Does gill boundary layer carbonic anhydrase contribute to carbon dioxide excretion: A comparison between dogfish (Squalus acanthias) and rainbow trout (Oncorhynchus mykiss)
Sf. Perry et al., Does gill boundary layer carbonic anhydrase contribute to carbon dioxide excretion: A comparison between dogfish (Squalus acanthias) and rainbow trout (Oncorhynchus mykiss), J EXP BIOL, 202(6), 1999, pp. 749-756
In vivo experiments were conducted on spiny dogfish (Squalus acanthias) and
rainbow trout (Oncorhynchus mykiss) in sea water to determine the potentia
l role of externally oriented or gill boundary layer carbonic anhydrase in
carbon dioxide excretion. This was accomplished by assessing pH changes in
expired water using a stopped-flow apparatus. In dogfish, expired water was
in acid-base disequilibrium as indicated by a pronounced acidification (De
lta pH=-0.11+/-0.01; N=22; mean +/- S.E.M.) during the period of stopped fl
ow; inspired water, however, was in acid-base equilibrium (Delta pH=-0.002/-0.01; N=22), The acid-base disequilibrium in expired water was abolished
(Delta pH=-0.005+/-0.01; N=6) by the addition of bovine carbonic anhydrase
(5 mgl(-1)) to the external medium. Addition of the carbonic anhydrase inhi
bitor acetazolamide (1 mmol l(-1)) to the water significantly reduced the m
agnitude of the pH disequilibrium (from -0.133+/-0.03 to -0.063+/-0.02; N=4
), However, after correcting for the increased buffering capacity of the wa
ter caused by acetazolamide, the acid-base disequilibrium during stopped fl
ow was unaffected by this treatment (control Delta[H+]=99.8+/-22.8 mu mol l
(-1); acetazolamide Delta[H+]=81.3+/-21.5 mu mol l(-1)). In rainbow trout,
expired water displayed an acid-base disequilibrium (Delta pH=0.09+/-0.01;
N=6) that also was abolished by the application of external carbonic anhydr
ase (Delta pH=0.02+/-0.01).
The origin of the expired water disequilibrium was investigated further in
acid-base disequilibrium was investigated further in dogfish, Intravascular
injection of acetazolamide (40 mg kg(-1)) to inhibit internal carbonic anh
ydrase activity nonspecifically and thus CO2 excretion significantly dimini
shed the extent of the expired water disequilibrium pH after 30 min (from -
0.123+/-0.01 to -0.065+/-0.01; N=6). Selective inhibition of extracellular
carbonic anhydrase activity using a low intravascular dose (1.3 mg kg(-1))
of the inhibitor benzolamide caused a significant reduction in the acid-bas
e disequilibrium after 5 min (from -0.11+/-0.01 to -0.07+/-0.01; N=14). The
se results demonstrate that the expired water acid-base disequilibrium orig
inates, at least in part, from excretory CO2 and that extracellular carboni
c anhydrase in dogfish may have a significant role in carbon dioxide excret
ion. However, externally oriented carbonic anhydrase (if present in dogfish
) plays no role in catalysing the hydration of the excretory CO2 in water f
lowing over the gills and thus is unlikely to facilitate CO2 excretion.