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COMPARATIVE AND EVOLUTIONARY PHYSIOLOGY
1Department of Biology, McMaster University, Hamilton, Ontario, Canada; 2Division of Marine Biology and Fisheries, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida; 3School of Biological Sciences, University of Plymouth, Devon, United Kingdom; 4Department of Zoology, University of British Columbia, Vancouver, Canada; 5Department of Biology, University of Ottawa, Ottawa, Ontario, Canada; and 6Laboratory of Ecophysiology and Molecular Evolution, Instituto Nacional de Pesquisas da Amazônia, Manaus, Brazil
Submitted 12 September 2006 ; accepted in final form 28 January 2007
| ABSTRACT |
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15 g) and large oscars (
200 g) to hypoxia were qualitatively similar, but the latter were more effective. Large oscars exhibited a rapid reduction in unidirectional Na+ uptake rate at the gills during acute hypoxia (PO2
10 mmHg), which intensified with time (7 or 8 h); Na+ efflux rates were also reduced, so net balance was little affected. The inhibitions were virtually immediate (1st h) and preceded a later 60% reduction (at 3 h) in gill Na+-K+-ATPase activity, reflected in a 60% reduction in maximum Na+ uptake capacity without change in affinity (Km) for Na+. Upon acute restoration of normoxia, recovery of Na+ uptake was delayed for 1 h. These data suggest that dual mechanisms may be involved (e.g., immediate effects of O2 availability on transporters, channels, or permeability, slower effects of Na+-K+-ATPase regulation). Ammonia excretion appeared to be linked indirectly to Na+ uptake, exhibiting a Michaelis-Menten relationship with external [Na+], but the Km was less than for Na+ uptake. During hypoxia, ammonia excretion fell in a similar manner to Na+ fluxes, with a delayed recovery upon normoxia restoration, but the relationship with [Na+] was blocked. Reductions in ammonia excretion were greater than in urea excretion. Plasma ammonia rose moderately over 3 h hypoxia, suggesting that inhibition of excretion was greater than inhibition of ammonia production. Overall, the oscar maintains excellent homeostasis of ionoregulation and N-balance during severe hypoxia. teleost fish; ionoregulation; nitrogen metabolism; sodium-potassium-ATPase; ion channels
First, the respiratory-osmoregulatory compromise at the gills has been well documented in exercise studies on several teleost species: the effective gill area and diffusion distance are adjusted as a trade-off between providing the permeability required for gas exchange, while minimizing diffusive ion losses and osmotic water gain (12, 13, 57, 58). During environmental hypoxia, it is probable that similar lamellar recruitment and decreased diffusion distance occurs to help sustain O2 uptake (17, 18) because gill O2 transfer factor, an index of effective O2 permeability, increases markedly in both hypoxia and exercise (36). We therefore hypothesized that increases in diffusive Na+ loss rates to the water and a possible reduction of plasma ion levels would also occur.
Secondly, ionoregulation is a costly process in freshwater fish, with estimates generally falling in the range of 220% of resting metabolism at the whole animal level (reviewed in Ref. 11). The very dilute nature of many Amazonian waters ("slightly contaminated distilled water;" 41) may exacerbate these costs, and a general tendency for reduced ion levels in the plasma of Amazonian teleosts has been noted (28). In other fish, the rate of O2 utilization by artificially perfused and ventilated gill tissue amounts to about 412% of resting O2 uptake by the whole animal (26, 31, 59), that is, in the same range as estimates of the costs of ionoregulation. About half of this O2 used by gill cells comes directly from the water, and the other half comes from the perfusate or blood, which itself has just been oxygenated in the arterial-arterial pathway of the gill lamellae before reaching the ionocytes (33, 52). Thus gill ionocytes will be on the front line of hypoxia exposure and the very first cells to experience an O2 deficit during environmental hypoxia. By way of analogy, in neural cells, the cost of ion pumping appears to be second only to that of protein synthesis, and both processes are markedly turned down during hypoxia in model species, such as the turtle and crucian carp, which are capable of severe hypometabolism (reviewed in Refs. 6, 7, and 19). Therefore, we hypothesized that active Na+ influx rates from the water could fall during hypoxia for two reasons: 1) as a direct response to O2 starvation of the working ionocytes and 2) as a result of downregulation of uptake channels and/or Na+-K+-ATPase activity to save metabolic costs.
