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First published online June 15, 2007
Journal of Experimental Biology 210, 2311-2319 (2007)
Published by The Company of Biologists 2007
doi: 10.1242/jeb.02778
Effect of aerial O2 partial pressure on bimodal gas exchange and air-breathing behaviour in Trichogaster leeri
1 Environmental Biology, School of Earth and Environmental Sciences,
University of Adelaide, Adelaide, South Australia, 5005, Australia
2 School of Biosciences, University of Birmingham, Edgbaston, Birmingham,
B15 2TT, UK
* Author for correspondence (e-mail: lesley.alton{at}alumni.adelaide.edu.au)
Accepted 15 March 2007
| Summary |
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O2), increasing
mean O2 uptake per breath
(
O2/breath) and
decreasing aquatic
O2 to maintain a
constant total
O2. The rate of
oxygen uptake from the air-breathing organ (ABO) during apnoea
(
O2,ap) was
derived on a breath-by-breath basis from
VO2/breath and apnoea duration.
O2,ap and
estimates of ABO volume were used to calculate the
PO2 in the ABO at the end of apnoea. This
increased with increasing PO2,air, suggesting
that ABO-PO2 is not regulated at a constant
level by internal chemoreceptors. Furthermore, mean
O2,ap increased
with increasing PO2,air, indicating that the
observed increase in
O2/breath with
increasing PO2,air was facilitated not only by
an increase in apnoea duration but also by an increase in the airblood
PO2 gradient.
Key words: fish, respiration, air-breathing, bimodal gas exchange, aerial O2, air-breathing organ, O2 chemoreceptor
| Introduction |
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|
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Since there is evidence to suggest that chemoreceptors are located at the
site of aquatic respiration in air-breathing fish, it is reasonable to
contemplate the existence of chemoreceptors at the site of aerial respiration,
i.e. within the air-breathing organ (ABO). A common method used to identify
sites of chemoreceptors in conscious air-breathing fish is to observe
behavioural responses to independent changes in aquatic and aerial gas
contents (e.g. Burggren, 1979
;
Graham et al., 1995
;
Hedrick and Jones, 1993
;
Hughes and Singh, 1970
;
Johansen and Lenfant, 1968
;
Sanchez et al., 2001
). Studies
involving manipulations of aquatic O2 content by far exceed studies
involving manipulations of aerial O2 content. However, experimental
manipulations of aerial O2 content have the potential to offer
insight into the presence and role of ABO-O2 chemoreceptors.
Air-breathing fish generally respond to aerial hypoxia by reducing apnoea
(i.e. breath-hold) duration, whereas hyperoxia often lengthens it
(Shelton et al., 1986
).
However, conclusions arising from experiments involving aerial O2
manipulations are limited in that the activity of chemoreceptors within the
ABO cannot be discriminated from those located remotely, in the efferent
vasculature (Graham, 1997
).
Simulated breathing by injection of either hypoxic or hyperoxic gas into the
ABO produces the same results as changes in aerial gas composition (e.g.
Johansen and Lenfant, 1968
).
However, gas injection also increases the volume of the ABO, and such
experiments may therefore be confounded by activation of ABO mechanoreceptors
that transmit information about the rate or extent of organ wall deformation
(Milsom, 1990
;
Pack et al., 1990
).
Evidence for ABO-O2 chemoreceptors was found for the swamp eel,
Monopterus albus, by Graham et al.
(Graham et al., 1995
). M.
albus was observed to expel severely hypoxic or anoxic breaths within a
few seconds of inspiration. The rapidity of the gas-voiding reflex suggested
the presence of an ABO chemoreceptor, because it occurred about two to four
times faster than would be expected if O2 levels in the ABO had to
be conveyed by blood flow to remote vascular receptors located somewhere in
the systemic circulation. By contrast, the response of the blue gourami,
Trichogaster trichopterus, to changes in aerial
PO2 was not immediate, suggesting that
chemoreceptors were more centrally located
(Burggren, 1979
).
