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  • 1
    ISSN: 1432-1939
    Keywords: Photoinhibition ; Crassulacean acid metabolism (CAM) ; 77K fluorescence ; Quantum yield ; Stress physiology
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Summary Diurnal measurements of low temperature (77K) fluorescence at 690 nm (PS II) from north, south, east, and west facing cladode surfaces of Opuntia basilaris in Death Valley, California were made on six occasions during 1985. The absolute levels of F o(instantaneous fluorescence) and F m(maximum fluorescence), as well as the ratio F v/F m(variable fluorescence, F m-F o, over maximum fluorescence), were greater in the north face relative to the other faces. Diurnal decreases in F o, F mand F v/F mwere found concomitant with increases in incident photon flux area density (PFD). F v/F mwas fairly low throughout the year, indicative of photoinhibition, but became somewhat elevated after a spring rain. In early fall the quantum yield of the south face was considerably depressed relative to that of the north face, and corresponding differences were observed in F v/F m. A decrease in PFD during growth of glasshouse plants led to an increase in chlorophyll concentration, F oand F m, but not F v/F m. Although there was some variability in the quantum yield of well watered glasshouse cladodes, a correlation was found between quantum yield and the light and CO2 saturated rate of photosynthesis. When O. basilaris was water stressed under glasshouse conditions, reductions in quantum yield, F m, and F v/F mwere observed. Reductions in F v/F malways indicated a reduced quantum yield, although the converse was not necessarily so in well watered glasshouse plants. The results of this study indicate that O. basilaris is likely to experience photoinhibition throughout much of its life in Death Valley.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1432-2048
    Keywords: C3, C4 plants (H-isotope composition) ; Deuterium ; Hydrogen-isotope composition ; Leaf (H-isotope composition)
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract The natural abundance hydrogen-isotope composition of leaf water ( $$\delta _{\text{D}}^{{\text{H}}_{\text{2}} {\text{O}}} $$ ) and leaf organic matter (δ D org ) was measured in leaves of C3 and C4 dicotyledons and monocotyledons. The $$\delta _{\text{D}}^{{\text{H}}_{\text{2}} {\text{O}}} $$ value of leaf water showed a marked diurnal variation, greatest enrichment being observed about midday. However, this variation was greater in the more slowly transpiring C4 plants than in C3 plants under comparable environmental conditions. A model based on analogies with a constant feed pan of evaporating water was developed and the difference between C3 and C4 plants expressed in terms of either differences in kinetic enrichment or different leaf morphology. Microclimatic and morphological features of the leaves which may be associated with this factor are discussed. There was no daily excursion in the δ D org value in leaves of either C3 or C4 plants. When δ D org values were referenced to the mean $$\delta _{\text{D}}^{{\text{H}}_{\text{2}} {\text{O}}} $$ values during the period of active photosynthesis, the discrimination against deuterium during photosynthetic metabolism (ΔD) was greater in C3 plants (-117 to -121‰) than in C4 plants (-86 to -109‰). These results show that the different water use “strategies” of C3 and C4 plants are responsible for the measured difference in deuterium-isotope composition of leaf water. However, it is unlikely that these physical processes account fully for the differences in hydrogen-isotope composition of the products of C3 and C4 photosynthetic metabolism.
    Type of Medium: Electronic Resource
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