Factors affecting DNA uptake by mammalian cells

The ability to introduce DNA and express custom DNA sequences in bacteria opened the door for improvements in a large number of fields including agriculture, pharmacology, medicine, nutrition, etc. The ability to introduce foreign DNA sequences into mammalian cells in an efficient manner would have a large impact on therapeutic applications especially gene therapy. The methods in use today suffer from low efficiencies and sometimes toxicity. In this work a number of factors were evaluated for their effect onONA uptake efficiency. The factors studied included exposure to sublethal concentration of hydrogen peroxide which have been show to lead to destabilisation ofthe lysosomes. These exposures have proven to be very toxic to cells when combined with either the calcium phosphate or the lipofectAMINE® transfection methods. Another factor evaluated was exposure to Electro-Magnetic Fields (EMF). This was fuelled by the fact that EMF have been shown to mediate a number of effects on cell structure and/or physiology. EMF exposure by itself was not sufficient to induce the cells to pick up the DNA, therefore its effect on calcium phosphate and lipofectAMINE® was tested. Although some positive results were obtained, the variability of these results exceeded by far any observed enhancements which discouraged any further work on EMF. Also tested was the possible effect the presence of the cytomegalovirus (CMV) sequence might have on DNA uptake (based on previous results in this lab). It was found that the presence ofCMV in the DNA sequence does not enhance uptake or slow down degradation of the internalised DNA. The final factor tested was the effect of basic amino acids on transfection efficiency. It was found that arginine can enhance DNA uptake by about 170% v/ith calcium phosphate and about 200% with LipofectAMINE®. A model was proposed to explain the effect of arginine as well as the lack of effect from other amino acids.

L-Glutamate uptake, decarboxylation to -aminobutyric acid and GABA efflux in isolated Asparagus sprengeri mesophyll cells

Addition of L-glutamate caused alkalinization of the medium surrounding Asparagus spreng.ri mesophyll cells. This suggests a H+/L-glutmate symport uptake system for L-glutamate. However stoichiometries of H+/L-glutamate symport into Asparagus cells were much higher than those in other plant systems. Medium alkalinization may also result from a metabolic decarboxylation process. Since L-glutmate is decarboxylated to r-amino butyric acid (SABA) in this system, the origin of medium alkalinization was reconsidered. Suspensions of mechanically isolated and photosyntheically competent Asparagus sprengeri mesophyll cells were used to investigate the H+/L-glutamate symport system, SABA production, GABA transport, and the origin of L-glutamate dependent medium alkalinization. The major results obtained are summarized as follows: 1. L-Glutamate and GABA were the second or third most abundant amino acids in these cells. Cellular concentrations of L-glutamate were 1.09 mM and 1.31 mM in the light and dark, respectively. Those of SABA were 1.23 mM and 1.17 mM in the light and dark, respectively. 2. Asparagine was the most abundant amino acid in xylem sap and comprised 54 to 68 1. of the amino acid pool on a molar basis. GABA was the second most abundant amino acid and represented 10 to 11 1. of the amino acid pool. L-Slutamate was a minor component. 3. A 10 minute incubation with 1 mM L-glutamate increased the production of GABA in the medium by 2,743 7. and 2,241 7. in the light and dark, respectively. 4. L-Glutamate entered the cells prior to decarboxylation. 5. There was no evidence for a H+/GABA symport process • 6. GABA was produced by loss of carbon-1 of L-glutamate. 7. The specific activity of newly synthesized labeled GABA suggests that it is not equilibrated with a storage pool of GABA. 8. The mechanism of GABA efflux appears to be a passive process. 9. The evidence indicates that the origin of L-glutamate dependent medium alkalinization is a H+/L-glutamate symport not an extracellular decarboxylation. The possible role of GABA production in regulating cytoplasmic pH and L-glutamate levels during rapid electrogenic H+/L-glutamate symport is discussed.

Timing of di-ammonium phosphate addition to fermenting chardonnay must : effect on nitrogen utilization, ethyl-carbamate formation, and CAR1 expression by yeast /

