New Australopithecus Femora from East Rudolf, Kenya
Alan Walker Department of Human Anatomy. University of Nairobi, Kenya
New fossil femora attributed to Arcstra1ofdhc.u-s from East Rudolf, Kenya, form the basis for a three-dimensional reconstruction of a compIete femur. The reconstruction and the known fossils are compared with the femora of Homo sapins. Although many of the features of the fossil bones fall within the overall ranges to be found in modern man, there seems, nevertheless, to be a distinctive total pattern in the femoral anatomy of Australopithcus. Biomechanical explanations for this pattern may be possible when other postcranial bones can be reconstructed with the same degree of certainty as the femur.
Received 26 October 1972
1. Introduction Until recently proximal remains.
our knowledge
of the femur of AustraZo@zecus has been limited
to either
or distal fragments from deposits yielding Australopithecus dental or cranial As yet no definite association of femoral and dental material has been shown, but
other associated parts from East Rudolf strongly suggest that the past and present assigning of nearly all the femoral fragments discussed here to Australopithecus species is probably correct. femoral
New material fragments,
from
East
Rudolf,
one of which comprises
Kenya
(Leakey,
197 1, 1972)
the distal end together
includes
four
with most of the shaft.
These new fossils give a much more complete idea of the size and morphological variability of this bone and also provide a sound basis for a complete reconstruction of one size of femur. In this account state
that
Australopithecus
specimens,
I am not involved motor
I shall be referring
to previous
I can find no real differences,
apart
descriptions
here with the question
as to whether
that all the Australopithecus
from one variable
and/or dimorphic
species through
similar
to attempt
proximal
time.
a composite
2. Femora from South than East Rudolf Three
of
this reflects merely similar loco-
or the possibility
is sufficiently
anatomy
whether referred to as A. africanus, A. robustus or any other species.
capabilities,
morphology
and must at the outset
from size, in the femoral
specimens
In any event,
description and East
pieces and two distal pieces have been recorded
proximal fragment is known from Olduvai Gorge in Tanzania. Sts 14. The proximal fragment from Sterkfontein is associated
are sampled the femoral
for Australopithecus. Africa
Elsewhere
from South Africa.
One
with a pelvis and partial
vertebral column. Broom & Robinson (1950) reported this bone as “rather badly crushed” and that “for the most part the surface of the bone is not well enough preserved to show satisfactorily the muscular ridges.” Dr C. K. Brain (in Day, 1969) is quoted as saying that the bone is badly crushed, the head extensively reconstructed and the surface of the bone damaged. My own observations confirm the essentially fragmentary nature of the specimen. The whole surface has the appearance of very many splinters of bone recemented by matrix. The “head” is almost totally comprised of plaster of Paris and fairly crudely Journal of Human Evolution (1973) 2, 545-555
546
A.
WALKER
reconstructed and it is not clear whether the neck length has been correctly gauged, although the acetabulum from the same side of the same individual gives a fair indication of head size. I could see no way of reasonably
estimating any measurements
or angles and,
short of gaining the impression that this is the smallest known femur of Australopithecus, very few useful points of comparison can be made. This is not to say that the sketch reconstruction
given by Broom
what it is, namely an attempt man.
& Robinson at comparing
is fanciful,
but that it should be taken for
the fossil fragment
with a femur of modern
SK 82. This is the proximal part of a right femur from Swartkrans and includes the head, neck, lesser trochanter and part of the shaft. It is much bigger than Sts 14 but again is reconstructed in part. Most of the greater trochanter is reconstructed and large cracks on the posterior
aspect of the shaft and lesser trochanter
have been filled with plaster.
The head is small and is just a little more than a hemisphere. flattened
anteroposteriorly
with a well-marked
robust and slightly platymeric divided into a smaller proximal SK 97. most
Much
The neck is long and
groove.
below the lesser trochanter. and larger distal fossa.
and
the shaft is cracked
details such as the double
and crushed
trochanteric
below
shaft is quite
trochanteric
fossa is
It is a little larger in the lesser trochanter.
fossa and the presence of an obtu-
rator groove are similar in the two specimens. Olduuai Hominid 20 (O.H. 20). Th is is part of the proximal lacking the head, part of the greater trochanter
The
The
the same parts are preserved in this as in SK 82.
dimensions
Morphological
obturator
portion
and lesser trochanter.
of the left femur, It is quite similar
in size and morphology to the two Swartkrans fragments (Day, 1969). 3s 34. This is the distal extremity of a right femur from Sterkfontein with the posterior part of the medial condyle
missing.
