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<strong>Plant</strong> Physiol. (1979) 64, 735-738<br />

0032-0889/79/64/0735/04/$00.50/0<br />

<strong>Photosynthesis</strong> <strong>and</strong> <strong>Photorespiration</strong> <strong>in</strong> <strong>Whole</strong> <strong>Plant</strong>s of Wheat<br />

Received for publication February 27, 1979 <strong>and</strong> <strong>in</strong> revised form May 30, 1979<br />

ALAIN GERBAUD AND MARCEL ANDRE<br />

Departement de Biologie, Service de Radioagronomie, C.E.N. Cadarache Bofte Postale 1, No. 13115 Sa<strong>in</strong>t-<br />

Paul-Lez-Durance, France<br />

ABSTRACT<br />

Wheat was cultivated <strong>in</strong> a small phytotronic chamber. 1802 was used to<br />

measure the 02 uptake by the plant, which was recorded simultaneously<br />

with the 02 evolution, net CO2 uptake, <strong>and</strong> transpiration. At normal<br />

abtospheric CO2 concentration, photorespiration, measured as 02 uptake,<br />

was as important as the net photosynthesis. The level of true 02 evolution<br />

was <strong>in</strong>dependent of CO2 concentration <strong>and</strong> stayed nearly equal to the sum<br />

of net CO2 photosynthesis <strong>and</strong> 02 uptake. We conclude that at a given<br />

light <strong>in</strong>tensity, 02 <strong>and</strong> CO2 compete for the reduc<strong>in</strong>g power produced at<br />

constant rate by the light reactions of photosynthesis.<br />

<strong>Photorespiration</strong> is commonly measured us<strong>in</strong>g carbon isotopes.<br />

Such methods give the CO2 efflux from the plant, but are <strong>in</strong>evitably<br />

biased by the recycl<strong>in</strong>g of CO2 (21). The measurement of<br />

photorespiratory 02 uptake does not have the same drawback<br />

(22). Although the technique of 1802 has been used with algae (14,<br />

19), it has seldom been applied to higher plants. Mulchi et aL (15),<br />

Dimon (10), <strong>and</strong> Berry et aL (6) have shown an important uptake<br />

of 1802 <strong>in</strong> various plants, but limited their scope to the CO2<br />

compensation po<strong>in</strong>t. The method was also applied to C4 plants <strong>in</strong><br />

the presence of CO2 (1, 24), show<strong>in</strong>g a respiration identical <strong>in</strong> light<br />

<strong>and</strong> darkness at normal CO2 concentration <strong>and</strong> the <strong>in</strong>crease of<br />

light respiration at lower concentrations. The only measurements<br />

of the 02 uptake of C3 plants <strong>in</strong> conditions of photosynthesis were<br />

made by Volk <strong>and</strong> Jackson (23) <strong>and</strong> Ozbun et al. (16) With bean<br />

leaves the latter found an 02 uptake which was only 9%o of the<br />

photosynthesis; but the significance of this result is lessened by<br />

the weakness of the illum<strong>in</strong>ation used (300-1,500 ft-c). Furthermore,<br />

they did not f<strong>in</strong>d an <strong>in</strong>crease of the rate of 02 uptake with<br />

higher light <strong>in</strong>tensities, whereas it is currently thought that the rate<br />

of photorespiration <strong>in</strong>creases with higher light <strong>in</strong>tensities (8, 12,<br />

25)<br />

Ẇe found it useful to <strong>in</strong>vestigate the 02 exchange of a C3<br />

(wheat) <strong>in</strong> conditions approach<strong>in</strong>g those <strong>in</strong> the field: the plant was<br />

<strong>in</strong>tact, light <strong>in</strong>tensity <strong>and</strong> photosynthetic rate were high; CO2 was<br />

regulated first at normal, then at high <strong>and</strong> low levels.<br />

MATERIALS AND METHODS<br />

PLANT AND GROWTH CHAMBER<br />

The experiment was conducted on a whole plant of wheat<br />

(Triticum aestivum L., var. Chample<strong>in</strong>), aged 42 to 52 days. The<br />

plant was grown from a few days after sow<strong>in</strong>g a 7.7-liter growth<br />

chamber, a reduced design of the C23A system previously described<br />

(2). Day (14 h)/nght (10 h) temperatures were 20.5 ± 0.6<br />

C/18.5 + 0.6 C. The visible light measured at plant midheight<br />

(175 w m-2) was not saturat<strong>in</strong>g. The root compartment was<br />

separated from the aerial part by an air-tight putty jo<strong>in</strong>t. The roots<br />

dipped <strong>in</strong> a beaker conta<strong>in</strong><strong>in</strong>g 2.3 liters of Arnon-Hoagl<strong>and</strong> No.<br />

