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First published online May 29, 2009
Journal of Experimental Biology 212, 1949-1964 (2009)
Published by The Company of Biologists 2009
doi: 10.1242/jeb.028464
Regulation of gill transcellular permeability and renal function during acute hypoxia in the Amazonian oscar (Astronotus ocellatus): new angles to the osmorespiratory compromise
1 Department of Biology, McMaster University, Hamilton, Ontario, Canada, L8S
4K1
2 Division of Marine Biology and Fisheries, Rosenstiel School of Marine and
Atmospheric Science, University of Miami, Miami, FL 33149, USA
3 Department of Zoology, University of British Columbia, Vancouver, Canada, V6T
1Z4
4 Department of Biology, University of Antwerp, Groenenborgerlaan 171, B-2020
Antwerp, Belgium
5 School of Biological Sciences, University of Plymouth, Devon PL4 8AA, UK
6 Department of Biology, San Diego State University, 5500 Campanile Drive, San
Diego, CA 92182, USA
7 Laboratory of Ecophysiology and Molecular Evolution, Instituto Nacional de
Pesquisas da Amazônia (INPA), Manaus, Brazil
* Author for correspondence (e-mail: woodcm{at}mcmaster.ca)
Accepted 16 March 2009
| Summary |
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Key words: sodium flux, potassium flux, PEG-4000, diffusive water flux, urine flow rate, glomerular filtration rate, gill morphology, mitochondria rich cell, transepithelial potential, fish
| INTRODUCTION |
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Oscars commonly encounter hypoxia in their natural environment when they
enter the seasonally flooded jungle to feed and reproduce; adults are reported
to survive up to 6 h of complete anoxia, and can tolerate levels of
5–20% air saturation for 20–50 h
(Almeida-Val and Hochachka,
1995
; Muusze et al.,
1998
; Almeida-Val et al.,
2000
). This ability appears to be the result of exceptional
capacities to both downregulate aerobic metabolic rate and to survive on
glycolytic metabolism (Muusze et al.,
1998
; Almeida-Val et al.,
2000
; Sloman et al.,
2006
; Richards et al.,
2007
). Thus one possible explanation is that under severe
O2 limitation, oscars do not attempt to increase gill O2
transfer in a situation where the potential for O2 uptake from the
water has become very slight. Instead they may simply close down the gills to
reduce osmoregulatory costs at a time when active ion influx has been reduced
by O2 starvation of the gill ion pumps. To address this
possibility, we recently measured ventilation and the branchial O2
transfer factor in adult oscars exposed to progressive, severe hypoxia, as
well as the O2 consumption rate of isolated gill epithelial cells
(Scott et al., 2008
). The
transfer factor is a measure of the relative ability of the respiratory
surface to exchange O2 and defined as the rate of O2
consumption divided by the mean PO2 driving
force for diffusion across that surface
(Randall et al., 1967
).
Contrary to these interpretations, ventilation increased down to a
PO2 of 10 torr, branchial O2
transfer factor increased down to a PO2 of 20
torr and returned to normoxic levels at 10 torr, and gill epithelial
O2 consumption actually increased down to a
PO2 below 5 torr. Thus, oscars increase
ventilation and the effective permeability of the gills to O2
during severe hypoxia in a comparable manner to hypoxia-intolerant teleosts
such as trout (Holeton and Randall,
1967
; Randall et al.,
1967
), and there is no evidence that the gill cells are
O2-starved at this time.
Therefore, in the present investigation, which used a
normoxia–hypoxia–normoxic recovery regime, our particular focus
was to elucidate the mechanism(s) behind the decrease in iono/osmotic
permeability which occurs in the absence of a reduction in O2
permeability during acute hypoxia. Our first objective was to ensure that the
previously observed reduction in Na+ efflux during acute hypoxia
was not an artefact of the indirect measurement technique used by Wood et al.
(Wood et al., 2007
) where
efflux was measured in the standard manner (cf.
Kirschner, 1970
;
Wood, 1992
) as the difference
between radioisotopically determined influx and non-radioactive net flux.
Therefore, in the present study, the fish were loaded with 22Na for
direct measurement of Na+ efflux. A further objective was to ensure
that the reduction in efflux was a gill phenomenon, by collecting urinary
output separately. Another goal was to eliminate the possibility that the
Na+ efflux reduction was simply a consequence of the reduction in
Na+ influx because of possible linkage of the two by exchange
diffusion [direct 1:1 coupling of a portion of Na+ efflux to
Na+ influx (cf. Gonzalez et
al., 2002
)]. Heart rate and ventilation rate were also measured
during the exposure regime to assess how these might contribute to the
observed responses. After clarification of these issues, a central objective
became the examination of other markers of gill permeability, which might be
diagnostic of changes in either paracellular permeability, transcellular
permeability, or both during acute hypoxia. These included net K+
flux, ammonia flux, osmotic water flux (by urine flow rate and weight
changes), diffusive water flux (by 3H2O exchange),
transepithelial potential (TEP), and tritium-labelled polyethylene glycol
([3H]PEG-4000) flux. The latter is a high molecular mass
paracellular permeability marker (Wood and
Pärt, 1997
), which is also an excellent extracellular space
(Munger et al., 1991
) and
glomerular filtration rate marker
(Beyenbach and Kirschner, 1976
)
in teleosts, so this allowed a more detailed assessment of kidney function
during acute hypoxia. Finally, we employed scanning electron microscopy to
look for morphological correlates of the reduction in gill permeability that
was observed. Overall, the results support the hypothesis that reduced
iono/osmotic permeability in the gills during severe hypoxia is through
channel arrest, i.e. through reduced transcellular permeability.
| MATERIALS AND METHODS |
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Experimental protocols
Soft water from the same well-water source as used during holding was
employed in all trials. Experimental temperature was 28±1.5°C.
Experimental chambers were 2.5 l Nalgene kitchen containers, which fitted the
horizontally flattened morphology of the fish. The lids accommodated a
portable O2 probe. The chambers (up to 12 at one time) were mounted
on a trough, which served as a water-bath, keeping the external water level
slightly below the internal water level for temperature control. The entire
trough drained into a vigorously aerated 800 l reservoir, from which water was
pumped back to the individual chambers at about 200 ml min–1.
Water in the reservoir was replaced daily. Thus each chamber was fitted with
an individual water line for flushing, and with an individual air-stone for
air or N2-gassing. Fish were placed in these individual containers
the evening before an experiment and left overnight to settle with continuous
water flow-through and aeration; black plastic shielding minimized visual
disturbance.
The standard protocol, with some variations, was a 3-h control period of normoxia, followed by 3–4 h of acute hypoxia, and then 2–3 h of normoxia again. In order to measure flux rates of various substances, the water inflow into each box was stopped at the beginning of the experiment, and the level set to a nominal volume of 1.5 l (or kept at 5.5 l in the blood gas trials). Exact volumes were determined by subtracting the mass of the fish when they were weighed at the end of the experiment. Flux rates were generally measured by withdrawing 10 ml or 20 ml water samples for assay at 0.5-h or 1-h intervals, depending on the experiment.
