98 G.G.
SCOTT &
K.CRICHARDSON
B
A
cFIGURE
3. Cranial view oftheleft humerus in (A)L
latifrons and (B) V. ursinus. Where a, teres tuberosity;
b, deltoid tuberosity;c, medial epicondyle;d, lateral epi-
condyloid crest. Scale line is 2 cm.
B
FIGURE
5. Craniomedial viewof the left radius in (A)V. ursinus and(B)L. latifrons. Where a, neck; b, radial tuberosity;c,arrowed,styloid process. Scalelineis2 cm.
B
FIGURE
4. Lateralviewoftheleft ulnain(A) V. ursinus and (B) L, latifrons.Where
a, olecranon; h, arrowed, coronoidprocess; c.arrowed,pit For Ihe radial tuberosity;d, styloid process. Scale line is 2cm.
Humerus
L. latifrons Deltoid acutely angled tuberosity ridge
Teres tuberosity small
Lateral epi- straight caudal shallowly condyloid crest border convex proxi-
mally, concave distallv
V. ursinus shallow angled ridge
elongate
Ulna Anconeal
process(i) crantoproxi
mal
surface(ii) viewed
laterally
Coronoid
process Shaft(i) Depression for radial tuberosity
(ii) Lateral surface
L, latifrons
K
ursinusridge large process
cranial surface sickle-shaped parallel to
caudal surface
elongated circular
shallow larger circular pit
Hat proximally, concave
and
concavedistally
,*?,?•?*
Proximal view of^ft radial carpal bone in(A)
L
latifronsand(B) V.ursinus. Wherea,radialsurface- b. palmar tuberosity; c, medial tubercle. Proximal view ofright ulnar carpal bone in(C)L. latifronsand(D) Vursinus. Whered, palmartuberosity;eTulnarsurface.Scale line is 5
mm.
Radius
Neck
L. latifrons V. ursinus shallow con- deeply concave cavity proximal
to radial tuberosity
Shaft
Lateral surface flat
Distalforelimb Radial carpal bone:
deep oblique depression
Palmar
tuberosityA. latifrons
small
Medial tubercle small
and
taperedV. ursinus large
massive
and
bluntUlnar carpal hone; Third carpal bone:
L. latifrons V. ursinus
L
latifrons V. ursinus Mediodistal largeand
broadand
Ulnar articular small
and
oval large, concave process pointed squatfacet
and
semi- shallow deepcircular Proximal sulcu3
Accessory car- small pal articular
facet
circular with
pronounced
lateral tubercle
Fourth carpal bone:
L, latifrons
Palmar
artic- smalland
V. ursinus large arid deep
Palmar
facetelongate for 3rd
and
4th carpalcircular
ular facet for 4th
and
5th metacarpalsshallow
bones
Hamulus narrow
broad at itsAccessory carpal bone: base
L. latifrons Ulnar carpal lateral border articular facet short
and
square
V. ursinus lateral border elongate
Body
of ulnar shallow fossa carpal separatedfrom
hamulus
by-
deep fossa
Medial prox- imal tubercle Shaft
small
pronounced
broad
and
Hat constricted inmiddle
B
No
consistent gross morphological differenceswere found forthe first carpalbone,second carpal bone, metacarpals or phalanges.Pelvis
L. latifrons V. ursinus Iliac crest (i) points points caudally
laterally
and
'sickle-shaped' forms sharpangle with
body
of ilium pointed
(ii) lateral extremity broad
Iliac fossa present absent
lliopectineal large small
eminence
Ramus
ofsame
width as half width of pubicbone
pubicbone
bet- pubicbone
bet\y
FIGURE
7. Proximal view oftheright accessory carpal bone in (A) L. latifrons and (B) V. ursinus. Where a, proximal face! for the ulnar carpal bone; b, constricted shaft. Medioproximal viewof theright 3rd carpal bonein (C)Li latifrons and (D) V, ursinus.
