Intestinal chloridebicarbonate exchange is involved in osmoregulation

GROSELL, M.; WILSON, R.; RSMAS, Univ. of Miami, Fl; Univ. of Exeter, UK: Intestinal chloride/bicarbonate exchange is involved in osmoregulation

Marine teleosts combat dehydration by drinking. In addition to apical Na+:Cl and Na+:K+:2Cl co-transport, Cl/HCO3 exchange is involved in intestinal Cl and water absorption. This exchange enables water and Cl absorption in absence of luminal Na+ and can account for up to 50% of intestinal Cl absorption. A consequence of this anion exchange is high [HCO3] (> 100 mM) and high pH (>8.5) in the intestinal fluids. Considering the electrochemical gradients for both Cl and HCO3 across the intestinal epithelium of most species, the Cl/HCO3 exchange perform active transport of both anions. The source of HCO3 is carbonic anhydrase mediated hydration of CO2 and apical anion exchange seems to be fueled by active extrusion of H+ across the basolateral membrane. In some species, intestinal HCO3 secretion exhibits serosal Na+ dependence and amiloride sensitivity suggesting H+ extrusion via a Na+/H+ exchange mechanism. In these species, active HCO3 secretion (and Cl absorption) is fueled by the electrochemical Na+ gradient created by the Na/K-ATPase. In the European flounder (Platichthys flesus), however, HCO3 secretion is insensitive to serosal amiloride and not dependent on serosal sodium, suggesting active proton extrusion via a basolateral H+ ATPase. As a result of the alkalinity in the intestinal lumen and the high Ca2+ concentration in seawater, substantial precipitation of CaCO3 occurs in the intestine. This is advantageous to marine teleosts because 1) it reduces intestinal Ca2+ uptake and thus the need for renal Ca2+ excretion and 2) it lowers the osmolality of the intestinal fluids aiding in fluid absorption. Intestinal bicarbonate secretion is stimulated by elevated luminal Ca2+ in the mM range suggesting the involvement of an apical membrane-bound Ca2+ sensing receptor (CaR).

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