Mode of action of a surfactant–polymer formulation to support performance of the entomopathogenic nematode Steinernema carpocapsae for control of diamondback moth larvae (Plutella xylostella)

The use of entomopathogenic nematodes on cabbage leaves against larvae of the diamondback moth (DBM) Plutella xylostella requires the addition of formulation adjuvants to achieve satisfying control. Without adjuvants nematodes settle in the tank mix of backpack sprayers causing uneven distribution. The polymers arabic and guar gum, alginate and xanthan were used in concentrations between 0.05 and 0.3% to retard sedimentation of Steinernema carpocapsae. Arabic gum had no effect, guar gum prevented sedimentation at 0.3% but the effect dropped significantly at lower concentration. At 0.05%, xanthan prevented nematode sedimentation better than alginate. Deposition of nematodes on the leaves was significantly increased by the addition of any of the polymers. Spraying nematodes on leaves with an inclination of 45° without the addition of any formulation resulted in 70% run-off. Adding 0.2% alginate or xanthan reduced the losses to <20%. The use of a surfactant–polymer formulation significantly reduced defoliation by DBM larvae. Visual examinations provided evidence that nematodes are not ingested by DBM larvae. Invasion of S. carpocapsae is an active process via the anus. The function of the formulation is not to prolong nematode survival, but to provide environmental conditions which enable rapid invasion of the nematodes. Nematode performance was improved by selection of the best surfactant in combination with xanthan and by optimisation of the concentrations of the surfactant Rimulgan® and the polymer xanthan. The best control results were achieved with Rimulgan® at 0.3% together with 0.3% xanthan, causing DBM mortality of >90% at 80% relative humidity and >70% at 60%. The formulation lowered the LC₅₀ from 12 to 1 nematode/larva. The viscosity of the surfactant–polymer formulations correlated well with nematode efficacy, prevention of sedimentation and adherence to the leave. This physical parameter can therefore be recommended for improvement of nematode formulations to be used for foliar application against DBM.     

Physicochemical characterization of alpha-crystallins from bovine lenses: hydrodynamic and conformational properties

A detailed investigation of hydrodynamic and conformational behavior has been made of the HM-crystallin and -crystallins of bovine lens. Results from this study indicated that HM (high-molecular-weight -crystallin) and (low-molecular-weight -crystallin) possess considerable size and charge heterogeneities in their native structures and subunit polypeptides, respectively. Sedimentation velocity showed a heterogeneous polydisperse system of HM with an average sedimentation coefficient of about 50 S and a more homogeneous system of -crystallin of 20 S. Viscosity and circular dichroism studies pointed to a compact and globular shape of dominant -sheet conformation for -crystallin, yet a highly asymmetrical and aggregated form for HM. The conformational stability of -crystallin was investigated in the presence of various denaturants. The evidence presented shows that hydrogen bonding is the main force in maintaining the quaternary structure of compact native -crystallin. Conformational flexibility of -crystallin demonstrated in the equilibrium unfolding study indicated a multistep transition that made the extraction of thermodynamic data from the heat denaturation study difficult. Temperature perturbation on -crystallin suggested the possible involvement of hydrophobic interaction in the aggregation process, leading to the formation of HM from -crystallin. The comparison of conformational properties between HM and -crystallin strongly indicated that HM is a denatured form of -crystallin.     

Hydro-sedimentology of the Johnstone River estuary

This paper examines the physical consequences of increased catchment sediment yields on the sediment budget and the hydrodynamic setting of the South Johnstone River estuary in North Queensland. A combined study involving hydrological monitoring, assessment of sediment sources, estimation of riverine sediment budget and hydro-sedimentological numerical modelling for estuarine sediment transport is currently underway. Initial field and laboratory observations indicate that the sediment delivery from highly erosion-prone sugar cane cultivations in the tropical catchment has increased dramatically during the last 10 years. This has subsequently given rise to elevated flood levels in both the lower and upper catchment areas, as well as significant modifications to the river bed morphology.     