The maximum
bicondylar
width is 64.0 mm.
bone is relatively small compared the shaft relative measure
The
to the same part in modern man but the robusticity angle is difficult to the width is quite great. The condylofemoral
but estimates have ranged from “at least 7””
(Clark,
1947) to 15’ (Heiple
of to &
Lovejoy, 1971). The patellar groove is quite deep and the lateral lip is more strongly developed than the medial. The condylar contours show a flattening on their most distal parts.
The intercondylar
fossa has been considered
deep but falls in the range of modern
man. TM 1513. This is approximately the same part as preserved in Sts 34, but from the Some outer bone is missing from the left femur of another individual from Sterkfontein. suprapatellar
area and a large flake of bone is missing from the lateral epicondylar area. MLD 17. Half a femoral head from Makapansgat, noted and figured by Bone (1955), is roughly the right size to be from an Australopithecus femur, but it has a peculiar widened fovea and an oddly formed epiphyseal line. Identification of this fragment is uncertain, to say the least, and I consider it unwise to include this in the Australopithecus sample. 3. Femora
from
East
Rudolf,
Kenya
The following specimens have been recorded and described from the East Rudolf deposits (Leakey, 1971,1972; Leakey, Mungai &Walker, 1971, 1972; Leakey & Walker, 1973). KNM. ER. 738. This is the head, neck, lesser trochanter and part of the shaft of a left femur of small size. The head is small and nearly hemispherical, and the neck is long and The shaft is intact for some distance below the lesser anteroposteriorly compressed.
NEW
FEMORA
AUSTRALOPITHECUS
FROM
547
KENYA
trochanter but more distally it is split roughly sagittally and only the medial half preserved. On this distal part of the shaft there is clear evidence,
amplified
by skiagrams,
of a
the cortex fracture callus. The osteone arrangement on the surface is disorganized, strikingly thickened and the skiagram shows the typically “woven” appearance of the healed fracture. Because of this fracture and the possibility of compensatory remodelling of the neck region, it is perhaps unwise to take the morphology exactly typical. KNM. ER. 815.
This is the proximal
of this specimen
as being
part of a left femur with the neck, most of the The neck is long as judged by the distance
lesser trochanter and part of the shaft preserved.
to the epiphyseal line and strongly compressed anteroposteriorly. This compression is so strong that an inferior crest is developed where the anterior and posterior surfaces of the neck meet at an acute angle. The distal part of the lesser trochanter is preserved. This is directed at an angle of about 40’ to the axis of the neck when seen in superior view. The gluteal
tuberosity
posteromedial
is a low, roughened area and an hypotrochanteric fossa is present to it. The shaft is very platymeric as far as it is preserved and the medullary
cavity at the level of the distal fracture is surprisingly narrow. KNM. ER. 736. This is part of the shaft of a massive left femur. lesser trochanter
to about
the divergence
of the supracondylar
It extends from the
lines.
The shaft has a
gently convex anterior surface and is buttressed behind by a massive, trenchant femoral crest. The cortex in the region of the base of the neck is very thick as seen on the proximal fracture and in skiagrams. This specimen is the distal three-quarters of a right femur with the Some areas are affected by abrasion fracture just below the lesser trochanter. corrosion. These are the suprapatellar area, the distal part of the medial surface,
KNM. ER. 993. proximal and/or
the popliteal
surface and the condyles,
particularly
the lateral.
The shaft is moderately
robust and platymeric in its proximal part but pilaster development gives the bone a more nearly circular cross section in the midshaft region. The anterior surface is evenly convex but this changes to give relatively flat medial and lateral surfaces on either side of the pilaster. The shaft is bowed anteriorly to a moderately strong degree and the pilaster development
does not make the linea aspera straight in lateral profile as in KNM.
The area of the popliteal
ment of a ridge that divides it into medial and lateral portions. not much raised above
ER. 736.
surface is relatively small and gently convex due to the developthe level of the suprapatellar
The patellar groove is
area in the midline.