The maximum amount of ethyl carbamate (EC), a known animal carcinogen produced by the reaction of urea and ethanol, allowed in alcoholic beverages is regulated by legislation in many countries. Wine yeast produce urea by the metabolism of arginine, the predominant assimilable amino acid in must. This action is due to arginase (encoded by CARl). Regulation of CARl, and other genes in this pathway, is often attributed to a well-documented phenomenon known as nitrogen catabolite repression. The effect of the timing of di-ammonium phosphate (DAP) additions on the nitrogen utilization, regulation of CARl, and EC production was investigated. A correlation was found between the timing of DAP addition and the utilization of nitrogen. When DAP was added earlier in the fermentations, less amino nitrogen and more ammonia nitrogen was sequestered from the media by the cells. It was also seen that early DAP addition led to more total nitrogen being used, with a maximal difference of ~25% between fermentations where no DAP was added versus addition at the start of the fermentation. The effect of the timing ofDAP addition on the expression of CARJ during fermentation was analyzed via northern transfer and the relative levels of CARl expression were determined. The trends in expression can be correlated to the nitrogen data and be used to partially explain differences in EC formation between the treatments. EC was quantified at the end of fermentation by GC/MS. In Montrachet yeast, a significant positive correlation was found between the timing of DAP addition, from early to late, and the final EC concentration m the wine (r = 0.9226). In one of the fermentations, EC levels of 30.5 ppb was foimd when DAP was added at the onset of fermentation. A twofold increase (69.5 ppb) was observed when DAP was added after 75% of the sugars were metabolized. When no DAP was added, the ethyl carbamate levels are comparable at a value of 38 ppb. In contrast, the timing of DAP additions do not affect the level EC produced by the yeast ECU 18 in this manner. The study of additional yeast strains shows that the effect of DAP addition to fermentations is strain dependent. Our results reveal the potential importance of the timing of DAP addition to grape must with respect to EC production, and the regulatory effect of DAP additions on the expression of genes in the pathway for arginine metabolism in certain wine yeast strains.

Investigations of 2-alkyl-3-methoxypyrazines in three ladybug species and wine /

Investigations of 2-alkyl-3-methoxypyrazines (2-isopropyl-3-methoxypyra2ine, 2- secbutyl-3-methoxypyrazine and 2-isobutyl-3-niethoxypyrazine) in ladybug species {Coleoptera: Coccinellidae) and wine samples have been conducted. Headspace sampling coupled with gas chromatography-mass spectrometry was used to determine amounts of 2-alkyl-3-methoxypyra2ines in the ladybug species. Hippodamia convergens had the highest amount of alkybnethoxypyrazines, followed by Harmoma axyridis and the least in Coccinella septempunctata. Using a solvent extraction method, the precoccinelline alkaloid was found present in Hippodamia convergens and Coccinella septempunctata but not Harmonia axyridis. Steam distillation followed by a soHd phase extraction method as a sample preparation technique, enhanced detection while the isotope dilution method afforded accurate quantitation of the alkyknethoxypyrazines in the wine samples. Both ladybug-tainted and commercial wine samples were found to contain the 2- alkyl-3-methoxypyrazines. Wine samples prepared in 2001 generally contained higher levels than the corresponding 2003 samples. Levels of the 2-alkyl-3-methoxypyrazines found in the commercial wines ranged from a minimum value of 6 ng/L to 260 ±10 ng/L. Analyses revealed that for both ladybug species and wine samples, the 2- isopropyl-3-methoxypyrazine had the highest concentration, followed by 2-isobutyl- 3-methoxypyrazine and the least being the 2-secbutyl-3-methoxypyrazine. Possible contamination of the wine samples by ladybugs is thoroughly discussed. Furthermore, attempts to remove or reduce the levels of the alkylmethoxypyrazines with molecularly imprinted polymers from wine samples are presented in detail.

Petrography, Petrochemistry and petrogenesis of Huronian volcanic rocks of the Elliot Lake region, Ontario

In the Elliot lake region of northern Ontario, Yolcanlc lava piles represent the lowermost units of the Huronian SUpergroup. These rocks general1y trend east-west and belong to the Elliot lake Group. They are s1tuated on the north and south limbs or the QuIrke lake Syncline. The volcanIc rocks of this study contain a secondary minerai assemblage consisting of actinolite, biotite, chlorIte, eptdote/cllnozoislte tttanomagnettte and calcite characteristic of greenschist metamorphism. Compilation of data suggests that metamorphism of the volcanic rocks proceeded between 325- and 425-C and between 2.4 and 4.7 kb. Geochemtcally these lavas represent tholeiitic and calc-alkaline assemblages. The tholeiites are character1sttcally enriched tn Fe and Tt and consist mainly of basalts, basaltic andesites and andesites. These rocks are believed to have formed by the partIal melting of a peridottte source at low P-T. In contrast, the calc-alkaline rocks are depleted in Fe and TI, but show a signIficant enrichment In 51 and Zr; andesIte Is the major rock type for thIs assemblage. I·t Is postUlated that the calc-alkalIne sU1te of rocks was the result of eIther the partIal meltIng of abasaltic·magma at shallow depth, or the melttng of s1al1c crustal materIal due to the added we1ght of tholeiitIc material on an unstable crust and to downwarplng processes Inttlated by convection cells.

HG 186.9-187.0 D.E-2

Coarse grained sediment with small patches of a fine grained domain. The domain may contain organic material. Lineations and minor grain stack present throughout the section.

HG 186.15-186.25-2

Major grains crushing towards the top left with two fine grained domains in coarse grained sediment.

HG 186.55-186.75-2

Fine grained sediment, quite structure-less.