Abstract:Fractionation of carbon isotopes (13C/12C) by glycine decarboxylase (GDC) was investigated in mitochondrial preparations isolated from photosynthetic tissues of different plants (Pisum, Medicago, Triticum, Hordeum, Spinacia, Brassica, Wolffia). 20 mM glycine was supplied to mitochondria, and the CO2 formed was absorbed and analyzed for isotopic content.CO2 evolved by mitochondria of Pisum was enriched up to 8 %o in 12C compared to the carboxylic atom of glycine. CO2 evolved by mitochondria of the other plan… Show more
“…He proposed also that carbon isotope fractionation during photosynthesis is connected at least in part to depletion of CO 2 by Rubisco and its release during glycine decarboxylation (Ivlev, 1989). Subsequent studies have experimentally verified this hypothesis (Ivlev et al, 1996;Igamberdiev et al, 2001Igamberdiev et al, , 2004.…”
“…He proposed also that carbon isotope fractionation during photosynthesis is connected at least in part to depletion of CO 2 by Rubisco and its release during glycine decarboxylation (Ivlev, 1989). Subsequent studies have experimentally verified this hypothesis (Ivlev et al, 1996;Igamberdiev et al, 2001Igamberdiev et al, , 2004.…”
“…Theory predicts interactions between f and e, but these are minor across the range of plausible f values (Tcherkez, 2006). The in vitro estimates of g for different C 3 species (Table II) span a large range of 216& to 18& (Ivlev et al, 1996;Igamberdiev et al, 2001;Ivlev, 2001). However, these results cannot easily be related to f. The measurements were performed on purified enzymes or isolated mitochondria at a range of pH values and with various cofactors (e.g.…”
The magnitude of fractionation during photorespiration and the effect on net photosynthetic 13 C discrimination (D) were investigated for three Senecio species, S. squalidus, S. cineraria, and S. greyii. We determined the contributions of different processes during photosynthesis to D by comparing observations (D obs ) with discrimination predicted from gas-exchange measurements (D pred ). Photorespiration rates were manipulated by altering the O 2 partial pressure (pO 2 ) in the air surrounding the leaves. Contributions from 13 C-depleted photorespiratory CO 2 were largest at high pO 2 . The parameters for photorespiratory fractionation (f ), net fractionation during carboxylation by Rubisco and phosphoenolpyruvate carboxylase (b), and mesophyll conductance (g i ) were determined simultaneously for all measurements. Instead of using D obs data to obtain g i and f successively, which requires that b is known, we treated b, f, and g i as unknowns. We propose this as an alternative approach to analyze measurements under field conditions when b and g i are not known or cannot be determined in separate experiments. Good agreement between modeled and observed D was achieved with f 5 11.6& 6 1.5&, b 5 26.0& 6 0.3&, and g i of 0.27 6 0.01, 0.25 6 0.01, and 0.22 6 0.01 mol m 22 s 21 for S. squalidus, S. cineraria, and S. greyii, respectively. We estimate that photorespiratory fractionation decreases D by about 1.2& on average under field conditions. In addition, diurnal changes in D are likely to reflect variations in photorespiration even at the canopy level. Our results emphasize that the effects of photorespiration must be taken into account when partitioning net CO 2 exchange of ecosystems into gross fluxes of photosynthesis and respiration.
“…Dark respiration and photorespiration were shown to cause 13 C enrichment of respired CO 2 relative to the plant material (cf. Ivlev, Bykova & Igamberdiev 1996;Duranceau et al 1999;Ghashghaie et al 2001), which, depending on the respiration rate, may significantly deplete the plant material. Duranceau et al (1999) found a depletion of 1‰ in the plant material, which was attributed to dark respiration.…”
Section: Annual Cyclicity In D D D D 13 Cmentioning
In the present study, the high-resolution stable carbon ( 13 C/ 12 C) and oxygen ( 18 O/ 16 O) isotope ratio profiles in the wood of the mangrove Rhizophora mucronata Lam., a tropical tree species lacking distinct growth rings, were investigated. Variations of both isotope ratios revealed a remarkable annual cyclicity with lowest values occurring at the latewood/earlywood boundary (April-May) and highest values during the transition from earlywood to latewood (October-November). Based on the current knowledge of the physiology of this mangrove species, as well as on the current literature available on high-resolution profiles of stable isotope ratios in tree rings, possible driving forces responsible for this seasonal pattern are discussed. The annual cyclicity, together with a conspicuous isotope pattern appearing in the El-Niño year 1997, promises great potential for tropical dendrochronology.
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