The present study investigates the effect of aerial O2 partial
pressure (PO2,air) on bimodal gas exchange and
air-breathing behaviour in an air-breathing fish, the pearl gourami,
Trichogaster leeri Bleeker 1852 (sub-order Anabantoidei, family
Belontiidae). T. leeri is a freshwater pelagic fish that has a pair
of suprabranchial chambers serving as its ABO
(Peters, 1978
). Changes in
air-breathing frequency (fab), aerial and aquatic
O2 consumption rate
(
O2) and mean
O2 uptake per breath (VO2/breath)
are analysed. Using a novel approach, apnoeic
O2
(
O2,ap=rate of
O2 uptake from the air within the ABO while the fish is submerged)
is derived by a breath-by-breath assessment of O2 uptake and apnoea
duration.
O2,ap
is used to address two questions: (1) is the response of T. leeri to
changes in PO2,air regulated by
ABO-O2 chemoreceptors and (2) is a change in mean
VO2/breath with changing
PO2,air facilitated by a change in the
airblood PO2 gradient as well as a
change in apnoea duration?
To address the first question,
O2,ap and
estimated measurements of ABO volume (VABO) are used to
calculate the PO2 in the ABO at the end of
apnoea. It is hypothesised that if the PO2 in
the ABO is regulated by ABO-O2 chemoreceptors, then the
PO2 in the ABO at the end of apnoea should not
be significantly different across treatments of varying
PO2,air. This would suggest the existence of an
ABO-PO2 threshold, which, once reached,
triggers fish to renew the gas in their ABO.
The second question arises because O2 uptake during apnoea may
change simply as a result of changes in apnoea duration, i.e.
VO2/breath may increase during aerial hyperoxia
because T. leeri holds its breath for longer. However, a change in
the airblood PO2 gradient may also
facilitate O2 uptake during apnoea. Thus, it is hypothesised that
if a change in apnoea duration is solely responsible for a change in mean
VO2/breath then
PO2,air will not have an effect on mean
O2,ap. This is
because mean
O2,ap accounts
for variations in apnoea duration between treatments, and thus if mean
O2,ap changes
with changing PO2,air then a change in the
airblood PO2 gradient must also be
responsible. To our knowledge, this is the first study to examine how changes
in the airblood PO2 gradient associated
with aerial hypoxia and hyperoxia influence O2 consumption in an
air-breathing fish.
| Materials and methods |
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Aerial respirometry
Prior to experimentation, food was withheld for 24 h and fish were
individually placed in 1 litre bottles (Schott Duran, Germany) that were
covered in black plastic to minimise stress. Bottles containing fish were held
in a constant-temperature water bath maintained at 25±1°C by a
heater (Thermomix 1419; B. Braun, Melsungen, Germany). Fish were allowed 12 h
to acclimate to the chambers and to recover from handling prior to each
experiment. An air stone gently aerated the water during the acclimation
period.
Respiratory studies were conducted with an open-flow respirometer system.
O2 and N2 were supplied from compressed cylinders (BOC
Gases, Adelaide, Australia) and delivered to the respirometry chamber at a
desired O2 content (FIO2)
and flow rate (
I; 100, 150
or 200 ml min-1). The flow rate for each trial was selected to
minimise the washout time while providing reliably detectable changes in the
excurrent O2 content
(FEO2). O2 content and
flow rate were controlled by mass flow controllers (model GFC171; Aalborg
Instruments and Controls, New York, NY, USA; 01 l min-1,
rated accuracy ±15 ml min-1) using a PC running
digitalanalogue control software and hardware (PowerDAQTM PD2-AO
and ProfessorDAQTM; United Electronic Industries, Canton, MA, USA). Flow
controllers were calibrated to each gas with a 3.5 litre calibrator (model
1057A Vol-U-Meter Calibrator; Brooks Instruments, Hatfield, PA, USA; accuracy
of calibrated controllers was better than 5% of reading, usually 12% of
reading). To ensure uniform mixing of O2 and N2, these
gases were passed through a 1 litre, rigid mixing chamber before entering the
respirometer. Nevertheless, the O2 level was not as constant as
expected in normal open-flow respirometry with atmospheric air, so the
variability had to be accounted for in the analysis (see below).
