Horizontal distribution of crustaceans in Lake Glubokoe

A study has been made on the distribution of crustaceans along a profile of 6–9 stations from depths of less than 2 m to 20 m, in summer, autumn and early spring. The species composition, abundance, size-frequency distribution, biomass and diurnal dynamics were estimated. Many species abundant in the pelagic zone were found to be absent or scarce out to depths of 5 m. In the daytime, at depths out to 3 m, crustaceans greater than 1.0 mm were seldom found, while those 0.15–0.40 mm long were most abundant. At depths out to 5 m, not only was the total average size of crustaceans found to be smaller, but also that of individual species, including small ones: Ceriodaphnia and Chydorus. The biomass of crustaceans in shallow water and in the open lake differs in summer by more than 100 times, and in late autumn and early spring by more than 10 times. At the depth of 1 m, in none of the seasons did it exceed 0.026 mg l^-1. All the crustaceans except for nauplii and Chydorus considerably increased in numbers in the shallow water at night. The impoverishment of the littoral plankton in Lake Glubokoe is regarded as a specific case of the well-known phenomenon of ‘avoidance of the littoral’ by euplankton (Hutchinson, 1967; Kiselyov, 1980). It is pointed out that there is a possible relationship between diurnal horizontal migrations of plantivorous fish and the impoverishment of plankton near the shore. An attempt has been made to substantiate the assumption that the ‘avoidance of the littoral’ by pelagic crustaceans is due to high numbers of fish in shallow water.     

The species composition,occurrence and temporal stability of submerged aquatic macrophyte patches along the main channel border of pool 5A,Upper Mississippi River

Species composition, relative abundance, distribution and physical habitat associations of submerged aquatic macrophytes in the main channel border (MCB) habitat of Pool 5A, Upper Mississippi River (UMR) were investigated during the summers of 1980 and 1983. The submerged aquatic macrophytes in Pool .5A MCB were a small and stable component of the river ecosystem. Submerged plants occurred primarily in small, monospecific clumps. Clumps in close proximity to each other formed plant patches. Plant patches were stable in location and number between 1980 and 1983; 82.5% of the patches first observed in 1980 were present in 1983. Submerged macrophytes covered about 10–12 ha of the 201 ha MCB in Pool 5A. Submerged plants were most common in the lower two-thirds of the pool. Ten species of aquatic macrophytes occurred on rock channel-training structures and eleven occurred on non-rock substrates in the MCB. The most common submerged plants, in order of abundance, were Vallisneria americana Michx., Heteranthra dubia Jacq., Potamogeton pectinatus L., Ceratophyllum demersum L. and Potamogeton americanus C. & S.     

Pelagic rotifers of Lake Glubokoe from 1897 to 1984

After alteration in the pattern of drainage of run-off from the surrounding swamps and changes in the colour and transparency of the Lake Glubokoe water, the previously epilimnial Trichocerca similis, Conochilus unicornis and Keratella cochlearis showed a shift of their maximum numbers to deeper layers. Pompholyx sp. and Trichocerca capucina, which are regarded as indicators of eutrophic waters, have disappeared from the pelagic zone of the lake and Conochilus hippocrepis, Synchaeta pectinata, Gastropus stylifer, Asplanchna herricki, Ascomorpha ecaudis, Ascomorpha saltans, Euchlanis dilatata and Trichocerca porcellus have made their appearance. Most of the new species are considered to be indicators of oligotrophic conditions. However the total density of pelagic rotifers remained at the same level. Apparently the establishment of the new species of rotifers was possible due to some ‘rarefaction’ of the epilimnion, the disappearance of predaceous Mesocyclops leuckarti and the invasion of the pelagic zone by Peridinium cinctum.     