Normoxia (PO2 >130 torr) was maintained by vigorous aeration during the normoxic periods, and water PO2 was checked once per hour in each chamber with the portable O2 probe. Acute hypoxia was induced by changing the vigorous gassing to N2, and then maintaining the PO2 between 10–20 torr with more gentle gassing with N2 or air as required. During the hypoxia period, water PO2 was checked in each chamber every 15 min to ensure it stayed within the target range.
Series 1
The objective of this series was to confirm, by direct measurement, that
unidirectional Na+ efflux
(
) fell during acute
hypoxia, as previously recorded by indirect measurement
(Wood et al., 2007
), and that
the phenomenon occurred at the gills. This was accomplished by radiolabelling
the internal Na+ pool with 22Na, and recording the
appearance of radioactivity in the external water. Na+ net flux
(
) was also recorded, so
this approach allowed indirect measurement of Na+ influx
(
; see Calculations
section below). Net branchial K+ and ammonia fluxes were also
measured. The oscars were fitted with urinary bladder catheters to collect
urine flow outside the chamber, thereby allowing quantification of any renal
contribution to the responses. In addition this approach allowed direct
measurement of urine flow rate (UFR), an index of osmotic water permeability
(e.g. Potts et al., 1967
).
Oscars (N=7) were anaesthetized in 0.5 g l–1
MS-222 neutralized with 1.0 g l–1 NaHCO3 and
fitted with internal urinary bladder catheters (Clay-Adams PE50 tubing, with 2
cm PE160 sleeves attached by cyanoacrylate glue) as described by Wood and
Patrick (Wood and Patrick,
1994
). The sleeves were glued to the catheters and in turn were
anchored to the body wall by silk sutures. At this time, each fish received an
intra-peritoneal injection of 0.2 ml Cortland saline
(Wolf, 1963
) containing 10
µCi 22Na (manufactured by New England Nuclear-Dupont, Boston,
MA, USA, and supplied by REM, Sao Paulo, Brazil). The oscars were then
returned to their individual chambers and allowed to recover overnight
(
12 h) while UFR was collected to verify that the catheter was patent.
22Na equilibrates very rapidly in fish; for example, in the
killifish, Wood and Laurent (Wood and
Laurent, 2003
) found no differences in internal radiolabelled
Na+ pool if fish were injected and sampled after only 3 h or
allowed to equilibrate for 24 h. Therefore, in the oscar, 22Na was
fully equilibrated by the time experiments began the next morning.
Before the start of the experiment, the water in the reservoir was replaced and the fish boxes flushed to remove radioactivity, which had accumulated during the recovery and equilibration period. The chambers were then closed, and fluxes measured by sampling at 1-h intervals during 3 h of normoxia, 4 h of hypoxia, and 2 h of normoxic recovery. Water was analysed for 22Na radioactivity, and the concentrations of total Na+, K+ and ammonia. Urine was collected at hourly intervals for analysis of UFR, Na+, K+ and ammonia concentrations. At the end of the experiment, the fish were individually anaesthetized as before, and a 0.3 ml blood sample withdrawn by caudal puncture into a heparinized syringe. Plasma was separated by rapid centrifugation (2 min at 7000g) and analysed for 22Na radioactivity and total Na+ concentration. The fish were then returned to their chambers under flow-through conditions for overnight recovery before the experiments of Series 3. UFR collection was resumed to ensure continued patency of the urinary catheters.
Series 2
The objective of this series was to employ direct measurements of
to confirm that the
patterns previously reported by Wood et al.
(Wood et al., 2007
) in
uncannulated oscars occurred similarly in fish that had previously experienced
MS-222 anaesthesia and surgery so as to fit them with urinary bladder
catheters. A second objective was to confirm the indirect measurements of
of Series 1. This series
also supplied additional data on UFR and urine composition.
Oscars (N=10) were fitted with internal urinary bladder catheters as in series 1, but were not injected with 22Na. After overnight recovery, water flow to the fish chambers was stopped, and 2 µCi of 22Na was added to each chamber and allowed to mix for 1 h. The experiment was then started with the same protocol as in series 1: 3 h of normoxia, 4 h of hypoxia and 2 h of normoxic recovery. Water was sampled hourly for measurement of 22Na radioactivity and total Na+ concentration, and urine was collected at 1-h intervals for analysis of UFR, Na+, K+ and ammonia concentrations. Water samples were also analysed for K+ in six of the fish. Blood was not sampled at the end of the protocol, but instead oscars were left undisturbed under normoxia (with flow-through water) for an overnight collection of urine to further assess the recovery of UFR.
Series 3
The goal here was to check whether the phenomenon of exchange diffusion
(direct 1:1 linkage of a portion of
to
) was present in the gills
of oscars. This process was found in approximately half of the Amazonian
teleosts surveyed by Gonzalez et al.
(Gonzalez et al., 2002
), but
Astronotus ocellatus was not included in that survey.
After overnight recovery, replacement of the water in the reservoir and
flushing of the chambers, the urinary-catheterized fish (N=7)
originally used in Series 1 were subjected to two successive 3-h flux
measurements under normoxia. These oscars were still radiolabelled with the
22Na injected earlier. In the first flux determination, the
background Na+ concentration of the external water
([Na+]ext) was used. In the second,
[Na+]ext was acutely raised approximately 10-fold by
addition of sufficient NaCl, so as to stimulate
to approximate maximum
transport velocity, according to the
versus
[Na+]ext kinetic relationship reported by Wood et al.
(Wood et al., 2007
). Water
22Na radioactivity and total Na+ concentrations were
measured. At the end of the second flux determination, fish were anaesthetized
and blood-sampled as above for assay of plasma 22Na radioactivity
and total Na+ concentration. These determinations allowed direct
measurements of
and
, and therefore indirect
measurement of
.
Series 4
The goal here was to measure changes in heart rate and breathing rate
during the regime. Oscars (N=5) were anaesthetized as above, and
fish-hook impedance electrodes (varnish-coated copper wire, bare at the ends)
were implanted anterior and posterior to the heart using #22 hypodermic
needles. An impedance converter was used to check the positioning. Once a
strong signal was achieved, the needles were removed and electrodes were sewn
in place to the body wall with silk sutures, and the wires threaded through
PE60 tubing to avoid tangling. After overnight recovery, the fish were
subjected to a regime of 3 h of normoxia, 3 h of hypoxia, and 3 h of normoxic
recovery. Heart rate was recorded using the impedance converter, and breathing
rate was determined visually. Measurements were made at 0, 60, 120 and 180 min
of normoxia, at 5, 10, 15, 30, 45, 60, 90, 120, 150 and 180 min of hypoxia,
and at 5, 15, 30, 45, 60, 90, 120, 150 and 180 min of normoxic recovery.
Series 5
The objective of this series was to monitor transepithelial potential (TEP)
as a potential index of paracellular permeability changes. The
intra-peritoneal catheter technique pioneered by Potts and Eddy
(Potts and Eddy, 1973
), which
was validated against blood catheter measurements by Wood and Grosell
(Wood and Grosell, 2008
), was
employed. Oscars (N=7) were anaesthetized as above, and fitted with
saline-filled PE50 catheters inserted approximately 3–4 cm into the
coelom through a puncture site (made with a no. 19 hypodermic needle) in the
lateral body wall. A 2 cm PE160 sleeve, heat-flared at both ends, was glued to
the PE50 with cyanoacrylate glue and anchored to the body wall with several
silk sutures; this prevented the catheter from changing depth in the
coelom.
