Carbon Isotopes in Photosynthesis

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Carbon Isotopes in Photosynthesis Carbon Isotopesin Photosynthesis Fractionation techniques may reveal new aspects of carbon dynamics in plants Marion H. O'Leary he efficiencyof photosynthesis Other materials must be converted to continues to interest biochem- Currentstudies include CO2prior to analysis.Plants are ordi- ists, biologists, and plant narily converted to CO2 by combus- physiologists. Scientists interested in finely tuned, carefully tion. Individualcompounds isolated CO2 uptake are concerned about the from plants are sometimesconverted extent to which the uptake rate is controlled isotope to CO2 by chemical or enzymatic limited by such factors as stomatal fractionationsunder degradation. diffusion and the chemistry of the For naturalmaterials (plants, ani- CO2 absorption process. The frac- defined environmental mals, and minerals), R is approxi- tionation of carbon isotopes that oc- mately0.0112, andonly the lastdigit curs during photosynthesis is one of conditions in this ratio varies. For convenience, the most useful techniques for investi- R valuesare generallyconverted to gating the efficiency of CO2 uptake. valuesof 813C, Atmospheric carbon dioxide con- used to study mechanisms of chemical tains approximately 1.1% of the non- (Melander and Saunders 1980) and 1000 813C 3C [R(sample)R ] radioactive isotope carbon-13 and biochemical (Cleland 1982) process- = (standard)- 1 x 1000 98.9% of carbon-12. During photo- es. Isotopes are used in ecology to synthesis, plants discriminate against establish food chains and biological The standard is carbon dioxide ob- C because of small differences in pathways (Fritz and Fontes 1980, tained from a limestone, called PDB, chemical and physical properties im- 1986, Rounick and Winterbourn from the Pee Dee formation in South parted by the difference in mass. This 1986), and isotope studies of tree Carolina (Craig 1957). The units of discrimination can be used to assign are used to recreate cli- 813C are called mil," or A rings past "per 0/0o. plants to various photosynthetic mates (Hughes et al. 1982). Isotope more negative 8 C means more groups. The isotope fractionation studies of plants are related to all or lighter in mass; a more positive also reflects limitations on photosyn- these areas, because their basis is in 813C means more 13C, or heavier. thetic efficiency imposed by the vari- fundamental chemical processes, and Most natural materials have negative ous diffusional and chemical compo- many of their applications are in the 813C values because they contain less nents of CO2 uptake. When analyzed area of ecology (O'Leary 1981, 13C than the standard. The precision in detail, this fractionation provides Troughton 1979, Vogel 1980). Re- of modern mass spectrometers is at information .about water use efficien- cently developed methods are allow- least ?i0.02 %o0, but sample prepara- cy and indicates that different strate- ing biologists to examine in greater tion errors may bring the total repro- gies are needed for improving water- detail the carbon flow in plants. ducibility of measurements on plant use efficiency in different kinds of materials to 10.2 0/0o. Thus, interpre- plants. Measurement of carbon tations based on differences smaller fractionation in than 1 should be made with Isotope simple isotopes o/ physical and chemical processes is caution. well understood and is commonly The "3C content of carbon dioxide is In the absence of industrial activity, usually determined with a mass spec- the 813C value of atmospheric CO2 is This value for the atmo- Marion H. is a in the trometer specially designed for high- -8 0/oo. O'Leary professor measurement of the ratio is more of Chemistryand Biochem- precision R, sphere slowly becoming nega- Departments combustion of fossil istry at the University of Wisconsin in defined by tive due to the Madison 53706. ? 1988 AmericanInsti- fuel (813C for fossil fuel is approxi- R = -30 tute of BiologicalSciences. 3CO2/12CO2 mately %/oo) (Hoefs 1980). 328 BioScience Vol. 38 No. 5 This content downloaded from 129.236.31.165 on Wed, 09 Sep 2015 19:33:03 UTC All use subject to JSTOR Terms and Conditions Isotopevalues of plants In the 1950s, Craig (1953, 1954) and Baertschi(1953) measured813C val- ues of a variety of natural materials, including plants (reviewed by O'Leary1981). They found that most plants had 813Cvalues in the range -25 to -35 0o/0. They failed to find large species or environmentaleffects on thesevalues. The plants in these initial studies were C3 plants, which fix principally .. !!i CO2 by the action of the enzyme .... ..... .. .. ..... .. ii . ! .iiiii~•iiii:i. ..........".. i i ?iY :ii•: . ribulose bisphosphate carboxylase. ii iil! iii iii.. :.... The C4 photosynthetic pathway, in ..... xt.::::I : . .i ??'