Upon exiting the respirometry chamber, gases passed through a U-tube containing DrieriteTM (Hammond Drierite Co. Ltd, Xenia, OH, USA) to remove water vapour and into a differential O2 analyser (FC-2 Oxzilla I; Sable Systems International, Las Vegas, NV, USA). The analyser was calibrated using dried (DrieriteTM), CO2-free (AscariteTM; Arthur H. Thomas Company, Swedesboro, NJ, USA) atmospheric air (0.2095 O2). The analyser measured FEO2 approximately every 1.25 s and used a running five-sample average for each data point. The data output from the O2 analyser was received simultaneously in an analogue and digital format. The analogue output was recorded at 2 s intervals with a digital multimeter (model TX3 True RMS and WaveStarTM Version 2.2; Tektronix, Beaverton, OR, USA) interfaced with a PC via the RS232 port. Depending on the analogue output scaling chosen, these voltage values were converted to FEO2 using relationships provided by Sable Systems International. The Oxzilla digital output was received by a DOS terminal program (SERIN; Sable Systems International) and recorded at intervals of approximately 1.1 s on a second PC. For analyses, WaveStar data were preferred due to SERIN's unstable timing interval, but SERIN data were used in two cases where high-frequency noise in the analogue data signal prevented reliable detection of breaths.
Experimental protocol
Aerial PO2
(PO2,air) in the respirometry chamber was
manipulated to nominal levels of 5, 10, 21 (control), 40 or 60 kPa (actual
PO2,air range: 5.45.5, 9.610.1,
19.920.7, 38.439.0 and 57.557.9 kPa, respectively).
Treatments were executed in random order and an arbitrary exposure time of 1 h
was set so as to reduce the effect of declining aquatic
PO2. However, due to the instability of
FEO2, some fish were exposed for
longer than 1 h (maximum exposure time was 3 h), in order to accumulate 1 h
worth of interpretable data. During trials, aquatic
PO2 dropped 2.3, 1.8, 1.5, 1.2 and 0.6 kPa
h-1 in the 5, 10, 21, 40 and 60 kPa treatments, respectively. To
determine whether declining aquatic PO2 had an
effect on aerial respiration, fab, aerial
O2 and
O2/breath in the
first and final 15 min of each trial were compared. In each case, there was no
significant difference between the first and final 15 min (P=0.22,
0.94 and 0.56, respectively). Following exposure to each treatment, fish were
given at least 24 h rest before the next treatment. During this time, either
the water in the chamber was aerated with an air stone or the fish were
returned to their aquarium.
|
O2; ml
h-1) was by integration of
FEO2 inverted spikes. Each spike
represented one exhalation, confirmed by visual observation. The duration of
the spike depended on the washout characteristics of the respirometry system.
Because these occurred on an unstable baseline
(Fig. 1), a spreadsheet method
was devised to isolate the spikes from the baseline. To select data
representing periods of apnoea, a coefficient of variation (CV=s.d./mean) was
calculated for 15 consecutive measurements, and a CV threshold value (e.g.
3.3x105) was manually set at a level that separated
high-frequency, low-amplitude FEO2
baseline noise from air-breathing events that were low frequency, high
amplitude (Fig. 1B). Values
below this threshold were considered to be baseline values, and, for every
value above the threshold, a new baseline was linearly interpolated between
previous and subsequent sub-threshold values. Where breaths were too frequent
for the program to isolate values representing baseline
FEO2, a polynomial regression was
fitted to the baseline trace and entered in place of the CV threshold
criteria. The final baseline was then produced by completing two rounds of
9-point nearest-neighbour averaging to remove high-frequency noise
(Keller et al., 1994
O2 was then
calculated for each data point (Fig.
1C) from the air flow rate through the chamber
(
I; ml min-1)
and the respiratory quotient (RQ) according to Depocas and Hart
(Depocas and Hart, 1957
![]() | (1) |
Each breath was integrated individually to arrive at a breath-by-breath
estimate of O2 uptake from the ABO during the apnoeic period
(VO2/breath; ml). This was summed across the
trial and divided by trial duration to calculate aerial
O2.
Additionally, this approach measured fab (breaths
h-1) by tallying the number of breaths during a trial and dividing
by trial duration.