After overnight recovery, the fish were exposed to 3 h of normoxia, 3 h of
hypoxia, and 2 h of normoxic recovery, with hourly measurements of TEP. The
fish were then left under normoxic flow-through conditions for a further
overnight period. Thereafter, the oscars (now six, because of one catheter
failure) were exposed to sequentially increasing concentrations of external
Ca2+ ([Ca2+]ext) under normoxia in
half-logarithmic steps. The goal here was to test whether TEP in oscars
responded to [Ca2+]ext in the standard manner described
for many other teleosts, which is thought to reflect paracellular permeability
changes (Potts, 1984
). This
was achieved by addition of small volumes of a CaSO4 stock solution
at 0.5-h intervals. TEP was measured at the end of each 0.5-h period, at
nominal [Ca2+]ext concentrations of background (
18
µmol l–1) followed by 100, 320, 1000 and 3200 µmol
l–1.
Series 6
Diffusive exchange of water was measured by monitoring the efflux of
tritiated water (3H2O; manufactured by Perkin-Elmer
Wellesley, MA, USA, and supplied by REM, Sao Paulo, Brazil). Intraperitoneal
catheters were implanted as in Series 5, and the fish allowed to recover from
anaesthesia overnight. In preliminary trials under normoxia, we found that a
minimum equilibration period of 1 h was needed after intraperitoneal injection
before 3H2O efflux rates became stable. Thereafter
stable rates could be recorded for 3 h, after which recycling of the
radioisotope became a problem, because external specific activity exceeded 10%
of internal specific activity (Kirschner,
1970
). Therefore it was necessary to use three experimental groups
to cover the entire normoxia-hypoxia-normoxic recovery regime.
In the first group, covering the normoxic period, oscars (N=9) were injected under normoxia with 3H2O (10 µCi 3H2O in 200 µl Cortland saline, washed in with a further 200 µl saline). Injection via the intraperitoneal catheter avoided any handling or disturbance of the fish. After 1 h equilibration, water samples were withdrawn at 0.5-h intervals for a further 3 h. In the second group, covering the hypoxic period, oscars (N=10) were injected with the same dose of 3H2O under normoxia. However, after 1 h equilibration, hypoxia was instituted, and water samples taken at 0.5-h intervals for a further 3 h under hypoxia. In the third group, covering the normoxic recovery period, the fish (N=8) were first exposed to normoxia, and then to hypoxia for 2 h, at which time they were injected with the same dose of 3H2O. After a further 1 h equilibration under hypoxia, normoxia was restored and water samples were taken at 0.5 h intervals for the 3-h period of normoxic recovery. In all three groups, the boxes were then left closed with aeration for approximately 30 h after the original injection. A final water sample was taken to ascertain the exact dose of 3H2O which had been administered to each fish, because by this time the radioisotope had completely equilibrated between the fish and the water (see Calculations).
Series 7
The primary objective of this series was to measure the efflux of
tritium-labelled polyethylene glycol ([3H]PEG-4000; MW=4000, 1.28
mCi g–1; manufactured by New England Nuclear-Dupont, Boston,
MA, and supplied by REM, Sao Paulo, SP, Brazil) as a marker of gill
paracellular permeability (Wood and Part,
1997
). However since only a small portion of injected
[3H]PEG-4000 is excreted via the gills in teleosts, and a
much larger portion by the kidney (Curtis
and Wood, 1991
; Scott et al.,
2004
), it was essential that the fish be fitted with urinary
catheters to collect all renally excreted [3H]PEG-4000 outside the
fish chambers. Therefore, only branchially excreted [3H]PEG-4000
appeared in the external water. Additionally, this approach allowed us to
follow up the results of Series 1 with a more detailed assessment of kidney
function, because [3H]PEG-4000 is an excellent glomerular
filtration rate marker in teleosts
(Beyenbach and Kirschner,
1976
).
Oscars (N=12) were fitted with internal urinary bladder catheters
as in Series 1. While still anaesthetized, each fish was injected via
the caudal vein with 8 µCi [3H]PEG-4000 in 0.25 ml of saline,
washed in with a further 0.25 ml of saline. The fish were then allowed to
recover overnight for approximately 14 h for full equilibration of the label
throughout the extracellular compartment
(Munger et al., 1991
), during
which time UFR was monitored to ensure patency of the urinary catheters. Prior
to the start of the experiment, the water in the reservoir was replaced and
the fish boxes flushed to remove radioactivity that had accumulated during the
recovery and equilibration period. The chambers were then closed. The exposure
regime consisted of 3 h of normoxia, 3 h of hypoxia, and 3 h of normoxic
recovery, with water and urine samples collected at hourly intervals. At the
end of the experiment, the fish were individually anaesthetized as before, a
0.3 ml blood ample withdrawn by caudal puncture into a heparinized syringe,
and plasma was immediately separated by centrifugation. Water samples were
analysed for [3H]PEG-4000 radioactivity, and plasma and urine
samples were assayed for [3H]PEG-4000 radioactivity and
Na+ concentration. These measurements allowed calculation of gill
[3H]PEG-4000 clearance rate, glomerular filtration rate (GFR,
equivalent to renal [3H]PEG-4000 clearance rate), and renal
Na+ handling (see Calculations below).
Series 8
Reductions in UFR recorded in Series 1, 2 and 7 suggested that osmotic
water permeability (cf. Potts et al.,
1967
) was reduced during hypoxia. However, if rates of net water
entry (through the gills), and exit (through the kidney) were not in
equilibrium, then the change in UFR may not accurately reflect the change in
osmotic water permeability. The goal of this series was to address this issue
by measuring changes in body mass. As any handling may alter water fluxes in
fish, a paired design was employed where each fish served as its own control.
Oscars (N=10) were acclimated to their chambers overnight, then
anaesthetized as above, drained head-down in air for 15 s, patted thoroughly
dry with soft towels, and weighed to 0.01 g accuracy. They were then returned
to their chambers for a 6-h period of normoxia. The anaesthetization and
weighing procedure was then repeated, and the change in body mass recorded.
This protocol was duplicated in a second series with the same fish
(N=10) after a further 24 h of normoxia. The fish were again
anaesthetized, and the initial mass was measured as before. However, the final
mass was recorded after 3 h of normoxia plus 3 h of hypoxia, and the final
anaesthetic solution was equilibrated to the hypoxic
PO2. In each series, the change in body mass
was expressed relative to the initial mass as g kg–1 of the
initial mass.
Series 9
The objective of this final series was to look for possible changes in
branchial surface morphology accompanying the changes in gill permeability
seen during the normoxia–hypoxia–normoxic recovery regime in the
preceding series. Oscars were allowed to settle in their chambers overnight,
then killed under normoxia (N=6), and after 1 h of hypoxia
(N=6), 3 h of hypoxia (N=6), 1 h of normoxic recovery
(N=6) and 3 h of normoxic recovery (N=6). The fish were
anaesthetized as above, and then killed by cephalic concussion. The second
gill arch from the right hand side of each fish was excised, quickly rinsed in
water, then immediately placed in cold Karnovsky's fixative for storage at
4°C. The samples were later shipped to San Diego State University, CA,
USA, for examination by scanning electron microscopy.
