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A survey of photosynthetic carbon metabolism in 4 ecotypes of Phragmites australis in northwest China: Leaf anatomy, ultrastructure, and activities of ribulose 1,5‐bisphosphate carboxylase, phosphoenolpyruvate carboxylase and glycollate oxidase
Author(s) -
Zheng W. J.,
Zheng X. P.,
Zhang C. L.
Publication year - 2000
Publication title -
physiologia plantarum
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.351
H-Index - 146
eISSN - 1399-3054
pISSN - 0031-9317
DOI - 10.1034/j.1399-3054.2000.110209.x
Subject(s) - ecotype , phragmites , rubisco , photosynthesis , biology , botany , phosphoenolpyruvate carboxylase , chloroplast , swamp , vascular bundle , c4 photosynthesis , halophyte , salinity , ecology , wetland , biochemistry , gene
Four ecotypes of Phragmites australis from different habitats in northwest China were examined to compare their photosynthetic characteristics. In a swamp ecotype, the Δ 13 C value of leaf materials was −34.0‰, and bundle sheath cells contained a small amount of organelles and round‐shaped chloroplasts, as being similar to typical C 3 plants. In a dune ecotype, the Δ 13 C value was −20.9‰ and bundle sheath cells contained oval‐shaped chloroplasts with poorly‐developed grana. In light and heavy salt meadow ecotypes, Δ 13 C values were −30.6‰ and −35.6‰, respectively. The shape of bundle sheath chloroplasts in the light salt meadow ecotype was intermediate between those of the swamp and dune ecotypes. Abundance of bundle sheath organelles in the heavy salt meadow ecotype was intermediate. The swamp ecotype had photosynthetic enzyme activities typical of C 3 type plants, whereas the dune ecotype had an increased activity of phosphoenolpyruvate carboxylase (PEPC), a key C 4 enzyme, and a decreased ribulose 1,5‐bisphosphate carboxylase (Rubisco) activity. The light salt meadow and heavy salt meadow ecotypes had substantial activities of PEPC, which indicates potential for C 4 photosynthesis. These data suggest that this species evolved the C 3 ‐like ecotype in swamp environments and the C 4 ‐like C 3 ‐C 4 intermediate in dune desert environments, and C 3 ‐like C 3 ‐C 4 intermediates in salt environments.