Plant Physiol. Journal of Pharmacology and Experimental Therapeutics
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Plant Physiology 91:1551-1557 (1989)
© 1989 American Society of Plant Biologists

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Metabolism and Enzymology

Anaerobic Carbon Metabolism by the Tricarboxylic Acid Cycle 1

Evidence for Partial Oxidative and Reductive Pathways during Dark Ammonium Assimilation

Greg C. Vanlerberghe, Anne K. Horsey, Harold G. Weger and David H. Turpin

Department of Biology, Queen's University, Kingston, Ontario, Canada K7L 3N6

Nitrogen-limited cells of Selenastrum minutum (Naeg.) Collins are able to assimilate NH4+ in the dark under anaerobic conditions. Addition of NH4+ to anaerobic cells results in a threefold increase in tricarboxylic acid cycle (TCAC) CO2 efflux and an eightfold increase in the rate of anaplerotic carbon fixation via phosphoenolpyruvate carboxylase. Both of these observations are consistent with increased TCAC carbon flow to supply intermediates for amino acid biosynthesis. Addition of H14CO3 to anaerobic cells assimilating NH4+ results in the incorporation of radiolabel into the {alpha}-carboxyl carbon of glutamic acid. Incorporation of radiolabel into glutamic acid is not simply a short-term phenomenon following NH4+ addition as the specific activity of glutamic acid increases over time. This indicates that this alga is able to maintain partial oxidative TCAC carbon flow while under anoxia to supply {alpha}-ketoglutarate for glutamate production. During dark aerobic NH4+ assimilation, no radiolabel appears in fumarate or succinate and only a small amount occurs in malate. During anaerobic NH4+ assimilation, these metabolites contain a large proportion of the total radiolabel and radiolabel accumulates in succinate over time. Also, the ratio of dark carbon fixation to NH4+ assimilation is much higher under anaerobic than aerobic conditions. These observations suggest the operation of a partial reductive TCAC from oxaloacetic acid to malate, fumarate, and succinate. Such a pathway might contribute to redox balance in an anaerobic cell maintaining partial oxidative TCAC activity.


1 Supported by the Natural Sciences and Engineering Research Council of Canada. G. C. V. acknowledges an NSERC postgraduate scholarship. A. K. H. acknowledges an NSERC summer scholarship.







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