Analytical techniques
Water PO2 was routinely monitored using a
portable O2 probe and meter (WTW Oxi325 Oximeter, Weilheim,
Germany). Water and urine total ammonia concentrations were measured
colorimetrically by the salicylate hypochlorite assay
(Verdouw et al., 1978
).
Na+ and K+ concentrations in water, plasma and urine
were determined by flame atomic absorption spectrophotometry (AAnalyst 800,
Perkin-Elmer, Wellesley, MA, USA). All radioactivity measurements
(22Na, 3H2O, [3H]PEG-4000) were
made by scintillation counting (LS6500, Beckman Coulter, Fullerton, CA, USA)
on sample volumes of 5 ml for water, and 20–100µl for plasma and
urine, made up to 5 ml with water, added to 5 ml of Packard Ultima Gold AB
Fluor (Perkin-Elmer, Wellesley, MA, USA). Internal standardization tests
demonstrated that quenching was constant, so no correction was necessary.
Urine flow rate (UFR) was determined gravimetrically.
Heart rate was measured using a Transmed 2991 impedance converter (Fullerton, CA, USA). Transepithelial potential (TEP) was measured by means of 3 mol l–1 KCl–agar bridges connected via Ag/AgCl electrodes (WPI, Sarasota, FL, USA) to a high impedance electrometer (Radiometer pHM 82 meter, Copenhagen, Denmark). The reference bridge was placed in the water in the fish chamber, and the measurement bridge was connected to the saline-filled intraperitoneal catheter. TEP measurements were expressed relative to the water side as 0 mV after correction for junction potential, which was less than 2 mV in all cases.
For gill morphology, the Karnovsky-fixed gill samples were rinsed in 0.1 mol l–1 phosphate-buffered saline (PBS), and post-fixed in 1% osmium tetroxide. The samples were then dehydrated in ascending concentrations of ethanol from 30%, concluding at 100%, critical-point-dried with liquid CO2, mounted on the stubs and sputter-coated with gold for examination by scanning electron microscopy (SEM). The general structure of the gills and surface structure of the filamental and lamellar epithelia were examined with a Hitachi S 2700 scanning electron microscope (Tokyo, Japan) at an accelerating voltage of 20 kV. Morphometric quantification of mitochondria-rich cells (MRC) density (number of MRCs per mm2 was performed on randomly selected areas of trailing edges of filaments behind the respiratory lamellae. SE micrographs (x2000 magnification) of five randomly selected areas of filament epithelium for each fish were analysed. The number of apical crypts of MRCs per unit area was counted. The individual surface areas of 30 MRCs were calculated on photographs at x6000 magnification according to the shape of their two-dimensional apical openings, which varied from circular to oval, triangular and roughly trapezoidal.
Calculations
Net flux rates (in µmol kg–1 h–1) of
Na+ (
),
K+ and total ammonia were calculated from changes in concentration
(in µmoll–1), factored by the known fish mass (in kg),
volume (in l), and time (in h). The traditional method for determining
unidirectional Na+ fluxes
(Kirschner, 1970
;
Wood, 1992
) is to measure
influx (
, by convention
positive) directly as the disappearance of 22Na radioactivity from
the external water, and to calculate efflux
(
, by convention
negative) as the difference, using the conservation equation:
![]() | (1) |
![]() | (2) |
However, it is also possible to measure Na+ efflux directly by the appearance of 22Na radioactivity in the external water, from the extracellular fluid of the fish. This approach is rarely used because it requires far more radioisotope, but was employed in Series 1 and 3.
In this method, efflux is calculated as:
![]() | (3) |
, so no correction was
made.
In Series 6, the rate constant of 3H2O efflux was
calculated from the rate of decline in total 3H2O in the
fish, which was approximately exponential with time
(Evans, 1967
):
![]() | (4) |
Absolute rates of diffusive water efflux were calculated as the product of
k multiplied by the water space of the fish (assumed to be 800 ml
kg–1) (Holmes and Donaldson, 1971;
Olson, 1992
). In practice,
water efflux rates were calculated for each 1-h period of the experiment, by
regressing the three measurements of CPM at 0, 0.5 and 1 h against
time to yield the slope k. By measuring the 3H in the water after
30 h, when complete equilibration between the fish and the water had occurred,
it was possible to calculate accurately the total amount of radioactivity
(CPMtotal) in the system. The volume of the system was
taken as the measured volume of external water plus the water space of the
fish. Therefore, from CPMtotal and from measurements of
3H appearance in the water at each time interval, it was possible
to keep track of CPM in the fish at each time during the
experiment.
In Series 1, 2 and 7, urinary excretion rates (ER) were calculated as the
product of urine flow rate (UFR) multiplied by the measured concentrations
(e.g. Na+, K+, total ammonia, [3H]PEG-4000)
in the urine. In Series 7, the rate of clearance of [3H]PEG-4000
across the gills and through the urine were calculated. As clearance rate
represents the volume of plasma cleared per kg per h, the calculation requires
an estimate of [3H]PEG-4000 radioactivity in plasma at each time
during the experiment. We assumed that this marker was distributed at plasma
concentration in a space of 250 ml kg–1, i.e. a volume chosen
to approximate the extracellular space (Holmes and Donaldson, 1971;
Olson, 1992
). We calculated
the total [3H]PEG-4000 radioactivity in the fish at the end of the
experiment as the product of this extracellular space multiplied by the final
measured plasma concentration in the terminal blood sample. By keeping track
of the total amount of [3H]PEG-4000 radioactivity excreted into the
water and in the urine in each flux period, we were able to calculate the
amount present in the extracellular space at the beginning and end of each
flux period, and therefore the average plasma concentration of
[3H]PEG-4000 during the flux period in question. Clearance rates
(in ml plasma kg–1 h–1) were then calculated
as the amounts excreted through each route during the flux period, factored by
the fish mass, time, and average plasma concentration:
![]() | (5) |
![]() | (6) |
In Series 7, urinary Na+ and water handling (cf.
Wood and Patrick, 1994
) were
assessed as:
![]() | (7) |
![]() | (8) |
![]() | (9) |
![]() | (10) |
![]() | (11) |
All data have been reported as means ± 1 s.e.m. (N).
Relationships were assessed by one-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. Student's two-tailed
t-test was used for single comparisons. A significance level of
P
0.05 was used throughout.
| RESULTS |
|---|
|
|
|---|
and
at the gills during hypoxia
was reduced during acute
hypoxia, and that this occurred at the gills. The control rates under normoxia
were approximately –350 µmol kg–1
h–1. The decrease in
became significant by
the second hour of hypoxia and persisted through to the fourth hour, averaging
about a 55% reduction (Fig.
1A).
increased significantly during the first hour of normoxic recovery, returning
immediately to the original normoxic control levels.