The effects of low concentrations of particulates from paper mill effluent on the macroinvertebrate community of a fast-flowing stream

The effects of a paper mill effluent on the macroinvertebrate community were assessed for the riffle areas of a large fast-flowing stream, the lower reaches of the Saranac River of northern New York State, U.S.A. The effluent caused few changes in dissolved oxygen concentration, pH, biochemical oxygen demand, temperature or nutrient content; however, significant differences in transmitted light, concentrations of particulates and accumulated debris on the substrate were observed. A moderate decrease in invertebrate diversity correlated with increased levels of particulates and substrate debris. An analysis of the response of invertebrate functional groups revealed the effluent had little effect on the density of gathering collector organisms. The functional groups most severely reduced in density were the filtering collectors and scrapers. Predators showed a moderate reduction in density in response to the effluent. The alterations in invertebrate densities were attributed largely to the alterations in seston and substrate caused by the introduction of particulates composed mainly of paper fiber and inert dye.     

Particulate phosphorus sedimentation at the river inflow to a lake

Sedimentation at the Krutynia River inflow to Lake Kujno was closely related to hydrological regime. The highest sedimentation rates, recorded in spring, decreased during summer by two orders of magnitude. Granulometric segregation of settling seston along the inflow zone was related to differentiation of phoshorus content. Smaller particles were richer in P, producing a gradient of increasing P concentrations in the settling material. A substantial loss of P from polyphosphate and various organic fractions was found after settlement of river suspensoids. Mechanisms of P losses are discussed and possibilities of P retention within the inflow zone are considered.     

Epidermal calcium-binding protein: a marker of early differentiation of basal layer keratinocytes of rats

Epidermal calcium-binding protein (ECaBP) is present in the cells of the basal layer of the epidermis and other stratified epithelia. Since the basal layer compartment contains at least two types of cells: slow-cycling, poorly-differentiated, and actively proliferating, more differentiated cells, it was of interest to determine whether they both contained ECaBP. Basal and nearly suprabasal layer keratinocytes from newborn rat epidermis were fractionated into three fractions on the basis of cell size, using low-gravity sedimentation. The cell differentiation in each subgroup was estimated by cell size, morphology, cell cycle stage, RNA/DNA content, and the presence of specific keratins. The presence of ECaBP in these fractions was detected by immunocytochemistry and immunoblotting. Double staining with ECaBP antibodies and propidium iodide followed by flow cytometry was used to correlate ECaBP production and the stage of cell cycle. The relative cell size, measured by the light scattering was used to study the relationship between cell size and ECaBP production. The results show that small keratinocytes with low DNA and RNA content (G₀ cells) do not express ECaBP. ECaBP was found only in intermediate size basal keratinocytes with higher DNA and RNA contents, corresponding to actively proliferating S phase cells. Large keratinocytes, which express suprabasal keratin and have low DNA and high RNA content, cease to express ECaBP. ECaBP may, therefore, be a useful marker for assessing the movement of cells from poorly differentiated reserve compartment towards proliferation and further differentiation in both physiological and pathological situations.     

Sedimentation properties of chitosomes fromMucor rouxii

Summary This study was undertaken to assess the distribution and localization of chitin synthetase in a fungal cell and to evaluate the sedimentation behavior of chitosomes (microvesicular containers of chitin synthetase). Chitosomes were isolated from cell-free extracts of yeast cells ofMucor rouxii by rate-zonal and isopycnic sedimentation in sucrose density gradients. Because of their small size and low density, chitosomes were effectively separated from other subcellular particles. Rate-zonal sedimentation was a suitable final step for isolating chitosomes as long as ribosomes had been eliminated by enzymic digestion. By isopycnic centrifugation, chitosomes could be separated directly from a crude cell-free extract; they cosedimented with a sharp symmetrical peak of chitin synthetase at a buoyant density of d=1.14–1.15g/cm³; the only significant contaminants were particles of fatty acid synthetase complex. From such sedimentations, we estimated that 80–85% of the chitin synthetase activity in the cell-free extract was associated with chitosomes; the rest was found in two smaller peaks sedimenting at d=1.19–1.20 and d=1.21–1.22 (5–10%), and in the cell wall fraction (5–10%). By consecutive rate-zonal and isopycnic sedimentations, chitosome preparations with relatively few contaminating particles were obtained. Potassium/sodium phosphate buffer (pH 6.5)+MgCl₂ was the most effective isolation medium for chitosomes. Other buffers such as TRIS-MES+MgCl₂ led to massive aggregation of chitosomes and a change in sedimentation properties. This tendency of chitosomes to aggregate could explain why most of the chitin synthetase activity of a fungus is sometimes found associated with other subcellular structures,e.g., plasma membrane.     

