Hydrodynamic aspects of shark scales

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William G. Raschi and John A. Musick rn.~T'TD .!. r'T ,N.! ... The College of William and Mary. Gloucester Point .... M. MacDonald (Rutgers Univ.), M. Namack, J.
NASA Contractor Report 3963

NASA-CR-396319860013418

Hydrodynamic Aspects of Shark Scales

William G. Raschi and John A. Musick

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NASA Contractor Report 3963

Hydrodynamic Aspects of Shark Scales

William G. Raschi Bucknell University Lewisburg, Pennsylvania John A. Musick Virginia Institute of Marine Science The College of William and Mary Gloucester Point, Virginia

Prepared for Langley Research Center under Contract NASl-16042

NI\S/\

National Aeronautics and Space Administration

Scientific and Technical Information Branch 1986

LIST OF FIGURES

Figure

Ti tle

Page

1

Scale measurements used in this study ........•...•....•..•••.•.•

2

Scanning electron micrographs of scales from Prionace glauca showing the presence of microrelief. ......•....•.••••••••

3

Scanning electron micrograph of the posterior margin

5

10

of

scales from Carcharhinus pl umbeus ..•. -. . . . . . • . . • . . .• . • • • • • • . • . • ••

14

4

Scale morphometries for ~. plumbeus.............................

16

5

Scanning electron micrograph of scales from Carcharhinus obscurus taken from the posterior ••••.••.•••.••••••••.••••• ~ •••.

20

6

Scale morphometries for C. obscurus •••...•.•.•.••••••••••••.••••

22

7

Scanning electron micrograph of the posterior margin of scales from Prionace glauca.....................................

25

8

Scale morphometries for~. glauca ••.••.•••••.•.•.••...•....•..••

28

9

Scanning electron micrograph of the posterior margin of scales from Carcharhinus signatus ••.•••••••.•••••••••••••••••...

31

10

Scale morphometries for C. signatus •..•.•.••...••••••••.•••.....

33

11

Scanning electron micrograph of the posterior margin of scales from Rhizoprionodon terraenovae ........••..•.•.•.•••••...

37

12

Scale morphometries for R. terraenovae ••••.•••.••••••.•.•••..••.

39

13

Scanning electron micrograph of the posterior margin of scales from Carcharhinus falciformis •••...•..••••••••••.•.•.....

43

14

Scale morphometries for C. falciformis ..••..••...••••.•••••..•..

45

15

Scanning electron micrographs of the posterior margin of scales from Carcharhinus leucas.................................

16

49

Scanning electron micrograph of a scale from Carcharhinus limbatus and Ginglymostoma cirratum .•••.••••....•.•••••...•.•... iii

52

LIST OF FIGURES (Continued)

Figure

Title

17

Scanning electron micrograph of the posterior margin of

Page

scales from Sphyrna mokarran and Isurus oxyrinchus •••..•••.•.••• 55 18

Scanning electron micrograph of the posterior margin of scales from Sphyrna lewini......................................

19

58

Scanning electron micrograph of the dorsal surface of scales from Mustelus canis......................................

61

20

Scale morphometrics for M. canis •••.•.•••••••.••••••••••••••••••

63

21

Scanning electron micrograph of the posterior margin of scales from Galeocerdo cuvieri ••••••••...•.•••..••••••••.•••••••

67

22

Scale morphometrics for G. cuvieri .••.•••••••••••••••••.••••...•

69

23

Scanning electron micrograph of scales from Odontaspis taurus. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .

Q. taurus •••.••••••....•••••...••••••.•• 75

24

Scale morphometrics for

25

Lengths and widths of scale crowns as estimated from growth

. equa tJ.ons •.••••.••.••..•.•••••.•...•.•••.•••.•.•••.•..•.••••••.• 26

82

The relationship between keel spacings as measured from a variety of species and the length of the fish •.•.•.•••••••••.•••

28

79

Heights and spacings of keels on the scale crowns as estimated from growth equations ..•.•..••••••••.•.••••••..•.•.•••

27

72

90

The relationship between keel heights as measured from a variety of species and the length of the fish ••.••••..•.••••.•••

iv

93

LIST OF TABLES

Table

Title

Page

I

Summary of the material collected for scale examination.....

4

II

Occurrence of microrelief ...................................

12

III

Scale morphometrics for the additional species as listed in the text.................................................

IV

48

Summary of slopes of the growth characteristics from scales of the nine species of which adequate numbers of specimens are available............................................... 84

V

Reduction in the secondary and tertiary keel spacing and heights (expressed in percentages) as compared with primary

values......................................................

98

Collection data for the material examined ...................

108

Appendix

I

v

ACKNOWLEDGEMENTS Embarrassingly, and

the

this

study has taken nearly five years to complete

futility of trying to remember everyone who has helped collect

all of the material we've used becomes immediately apparent. The removal of

these skin samples was often an ancillary task, occassionally deemed

unduly

onerous (Mundy, 1981), and very often accomplished at the end of

rather long and tiring days. Be assured that those omitted here are done so completely accidentally. For

help

in the field, we'd like to again thank M.E. Anderson (Cal.

Acad. Sci.), J. Gourley, D. Koester (Eye and Ear Hospital of Pittsburg), M.

MacDonald

(Rutgers Univ.), M. Namack, J. Smith (NMFS, Beaufort) and

in particular, the invaluable help of J. (VIMS)

Colvocoresses (VIMS). P. Mason

provided ample technical assistance for the SEM preparations, as Baumgardner and J. Estep (Bucknell Univ.) in the preparation of

did

K.

the

manuscript.

Bucknell University provided additional facilities and

financial support.

vi

INTRODUCTION The

energetics

thrust the

and

drag.

seeming

of

fish

locomotion

depends

on a balance between

The interest stimulated by "Gray's Paradox", that is

lack of sufficient power to overcome many of the estimated

values of drag, has resulted in the delineation of a number of potential drag

reducing

variety

of

mechanisms

structural

(Walters,

1962)

and

increase

surface

(Webb,

mechanisms, scale

Elasmobranch

perform

function.

this

type

layer,

a

particular interest is a

as scombroid scale corselets

(Burdak,

and

thereby

1969; Bone, 1972), which boundary

alter

layer

placoid scales, or dermal denticles, may

Bone and Howarth (1966) have suggested that

of scale reduces drag by creating turbulence in the boundary

thereby

preventing

Weinstein

(1978)

arranged

v-shaped

reduction number

such

Of

ctenii

roughness

characteristics. such

1975).

in

the

have

its

shown

grooves turbulent

separation.

More

recently, Walsh and

that surfaces composed of longitudinally

can

significantly

bursting

reduce

drag

through a

activity. Placoid scales from a

of galeoid shark species exhibit this type of surface morphology

and may therefore represent a potential drag reduction mechanism. Following

its

eruption

through

the

epidermis,

a

typical scale

consists of three parts (Applegate, 1967). An expanded, plate-like crown lies narrow scale

above neck into

the

surface of the skin and is attached by a somewhat more

or pedicel to a rectangular or stellate base anchoring the the

integument. The crown normally exhibits a large medial

ridge or keel which runs longitudinally along the midline and is flanked along

either

side by one or more lateral keels (Compagno, 1979). These

I

keels

often

lateral

extend

cusps.

the

This

posterior margin of the crown into medial and

general

arrangement

is

found

in

many

widely

separated phylogenetic groups (White, 1937). comparison

A

of

theoretical,

grooved

difficult

obtain

to

reasons. from

Although

various

Radcliffe, and

from

specimen,

including

not

inclination 1970)

and

as by

existing

drawings.

only

Walsh

and

literature

for

of

the

Weinstein

is

a number of

1948~

Castro, 19831

In

addition,

a

great deal of

their

general

shape (Applegate,

1967~

Sayles and Hershkowitz, 1937) but also the

1928~

of the crown to the body surface (Chernyshov and

well. a

Finally,

all

synchronomorial

living species of galeoids are

scale type (Compagno, 1973) whose

shape often change dramatically through replacement (Garrick, 1917~

Radcliffe,

this

study

from

a

examine

these

Daniel,

1979~

of

1960;

by

that

found between scales from different locations on a single

characterized size

the

proposed

with

1916), it is often difficult to determine their actual sbapes

is

Zayets,

from

dimensions

several authors have presented representative scales

variation

angle

surface

crown

shark species (Bigelow and Schroeder,

dimensions

Compagno,

various

then,

variety what

Raschi, et al.,

1982~

Reif, 1974). The aims of

are to compare the surface structure of scale crowns of

shark

changes

species may

occur

replacement.