The lateral
margin is much more developed
than the medial and is essentially continuous with the ridge that forms the lateral surface of the suprapatellar area. The intercondylar fossa is deep and wide and impressions for the cruciate ligaments are as in modern man. The total epiphysis is wider mediolaterally than it is anteroposteriorly femorocondylar angle to the diaphysis.
4. Evidence
from
and is set at a marked
the Skiagrams
Only a preliminary study has yet been made of the skiagrams of the East Rudolf fossils. Two points are worth mentioning at this stage. One is that the cortical thicknesses of the shaft are very great and the other is that the cortex of the inferior part of the neck is thickened for a considerable distance medially. The radiation of trabeculae that fans out into the femoral
head and which is seen in the anteroposterior
view, begins where the
548
A. WALKER
neck cortex thins out about mid-way and neck as in modern
along the neck and not at the junction
of the shaft
man.
5. The Size Range in Australopithecus
Femora
There have been suggestions in the past that the post cranial bones of robust and gracile australopithecines show distinguishing features other than size. As the femoral evidence from South Africa stands, the gracile form is represented by one crushed and fragmentary specimen
and two distal pieces.
based on Broom’s on the specimen. no meaningful
The
differences
put forward
sketch of Sts 14 and on Broom Zihlman
(1971),
by Napier
& Robinson’s
tentative
(1964)
were
observations
noting the crushed nature of the specimen,
could find
differences between the Sterkfontein and Swartkrans femora.
Heiple & Lovejoy in a series of papers have convinced Broom’s reconstruction, that the differences are minimal. from deposits that have yielded
More recently themselves, while accepting The East Rudolf fossils come
many cranial and dental remains of Australopithecus
and
the situation there seems to have been made much simpler, in that only one sexually dimorphic
species seems to have been sampled
range in cranial
and dental
(Leakey,
1972).
Just as there is a wide size
parts, there is also a wide size range in the post cranial
material, including femora. After an examination of the South African post cranial fossils, I am myself convinced that there is as yet no clear evidence of any major differences in morphology
between
specimens
that could be called robust or gracile sampled from the
various sites. As far as size alone goes, the new East Rudolf the known femoral material in some, more or less accurate,
material
smallest to largest, the femoral fragments are : Sts 14; KNM. TM
1513;
particular
Sts 34 and SK 82; SK 97, O.H. 20 and KNM. interest is the close agreement
one from Sterkfontein
allows us to place
order of size. In order, from ER. 815;
ER. 993;
KNM.
KNM.
ER. 738;
ER. 736. Of
in overall femur size between Sts 34 and SK 82,
and the other from Swartkrans.
the shaft of proximal fragments. The maximum width of the distal epiphysis
Table
is as follows:
1 gives size indications TM
of
1513, 57.0 mm (est) ;
Sts 34,64-O mm and KNM. ER. 993,69-O mm (est). I realize, of course, that at least two femora of different size and on which upper and lower measurements can be taken are needed to place accurately any isolated proximal or distal part in its size order, but KNM.
ER. 993 does allow a strong impression to be gained, for the first time, of upper and
lower sizes, and the size order given here is unlikely to be substantially
Table
Diameters
1
of shaft
Anteroposterior diameter (AP) Specimen Sts 14 KNM. ER. KNM. ER. SK 82 SK 97 O.H. 20 KNM. ER. KNM. ER.
(mm) 815 738
993 736
just
below
Mediolateral diameter (ML) (mm)
Not measurable but very small 18.3 26.2 22.5 26.5 25.0 30.0 24.2 33.3 26-O 33.0 25-5 32.4 30.0 40.0
the lesser
AP+ML 2 (mm) 22.25 24.50 27.50 28-75 29.50 28-95 35.00
incorrect.
In any
trocbanter
Platymeric Index AP x 100 ML
69.84 84.90 83.33 72.67 78.78 78-70 75.00
NEW
549
PEMORA FROM KENYA
AUSTRALOPITHECUS
event, the evidence indicates that femora of the same size are likely to be found at Sterkfontein and Swartkrans. 6. A Reconstructed
Femur of Australopithecus
An attempt
has been made to model a complete femur based mainly on East African KNM. ER. 993 provides the specimens. Figure 1 gives four views of this reconstruction. basis for the reconstruction, with other East Rudolf specimens and O.H. 20 giving the of the abraded condylar guide lines for the trochanters, head and neck. Remodelling surfaces was attempted ligament
using the remaining
morphological
pit) and skiagrams as well as following
points (e.g. fibular collateral
the contours of the remaining
patches of
outer bone. I must admit, however, that memories of the two Sterkfontein distal fragments must inevitably have led my hand during this part of the reconstruction. The total length of the reconstruction (Martin & Sailer, No. 2) is 360-O mm. In anterior view the shaft is stout and straight and the proximal platymeria and the supracondylar The neck is long and set at a low angle expansion distally give it a waisted appearance. to the shaft.