2 solution with iron as FeSO4 (3), which was changed every day<br />

before light<strong>in</strong>g <strong>and</strong> was aerated by bubbl<strong>in</strong>g with C02-free air. A<br />

s<strong>in</strong>gle seed grew to a tuft of up to 25 tillers with about 20 leaves.<br />

As the plant did not undergo the w<strong>in</strong>ter frosts, it did not flower<br />

<strong>and</strong> the formation of tillers went on for 70 days <strong>and</strong> more. Dur<strong>in</strong>g<br />

the 10 days of the experiment the photosynthesis <strong>in</strong>creased by 2%<br />

per day up to 0.5 liter CO2 per day <strong>and</strong> the relative growth rate<br />

calculated from the cumulative CO2 uptake was 5% per day.<br />

METHODS<br />

<strong>Photosynthesis</strong> <strong>and</strong> dark respiration were determ<strong>in</strong>ed by quantitative<br />

monitor<strong>in</strong>g of the CO2 concentration <strong>in</strong> the cell through<br />

<strong>in</strong>jection of pulses of CO2 or CO2 trapp<strong>in</strong>g <strong>and</strong> transpiration by<br />

the uptake of water by the roots (2, 3).<br />

To regulate 02 pressure <strong>in</strong> the chamber at 20%Yo, one should<br />

dilute every volume of 02 produced by the plant by four volumes<br />

of N2. Practically we dilute the <strong>in</strong>jected CO2 <strong>in</strong> about four (exactly<br />

k = 3.44) volumes of N2. In fact, dur<strong>in</strong>g the night, 02 concentration<br />

dim<strong>in</strong>ishes as a consequence of dark respiration; dur<strong>in</strong>g the day,<br />

it goes up aga<strong>in</strong> toward an equilibrium concentration. These<br />

oscillations do not exceed 1%.<br />

Gas concentrations were measured every 20 m<strong>in</strong> by a quadripolar<br />

mass spectrometer Riber QMM 17; CO2 concentration was<br />

cont<strong>in</strong>uously measured by an URAS II A <strong>in</strong>frared analyzer. All<br />

raw data were recorded <strong>and</strong> processed <strong>in</strong> real time by a Telemecanique<br />

T 1600 computer which gave them back as files of hourly<br />

<strong>and</strong> daily means <strong>and</strong> curves. The computer also controlled the<br />

<strong>in</strong>jections of CO2 <strong>in</strong>to the chamber (or CO2 trapp<strong>in</strong>g at night) to<br />

regulate its level at any present level.<br />

02 uptake was measured accord<strong>in</strong>g to the follow<strong>in</strong>g pr<strong>in</strong>ciple:<br />

a small quantity of nearly pure 1802 is <strong>in</strong>troduced <strong>in</strong>to the air-tight<br />

chamber. The concentration of 1'802 dim<strong>in</strong>ishes afterwards due to<br />

two causes: (a) the plant takes up 1802 as well as 1602 <strong>in</strong> the<br />

processes of photorespiration <strong>and</strong> respiration. (b) the <strong>in</strong>jections of<br />

CO2 <strong>and</strong> N2 result <strong>in</strong> a nearly equal volume of the gas <strong>in</strong> the<br />

chamber be<strong>in</strong>g swept out. This second phenomenon is measured<br />

by the progressive dilution of a reference gas. We chose Neon<br />

(isotope 20), as it is neutral to the plant <strong>and</strong> is present only <strong>in</strong><br />

trace amounts <strong>in</strong> the atmosphere. We use the follow<strong>in</strong>g symbols:<br />

V: volume of the chamber, dv: volume swept out of the chamber<br />

<strong>in</strong> time dt; u: rate of 02 uptake; U: daily mean rate of 02 uptake<br />

= (l/T) fT u.dt; o, T: <strong>in</strong>itial <strong>and</strong> f<strong>in</strong>al time of day; pc: rate of net<br />

photosynthesis (CO2); P,: daily mean rate of net photosynthesis<br />

(CO2) = (I/T) fT pc dt; PO daily mean rate of net photosynthesis<br />

(02)-<br />

The volume dv of gas go<strong>in</strong>g out of the cell <strong>in</strong> time dt conta<strong>in</strong>s<br />

[Nel. dv of neon gas, so the decrease of Ne is<br />

V.d[Ne] = - [Nel . dv or d[Ne] / [Ne] = - dv/V (1)<br />

The decrease of 1802 is due to both displacement, <strong>and</strong> plant<br />

uptake u.dt:<br />

735<br />

Downloaded from www.plantphysiol.org on January 11, 2014 - Published by www.plant.org<br />

Copyright © 1979 American Society of <strong>Plant</strong> Biologists. All rights reserved.