2

with the above model as well as to to

these

scales

during

their

METHODS AND MATERIALS A

total

(Table

of 129 skin samples from 15 species of sharks was examined

I).

The

sportfishing clubs)

or

Institute

majority

tournaments through

the

of

the

fish

(Virginia longline

were

obtained

from

either

Beach and Charleston Shark fishing surveys

conducted

by

the Virginia

of Marine Science (VIMS) during the summers of 1981 and 1982.

Additional

material

was also collected from a variety of other sources

including the R/V Columbus Iselin cruise CI-7803, Taute Bros. (Marathon, Pflueger

Fla. ),

Marine

sportfishermen.

Collection

and

are

longitudes

fishing the

not

tournaments

Institut

Taxidermy data

and

a

number

of

individual

is presented in Appendix I. Latitudes

available

for

those

specimens collected at

in Charleston, S.C.; for specimen #64 on loan from

Fondamental

d'Afrique

Noire

and

for

the two aquarium

specimens, #82 and 83. Nomenclature follows Robins et ale (1980). Skin the

patches,

measuring 25-50 sq. cm, were removed from just below

anterior margin of the first dorsal fin. Subsamples were washed and

placed

in

a concentrated solution of sodium hypochlorite to remove the

scales

while

examination. distilled sample

the

Individual

water

were

remainder

and

then

of

the

scales

were

sample washed

was in

frozen several

for

future

rinses

of

air dried. Approximately fifteen scales from each

mounted

on

an

aluminum

SEM

stub and coated with

gold-palladium by vacuum evaporation. Four

sets

of

measurements

were made on five separate scales from

each

stub (figure 1). Initially, the length and width of each crown was

taken

from directly above its surface (0-20 degree tilt). Secondly, the

3

Table I.

Summary of the material collected for scale examination. Number of individuals examined

Size range (total length in cm)

Carcharhinus falciformis

5

103-268

Carcharhinus leucas

4

169-278

Carcharhinus limbatus

5

148-173

Carcharhinus obscurus

17

86-334

Carcharhinus p1umbeus

30

59-216

Carcharhinus signatus

8

76-222

12

156-404

Species

Galeocerdo cuvieri Ginglymostoma cirratum

2

72-77

Isurus oxyrinchus

3

132-182

----

10

37-127

Odontaspis taurus

9

165-247

13

34-348

Rhizoprionodon terraenovae

7

40-106

Sphyrna lewini

3

54-225

Muste1us canis

Prionace glauca

1 129

Sphyrna mokarran

4

252

Fig. 1. as follows:

Scale measurements used in this study.

Abbreviations are

"A", crown widths; "B", crown length; "C", primary inter...

keel distance; "D", primary keel height; 1°, 2°, 3° are the primary, secondary, and tertiary keels.

(Redrawn by J. Estep)

5

inter-keel

distance,

or

spacing,

was

measured

between the peaks of

adjacent

keels. These were taken from a posterior aspect with the crown

surface

tilted between 30 and 50 degrees. The bilaterally averaged pair

of

spacings

lateral,

or

Similarly, adjacent values. was on

between secondary

the

medial,

keels,

or

is

primary

designated

keel, and the adjacent as

the

primary value.

that pair of distances between the secondary keels and their lateral,

or

tertiary

keels,

are

considered

the secondary

Similar nomenclature is used for each subsequent pair. The mean

then calculated for all the averaged values for each of these pairs a

crown.

Finally, the heights of the ridges were measured with the

crown

tilted

so

degrees and

tilt).

compared

each

crown

from

the

Pairs of the secondary and tertiary keels were averaged with the primary ridge. A mean value for all the keels on

was CRT

magnifications scale

as to provide a view parallel with its surface (70-90

also screen between

calculated. All measurements were taken directly to 180

the

nearest five microns, with specimens at

and

200

X. The actual angle to which

was tilted depended on both the angle at which the crown sat

a on

the

scale

the

stub. In addition to the above measurements, the number of keels on

each

scale was counted and a photograph of one scale from each specimen

taken body

base as well as on variations of the seating of the scale on

for future reference. The regressions of all these measurements on lengths

for each species follows Snedecor and Cochran (1967) with

significance set at the 99% level.

7

RESULTS Scale Types Three this

different morphological types of scales were distinguished in

study.

crown

The first (figure 3) is characterized by a relatively thin

exhibiting a single, prominent primary keel and a variable number

of lateral, often smaller, keels. The anterior margin is normally evenly rounded found

with on

all

oxyrinchus, and

the

similarly

Prionace glauca, Rhizoprionodon terraenovae, Sphyrna lewini

thin pairs

lanceolate

shape,

of

posterior

Mustelus

the

The second morphological type (figure 19) exhibits a

crown

successive

pointed

either emarginate or smooth. This type is

specimens in the genus Carcharhinus as well as on Isurus

mokarran.

S.

species

posterior

canis

in

with

media~

a

lateral

pair of primary keels flanked by

keels. It has a typically blade-like, or

with a broadly rounded anterior margin and a sharply margin. this

This study,

type but

is

found

only on specimens of

appears to be typical of all the

in the genus Mustelus (Bigelow and Schroeder, 1948), except for

South American M. dorsalis (Bigelow and Schroeder, 1940). The third ( figure

type

correspondingly thicker very

is

21) heavy

characterized

base.

The

scale

by

a

necks

very

thick

crown

and

are disproportionately

and tend to be somewhat reduced in height. The crown exhibits a

prominent

primary

keel with a somewhat smaller pair of secondary

keels. The margins are evenly rounded with the absence of any noticeable cusps.

This

type

of

scale is found on Galeocerdo cuvieri, Odontaspis

taurus and Ginglymostoma cirratum.

8

Microrelief In

addition

examined

In

this

microrelief pockets

to

the normal ridges, approximately 50% of the scales study

also

exhibit

additional

microrelief.

This

is typically arranged in the form of hexagonal or octagonal

(figure

2),

often becoming compressed along the scale margin.

The

surface area covered by microrelief, when present, varies from only

the

anterior

II).

c.

margin

to

the entire dorsal surface of the scale (Table

It is found in varying degrees on all specimens of signatus,

mokarran;

on ~.

obscurus,

By

only

a

glauca,

R.

terraenovae,

specimens

of

C.

P.

few

leucas,

falciformis,

s.

lewini, S.

C. limbatus, C.

plumbeus; and is completely absent from all specimens of G.

!.

cuvieri,

canis,

M.

~.

oxyrinchus,~.

dividing

designated

all

of

cirratum and O. taurus. the

scales

into

two artificial groups; one

as completely covered, with microrelief covering between 75%

and 100% of the crown surface (figure 2, 18) and the other designated as only

partially

(figure

5a,

19),

microrelief within

covered, it

becomes

development

each

species

with

microrelief apparent

reflects

the

covering

that relative

the

from

25% to 50%

relative degree of

size

of the specimen

(compare with Appendix I). In those species which

contain specimens exhibiting both complete and partial covering, such as C.

falciformis,~.

obscurus,

~.

plumbeus, P. glauca and

~.

terraenovae,

only the smallest individuals have completely covered scales while those from

larger

several

species

exhibited devoid

specimens

of

tend to be only partially covered. Furthermore,

examined, such as

~.

leucas,

~.

limbatus and

~.

canis,

only partially covered scales in addition to those completely any

microrelief; whereas none contained only specimens with

9

Fig. 2.

Scanning electron micrographs of scales from Prionace

glauca showing the presence of microrelief. (a) From a 34 cm TL male (specimen no. 106) at 190 X magnification, (b) From a 46 cm TL female (specimen no. 109) at 520 X magnification.

10

Table II.

