Glycolate metabolism by Pseudomonas sp., strain S227, isolated from a coastal marine sediment

Glycolate excreted by phytoplankton is a potentially important nutrient for bacteria in coastal and estuarine environments. The metabolism of glycolate by Pseudomonas sp., strain S227, originally isolated from the New York Bight Apex, has been studied. The specific growth rate for this strain on glycolate is 0.156 doublings h^-1. The apparent V_max and K_m for glycolate uptake are 83.6 nmol min^-1 mg cell protein^-1 and 7.4x10^-8 M, respectively. The preferential respiration of the carboxyl carbon (C-1) and the incroporation of the hydroxymethyl carbon (C-2) suggest that the glycerate pathway is used for growth on glycolate. Alternatively, another pathway can be utilized which results in the complete catabolism of glycolate. Glycolate and lactate metabolism are also closely linked either by a common metabolic pathway or a common transport system other than the monocarboxylate transport system. The magnesium ion concentration is also important in glycolate metabolism. The characteristics of glycolate metabolism observed in Pseudomonas sp., strain S227, are advantageous in coastal and estuarine environments where glycolate production is intermittent, and the concentrations are low.     

Ultrastructural alterations on chloride cells of the yellowtail Seriola quinqueradiata,following exposure to the red tide species Chattonella antiqua

By means of scanning and transmission electron microscopy, the influence of the red tide species Chattonella antiqua was examined with respect to the surface ultrastructures of chloride cells of the yellowtail Seriola quinqueradiata. Conspicuous ultrastructural alterations occurred on the apical surface of these cells. The majority of chloride cells in the control gills showed an apical surface with numerous cellular extensions, while more than half the chloride cells affected by red tide organisms exhibited an apical surface with fewer and smaller extensions, a wrinkled apical surface, or a protruded apical surface. These ultrastructural alterations of chloride cell surface may be due to the partial disturbance of salinity by C. antiqua, and reflect the changes of the ion-transport function in yellowtail gills exposed to red tide water.     

Measurement of photosynthetic production of a marine phytoplankton population using a stable 13C isotope

The use of stable isotope of carbon, ¹³C, for the determination of the photosynthetic rate of a marine phytoplankton population was examined. Particular concern was paid to the effects of non-phytoplanktonic organic carbon and the enrichment of inorganic carbon on the estimation of the photosynthetic rate. Photosynthetic rates determined by the ¹³C method showed a remarkable agreement with those determined by the ¹⁴C method. Insitu determinations of photosynthetic rate were made in three different water types: open ocean, coastal and neritic waters, which included oligo- and mesotrophic waters, by using the ¹³C method established.     

The effect of Po river discharge on phytoplankton dynamics in the Northern Adriatic Sea

An oceanographic transet,, extending from Yugoslavia across the Northern Adriatic Sea to the Po delta in Italy, was occupied during 1972 and 1973 to establish the effect of Po river discharge on the phytoplankton communities of the region. Density distribution showed distinct seasonal features: a winter-spring period of low stability throughout the water column, and a summer period of stratification. The total water-column plant nutrients (nitrate, nitrite, phosphate, silicate) showed a 1.3 to 4.5-fold decrease eastward, with semi-eutrophic conditions restricted to an area off the Po delta. Nannoplankton usually dominated the phytoplankton community, in terms of cell density, surface chlorophyll a concentrations, and surface primary production rates. However, all significant maxima in these characteristics resulted from increases in the microplankton component. Changes in the frequency of major microplankton groups characterized three periods of the annual cycle: September–December, neritic, temperate diatom flora with some littoral elements (e.g. Nitzschia seriata); January–May, neritic, temperate diatom flora of different composition (e.g. Lauderia borealis, Skeletonema costatum); May–August, dinoflagellates (e.g. Prorocentrum micans) at western stations and dinoflagellates plus neritic, warm-water diatoms at eastern stations. The seasonal cycle was characterized by spring and fall maxima tending to coincide with maximum Po river discharge and/or periods of low water-column stability and vertical mixing. The higher nutrient input at western stations was correlated with the co-dominance of only a few species of microplankton during bloom periods, suggesting that these species (S. costatum, N. seriata, and 5 others) can serve as indicators of eutrophic conditions in this region. Assimilation ratios of both the micro- and nannoplankton suggested borderline nutrient conditions. Phosphate was implicated as the limiting nutrient.     

A population study of the polychaete Capitella capitata at plymouth

A population of Capitella capitata (Fabricius) was sampled from January, 1973 to February, 1974. Size of the worms was measured and sexual maturity determined. There is an extensive breeding season, spawning occurring asynchronously throughout the year. Females containing ripe oocytes were almost always present, but most females at any one time contained immature oocytes. A high percentage of males contained active sperm. Oocytes are not released into the coelomic fluid until almost fully developed, and all are released at a single spawning. A large number of eggs are produced at each spawning and there is some evidence to suggest that larval development may be completely benthonic. Gametes first develop in 7 to 8 month old worms and take about 4 months to complete development. Analyses of the female population structure suggests that there are 3 breeding classes. The growth rate is estimated at 30 mm per year, and few worms are believed to survive longer than 2 years.     

Inorganic nitrogen metabolism in marine bacteria: The intracellular free amino acid pools of a marine pseudomonad

The marine pseudomonad bacterium PL₁ contains an intracellular pool of free amino acids which consist mainly of glutamate with small amounts of glutamine and aspartate when grown in a nutrient medium containing 0.2 M NaCl. When the NaCl concentration of the growth medium is increased to 0.8 M, proline becomes a major component of the intracellular pool together with glutamate—at this molarity and under suitable nutrient conditions these amino acids comprise 20% of total bacterial amino acid nitrogen. When grown in a nutrient growth medium containing a constant level of NaCl, the intracellular pool size can vary by a factor of 4 depending on the concentration of carbon and nitrogen in the medium. Experiments show that the amino acid pool can act as a nitrogen reserve but has little function as a carbon reserve. At high NaCl concentrations there is a marked dependence for growth on the presence of sufficient potassium in the medium. However, no correlation between K⁺ and glutamate concentration in either nitrogen or K⁺-limited cultures has been found. None of the enzymes associated with glutamate biosynthesis was influenced by NaCl levels between 0.2 and 0.5 M. Neither Na⁺ or K⁺ stimulated the activity of these enzymes when tested in vitro.     

Prodigiosin metabolites of a marine Pseudomonas species

The major pigment of a marine micro-organism was identified as prodigiosin on the basis of analytical and spectral data. Two minor pigments were tentatively assigned structures, from thin-layer chromatography (TLC) and mass spectral data, as prodigiosin homologs with 3-n-hexyl and 3-n-heptyl side-chains. The micro-organism was classified as a new Pseudomonas species on the basis of its morphological and biochemical characteristics. It was named Pseudomonas magnesiorubra (ATCC No. 21856).     

Feeding behavior of some carnivorous fishes (Serranidae and Scorpaenidae) from Tuléar (Madagascar)

The feeding behavior of 8 species of sea basses (Serranidae) and 17 species of scorpionfish (Scorpaenidae) has been studied by quantitative analysis of their stomach contents. Most of the 459 specimens analysed were collected from the barrier reef of Tuléar (Madagascar). Examination of stomach contents revealed that in each species feeding behavior varies according to a nyctemeral rhythm, individual size of specimens, biotope and geographical area. Prey consumption by sea basses and scorpionfish on a reef tract is discussed in general terms.