Third, if ion transport processes are affected by hypoxia, ammonia excretion might be affected as well. The gills excrete more than 80% of the metabolic ammonia production in fish, and the mechanism is thought to be linked in some way to the active uptake of Na+ (see Refs. 50, 51, 53, 56 for a review). Original ideas about direct Na+/NH4+ exchange coupling in the gill cells (e.g., 21, 27, 60), while not entirely disproven, have given way in recent years to the concept that the coupling is indirect (3, 25, 34). Thus an H+ pump on the apical membrane provides the electrical gradient needed to drive Na+ uptake from the water through coupled Na+ channels, and the associated acidification of the gill boundary layer enhances the "diffusion-trapping" of NH3 as NH4+, thus sustaining the PNH3 gradient for diffusive NH3 efflux (9, 54). We, therefore, hypothesized that if hypoxia interferes with the Na+ uptake-H+ pumping mechanism (or Na+/NH4+ exchange), ammonia excretion would be inhibited, and/or uncoupled from Na+ uptake. However, the situation is complicated by the fact that the rate of metabolic ammonia (and urea) production may also be reduced by down-regulation of aerobic metabolism (i.e., less deamination of amino acids for fuel; Refs. 47 and 48), though at least one study has shown an increase in ammonia production during hypoxia (22). Regardless, metabolic rate depression per se is another reason to suspect that ammonia excretion could be sensitive to hypoxia. Therefore, we also measured plasma ammonia levels as an indicator of whether the excretion processes or the production processes were altered to the greater extent, as well as changes in urea excretion as a general indicator of N-metabolism during hypoxia.
In addition to the effects of hypoxia on ion balance and ammonia excretion in general, we explored the influence of body size. Large oscars are more tolerant of hypoxia than small oscars, in contrast to the pattern in many other teleost species (e.g., 8, 38, 43). Large oscars possess lower mass-specific MO2s and a greater aerobic ability to sustain MO2 during hypoxia (i.e., lower PO2crit; Ref. 42), a much greater anaerobic capacity (2), and different behavioral responses (42). We therefore looked for possible qualitative or quantitative differences between large and small fish in Na+ and ammonia flux responses to hypoxia.
| MATERIALS AND METHODS |
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Experimental protocols. Experimental temperature was 28 ± 1.5°C, and the same soft water was used in all trials. Most experimental protocols consisted of exposing the fish (n = 59 per experiment) to various O2 regimes, while simultaneously measuring unidirectional Na+ fluxes with 22Na (manufactured by New England Nuclear-Dupont, Boston, MA, and supplied by REM, Sâo Paulo, Brazil) and net ammonia and urea fluxes. Experimental chambers for large fish were 2.5-liter sealable Nalgene kitchen cutlery containers mounted on their sides; the horizontally flattened shape fitted the morphology of the fish. For small fish, 700-ml Nalgene beakers with sealable lids were employed. The chambers were shielded with black plastic to minimize visual disturbance and fitted with individual water lines for flushing, and air-stones for air or N2 gassing. The chambers were 80% submerged in a flowing water bath to maintain the experimental temperature of 28 ± 1.5°C. Fish were placed in these individual containers the evening before an experiment and left overnight to settle with flow-through flushing and continuous aeration.