Where
c, medial process; d,sulcus;e,articular surfacefor3rd metacarpal.Proximal view of the right 4th carpal bone in (£) A.
latifronsand(F) V.ursinus. Wheref, hamulus;g, articular facet forulnar earpa)bone; h» fossa.Scale lineis4
mm.
ween
the obtur-ween
the obtur- ator foramina ator foramina Rectus femorisdeep
fossaon
indistinctm.
originbody
of ilium Surface area of approximately Ischiatic tablesame
as obtur-ator
foramen
Ischiatic tuberosity
narrow, approximately 20
mm
wide at point of maxi-mum
widthmuch
smallerwell-developed, approximately
40 mm
widetoo G.G.
SCOTT &
K.C.RICHARDSON
;•::::::; '
v.v
o 3
i^% *
*
FIGURE
8- Ventralviewofthe pelvisin(A)L
latifronsantl(B) V.ursinus. Wherea,iliaccrest;b,arrowed,iliopeetineal eminence; c, arrowed, pecten; d, obturator foramen; c, acetabulum; f, ischiatic table; g, ischiatic tuberosity. Scale line is 2 cm.M
i.
^^hEbmSP
FIGURE
9.Dorsalviewofrightepipubicbonein (A)L.futifronsand (B) V. ursinus. Where a, articularsurface forpecten ofpubis;b.arrowed, proximaltubercle; c,shaft.
Scale line is 2 cm.
FIGURE
10. Cranial viewofleft femurin(A)/.. latifrons and(B) V. ursinus. Wherea,head; b, greatertrochanter;c,3rd trochanter;d»lessertrochanter;e, medialcondyle.
Scale line is 2cm.
Epipubic
bone Femur
Articular sur- face for pectin o( pubic
bone
L. latifrons elongate with medial surface
much
broaderV. ursinus
narrow
elongate with parallel sidesGreater trochanter
L. latifrons deeply grooved
V. ursinus indistinct groove than lateral
surface
Lesser trochanter
present
pronounced
Proximal ven- concave Hal
tral surface
Lateral tubercle indistinct
pronounced
Third trochanter
pronounced
presentB
—
aFIGURE
II.Lateral view ofleft tibia in (A) /.. lutifrons and(B) t ur&inus. Wherea,arrowed,medialintercondylar eminence: b. arrowed, articular surface For fibula. Scale line is 2 cm.Tibia
Medial inter-
eondylar
L'lJlillCllCC
/.,
Uuifmns same
size as lateralLateral condyle
(i) lateral almost flat
surface
(ii) articular circulai surface for
lateral condyle of femur
V. ursinus latgei Ihaii lateral
angled elongate
Fihuta Malleolus (plantar view)
/.. lutifrons
K
ursttmsrounded, square medial surfaces
Distal hindlitnh
Tarsal
bone morphology
variedconsiderably within each genus.No
diagnostic differences were found between the twowombat
genera for the tibiolarsal, fibulartarsal, centraltarsal bones, or for 1st, 2nd, 3rdand
4th tarsal bones.No
morphologicaldiffer- ences were observed for the metatarsalsand
phalanges.Distt SSION
This Study found that a
number
ofthemorphea
logical features claimed by
Murie
(1867) as being diagnostieally significant forseparating the fore-limbboneso(L.
Uuifmns
from those of \. ursinub are not reliable. For instance Murie's claim ihai amarked
differenceexists between the proportion of lengthtobreadth ofthescapulaoftheiwowombat
taxa
(56%
in L. lutifronsand
72'Vo in V. ursinus) was found to bemarginal.Other
differences such as scapula shapeand
curvature of the scapularspine,as well asthe varialions indepthof(hesulcus forthebicipital lendonasdescribed by
Murie
(1867) werefound to be inconsistentand
ofno
diagnostic- value.Likewise
Murie
(1X67)claimed that the anterior border of the ilium pointsdownwards
in I.lutifrons, but outwards in
K
ursinus,and
that the femoral shaftbreadth isgreatest inL
lutifrons.He
also reported thai the fibula length
was
equal inboth
wombat
genera,and
that the fibula shaft Wfiflstraighler inL. tatifrons.
