|
|
|
|||
| Home Help Feedback Subscriptions Archive Search Table of Contents | ||||
First published online June 16, 2005
Journal of Experimental Biology 208, 2549-2554 (2005)
Published by The Company of Biologists 2005
doi: 10.1242/jeb.01665
Emperor penguins adjust swim speed according to the above-water height of ice holes through which they exit
1 International Coastal Research Center, Ocean Research Institute,
University of Tokyo, 2-106-1 Akahama, Otsuchi, Iwate 028-1102,
Japan
2 Center for Marine Biotechnology and Biomedicine, Scripps Institution of
Oceanography, University of California San Diego, La Jolla, CA 92093-0204,
USA
3 Laboratory of Physiology, Department of Biomedical Sciences, Graduate
School of Veterinary Medicine, Hokkaido University, North 18, West 9, Sapporo
060-0818, Japan
4 Biologging Institute, 2-31-10, Rex Yushima 301, Yushima Bunkyo, Tokyo
113-0034, Japan
* Author for correspondence (e-mail: katsu{at}wakame.ori.u-tokyo.ac.jp)
Accepted 26 April 2005
| Summary |
|---|
|
|
|---|
Key words: data logger, leap, kinetic energy, gravitational potential energy, buoyancy, Emperor penguins
| Introduction |
|---|
|
|
|---|
We deliberately changed the above-water heights of two ice holes through which emperor penguins exited. Swim speed, stroke frequency, body angle and depth were monitored using animal-born recorders. Time of exit and hole choice of penguins were simultaneously monitored by observers on the ice. We obtained the first field data to test the hypothesis that penguins adjust swim speed according to the above-water height of holes. We also described their behavior after failed exits onto the sea ice and determined whether they change holes after failed exits and/or whether they increase their swim speed in the subsequent trials.
| Materials and methods |
|---|
|
|
|---|
Recordings
Multi-sensor data loggers (W1000L-PD2GT: 22 mm diameter, 124 mm length; 80
g in air; Little Leonardo Corp., Tokyo, Japan) were used to record swim speed
at 0.25-s intervals for six deployments in 2003 and 0.125 s intervals for
seven deployments in 2004, depth at 1 s intervals, two-dimensional
accelerations (for detecting flipper movement from heaving acceleration and
body angle from surging acceleration; see
Sato et al., 2004
) at 1/16 or
1/32 s intervals, and ambient temperature at 10 s intervals. The data loggers
were attached to the back of penguins using waterproof Tesa tape
(Wilson and Wilson, 1989
) and
plastic cable ties. Swim speed was recorded as rotations of an external
propeller. It was converted to swimming speed using the calibration method of
Sato et al. (2003
). The data
loggers were deployed on the birds for 26.1-60.9 h. During the deployment,
birds repeatedly entered and exited through the holes with the other
non-instrumented birds.
Behaviors of the instrumented birds were monitored [time (h:m:s) of exit
and hole choice by birds] and recorded. A total of six deployments on four
birds were monitored from November 12 to Dececember 6 in 2003 and seven
deployments on five birds were monitored from November 14 to December 5 in
2004. Body masses were measured using a platform scale at deployment and
retrieval of the recorder. Body mass at deployment, ranging from 22.2 kg to
29.5 kg (Table 1), were used
for analysis. Food intake during the daily dives has been inferred from guano
deposition on the ice (Ponganis et al.,
1997
) and confirmed by animal-born video cameras
(Ponganis et al., 2000
). They
usually gained weight during the daytime and lost weight during the night.
|
The above-water heights of the two ice holes (between the edge of the ice
and sea surface) were purposefully changed between two holes and among
deployments in 2003 (Table 1).
At the beginning of the second year (from 7th to 10th deployments), the
above-water heights of the holes were purposefully adjusted within 10 cm
difference (Table 1). The
heights were modified with a chainsaw and ice chisel. Positions of higher and
lower holes were occasionally changed between deployments. Underwater
observations of departures and returns to the dive hole were made from a
sub-ice observation chamber (Kooyman,
1968
).
Analyses and graphics were performed with IGOR Pro (version 3.1) and StatView (version 5.0). The results of statistical tests were assumed to be significant at P<0.05.
Calculations
Consider a penguin of mass Mb that exits for a leap
with initial vertical velocity V. As the penguin rises to the highest
point in its leaping and lands on the ice on its belly, the vertical velocity
falls to zero, and the associated kinetic energy just under the sea surface is
converted to gravitational potential energy on the ice:
![]() | (1) |
![]() | (2) |
in Fig.
1), especially when the above-water height of the ice at the hole
was low. The theoretical vertical velocity could be considered to be the
minimal swim speed to reach the above-water height of the ice. Note that the
required speed is independent of the mass of bird in
Eq. 2. This is why data from all
birds were pooled when comparing measured speeds and the above-water heights
of the ice at the holes.
|
|
| Results |
|---|
|
|
|---|
Swim speeds in relation to the above-water heights of holes
Fig. 2 shows typical depth,
acceleration and swim speed profiles before an exit from the ice hole. The
bird adopted a stroke-and-glide method as it approached the hole. Gliding
phases between wing strokes were observed. Swim speed fluctuated around 2 m
s-1 in correspondence with the stroke pattern. The final
acceleration with three strokes enabled the penguin to reach a speed of 2.8 m
s-1 in less than 2 s. The final decrease in speed indicates that
the bird leapt out of the water, because the propeller does not rotate in the
air. The maximum swim speeds within 1 s before exit, which is represented by a
closed circle in Fig. 2, were
used for further analyses.