At the start of a standard experiment, the water flow was stopped but aeration continued, and an aliquot of 22Na (typically 2 µCi/l) was added to each container and allowed to equilibrate for 1 h. Water samples (4 x 5 ml for 22Na, total Na+, ammonia, and urea measurements) were taken at the start of the experiment (0 h) and at subsequent 1-h intervals up to 7 h, when the experiment was terminated and the animal was weighed. During this period, the O2 regime was experimentally manipulated by vigorous gassing with either air or N2, followed by more gentle gassing for maintenance. Tests demonstrated that PO2 changes were complete within 10 min, so water PO2 was routinely monitored (1-ml samples) at the midpoint of each 1-h flux. The overall 7-h measurement period was chosen so as to avoid the need to perform correction for back flux of the radioisotope, with its attendant uncertainties (cf. 20, 55). Theoretical calculations, confirmed by blood samples in preliminary trials, indicated that internal specific activity reached only 26% of external specific activity by this time, below the threshold (10%), in which back-flux correction would become necessary.
One exception to this basic protocol occurred in an experiment with large oscars, where fluxes were measured over a 3-h period, which included 1 h of normoxia and the first 2 h of hypoxia, and then again at 79 h of hypoxic exposure. The external radioisotope concentration was tripled at 6 h of hypoxia so as to avoid a back-flux problem. A second exception occurred in kinetic flux experiments with large oscars, in which the concentration dependence of Na+ uptake was measured at successively higher external Na+ concentrations in five steps over an 11-h period (cf. 55). In these experiments, 22Na and "cold" Na+ were raised in direct proportion to one another by adding aliquots of a 22Na-labeled 180 mmol/l NaCl solution in a geometrically increasing series. At each concentration, a 0.5-h mixing period was followed by a 1-h to 2-h period of flux measurement. Similar experiments were attempted with small oscars, but the higher volume-to-mass ratio used precluded accurate Na+ uptake measurements at higher Na+ concentrations, so only ammonia flux data from the latter experiments have been reported.
One experimental series focused on terminal blood and tissue sampling. Large oscars were set up in their individual containers exactly as during flux tests, but 22Na was not added. A typical O2 regime of normoxia, followed by 3 h of severe hypoxia and 3 h of normoxia restoration was implemented. Fish (n = 7 per sampling point) were rapidly killed with a lethal dose of benzocaine (0.5 g/l; Sigma, St. Louis, MO) during normoxia, after 1 and 3 h of severe hypoxia, and after 1 and 3 h of normoxia restoration. In this series, water PO2 was measured at each sampling time and also at 10 min after the changes from normoxia-to-hypoxia and from hypoxia-to-normoxia. Blood samples (1 ml) were taken by caudal venipuncture, and then samples of gill filaments and epaxial white muscle were excised. Plasma and tissue samples were snap-frozen in liquid N2 and stored at 80°C for later analysis.
Finally, a separate experimental series using an identical normoxia-hypoxia-normoxia regime and duplicating the exact conditions used during the flux and tissue sampling experiments was carried out with five large oscars. Water pH was monitored at 30-min intervals throughout to ensure that it was not a confounding factor in interpretation of results.
Analytical techniques and calculations. Water PO2 was monitored by injecting 1-ml samples into an O2 electrode (Radiometer-Copenhagen, Denmark) thermostatted to the experimental temperature and connected to a Cameron OM-200 oxygen meter (Cameron Instruments, Port Aransas, TX). Water pH was monitored with a Radiometer GK24O1C combination electrode suitable for use in ion-poor water. Water total ammonia (salicylate hypochlorite assay; Ref. 49) and urea concentrations (diacetyl monoxime assay; Ref. 35) were determined colorimetrically. 22Na activities in water samples were measured via liquid scintillation counting (LS6500, Beckman Coulter, Fullerton, CA) on 5-ml water samples added to 5-ml of Packard Ultima Gold AB fluor (Perkin Elmer, Wellesley, MA). Tests demonstrated that quenching was constant, so no correction was necessary. Water total Na+ concentrations were measured using flame atomic absorption spectrophotometry (AAnalyst 800, Perkin Elmer). Na+ influx rates (JNain, by convention positive) were calculated from the mean external specific activity, and the disappearance of counts from the external water (factored by time, volume, and fish mass); Na+ net flux rates (JNanet) were calculated from the change in total Na+ concentration in the water (similarly factored); and Na+ unidirectional efflux rates (JNaout, by convention negative) were calculated by difference, as outlined in detail by Wood (55). This approach makes no assumptions about steady state and allows for comparisons of different treatments over time. Net flux rates of ammonia (JAmm) and urea (JUrea) were calculated as for JNanet. In kinetic analyses, the coordinates of the Michaelis-Menten equation (Km, Jmax) and their SE estimates were fitted by nonlinear regression using Sigmaplot 8.
