Abstract
Summary
When incubated with human blood, C-14 oxalate is distributed between cells and plasma with a significant preference for the cells. After incubation with inorganic P32 phosphate and oxalate, rate of loss of P32 from the erythrocytes suspended in buffered-normal saline was lower in the case of erythrocytes pre-incubated with oxalate, reaching a minimum value with 0.00075 molar oxalate. Inhibition of P32 loss from erythrocytes by oxalate was slightly enhanced by potassium but was reversed by calcium and magnesium ions in physiological concentrations. Concentration of the cellular organic phosphates of the acid-soluble ester fraction changes significantly after incubation of erythrocytes with inorganic P32 and oxalate. The changes caused by oxalate may in each case be attributed directly or indirectly to a reduction in available magnesium.
Acknowledgement is made to Professor A. Grollman for professional assistance and to Mildred Watkins and Mr. J. W. Jackson for technical aid.
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