%), mainly Schistomyzis spiritus. Centropages hamatus was the most abundant copepod species in the NOC and accounted for 32% of the total holoplankton omnivore standing stock. In the NOC and IC, the carnivorous plankton accounted for 24 and 11% of the total plankton biomass, respectively. In the two sub-regions, 20 and 21% of the carnivores were meroplanktonic (primarily larvae of sprats and pilchards), while the holoplankton carnivores contributed 75 and 74% to the NOC and IC, respectively (Sagitta elegans, Pleurobrachia pileus). S. elegans dominated the holoplankton carnivore biomass for the majority of the year and accounted for 96% in the NOC and 60% in the IC. The integrated total particulate carbon over the 307 d period was 200 g C m-3 (≡6 600 g C m-2) in the NOC and 838 g C m-3 (≡15 084 g C m-2) in the IC. The annual primary production ranged from 164.9 g C m-2 yr-1 in the Outer Channel (North and South) to 6.8 g C m-2 yr-1 in the IC. The zooplankton biomass reached a maximum in July. The total particulate carbon (TPC) in July was 400 mg C m-3 in the NOC of which ca. 78 mg C m-3 were phytoplankton and ca. 21 mg C m-3 were zooplankton; these values compare favourably with those found in the adjoining Celtic Sea. In the IC, the TPC was 2 800 mg C m-3, of which ca. 107 mg C m-3 were “phytoplankton” and 2.8 mg C m-3 were zooplankton. From the low primary production estimates for the IC it can be concluded that the majority of the chlorophyll, like the TPC, was allochthonous in origin. Furthermore it is suggested that zooplankton plays a minor role in this estuarine ecosystem and is not the main consumer of the suspended particulate carbon; the benthic filter-feeding communities are presumed to fulfill this role in the Bristol Channel.

Notes: Abstract The vertical distributions of eggs, nauplii, copepodites and adults of Calanus helgolandicus (Claus) from five oblique plankton-net hauls taken in May (1980), March and September (1981) and January (1982) at a site in the shelf sea to the south-west of the United Kingdom are described. The water depth is approximately 95 m and becomes thermally stratified during the summer months when a thermocline of ∼6 C° develops. In early spring when the water column was isothermal (∼8 °C), the development of the eggs and nauplii took place below 60 m and a single ontogenetic migration was observed between Nauplius VI (NVI) and Copepodite I (CI). As the temperature of the water increased, this migration occurred in progressively earlier naupliar stages. The eggs were distributed throughout the water column in the profile taken in early May when a 1 C° thermocline occurred between 30 to 40 m. The majority of the NI to NIV stages occurred below 40 m, with the ontogenetic migration taking place in the NIV stage; the NV and NVI stages were found above the thermocline. In September, the eggs were again distributed throughout the water column (101 490 m-2), with a maximum number of 〉4 500 m-3 occurring in the surface to 5 m depth interval. Nauplius I and II were found at all depths, demonstrating that hatching occurred throughout the water column. The ontogenetic migration in these late-summer profiles took place between the NII and NIII stages, the remainder of the nauplii being found above the thermocline in the top 20 m. This is the first time that an ontogenetic migration, similar to the developmental ascent observed in the naupliar stages of the euphausiid Euphausia superba in the deep ocean, has been shown for a copepod nauplius.

Notes: Abstract The geographical distributions, seasonal variations in numerical abundance and biomass (mg C m-3) of the predators of the holoplankton of the Bristol Channel, between November 1973 and February 1975, are described. The predator numbers and biomass were dominated by the chaetognath Sagitta elegans Verrill. This species represented 96% of the holoplankton carnivore biomass in the outer, seaward region of the Channel and 60% in the inner region; the remainder being ctenophores. The maximum numerical abundance of S. elegans occurred in September at 129 individuals m-3 (≡18 mg C m-3). Juveniles (〈5 mm) reached maximum numbers of 55 individuals m-3 during June, August and September, demonstrating the reproductive activity of the population. The peak numbers were probably the result of the development of two major generations over the 90 d period from mid-June to mid-September. The tentaculate ctenophores were represented by Pleurobrachia pileus (O. F. Müller). The highest abundance was 81 individuals m-3 (≡3.0 mg C m-3) at a single site in July in the South Central Channel. However, June was the only month when the ctenophores dominated the carnivore biomass in all regions of the Channel; thereafter, S. elegans was more abundant. Reproduction of the ctenophore occurred from April to September, with juveniles reaching maximum abundance in June at 12 individuals m-3. The estimated food demand of the population in May for the outer region of the Channel was approximately 31% of the daily production of copepods. When the population reached its peak abundance in June, the estimated food requirement outstripped the daily production of copepods and a decline in both the prey and predator standing stocks was observed. Similar estimations were derived for the inner region of the Channel. S. elegans increased from a standing stock of 0.038 mg C m-3 in March to 6.35 mg C m-3 in September. Estimates of the copepod production compared with the derived demand of the chaetognath population showed that the decline in the copepods in the late summer was the result of feeding by this predator. The holoplankton carnivore population was approximately 66% of the copepod standing stock for the 10 mo period November 1973 to September 1974 in the outer region of the Channel and 45% of that in the inner region. The carnivores formed the greater part of the total holoplankton biomass from September through the winter months to February, suggesting a predator-dominated community.