Plasma samples were analyzed for Na+, Ca2+, Mg2+ (all by atomic absorption spectrophotometry using a Varian SpectrAA-220FS; Varian, Mulgrave, Australia), Cl by coulometric titration (CMT10, Radiometer-Copenhagen, Denmark), total ammonia by the glutamate dehydrogenase method (Raichem, Ammonia Reagent, Product No. 85446, Columbia, MD), cortisol by radioimmunoassay (ICN Pharmaceuticals, Costa Mesa, CA), and glucose and lactate by standard enzymatic assays (10, 37). Muscle samples were similarly analyzed for lactate, but some samples were lost due to accidental thawing. Gill Na+-K+-ATPase activity was determined by the microplate method of McCormick (29) and normalized to total protein content (measured using the bicinchoninic acid method; Sigma).
All data are reported as means ± SE (n = number of fish). Relationships were assessed by 1-way ANOVA followed by the Bonferroni multiple comparison test for independent data or Dunnett's multiple comparison test for paired data, as appropriate, to determine when values became significantly different from reference means. A significance level of P
0.05 was used throughout.
| RESULTS |
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10 mmHg; e.g., Fig. 1D), but in preliminary experiments, it was found that some small oscars succumbed at this level, so a less severe hypoxia (
20 mmHg) was used for the latter (e.g., Fig. 1A).
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An experiment was carried out with large fish to determine whether the inhibition of JNain and JNaout would persist during prolonged hypoxia. Indeed, the responses appeared to intensify over time, such that the reduction of JNain was greater at 7 and 8 h of severe hypoxia than it had been at 1 h and 2 h (Fig. 3B). Similarly, the reduction of JNaout was also greater, at least at 8 h.
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The kinetic experiment was repeated on the same large oscars 2 days later during hypoxia (PO2 = 17.0 ± 0.9 mmHg). The coupling of JAmm to environmental [Na+] was entirely blocked by hypoxia (Fig. 5B).
Kinetic experiments with small oscars (not shown) demonstrated a very similar relationship between JAmm and environmental [Na+] during normoxia (PO2 = 125 ± 6 mmHg), with an identical Km (122 ± 49 µmol/l) to that in large oscars, but a much larger mass-specific Jmax (1,319 ± 156 µmol·kg1·h1), as would be anticipated from allometric considerations. However, JNain values could not be determined in these small fish experiments (see MATERIALS AND METHODS). Notably, the coupling of JAmm to environmental [Na+] was again eliminated by hypoxia (PO2 = 29 ± 4 mmHg).
JAmm was measured in all time-course experiments (e.g., Figs. 14) and invariably declined during hypoxia and increased again after restoration of normoxia. Responses were generally more pronounced in large fish (e.g., Fig. 1, C and F). The trends were therefore qualitatively similar to those in JNain and JNaout, but the relative changes in JAmm were often larger than in the Na+ fluxes, and the time courses of the responses were not always matched, again suggesting that any coupling must be indirect. Thus in the acute and gradual hypoxia exposures of Figs. 3C and 4C, respectively, the initial declines in JAmm lagged behind the initial declines in JNain (Figs. 3B and 4B), but the reductions in JAmm did become more intense over time during prolonged severe hypoxia (Fig. 3C). During the first hour of normoxia restoration, JAmm exhibited either no recovery (e.g., Fig. 1C and an additional small fish experiment not shown) or only partial recovery (e.g., Figs. 1F and 2C), but thereafter was always fully restored to the original normoxia level.