(approximately –90
µmol kg–1 h–1) did not change
significantly during the regime relative to normoxic control levels, but
became more negative than during hypoxia in the first hour of normoxic
recovery (Fig. 1A).
Measurements of
and
allowed calculation of
, which showed similar
trends to
, approximately +260
µmol kg–1 h–1 under normoxia, declined
significantly during acute hypoxia, the decreases becoming significant by the
second hour and averaging about 70% through to the fourth hour
(Fig. 1A).
increased significantly
upon re-institution of normoxia, returning to values not significantly
different from the original control levels.
|
by measurement of
22Na disappearance from the water, using bladder-catheterized
oscars (Series 2), produced data very similar to those reported earlier by
Wood et al. (Wood et al.,
2007
was measured directly.
In Series 2, directly measured
fell by 80% and
indirectly measured
fell by 60%
during acute hypoxia, without significant change in
. The only substantive
difference from the pattern of Fig.
1A was that directly measured
remained significantly
depressed during the first hour of normoxic recovery, but was restored during
the second hour, in accord with the report of Wood et al.
(Wood et al., 2007
|
Ammonia excretion rates via the gills during hypoxia
In Series 1, ammonia excretion rates were around –440 µmol
kg–1 h–1 under control normoxic conditions,
but declined markedly during hypoxia (Fig.
1C). There was no change in the first hour, but thereafter they
stabilized at a 75% reduction through to the fourth hour. Ammonia excretion
increased significantly during the first hour of normoxic recovery, returning
to values not significantly different from the original control levels at this
time. An almost identical pattern was seen in Series 2 (data not shown).
Urine flow rate and urinary excretion rates during hypoxia
The urine collections (combined data of Series 1 and 2) demonstrated that
UFR, which was approximately 3 ml kg–1 h–1
under normoxic control conditions, fell by about 75% during hypoxia; the
decrease became significant by the second hour of exposure, and remained
significant in the first hour of normoxic recovery
(Fig. 2A). Thereafter, UFR
recovered and indeed rebounded above the original control rate during the
following overnight collection, a period of about 12 h. In Series 1 the fish
were handled (blood-sampled) before this second overnight collection, whereas
in Series 2 the fish were not handled, but the overshoot occurred in both
series, so the data were combined.
Urinary [Na+] was about 11 mmol l–1 under
normoxia, and tended to rise slightly during hypoxia, and decline during
normoxic recovery but the changes were not significant
(Fig. 2C). Therefore urinary
Na+ excretion rate (ERNa) tended to track UFR,
falling from control rates of approximately –33 µmol
kg–1 h–1 under normoxia to –15 µmol
kg–1 h–1 under hypoxia
(Fig. 2B). The decreases in
ERNa were significant in the second and fourth hours of
hypoxia, and the first hour of normoxic recovery. Thereafter, control rates of
ERNa were restored. Overall, urinary Na+ losses
(Fig. 2C) were only about 25%
of the total, the other 75% occurring across the gills as
(cf.
Fig. 1A).
Urinary [ammonia] was less than 3 mmol l–1 and remained stable during hypoxia and normoxic recovery (Fig. 2C), so ERAmm (Fig. 2B) directly tracked the changes in UFR (Fig. 2A). Excretion of ammonia through the urine was very low (about –7 µmol kg–1 h–1 under normoxia), averaging less than 2% of the excretion rate across the gills (cf. Fig. 1C).
Urinary [K+] was not measured on all samples because of sample volume limitations. However, as for [Na+] and [ammonia], urinary [K+] appeared to remain stable [1.09±0.09 mmol l–1 (15) under normoxia versus 0.83±0.14 mmol l–1 (13) under hypoxia], so ERK again appeared to track UFR, and amounted to only about 10% of net rate of K+ loss across the gills (cf. Fig. 1B).
Lack of Na+ exchange diffusion
When water [Na+]ext was acutely increased from
135±2 µmol l–1 (7) to 1232±43 µmol
l–1 (7) in bladder-catheterized oscars of Series 3,
increased almost
threefold in the expected fashion, but branchial
, measured directly, did
not change, so
became
positive (Fig. 3). Therefore
the phenomenon of exchange diffusion, an obligatory 1:1 linkage of a portion
of
to
, does not appear to occur
in the gill Na+ transport system of oscars.
|
|
|
|
Clearance rates of [3H]PEG-4000 via the gills during hypoxia
The rate of clearance of the paracellular permeability marker polyethylene
glycol (M.W.=4000; [3H]PEG-4000) across the gills in
bladder-catheterized oscars of Series 7 did not change significantly during
acute hypoxia or during normoxic recovery
(Fig. 7). Gill clearance rates
were extremely low, averaging only about 0.4 ml plasma kg–1
h–1, or about 5% of the simultaneously measured clearance
rate of [3H]PEG-4000 via the urine (cf.
Fig. 8A).
|
|
Calculations of renal Na+ handling (cf. Eqns 7, 8, 9, 10) in Series 7, summarized in Table 1, demonstrated that tubular Na+ reabsorption rate (RRNa) closely tracked the glomerular filtration rate of Na+ (FRNa). Both fell greatly during hypoxia, and recovered upon return to normoxia. Urinary Na+ excretion rate (ERNa) also fell significantly during hypoxia, and recovered thereafter during normoxia (Table 1), in accord with the results of Series 1 and 2 (cf. Fig. 2B). Under normoxia, the clearance ratio for Na+ was about 0.04, indicating highly efficient fractional reabsorption (96%), whereas that of water was about 0.61, indicating only 39% reabsorption. During hypoxia, the tubules became slightly less efficient at discriminating between Na+ and water, as the Na+ clearance ratio (CRNa) doubled, indicating 92% reabsorption, whereas the clearance ratio of water (CRH2O; cf. Eqn 11) decreased slightly, indicating 46% reabsorption. These trends reversed during normoxic recovery (Table 1).
|
Surface morphology of the gills during hypoxia
In Series 9, scanning electron microscopy revealed a typical teleost gill
structure with long filaments and well-defined respiratory lamellae. At a
macro-level, this structure did not change during hypoxia and normoxic
recovery, but there were pronounced changes in surface morphology. These
changes were already substantial by 1 h of hypoxia, but even more pronounced
by 3 h; they were partially reversed by 1 h of normoxic recovery, and fully
reversed by 3 h. Under normoxia, there were abundant mitochondria rich cells
(MRCs) on the trailing edges of the filaments and on the lamellae
(Fig. 9A). The MRCs were
recessed, opening to the surface by irregularly shaped apical crypts in
between large pavement cells (PVCs) with complex surface patterns composed of
numerous apical microridges (Fig.
9B). Occasional mucus cells (MCs) were visible, interdigitating
between the PVCs. At higher magnification, typical apical crypts were
relatively flat, and roughly trapezoid or triangular with a sieve-like surface
structure composed of interdigitated and fused microplicae
(Fig. 9C). During hypoxia, MRCs
disappeared from the lamellar surface and became far less abundant on the
filamental surface as many of the apical crypts closed
(Fig. 9D). The remaining MRC
crypts were much smaller, and more deeply recessed
(Fig. 9E). PVC morphology was
also altered, becoming simpler with a smooth central part and fewer concentric
microridges concentrated at the outer edges of the cells, suggesting a
stretching associated with covering of the crypts. At higher magnification,
apical crypts of the MRCs were greatly reduced in surface area, and tended to
be highly concave (Fig. 9F).