The head is small and not much more than hemispherical,
rather than the
Figure 1. (a), Anterior, (b), posterior, (c), medial and (d), lateral views of reconstructed femur of Austrdofiopithecus. The total length (head to medial condyle) is 360 mm.
550
A.
usual human
condition
does not project modern man. are placed tubercle
WALKER
where it is about
far proximally,
The femorocondylar
on a horizontal.
merging
two-thirds
of a sphere.
The greater
nor is it flared from the lateral
The
into the lateral
trochanter
side of the shaft as in
angle gives a strong valgus position when the condyles patellar ridge
groove
is wide with a well-developed
that borders
the depressed
The groove is not much raised above the suprapatellar aspera is short and the hypotrochanteric
area.
lateral
suprapatellar
In posterior
area.
view the linea
fossa is placed quite distally with a low tuberosity.
The lesser trochanter is placed rather medially on the shaft, even allowing for minor neck anteversion, and a distinct ridge, probably associated with the iliacus portion of m. iZz$soas runs laterally The intercondylar In lateral strong
to join
the medial proximal
expansion
fossa is wide and the popliteal
and medial
pilaster.
The
surface
views the shaft is anteriorly
lateral
condyle
of the linea aspera below it.
convex.
bowed and buttressed
has a flatter
curvature
than
behind
the medial,
by a
but the
posterior part of the lateral condyle has a smaller radius of curvature than that of the medial. The fovea is situated posterior to the coronal equator of the head. In superior view the neck is strongly compressed at an angle of about into a proximal condylar lateral
anteroposteriorly
smaller
pit and a distal much
deeper
fossa is deep and wide and the patellar tubercle
and the lesser trochanter
40” to the long axis of the neck.
more strongly
fossa is divided
one.
view the inter-
it must be remembered
specimens,
Martin
value
& Saller
of about
(1957)
12.0.
the robusticity
The
and Previous
is of a femur
mean
index (of Martin
is 15.36,
that would be
human
femora,
within
and Saller)
(but shows
where the index usually
for H. safiiens neanderthalensis is given
as 13.5 with Spy 14.1 and La Chapelle
Australopithecus reconstruction
Statements
fossils, and is based on one of the larger
the bone to be much more robust than modern has a mean
with the
Anatomy
that this reconstruction
called robust in terms of the South African East Rudolf
in profile,
developed.
on Femoral
not the largest)
In inferior
groove is V-shaped
7. The New Reconstruction
Although
is directed
The trochanteric
the range
14.0.
by
The index of the
of Pan troglodytes and Pongo
pygmaeus among the anthropoids. This robusticity could be due to several factors but among them are: d’ff I erences in bodily proportions between Australopithecus and H. sapiens (specifically a greater proportion resistance to greater bending moments neck,
greater
muscular
bodily proportions
development
of the mass in the head, neck, arms and trunk), in the femoral shaft due to the relatively longer in the thigh
of Australopithecus is practically
and lower limb bones are limited
to the humerus
To assume that they had bodily proportions to circularity of argument Lovejoy & Heiple (1970) since it is associated with think, given the state of the which the reconstruction Broom’s
of Australopithecus.
lacking since definitely
similar
and foot fragments
Evidence associated
for the upper
from Kromdraai.
to those of H. sapiens is likely to lead
when dealing in functional terms. attempted a reconstruction based mainly on the Sts 14 femur a pelvis that provides the interacetabular diameter. I do not Sts 14 femur, that the reconstruction is valid, but the method by was made is sound in principle. Measurements taken from
sketch and from published photographs do not, however, lend themselves to The East Rudolf material now makes it clear that the distal fragments from accuracy. Sterkfontein are from substantially larger femora than Sts 14 and this too affects the
NEW
Lovejoy
smaller
FROM
551
KENYA
The Sts 34 and SK 82 pieces that these authors
& Heiple reconstruction.
are now seen to come from femora much
FEMORA
AUSTRALOPITHECLJS
of approximately
than the reconstruction
used
the same size and which were not
based on KMN.
