The chloride cells of the gill secretory epithelium of fish that make the transition from fresh water to sea water adapt to the increased salinity by responding to a rapid signal that stimulates chloride secretion. In this paper, data are presented supporting the view that the transient increase in plasma osmolarity that can be measured during the transition is responsible for the stimulation of chloride secretion. A maximal increase of 65 mOsm in the plasma of Fundulus heteroclitus (the killifish) was found during acclimation to sea water. Similar or greater increases of osmolarity induced by mannitol on the basolateral side of isolated opercular epithelial membranes of the same species of fish containing great numbers of chloride cells produced stimulation of chloride secretion detected as the short circuit current. The shrinkage of the chloride cell activates the Na-K-2Cl cotransporter, and the Na/H exchanger and requires the integrity of apical chloride channels and normal levels of Ca. A Cl/HCO3 exchanger did not participate in this osmotic response to higher salinity. Chloride cell volume responses to osmolarity were studied with imagine and quantitative optics.
Download full-text PDF |
Source |
---|---|
http://dx.doi.org/10.1038/ki.1996.225 | DOI Listing |
Enter search terms and have AI summaries delivered each week - change queries or unsubscribe any time!