The Physiological Basis for Altered Na+and Cl−Movements across the Gills of Rainbow Trout (Oncorhynchus mykiss) in Alkaline (pH = 9.5) Water
Journal Articles
Overview
Research
Identity
Additional Document Info
View All
Overview
abstract
To test the hypothesis that internal ion imbalances at high pH are caused by altered branchial ion transporting capacity and permeability, radiotracers (24Na+ and 36Cl-) were used to measure ion movements across the gills of intact rainbow trout (Oncorhynchus mykiss) during 3 d exposure to pH 9.5. At control pH (pH 8.0), the trout were in net ion balance, but by 8 h at high pH, 60%-70% reductions in Cl- influx (JClin) and Na+ influx (JNain) led to net Cl- and Na+ losses of -200 micromol kg-1 h-1. Outflux (diffusive efflux plus renal ion losses) was not initially altered. By 72 h, net Cl- balance was reestablished because of a restoration of JClin. Although JNain remained 50% lower at this time, counterbalancing reductions in Na+ outflux restored net Na+ balance. One-substrate ion-uptake kinetics analyses indicated that reduced ion influx after 8 h at pH 9.5 was caused by 50% decreases in Cl- and Na+ maximal transport rates (JClmax, JNamax), likely reflecting decreased numbers of functional transport sites. Two-substrate kinetic analyses indicated that reduced internal HCO-3 and H+ supply for respective branchial Cl-/base and Na+/acid transport systems also contributed to lower JClin and, to a lesser extent, lower JNain at pH 9.5. Recovery of JClmax after 3 d accounted for restoration of Cl- balance and likely reflected increased numbers of transport sites. In contrast, JNamax remained 33% lower after 3 d, but a lower affinity of the gills for Na+ (fourfold greater KNam) accounted for the chronic reduction in Na+ influx at pH 9.5. Thus, reestablishment of Cl- uptake capacity and counterbalancing reductions in Na+ outflux allows rainbow trout to reestablish net ion balance in alkaline waters.