JUrea was also measured in all time course experiments (not shown). As with JAmm, JUrea was several-fold larger on a mass-specific basis in small fish relative to large fish, as expected from allometry. Under normoxia, JUrea was only 10.9 ± 2.5% (n = 34) of JAmm on a per unit N basis, and during hypoxia, declines in JUrea almost always occurred in parallel to declines in JAmm. Thus, as with JAmm, decreases in JUrea were relatively larger in large oscars than in small oscars. However, the relationship between JUrea and JAmm was not one of direct proportionality (Fig. 6). The slope of the regression relating percentage change in urea-N excretion to that in ammonia-N excretion was only 0.57, and the intercept was significantly greater than zero. Therefore, at greater than about 50% inhibition, the relative declines in JAmm were greater than the relative declines in JUrea. Under severe hypoxia, when JAmm was greatly depressed, JUrea was 27.2 ± 5.9% (n = 34) of JAmm on a per unit-N basis.
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| DISCUSSION |
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Small vs. large oscars. Although Na+ influx kinetics were measured only for large oscars, they fit the pattern of relatively high Km (i.e., low Na+ affinity) and low influx and efflux rates (i.e., low permeability) reported for other Amazonian cichlids (reviewed in Ref. 16), very different from the characids, which are abundant in the same environment and which exhibit low Km (i.e., high Na+ affinity) and much higher Na+ turnover rates (14, 15). The cichlid strategy is presumably more economical because it necessitates less active ion pumping. The fact that mass-specific Na+ turnover rates are not greater in small oscars than large oscars in the expected allometric fashion (e.g., Ref. 4) may in itself represent a cost-saving adaptive strategy for these small fish in ion-poor water. However, mass-specific ammonia excretion rates (JAmm) were higher in small fish than in large fish (Fig. 1, C and F), and the differences were relatively larger than in MO2 (42), suggesting that small oscars rely on protein oxidation to a greater extent (23, 47).
The responses to hypoxia, including reductions in JNain, JNaout, JAmm, and JUrea, were qualitatively similar between large and small oscars and differed only in quantitative detail. The reductions in JNain and JNaout during hypoxia became significant more rapidly in large fish (first hour vs. second or third hour), and the inhibitions of JAmm and JUrea were more pronounced than in small fish (Fig. 1). Note, however, that a less severe level of acute hypoxia was used for small fish (
20 vs.
10 mmHg in large fish) because of their lower hypoxic tolerance. These responses should be interpreted with respect to the metabolic responses of large and small oscars to hypoxia, as determined through respirometry in a parallel study under very similar conditions (42). Sloman et al. (42) reported that MO2 was around 2,200 µmol·kg1·h1 under normoxic conditions in large fish and remained stable down to a PO2 of 50 mmHg, where it was significantly depressed (by 26%). In contrast, MO2 was around 4,900 µmol·kg1·h1 under normoxia in small oscars and tended to fall progressively as PO2 declined, with the first significant decrease (by 27%) occurring at 70 mmHg. In both large and small fish, MO2 fell steadily with PO2 below these thresholds. On the basis of model equations fitted to these data (42), a 200-g fish would have exhibited a 75% decline in MO2 at 10 mmHg, whereas a 15-g fish would have exhibited a 68% decline at the higher PO2 of 20 mmHg and a 79% decline had 10 mmHg been used.