Aquatic respirometry
To evaluate the partitioning of aerial and aquatic respiration, aquatic
O2 consumption (aquatic
O2; ml
h-1) was measured. For technical reasons, this was measured
separately from aerial respirometry studies. Prior to experimentation, fish
were treated in the same manner as they were for aerial respirometry. The
aerial gas mix was produced as previously described but was vented to the
atmosphere rather than fed through the O2 analyser. A fibre-optic
O2 sensor (Implantable Oxygen Microoptode; Presens, Regensburg,
Germany) encased within a Pasteur pipette was mounted through the respirometer
lid to measure aquatic O2 content (% air-saturation). The
O2 sensor was connected to a single-channel,
temperature-compensated O2 meter and software (Microx TX3, OxyView
TX3-V5.20; Presens) that recorded at 1 min intervals. A trial without a fish
(control) was conducted for each PO2,air
treatment to account for aquatic O2 depletion not related to fish
respiration. A linear regression was fitted to the data of O2
content (% air-saturation) on time, and aquatic
O2 was
calculated using the equation:
![]() | (2) |
Apnoeic
O2 calculation
To calculate oxygen uptake from the ABO during apnoea
(
O2,ap;ml
h-1), VO2/breath (ml) was plotted
against the apnoea duration (h) for each breath of each fish under each
treatment (e.g. Fig. 2). A
linear regression was fitted to the data, with the derived slope of the
regression representing
O2,ap (ml
h-1) (e.g. Fig.
2).
|
![]() | (3) |
26°C after an apnoea duration of approximately 120 s
[VABO(120)].
Schuster stated that if one measurement of VABO is
known, the VABO at any instant time during apnoea
(t; s) at 25°C is given by:
![]() | (4) |
VABO(t0) and the
PO2 in the ABO at the beginning of apnoea (i.e.
initial PO2) are needed to calculate the
initial volume of O2
[VO2(t0); ml] in the ABO
(Eqn 5). The initial
PO2 was assumed to be equivalent to
PO2,air. This is reasonable because during
expiration practically all of the gas in the ABO is displaced out of the mouth
with water from the opercular cavity
(Peters, 1978
):
![]() | (5) |
The volume of O2 consumed during apnoea is calculated using
O2,ap (ml
h-1) and mean apnoea duration (tap, h) for each
fish under each treatment, and this is subtracted from
O2(t0)
to arrive at the volume of O2 in the ABO at the end of apnoea
(VO2,end; ml):
![]() | (6) |
O2,ap is halved
because it represents the rate of O2 uptake across the surface area
of the entire ABO (i.e. both suprabranchial chambers) and
VO2,end is calculated for a single
suprabranchial chamber.
Although Schuster found that the ABO of C. lalia decreased in
volume as O2 was consumed
(Schuster, 1989
), the ABO of
T. leeri is a bony structure
(Graham, 1997
;
Peters, 1978
) (L.A.A.,
personal observation) and the rate of change in VABO with
declining ABO-O2 may be different from that in C. lalia,
or may not occur at all. Therefore, end-apnoea
ABO-PO2 was calculated with two assumptions
that bracket reality (note that the following calculations make the
simplifying assumption that CO2 is not present within the ABO): (1)
VABO remained constant as O2 was consumed
(Eqn 7) and (2)
VABO decreased as if the ABO was totally compliant [i.e.
VO2,end (ml) is subtracted from
VABO(t0) (litres);
Eqn 8]:
![]() | (7) |
![]() | (8) |
End-apnoea ABO-PO2 assuming both a constant and totally compliant ABO volume was determined for each fish and compared between treatments.
Airblood PO2 gradient
To ascertain whether a change in apnoea duration is solely responsible for
a change in mean VO2/breath with changing
PO2,air, or whether a change in the
airblood PO2 gradient is also a
contributing factor, mean
O2,ap was
calculated for each treatment and plotted against
PO2,air.
Statistical analysis
Where appropriate, mass-specific values were used to account for the
variation attributed to mass differences between fish
(McNab, 1999
). Although this
procedure does not completely remove mass effects
(Packard and Boardman, 1999
)
because
O2
scales allometrically in fish (White et
al., 2006
), the body size range was too small to determine the
intraspecific allometric exponent for T. leeri accurately and arrive
at mass-independent values.