The maximum swim speeds before exits were significantly correlated with the above-water heights of the holes (Fig. 3, N=386 exits in 13 deployments by nine birds; Spearman R=0.421, P<0.0001). Most speeds of successful exits were above the minimum vertical velocity theoretically needed to reach the height (solid curve in Fig. 3). Swimming speeds of failed exits were sometimes lower than the theoretical minimum values (Fig. 3).
|
In the first six deployments in 2003, the differences in the above-water height of holes were larger than 10 cm (Table 1). The maximum swim speeds before exits from higher holes were greater than those of lower holes and there were significant differences in the speeds between holes in four of the six deployments in 2003 (two-tailed Mann-Whitney U tests; Fig. 4). In following four deployments from the 7th to the 10th in 2004, the above-water heights of the two holes were almost the same level (to within 10 cm; Table 1). There was no significant difference in the four deployments (two-tailed Mann-Whitney U tests; Fig. 4). In the last three deployments, the differences in the heights between the two holes were larger than 10 cm (Table 1). In these last deployments, the swim speeds in higher holes were greater than those of lower holes and there were significant differences in the speeds between higher and lower holes in one of the three deployments (two-tailed Mann-Whitney U tests; Fig. 4).
|
| Discussion |
|---|
|
|
|---|
Pooled data from all 13 deployments indicate that the swim speed increased significantly as the above-water height increased (Fig. 3). When the above-water heights were smaller than 20 cm, most observed swim speeds were much greater than the minimal theoretical values (the solid curve in Fig. 3). This might be because of the shallow body angles of penguins. If penguins adopt shallow body angles for lower ice heights, they need higher swim speeds to obtain the necessary vertical speeds for the heights (as indicated by dotted curves in Fig. 3). It is likely that penguins chose vertical take-off angles and minimum speeds to exit through the holes, especially for the higher holes (>40 cm), to avoid using excess energy for swimming before leaping (Fig. 3).
|
Several factors may contribute to the range of exit speeds observed in this study. In some instances, birds were chased by a Weddell seal (observation from a sub-ice chamber), so escape from predators might be one reason of some of the high speeds. In addition, the kinetic energy of swimming penguins may be converted not only to gravitational potential energy but also to the creation of waves at the surface, and to kinetic energy of some amount of splash. However, the present study could not deal with these aspects because of the difficulty in obtaining quantitative information.
The birds may obtain information on the above-water height of each ice hole
before leaps because they repeated dives and commuted frequently between the
water and the ice throughout the deployments. According to our observation,
they sometimes surfaced in the ice hole for a while, looked at their
surroundings, and then made a brief excursion below the surface before exiting
through the hole. Yoda and Ropert-Coudert
(2004
) demonstrated that
Adélie penguin adjusted their take-off angle to move out of the water
onto the ice. This study indicates that emperor penguins also have a capacity
to adjust swim speed before exits according to the above-water height of the
holes, and that they decided to increase swim speed for subsequent trials
after failed exits, instead of selecting the lower holes.
| Acknowledgments |
|---|
| Footnotes |
|---|
| References |
|---|
|
|
|---|
Kooyman, G. L. (1968). An analysis of some behavioral and physiological characteristics related to diving in the Weddell seal. Antarct. Biol. Ser. 11,227 -261.
Ponganis, P. J., Kooyman, G. L., Starke, L. N., Kooyman, C. A. and Kooyman, T. G. (1997). Post-dive blood lactate concentrations in emperor penguins, Aptenodytes forsteri. J. Exp. Biol. 200,1623 -1626.[Abstract]
Ponganis, P. J., van Dam, R. P., Marshall, G., Knower, T. and Levenson, D. H. (2000). Sub-ice foraging behavior of emeperor penguins. J. Exp. Biol. 203,3275 -3278.[Abstract]
Sato, K., Naito, Y., Kato, A., Niizuma, Y., Watanuki, Y.,
Charrassin, J.-B., Bost, C.-A., Handrich, Y. and Le Maho, Y.
(2002). Buoyancy and maximal diving depth in penguins: do they
control inhaling air volume? J. Exp. Biol.
205,1189
-1197.
Sato, K., Mitani, Y., Cameron, M. F., Siniff, D. B. and Naito,
Y. (2003). Factors affecting stroking patterns and body angle
in diving Weddell seals under natural conditions. J. Exp.
Biol. 206,1461
-1470.
Sato, K., Charrassin, J.-B., Bost, C.-A. and Naito, Y.
(2004). Why do macaroni penguins choose shallow body angles that
result in longer descent and ascent durations? J. Exp.
Biol. 207,4057
-4065.
van Dam, R. P., Ponganis, P. J., Ponganis, K. V., Levenson, D. H. and Marshall, G. (2002). Stroke frequencies of emperor penguins diving under sea ice. J. Exp. Biol. 205,3769 -3774.
Wilson, R. P. and Wilson, M. P. (1989). A package-attachment technique for penguins. Wildl. Soc. Bull. 17,77 -79.
Yoda, K. and Ropert-Coudert, Y. (2004). Decision-rules for leaping Adélie penguins (Pygoscelis adeliae). J. Zool. 263, 1-5.[CrossRef]
| |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||