During the gradual hypoxia trials, in large fish, reductions in both JNain and JNaout first became significant at a threshold PO2 of about 40 mmHg (Fig. 4, A and B; corresponding to a decline in MO2 of only 37%), slightly below the threshold PO2 (PO2crit = 50 mmHg), at which aerobic metabolic rate depression started. This suggests that reduced ion turnover at the gills is part of the strategy for metabolic rate depression in large oscars and is likely regulated in some fashion. However, in small fish, the PO2 threshold for significant reduction in unidirectional Na+ fluxes was about 20 mmHg, corresponding to a 68% decline in MO2, whereas PO2crit was 70 mmHg. In small oscars, physiological regulation may be less developed, so that direct effects of O2 starvation on the gills (with later onset) may be the dominant mechanism. In summary, it appears that large oscars are better able to implement these cost-saving responses more quickly, at a higher PO2, without compromising net Na+ balance, another indicator of their better hypoxia tolerance relative to small oscars (cf. Refs. 2 and 42). Interestingly, Lewis et al. (24) recently reported that protein synthesis rates in the gills of large oscars were reduced by 50% during a comparable hypoxic exposure but recovered without overshoot within 1 h after restoration of normoxia.
Influence of hypoxia on ionoregulation. Contrary to predictions based on the respiratory-osmoregulatory compromise, JNaout and JNanet did not increase, and plasma ions did not fall during severe hypoxia. The situation is very different than during exercise, where increases in MO2 are associated with increases in ion losses in a number of species (12, 13, 57, 58). However, unlike exercise, where MO2 clearly increases, there is a marked decrease in MO2 during hypoxia (32, 42). Gill blood flow changes may be rather different during hypoxia, because in contrast to the overall branchial vasodilation that accompanies exercise, there is a branchial vasoconstriction and an increase in the arterio-venous flow, which returns O2 to the heart (17, 44, 45). At present, we have no evidence that increased lamellar blood flow actually occurs during hypoxia in Astronotus ocellatus. This is an important area for future investigation, as are possible changes in the perfusion of the secondary circulation to the skin, and alterations in the relative surface areas and diffusion distances from water to blood of the gills vs. other parts of the body during the hypoxic exposure.
The only study with a comparable focus is that of Thomas et al. (46), in which rainbow trout, a hypoxia-intolerant species, were acutely exposed to a PO2 of 40 mmHg. Thomas et al. (46) were able to measure net flux rates of Na+ and Cl with the water in only a few trout due to fecal contamination problems but concluded that these remained approximately stable during hypoxia, in accord with the present study. Furthermore, plasma [Na+] and [Cl] actually increased, again in agreement with the present results (Fig. 7B), attributed to a fluid shift into the intracellular compartment (i.e., hemoconcentration), as well as a preferential movement of Na+ into the extracellular fluid to balance the lactate anion. Comparable explanations likely apply for the oscar, as all plasma ions tended to increase, there was a rapid appearance of lactate in the extracellular fluid (Table 1) and a marked rise in muscle lactate occurred (the measured concentration of 17.4 mmol/kg at 13 h of hypoxia would have amounted to about 24 mmol/l on an intracellular fluid basis). This rapid response of lactate production, as well as the moderate fall in plasma glucose (Table 1), are in accord with previous reports on the well-developed anaerobic potential of white muscle in large oscars (2, 32). Lactate production from glycogen stores would have driven a shift of fluid out of the extracellular compartment into muscle by osmosis. The rapid appearance of lactate and its equally rapid clearance after return to normoxia may have been associated with the sharp increases and decreases in cortisol at these times (Table 1; see Refs. 10 and 30). Very recently, Richards et al. (37) have reported a detailed biochemical study on Astronotus ocellatus exposed to a similar hypoxic regime and have confirmed many of the trends seen in the present study, including lactate accumulation, glycogen depletion, hemoconcentration, and apparent fluid shift to the intracellular compartment.
