According to the classical hypothesis, ion transporters and channels in the choroid plexus epithelial cells account for the main part of cerebrospinal fluid (CSF) production. The apically expressed Na+/K+-ATPase, central to CSF secretion, creates the electrochemical gradient for Na+ that is imported via the Na+/H+ exchanger, NHE1 and/or the Na+-HCO3- co-transporter, NCBE in the basolateral membrane. Co-import of HCO3- via NCBE and hydration of CO2 by carbonic anhydrase (C.A) increase the intracellular concentration of HCO3-, which creates an electrochemical gradient that drives the efflux of HCO3- via the basolateral-located Cl-/HCO3- exchanger, AE2 and apical HCO3- channels. The operation of AE2 generates a rise in intracellular Cl- driving the apical export of Cl- through the NKCC1 and Cl- channels. The final result of these processes at the choroid plexus epithelium is a net flux of Na+, HCO3- and Cl- from the blood across the epithelium to the ventricles, which generates the osmotic gradient that makes water move through AQP1 thereby producing the CSF.