ER. 993.
I would estimate
the
length of such a femur as about 330-340 mm. This is greater than Lovejoy & Heiple’s estimate and probably reflects a greater interacetabular distance than that of the Sts 14 pelvis. The Sts 14 femur must have had a much smaller distal part than Sts 34 and this in turn means that the total reconstructed length must be somewhat smaller than Lovejoy & Heiple’s estimate of 276 mm. This is the smallest femur known and the total length may have been no more than 250 mm. The size of the head in the new reconstruction is small relative to other parts of the end of the bone. The diameter of the reconstructed head is 34-O mm. Values fen-
proximal
populations 1957).
of modern
When
man have means
ranging
the head size is normalized
from 36.0
to 47.8
for total femur length
(Martin
& Sailer,
(head diameter
x lOCl/
total femur length), the value for the reconstruction is 9.44, compared with a total range of 8.76 to 10.63 and a mean of 9.81 for modern East African femora. Of the fossil specimens available femoral
for which head diameters
can be taken the values are given in Table
heads in Australopithecus do not seem, therefore,
to be small for the femur length, although small relative to the shaft dimensions. When
Gieseler
compared
(1926)
with the total
of necklength
The
since the femur is very robust the heads may be
The neck length in the reconstruction mm.
2.
as some writers have suggestedl,
(as defined by Martin femur
x loo/total
length,
femur
& Saller No. 14~) is 5000
the necklength
length
is 13.89.
index This
as used by
compared
with
modern East African femora shows an exceedingly long neck. This index in H. sapiem ranges from 8.55 to 1 I.01 with a mean of 9.74. Using Martin & Sailer’s necklength (No. 14) in which the head too is taken into account, shaft index (Martin
& Sailer necklength
man that range from 15.00 to 20.00. #ygm.aeus and Gorilla gorilla, it is higher high index in the reconstruction extremely
small for the femur
index)
the length
of 20.28,
Although
is 73.0 mm, giving a neck/
compared
with those of modern
smaller
than the usual values for Pongo This than the mean for Pan troglodytes of 18.80.
is made more striking
by the fact that the head is not
A head of the mean diameter of modern man would give an even larger value for this necklength index. Neck lengths for Australopithecats are given in Table The neck-shaft Table
3.
modern
3. angle in the reconstruction
A total variation man, but Pearson
demonstrates
length.
is 116” and values for the fossils are given in
of 23” has been
recorded
& Bell (19 19) record
sexual dimorphism
by Martin
in man, with females having
by sometimes as much as 3” between the means of the sexes. lations of H. sa$ens range from 121” to 133” with an overall Australopithecus angles are, then, significantly
Table
2
Femoral
head
Specimen
Anteroposterior (mm)
SK 82 SK 97 KNM. ER. 738
34.2 37.2 33.5
& Sailer
(1957)
for
angles from 111.5” to 150” ! This angle higher angles than males Means for different popumean of about
127”.
The
less than is usual in H. sapiens. The neck in
diameters
diameter
in
Austrnlopithecus Superoinferior diameter (mm) 33.0 35.0 33.2
-
552
A.
Table 3
WALKER
Neck
diameters,
angles and neck-shape
indices
in Awtralo-
pithecus femora
Specimen SK 82 SK 97 KNM. ER. 738 KNM. ER. 815 O.H. 20
the
reconstruction
indices (of Martin
Anteroposterior diameter
Superoinferior diameter
(AP) (mm) 18.2 19.0 16.5 15.9 19-5
(SI) (mm)
SI (Martin and Saller) p. 569
Neck-shaft angle (Martin and Saller) No. 29
26.5 26.0 26.5 25.0 (min) 33.0 (est)
50.0 52.0 40.0 41.0 (est) 50.0 (est)
68.67 73.08 62.26 63.60 59.09
120” 118” 115” 115” (est) 115’ (est)
is compressed & Sailer,
Index AP x 100 Neck length (Martin and Sailer) No. 14c (mm)
anteroposteriorIy.
