Dimorphism in a new isolate of Saccharomycopsis Schiönning

1972 ◽  
Vol 18 (6) ◽  
pp. 901-907 ◽  
Author(s):  
Edward J. Buecher ◽  
Herman J. Phaff

Two strains of Saccharomycopsis guttulata Robin (Schiönning) were isolated from two out of four specimens of Lepus californicus, the wild jack rabbit of California. One isolate was similar to typical strains with budding cells occurring in domestic rabbits. The second strain was atypical in being dimorphic. Colonies of the yeast form, consisting of budding cells, were smooth and glistening, while those of the filamentous form were irregular, rough, and dull. The filamentous form consisted of septate, branched hyphae, radiating from a central origin of growth. New filaments generally were initiated by fragmentation. The two new strains were similar to domestic strains in assimilation and fermentation reactions and grew only between 30 and 40C. Both strains formed ascospores at 18C. The filamentous strain, unlike other S. guttulata strains, was not carbon dioxide dependent at 37C but did require oxygen. At 30C it became carbon dioxide dependent. During the stationary phase, a morphogenetic change occurred from the filamentous form to a yeast form, which was stimulated by anaerobic conditions. The budding form of the filamentous strain was relatively stable in culture and at either 30 or 37C it was carbon dioxide dependent. Spontaneous reversions from the budding to the filamentous form appear to occur sporadically.

1946 ◽  
Vol 24f (1) ◽  
pp. 1-11 ◽  
Author(s):  
G. A. Adams

Aeration by mechanical agitation of 15% wheat mash fermented by Aerobacillus polymyxa inhibited the formation of 2,3-butanediol and particularly of ethanol. Aeration of similar mashes by passage of finely dispersed air or oxygen at the rate of 333 ml. per minute per litre of mash increased the rate of formation and yield of 2,3-butanediol but inhibited ethanol formation. However, the over-all time required for the completion of fermentation was not shortened from the usual 72 to 96 hr. required for unaerated mashes. There was no evidence of a shift from fermentative to oxidative dissimilation. Under aerobic conditions, the final butanediol–ethanol ratio was approximately 3:1. Anaerobic conditions, as produced by the passage of nitrogen or hydrogen through the mash, increased the rate of formation of both butanediol and ethanol and shortened the fermentation time to about 48 hr. Under these conditions, the butanediol–ethanol ratio was reduced to about 1.3:1.0. Carbon dioxide gave a butanediol–ethanol ratio resembling that of anaerobic fermentation but did not reduce fermentation time.


1931 ◽  
Vol 8 (3) ◽  
pp. 319-329
Author(s):  
JOSEPH NEEDHAM ◽  
MARJORY STEPHENSON ◽  
DOROTHY MOYLE NEEDHAM

1. The vitelline membrane of the infertile hen's egg exhibits no dehydrase activity. 2. The vitelline membrane has no measurable aerobic respiration in vitro, nor has the yolk of the infertile egg. This confirms the view that the carbon dioxide production of the intact egg is not the result of any true respiration. 3. When incubated anaerobically in vitro, bacteriologically sterile yolk produces consistently small amounts of lactic acid. 4. This glycolysis is not the result of any catalytic activity of the vitelline membrane, but takes place throughout the substance of the yolk. 5. Under similar conditions, bacteriologically sterile yolk produces small amounts of a substance or substances estimatable as ethyl alcohol. 6. If the yolk suspension is bacterially contaminated, however, lactic acid and alcohol are produced in amounts closely similar to those found by earlier workers on this subject. 7. The heat of glycolysis, under anaerobic conditions, calculated from the amounts of lactic acid experimentally found to be formed, is of the same order as (a) the calculated requirement of the vitelline membrane (Straub), and (b) the observed heat production (Langworthy and Barott). Thus even if the vitelline membrane is capable of using energy to do osmotic work, the yolk is only capable of supplying it by means of its glycolytic mechanism if the whole energy output of the whole yolk can be made available for doing work at the membrane.


2017 ◽  
Vol 21 (1) ◽  
pp. 26 ◽  
Author(s):  
EllIN HARlIA HARlIA ◽  
MARlINA ET ◽  
MASITA R ◽  
RAHMAH KN

The natural methane formed by bacteria in anaerobic conditions is known as biogenic gas. Gas trapped in coal, formed through thermogenesis as well as biogenesisis known as coal-bed methane (CBM). The availability of organic material as decomposition of this material into methane is continuously required for the production of methane in the coal aquifer. The aim of this research was to investigate whether or not cattle feces bacteria were able to grow and produce methane in coal. Parameters measured were Volatile Fatty Acids (VFA) and the production of biogas, such as nitrogen, hydrogen, carbon dioxide, and methane. Explorative method was used and data obtained was analyzed by descriptive approach. The results showed that the bacteria found in the feces survived in the coal and produce biogas. On day 2 when the process was at the acidogenesis phase, it produced VFA with the largest component of acetic acid. Acetic acid would undergo decarboxylation and reduction of CO2 followed by reactions of H2and CO2 to produce methane (CH4) and carbon dioxide (CO2) as the final products. ,


