H. Preuschoft et C. Tardieu, BIOMECHANICAL REASONS FOR THE DIVERGENT MORPHOLOGY OF THE KNEE-JOINT AND THE DISTAL EPIPHYSEAL SUTURE IN HOMINOIDS, Folia primatologica, 66(1-4), 1996, pp. 82-92
The obliquity of the femoral diaphysis accounts for the valgus positio
n of the human knee joint and reduces bending moments in the frontal p
lane, A high angle of obliquity is considered a hallmark of hominid bi
pedality, but its functional importance has rarely been identified cor
rectly. A biostatic investigation of the knee joint in various realist
ic positions unveils resultant joint forces which do not deviate great
ly from the long axis of the femoral shaft. This is due to the length
of the femur and to the shortness of the human foot, The flat epiphyse
al suture is more or less perpendicular to these joint forces, and the
equal size of the femoral condyles reflects the even distribution of
forces between them. In great apes the resultant forces acting in the
knee joint vary considerably in dependence on the degree of flexion an
d rotation of the knee joint. The resultant joint force may be in line
with the femur shaft or diverge. The epiphyseal surfaces offer facets
to all joint forces found in the course of the study. Due to the pron
ounced varus position of the knee joint, the joint itself and the adja
cent part of the femur are under medially concave bending moments, whi
ch lead to higher compressive forces at the medial than at the lateral
condyle. The enlarged medial condyle allows the distribution of media
lly displaced joint forces over a relatively large area, and the ellip
tic cross-section yields high bending resistance in the frontal plane.
A human-like angle of obliquity is present in the early australopithe
cines, the values being mostly within the range of variation of childr
en. The valgus position of the australopithecine knee joint is conside
red to be a functional, and epigenetic consequence of habitual bipedal
ity. It is particularly pronounced because of the short length of the
femur and the great bitrochanteric width.