However, MCs did not change their appearance.
|
Morphometric analysis of high power micrographs demonstrated that apparent MRC density (i.e. number of apical crypt openings per mm2) on surfaces of the trailing edges of the filaments (about 1700 mm–2 under normoxia) fell significantly by 1 h, and was reduced by 47% after 3 h of hypoxia (Fig. 10A). Simultaneously, the average surface area of individual apical crypts, which was approximately 5.6 µm2 under normoxia, declined by 65% during hypoxia (Fig. 10B). Thus total exposed MRC area on the filament surfaces declined by about 80% during hypoxia. By 1 h of return to normoxia, these effects were significantly reversed, and by 3 h, recovery of both MRC density (Fig. 10A) and apical crypt surface area (Fig. 10B) was complete.
|
| DISCUSSION |
|---|
|
|
|---|
at the gills, as well as a large inhibition of
, such that net
Na+ balance remains approximately constant
(Fig. 1A). This is in accord
with our earlier work, in which reciprocal methodology (direct measurement of
by 22Na
disappearance from the water, indirect determination of
) was employed, and
urinary Na+ efflux was not collected separately
(Wood et al., 2007
is not
directly due to the reduction of
via an
obligatory 1:1 linkage. The two phenomena appear to be independent, which is
also evidenced by the fact that in some individual fish
was markedly reduced
before
(or vice
versa) during hypoxia, and/or increased after
during normoxic
recovery. These trends have also been seen in the overall means in some
experimental series [e.g. figure
1B and figure 2B of
Wood et al. (Wood et al.,
2007
Whatever their causes, the advantages of these changes are obvious in a
species that is routinely exposed to severe O2 regimes that are
inescapable and part of its normal lifestyle in the Amazon floodplain
(Val and Almeida-Val, 1995
).
The cost of ionoregulation in freshwater fish has been estimated as
2–20% of resting metabolism (reviewed by
Febry and Lutz, 1987
), and
direct measurements of O2 consumption by perfused gills yield
similar values (4–12%) (Wood et al.,
1978
; Lyndon,
1994
; Morgan and Iwama,
1999
). The ion-poor nature of Amazonian waters
(Sioli, 1984
) may exacerbate
these costs, so at a time of severe O2 limitation, it makes sense
to turn down active ion uptake at the gills, as long as ion efflux can be
similarly reduced. Dispersed gill cells of oscars appear to be perfectly
capable of maintaining cellular O2 uptake at
PO2s even lower than used in the present study;
indeed, even the PO2 of expired water during
severe hypoxia was higher than the levels that inhibited gill cell respiration
(Scott et al., 2008
).
Therefore, reduction of active transport during hypoxia is probably a
regulated phenomenon, rather than an automatic consequence of O2
starvation. Indeed both Richards et al.
(Richards et al., 2007
) and
Wood et al. (Wood et al.,
2007
) reported that gill Na+/K+-ATPase
activity was downregulated by 60–65% after 3–4 h of severe
hypoxia, and Lewis et al. (Lewis et al.,
2007
) noted a comparable decrease in gill protein synthesis
rate.
The present results confirm that ion efflux rates at the gills are greatly
reduced during severe hypoxia (Fig.
1A,B). Therefore plasma ion levels do not fall during hypoxia
(Richards et al., 2007
;
Wood et al., 2007
). In
addition, ion loss rates through the urine are also decreased
(Fig. 2B;
Table 1), providing a smaller
but still significant benefit. The larger cost-saving at the kidney may lie in
the fact that Na+ reabsorption rate in the kidney tubules, which is
presumably active (Hickman and Trump,
1969
; Wood and Patrick,
1994
), is able to fall by 70% during hypoxia
(Table 1) yet still achieve
improved Na+ conservation, thanks to the fact that glomerular
filtration rate (Fig. 8A) and
therefore filtered Na+ load
(Table 1) both decline so
dramatically at this time.
Note that even during normoxia, these fasted oscars were in net negative
Na+ balance (Fig.
1A). Negative ion balance is typical of Amazonian fish in ion-poor
native waters, and almost certainly the deficit is normally made up by
electrolytes in the natural diet (Gonzalez
et al., 2002
; Gonzalez et al.,
2005
). The pellet diet which keeps these fish healthy in the lab
contains substantial quantities of electrolytes (see Materials and
methods).
Renal function during hypoxia
Renal function has not been assessed previously in Astronotus
ocellatus or closely related species, but resting normoxic levels of GFR,
UFR, and urinary Na+ and ammonia excretion lie within the ranges
reported for other freshwater teleosts
(Hickman and Trump, 1969
;
Wood and Patrick, 1994
). We
are aware of only four previous studies on renal function during acute hypoxia
in fish, all on the freshwater rainbow trout, and all showing exactly opposite
trends to those in oscar – i.e. increased UFR and increased urinary
Na+ excretion rate (Hunn,
1969
; Swift and Lloyd,
1974
; Kobayashi and Wood,
1980
; Tervonen et al.,
2006
). Tervonen et al.
(Tervonen et al., 2006
)
implicated the mobilization of cardiac natriuretic peptide in the
hypoxia-induced diuresis. Although GFR was not measured in any of these
investigations, the responses were probably analogous to the situation during
exercise in trout, where GFR and UFR increase in parallel and urinary
Na+ excretion rises (Wood and
Randall, 1973b
; Hofmann and
Butler, 1979
). These responses to exercise were attributed to the
traditional osmorespiratory compromise – i.e. increased osmotic water
entry at the gills accompanying increased
O2. By contrast,
the decrease in both GFR (Fig.
8A) and UFR (Fig.
8B) during acute hypoxia in the oscar appears to be facilitated in
part by a reduction in the rate of osmotic water entry at the gills, but this
is not the complete explanation. UFR declined by 70% during hypoxia in both
Series 2 and 3 (Fig. 2A) and in
Series 7 (Fig. 8B). The
measurements of mass gain during hypoxia in Series 9 indicated that only about
42% of the reduction in UFR during hypoxia was actually due to decreased
osmotic water entry, the remainder representing water that accumulated in the
fish as a result of the reduction in GFR. This accumulated water was
subsequently cleared by the overshoot in UFR during overnight normoxic
recovery (Fig. 2A). Thus the
rate of osmotic water entry fell by only 30% during hypoxia, while the GFR and
UFR declines were both greater. Hypoxia is known to alter organ blood flow
distribution (Schwerte et al.,
2003
) so the decline in GFR may reflect a fall in kidney
perfusion. This can be viewed as another cost-saving measure, minimizing
workloads of both the cardiovascular system and tubular Na+
reabsorption (Table 1), as
argued previously. Interestingly, Na+ reabsorption and the
discrimination between Na+ and H2O reabsorption became
slightly less efficient, as indicated by the clearance ratio analysis of
Table 1. This may reflect
direct effects of low blood PO2s on tubular
reabsorption processes (Epstein et al.,
1994
).