Occurrence of microrelief Specimen number Complete

c.

fa1ciformis

1-3

Partial 4, 5 6

C. 1eucas

c.

limbatus

c.

obscurus

15-17, 19

c.

p1umbeus

32-40

c.

signatus

62-64, 67-69

13, 14 18, 20-23, 25-31 41 65, 66 87-96

M. canis P. glauca

106-115

116-118

R. terraenovae

119-121

122-125

S. 1ewini

126

127, 128

S. mokarran

129

12

completely covered scales. Both pieces of evidence strongly suggest that microrelief

is more prevalent on smaller scales from smaller specimens,

decreasing

in

significance

relative

of

degree

microrelief

on

larger

replacement

scales.

The

will be further discussed in a subsequent

report. The

dimensions

intraspecific

of

variation

the and

scale will

crowns

exhibit

considerable

be used to characterize scales from

each individual species.

Species Descriptions C. plumbeus

The

greatest

ontogenetic cm 83%

of

1948) The

scale

intervals

and

most

reliable

picture

of

postpartum,

total

total lengths of 59 to 216 cm. This accounts for

size range of between 56 cm (Bigelow and Schroeder,

249 cm (Garrick, 1982) previously recorded for this species.

scale

generally

the

development. Scales were removed from specimens at 5

between

the

of scales were examined from this species and

provide

therefore

may

number

crown

is moderately thick with very prominent ridges. It is

ovoid in shape, with broadly rounded margins and a relatively

short pedicel (figure 3). The size

width

range

replacement an

estimated

of

the

studied

crown is greater than the length throughout the

(figure

4).

widths increase ontogenetically with

at a rate of 3.02 microns/cm (r crown

width

= 0.93**).

This rate yields

of from 150 microns to 703 microns over the

total size range. Actual measurements range from 170 microns (specimen # 37)

to

785

microns

(specimen

#

61).

13

Crown

lengths

also increase

Fig. 3.

Scanning electron micrograph of the posterior margin

of

scales from Carcharhinus plumbeus. (a) From a 88 em TL female (specimen no. 37), (b) From a 188 cm TL female (specimen no. 57).

14

Fig. 4.

Scale morphometrics for

£.

resents the average of five measurements.

plumbeus.

Each data point rep-

Spacings and heights are

average values for all the keels on each crown.

Line equations are

calculated from the total number of individual measurements.

The

equation describing the increase in the number of keels is based on only those specimens larger than 110 cm TL (specimen no. 42-61).

16

.... -..... -- --

600

.... --- -

_

.....

.....

500

ya-189!5 . +3.02X

I-'

"

400



a

o

a

o



a

Il:



a

z

(.)

~

SCALE SCALE TOTAL TOTAL

....

/0 0

..

/' ~.

~--6'.~

•••• /0

. /0 6~



WIDTH LENGTH INTER-KEEL KEEL HEIGHT



o

./.

300

200

. //

. /.Y ../. ·0· /

...

....

TL (em)

(J)



,.-

NUMBER OF KEELS



(p

~

0

0

o

0

0

,./".......... 0

/0 0

0

Y--26 .08 .. 2.34 X

o

0

Carcharhinus plumbeus

0

o~v

~- ~

o

ct

ya 48.156 .. 0.30 X



••



_.a-a-----_--ro;----..-.--·----..---------- - - --

100

_ • • _ . _ . _ . _ . _ . _. ._. _ _ _. .

40

60

80

100

120

~

~. y I9.16+ 0.08X ... .--.-.~••-~ .6 Aa

_

• 140

TOTAL LENGTH (em)

.......

160

180

200

ontogenetically corresponding the

total

at

a

rate of 2.34 microns/em (r

estimated

size

range

range.

=

0.91**), yielding a

of from 105 microns to 533 microns over

Actual

measurements

range

from

125 microns

(specimen # 32, 37) to 625 microns (specimen # 61). Smaller prominent number TL

ridges,

c.

of

whereas

plumbeus

on

exhibit scales with only three

fish longer than 120 to 140 em TL, that

increases with the replacement scales at a rate of 0.03 keels/em 6.32**).

(t

crown 53,

specimens

The averaged, total inter-keel distance on a single

ranges from 55 microns (specimen # 38) to 125 microns (specimen # 56,

61).

These

of

0.30

microns/cm-rL(t

rate

spacings

of

from

spacing values also increase ontogenetically at a

65

16.62**).

microns

to

This rate yields estimated

120 microns. The primary inter-keel

distance varies from 55 microns (specimen # 38) to 150 microns (specimen #

61),

while the average secondary inter-keel distances are between 75

microns

to

183 microns. This corresponds to a decrease of between 6.1%

and 31.0% (average

=

18.6%) from the primary.

Keel heights tend to remain relatively constant, with an increase in the

average

height

=

microns/em TL (t (specimen

#

37,

all

keels

on

a

single

crown of only 0.08

7.74**). Total averaged heights range from 18 microns 41)

to

only

52 24

microns (specimen # 46), while predicted

values

range

range.

The primary keel is normally from 20 microns (specimen # 32, 34,

37,

from

for

microns to 38 microns over the total size

38, 39, 41) to 70 microns (specimen # 53) high. The secondary keels

exhibit an average reduction in height from that of the primary by 10.9% (ranging

from

an

increase

of

33%

to

a

decrease of 40%), with the

bilaterally averaged measurements ranging between 18 microns (specimen #

18

32,

41)

and

greater 75%),

55

microns

reduction with

of

values

(specimen # 53). Tertiary keels show a still

45.7%

ranging

from the primary keel (ranging from 7% to between

microns (specimen # 43) and 43

5

microns (specimen # 61)

c.

obscurus This

et

species

aI,

1973)

examined

to

from

generally

is larger than a

maximum

over

smaller.

~.

of

plumbeus, ranging from 69 em (Bass, 363

em (Garrick, 1982). Scales were

84% of this range. By comparison, these scales are Their

crowns

appear much thinner and less heavily

sculptured (figure 5). The anterior margin is broadly rounded while that of the posterior is always emarginate. Scales

are

approximately 22)

to

500

wider

190

cm

than

long

only

on

specimens

smaller

than

(figure 6), ranging from 180 microns (specimen #

microns

(specimen

#

31).

These

values

increase

ontogenetically

at a rate of 0.66 microns/em TL (r = 0.85**), result.ing

in

smaller

a

somewhat

microns. scales

Similarly, at

a

rate

the of

estimated length

range

of

from

229 microns to 418

of the crown increases on replacement

0.99 microns/em TL (r

=

0.87**). Actual lengths

measured between 170 microns (specimen # 22) and 560 microns (specimen # 31)

as compared with the projected estimated values of from 188 microns

to 472 microns. The

number

of ridges range from 3 on smaller specimens to 7 on the

larger. This number increases at a rate of 0.01 keels/em TL which is not significantly

different from 0 (t

=

2.21). The average total inter-keel

distance increases with body length at a rate of 0.05 microns/em TL (t

19

=

Fig. 5.

Scanning electron micrograph of scales from Carcharhinus

obscurus taken from the posterior, (a) From a 127 cm TL male (specimen no. 23), (b) From a 334 cm Tl female

(s~ecimen

20

no. 31).

Fig. 6.

Scale morphometrics for

£.

obscurus.

represents the average of five measurements.

Each data point

Spacings and heights are

average values for all the keels on each crown.

Line equations are

calculated from the total number of individual measurements.

22

...

~

~

600

•. . •



y- 4.08.0.01)(

NUMBER OF KEELS

500

90

120

150

180

210

240 270

o

aoo aao

TL (em)

C/)

z

N W

400

o o

• • SCALE o • SCALE • • TOTAL A • TOTAL

Y-1I9.99+0.99X

WIDTH LENGTH INTER-KEEL KEEL HEIGHT

0:: ~

300

••

•!~ ~.,.--.

i

___ 0."- .-----------o ----->'

0

a::

o • SCALE • • SCALE • a TOTAL • • TOTAL



Y=2.33+ O.OOX

300

330

360

390

(em)

ya-179.33 + 2.36 X

LENGTH WIDTH INTER - KEEL KEEL HEIGHT

o

o

600

y a 36.23+ 1.73X

o

0

:t

o

400

Galeocerdo cuvierl

. . . -.-...-- • o



~-~:.----



ya 22.31 + 0.63 X

.-~-~----

200

• ya2.14 +0.25X

o 150

180

210

240

270

300

330

360

390

TOTAL LENGTH (em)

.