736<br />

[180<br />

V. d[ 180 = [180 . dv - 2 u. dt<br />

2 2 [16Q is<br />

I 02] + I 0 ]<br />

dl[ 180 -dv u.dt/V<br />

[180] V 1[1602] + [180 ]<br />

By subtract<strong>in</strong>g equation I from equation 3:<br />

GERBAUD AND ANDRE <strong>Plant</strong> Physiol. Vol. 64, 1979<br />

The comparison of the P, derived from this formula with the value<br />

(2) already known is a test of the validity of our measures.<br />

PHYSIOLOGICAL VALUE OF THE MEASUREMENTS<br />

The measure of the true rate of 02 uptake can be biased by two<br />

(3) causes. (a) If the 02 from photosynthesis is taken up as well as the<br />

external 02 <strong>in</strong> the process of photorespiration, then our measurement<br />

will be less than the true rate. This sort of recycl<strong>in</strong>g seems to<br />

be neligible, due to the high relative pressure of the outer 02 (22).<br />

d[ 80 1 d[Ne] - u.dt/V<br />

1 2] [Ne] 160 ] + [ 180<br />

Dur<strong>in</strong>g the course of the day, the total 02 concentration [02] stays<br />

<strong>in</strong> the range 21 to 22%, so that we may consider it as a constant <strong>in</strong><br />

the <strong>in</strong>tegration of equation 4:<br />

(4)<br />

z<br />

0<br />

z<br />

8<br />

Trd[Ne] d[ 1802 2<br />

1 T<br />

=Fu.dt<br />

INe 118 O<br />

Jo [Ne] [ °2]- [02].V 0<br />

Hence:<br />

[02] *V I[0210 [Ne]1<br />

U = <strong>in</strong> TJ<br />

[[118021 [NeIT<br />

(5)<br />

(6)<br />

The net 02 evolution P0 was calculated from the <strong>in</strong>crease of 02<br />

concentration <strong>in</strong> the chamber. In the unit time the plant assimilates<br />

a volume Pc of CO2, (k+ 1) Pc of the mixture (CO2 + kN2) is<br />

<strong>in</strong>jected <strong>in</strong>to the chamber <strong>and</strong> the plant produced P0 of 02;<br />

therefore the follow<strong>in</strong>g volume must be expelled from the chamber:<br />

Lv<br />

=<br />

(k+1)Pc<br />

+<br />

P0 - Pc<br />

or<br />

Av<br />

=<br />

k.P c<br />

+P<br />

(7)<br />

conta<strong>in</strong><strong>in</strong>g an amount 11602] Av of 1602.<br />

The plant produces only 1602, <strong>and</strong> <strong>in</strong> our case 1802 is about 50<br />

times less concentrated <strong>in</strong> the cell than 1602, so that we shall<br />

equate here the uptake of 1602 with the total 02 uptake U. Hence<br />

the <strong>in</strong>crease of 1602 <strong>in</strong> the chamber is:<br />

V A[ 16 ] 1<br />

T<br />

0 2<br />

1 [ + k p [16<br />

T<br />

1160<br />

L<br />

2<br />

'r 64<br />

(8) .f<br />

-E<br />

z<br />

(9) o<br />

w<br />

A<br />

HOURS<br />

C02<br />

0 x<br />

D<br />

a<br />

a<br />

k.<br />

- 2C<br />

From P. we calculate the photosynthetic ratio po/PC. The gross 02<br />

evolution E was calculated from the net evolution plus the uptake:<br />

E = PO + U.<br />

Test of <strong>Photosynthesis</strong>. There is another way of measur<strong>in</strong>g<br />

photosynthesis than count<strong>in</strong>g the pulses of <strong>in</strong>jected CO2: the<br />

decrease of neon concentration is related to volume dv, (eq. 1),<br />

which is proportional to the photosynthesis, because AV = k<br />

Pc+P0 <strong>in</strong> equation 7 can be replaced with<strong>in</strong> a good approximation<br />