2000 ◽  
Vol 3 (01) ◽  
pp. 35-41 ◽  
Author(s):  
M.I. Kuhlman ◽  
H.C. Lau ◽  
A.H. Falls

Summary Laboratory results demonstrate that surfactant adsorption on sandstones is minimized and foam performance improved by reducing the ethoxylate chain length in alcohol ethoxy sulfonates and blending unethoxylated and ethoxylated sulfonates to optimize desirable properties. The results also show that laboratory adsorption measurements can only be extrapolated to reservoirs by (1) replicating the anaerobic conditions of reservoirs, and (2) differentiating authogenic minerals from drilling mud found in reservoir cores. Introduction If a foam is to be designed to provide mobility control throughout reservoirs with a thousand meters between wells, the properties of that foam and the surfactants used to create the foam must differ substantially from foams and surfactants used to reduce mobility in near-wellbore applications. First, it is absolutely necessary to maintain very low surfactant adsorption and limited mobility control in order to use foam in the reservoir, yet the foam must survive when the capillary pressure is high. Surfactants with very high critical micelle concentrations (CMC) used below their CMC appear to satisfy these criteria.1 Surfactants used below their CMC have low adsorption and limited mobility control because solid/fluid and fluid/fluid interfaces are not completely filled with surfactant molecules. Then, surfactant adsorption is so low that low concentrations of surfactant can propagate faster than high concentrations.1–3 Yet foam stability and mobility control are sufficient to limit gravity override of gas.1 Second, oil is likely to spread4 around carbon dioxide-rich gas bubbles when they are some distance from an injector because light hydrocarbons have not yet been stripped from the oil. This can mean that another type of foam, gas/oil, is possible.5 Finally, surfactant must somehow propagate where water is not mobile. A good example of this is at the top of an oil reservoir where water saturation is low, water mobility is low, and surfactant does not propagate far in the water. Some evidence suggests5 that the portion of a surfactant which dissolves in the oil does propagate where water is immobile and can stabilize gas/oil lamellae. This gas/oil foam observed in microvisual experiments at reservoir conditions is known to reduce gas mobility when water is absent,5 and shown with simulations to be the likely cause of mobility control in some laboratory experiments.5 This paper describes optimization of surfactant structure and composition as well as the laboratory controls to properly test surfactant performance. The desirable properties of these surfactants are (a) rapid propagation, (b) limited mobility control, and (c) mixed wettability versus water wetness. Because the surfactant is used below its CMC, micelles do not stop chromatographic separation of surfactant components. Experimental Details Experiments were conducted at 170°F (75°C) with the high salinity brines described in Table 1. The surfactant types and equpment used in this study have been described in previous papers.1,5 The surfactants, Fig. 1, were generally alcohol ethoxy [?CH2?CH2 O?] glyceryl [?CH2?CHOH?CH2] sulfonates (AEGS X-Y) supplied by Shell Chemical Co. X and Y refer to the hydrophobe size or range and ethoxylate (EO) number. Results for alpha olefin sulfonates (AOS X) and their mixtures with AEGS surfactants were also discussed. Unethoxylated alkyl biphenyl disulfonates (DOWFAX) were also used. Three types of surfactant adsorption and propagation experiments were conducted. The first, conducted in Berea cores cleaned with a 3 PV 0.1% sodium dithionite rinse, were used to characterize components which propagated with least adsorption. The second group conducted in similarly cleaned Berea cores or slim tubes packed with disagregated reservoir cores were used to optimize surfactant design. The third group, conducted in tubes packed with reservoir sand, were used to demonstrate that surfactants would propagate under reservoir conditions. Some of these were conducted at anaerobic conditions. A limited number of mobility control experiments in slim tubes packed with 2% illite-sand mixture2,5 were also conducted to demonstrate the effectiveness of the surfactants. Surfactant Characterization. The propagating surfactant was initially characterized with 1H nuclear magnetic resonance (NMR), isotachophoresis, and fast atom bombardment mass spectroscopy (FABS) after effluent from a coreflood had been de-salted using the following procedure: One PV of solution from a coreflood was evaporated to dryness and the residue digested in hot methanol to extract the surfactant. The solution was cooled, filtered, and evaporated to dryness. The residue was dissolved in 50/50 H2O then salted out with Na2 CO3 to produce aqueous and isopropanol layers. Water was added to the isopropanol layer and the salting out procedure repeated a second time. The final isopropanol layer was evaporated to dryness to give a de-salted surfactant-rich residue. 1H NMR was conducted at 360 MHz after the surfactant residue had been dissolved in D2O Isotachophoresis was conducted by injecting the surfactant residue into a capillary column in an electric field. Species of different charge are separated and detected by changes of potential gradient at zone boundaries. In FABS, a sample is bombarded by low-energy-charged atoms, which transfer their charge without breaking up the original molecule. The mass of charged species can be determined to four decimal places and used to confirm the identity of a species. Surfactant Adsorption. Surfactant adsorption was measured by injecting a surfactant solution into Berea cores, or 5/8 in.×12 tubes filled with reservoir sand at Sorw. The brines contained sodium dithionite in most of the experiments. The amount of surfactant adsorbed was determined with a methylene blue dye two-phase extraction technique.6 Mineralogy. The mineralogy of reservoir core material was determined by x-ray diffraction and thin-section point counting. The volumes of foreign mud and fines determined from thin-section analysis was subtracted from the total minerals to determine a more realistic reservoir core description.


