|
|
||||||||
1 Department of Zoology, CB2 3EJ Cambridge; and 2 Sea Mammal Research Unit, Gatty Marine Laboratory, University of St. Andrews, KY16 8LB Fife, United Kingdom
| |
ABSTRACT |
|---|
|
|
|---|
Breath-by-breath measurements of
end-tidal O2 and CO2 concentrations in harbor
porpoise reveal that the respiratory gas exchange ratio
(RR; CO2 output/O2 uptake) of the
first lung ventilation in a breathing bout after a prolonged
breath-hold is always well below the animal's metabolic respiratory
quotient (RQ) of 0.85. Thus the longest apneic pauses are
always followed by an initial breath having a very low RR
(0.6-0.7), which thereafter increases with each subsequent breath
to values in excess of 1.2. Although the O2 stores of the
body are fully readjusted after the first three to four breaths
following a prolonged apneic pause, a further three to four
ventilations are always needed, not to load more O2 but to
eliminate built-up levels of CO2. The slower readjustment of CO2 stores relates to their greater magnitude and to the
fact that they must be mobilized from comparatively large and
chemically complex HCO
respiratory quotient; respiratory gas exchange ratio; O2 and CO2 stores
| |
INTRODUCTION |
|---|
|
|
|---|
CETACEANS ARE EXCLUSIVELY aquatic mammals that range in size from the smallest porpoises (70-100 kg) to the largest animal on the planet, the 150-ton blue whale. They spend the vast majority of their life underwater and surface only periodically to ventilate their lungs with a single breath. The largest whales, with their unusually large blood volumes and high Hb and myoglobin concentrations, can take aboard enough oxygen at the surface to sustain their low mass-specific metabolic rates for dives lasting >1 h (6, 7, 14). Because harbor porpoises represent the lower extreme of cetacean body size, they are of intrinsic interest to respiratory physiologists because they are presumed to have the highest mass-specific metabolic rates and to enjoy the most active lifestyle of all whales.
We had a unique opportunity to study the respiratory physiology of captive harbor porpoises in a strandings rehabilitation facility for marine mammals in Harderwijk, Netherlands. Our experiments on juvenile harbor porpoises confirm that they have the highest oxygen consumption per kilogram body weight and the highest heart rates of all cetaceans studied thus far (13). Whereas their diving O2 stores in blood, lung, and muscle are slightly greater than one would predict for a terrestrial mammal of comparable size, their high mass-specific metabolic rate dictates a lifestyle that restricts aerobic underwater activities to 3-4 min [their so-called aerobic dive limit (ADL)] (10, 13) before having to surface to breath. This offers them little scope to achieve great diving depths and almost certainly limits their foraging activities to shallower environments than the larger whales. Indeed, recent field studies of free-ranging juvenile harbor porpoises instrumented with time-depth recorders bear out our measurements of a 3- to 4-min ADL (13) as maximum depths and dive durations were on the order of 150 m and 3.5-4.7 min (8, 15). After such dives, harbor porpoises normally visit the surface for up to 6 "rolls" spaced ~10 s apart (15). Each roll coincides with a lung ventilation, or blow, lasting <1 s (13) during which time all gas exchange must occur. Our survey of cetacean ventilatory dynamics (13) indicates that rapid, high-flow velocity breathing is a characteristic feature of all whales, enabling them to exchange large percentages of their total lung gas during the brief periods when they "porpoise" through the air-water interface.
Current concepts of diving in marine mammals focus on oxygen as a "resource" that must be periodically recharged at the expense of loss of time underwater. As such, the time taken to "gather" the resource at the surface is viewed as an inescapable "cost" of the diving habit. We present data showing that the O2 store of the porpoise is fully readjusted after the first three to four breaths after a prolonged apneic pause. However, a further two to three ventilations are needed, not to load more O2 but to eliminate built-up levels of CO2. Although the slower readjustment of CO2 stores is a predictable feature of unsteady-state gas exchange, its potential importance as the proximate signal that brings the surface period to an end has been largely ignored.