by (k+ 1) Pc, that is, set <strong>in</strong> the differential form: dv = (k+ 1) Pcdt,<br />

hence:<br />

d[Ne] / [Ne] = - (k+1) pC.dt / V (10)<br />

1 T dN 1 [me]0<br />

= 1T kV1 d{Ne] = 1 V n (11)<br />

P =<br />

_ln ---<br />

c T k+1 o [Ne] T k+1 [HeiT<br />

0<br />

-<br />

y 2( to -10DO<br />

Y.<br />

R<br />

I-<br />

- T<br />

n n n<br />

of I I 1- 1 a I I I I I I 0<br />

Q, I - - - - - "<br />

2 4 6 8 10 12 1x 16 18 20 22 24<br />

HOURS<br />

FIG. 1. Recorded data dur<strong>in</strong>g a typical day of a 46-day-old plant of<br />

wheat (day/night temperature 20.3 C/18.4 C, PAR irradiance 175 w m-2,<br />

02= 21%, CO2 = 335 ,l/1). The two parts show <strong>in</strong> parallel the time course<br />

of the gas exchanges (A), <strong>and</strong> the isotopic concentrations (B). PR: net<br />

photosynthesis (C02); R: night respiration; T: transpiration. The decrease<br />

of 1802 traces the 02 traces the 02 uptake by the plant, us<strong>in</strong>g Ne as an<br />

<strong>in</strong>ternal st<strong>and</strong>ard. The slight variations of 1602 correspond to the photosynthesis<br />

or respiration. Initial concentrations were [18021 = 2970,l/1, [Ne]<br />

= 3,160 ul/l; isotopes were added before the beg<strong>in</strong>n<strong>in</strong>g of the light periods<br />

when their concentrations went under 0.5%.<br />

Downloaded from www.plantphysiol.org on January 11, 2014 - Published by www.plant.org<br />

Copyright © 1979 American Society of <strong>Plant</strong> Biologists. All rights reserved.


(b) If the absorbed 02 is recycled through the plant <strong>in</strong>to the<br />

atmosphere, our measure will also be underestimated.<br />

Dimon (10) has shown <strong>in</strong> short term experiments (1 h) that<br />

plants do not discrim<strong>in</strong>ate between isotopes of 02 <strong>and</strong> the photosynthetic<br />

02 is not enriched <strong>in</strong> 1802. We have checked that no 1802<br />

is released from the plant even after several days of 1802 consumption.<br />

As the evolved 02 comes from water, which has only<br />

one atom of 02, any evolved 180 would be predom<strong>in</strong>antly <strong>in</strong><br />

18016O molecules. As we detect no enrichment of the evolved 02<br />

<strong>in</strong> 18016O, we consider that there is no recycl<strong>in</strong>g of the photorespiratory<br />

02-<br />

From these two po<strong>in</strong>ts we conclude that the disappearance of<br />

1802 from the atmosphere is a good measure of the true flux of 02<br />

<strong>in</strong> photorespiration.<br />

RESULTS AND DISCUSSION<br />

Normal CO2 Level. Figure 1 shows the data obta<strong>in</strong>ed with a<br />

plant of wheat dur<strong>in</strong>g the course of a typical day at normal CO2<br />

level (average 335 t,ll). Net photosynthesis P, calculated from the<br />

number of pulses of <strong>in</strong>jected CO2 is 43 ml/h. As a verification, net<br />

photosynthesis, as seen by neon (equation 11) is 45 ml/h. From<br />

the curves of Ne <strong>and</strong> 1802 we calculate U = 43 ml/h, that is, as<br />

much as Pc. From the <strong>in</strong>crease of 1602 concentration (from 20.6 to<br />

21.5%), we calculate the net 02 evolution PO = 46 ml/h <strong>and</strong> the<br />

gross 02 evolution E = 88 ml/h. The photosynthetic ratio P./PC<br />

is 1.07. Other experiments <strong>in</strong> the same conditions give U/P, =<br />

1.02 ± 0.05 (four measures) <strong>and</strong> P./P, = 1.05 ± 0.02. We also<br />

found the same P./P, at other CO2 concentrations <strong>and</strong> the same<br />

U/Pc at half-light <strong>in</strong>tensity (experiment not described here).<br />

