Plant Physiology 46:738-742 (1970)
© 1970 American Society of Plant Biologists
Articles
Biogeochemistry of the Stable Isotopes of Hydrogen and Carbon in Salt Marsh Biota 1
Bruce N. Smith2 and
Samuel Epstein
a Division of Geological Sciences, California Institute of Technology, Pasadena, California 91109
Deuterium to hydrogen ratios of 14 plant species from a salt marsh and lagoon were 55 depleted in deuterium relative to the environmental water. Carbon tetrachloride-extractable material from these plants was another 92 depleted in deuterium. This gave a fractionation factor from water to CCl4 extract of 1.147. This over-all fractionation was remarkably constant for all species analyzed. Plants also discriminate against 13C, particularly in the lipid fraction. Data suggest that different mechanisms for carbon fixation result in different fractionations of the carbon isotopes. Herbivore tissues reflected the isotopic ratios of plants ingested. Apparently different metabolic processes are responsible for the different degrees of fractionation observed for hydrogen and carbon isotopes.
2 Present address: Department of Botany, The University of Texas, Austin, Texas 78712.
1 This work was generously supported by the National Science Foundation, Grant BG 7517.
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