DURING the formation of the mature mammalian erythrocyte, the reticulocyte sheds its nucleus, endoplasmic reticulum and mitochondria leaving a featureless cytoplasm with a high haemoglobin content surrounded by a plasma membrane. All Ca-accumulating organelles are lost and the mature red cell is maintained virtually Ca-free throughout its life1 by the low Ca permeability of its membrane2 perhaps aided by a powerful Ca-extrusion pump3. Most of our knowledge of Ca transport in red cells comes from studies with resealed ghosts, but in this preparation the results are often affected by alterations to the membrane and metabolism of the cell2–4. The main difficulty of using intact fresh cells in physiological conditions has been the impossibility of increasing their Ca content in a controlled way and of assessing the fraction of Ca which is ionised. Using a divalent-cation ionophore, A23187 (ref. 5), however, we have overcome these difficulties and found that cytoplasmic Ca buffering occurs as if the cell had a single large-capacity, low-affinity Ca buffer and that there are two Ca-translocating sites of equal affinity at the internal surface of the Ca pump.
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A23187: a divalent cation ionophore.
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1972,
The Journal of biological chemistry.