Carbon dioxide (CO2) is produced in tissues as a byproduct of normal aerobic metabolism. It dissolves in the solution of blood plasma and into red blood cells (RBC), where
carbonic anhydrase catalyzes its hydration to
carbonic acid (H2CO3). Carbonic acid then spontaneously
dissociates to form bicarbonate Ions () and a
hydrogen ion (H+). In response to the decrease in intracellular
pCO2, more CO2 passively diffuses into the cell. Cell membranes are generally impermeable to charged ions (i.e. H+, ) but RBCs are able to exchange bicarbonate for chloride using the anion exchanger protein
Band 3. Thus, the rise in intracellular bicarbonate leads to bicarbonate export and chloride intake. The term "chloride shift" refers to this exchange. Consequently, chloride concentration is lower in systemic venous blood than in systemic arterial blood: high venous pCO2 leads to bicarbonate production in RBCs, which then leaves the RBC in exchange for chloride coming in. The chloride shift may also regulate the affinity of
hemoglobin for
oxygen through the chloride ion acting as an
allosteric effector. == Reaction ==