Structure of F1-ATPases

F₁-ATPases are large multimeric proteins that can be isolated from the membrane bound system that catalyzes the phosphorylation of ADP by inorganic phosphate in bacteria, plants, and mitochondria. They can be visualized in electron micrographs of the inner mitochondrial membranes where they appear as large protruding spheres 90 Å in diameter. The purified F₁-ATPases have a molecular weight of 320,000 to 400,000 daltons and are composed of five non-identical subunits (, , , and ). The stoichiometry of these subunits in the complex is still unknown but compositions of the type ₃₃ and ₂₂₂₂₂ were found to be consistent with some of the available experimental data. This review discusses the recent data and the experimental approaches utilized for the structural characterization of F₁-ATPases.     

Zinc in water and sediments of two finnish lakes

The distribution of zinc in Lake Vanajavesi and Lake Mallasvesi, South Finland, was determined on the basis of water and sediment studies. Lake Vanajavesi is one of the most polluted of large inland lakes, in Finland. The zinc load comes mainly from industrial sources. Lake Mallasvesi, situated near Vanajavesi, is in almost natural condition. The water samples were taken by a Ruttner sampler. In collecting sediment samples, a freezing technique was used. The results of zinc analyses indicate that, during several winters, zinc has spread with waste water to different parts of L. Vanaja against the main course of flow. A close correlation between sedimentation of zinc and waste discharge from a textile factory was found in the present study.     

Climatic and anthropogenic effects on the sedimentation and geochemistry of Lakes Bourget,Annecy and Léman

During the last glaciation, the Rhone glacier extended as far as the region of Lyon and covered Lakes Bourget, Annecy and Léman. Glacial retreat successively freed Lakes Bourget and Annecy, it reached Geneva around 14 000 B.P. and the head of Lake Léman at about 12 000 B.P. Deposits situated between Nyon and the foot of the Jura provide a complete palynological zonation and serve as a type section for the lake core studies. A palynological horizon (about 1 800 A.D.) has been found in Lake Bourget and wood has been dated at 3 230 ± 65 B.P. (¹⁴C) in a core from Lake Léman. Three 6 m cores from each lake were sampled together with many 0.5 m cores from Léman. The short Lake Léman cores have been dated by ¹³⁷Cs and provide a precise indication of changes in the basin during recent decades. Holocene climatic variations are evident in the Léman cores and are reflected by concentrations of carbonate and organic carbon which increase at the end of the Alleröd and reach a maximum in the Atlantic Period (climatic optimum). Human settlement on the shores of Lake Annecy is shown by increases in heavy metals; increased sedimentation rates suggest settlement at the beginning of the Christian era. All the cores show increases in the organic matter and nutrients; from the turn of the century in the Léman, and later for the other lakes where eutrophication started only a few decades ago. NAI-P shows a very recent increase, around 1965 in the Leman. Heavy metals (Hg, Cd and Pb) show increases at about 30 years ago in Annecy, at about the turn of the century in Lake Léman and in the mid-19th century in Lake Bourget.

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Résumé Lors de la dernière glaciation, le glacier du Rhône a atteint la région de Lyon et recouvert les lacs du Bourget, d'Annecy et le Léman. Son retrait a successivement libéré les lacs du Bourget, d'Annecy, puis le Léman de leur carapace de glace. Aux environs de 14 000 ans B.P. son front se trouvait au voisinage de Genéve, puis vers 12 000 B.P. à l'embouchure du Rhône en amont du Léman.La chronostratigraphie des grandes carottes (6 m) prélevées dans les trois lacs a été établie par la palynologie, sur la base des zonations obtenues dans un profil complet provenant d'un marais situé entre Nyon et le pied du Jura. Elles ont pu être contrôlées par un marqueur palynologique dans le lac du Bourget (150 B.P.) et la datation au ¹⁴C d'un fragment de bois dans le Léman (3 230 ± 65 B.P.). Une série de carottes de grand diamètre provenant de ce dernier lac, datés par le ¹³⁷Cs, ont donné une image très précise du l'évolution du milieu durant les dernières décades. D'une facon générale, toutes les carottes montrent une augmentation des teneurs en matière organique, puis en nutrients, vers le fin du 19ème siècle pour le Léman et quelques dizaines d'années plus tard pour les lacs du Bourget et d'Annecy. Le début du l'etrophisation se situe beaucoup plus tard dans le Lémen avec l'accroissement des teneurs en phosphore, principalement de ses formes NAI-P et O-P, soit aux environs de 1965.