Doi, Hiroyuki

Marine teleost fish precipitate divalent cations as carbonate deposits in their intestine to minimize the potential for excessive calcium entry and to stimulate water absorption by removing osmolyte ions. This carbonate deposit formation therefore plays an important role in osmoregulation in the seawater environment and also requires controlled secretion of HCO 3 − to match the amount of calcium entering the intestinal lumen. Despite this physiological importance, the process of carbonate precipitate formation has not been characterized at the molecular level. We first isolated 24 candidate cDNA clones representing all possible membrane proteins capable of transporting HCO 3 − from the euryhaline pufferfish, mefugu Takifugu obscurus based on the DNA sequence information on the T. rubripes genome, then performed Northern blot analyses to select clones highly expressed in the intestine of seawater mefugu, and finally determined the cellular locations by immunohistochemistry. Based on these observations, we proposed a model for HCO 3 − excretion across the intestinal epithelium of marine teleost fish that includes a basolateral NBCe1 (Na + /bicarbonate cotransporter) and apical Slc26a6 (Cl − /HCO 3 − exchangers).