~

.......... ----,----------------.-------~----

~

species. Scale

crowns

increasing (and

at

at

from

1

to

3

ridges,

a rate of 0.02 keels/cm TL (t

primary)

scales

exhibit

keel

a

=

with

values slowly

4.818**). Averaged total

spacings on a single crown increase on replacement

rate of 0.63 microns/cm TL (t

=

9.405**), ranging from 63

microns (specimen # 70) to 275 microns (specimen # 81). Estimated values range

between 51 microns and 489 microns over the published size range.

Similarly, increase

averaged

total

keel

heights

on

an individual crown

ontogenetically at a rate of 0.25 microns/cm TL (t

=

6.349**),

from 35 microns (specimen # 70) to 153 microns (specimen # 81).

ranging This

the

yields estimated values of between 14 microns and 187 microns over

the

published

#

(specimen averaged microns from

size 73)

range.

190 microns (specimen # 81) while the bilaterally

to

secondary

Primary keel heights range from 75 microns

keels

from 5 microns (specimen # 70) to 135

range

(specimen # 81). This amounts to an average reduction in height

the

particular specimens

primary

keel

interest

of

is

from 28.9% to 94.7% (average of 77.9%). Of

the striking change in general shape in larger

(as in specimen # 81) to one with proportionately much larger

and prominent ridges.

Odontaspis taurus Scales those

of

from this species (figure 23) are similar in many aspects to G.

proportionately generally

cuvieri. larger

limited

disproportionately

They

are

generally very large and heavy, with

bases. Keels also tend to be very large and are

to

three

larger

and

in

number,

with

the

primary

being

the secondary ridges confluent with the

71

Fig. 23.

Scanning electron micrograph of scales from Odontaspis

taurus, (a) Dorsal view of a scale from a 210 em TL female (specimen no. 100), (b) Apical view from a scale from a 235 cm TL male (specimen no. 104).

72

lateral

margins

narrow

of

the

crowns. Skin samples were removed from a very

portion (37.6%) of this species' published size range of between

100 cm (Castro, 1982) and 318 cm (Bigelow and Schroeder, 1948). Scale

crowns

are

generally

wider than long (figure 24) on fish

smaller than between 210 cm and 220 cm TL. Individual crown widths range from

340

microns

increasing 0.38**). 541

with

This

microns

#

(specimen body

length

97) at

a

to

565

rate

microns (specimen # 99),

of

0.84 microns/cm TL (r

=

rate results in estimated values between 358 microns and over the published size range. Crown lengths range between

265 microns (specimen # 97) and 615 microns (specimen # 103), increasing ontogenetically lengths

vary

at a rate of 2.72 microns/cm TL (r from

146

= 0.69**).

Estimated

microns to 739 microns over the published size

range. Crowns rate

of

exhibit 0.02

average

from 1 to 3 ridges, increasing ontogenetically at a

keels/cm

distance

of

TL

from

=

(t 130

3.279**). These keels are located an

microns (specimen # 97) to 225 microns

(specimen # 104) apart. These spacings increase on replacement scales at a

rate

of

estimated

0.59 value

microns/cm of

TL

between

(t

106

= 3.709**),

microns

and

a rate which yields an 235

microns

over the

published size range. Average keel heights for all the keels on a single crown

also increase with body length at a rate of 0.53 microns/cm TL (t

2.755**), (specimen values

of

#

ranging

from

32

microns

(specimen # 98) to 160 microns

99). Similarly, this rate yields a wide range of estimated from 15 microns to 130 microns over the published size range

for this species. Primary keel heights vary between 50 microns (specimen

#

100) and 160 microns (specimen # 99). Secondary keels are between 29%

74

Fig. 24.

Scale morphometrics for

sents the average of five measurements.

£.

taurus.

Each data point repre-

The spacings and heights are

average values for all of the keels on each crown.

Line equations are

calculated from the total number of individual measurements. are the same as in other graphs.

75

Symbols

6

600

C/)

yaS.SI-0.02X

4

2

500

NUMBER OF KEELS



• •• 170

-

190

-.

400

z o a:: o

~

ISO

200 TL

210

• • • • 220

230

Y·-126.27 + 2.72 X

o

i"

0



240

e-------::

0

(em)

• y. Z73.87 + 0.84 X

Odontasp/s taurus

300

Y·47.79 + 0.S9X

200

------------------------.---------------------.----.--A

100

___ 160

A

__--------A------------------~----------A-----------~A

170

180

190

200

210

TOTAL LENGTH (em)

A

A

Y·-3S.06 + 0.!S3X

220

230

240

and

91%

shorter

(average

of

56.9%)

than the primaries, with values

between 8 microns (specimen # 98) and 68 microns (specimen # 103). Finally, available

the

two

for

specimens

study

of

Ginglymostma

possessed

scales

cirratum which were

which

exhibited

many

characteristics similar to those of both G. cuvieri and O. taurus. These scales

(figure

conspicuous

16b)

cusps.

were

generally

Individual

crown

broadly lengths

rounded range

and

free

of

from 455 microns

(specimen

# 83) to 675 microns (specimen # 82), with average values for

the

five

scales from each specimen between 539 microns (specimen # 83)

and

599

380

microns

range and

microns (specimen # 82). Similarly, crown widths range between

of 566

part

(specimen

microns (specimen # 82). While distinct keels are for the most

elevations.

there

Distances

are

distinguishable

between

these

ridges

ridges range

or from

longitudinal 115 microns

# 83) to 220 microns (specimen # 82), with average values for

(specimen

specimen

heights

83) and 690 microns (specimen # 82) with the

for each specimen between 531 microns (specimen # 82)

values

absent,

each

#

between

175

microns

and 197 microns. Similarly, ridge

range from 18 microns (specimen # 83) to 42 microns (specimen #

82), with total averaged values between 26 microns and 39 microns. These values to

less

1982),

however, are from specimens only 70 to 80 em long, which amounts than and

may

1/4

of the total'length of 425 cm of the adult (Castro,

therefore

only

be considered as an indication of the

typical scale morphology from the juveniles of this species.

77

DISCUSSION Previous studies of the squamation on pelagic galeoids by Reif and Dinkelacker (1982) provide scale keel spacing values for eleven species which closely agree with the average values obtained in this study.

Individual measurements for

glauca and

i.

while those of

£.

obscurus,

l.

oxyrinchus,

f.

lewini fall within the range obtained in this study,

£.

falciformis are only slightly larger than those

obtained here. A comparison of crown morphooetrics projected over the total size range for each species shows considerable intraspecific similarity (figure 25).

In the majority of species, crown lengths range from

approximately 100 microns on juveniles to nearly 500 microns on the largest adults, while crown widths exhibit a somewhat narrower range of from 125 microns on juveniles to a maximum of 425 microns on adults.

Crowns of similar size were observed on smaller species, such

as Rhizoprionodon terraenovae, as well as the much larger species, such as Carcharhinus obscurus.

Even the greatly elongated crowns of

the scales froo Mustelus canis exhibit comparable widths and only slightly greater lengths.

In contrast however, a few species possess

scales with noticeably larger crowns.

Carcharhinus plumbeus, for

example, possesses crowns with maximum widths up to 703 microns and lengths up to 533 microns.

Moreover, much larger dimensions are found

on both Odontaspis taurus and Galeocerdo cuvieri.

The largest

individuals of this last species, for example, would appear to possess scales whose crowns are somewhat longer than 1300 microns and wider than 1500 microns.

A few of the additional species, such as

78

Fig. 25. equations.

Lengths and widths of scale crowns as estimated from growth

Only those species are included for which sufficient data was

available for such calculations.

79

ex:>

--

LENGTH

0

II

II

.400

1000

100

200

fl. ~II"'." 0.11111'11. C. plll", ••II.

---200

MICRONS

M. ~II"'.

c.•••~II'U. WIDTH

If

,'.lItI.

c. ."".,••

c. ,.,.".,"". If. ,." •••••••

100

1000

1400

laoo

Carcharhinus leucas and Ginglymostoma cirratum, also appear to possess scales with significantly larger crowns. The

overall

interspecific between 100

similarity

adjacent

microns

probably

in

C.

(figure

also

26).

exhibit

The

a

great

average

deal

of

maximum distance

keels on a crown normally lies between 50 microns and most

species.