| |
MATERIALS AND METHODS |
|---|
|
|
|---|
Two juvenile harbor porpoises (28.3 and 27.8 kg) were trained in a small tank to breathe freely into a facemask that was positioned over the blowhole each time the animal surfaced to ventilate its lungs. Over a 3-wk training period, the animals were lifted each day from the holding tank (an oval pool 8 × 6-m diameter, 1.5-m deep) to the experimental tank (2 × 0.8 × 0.8-m). During each experimental session, the animal was allowed to breathe freely through a Hall's facemask (VetDrug, Bury St. Edmunds, UK), and breath-by-breath O2 ([O2]) and CO2 concentrations ([CO2]) were recorded. The facemask was a wide rubber funnel with flexible rims (so that it fit easily over the blowhole without allowing any air to escape), and both the mask and the flow meter had minimal resistance to the porpoise's respiratory flows, being essentially open tubes. The inspiratory and expiratory flows were measured using an ultrasonic low-resistance flow meter (BRDL, Birmingham Univ.; 20-l/s version; see Ref. 12) mounted on the top of the mask so that the porpoise could breathe freely through the flow meter. Respiratory gases were measured by drawing a continuous subsample of the animal's expiratory and inspiratory flows at a constant flow rate (600 ml/min) through capillary tubing from the center of the respiratory gas flow, passing through a Ministart drying filter (deadspace 0.1 ml, Sartorius) to Servomex gas analyzers (model 1505 miniature infrared CO2 and 728 zirconia O2; Servomex). O2 and CO2 measures were output as percent end-tidal (minimum) O2 and percent end-tidal (maximum) CO2 and converted to partial pressures (assuming partial pressure of water in air at 37°C is 6.26 kPa). The response time of the oxygen analyzer (installed in the system) was ~500-600 ms, whereas that for CO2 was ~300-400 ms. The maximum possible sample gas flow rates were used to minimize the delay of the system, and the gas analyzers were positioned on a wheeled platform next to the experimental container to minimize the delay between sampling and analysis. The O2 and CO2 gas sensors were calibrated using precision gas mixtures (pure N2; 12% O2 and 4% CO2 in N2; 10% CO2 in N2; supplied and certified to 0.01% by Hoekloos Gases, Amsterdam, Netherlands). Data were sampled and stored by a 386 Dell PC with "ANALYSE" software specifically developed for this work. For further details of the respirometry system, instrument response times, calibration, and system operation, see Reed et al. (12).
| |
RESULTS AND DISCUSSION |
|---|
|
|
|---|
Breathing episodes after the longest breath-holds in the present
study were normally grouped into distinct bouts of six to eight lung
ventilations, with short interbreath intervals (Fig. 1). Breath-by-breath measurements of
end-tidal [O2] and [CO2] in porpoise
revealed that the respiratory gas exchange ratio (RR; the
ratio of CO2 output and O2 uptake) of the first
lung ventilation in a breathing bout after a prolonged breath-hold was
always well below the animal's time-averaged metabolic respiratory
quotient (RM) of 0.85 (13). Thus the longest
apneic pauses were always followed by an initial breath having a very
low RR (0.6-0.7), which thereafter increased with each
subsequent breath to values in excess of 1.2 (Fig.
2). It is evident from these data that over the course of the breathing bout, the CO2 stores
readjust relatively slowly compared with oxygen.
|
|
The effects of differential rates of store adjustment on the
RR can be conveniently illustrated on the
O2-CO2 diagram (5). The gas
exchange ratio of the stores is indicated by a fan of lines radiating
from the inspired gas composition (Fig.
3). Although diving physiologists have
normally assumed the postdive ventilation of marine mammals to be
concerned primarily with the recharging of O2 stores, our
data for harbor porpoises show that when the O2 stores have
attained near-equilibrium values (Hb-O2 saturation, >95%), the CO2 stores are still readjusting (Figs. 1 and
3). Indeed, this is to be expected if one considers that the majority
of the CO2 eliminated during breathing must be mobilized
from large and chemically complex
HCO
-CO2 =
[CO2]/
PCO2) for body
tissues is much higher than the corresponding O2
capacitance (
-O2 =
[O2]/
PO2), because
-CO2 is determined by both the physical solubility
(
-CO2), which is ~25 times higher than for
O2, and the chemical binding of CO2 as
bicarbonate; i.e.,
-CO2 =
-CO2 + (
[HCO
PCO2),
where changes in bicarbonate concentration are stoichiometric with the
amount of proton buffering (9). Thus, whereas the major
tissue O2 stores are confined to muscle, any tissues with
chemical groups that act as H+ acceptors can act as
potential CO2 stores. The high capacitance for
CO2 compared with O2 means that for a given
change in the stores (e.g., if RM = 1), the corresponding
change in PCO2 will be much smaller than that
for PO2. This is why increases of arterial blood PCO2 of only 10 mmHg are seen during
20-min voluntary dives of Weddell seals, when corresponding
oscillations in arterial PO2 reach upwards of
60 mmHg (11), and why lung RR < RM in the initial stages of the postapneic breathing bout
(Figs. 1, 2, and 4).