The
diameters
1957) of the fossils are given in Table
3.
and
index of neck shape has a mean of about 80.0 and a range of 70.0 to 90.0. to attribute
this compression
to greater
abduction/adduction
trochanter
does not flare out from the lateral
shape
man,
the
It is tempting
forces than in modern
man,
1971) are thwarted
by the
but bending moment studies such as those of Preuschoft (1970, presence of trabecular bone such as is found in the neck. The greater
neck
In modern
border of the shaft, a feature
that several authorities have noted (Napier, 1964; Day, 1969 ; Lovejoy & Heiple, 1972). Broom & Robinson (1950) hinted that the trochanter in Sts 14 was flaring as in modern man. I could not judge the issue on that imperfect pected then it would be atypical of Australopithecus Lovejoy
& Heiple
(1972)
state that the absence
due to the more laterally condylar
placed
projected
and maintaining
of flaring in the Swartkrans
There
of the trochanteric
fossa in Australopithecus,
rather
the proximal
the angle between
the body as in man. insertion
but if it was as they susas we now know them.
shaft, but this could also be related
angle at the distal end of the bone causing
more laterally
specimen, specimens
placed
of the m. obturator extemus tendon inferiorly.
with
arrangement
the mm. obturator
of
of the details
internus and gemelli
and a much deeper and separate This impression
is
part of the shaft to be
the neck and the midline
seems to be a more or less constant
high and anteriorly
specimens
to the high femoro-
impression
is very deep indeed in SK 97.
The position of the lesser trochanter has been stated frequently as being more laterally placed than in modern man. Recently, Lovejoy & Heiple have questioned this and point out the problems associated with anteversion of the femoral neck and the static position of the trochanter.
An illustration
of the variability
in this feature in modern
even more dramatic than Lovejoy & Heiple’s figure is Martin & Saller’s it happens the femora from East Rudolf possibly have the lesser trochanters
man that is
figure 437. As more medially
placed than in modern man and it is quite clear that there is just as much variability
here
as in H. sapiens. The question of the development of the intertrochanteric line in Australopithecus has also been dealt with by Lovejoy & Heiple (1972). They point out that the line is variably developed in man and that Australopithecus does not fall outside the human range in this feature, as had been claimed previously. The line in the fossils seems to curve rather medially on its course towards the lesser trochanter and this is probably due to the long neck. Despite this, the fact remains that, of five specimens that have the region well enough preserved, there is not one that shows a strongly developed intertrochanteric line.
NEW
The
shaft is platymeric
diameters
to hyperplatymeric
in the midshaft
evidence
available
A low gluteal elongated
AUSTRALOPITHECUS
region,
at present,
hypotrochanteric
FROM
in its upper
especially
it appears
swelling is present
FEMORA
part,
in the larger
but has more
individuals,
that pilaster development
553
KENYA
where
equal on the
is proportional
to size.
on all the fossil bones with that part preserved
and an
fossa is again
present
on all bones
that show the area.
A
small crest proximal to the fossa may or may not be present. In the large specimen, KNM. ER. 736, the fossa is very low on the shaft, centred some 60.0 mm below the distal margin of the lesser trochanter. The suprapatellar surface in the reconstruction as Heiple anterior could
& Lovejoy position
(1971)
relative
not know,
angle
and the condyles are placed, distal pieces,
to the most distal part of the diaphysis.
however,
is that
the excavated
bowing of the shaft brings the more proximal to the condyles,
is concave
showed for the two Sterkfontein suprapatellar
What area
and
the position in modern man. Most previous estimates the vertical.
an
the anterior
parts of the shaft more anteriorly
thus approaching
is 105” or 15” from
in rather
these authars in relation
The femorocondylar of the angles in the
Sterkfontein pieces have been lower, probably, than the true values, mostly because the remaining distal portions of the shaft are too short to determine the shaft axis accurately. Clark (1947)
said that the obliquity
he arrived at his estimate. a range
of 4-17”
criticized critique
for normal
(if not scorned)
in TM
1513 was “at least 7”“, and he described
He also quoted Parsons male
English
by Pearson
femora.
& Bell
of possible (and to them actual)
(1914)
(1919)
problems
how
as giving an average of 10’ and
Parsons’ methods were severely and those authors give a lengthy
of mensuration
of this angle.