However,

C.

plumbeus,

~.

glauca and

leucas, possess scales with slightly larger spacings while

o.

those from

dimensions

keel

taurus, G. cuvieri, and probably

~.

cirratum, exhibit much

larger values. For example, the maximum spacing is more than 200 microns on

scales

average

keel

species, Isurus

o.

from

heights

with

and

and

remain

estimated

oxyrinchus

cuvieri

taurus

and

nearly 500 microns on G. cuvieri. The

less

maximum Sphyrna

probably

C.

than 50 microns in the majority of heights even as low as 10 microns in

lewini.

leucas,

Again

possess

however,

crowns

o.

whose

taurus, G. keels

are

significantly higher, up to four times so in Galeocerdo. The rates at which crown lengths and widths increase hO\\'ever, show a great

deal of interspecific variation (Table IV). Lengths of successive

replacement scales increase at rates between 0.50 microns/cm body length (C.

falciformis)

and

2.34 microns/em

(0.

taurus);

may

not

glauca.

Similarly,

replacement 0.39

or

scales

microns/cm

(P.

the

~.

plumbeus) or 2.72 microns/em

increase at all, as in the case of Prionace

rates

at

,"hich

the crown widths increase on

are also variable. Widths may increase as slowly as glauca)

and

0.66 microns/cm (C. obscurus) or as

rapidly as 3.02 microns/cm (C. plumbeus). Scales protective

on

the

majority

of

galeoid

species

perform

either

a

or hydrodynamic function (Reif, 1982). In either case, most,

81

Fig. 26.

Heights and spacings of keels on the scale crowns as esti-

mated from growth equations.

Only those species are included for which

sufficient data was available for such calculations.

82

SNO~~IW

ooz

o

001

001

I/UllfJ 'W

I

I

./UI.ltJJlfJ/"J '3

I

I

_IIAOUOII.l.l., '1/

I

.nJnfJ.qo ·3

lH913H

.'NIIU6/. ·3 DfJnllll (:I

I

.m,qUln/d '3

I

"n.lnlJl '0 !.I.,Atul '9

ooz

002

OOg

I 9NI~\fcJS

I

I

I

II III

-

(Y')

co

Table IV. Summary of slopes of the growth characteristics from scales of the nine species for which adequate numbers of specimens are available.

Species are arranged in order of

increasing rates of keel spacings. Species

Length

Width

Spacing

Height

C. signatus

0.57

1.16

-0.09

0.00

R. terraenovae

1.13

2.28

0.00

0.00

M. canis

2.06

2.30

0.00

0.,00

C. fa1ciforrnis

0.50

0.77

0.00

0.03

C. obscurus

0.99

0.66

0.05

0.03

P. glauca

0.00

0.39

0.06

0.03

C. p1urnbeus

2.34

3.02

0.30

0.08

o.

2.72

0.84

0.59

0.53

1. 73

2.36

0.63

0.25

taurus

G. cuvieri

84

if

not

all, of the external surface of the fish's body must be covered

despite

an

growth.

This requires that the ratio of the area of the skin covered by

scales

increasing

with

the

individual's

surface area which results from continuous body

total

area

of

skin remains constant throughout the

ontogeny (Reif, 1980). The amount of area covered by scale

crowns results from a combination of an increase in the number of scales with of

the increase in the size of the individual croWD. The wide variety scale

growth

rates observed in this study reflects the interaction

between these two processes. A The

sharp dichotomy exists in growth rates of the keel morphometrics.

majority

keel

spacings,

distance

of

microns/cm

Similarly, signatus, in

C.

species ranging

in

from

an

to

actual

the

decrease

in

the inter-keel

very slow rate of from 0.05 to 0.06

C. obscurus and P. glauca. Several species, including

falciformis

C.

the R.

exhibit extremely slow rates of increase for

signatus

C.

terraenovae,

as

of

keels

and M. canis, exhibit no increase at all.

remain

either ~.

terraenovae and

falciformis,~.

~.

at

a

constant height, as in C.

canis, or increase only very slightly,

obscurus and P. glauca. In a second group of

species however, inter-keel distances increase very rapidly; at rates up to

0.60

microns/cm,

Moreover, rates

between

cuvieri. these

the

Only

two

on

scales

from

both

O. taurus and G. cuvieri.

heights of these keels increase on replacement scales at 0.25

microns/cm plumbeus

C.

groups,

with

on O. taurus and 0.53 microns/cm on G.

occupies

keel

an intermediate position between

spacings

increasing

at a rate of 0.30

microns/cm and heights at a rate of 0.08 microns/cm. In

summary,

these

scales appear divided into two morphometrically

85

distinct

groups.

increase

in

The

size

approximately

425

majority

at

a

wide

of species exhibit scales whose crowns variety

of rates to a maximum width of

microns and a length of 500 microns. Ridges on these

crowns remain a nearly constant 50 microns high throughout each species' size

range

largely

characteristic of both the first and second morphological type·s

described possess

earlier

reaching

group.

microns from and

in

this report. A second group of species, however,

a much thicker, heavier scale. Crowns on these scales grow very

rapidly, first

and are normally located 100 microns apart. Such crowns are

widths and lengths nearly twice that of the

The keels on these scales are set further apart, from 235 taurus)

(0.

160

maximum

to 490 microns

~.

cuvieri), and are much higher, ~.

cuvieri). Both heights

replacement

scales. These species

microns (0. taurus) to 187 microns

spacings

increase

largely

comprise

exhibit

intermediate

plumbeus,

C.

growth rates

the

rapidly third

on

morphological

values

for

keel

group.

spacings

Only a few species G.

cirratum,

C.

leucas and P. glauca), keel height (C. leucas) or general

1£.

plumbeus).

In order to compare these measurements with a hypothetical model for drag

reduction,

each

species. The little information presently available can be divided

roughly

it

is first necessary to consider swimming speeds for

into two categories. Burst speeds, such as those which might be

used in capturing highly mobile prey or in escaping predators, have been estimated

at

522

cm/sec for

s.

brevirostris

leucas and at 244 cm/sec for the lemon

shark,

Negaprion

cm/sec

have been recorded for Carcharhinus (Prionace) glauca (Nikolsky,

1978).

Secondly,

a

limited

(Gero,

number

86

1952).

Values as large as 1000

of measurements are available for

voluntary, or sustained, speeds.

Beamish (1978) estimated sustained

speeds of between 18 and 202 cm/sec for

£.

leucas based on Thorson's

(1971) tagging studies while Heard and Ripley (1951) have reported similar speeds of 43 cm/sec for the soupfin shark (Galeorhinus zyopterus); both being based on longer-term

~igrational

studies.

Specific shorter-term observations of cruising speeds have been reported for

f.

leucas of 56 to 83 cm/sec and for

£.

plumbeus of 60 to

67 cm/sec (Weihs, et al., 1981) from an aquarium study. Due to the very limited number of actual measurements, it is necessary to rely only on estimates for the majority of other species. Weihs (1977) proposed the use of the following equation to predict voluntary swimming speeds: U = 0.503 L 0.43 where U is the voluntary swimming speed and L is the body length. This equation closely approximates those values previously reported for both

£.

plumbeus and

£.

leucas.

Similarly, Wardle (1975)

proposed the following equation to predict maximum burst speeds: U

= AL/2T

where A is the stride length, based on Bainbridge's (1958) estimate of forward motion of from 60% to 80% of both length (L), (60% was used in the present study) and T is muscle contraction time (estimated to be about 0.08 S for fish of about 2 m in length, using Wardle's 1975 curves).

While this equation has only been verified with teleost

87

data, it appears to provide a sufficient estimate for elasmobranchs. Therefore for example, estimated swimming speeds for a specimen of

£.

leucas between 1.5 and 2.0 neters long should lie between voluntary swinmling speeds of 53 cm/sec to 60 em/sec and burst swimnling speeds of 900 em/sec to 1200 em/sec, values close to those previously reported from the literature. It is now possible to evaluate the keel morphometrics" exhibited by each species in terms of potential drag reduction.

