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A suitable growth medium must contain all the nutrients required by the organism to be cultivated, and such factors as pH, temperature, and aeration must be carefully controlled. A liquid medium is used; the medium can be gelled for special purposes by adding agar or silica gel. Agar, a polysaccharide extract of a marine alga, is uniquely suitable for microbial cultivation because it is resistant to microbial action and because it dissolves at 100°C but does not gel until cooled below 45°C; cells can be suspended in the medium at 45°C and the medium quickly cooled to a gel without harming them.
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On the previous pages, the function of each type of nutrient is described, and a list of suitable substances presented. In general, the following must be provided: (1) hydrogen donors and acceptors, about 2 g/L; (2) carbon source, about 1 g/L; (3) nitrogen source, about 1 g/L; (4) minerals: sulfur and phosphorus, about 50 mg/L of each, and trace elements, 0.1–1 mg/L of each; (5) growth factors: amino acids, purines, and pyrimidines, about 50 mg/L of each, and vitamins, 0.1–1 mg/L of each.
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For studies of microbial metabolism, it is usually necessary to prepare a completely synthetic medium in which the exact characteristics and concentration of every ingredient are known. Otherwise, it is much cheaper and simpler to use natural materials such as yeast extract, protein digest, or similar substances. Most free-living microbes grow well on yeast extract; parasitic forms may require special substances found only in blood or in extracts of animal tissues. Nevertheless, some parasitic microbes (eg, Treponema pallidum) cannot be grown in vitro or grow inside eukaryotic cells (eg, Chlamydia trachomatis).
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For many organisms, a single compound (eg, an amino acid) may serve as energy source, carbon source, and nitrogen source; others require a separate compound for each. If natural materials for nonsynthetic media are deficient in any particular nutrient, they must be supplemented.
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Hydrogen Ion Concentration (pH)
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Most organisms have a fairly narrow optimal pH range. The optimal pH must be empirically determined for each species. Most organisms (neutralophiles) grow best at a pH of 6.0–8.0, although some forms (acidophiles) have optima as low as pH 3.0, and others (alkaliphiles) have optima as high as pH 10.5.
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Microorganisms regulate their internal pH over a wide range of external pH values by pumping protons in or out of their cells. Acidophiles maintain an internal pH of about 6.5 over an external range of 1.0–5.0, neutralophiles maintain an internal pH of about 7.5 over an external range of 5.5–8.5, and alkaliphiles maintain an internal pH of about 9.5 over an external range of 9.0–11.0. Internal pH is regulated by a set of proton transport systems in the cytoplasmic membrane, including a primary, ATP-driven proton pump and an Na+/H+ exchanger. A K+/H+ exchange system has also been proposed to contribute to internal pH regulation in neutralophiles.
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Different microbial species vary widely in their optimal temperature ranges for growth (Figure 5-2): Psychrophilic forms grow best at low temperatures (–5 to 15°C) and are usually found in such environments as the Arctic and Antarctic regions; psychrotrophs have a temperature optimum between 20°C and 30°C but grow well at lower temperatures. They are an important cause of food spoilage. Mesophilic forms grow best at 30–37°C, and most thermophilic forms grow best at 50–60°C. Some organisms are hyperthermophilic and can grow at well above the temperature of boiling water, which exists under high pressure in the depths of the ocean. Most organisms are mesophilic; 30°C is optimal for many free-living forms, and the body temperature of the host is optimal for symbionts of warm-blooded animals.
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The upper end of the temperature range tolerated by any given species correlates well with the general thermal stability of that species’ proteins as measured in cell extracts. Microorganisms share with plants and animals the heat-shock response, a transient synthesis of a set of “heat-shock proteins,” when exposed to a sudden rise in temperature above the growth optimum. These proteins appear to be unusually heat resistant and to stabilize the heat-sensitive proteins of the cell.
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The relationship of growth rate to temperature for any given microorganism is seen in a typical Arrhenius plot (Figure 5-3). Arrhenius showed that the logarithm of the velocity of any chemical reaction (log k) is a linear function of the reciprocal of the temperature (1/T); because cell growth is the result of a set of chemical reactions, it might be expected to show this relationship. Figure 5-3 shows this to be the case over the normal range of temperatures for a given species; log k decreases linearly with 1/T. Above and below the normal range, however, log k drops rapidly, so that maximum and minimum temperature values are defined.