PHOTORESPIRATION IN WHEAT<br />

<strong>Plant</strong> Physiol. Vol. 64, 1979 737<br />

Our estimation of the importance of photorespiration is much<br />

larger than the most frequently found values: many authors<br />

estimate the CO2 evolution <strong>in</strong> the light from one-sixth to one-half<br />

of the apparent photosynthesis (8, 12, 25). These differences arise<br />

primarily from the difficulty <strong>in</strong> measur<strong>in</strong>g the CO2 evolution (12).<br />

It is known that all measures us<strong>in</strong>g '3C or "C, even corrected for<br />

the biochemical recycl<strong>in</strong>g of the assimilated carbon, are still<br />

underestimated because photorespired CO2 is recycled <strong>in</strong>to photosynthesis,<br />

to an extent depend<strong>in</strong>g on the different diffusion<br />

resistances <strong>in</strong> the pathway of CO2 (21). This recycl<strong>in</strong>g could even<br />

be complete, prevent<strong>in</strong>g any release of CO2 (4) at normal CO2<br />

level. On the other h<strong>and</strong>, the present results are <strong>in</strong> agreement with<br />

the observed stimulat<strong>in</strong>g effect of low 02 pressures on plant<br />

growth: + 90%o for dry weight <strong>in</strong> Mimulus card<strong>in</strong>alis (7), + 103%<br />

<strong>in</strong> soybean (18), + 90 to 106% <strong>in</strong> Phaseolus vulgaris (17). Park<strong>in</strong>son<br />

et al. (17) observed that such an effect corresponds to an <strong>in</strong>crease<br />

of the photosynthetic efficiency of up to 100/o at 5% 02 concentration.<br />

The order of magnitude of the flux of 02 raises the problem of<br />

its pathway(s). We know that atmospheric 1802 labels glycolate<br />

<strong>and</strong> further metabolites of the glycolate pathway, as well as the<br />

evolved CO2 (5, 6, 11), but it is not established if all of the<br />

absorbed 02 goes <strong>in</strong>to the glycolate pathway, which should then<br />

be as active as the Calv<strong>in</strong> cycle (13). Otherwise, other reactions,<br />

such as the pure Mehler reaction (pseudocycic electron flow),<br />

have to occur concurrently (10).<br />

Response to Various CO2 Levels. For 10 days we subjected the<br />

plant to low (200 A1/1), normal (300-400 1il/l), <strong>and</strong> high (680-<br />

12,000 p1/l) CO2 levels; each level was ma<strong>in</strong>ta<strong>in</strong>ed for I or 2 days<br />

-1 I I I I I<br />

41 42 43 44 45 46 47 48 49 50 51 52<br />

DAYS AFTER SOWING<br />

FIG. 2. Gas exchange of a plant of wheat at various CO2 levels. U: photorespiration (02 uptake <strong>in</strong> light); E: gross 02 evolution: Pc + U: photosynthesis<br />

+ photorespiration. Other symbols <strong>and</strong> conditions, except CO2, are as <strong>in</strong> Figure 1.<br />

Downloaded from www.plantphysiol.org on January 11, 2014 - Published by www.plant.org<br />

Copyright © 1979 American Society of <strong>Plant</strong> Biologists. All rights reserved.


738<br />

GERBAUD AND ANDRE <strong>Plant</strong> Physiol. Vol. 64, 1979<br />

-c 75<br />

A a E 1/ A A 4<br />

z<br />

0<br />

P 50<br />

_<br />

IC<br />

A<br />

.-I<br />

0<br />

w<br />

0<br />

w 25<br />

a-<br />

/~~~~<br />

/~~~~~~~~~<br />

n<br />

0 200 400 600 800 12000<br />

CO2 (p.l-1)<br />

FIG. 3. Gas exchange of a plant of wheat as a function of CO2 concentration. Data were comparable by correct<strong>in</strong>g them for the size of the plant,<br />

suppos<strong>in</strong>g a uniform growth throughout the experiment. Abbreviations as <strong>in</strong> Figures I <strong>and</strong> 2.<br />

(Fig. 2). 02 concentration was always normal. Diurnal transpiration<br />

rates were nearly constant, <strong>in</strong>dicat<strong>in</strong>g that stomata can be<br />

considered open throughout the light periods.<br />

As expected, photosynthetic rates follow the concentration of<br />

CO2 <strong>and</strong> respiration varies as Pc but to a smaller extent: it<br />

dim<strong>in</strong>ishes only 20%o when P is halved.<br />

<strong>Photorespiration</strong> varies oppositely to photosynthesis, so that<br />

their sum P, + U depends only on the age <strong>and</strong> size of the plant.<br />