The actual

measurements, expressed in metric terms, can be expressed in terms of law of the Wall coordinates through the following two equations (Walsh and Weinstein, 1978): h+

= hu/v (C /2) 1/2 s + = su/v (C /2) 1/2 f

f

. where h + and s + are heights and spacing in terms of law of the Wall coordinates, hand s are heights and spacing in em, u is the free stream velocity (here expressed in swimming speeds), v is the kinematic viscosity of sea water and C is skin friction. f

This later

term can be calculated from the following equation: C

f

=

.074 R- 1/ 5

where R is the Reynold's number: defined above.

R

= Lu/v; L, u, and v having been

The major limitation on these equat ions lies in the

paucity of information on specific swimming speeds.

88

Throughout their ontogeny, all of the species examined in this study (with

the

cuvieri)

possible possess

optimal

value

swimming

exception

scales

of

speeds

16

of

with

(in

(figure

the

ridge

law

of

27).

very

largest

spacings

specimens ofG.

less than the proposed

the Wall coordinates) at voluntary

Moreover,

a

number

of

these species

maintain keel spacings which approximate the optimal value projected for burst

swimming

£.

limbatus, and

S.

speeds. This is particularly true in

£.

obscurus,

mokarran.

In

£.

falciformis,

£.

signatus, Isurus oxyrinchus, Sphyrna lewini,

contrast,

the ridge spacings on the scales from

Galeocerdo cuvieri, Odontaspis taurus and Ginglymostoma cirratus rapidly increase ontogenetically to values well above this optimal level. Similar heights

trends

are

also

observed

in a comparison of actual keel

to the corresponding theoretical optimal values (figure 28). At

voluntary

swimming

maintain optimal

scales value

speeds, all of the species which were examined here

whose of

8

keels (again

are

noticably smaller than the proposed

expressed in terms of the law of the Wall

coordinates). Moreover, keel heights closely approach the optimal values predicted cuvieri,

for ~.

cirratum and

Lastly, scale

levels.

additional

relief

relative

burst swimming speeds in all of these species, except G.

is

dimensions

taurus.

insight

available

closeness Whereas

2.

of

both

into

through

the hydrodynamic significance of interspecific

comparisons of the

keel morphometrics to these theoretical optimal C.

falciformis

and

C.

signatus maintain keel

suprisingly close to those predicted for burst values, quite

89

Figure 27.

Scale ridge spacing compared to predicted optimal

dimensions for sustained (A - A') and burst (B - B') swimming speeds as a function of fish length.

Species are as follows:

(1) Galeocerdo cuvieri, (2) Odontaspis taurus, (3) Carcharhinus plumbeus, (4) Prionace glaucs, (5) Carcharhinus obscurus, (6) Carcharhinus signatus, (7) Carcharhinus falciformis.

90

morphometrics intermediate deviation burst

observed

is

opposite

the

for

C.

these

scale

swimming

G.

obscurus,

between

in

on

C.

two

topography

speeds

may

cuvieri

and

O.

taurus.

plumbeus

and

P.

glauca

extremes. from

be

The

explanation

Scale appear

for this

optimal conditions predicted for

partially

found through interspecific

comparisons of swimming speeds. In

conclusion,

study drag

exhibit

a

reduction

falciformis, mokarran, optimal

keel

majority

the

signatus, C. limbatus,

values

exhibit

between

values. While the majority of the species, including C.

possess

O.

keel morphometrics of species examined in this

wide range of values with respect to proposed optimal

C.

species,

the

scales

!.

oxyrinchus,

~.

lewini and S.

whose keel heights and spacings approach the

predicted for burst swimming speeds, at least two other

taurus and G. cuvieri, appear not to follow this trend and

of

heights

and

spacings

well

above

such levels over the

their size range. Such differences may reflect the balance

thicker,

thinner,

narrower scales adaptive for protection functions and

more

specifically

sculptured

scales

adaptive for drag

reduction.

The

presence

of

either

scale

type

should, in part, reflect the

overall

speeds of each species. While this assumption is again hampered

by

absence of actual measurements, generalizations can be inferred

from and

the

natural history information such as that found in works by Bigelow Schroeder

others.

Of

suggesting

(1948), Castro (1982), Clark and von Schmidtt (1965) and

those

species which possess scales with keel morphometrics

optimal drag reduction capabilities, there is ample evidence

92

Figure 28.

Scale ridge height compared to predicted optimal dimensions for

sustained (A - A') and burst (B - B') swimming speeds as a function of fish length.

Species are as follows:

(1) Galeocerdo cuvieri, (2)

Odontaspis taurus, (3) Carcharhinus plumbeus, (4) Prionace glauca, (5) Carcharhinus obscurus, (6) Carcharhinus signatus, (7) Carcharhinus falciformis.

93

A

--

--

250

--

--

---

A'

200 en

c: 0

~

u

-E

~

+=:>

150

.&:.

at

CI)

100

:::I:

50

4

_ _ _ __ __ __ 6 8~~~~==~~======~~~~---------------=~5=

--===~.-,-....;;;;-;;...=:...:=-=

- - - - - - - - - - - - - - - - - - - - - - - - - - __ J __ _

~

8'

o

1.5

2.0

2.5

Total Length (m)

3.0

to

indicate

generally

high swimming speeds. Carcharhinus signatus, C.

falciformis

and

I.

al.,

and

Strasburg,

1982;

adaptations predator

which

in

variously

oxyrinchus are epipelagic (Castro, 1983; Raschi et

are

1958)

and exhibit a variety of structural

necessary for the increased speed required by a

such an environment, including a conical or pointed snout,

reduced

fins

and,

in

the last species, a lunate tail with

lateral keels on the caudal peduncle. Furthermore, the prey consummed by including

sharks,

these

falciformis

(Bane,

exocoetids

for

and

sharks

other

1966),

C.

swimmers

whose

addition,

both

and

small

tuna

(Thunnus)

for

C.

squid

and

a variety of teleosts including

signatus (Raschi, et al., 1982) and swordfish, tuna for

I. oxyrinchus (Randall, 1963), are fast, active

capture

!.

squid

would

require

oxyrinchus and

E.

higher

swimming

speeds.

In

limbatus, exhibit jumping behavior

(Garrick and Schultz, 1963; Springer, 1963). Finally, the two species of hammerheads

examined,

morphologies reduction. argument

matching This

as

particularly

a fast

lewini

those

and S. mokarran, possess scales with

leading

to

the

proposed

optimal

drag

is particularly interesting in light of the occasional

presented

functions

S.

that

the

hydroplaning and

lateral device

expansion for

what

of the sphyrnid head many consider to be a

agile group of sharks (see arguments in Budker,

1971). In

contrast,

sluggish.

both

Odontaspis

waters.

Whereas

teleost

and

its

G.

cuvieri

and

o.

taurus

probably are more

taurus normally is found in very shallow, coastal stomach

elasmobranch

contents

fish,

include a wide variety of both

it also feeds on a variety of benthic

invertebrates and carrion (unpublished VIMS longline data). This species

95

tends

to be very heavy bodied, with relatively large fins. Furthermore,

O. taurus has been observed swallowing air and remaining motionless near

the

bottom

(Bass

considered

a

(Randall, hunger

sluggish

(Castro,

species,

1982).

however,

observation consists

that

of

often swimming somewhat indifferently

certainly

Overall

as

the

suggested bird

swimming by

fraction

speeds

Dodrill in

may

and

this

be

less

Gilmore's

than (1978)

species' diet actually

dead or moribund individuals. Galeocerdo cuvieri occurs in

oceanic

and

Ballard, 1972). Galeocerdo cuvieri must also be

1963), although it may become quite active when stimulated by

estimated

both

and

and

shallower

coastal

waters.

While

stomach contents

include a wide variety of more active teleosts, elasmobranchs

even cetaceans, a significant fraction of its diet includes garbage (Gudger,

carrion

and

invertebrates

and

sea

1949),

1948, turtles.

as

well

as

slower

benthic

Like the previous species, it also is

relatively heavy-bodied. Additional examples of this trend can be found in those species with intermediate of

£.

scale

characteristics. The more heavily sculptured scales

leucas, for example, reflect both its relatively sluggish behavior

(Randall, species

1963) often

plumbeus

is

as

well

entering also

as its shallower, benthic distribution, this shallow

estuaries

and

rivers.