Three possible explanations, which are by no means mutually exclusive, come to mind for the observed decreases in JNaout during hypoxia (Figs. 1, B and E, 2B, 3B, and 4B). The first is channel arrest, a well-documented phenomenon at the cellular level in hypoxia-tolerant species (6, 7, 19). If this occurred at the gills, it could reduce both JNain and JNaout, and perhaps also JAmm. The second possibility, a different interpretation of the respiratory-osmoregulatory compromise, is that a hypoxia-tolerant species such as the oscar actually reduces gill area and permeability during severe hypoxia by reducing lamellar perfusion so as to reduce ionoregulatory costs in a situation in which the potential for MO2 uptake from the water has become very slight. This might occur in association with depressed protein synthesis in the gills (24), with a change in the pattern of cardiac output (the well-documented bradycardia without fall in stroke volume) and/or a possible change in circulatory pattern in the gills during hypoxia (17, 18, 44, 45), as discussed earlier. Measurements of water flux across the gills would illuminate whether effective branchial water permeability is turned down in parallel to apparent branchial Na+ permeability, which would support this explanation. The third possibility is that an exchange diffusion transport system occurs at the gills and is turned down during hypoxia, so that the reduced JNaout is directly coupled to the reduced JNain. Exchange diffusion has been seen during normoxia in many freshwater teleosts and crustaceans (e.g., 40, 58), including about half of the Amazonian teleosts surveyed by Gonzalez et al. (15), but to our knowledge, it has never been studied during hypoxia.
In both large and small oscars, JNain declined substantially during hypoxia (Figs. 14), in accord with our original hypothesis that this expensive process would be limited by O2 availability. However, several lines of evidence point to, at least, a partial temporal disconnection between the O2 regime and the simultaneously measured ion fluxes, suggesting that two (or more) mechanisms may be causing the reduction in Na+ turnover during hypoxia.
The first is that in the large fish experiment of Fig. 7C, branchial Na+-K+-ATPase activity was fully maintained at the end of 1 h of hypoxia, despite the fact that Na+ influx and efflux rates had already declined over the first hour in a comparable series (Fig. 1E). Na+-K+-ATPase activity did fall greatly (by about 60%) by 3 h of hypoxia but had fully recovered by 1 h of normoxia reestablishment (Fig. 7C), yet unidirectional flux rates remained depressed during this first hour (Fig. 1E). An important caveat here is the recent demonstration that in trout hepatocytes, low PO2 can reduce the transport activity of Na+-K+-ATPase before its ATP hydrolytic capacity (the parameter measured in the assay) is affected (5). It must be remembered, that Na+-K+-ATPase activity is assayed under optimal conditions in vitro, whereas in vivo, the intracellular milieu of the enzyme may change during hypoxia. This is an important area for future investigation. Second, during prolonged exposure to severe hypoxia, both JNain and JNaout were further reduced at later times (Fig. 3B), again pointing to the involvement of a second mechanism that intensified the effect of the initial inhibition. Third, in the kinetic analysis of JNain, Jmax was significantly depressed by about 60% during prolonged hypoxia (Fig. 5A), as might be expected from the observed 60% reduction in branchial Na+-K+-ATPase activity (Fig. 7C), that is, a reduction in the number of transport sites without a change in their affinity for Na+.
In summary, the data are consistent with downregulation of Na+ influx (and efflux) rates by at least two mechanisms during hypoxia. One is clearly by a delayed reduction in Na+-K+-ATPase hydrolytic activity. Notably, this appears to occur by posttranslational modification of enzyme activity, because specific Na+-K+-ATPase mRNA and protein abundance did not fall in a comparable experiment on Astronotus ocellatus, in which branchial Na+-K+-ATPase hydrolytic activity was depressed by about 50% after 4 h of hypoxia (37). There is also clearly another mechanism(s), which is (are) more rapid and more persistent, but additional work will be required to determine the relative contributions of O2 starvation on Na+-K+-ATPase transport activity, on channel closing, on changes in lamellar perfusion, and on alterations in the activity of other proteins (e.g., H+-ATPase, Na+/H+, and Na+/Na+ exchangers) in the observed responses. Regardless, the bottom line is that Astronotus ocellatus can withstand severe hypoxia without a marked disturbance of internal ion status, by simultaneously reducing Na+ pumping and leak rates at the gills.