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Beyond their effects on growth rate, extremes of temperature kill microorganisms. Extreme heat is used to sterilize preparations (see Chapter 4); extreme cold also kills microbial cells, although it cannot be used safely for sterilization. Bacteria also exhibit a phenomenon called cold shock, which is the killing of cells by rapid—as opposed to slow—cooling. For example, the rapid cooling of Escherichia coli from 37°C to 5°C can kill 90% of the cells. A number of compounds protect cells from either freezing or cold shock; glycerol and dimethyl sulfoxide are most commonly used.
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The role of oxygen as hydrogen acceptor is discussed in Chapter 6. Many organisms are obligate aerobes, specifically requiring oxygen as hydrogen acceptor; some are facultative anaerobes, able to live aerobically or anaerobically; some are obligate anaerobes requiring a substance other than oxygen as hydrogen acceptor and are sensitive to oxygen inhibition; some are microaerophiles, which require small amounts of oxygen (2–10%) for aerobic respiration (higher concentrations are inhibitory); and others are aerotolerant anaerobes, which are indifferent to oxygen. They can grow in its presence, but they do not use it as a hydrogen acceptor (Figure 5-4).
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The natural by-products of aerobic metabolism are the reactive compounds hydrogen peroxide (H2O2) and superoxide (O2−). In the presence of iron, these two species can generate hydroxyl radicals (•OH), which can damage any biologic macromolecule:
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Many aerobes and aerotolerant anaerobes are protected from these products by the presence of superoxide dismutase, an enzyme that catalyzes the reaction
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and by the presence of catalase, an enzyme that catalyzes the reaction
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Some fermentative organisms (eg, Lactobacillus plantarum) are aerotolerant but do not contain catalase or superoxide dismutase. Oxygen is not reduced, and therefore H2O2 and O2− are not produced. All strict anaerobes lack both superoxide dismutase and catalase. Some anaerobic organisms (eg, Peptococcus anaerobius) have considerable tolerance to oxygen as a result of their ability to produce high levels of an enzyme (NADH oxidase) that reduces oxygen to water according to the reaction
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Hydrogen peroxide owes much of its toxicity to the damage it causes to DNA. DNA repair-deficient mutants are exceptionally sensitive to hydrogen peroxide; the recA gene product, which functions in both genetic recombination and repair, has been shown to be more important than either catalase or superoxide dismutase in protecting E coli cells against hydrogen peroxide toxicity.
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The supply of air to cultures of aerobes is a major technical problem. Vessels are usually shaken mechanically to introduce oxygen into the medium or air is forced through the medium by pressure. The diffusion of oxygen often becomes the limiting factor in growing aerobic bacteria; when a cell concentration of 4–5 × 109/mL is reached, the rate of diffusion of oxygen to the cells sharply limits the rate of further growth.
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Obligate anaerobes, on the other hand, present the problem of oxygen exclusion. Many methods are available for this: Reducing agents such as sodium thioglycolate can be added to liquid cultures, tubes of agar can be sealed with a layer of petrolatum and paraffin, the culture vessel can be placed in a container from which the oxygen is removed by evacuation or by chemical means, or the organism can be handled within an anaerobic glove box.
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Ionic Strength and Osmotic Pressure
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To a lesser extent, such factors as osmotic pressure and salt concentration may have to be controlled. For most organisms, the properties of ordinary media are satisfactory; however, for marine forms and organisms adapted to growth in strong sugar solutions, for example, these factors must be considered. Organisms requiring high salt concentrations are called halophilic; those requiring high osmotic pressures are called osmophilic.
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Most bacteria are able to tolerate a wide range of external osmotic pressures and ionic strengths because of their ability to regulate internal osmolality and ion concentration. Osmolality is regulated by the active transport of K+ ions into the cell; internal ionic strength is kept constant by a compensating excretion of the positively charged organic polyamine putrescine. Because putrescine carries several positive charges per molecule, a large drop in ionic strength is effected at only a small cost in osmotic strength.