Carcharhinus

generally slower swimming, as suggested by the large

numbers of crustacea and mollusks in its diet, and its normal habitat of shallow, which

waters. In contrast, it sibling species,

£.

obscurus,

is semipelagic and seems to include a larger proportion of active

teleosts much

coastal

less

in

its diet, appears to be a more active species and exhibits heavily

sculptured scales. Finally, P. glauca appears to be

96

something 1958)

of

and

an

exception.

physically

is

This species is truly pelagic (Strasburg,

very streamlined, with long pectoral fins, a

long, pointed snout and a relatively thin body, all suggesting that this species

is

cephalopods example the

a

very active swimmer. Furthermore, it frequently feeds on

(Clarke

Tricas,

scales

and

1979).

should

Stevens,

1974)

and faster teleosts (see for

Therefore, it might be expected that ridges on

be somewhat lower and more closely spaced than they

actually are on the larger individuals. The

values

average

reported

values.

morphometrics Furthermore, values

in

which

keel

scales

heights allow

might

more

role

and and

both keel heights and spacings are

then,

has a range of values for the keel

function

lateral

over

a

wider

range

of speeds.

values

(Table

V)

might

Comparing Tables IV and V, those species whose

the most rapid growth rates, such as ~.

~.

falciformis,

~.

glauca, also exhibit the greatest reduction in lateral

spacings

therefore,

function in a

for those species with significant rates of increase

morphometrics. exhibit

obscurus

scale

for

the reduction in the heights and spacings from the primary

through

compensatory

Each

here

for

when compared with the primary values. This will some

portion

of

the

scale

to

exhibit

more

appropriate values even while the overall dimensions increase rapidly. In in

conclusion, it appears that the majority of the species examined

this

scales at

with

dimensions which should promote significant drag reduction

estimated burst speeds. Different scale morphologies in the last two

species such

study, with the exceptions of O.taurus and G. cuvieri, possess

as

may

be

associated

protection.

with adaptations other than hydrodynamics,

The remaining species (C. leucas, C. obscurus, C.

97

Table

v.

Reduction in the secondary and tertiary keel spacing and

heights (expressed in percentages) as compared with primary values.

These

values are rounded to the nearest whole percentage and represent the average and range (in parentheses). Keel Spacing

Species 2

0

c.

p1umbeus

19 (6-31)

c.

signatus

20 (7-37)

Keel Height 3

0

46 (35-59)

2

0

3

0

11 (+33-40)

46 (7-75)

17 (0-36)

43 (25-61)

18 (17-40)

48 (25-80)

21 (0-50)

51 (25-75)

R. terraenovae

22 (14-32)

c.

fa1ciformis

24 (9-39)

c.

obscurus

30 (13-45)

33

58

P. glauca

39 (34-43)

20 (21-54)

83 (81-85)

M. canis

18 (0-42)

36 (13-71)

61 (43-82)

32 (23-41)

25 (8-39)

o. taurus

57 (29-91)

G. cuvieri

78 (29-95)

98

plumbeus, scale

G.

cirratum and P. glauca) vary in the agreement of observed

dimensions to predicted optimal values. This variability probably

reflects

the

differences

in

overall

behavioral differences.

99

swimming

speeds

suggested

by

FUTURE STUDIES While are

the data presented here strongly suggests that placoid scales

capable

shark

species,

enhance scale

this

providing several

picture.

morphologies

values. from

of

While

natural

The

drag reduction for a number of

lines

of

research

could greatly

most troublesome point in evaluating these from

the paucity of reliable swimming speed

was circumvented to some extent through inferences

history information, an understanding of overall swimming

budgets,

speed

additional

arose

this

significant

measured

for

extended

periods

of

time,

would

be

invaluable. Such work is now possible using radio telemetry in the field (for

example,

feasible types

of

for

see

Sciarrotta and Nelson, 1977) and would certainly be

most

of the species included in this report. "Flowmeter"

equipment

could

potentially provide actual speeds, avoiding

many of the problems inherent in long term tagging studies. Secondly, extremes

in

material

for

oxyrinchus

an

examination

swimming

speeds

of

additional

should

species characterized by

be highly recommended. While the

an evaluation of a more complete series of scales from I.

and

c.

limbatus has recently become available, the inclusion

of additional "fast" species, in particular many of the lamnids would be particularly sedentary

interesting.

species,

Similarly,

more

scales

from

additional

such as the orectolobids, would provide information

on non-drag related scales. Finally, hydrodynamics

a

reevaluation may

be

of

the

fossil record, in light of scale

particularly fruitful (Schaeffer, 1967). While a

large amount of information is currently available regarding the overall

100

shape

of

individual

measurements Many

of

required

these

scales,

from

scales for

fossil

species,

the

adequate

hydrodynamic comparisons are still lacking.

such

as

those

found on members of the genus

Orodus, appear appropriately shaped and arranged (Zangerl, 1968) despite their cyclomorial nature and may provide a suitable starting point.

101

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and C. Patterson (eds.). Academic Press, New York • • 1979. Carcharhinoid sharks: morphology, systematics and phylogeny. PhD Thesis, Stanford University. Daniel,

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Elasmobranch Fishes. University of California

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E.W.

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The tiger shark, Galeocerdo tigrinus, on the North and

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Florida,

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habits. Copeia 1: 39-47. Heiald, E.S. and W.E. Ripley. 1951. The relative abundance of sharks and bat stingrays in San Francisco Bay. Calif. Fish Game 37: 315-329.

104

Mundy,

P.R.

1981.

Drag

reduction support activity. Final Report. Old

Dominion University Research Foundation 1-10. Nikolsky,G.V. 1978. The Ecology of Fishes. (Trans. by L. Birkett) T.F.H. Publications, Neptune City, N.J. Poll,

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1951. Poissons. Exped. Oceanogr. BeIge Eaux cotieres Afr. Sud

(1948-1949). Result. Sci. 4/1. Radcliffe,

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The

Bull. U.S. Bur. Fish. 1917.

sharks and rays of Beaufort, North Carolina. 34~239-284.

Notes on the taxonomic value of dermal denticles and teeth

in identifiying sharks. Copeia 1917: 25-28. Randall, J.E. 1963. Dangerous sharks of the western Atlantic. In: Sharks and Survival. P.W. Gilbert (ed.) D.C. Heath and Co. Boston, Mass. Raschi,

W., J.A. Musick and L.J.V. Compagno 1982. Hypoprion bigelowi, a

s~nonym

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Carcharhinus

signatus (Pisces: Carcharhinidae), with a

description of ontogenetic heterodonty in this species and

notes on

its natural history. Copeia 1: 102-109. Reif

1974.

W. E.

Morphogenese

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Hautzahnchen-Skelettes von Heterodontus. Lethaia 7: 25-42 • • 1980. A model of morphogenetic processes in the dermal skeleton of elasmobranchs. N. Jb. Geol. Palaont. Abh. 159: 339-359. 1982.

Morphogenesis and function of the squamation in sharks. I.

Comparative

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sharks. N. Jb. Geol. Palaont. Abh. 164: 172-175. and

Dinkelacker

1982.

Hydrodynamics

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swimming sharks. N. Jb. Geol. Palaont. 164: 184-187. Robins,

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L.P.

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S.G. Hershkowitz 1937. Placoid scale types and their

distribution in Squalus acanthias. Biol. Bull. 78: 51-66. Schaeffer,

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Sharks,

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Comments

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Skates and Rays. P.W. Gilbert, R.F. Mathewson and D.P. Rall

(eds.). The Johns Hopkins Press. Baltimore, Maryland. Sciarrotta,

T.C. and D.R. Nelson 1977. Diel behavior of the blue shark,

Prionace glauca, near Santa Catalina Island, California. Fish. Bull. 75: 519-528. Snedecor,

G.W.

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Cochran 1967. Statistical Methods. The Iowa

State University Press, Ames, Iowa.

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Distribution,

abundance, and habits of pelagic

sharks in the central Pacific Ocean. Fish. Bull. 138/38. Tricas, T.C. 1979. Relationships of the blue shark, Prionace glauca, and its prey species near Santa Catalina Island, California. Fish. Bull. 77: 175-182. Thorson,

T.B.

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Movement

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Sea and Lake Nicaragua demonstrated by taggiong.

