C. Hogstrand et al., EFFECTS OF ZINC ON THE KINETICS OF BRANCHIAL CALCIUM-UPTAKE IN FRESH-WATER RAINBOW-TROUT DURING ADAPTATION TO WATERBORNE ZINC, Journal of Experimental Biology, 186, 1994, pp. 55-73
The effects of sublethal waterborne Zn2+ (150 mu g 1(-1)=2.3 mu mol 1(
-1)) on the kinetics of unidirectional Ca2+ influx were studied in juv
enile freshwater rainbow trout during chronic exposure (60 days) at a
water [Ca2+] of 1.0 mmol 1(-1). An unexposed group held under identica
l conditions served as control. The presence of Zn2+ in the water incr
eased the apparent K-m for Ca2+ influx by up to 300 % with only a smal
l inhibitory effect (35 % at most) on the maximum rate of uptake (J(ma
x)) These results, in combination with earlier data showing that Ca2competitively inhibits Zn2+ uptake, suggest that Zn2+ and Ca2+ compete
for the same uptake sites. Acute withdrawal of Zn2+ after 3 h of expo
sure resulted in a 23-fold reduction in K-m for Ca2+, but a persistent
small depression of J(max) During prolonged exposure to Zn2+, the app
arent K-m for Ca2+ remained greatly elevated and J(max) remained sligh
tly depressed. The actual Ca2+ influx in hard water ([Ca2+]=1.0 mmol 1
(-1)) decreased marginally and paralleled the small changes in J(max).
The increases in apparent K-m had a negligible influence on the actua
l Ca2+ influx because K-m values (38-230 mu mol 1(-1)), even when elev
ated by Zn2+, remained below the water [Ca2+] (1000 mu mol 1(-1)). Rai
nbow trout exposed to Zn2+ exhibited a slower rate of protein synthesi
s in the gills (measured on day 23) and an increased tolerance to Zn2 challenge (measured on both days 27 and 50). Unidirectional Zn2+ infl
ux, measured at the end of the exposure period, was significantly redu
ced in the Zn2+-exposed fish. There were no changes in hepatic or bran
chial Zn2+, Cu2+ or metallothionein concentrations. We hypothesize tha
t, during exposure to sublethal [Zn2+] in hard water, the fish may cha
nge the K-m for a mutual Ca2+/Zn2+ carrier so as to reduce markedly Zn
2+ influx without greatly altering Ca2+ influx. This reduced Zn2+ infl
ux, rather than metallothionein induction, may be the basis of adaptat
ion to elevated concentrations of waterborne Zn2+.