1976 ◽  
Vol 22 (2) ◽  
pp. 159-164 ◽  
Author(s):  
Chii-Guary Tsai ◽  
Diane M. Gates ◽  
W. M. Ingledew ◽  
G. A. Jones

Under anaerobic conditions, resting cell suspensions of Coprococcus sp. Pe15 degraded 1 molecule of phloroglucinol to 2 molecules of acetic acid and 2 molecules of carbon dioxide. The organism metabolized the flavonoids rhamnetin and quercetin anaerobically in 20% rumen fluid medium but failed to grow under similar conditions at the expense of any of 39 other aromatic or flavonoid compounds tested.


1957 ◽  
Vol 8 (1) ◽  
pp. 55 ◽  
Author(s):  
SJ Edmonds

The consumption of oxygen of Dendrostomum cymodoceae at 22'C in aerated sea-water varied from 4-5-5.5 μl/g (wet weight)/hr for adults to 20-31 μ/g/hr for juveniles. The production of carbon dioxide was 13-17 μ/g/hr (juveniles) and the R.Q. varied from 0.55 to 0.67 (juveniles). The rate of consunlption of oxygen decreased as the tension of the dissolved oxygen decreased. The oxygen combined with the pigment of the blood was 2.1 vols. of oxygen per 100 vols. of blood and the ratio of blood volume (ml) to total weight (g) of the animal was 0.47. D. cymodoceae was able to live under anaerobic conditions in sea-water for as long as 5 days and in paraffin oil for 4 days. The haemerythrin in the blood of animals kept under oil was found to be reduced after about 6 hr. Lactic acid was identified as one of the end-products of anaerobiosis. The concentration of lactic acid in the blood of animals living under anaerobic conditions increased after 60 hr from 7-12 to 46-61 μg/ml of blood. The ability to revert to anaerobiosis may have survival value for the species.


Excised pea-root tips were incubated for 4 h in gas mixtures containing 0.00001 to 100% oxygen, in order to determine the effect upon mitosis. Below 0.0005% oxygen, mitosis was completely arrested. Between 0.001 and 0.02% oxygen, cells initially in mitosis completed division, but no more cells started dividing. Between 0.05 and 0.2% oxygen, cells initially in interphase entered division, but did not finish. Above 0.5% oxygen, all cells not prevented from dividing by excision finished division within 4 h. After exposure to 0.05% oxygen for 4 h, an excessive proportion of cells was found in prophase; in 0.1% oxygen an excess of metaphases, and in 0.2% oxygen an excess of telophases resulted. The oxygen uptake and carbon dioxide output of root tips were measured in a range of oxygen tensions and in anaerobic conditions. The relationship between oxygen uptake and oxygen tension was hyperbolic; a half maximum rate of oxygen uptake was obtained at about 10% oxygen. It was concluded that the respiration of root tips was limited by slow diffusion of oxygen through the tissue. From the carbon dioxide output it was estimated that the amount of energy available to isolated root tips under anaerobic conditions was about 1% of that available under aerobic conditions. Possible mechanisms whereby extreme oxygen-lack could arrest mitosis were considered. It was shown that the arrest was not due to abolition of a gross supply of energy. No evidence was obtained as to what other mechanism might be operative. An hypothesis was formulated in an attempt to explain the complicated relationship between mitosis and oxygen tension. It was assumed that the visible phases of mitosis are immediately preceded by a phase with a higher requirement for oxygen than mitosis, and that preceding this is an earlier phase with a lower oxygen requirement than mitosis.


mSphere ◽  
2021 ◽  
Author(s):  
Rohan S. Wakade ◽  
Manning Huang ◽  
Aaron P. Mitchell ◽  
Melanie Wellington ◽  
Damian J. Krysan

Candida albicans is one of the most common causes of fungal infections in humans. C. albicans undergoes a transition from a round yeast form to a filamentous form during infection, which is critical for its ability to cause disease. Although this transition has been studied in the laboratory for years, methods to do so in an animal model of infection have been limited.


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