Copeia 2: 336-338. Walsh, with

M.J. and L.M. Weinstein 1978. Drag and heat transfer on surfaces small

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106

Paper No. 78-1161, AIAA 11th

Fluid and Plasma Dynamics Conference, Seattle, WA. Walters,

V.

1962.

Body form and swimming performance in the scombroid

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C.S.

1975.

Limit

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P.W.

1975. Hydodynamics and energetics of fish propulsion. Bull.

Fish. Res. Board Can. 190: 1-159. Weihs,

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p. 333-338. In: Scale Effects in Animal Locomotion. T.J.

Pedley (ed.). Academic Press. New York, N.Y. 1981.

Voluntary

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carcharhinid sharks. Copeia 1: 219-222. White,

E.G. 1937. Interrelationships of the elasmobranchs with a key to

the order Galea. Bull. Amer. Mus. Nat. Hist. 74: 25-138. Zangerl, scales

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The morphology and the developmental history of the Paleozoic sharks Holmesella

Symposium 4: 399-412.

107

and Orodus. Nobel

Appendix I.

Species

Carcharhinus falciformis

Collection data for the material examined

Specimen number

Total length (em)

103 111 115 189 268 169 201 215 278 148 150 157 167 173 86* 96 104 108

1 2

Carcharhinus leucas

Carcharhinus limbatus

3 4 5 6 7 8 9 10 11 12 13

Carcharhinus obscurus

Carcharhinus plumbeus

14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 27 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45

III

119 120 123 127 168 173 182 196 218 238 329 334 59 62 67 73 80 88 94 99 102 106 115 117 125 127

108

Sex

M M F F F F M M F M M M M M F F F F F F M F

M M F F M F F F F M F M

M F F M M M M F F F F

Latitude

Longitude

Not 37°03' 37°03' 37°03' Not 37°17' 37°17 ' Not Not 37°17'37°17' 36°54' 36°55 ' 37°17' 36°54' 36°55' 36°54' 37°00' 37°05' 36°55' 36°55 ' 36°54 ' 36°54' 37°00' 36°55' 37°00' 36°55 ' 37°00' Not 36°54 ' 36°54' 37°17' 37°17 ' 36°56 ' 37°05' 37°17' 37°05' 36°54' 37°05 ' 36°54' 37°05' 37°05' 37°05' 37°05' 36°54'

available 74°37' 74°37' 74°37' available 75°46' 75°46' available available 75°46 ' 75°46' 75°59' 75°42' 75°46' 75°59' 75°42' 75°59' 75°21' 75°55' 75°42' 75°42' 75°59' 75°59' 75°21' 75°42' 75°21' 73°42' 75°21 ' available 75°59' 75°59' 75°46 ' 75°46' 76°01' 76°08' 75°46' 75°55' 75°59' 76°08' 75°59' 76°08' 76°08' 75°55' 75°55' 75°59'

Species

Specimen number

Carcharhinus plumbeus (cont.imued)

46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 75 76

Carcharhinus signatus

Galeocerdo cuvieri

77

Ginglymostoma cirratum Isurus oxyrinchus Mustelus canis

78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96

Total length (cm)

132 136 145 146 152 158 161 167 173 178 185 188 191 196 207 216 76 94 179 192 211 215 217 222 156 173 188 213 217 223 238 252 258 271 292 404 72

77 132 163 182 37 52 56 61 93 101 109 113 116 127

109

Sex

Latitude

F F

37°00 ' 37°05' 36°54' 36°55' 37°00' 36°55' 37°00' 37°00' 36°55' 37°00 ' 37°00 ' 36°55' 37°00' 36°55 ' 37°00' 37°05'

M F F F F

M F F F F F F F F

M F F

M M M M M M F F

M M F

M F F F F F F

M M F F

M M M F

M M F F F F

Longitude

75°21' 76°08' 75°59' 75°42' 75°21' 75°42' 75°21' 75°21' 75°42' 75°21' 75°21' 75°42' 75°21' 75°42' 75°21' 76°08'

Not available Not available Abidj an "Reine Pokon" 38°54'

73°25'

Not available Not available Not available 38°54' 37°03' 37°07' 36°55' 37°00' 37°03' 36°55' 37°03'

73°25' 74°37' 75°41' 75°42' 75°21' 74°37' 75°42' 74°37'

Not available 36°54' 37°00' 36°55' 36°54'

75°59' 75°21' 75°42' 75°59'

Aquarium specimen Aquarium specimen 37°03'

74°37'

Not available 37°03' 37°07' 36°54'

74°37' 75°41' 75°59'

Not available 37°17' 37°00' 37°00' 37°07' 37°07' 36°55' 37°07'

75°46' 75°21' 75°21' 75°41' 75°41' 75°42' 75°41'

Species

Odontaspis taurus

Prionace ga1uca

Rhizoprionodon terraenovae

Sphyma 1ewini Sphyma mokarran

Specimen number

Total length (cm)

97 98 99 100 101 102 103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 119 120 121 122 123 124 125 126 127 128 129

165 194 204 210 224 229 231 235 247 34* 39* 42* 46* 165 181 190 202 214 228 248 287 348 40 83 98 95 97 101 106 54 221 225 252

*embryo

110

Sex

latitude

F

37°17' 37°17' 37°17' 37°05' 37°05' 37°05' 37°17' 37°00' 37°00'

M F F M M F M M M F F F M M M F M F M F F M M F F F F F F M M M

Longitude

75°46 ' 75°46 ' 75°46 I 76°08 ' 76°08' 76°08' 75° 46' 75°21 ' 75°21 ' Bermuda Bermuda Bermuda Bermuda

37°03' 37°03"' 37°03' 37°03' 37°03' 37°03' 37°03' 37°03' 37°03' Not Not 37°00' 37°05 ' 37°05' 37°05' 36°55 ' Not Not 37°00' Not

74°37' 74°37' 74°37' 74°37' 74°37' 74°37' 74°37' 74°37' 74°37' available available 75°21 ' 75°55' 75°55' 75°55' 75°42' available available 75°21 ' available

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1. Report No.

12. Government Accession No.

3. Recipient's Catalog No.

NASA CR-3963 4. Title and Subtitle

5. Report Date

March 1986 Hydrodynamic Aspects of Shark Scales

6. Performing Organization Code

7. Author(s)

8. Performing Organization Report No.

William G. Raschi and John A. Musick 10. Work Unit No.

9. Performing Organization Name and Address

Virginia Institute of Marine Science

I College of William and Mary

11. Contract or Grant No.

Gloucester Point, VA 23062

NASl-16042 13. Type of Report and Period Covered

12. Sponsorin" Agency Name and Address

National Aeronautics and Space Administration Washington, DC 20546

Contractor Report 1982-83 14. Sponsoring Agency Code

505-31-13

15. Supplementary Notes

Langley Technical Monitor: Michael J. Walsh William G. Raschi: Bucknell University, Lewisburg, Pennsylvania. John A. Musick: Virginia Institute of Marine Science, The College of William and Mary, Gloucester Point, Virginia. 16. Abstract

Ridge morphometries on placoid scales from 12 galeoid shark species were examined in order to evaluate their potential value for frictional drag reduction. The geometry of the shark scales is similar to longitudinal grooved surfaces (riblets) that have been previously shown to give 8 percent ski n-fri cti on reduction for turbul ent boundary 1ayers. The present study of the shark scales was undertaken to determine if the physical dimensions of the ridges on the shark scales are of the right magnitude to be used by the sharks for drag reduction based on the previous riblet work. The results indicate that the ridge heights and spacings are normally maintained between the predicted optimal values proposed for voluntary and burst swimming speeds throughout the individual's ontogeny. Moreover, the species which might be considered to be the "faster" possess smaller and more closely spaced ridges that based on the riblet work would suggest a greater frictional drag reduction value at the high swimming speeds, as compared to their more sluggish counterparts.

17. Key Words (Suggested by Authors(s))

Boundary layer Drag reduction

I

18. Distribution Statement

Unclassified - Unlimited Subject Category 34

19. Security Classif.(of this report)

Unclassified

/20. Security Classif.(of this page)

Unclassified

/21. No. of Pages 122. Price

116

A06

For sale by the National Technical Information Service, Springfield, Virginia 22161

NASA-Langley, 1986