?'':ii ::: :ii: ?::::N which CO2 is initially taken up N ... .... i~•?••,•.,,=•iiiiN ii. .i.:. -? .. through carboxylation of phospho- }.ii= X:': ........ was discovered in the ......... .. enolpyruvate, i??? ? ....: .. ,~i;:;~,:l~...il..i..i..........=i 1960s. Following this discovery, .. ?. Bender see also Smith (1968, 1971; -0 -!1_ -14 -16 -18 -20 -i2 -2.4 -26 -2•8 -30 -32• -34 and Epstein1971) discoveredthat C4 AE13r plants are isotopically distinct from C3 plants. C3 plants have 813Cvalues Figure1. Histogramshowing the distributionof 813Cvalues of plantmaterials. This of approximately -28 0/0o, whereas figureis basedon about1000 analysesperformed in fivedifferent laboratories. C4 plants are approximately -14 0/o In subsequentyears, a number of laboratoriesaround the world made fractionationhas a positive sign when boxylation step itself. Severalmathe- similar measurementson thousands 13Cis transformedmore slowly than matical models have been suggested of plants species and established a 12C (as is the case in most physical (Deleens et al. 1983, Farquharet al. clear distinction between C3 and C4 and chemicalprocesses).1 1982, O'Leary 1981, Peisker 1982, plants (Figure 1), with little overlap Many physical, chemical, and bio- 1984, 1985), all of which are based betweenthe two distributions.There- chemical processes have significant on the componentfractionations giv- fore, 13Canalysis has become a stan- isotope fractionations(Cleland 1982, en in Table 1. The overall fraction- dardtest for determiningthe pathway Melanderand Saunders1980). Frac- ation in such a complex system is a of CO2 fixation. What is the bio- tionations can occur both in time- combination of these components, chemicalsource of this difference? dependent processes (chemical reac- but it is not simply the sum of a series tions and transport) and in of individualfractionations-instead, Fractionationsin chemical and equilibriumprocesses (chemical equi- the fractionation mostly reflects the libria, dissolution, and phase rate-limitingstep or steps (i.e., those physicalprocesses changes), and both are importantin with the highest resistivity).As a step Plantscontain less '3Cthan the atmo- plants. Table 1 shows isotope frac- becomes more limiting, the observed sphere because the physical and tionations for processes of impor- fractionation approaches the frac- chemical processes involved in CO2 tance in photosynthesis. tionation for that step. uptakediscriminate against 13C. This The importantsteps in CO2 uptake discriminationoccurs because '3C is Theory of isotope in C3plants are shown in Figure2. In heavier than 12C and forms slightly fractionationin the first step, external CO2 is trans- strongerchemical bonds. In addition, plants ported through the boundary layer diffusionof '3CO2 is slower than that The principalfactor affectingthe iso- and the stomata into the internalgas of 12CO2because of this difference in topic compositions of leaves is the space. This process is always to some mass. For the conversion of com- isotope fractionation accompanying extent reversible.Internal CO2 then pound A into compound B, the iso CO2uptake. Followinginitial sugges- dissolvesin the cell sap and diffusesto tope fractionation is defined by tions of Craig (1953), Smith and Ep- the chloroplast,where carboxylation stein (1971), and others occurs. Because the - (O'Leary carboxylation [813C(A) 8'3C(B)] 1981), models for plant isotope frac- step is irreversible,steps subsequent 1 + 813C(A)/1000 tionation have focused on the physi- to carboxylationare not importantin cal and chemicalprocesses accompa- determiningthe isotope fractionation. This fractionation has units of o. nying CO2 uptake, including Both dissolving and diffusion show To avoid confusion with ordinary diffusion, dissolution, and the car- small isotope fractionations(Table 1), 813C values (which represent isotopic but the largest fractionation is that compositions, rather than fraction- 'However,note that some workersin the field connectedwith carboxylation (29 o/o). ations), we call this value A8. The use the opposite sign convention. It is generallyassumed that dissolu- May 1988 329 This content downloaded from 129.236.31.165 on Wed, 09 Sep 2015 19:33:03 UTC All use subject to JSTOR Terms and Conditions Table 1. Carbon isotope fractions associated with photosynthesis. photorespiration), then we could breeda that would take up CO2 Reference plant Process A, 0/00oo* more rapidly without sacrificingwa- ter-useefficiency. The alternativepos- Equilibria diffusive resist- Solubilityof CO2 in water 1.1 O'Leary1984 sibility, decreasing Hydrationof CO2 -9.0 Mook et al. 1974 ance, has only a very limitedpotential for increasing CO2 uptake, and this Transportprocessest increasewould come at a substantial CO2diffusion in air 4.4 O'Leary1981
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