At high concentrations of CO2, where it is admitted that photorespiration<br />

is <strong>in</strong>hibited, there rema<strong>in</strong>s some 02 uptake, about 10%<br />

of Pc; we suppose this is due to the cont<strong>in</strong>uation of night respiration<br />

<strong>in</strong> the light, which appears also <strong>in</strong> maize (1).<br />

Pc + U corresponds to the utilization of reduc<strong>in</strong>g power <strong>in</strong> the<br />

leaves of the plant; its production is measured by the 02 evolution<br />

E. We found E always slightly superior to Pc + U show<strong>in</strong>g that<br />

some reduc<strong>in</strong>g power is also consumed <strong>in</strong> the roots (nitrate reduction).<br />

If we abstract the <strong>in</strong>fluence of plant growth, E appears to be<br />

<strong>in</strong>dependent of CO2 (Fig. 3) <strong>and</strong> P, <strong>and</strong> U follow symmetrical<br />

curves. The mirror effect between Pc <strong>and</strong> U was observed by<br />

Radmer <strong>and</strong> Kok (19) with algae dur<strong>in</strong>g the <strong>in</strong>duction phase of<br />

photosynthesis at constant CO2 level <strong>and</strong>, with a lag time, after<br />

CO2 exhaustion by photosynthesis (20). The ma<strong>in</strong> result of the<br />

present work is the constancy of the gross evolution E under<br />

various conditions of CO2, <strong>in</strong> spite of wide variations of apparent<br />

photosynthesis <strong>and</strong> <strong>in</strong> long steady-state experiments, which shows<br />

that it is not a transient effect but a permanent mechanism. The<br />

permanency of this balance suggests that the electron transport<br />

cha<strong>in</strong> turns over at a constant rate, controlled by the light <strong>in</strong>tensity<br />

<strong>and</strong> <strong>in</strong>dependent of the nature of the f<strong>in</strong>al electron acceptor.<br />

When CO2 concentrations are low the excess of reduc<strong>in</strong>g power<br />

must be trapped by 02 reduction. If the mechanism is blocked for<br />

example by the simultaneous absence of 02 <strong>and</strong> CO2, <strong>in</strong>hibition<br />

or damage occurs (9) because unwanted compounds have to be<br />

reduced <strong>in</strong>stead of 02 or CO2.<br />

Acknowledgments-We are grateful to Mr. A. Daguenet <strong>and</strong> Mrs. J. Massim<strong>in</strong>o for their very<br />

valuable contribution to the experiments.<br />

LITERATURE CITED<br />

1. ANDRE M, A GERBAUD 1979 Consommation d'oxygene pendant la photosynthese chez Zea<br />

mays. CR Acad Sci Paris. In press<br />

2. ANDRE M, D MASSIMINO, A. DAGUENET 1978 Daily patterns under the life cycle of a maize<br />

1 I I I I I I I AI<br />

crop. l. <strong>Photosynthesis</strong>, transpiration, respiration. Physiol <strong>Plant</strong> 43: 397-403<br />

3. ANDRE M, D MASSIMINO, A DAGUENET 1978 Daily patterns under the life cycle of a maize<br />

crop. II. M<strong>in</strong>eral nutrition, root respiration, root excretion. Physiol <strong>Plant</strong> 44: 197-204<br />

4. ANDRE M, C RiCHAUD 1971 Decarboxylation <strong>in</strong> light <strong>in</strong> higher plants studied us<strong>in</strong>g carbon 13.<br />

Second Int Cong <strong>Photosynthesis</strong>, Stresa<br />

5. ANDREWS TJ, GH LORIMER, NE TOLBERT 1971 Incorporation of molecular oxygen <strong>in</strong>to glyc<strong>in</strong>e<br />

<strong>and</strong> ser<strong>in</strong>e dur<strong>in</strong>g photorespiration <strong>in</strong> sp<strong>in</strong>ach leaves. Biochemistry 10: 4777-4782<br />

6. BERRY JA, CB OSMOND, GH LORIMER 1978 Fixation of 02 dur<strong>in</strong>g photorespiration. <strong>Plant</strong><br />

Physiol 62: 954-967<br />

7. BJORKMAN 0, E GAUHL, WM HIESEY, F NICHOISON, NA NoBs 1969 Growth of Mimulus,<br />

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