Observations on the Aggregative Behavior of Mysidium columbiae, the Mangrove Mysid

Abstract. The mangrove mysid Mysidium columbine (Z immer ) occurs in aggregations of tens to millions of individuals. Few indepth studies on the aggregative behavior of this species have examined structural composition, response to light intensity changes, and its ability to reduce prcdation. Snorkel and SCUBA observations, as well as aquarium experimentation on shoals/ schools of this species in shallow waters around a mangrove archipelago were made at irregular intervals to determine their structure, dynamics, and influence on prcdation. In summer, aggregations occurred as large cylindrical shoals, in winter as small ovoid schools. In daylight, shoals/schools were very sensitive to changes in light intensity. At night the smallest juveniles formed compact swarms, while larger individuals became solitary. At sunrise a definite rc-shoaling behavior existed. Shoals/schools were stratified by life stages. A hypothesis stating that conspecific schools in winter did not mix was tested. Mysidium shoals/schools seemed to discourage prcdation by fishes.     

Population Parameters, Life Cycle, and Feeding of Mysidium columbiae (Zimmer) in the Waters Surrounding a Belizian Mangrove Cay

Abstract. The ecology of tropical Mysidacea is poorly known. Mysidium columbiae (Z immer ), because of its ubiquitous distribution in the tropical western Atlantic and the information available on its aggregative behavior, is an ideal subject of study to reconcile aspects of this problem. Information and data were obtained on abundance, population size, shoal/school structure, fecundity, development, and feeding of a M. columbiae population inhabiting waters surrounding Twin Cays, a mangrove archipelago in Belize. Although reproduction was continuous and proportions of life stages within shoals remained relatively constant throughout the year, population size decreased by an order of magnitude from summer to winter. Embryonic development averaged 4.7 days, with postlarvae being released near the surface before dawn. Aquarium experiments suggested that olfaction may be more sensitive than vision, although both senses were used to locate food. This species is a detritivore, but gut contents suggested that it may also be a predator.     

In situ Observations on Contraction Behaviour and Diel Activity of Halcampoides purpurea var. mediterranea (Cnidaria, Anthozoa) in a Marine Cave

Abstract. The contraction behaviour of the sand-dwelling sea anemone Halcampoides purpurea var. mediterranea was observed in situ in a cave of the Penisola Sorrentina (Gulf of Naples). The circadian rhythm of activity of two specimens, together with migrations of mysidacean swarms in and out the cave, was studied with time-lapse photography.     

Surf Zone Hyperbenthos of Belgian Sandy Beaches: Seasonal Patterns

Since surf zone hyperbenthos, although highly important in local food webs, has often been neglected and very little information is available, a survey of the Belgian sandy beaches was carried out from May 1996 until July 1997. Monthly samples were taken to give a complete record of hyperbenthic organisms occurring in the surf zone of Belgian sandy beaches and to evaluate the intensity by which this surf zone is used. In total 172 species were recorded. The number of species occurring in the surf zone is comparable to that of adjacent areas. As well as true hyperbenthic species, endobenthic and planktonic organisms were sampled. More than 75% of the average total sample composition consisted of mysids, mainly Mesopodopsis slabberi,Schistomysis spiritus and Schistomysis kervillei (holohyperbenthos). Apart from several resident species, active and passive seasonal migration towards the surf zone by a number of species is suggested. A large number of sporadic species adds to the composition of surf zone hyperbenthos. Within the merohyperbenthos, postlarval decapods and fish were the dominant organisms. During the year three recruitment peaks were observed. Average densities per month exceeded 1500 ind. 100 m⁻². Yearly biomass averages ranged from 300 to over 3000 mg ADW 100 m⁻². Densities of the common species are slightly higher in the surf zone than in other habitats, emphasising the importance of the area. Besides a possible nursery function, the surf zone may also be used as a transient area between different habitats. Finally, the influence of several abiotic factors on the hyperbenthic assemblages was evaluated. The main structuring variables determining the occurrence of most of the organisms are water temperature and hydrodynamic factors such as wave height and turbidity. The influence of wave height seems to be two-fold: several good swimmers such as mysids and some fish species are suggested to be able to actively avoid severe wave conditions, whereas other, more planktonic organisms, are passively transported towards the area if wave height increases.     

Horizontal Transfer of Matter by a Cave-Dwelling Mysid

Abstract. The role of a cave-dwelling mysid population as a matter carrier was evaluated in a cave of the Medes Is. (NW Mediterranean) during 1988–89. Hemimysis spehmcola (Ledoyer , 1963) is a gregarious mysid whose swarms migrate daily from the inner end of the cave - where they remain during the day–to the exterior where they feed during the night. Fecal pellet composition, pellet egestion and pellet decomposition were measured in order to evaluate the transfer of matter by mysids. Based on the strong daily behavioural rhythms of these mysids. special importance was attached to the sampling frequency (every 2 h). In order to assess seasonal variability, four daily cycles were evaluated within a year. In situ incubations were carried out to determine changes on the egestion rates, morphology, weight and composition (AA. C: N ratios) of pellets in the course of a day. The number of pellets deposited inside the cave was estimated using containers distributed along the cave bottom by SCUBA divers. Fecal pellets showed an amorphous composition, whereby diatom frustules, dinoflagellate loricae and coccolithoporids were very scarce. About 25% of the body weight were estimated to be egested daily as fecal pellets, suggesting a detritivorous feeding habit. The population oscillated seasonally between 1 and 12 millions. Individuals egested between 1.6 and 3.5 pellets a day into the cave, each averaging from 9.4 to 11.9 μg DW, 0.5 to 1.0 μg C and 0.046 to 0.27 μg N. Therefore, the population carried daily about 20 407 g DW POM. 2–21 g C and 0.5 2.7 g N from outside to inside the cave. Pellets decomposed very quickly; between 20 to 50% of both C and N were released from pellets in less than 2 h after egestion. Oxidation of pellets theoretically consumes an amount of oxygen which agrees with the high BOD values previously reported for this cave. Marine caves are generally viewed as strictly oligotrophic systems; dense mysid populations, however, could strongly modify the trophic relationships in marine caves.     

Some Aspects of Fluorite and Vaterite Precipitation in Marine Environments*

Abstract. Mysid shrimps of the genus Schistornysis precipitate either fluorite (CaF₂; S. spiritus) or vaterite (CaCO3; S. assimilis) for the formation of static bodies (statoliths). In S. assirnilis, 2.44 μg calcium and 3.66 μg carbonate are precipitated for each statolith. This corresponds to 69 mg or 30 mg ambient water, respectively, using the ion content of seawater for stoichiometrical comparison. Concentmtion factors of calcium or carbonate in relation to equivalent amounts of ambient water in the statocyst cavity are 760 or 3100, respectively. In S. spiritus, 3.79 μg calcium and 3.60 μg fluoride are precipitated. This corresponds to 9.3 mg or 2788 mg ambient water, respectively. Concentration factors with respect to statocyst water mass are 610 or 183.000. respectively. Ile high fluoride accumulation for the formation of statoliths alone contributes to a fluoride content of 4500 ppm with respect to body dry weight A minimum estimate for the role of mysids in the global fluoride cycle suggests that at least 62,000 tons of fluoride are bound in mysid statoliths. Due to rapid turnover of about seven days, mysid fluorite statoliths are a crucial factor by contributing to a turnover of at most 570,000 years for overall fluoride in the oceanic system.