Heart rate changes during hypoxia
In common with virtually all other teleosts, oscars exhibited a profound
bradycardia during hypoxia (Fig.
4A). This is undoubtedly of vagal origin. The adaptive
significance of the response remains controversial, but most interpretations
relate to either protecting cardiac function in the face of low
PO2 or a change in pattern of blood flow and/or
pressure at the gills so as to improve the efficiency of respiratory gas
exchange (reviewed by Sollid and Nilsson,
2006
; Farrell,
2007
). The latter is in accord with the increased branchial
O2 transfer factor down to a PO2 of
20 torr with a return to normoxic levels at 10 torr reported by Scott et al.
(Scott et al., 2008
) in
hypoxic oscars. None of the interpretations offered for bradycardia suggest
that gas exchange efficiency is reduced, so this is unlikely to be the cause
of the observed changes in gill permeability to ions and water.
How are oscars able to turn down gill ionic and osmotic permeability during hypoxia?
Permeability regulation at the gills of oscars during hypoxia is very
different from the traditional osmorespiratory during exercise. It could be
argued that this is because the gas exchange situation is different.
O2 declines
during hypoxia (e.g. Muusze et al.,
1998
; Sloman et al.,
2006
; Scott et al.,
2008
) but increases greatly during exercise. However branchial
O2 transfer factor does not fall during acute hypoxia
(Scott et al., 2008
).
Furthermore, Lewis et al. (Lewis et al.,
2007
) reported that during normoxic recovery from an acute hypoxic
exposure very similar to that used here, oscars exhibited a 270% overshoot in
O2 relative to
control levels, yet there was no elevation of ion loss rates
(Fig. 1) or water exchange
rates (Fig. 6) above control
levels at this time in the present study
(Fig. 1). So how are oscars
able to turn down gill ionic and osmotic permeability during hypoxia without
impeding respiratory gas exchange?
At a simpler level, we can ask whether this branchial permeability reduction is a transcellular or paracellular event. The various marker substances and experimental approaches used in this study cast some light on this issue, and with one exception (transepithelial potential), they point clearly to the former – a regulated reduction in transcellular permeability by 50–80%.
K+ loss rates, which fell markedly during hypoxia, and recovered
during normoxic restoration (Fig.
1B) are one such indicator. Because K+ concentrations
inside cells are about 100-fold greater than those in blood plasma, Lauren and
McDonald (Lauren and McDonald,
1985
) argued that K+ loss rates at the gills of
freshwater fish mainly reflect transcellular permeability. Had the gill cells
become depolarized during hypoxia, increased K+ leakage into the
water would have been expected (Boutilier,
2001
), but this did not occur.
Ammonia efflux rates (Fig.
1C), which followed a comparable pattern of reduction during
hypoxia (Fig. 1C), are another
such indicator. Note that plasma total ammonia levels increased during this
hypoxic regime, so this was not driven by decreased internal ammonia levels
(Wood et al., 2007
). Although
the exact mechanism(s) of ammonia efflux across the gills remains
controversial, all models propose a transcellular route (cf.
Wilkie, 2002
). Recent findings
that Rh glycoproteins in the gill cell membranes are central to the process
(Nakata et al., 2007; Nawata et al.,
2007
) reinforce this conclusion. The situation is slightly
complicated by the fact that there is an apparent coupling of ammonia efflux
to
during normoxia in
oscars, but this linkage is lost during hypoxia
(Wood et al., 2007
). Ammonia
production rates may also decline during hypoxia
(van den Thillart and Kesbeke,
1978
; van Waarde,
1983
), but since plasma total ammonia levels increase, ammonia
excretion rate must be inhibited to a greater extent than production rate.
There was a marked attenuation of the negative TEP during hypoxia
(Fig. 5A). Our original
rationale in monitoring TEP was to use it as an indicator of paracellular
permeabity changes, because the traditional interpretation of the TEP in
freshwater teleosts is that it is a diffusion potential caused by the
differential permeability of the gills to Na+ versus
Cl– (Potts,
1984
). The typical modulating effect of increasing
[Ca2+]ext (Fig.
5B), which has been seen in at least one other Amazonian fish
(Wood et al., 1998
) and many
temperate freshwater teleosts (Eddy,
1975
; McWilliams and Potts,
1978
; Wood and Grosell,
2008
) is attributed to the ability of divalent Ca2+ to
`tighten' the epithelium. The default assumption has always been that these
effects occur at the paracellular pathway junctions, but we are aware of no
definitive evidence that this is the case. Indeed, McDonald and Rogano
(McDonald and Rogano, 1986
)
reported that whereas higher water [Ca2+]ext greatly
reduced Na+ fluxes, it did not alter the clearance rate of the
paracellular marker mannitol across the gills of freshwater trout. If indeed
the bulk of Na+ leakage occurs through the cell membranes of the
branchial epithelium, then the `tightening effects' of both hypoxia and
[Ca2+]ext may instead be operating on transcellular
membrane channels.
Diffusive water efflux rate constants (k) measured with
3H2O (about 0.43 h–1 during normoxia),
were generally very low in comparison to other teleosts, and close to those
measured in the semi-terrestrial lungfish (reviewed by
Patel et al., 2009
). This fits
with the general conclusion that gill permeability is low to start with in
oscars as an adaptation to their challenging environment
(Wood et al., 2007
). The 70%
reduction in k values and diffusive water efflux rates during hypoxia, and
their rapid recovery during restoration of normoxia
(Fig. 6), when compared with
UFR data (Fig. 2A,
Fig. 8B) point to transcellular
regulation. Diffusive water flux at fish gills is generally considered to
occur by the transcellular route (Isaia,
1984
; McDonald et al.,
1991
). The present results are very different from those of Loretz
(Loretz, 1979
) working on
goldfish, who found a pronounced increase in diffusive water exchange during a
much less severe hypoxia, in accord with the prediction of the traditional
osmorespiratory compromise (Randall et
al., 1972
; Nilsson,
2007
). They also differ from those of McDonald et al.
(McDonald et al., 1991
) who
reported marked increases in diffusive water fluxes in rainbow trout, yellow
perch, and smallmouth bass subjected to confinement stress.
By reasonable estimate of internal (300 mOsm) and external (2 mosmol)
osmolarity, and the calculation approach developed by Potts et al.
(Potts et al., 1967
), it is
possible to estimate the net diffusive water flux from the data of
Fig. 6. This is about 0.53% of
the unidirectional efflux rates or about 1.70 ml kg–1
h–1 during normoxia, falling to 0.51 ml kg–1
h–1 after 3 h of hypoxia. UFRs, the traditional measure of
net osmotic water flux (Isaia,
1984
), are about 1.7–2.9-fold higher than these values. This
ratio is very typical for freshwater teleost fish. Isaia
(Isaia, 1984
) summarized
comparable calculations for four freshwater teleosts (trout, eel, goldfish and
flounder) yielding a mean ratio of 2.75 (range 2.1–3.3). This modest
discrepancy has been recognized for many years and reflects the idea that
diffusive water exchange mainly occurs through the cell membrane in freshwater
teleosts, whereas osmotic water flux may additionally involve bulk flow
through `pores' or paracellular channels
(Potts et al., 1967
;
Evans, 1969
;
Motais et al., 1969
;
Loretz, 1979
;
Isaia, 1984
). As calculated
earlier from the UFR and weight gain data, osmotic permeability (transcellular
plus paracellular flux) in the oscar fell by only 30% during hypoxia, while
diffusive water permeability (mainly transcellular flux) fell by 70%. The
implication is that most of the reduction was in the transcellular
component.