Measure-
ments for modern man are, however,
usually in the region of 9-l lo and Martin & Sailer give ranges of 4&l 7” for both sexes in man. Pearson & Bell’s mean values for males and females are: 8.7’ and 11.6’ for right and left male femora with S.D.‘S of 2.018 and 1.890, and 9.4” and 1 l-8” for right and left female femora with over 6 % of the 817 femora difficult to measure
that they measured
the angle in the Sterkfontein
of shaft was not enough to encourage to measure
confidence.
this angle on casts and furthermore KNM. ER. 993 vindicates
the event, specimen
S.D.‘S
of 2,135 and 1.890.
had angles over 14’.
A little
I myself found it
specimens, because the remaining length Heiple & Lovejoy however, attempted were brave enough to state it boldly. In their stand and their estimates of 15” and
14” for Sts 34 and TM 1513 conform with the angle in the new reconstruction. Kern & Straus (1949) took Clark’s figure and used it as an accurate one instead of an estimated minimum
value.
It is clear, then, that the genu ualgum of man was also similarly
Australopithecus. The building
seen also in Australopithecus. the lateral mass in his sketch of TM bone with no attempt had neither completely
present
in
up of the lateral border of the patellar groove as in man is KNM. ER. 993 shows that Clark probably underestimated
at reconstructing
15 13. Recently
Preuschoft
(197 1) has illustrated
the missing part and concludes
genu valgum nor genu varum, using this as evidence adapted for and quadrupedalism
incompletely
that bipedalism
abandoned.
this
that Australopithecus was in-
The angle between
the tangent drawn across the anterior patellar groove margins and the tangent across tlhe most posterior points of the condyles in distal view is of the order of 5’ in the human direction. Other anthropoid Primates have the angle in the opposite direction and this is presumably related to the genu varum position. The condylar index of Martin and Saller is 76.9 in the reconstruction. This is well within the range of the index for modern man, but somewhat higher than for H. sapiens
554
A.
WALKER
neanderthalem-is. Heiple & Lovejoy (1971) have discussed the shape and size of the intercondylar fossa and the contours of the condyles. Their conclusions are that most of the condylar features their findings. It is difficult
are very close to those of man and KNM.
to begin to understand
without
knowing
the morphology
material
from East Rudolf
the functional
and proportions
includes
ER.
993 serves to confirm
morphology
of one particular
bone
limb skeleton.
New
of the adjacent
part of a tibia as well as upper limb bones (Leakey
et al., 1972). It is highly likely that more postcranial bones of Austra~o~ithecus will be found in the East Rudolf area and the chances of finding associated bones are probably greater
there than in any other African
here is based on relatively remodelled
proximal
as much certainty
deposits now known.
material,
end is justified.
When
The reconstruction
but new finds will show whether
offered or not the
other limb bones can be reconstructed
as the femur and when the proportions
then biomechanical convincing
complete
analyses of the post cranial
of the limb skeleton
with
are known,
parts of Australopithecus will become
more
than they are at present.
8. Conclusions New fossil material
from East Rudolf
provides
the basis for a three-dimensional
recon-
struction of a moderately large-sized femur of Australopithecus. The foIlowing are the features by which the reconstructed femur, the fossils upon which it is based and other fossils described earlier, differ from H. sapiens femora: (I) The femur is more robust than is usual in H. sapiens. (2)
The femoral
relating
head diameter
lies in the low part of the range for H. sapiens. An index
head size to femur length is, however,
not much below the mean value for modern
man. (3) The
neck is very long and neck length
indices
fall well outside
the human
range.
Even when the head too is taken into account, an head + neck length index is higher than the highest in H. sapiens. This is despite the measuring of the neck length at a less oblique angle than in man (see 4). (4) The neck-shaft angle in Australopithecus is smaller
than is usual in H. sapiens, i.e. the
neck is set more nearly at right angles to the shaft axis. (5) The neck is more anteroposteriorly compressed in Australopithecus than in H. sapiens. (6)
The greater
trochanter
does not flare out from the lateral
profile
of the shaft as it
does in H. sapiens. (7)
The obliquity
of the femur in Australopithecus, as judged
is greater than is usual in H. sapiens. (8) There is a considerable size range in femora
by the femorocondylar
now attributed
angle,
to Australopithecus. The
smallest, from Sterkfontein, may have been only 250 mm long, while the largest, from East Rudolf, must have had a total length greater than the 360 mm reconstructed for the quite robust femur presented here. On the whole, Australopithecus femoral lengths are likely to be below and at the small end of the range of total lengths for human femora. (9) Although the human femur shows a high degree of variability and although many of the individual measurements and indices on Australopithecus fossils fall within the total ranges for those of H. sapiens, nevertheless a distinctive Australopithecus morphological pattern is gradually emerging as more specimens are found.