|
|
For comparative purposes, mean lung R values during postapneic breathing bouts were computed from breath-by-breath measurements of end-tidal PO2 and PCO2 in the porpoise (see Fig. 1) and the gray seal (12). When seals surface to breathe after a dive, they normally remain at the surface with their nares exposed to air for a series of lung ventilations. Our analysis shows that the RR values in the early stages of a postdive breathing bout are much lower than in the later stages of the bout, when RR values increase in both animals to levels far in excess of the metabolic RQ (Figs. 1 and 4). The only significant difference between the postapneic development of an increasing RR in harbor porpoises and gray seals is that the gas composition of the first few breaths after a dive in the seal is thought to reflect that of a largely underperfused lung during the breath-hold (12). As the circulation to the periphery of the seal is reestablished, the peak end-tidal PCO2 values increase far less than the corresponding fall in PO2, leading to an overall decrease in RR and to the curvilinear relationship for RR shown in Fig. 4. The fact that we do not see such curvilinear relationships in the harbor porpoise (Fig. 1) is further support of our contention that the lung is probably used as an O2 store throughout the breath-hold and that peripheral vasoconstriction is only slow to develop (13).
One may well ask whether the time a marine mammal spends at the surface after a dive always exceeds the time taken to recharge the O2 stores. For example, in Weddell seals diving voluntarily for up to 57 min, the mean time on surfacing to reach an expired PO2 of 60 mmHg (90% Hb-O2 saturation) was 0.56 min, whereas mean surface time was upwards of 3 min (10). In the case of the harbor porpoise, which surfaces for only one breath at a time, this means that after long dives, they may be constrained to a period of porpoising behavior near the surface if they are to readjust fully their body O2 and CO2 stores. Given that it takes more time to liberate CO2 than to uptake O2, one questions whether such animals would ever forego full readjustment of their CO2 stores. By rapidly charging themselves with O2, they could cut the surface period short, still dive aerobically, "put up with" the added CO2/pH burden, and then eventually offload the built-up CO2 at some later date by spending even longer times at the surface. There could well be times when loading O2 quickly might be advantageous if, for example, being at the surface posed a threat or getting underwater quickly (e.g., for feeding) temporarily outweighed the benefits of full readjustment of body gas stores.
The overriding emphasis in current models of marine mammal diving focuses on the effectiveness of O2 store management during the dive and on the time taken to recharge the O2 store at the surface. On the other hand, factors effecting the rate-dependent steps in CO2 storage, transport, and removal have been largely ignored. Taken together, the data we present suggest that we may need to refocus our interpretation of postdive breathing behavior in marine mammals to acknowledge the possibility that it is the readjustment of the body CO2 store, not the O2 store per se, that governs the amount of time an animal must spend ventilating at the surface.
Perspectives
The extended breath-hold capacities of diving marine mammals raise the question of whether these animals possess any special mechanisms to accelerate CO2 removal to facilitate greater matching between O2 and CO2 exchange rates. Some years ago, Boutilier et al. (1) showed that the nonbicarbonate buffering capacity (
-NB) of the separated
plasma of the killer whale and gray seal was two- to fourfold higher
than in terrestrial mammals. This suggested that the increased
-NB of separated plasma could facilitate enhanced CO2 removal directly from the plasma (i.e., thereby
avoiding rate-limiting red blood cell anion exchange) as long as there
were sufficient amounts of the enzyme carbonic anhydrase in contact
with the extracellular compartment. Although the presence of carbonic
anhydrase in the pulmonary vasculature of the rat is known to enhance
CO2 excretion (3, 4), it is not considered
nearly as important as the erythrocytic enzyme, owing to the relatively
low
-NB of separated plasma. All else being the same,
the greater
-NB of separated plasma in the diving forms
(1) would not only enable greater carriage of blood total
CO2 from the site of production to the lung but, when
there, could also facilitate enhanced extracellular formation of
CO2 by providing the protons needed to drive extracellular bicarbonate dehydration. Other buffering characteristics, such as the
comparatively high buffering power seen in the muscle of marine mammals
(2), indicate to us that prolonged voluntary dives (with
large acid-base disturbances and large amounts of tissue
CO2 storage) will be important to focus on in future
studies of unsteady-state gas exchange in these animals.
| |
ACKNOWLEDGEMENTS |
|---|
We gratefully acknowledge the technical support of the staff at the Harderwijk Marine Mammal Park; in particular, C. Staal, N. Schoonman, L. de Jong, and J. Hardeman. We especially thank the director, R. Kastelein, for making this work possible, and our colleagues C. Chambers, C. J. Hunter, and C. Lockyer for assistance during all phases of the project.
| |
FOOTNOTES |
|---|
This research was funded by a grant from the Natural Environmental Research Council to R. G. Boutilier. The experiments described herein comply with the laws on animal research in the Netherlands.
Address for reprint requests and other correspondence: R. G. Boutilier, Dept. of Zoology, Downing St., Cambridge, CB2 3EJ, UK (E-mail: rgb11{at}hermes.cam.ac.uk).
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.
