Biological production of carbon monoxide has been reported in algae (3, 7), in fungi (16), in higher plants (10,18), in siphonophores (19), and in man (12,17). It is now well established that during the breakdown of hemoglobin in senescent erythrocytes in humans, the heme ring is cleaved by removal of the a-methyne bridge carbon which is then oxidized to CO with the concomitant formation of bile pigment and iron (13). Recent work in this laboratory has shown that during the formation of phycocyanobilin, equimolar quantities of CO are similarly produced (15). Although CO can be measured by mass spectrometry (2), by gas chromatography (5), or by nondispersive infrared analysis (1), these methods require the availability of costly equipment and preclude certain kinds of metabolic experimentation on CO biosynthesis from radiolabeled precursors. The present paper describes, therefore, an inexpensive method for determining biological CO production in algae, which is generally adaptable to studies on CO formation in plants. Figure 1A. At 4-to 15-hr intervals, estimates of phycocyanobilin synthesized in the suspension (9) and of CO present in the gas reservoir were made.
MATERIALS AND METHODSCO Measurement. CO accumulated in the gas reservoir was passed through the train assembly shown in Figure lB RESULTS AND DISCUSSION The train shown in Figure 1B is designed to measure CO as catalytically derived CO2 after removal of CO2 (not derived) from the sample gas. In calibration experiments, 22.3 and 44.6 t-moles of CO, representing 0.5 and 1.0 ml of the pure gas, were injected with a tuberculin syringe into 95% 02-5% CO., contained in a 2-liter glass suction flask. The sample gas was then forced through the train by displacement from the flask with water. Under these conditions, recoveries of CO as derived CO2 exceeded 95% (Table I). Titration of alkali in the test trap (VI) preceding the Hopcalite catalyst (VIII) revealed that bicarbonate was lacking, which shows that the Baralyme, Ascarite, and NaOH absorbers had efficiently removed CO. from the gas sample.For calibration of the train with "CO standards (New England Nuclear, Boston, Mass.; 4.5 mc/mmole) radiolabeled CO was mixed with carrier gas as above and passed through the train. The disintegrations per minute in derived "CO2 were determined by driving "C-labeled bicarbonate from solution after titration of the residual alkali in the terminal traps (IX) to pH 8.5. "CO.. was collected in 5 ml of ethanolamine-methoxvethanol (2:1) and counted in 15 ml of toluene-methoxyethanol (2:1) containing 4 g/liter of 2,5-bis-2(tertiarybutylbenzoxazolyl)-,B-thiophene (Packard Instrument Co., Downers Grove. Ill.). All counting was done in a Tri-Carb liquid scintillation spectrometer. and the quench in each vial was determined by the addition of toluene-"C internal standard.The recovery of 33.0 and 34.0 1cmoles of "CO placed in 2 liters of 95%-0-5%o CO. and passed through the train was 376 www.plantphysiol.org on May 8, 2018 -Published by Downloaded from