A repeated-measures analysis of variance (ANOVA) was performed in JMP
Version 5.1 (SAS Institute, Cory, NC, USA) to determine the effect of
PO2,air on all variables. To fulfil assumptions
of normality and homogeneity of variance,
PO2,air was log transformed for the analysis of
fab, which was not transformed; aerial
O2, aquatic
O2,
O2/breath,
end-apnoea ABO-PO2 (assuming constant ABO
volume) and end-apnoea ABO-PO2 (assuming a
totally compliant ABO) were log transformed together with
PO2,air; and
O2,ap and total
O2 were log
transformed without PO2,air being transformed.
A Tukey's HSD test was used in post-hoc analyses where
repeated-measures ANOVA revealed significant treatment effects. Statistical
significance for all tests was determined with
=0.05.
| Results |
|---|
|
|
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O2
(F1,23=37.2, P<0.0001), with aerial
O2 increasing
from 20.1 ml kg-1 h-1 at 5 kPa to 60.8 ml
kg-1 h-1 at 60 kPa
(Fig. 3B). Complementary to
this, there was a significant positive effect of
PO2,air on
VO2/breath (F1,23=221.5,
P<0.0001), with VO2/breath
increasing from 0.5 ml kg-1 at 5 kPa to 5.5 ml kg-1 at
60 kPa (Fig. 3C).
|
Aquatic and total respiration
There was a significant negative effect of
PO2,air on aquatic
O2
(F1,27=17.8, P=0.0003), with a significant
increase in aquatic
O2 under the 5
kPa treatment (Fig. 3B). There
was no significant effect of PO2,air on total
O2
(F1,23=2.49, P=0.13)
(Fig. 3B).
|
Airblood PO2 gradient
A repeated-measures ANOVA revealed a significant positive correlation
between mean
O2,ap and
PO2,air (F1,21=34.7,
P<0.0001), with mean
O2,ap increasing
from 13.2 ml kg-1 h-1 at 5 kPa to 59.8 ml
kg-1 h-1 at 60 kPa. The relationship between mean
O2,ap and
PO2,air was described by the logarithmic curve:
O2,ap=45.8log(PO2,air)19.2
(r2 =0.63) (Fig.
5).
|
| Discussion |
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|
|
|---|
O2 of
T. leeri was 108.2 ml kg-1 h-1. This value is
lower than that found for the closely related T. trichopterus (156.2
ml kg-1 h-1)
(Burggren and Haswell, 1979
O2 and body
mass, the data obtained here for T. leeri are well within the 95%
prediction intervals (31.8290 ml kg-1 h-1) for
new data (White et al., 2006
Aerial hypoxia
The breathing frequency (fab) of T. leeri
under normoxic conditions was 21.8±5.9 breaths h-1 (mean
± s.d.), which is greater than that observed for T.
trichopterus (12.8± 4.1 breaths h-1)
(Burggren, 1979
). However, like
T. trichopterus, fab of T. leeri increased as the
gas phase became increasingly hypoxic (Fig.
3A). At a PO2,air of 5 kPa,
fab was twofold higher than control (normoxic) levels,
whereas T. trichopterus increased fab almost
threefold. However, fab calculated for T. leeri
at 5 kPa may be an underestimate, because only three fish yielded results
where some individual breaths could be isolated. For the remaining fish, no or
few breathing events were apparent. This suggests that the airblood
PO2 gradient was insufficient to promote
O2 uptake. The airblood PO2
gradient may have in fact been reversed, resulting in fish losing
O2 gained from the water to the air. This futile behaviour would be
expected, however, because severe aerial hypoxia is not encountered in the
natural environment, and fish are unlikely to have evolved an appropriate
response to such conditions.
An increase in fab in response to aerial hypoxia has
been observed in species that have a reduced gill surface area and are
therefore heavily reliant on aerial respiration. For example, M.
albus showed a significant reduction in apnoea duration when inspiring
gas mixtures containing 16 kPa O2 or less, and breaths containing
1.5 kPa O2 were exhaled almost immediately
(Graham et al., 1995
).
Monopterus cuchia increased tidal volume as well as
fab during hypoxic breathing
(Lomholt and Johansen, 1974
),
but no such change in ABO tidal volume occurred in T. trichopterus
(Burggren, 1979
).