Received 11 May 2000; accepted in final form 20 March 2001.
| |
REFERENCES |
|---|
|
|
|---|
1.
Boutilier, RG,
Nikinmaa M,
and
Tufts BL.
Relationship between blood buffering properties, erythrocyte pH and water content, in gray seal (Halichoerus grypus).
Acta Physiol Scand
147:
241-247,
1992.
2.
Castellini, MA,
and
Somero GN.
Buffering capacity of vertebrate muscle-correlations with potentials for anaerobic function.
J Comp Physiol [A]
143:
191-198,
1981.
3.
Crandall, ED,
and
O'Brasky JE.
Direct evidence for participation of rat carbonic anhydrase in CO2 reactions.
J Clin Invest
62:
618-622,
1978.
4.
Effros, RM,
Chang RSY,
and
Silverman P.
Acceleration of plasma bicarbonate conversion to carbon dioxide by pulmonary carbonic anhydrase.
Science
199:
427-429,
1978
5.
Farhi, LE,
and
Rahn H.
Gas stores in the body and the unsteady state.
J Appl Physiol
7:
472-484,
1955
6.
Kooyman, GL.
Diverse divers: physiology and behaviour.
In: Zoophysiology. Berlin: Springer-Verlag, 1989, vol. 23, p. 200.
7.
Lockyer, C.
Diving behaviour of the sperm whale in relation to feeding. In: Sperm Whale Deaths in the North Sea, edited by Jacques TG and Lambersten RH.
Bull Inst R Sci Nat Belg Biol
67:
47-52,
1997.
8.
Otani, S,
Naito Y,
Kawamura A,
Kawasaki M,
and
Kato A.
Diving behaviour and performance of harbour porpoises, Phocoena phocoena, in Funka Bay, Hokkaido, Japan.
Mar Mamm Sci
14:
209-220,
1998.
9.
Piiper, J.
Modeling of gas exchange in lungs, gills and skin.
In: Advances in Comparative and Environmental Physiology, edited by Boutilier RG.. Berlin: Springer Verlag, 1990, vol. 6, p. 15-44.
10.
Ponganis, PJ,
Kooyman GL,
and
Castellini MA.
Determinants of the aerobic dive limit of Weddell seals: analysis of diving metabolic rates, postdive end tidal PO2s, and blood and muscle oxygen stores.
Physiol Zool
66:
732-749,
1993.
11.
Qvist, J,
Hill RD,
Schneider RC,
Falke KJ,
Liggins GC,
Guppy M,
Elliot RL,
Hochachka PW,
and
Zapol WM.
Hemoglobin concentrations and blood-gas tensions of free-diving weddell seals.
J Appl Physiol
61:
1560-1569,
1986
12.
Reed, JZ,
Chambers C,
Fedak MA,
and
Butler PJ.
Gas exchange of captive freely diving grey seals.
J Exp Biol
191:
1-18,
1994[Abstract].
13.
Reed, JZ,
Chambers C,
Hunter CJ,
Lockyer C,
Kastelein R,
Fedak MA,
and
Boutilier RG.
Gas exchange and heart rate in the harbour porpoise Phocoena phocoena.
J Comp Physiol [B]
170:
1-10,
2000[Medline].
14.
Snyder, GK.
Respiratory adaptations in diving mammals.
Respir Physiol
54:
269-294,
1983[Web of Science][Medline].
15.
Westgate, AJ,
Read AJ,
Berggren P,
Koopman HN,
and
Gaskin DE.
Diving behaviour of harbour porpoises, Phocoena phocoena.
Can J Fish Aquat Sci
52:
1064-1073,
1995.
16.
Woakes, AJ,
Butler PJ,
and
Snow DH.
The measurement of respiratory air flow in exercising horses.
In: Equine Exercise Physiology, edited by Gillespie JR,
and Robinson NE.. Davis, CA: International Conference on Equine Exercise Physiology (Proceedings), 1987, vol. 2, p. 194-205.
This article has been cited by other articles:
![]() |
J. A. Goldbogen, J. Calambokidis, D. A. Croll, J. T. Harvey, K. M. Newton, E. M. Oleson, G. Schorr, and R. E. Shadwick Foraging behavior of humpback whales: kinematic and respiratory patterns suggest a high cost for a lunge J. Exp. Biol., December 1, 2008; 211(23): 3712 - 3719. [Abstract] [Full Text] [PDF] |
||||
![]() |
N. M. Elliott, R. D. Andrews, and D. R. Jones Pharmacological blockade of the dive response: effects on heart rate and diving behaviour in the harbour seal (Phoca vitulina) J. Exp. Biol., December 1, 2002; 205(23): 3757 - 3765. [Abstract] [Full Text] [PDF] |
||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| Visit Other APS Journals Online |