The distribution of Heterotrissocladius oliveri Saether (Diptera: Chironomidae) in Lake Michigan

Fifty one chironomid species were identified from 504 samples collected at depths ranging 8 to 267 m in Lake Michigan, U.S.A. Heterotrissocladius oliveri Saether occurred in 32% of these samples and had an average abundance of 22 m^–2 which was similar to other estimates from the Great Lakes. Maximum average lake-wide density was at 30 to 60 m (41 m^–2). At depths 60 m, H. oliveri was the dominant chironomid species comprising 75% of total Chironomidae. The substrate preference of H. oliveri differed within each depth regime considered: at 30–60 m, 2–3 ; at 60–120 m, 3–5 , 7–9 ; and at 120–180 m, 6–8 . Abundance was notably reduced at all depths in substrates characterized as medium silt (5–6 ). On a lake-wide basis, the distribution pattern suggested H. oliveri was most numerous from 30 to 60 m along the southwestern, eastern, and northern shorelines and at 60–120 m depths along the southern and eastern shorelines. Increased abundance in the South Basin was concurrent with evidence of increased sedimentation at 60 to 100 m. However, in several other areas of the lake, high densities were associated with medium to very fine sands relatively free of silts and clays. This observation suggested occurrence of H. oliveri was minimally affected by sediment type.Widely variable, but generally elevated water temperatures likely prevent H. oliveri from establishing a substantial population density at depths < 30 m. With increased depth, temperature fluctuation is negligible and food is more stable, though the source is variable. Factors limiting abundance of H. oliveri at depths 30 m were related to decreased food supply due to distance from shore, food sources of lower value (clays), and, most importantly, to reproductive replenishment.Although still oligotrophic in nature, high density occurrences in both high and low sedimentation areas of the lake suggest the trophic indicator status of H. oliveri might be broader than previously thought.     

Ionophore-induced efflux of sodium and potassium ions from sea urchin eggs

The efflux of K⁺ and Na⁺ from sea urchin eggs during Ca²⁺ ionophore A23187-induced parthenogenesis was studied in a K⁺ and Na⁺-free artificial seawater using extracellular ion-specific electrodes. We have probed this model system with monovalent cation-specific ionophores to determine if they affect K⁺ efflux in the unfertilized egg and whether any changes in ionophore sensitivity are observed during egg activation. In 500 mM choline chloride, 10 mM CaCl₂, 50 mM MgCl₂, 10 mM Tris-Cl pH 8.0, A23187 induced a rapid efflux of K⁺ and Na⁺ from the eggs after a short lag time (10–15 seconds). After the burst, the rate of K⁺ efflux remained higher than the pre-activation rate, but was lower than during the burst phase, while the rate of Na⁺ efflux became nearly zero. Monovalent cation-specific ionophores (valinomycin, gramicidin and nigericin) had no effect on K⁺ efflux from the unfertilized eggs in our model system. However, once the egg was activated by A23187, each of the above ionophores caused a prolongation of the burst phase for many minutes. These results show that the unfertilized egg plasma membrane (using our artificial conditions) is not susceptible to the monovalent cation-specific antibiotics and suggest that either the inserted cortical granule membrane or the developing fertilization envelope interacts with these ionophores to cause the change in rate-limiting step for K⁺ efflux observed egg activation.     

Evaluation of ion gradient-dependent H+ transport systems in isolated enterocytes from the chick

Summary The experiments reported here evaluate the capability of isolated intestinal epithelial cells to accomplish net H⁺ transport in response to imposed ion gradients. In most cases, the membrane potential was kept constant by means of a K⁺ plus valinomycin voltage clamp in order to prevent electrical coupling of ion fluxes. Net H⁺ flux across the cellular membrane was examined at pH 6.0 (the physiological lumenal pH) and at pH 7.4 using methylamine distribution or recordings of changes in media pH. Results from both techniques suggest that the cells have an Na⁺/H⁺ exchange system in the plasma membrane that is capable of rapid and sustained changes in intracellular pH in response to an imposed Na⁺ gradient. The kinetics of the Na⁺/H⁺ exchange reaction at pH 6.0 [K _t for Na⁺=57mm,V _max=42 mmol H⁺/liter 3OMG (3-O-methylglucose) space/min] are dramatically different from those at pH 7.4 (K _t for Na⁺=15mm,V _max=1.7 mmol H⁺/liter 3OMG space/min). Experiments involving imposed K⁺ gradients suggest that these cells have negligible K⁺/H⁺ exchange capability. They exhibit limited but measurable H⁺ conductance. Anion exchange for base equivalents was not detected in experiments performed in media nominally free of bicarbonate.