The branchial [3H]PEG-4000 clearance data
(Fig. 7) provide the most
compelling evidence that gill permeability in hypoxic oscars is downregulated
at a transcellular rather than a paracellular level. It is most unlikely that
this large, uncharged molecule would move through cell membranes, and for this
reason it has often been used successfully as an extracellular space marker
(Munger et al., 1991
;
Olson, 1992
) and gill
paracellular permeability marker (Curtis
and Wood, 1991
; Kelly and
Wood, 2002
; Scott et al.,
2004
) in teleost fish. The present results
(Fig. 7) demonstrate that gill
paracellular permeability to PEG-4000 does not change during hypoxia. However,
given the diversity of tight junction proteins, it remains possible that a
single molecule such as PEG-4000 may not serve as a faithful marker for all
paracellular fluxes. For example, a particular tight junction protein might
regulate paracellular Na+ flux more than paracellular
Cl– flux; this is an important area for future investigation.
It is also noteworthy that gill [3H]PEG-4000 clearance rates in
oscar (0.3–0.6 ml plasma kg–1 h–1;
Fig. 7) are lower than in other
freshwater teleosts such as trout (0.7–1.2 ml plasma
kg–1 h–1)
(Curtis and Wood, 1991
) and
killifish (1.3–4.3 ml plasma kg–1 h–1)
(Scott et al., 2004
), again
pointing to generally low gill permeability in Astronotus
ocellatus.
We propose that the reduction in gill transcellular permeability during
acute hypoxia in the oscar is caused by the effective closure of membrane
channels in the gill epithelial cells. This would conserve both ions and
energy as outlined above. This idea is reminiscent of the `channel arrest'
hypothesis proposed to explain survival of the brain and liver in other
severely hypoxia-tolerant organisms such as turtles and Crucian carp
(Hochachka, 1986
;
Boutilier, 2001
; Boutilier and
St-Pierre, 2001; Hochachka and Lutz,
2001
).
An obvious question is the nature of the channels that are effectively
closed. We speculate that they are in fact a wide variety of channels –
e.g. aquaporins for water (Evans et al.,
2005
), Rh proteins for ammonia
(Nakada et al., 2007
;
Nawata et al., 2007
), UT
proteins for urea (McDonald et al.,
2006
), and potassium channels for K+
(Boutilier, 2001
; Boutilier and
St-Pierre, 2001). The nature of the Na+ channel is particularly
interesting. Although most models of Na+ uptake in freshwater fish
incorporate an epithelial Na+ channel (e.g.
Evans et al., 2005
;
Marshall and Grosell, 2006
),
it has never been found at a genomic level. Regardless, since exchange
diffusion of Na+ is absent in Astronotus ocellatus and the
reduction in Na+ efflux appears not to be directly linked to the
reduction in Na+ influx during hypoxia, then the `Na+
channels' involved must be different from the ones contributing to
Na+ uptake. How does hypoxia close so many different channels? It
is possible that the channels actually close individually or are removed at
the level of the lipoprotein bilayer, but there may be a simpler explanation
as outlined below, which does not require that all the channels be
O2-sensitive by themselves.
Morphological correlates of the channel arrest hypothesis
Unlike several other hypoxia-tolerant species, such as the Crucian carp
(Sollid et al., 2003
;
Sollid et al., 2005
;
Sollid and Nilsson, 2006
)
goldfish (Sollid et al.,
2005
), and naked carp (Matey
et al., 2008
), the oscar did not exhibit `remodelling' of the gill
macrostructure during hypoxia. In the carp and goldfish, the gills actually
gained surface area by losing inter-lamellar masses during hypoxia, whereas we
had suspected that the opposite might occur in the oscar. Although it did not,
it is possible that such alterations might have been seen had the duration of
hypoxic exposure been longer. Nevertheless, we believe that the rapid and
dramatic changes in gill surface morphology recorded during acute hypoxia may
represent the morphological correlate of the channel arrest hypothesis. The
55–75% decreases in fluxes of Na+, K+, ammonia and
water may be explained by the approximately 80% decrease in exposed MRC
surface area, most of which occurred after only 1 h
(Fig. 10). Apparently, this
occurred by PVCs covering them. Generally low branchial flux rates of all
substances in the oscar may be explained by the fact that the MRCs open only
through small apical crypts, in contrast to much more extensive surface
exposure in species such as trout (Goss et
al., 1995
; Goss et al.,
1998
). Indeed, one of the tenets of the channel arrest hypothesis
is that effective ion channel densities should be inherently lower in
hypoxia-tolerant animals (Hochachka,
1986
; Boutilier,
2001
). In the case of the gills of oscar, only small changes in
PVC coverage are needed to effect closure of apical crypts. This
interpretation assumes that the MRCs, not the PVCs are the sites of these
transcellular fluxes in the oscar. Although this idea is unusual, to our
knowledge, there is as yet no definitive evidence apportioning transcellular
fluxes in a quantitative manner between MRCs and PVCs in any freshwater
teleost fish. However, it now seems to be widely accepted that changes in
coverage of the MRCs by PVCs plays a large role in ion and acid–base
fluxes responsible for correction of systemic pH disturbances
(Goss et al., 1995
;
Goss et al., 1998
). Our
argument, in the case of the oscar, is that comparable coverage plays an
important role in the rapid change in transcellular fluxes which occur during
acute hypoxia. In future, more extensive examination of MRC and PVC fine
structure in the gills of normoxic and hypoxic oscars, using transmission
electron microscopy, coupled with autoradiography to pinpoint the location of
labelled markers, may cast light on this idea.
| Footnotes |
|---|
| References |
|---|
|
|
|---|
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Almeida-Val, V. M. F., Val, A. L., Duncan, W. P., Souza, F. C. A., Paula-Silva, M. N. and Land, S. (2000). Scaling effects on hypoxia tolerance in the Amazon fish Astronotus ocellatus (Perciformes: Cichlidae): contribution of tissue enzyme levels. Comp. Biochem. Physiol. B 125,219 -226.[CrossRef][Medline]
Beyenbach, K. W. and Kirschner, L. B. (1976).
The unreliability of mammalian glomerular markers in teleostean renal studies.
J. Exp. Biol. 64,369
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Boutilier, R. G. (2001). Mechanisms of cell survival in hypoxia and hypothermia. J. Exp. Biol. 204,3171 -3181.[Medline]
Boutilier, R. G. and St-Pierre, J. (2000). Surviving hypoxia without really dying. Comp. Biochem. Physiol. A 126,481 -490.[CrossRef][Medline]
Curtis, B. J. and Wood, C. M. (1991). The
function of the urinary bladder in vivo in the freshwater rainbow
trout. J. Exp. Biol.
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