Protopterus aethiopicus increased fab when
N2 gas was injected into the ABO, and, interestingly, air breathing
was stimulated by N2 injection even when arterial
PO2 was higher than that towards the end of a
normal apnoea period (Johansen and
Lenfant, 1968
). Amia calva, a fish less reliant on aerial
respiration, increased fab twofold when air containing
only 8 kPa O2 was inspired
(Hedrick and Jones, 1993
). In
contrast to Amia, other fish with efficient aquatic gas exchange do
not show a change in fab when N2 gas is
injected into the lung (Neoceratodus forsteri)
(Johansen et al., 1967
) or air
bladder (Lepisosteus oculatus)
(Smatresk and Cameron, 1982b
).
The first and second gill arches of T. leeri are large and fully
developed (Munshi, 1968
), and
T. leeri is sensitive to aquatic hypoxia
(Miller, 2003
), unlike
Protopterus (Johansen and
Lenfant, 1968
) and Monopterus
(Lomholt and Johansen, 1974
).
It therefore seems likely that, although T. leeri is not as reliant
on aerial respiration as these species, aquatic respiration may not be
sufficient to meet its metabolic demands, making it an obligate air breather
(Graham, 1997
). T.
trichopterus is considered an obligate air breather at temperatures above
2025°C, as it shows signs of distress if denied access to air
(Burggren, 1979
).
Despite an increase in fab during aerial hypoxic
exposure, T. leeri was unable to sustain aerial
O2 equal to that
under normoxic conditions (Fig.
3B). Complementary to the observed decrease in aerial
O2 with
decreasing PO2,air,
VO2/breath also showed a decline
(Fig. 3C).
The contribution of aerial
O2 to total
O2 decreased
from 33% in normoxia to 25% when PO2,air was 10
kPa, and to 16% at 5 kPa. Similarly, under normoxic conditions at 27°C,
the ABO of T. trichopterus accounted for 42% of the total
O2 and less than
15% when PO2,air was reduced to 7.2 kPa
(Burggren, 1979
). Both species
showed an increase in aquatic
O2 to compensate
for their reduced ability to extract O2 from the air
(Fig. 3B). It is reasonable to
assume that this increase in aquatic
O2 arises almost
entirely from gas exchange via the gills, because cutaneous gas
exchange in air-exposed T. trichopterus accounts for only
10% of
the total gas exchange (Burggren and
Haswell, 1979
). Aquatic
O2 may be
increased via an increase in branchial ventilation frequency,
branchial tidal volume or both. Branchial ventilation is known to increase
initially in most air-breathing fish as aquatic
PO2 falls
(Hughes and Singh, 1971
;
Johansen et al., 1970
;
Pettit and Beitinger, 1985
;
Smatresk and Cameron, 1982a
),
but the effect of aerial hypoxia on branchial ventilation appears not to have
been investigated.
Aerial hyperoxia
At a PO2,air of 60 kPa,
fab significantly decreased in T. leeri
(Fig. 3A). Similarly, T.
trichopterus decreased fab when
PO2,air was increased to 80 kPa
(Burggren, 1979
). A decrease in
fab has been observed in almost all species exposed to
aerial hyperoxia: P. ethiopicus
(Lahiri et al., 1970
), L.
oculatus (Smatresk and Cameron,
1982b
), Electrophorus electricus
(Johansen et al., 1968b
) and
M. albus (Graham et al.,
1995
).
Despite a decrease in fab in hyperoxic air,
O2,ap increased
by almost twofold when PO2,air was 40 kPa;
however, no significant increase occurred when
PO2,air was increased to 60 kPa
(Fig. 3B).
Although aerial
O2 increased
significantly in aerial hyperoxia compared with normoxia, there was no
corresponding decrease in aquatic
O2, and total
O2 was unchanged
(Fig. 3B). However, because
aerial and aquatic respiration were measured separately, inherent variability
may have obscured the expected correlations.