None
o\ these findings art supported in this study.The
current study tabulates anumber
ofdiag- nostic morphological differences allowingmany
individual
wombat
bones ofthe appendicularskele- tonto be identified to generic level. In addition to this it was noted that thescapula of I' ursinus bears a larger surface area for the insertion ofM,
trapezius
and M.
deltoidius than does the scapula of L, tatifrons. However, theL
laiifrons scapulapossesses a larger
and more
developed surface loi(he insertion of
M. rhomboideus and M,
serratus ventralis.The
significance Of this difference in muscle insertion sites is reflected not only in differences in the overall structural mechanics of the thoraciclimbof
the twowombat
taxa, but alsoin differences in their burrowing
and locomotor
behaviour.For example,
R
ursinusmore
readilyaccommo-
dates the actionsofthe trapezius muscleto elevate
and
protract thelimband
the dcltoideus muscleto flex the shoulderjoint as well as tolift thehumerus,By
contrast L. lutifrons ismore
adapted toaccom- modate
the action ofrhomboideus
musclewhich
elevates
and
retracts the limband
shoulder,The
ventral serrate muscle supports the trunk,
and
carries the trunk forward or backward. These features are probably linked to L. tatifrons being a plains dweller
which
digs burrows into a flat,usuallylimestone-underlaid, topography; while
K
ursinus is an inhabitant of the
mountainous
eucalyptus forests,and commonly
resorts todiggingits burrows into
decomposed
granite.The
bones oftheforearm inbothgenera are well adapted for pronationand
supination, both impor- tant prerequisites for their burrowing. Il *9 also evident, that except for relative size, the general overall morphological structureoT
the forelimb skeleton in thewombat
is guile similar tothoseof thekangaroo and
the koala.Ultimately, differences in forelimb osteology of L. tatifrons
and
I ursinus can he explained by reference to differences in theirmyology and
structural mechanics.
Sonntag
(1923),and more
recently Hildebrand(1974) have set the lead in this respect. However, Sonntag only lookedat the
myo-
logy of V. ursinus* while Hildebrand only consid- ered thestructural mechanicsof
the forelimb ofL
laiifrons. In both cases their
work was
generalised102 GJG.
SCOTT & KjC RICHARDSON
and
did not attempt to explain the functionalanatomy
of thetwo wombat
genera.Of
all the hindlimb bones studied, the pelvisshows more
pertinent morphological differences between thetwo
extantwombat
species, However, relating these differences to the functionalanatomy
ofthe pelvis,and
the hindlimb in general, awaits comprehensive informationon
themusculatureof thehindlimb inthetwowombat
species.No
detailedwork
has beendone on wombat
hindlimb myology.Waterhouse
(1846), Macalister (1850),Sonntag
(1923),
and Elftman
(1929) provided only general informationon wombat
(V. ursinus) musculature.Their studies described the origins
and
insertions of a smallnumber
of muscle groups, but lacked detail, definitionsand
figures. Inmost
instances they areoflittlevalue for interpreting the functional musculoskeletalanatomy
ofthe pelvicregionofthe twowombats.
Although
this paper hascompared
the ost- eological differencesofthehindlimb ofL
latifronsand K
ursinus, the interpretation of these differ- ences in terms of their respective functional ana-tomy
awaitsadetailed investigationofthemyology
of the pelvic limb,ACKNOWl.fcUC.Mb.NTS
We
would like to lhankDr
C.P. Groves, Australian National University; DrT. Flannery, Australian Museum, DrD
Horton, Instituteof AboriginalStudies;JoanDixon, NationalMuseum
ofVictoria; DrR. Molnar, Queensland Museum; DrC. Kemper, South AustralianMuseum,
for making material available to us; and Dr D. Kitchener, WesternAustralianMuseum
forthespecimens usedinthe photographs. DrsC.P. Groves and D. Horton both gave valuable advice and support over the duration of the project.We
wishtothankMr
G.Griffiths forphotography andMs
D.Passmoreforsocarefullytypingthepaperandearlier drafts,Theprojectwasprimarilysupportedbyan Australian National Universitv Research Grant,
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DE
VIS, C.W. 1892. Remarks on post-tertiary Phaseo- lomyidae. Proc. Linn. Soc. N.S.tV, 6(2): 235-246.ELFTMAN,
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