The finding that external water pH did not change appreciably during hypoxia, and normoxia restoration demonstrates that the observed decreases in JNain and JNaout during hypoxia, and later increases during normoxic recovery were not an artifact of changing water pH. Furthermore, recent measurements of internal pH during a comparable hypoxia regime in the same species demonstrate that this is not a confounding factor either. Richards et al. (37) reported moderate acidosis of
0.15 units in both the blood plasma (extracellular fluid) and the white muscle (intracellular compartment) during hypoxia. By standard theory, this moderate internal acidification would be expected to "increase" Na+ influx (by stimulated Na+/H+ exchange, or stimulated H+-ATPase/Na+ channel activity; Refs. 3, 21, 25, 27, 34) so as to correct the acidosis, whereas we observed a "decrease" in Na+ influx during hypoxia.
Influence of hypoxia on ammonia excretion. Ammonia excretion rates (JAmm) were much higher on an absolute basis than Na+ influx rates (JNain) (Figs. 14), so any linkage of JAmm to JNain, if it occurs in the oscar, must be indirect. During normoxia, JAmm exhibited a Michaelis-Menten type dependence on external Na+ concentration (Fig. 5B), but the apparent Km was significantly lower (i.e., affinity for Na+ was higher) than for the simultaneously determined Michaelis-Menten dependence of JNain on external Na+ concentration, whereas the Jmax values were similar (Fig. 5A). Again, this result suggests that the coupling must be indirect rather than through a direct 1:1 Na+/NH4+ exchanger (e.g., 21, 27, 60). Regardless, the coupling is rapidly effective, such that experimental increases in water [Na+] quickly constrain an increase in JAmm. This is not seen in the rainbow trout (39), where arguments have been made for linkage either via a nonobligatory Na+/NH4+ exchanger (39) or via "diffusion-trapping" of NH3-linked to an H+-pump/Na+-channel system (3, 54).
During hypoxia, JAmm was reduced in a similar fashion to JNain and JNaout, and as with these Na+ fluxes, the inhibition became more intense during prolonged hypoxia and usually persisted during the first hour of restoration of normoxia (Figs. 14), again arguing for some sort of common mechanism. However, the responses often differed in exact time course and magnitude, and the apparent kinetic coupling of JAmm to external Na+ concentration was completely lost during prolonged hypoxia (Fig. 5B). It remains to be determined whether the declines in JAmm during hypoxia were driven primarily by a downregulation of the ammonia production rate (47, 48), or by specific hypoxia-induced blockade of the branchial ammonia excretion mechanism (e.g., by down-regulation of a Na+-linked transport system or channel arrest).
For several reasons, it appears likely that both phenomena were involved and that the latter predominated. Urea-N excretion (JUrea), although it represented only a small fraction of N-waste excretion, was reduced whenever JAmm was reduced during hypoxic exposures (Fig. 6). Urea arises from different metabolic pathways than ammonia in teleost fish (uricolysis or arginolysis rather than transdeamination or adenylate breakdown; see Refs. 51 and 56 for reviews). This suggests that a general reduction in metabolic N-waste production occurs during hypoxia, in parallel with depressed protein synthesis in many tissues (24). Likely, oxidation of N-rich fuels is reduced, while carbohydrate utilization is increased during hypoxia in accord with a general suppression of aerobic metabolic rate, reduction in protein turnover, and activation of anaerobic metabolism. However, the relative reduction in JAmm was greater than in JUrea (Fig. 7). Second, if the reduction in JAmm were simply a consequence of reduced production, it seems unlikely that it should persist during the first hour of normoxia restoration when aerobic metabolism was likely restored. And most cogently, plasma total ammonia concentration increased significantly by 3 h of hypoxic exposure (Fig. 7D), suggesting that the excretion mechanism was inhibited to a greater extent than the production mechanism. Nevertheless, the change in plasma ammonia was not large, so again the hypoxia-tolerant oscar appears to be rather good at maintaining internal homeostasis during severe O2 limitation.
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| ACKNOWLEDGMENTS |
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The costs of publication of this article were defrayed in part by the payment of page charges. The article must therefore be hereby marked "advertisement" in accordance with 18 U.S.C. Section 1734 solely to indicate this fact.
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