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Photorespiration: A classroom demonstration1 D. D. Wolf and E. W. Carson2 ABSTRACT An easily implemented test to show biochemical differences between plant species in photorespiration has proved to be an effective addition to the formal classroom lecture. The principle of the test is that leaves in a closed system cause the CO2 concentration (^CO?) to reach characteristic compensation values. The test uses a sodium bicarbonate indicator solution which is blue when in equilibrium with low CO2 atm (created by non-photorespiring species) and green in high CO2 atm (created by photorespiring species). This paper presents several modifications of a simple experiment to demonstrate differences between photorespiring (high CO2 compensation) and non-photorespiring (low CO2 compensation) plants. The method is less costly and less time consuming than that described by Moss (3). The method has also been used in a survey to categorize species and is modified from that described by Tregunna et al. (4). METHODS AND MATERIALS Additional index words: Visual aid. Carbon dioxide. Compensation value. Teaching aid. Two 50-ml beakers (other containers can be used) are placed side-by-side on the bottom of a 1 "D LANTS within both the Monocotyledoneae and Dicotyledoneae classes have distinct anatomical and -biochemical differences, and are subclassified into photorespiring and non-photorespiring groups. Characteristic of the non-photorespiring group are Kranz type, tropical, and C4-dicarboxyIic acid plants; plants having low CO2 compensation; and L syndrome. The identifying term of "nonphotorespiring," however, seems to have gained wide popular acceptance (2, 4, 5). Characteristic of the photorespiring group are C3 and Calvin cycle plants; temperate species; and plants having high CO2 compensation. Including the concept of photorespiration in introductory plant science courses stimulates student interest in the biochemistry of plant -growth, and can help them to relate crop yields to efficient photosynthetic and respiratory mechanisms. liter (1 qt) wide-mouth glass jar. About 30 ml of water are placed in one beaker. The leaf material (preferably with open stomata and a leaf area of at least 10 cm2) is detached, recut under water, and placed in the beaker containing water. About 5 ml of a sodium bicarbonate indicator solution (5 X 10~s M) containing 1% (v/v) Universal Indicator (Fisher Scientific Co.) is placed in the other beaker. The indicator solution will be greenish-yellow and can be stored. A closed system is created by securing the lid on the jar. A cover made of two layers of polyethylene plastic, such as a plastic bag held in place by a rubber band, also seals the jar. The plant material is continuously illuminated by a fluorescent desk lamp having two 40-W bulbs. A change in Contribution of the Agronomy Department, Virginia Polytechnic Institute and State University, Blacksburg, VA 24061. 2 Associate Professor and Professor. 114 JOURNAL OF AGRONOMIC EDUCATION, VOL. 4, AUGUST 1975 Visual demonstrations of biochemical differences between species help to stimulate interests in plant characteristics, e.g., the efficiency of yield capabilities. Any plant material that is photosynthetically active can be used, but the most effective way to standardize the system is to compare the color produced by two plants whose CO2 compensation points are known, for example, corn (low) and bean (high). This procedure builds upon and applies a number of basic concepts—diffusion, chemical equilibria, pH, organic indicators, respiration, and photosynthesis—which usually have been presented previously in chemistry, physics, and biology courses. The basic principles which should be stressed to 5. The Universal Indicator is a complex of pHspecific color indicators that show the pH of the equilibrium buffer solution and, thus, indicate the concentration of CO2 in the atmosphere of the container. Plant material selected should be grown under soil, water, and environmental conditions that would encourage open stomata. With open stomata and in a closed system, the atmospheric CO2 concentration will be reduced to compensation levels by photosynthesis within about 15 min if sufficient leaf area is present. Gentle swirling of the jar will help mix the indicator solution and speed the equilibrium. Time needed for color change will depend on rate of CO2 exchange with the solution and usually will occur in less than 4 hours. The leaves maintain equilibrium for several days. Alternatively, the lights can be turned off to demonstrate respiration. With lights turned on again, the original equilibrium returns. The effect of oxygen on photosynthesis and CO2 compensation value (1) can also be demonstrated in the following way. Set up two of the jars containing similar leaves of a photorespiring species. Flush one jar well with nitrogen before closing the lid. The leaves in the oxygen-free environment will create a lowPCQ 2 value (blue color) demonstrating blockage of photorespiratory processes, while the leaves in normal air will photorespire and create a students are: high/*CO2 value (green color). color of the solution indicates photosynthetically active tissue andPcO 2 reduction. A green solution indicates a PCO2 °f greater than 50 ppm (photorespiring plant), whereas a blue color indicates a low PCO2 °f IGSS than 5 ppm (non-photorespiring plant). The system can be checked by placing a sodium hydroxide solution in the beaker instead of water. Since sodium hydroxide creates a low/ ) CO 2 > the indicator will be blue at equilibrium. Once this experiment is assembled, the demonstration can be set up in a few minutes. RESULTS AND DISCUSSION 1. Under equilibrium conditions, the PCQ2 m the closed atmosphere will depend upon the physiology of the species being tested (photorespirer or non-photorespirer). 2. The concentration of CO2 in the atmosphere of the closed container and the concentration of CO2 dissolved in the indicator solution will attain an equilibrium due to simple diffusion into or out of the solution. 3. The final (equilibrium) concentration of CO2 in the indicator solution will be directly proportional to the concentration of CO2 in the container atmosphere. 4. The dissolved CO2 will chemically react with the water to produce carbonic acid: CO2 + H2O ^ H 2 CO 3 - H+ + HCO3" - H+ + CO32~