ABO-O2 chemoreceptors
The responsiveness of T. leeri to changes in aerial O2
content lends insight to the question of the existence of ABO-O2
chemoreceptors. Graham et al. give support for the existence of
ABO-O2 chemoreceptors in some air-breathing species
(Graham et al., 1995
). They
found that the rapidity of the gas-voiding reflex of M. albus to
changed aerial O2 content was indicative of ABO-O2
chemoreceptors, not chemoreceptors in the systemic circulation. They suggested
that an ABO-O2 chemoreceptor would be advantageous in the
regulation of cardiac responses to an air-breathing event. A common pattern of
cardiac arrhythmia found in fishes during an air-breathing event is
inspiration-induced tachycardia followed by the gradual onset of bradycardia
as the ABO-O2 content falls, leading to pronounced bradycardia with
exhalation (Farrell, 1978
;
Johansen et al., 1968a
;
Singh and Hughes, 1973
;
Smatresk, 1988
;
Smatresk, 1990
). Therefore, an
ABO-O2 chemoreceptor may be important in the modulation of
mechanoreceptor and other stimuli affecting air-breathing tachycardia, in
attenuating tachycardia as ABO-O2 declines and in terminating the
breath when ABO-PO2 becomes too low to promote
O2 uptake (Graham and Baird,
1984
). This would result in the effective matching of ventilation
and perfusion (Johansen, 1966
;
Johansen, 1970
).
However, the findings of Graham et al.
(Graham et al., 1995
) contrast
with Burggren's indication of more centrally located chemoreceptors (i.e. in
the brain) in T. trichopterus, which was based on the lag in
ventilation response time (several seconds) to stepwise changes in aerial
O2 content (Burggren,
1979
). Burggren argued that because aerial hypoxia is rarely, if
ever, encountered in the natural environment, selection pressures should not
be strong for the evolution of a peripheral chemoreceptor control system able
to differentiate between reduced systemic blood O2 resulting from
gill ventilation with hypoxic water and that resulting from ABO ventilation
with hypoxic gas.
More substantial evidence for ABO-O2 chemoreceptors in T.
leeri would have been an end-apnoea
ABO-PO2 that was independent of
PO2,air. This would have suggested the
existence of an ABO-PO2 threshold that, once
reached, triggered T. leeri to renew the gas in its ABO. However,
this was not the case in this study; end-apnoea
PO2 increased with increasing
PO2,air
(Fig. 4). This lack of
correlation between ABO-PO2 and renewal of ABO
gas has also been recognised in lungfish
(Johansen and Lenfant, 1968
)
and in Pacific tarpon that uses the swimbladder as an ABO
(Seymour et al., 2007
). It has
also been shown that apnoea termination occurs at high
ABO-PO2 levels when the rate of decline in
ABO-PO2 is rapid
(Shelton et al., 1986
). This
corresponds with the findings in this study; mean apnoeic
O2
(
O2,ap)
increased under hyperoxic conditions and end-apnoea
ABO-PO2 was higher than that under normoxic
conditions. These findings indicate that if ABO-O2 chemoreceptors
are present, then their regulation of bimodal control in air-breathing fish is
partial, and that respiration is mainly affected by chemoreceptors elsewhere
in the central and peripheral nervous system and possibly by mechanoreceptors
in the ABO.
Airblood PO2 gradient
Mean
O2,ap
increased with increasing PO2,air
(Fig. 5), supporting the
hypothesis that the observed increase in
VO2/breath with increasing
PO2,air
(Fig. 3C) was facilitated not
only by an increase in apnoea duration but also by an increase in the
airblood PO2 gradient. The logarithmic
function between
O2,ap and
PO2,air suggests that when there is no
O2 uptake occurring in the ABO (i.e.
O2,ap is equal
to zero), PO2,air is equal to 2.62 kPa.
Therefore, the air and blood are in equilibrium and the efferent blood from
the gills can be assumed to have a PO2
approximating this value. The relationship also indicates that in hyperoxia
O2,ap reaches a
maximum where it becomes independent of PO2,air
(Fig. 5). Because the
haemoglobin would be expected to be completely saturated in the hyperoxic ABO
(Herbert and Wells, 2001
),
aerial
O2
plateaus because the blood reaches a point where it can take up no more than
can be dissolved in the plasma.
List of symbols and abbreviations
I
O2
O2,ap
O2
| Acknowledgments |
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