NEW
AUSTRALOPITHECUS
FEMORA
FROM
KENYA
555
I thank Mr R. E. F. Leakey and the Museum Trustees of Kenya, Professor P. V. Tobias and Dr C. K. Brain for permission to study material in their care. I would like to thank my many colleagues who have freely discussed their ideas on the hominid post cranial skeleton, particularly, Professor M. H. Day, Professor P. R. Davis, Mrs G. Kennedy, Mr R. E. F. Leakey, Dr H. Preuschoft, Dr B. A. Wood and Professor M. H. Wolpoff. My sincere thanks go to Richard Leakey who made it possible for me to visit South Africa. References Bone, E. L. (1955). Quatre fragments post-craniens du gisements a Australopitheques de Makapansgat. Anthropologic 59, 462-469. Broom. R. & Robinson. T. T. (1950). Further evidence of the structure of the Sterkfontein ape-man, Plesikhropus. Transva~~Museu~ M&wir no. 9 (1). Clark, W. E. Le Gros (1947). Observations on the anatomy of the fossil Australopithecinae. Journal oj Anatomy 81, 300-333. Day, M. H. (1969). Femoral fragment of a robust australopithecine from Olduvai Gorge, Tanzania. Nature
221,230-233. Gieseler, W. (1926). Messtechnik der langen Gliedmassenknochen der Anthropoiden. Abderhalden’s Hdbch biol. Arbeits~t~de~ 7, 635. Heiple, K. G. & Lovejoy, C. 0. (1971). The distal femoral anatomy of Australopithecus. American Journal of Physical Anthropology 35, 75-84. Kern, H. M. & Straus, W. L. (1949). The femur of Plesianthropus transvaalensis. American Journal of Physical Anthropology 7, 53-77. Leakey, R. E. F. (1971). Further evidence of Lower Pleistocene hominids from East Rudolf, North Kenya. Nature 231,241-245. Leakey, R. E. F. (1972). Further evidence of Lower Pleistocene hominids from East Rudolf, North Kenya, 1971. Nature 237,264-269. Leakey, R. E. F., Mungai, J. M. & Walker, A. C. (1971). New australopithecines from East Rudolf, Kenya, American Journal of Physical Anthropology 35, 175-186. Leakey, R. E. F., Mungai, J. M. & Walker, A. C. (1972). New australopithecines from East Rudolf, Kenya (II). American Journal of Physical Anthropology 36, 235-252. Leakey, R. E. F. & Walker, A. Cl. (1973). New australopithecines from East Rudolf, Kenya (III). American Journal of Physical Anthropology (in press). Lovejoy, C. 0. & Heiple, K. G. (1970). A reconstruction of the femur of Austrulopithecus africanus. American Journal of Physical Anthropology 32,33-40. Lovejoy, C. 0. & Heiple, K. G. (1972). Proximal femoral anatomy of Awtralopithecus. Nature 235, 175-l 76. Martin, R. & Sailer, K. (1957). Lehrbuch der Anthropologic 1. Stuttgart: Fischer. Napier, J_ R. (1964). The evolution of bipedal walking in the hominids. Archives de Siologie Liege 75 (Suppl). 673-708. Parsons, F. G. (1914). The characters of the English thigh bone. JournaZ of Anatomy 48,238-267. Pearson, K. & Bell, J. (1919). A study of the long bones of the English skeleton. Drapers’ Company Memoirs. Biometric Series 10,l-224. Preuschoft, H. (1970). Functional anatomy of the lower extremity. In (G. Bourne, Ed.), The Chimpanzee 3. Basel: Karger. Preuschoft, H. (1971). Body posture and mode of locomotion in early Pleistocene hominids. Foliaprimatologica 14,209-240. Zihlman, A. (1971). The question of locomotor differences in Australopithecus. Proceedings of the 3rd International Congressof Primatologv, Zurich, 1970, 1, 54-66.