Title of article :
Does the degree of laminarity correlate with site-specific
differences in collagen fibre orientation in primary bone?
An evaluation in the turkey ulna diaphysis
Author/Authors :
John G. Skedros، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2004
Abstract :
de Margerie hypothesized that preferred orientations of primary vascular canals in avian primary cortical bone
mediate important mechanical adaptations. Specifically, bones that receive habitual compression, tension or
bending stresses typically have cortices with a low laminarity index (LI) (i.e. relatively lower cross-sectional areas of
circularly (C) orientated primary vascular canals, and relatively higher areas of canals with radial (R), oblique (O) or
longitudinal (L) orientations. By contrast, bones subject to habitual torsion have a high LI (i.e. relatively higher Corientated
canal area) [LI, based on percentage vascular canal area, = C/(C + R + O + L)]. Regional variations in
predominant collagen fibre orientation (CFO) may be the adaptive characteristic mediated by LI. Using turkey
ulnae, we tested the hypothesis that site-specific variations in predominant CFO and LI are strongly correlated. Middiaphyseal
cross-sections (100
±
5
μ
m) from subadult and adult bones were evaluated for CFO and LI using circularly
polarized light images of cortical octants. Results showing significant differences between mean LI of subadult
(40.0%
±
10.7%) and adult (50.9%
±
10.4%) (
P <
0.01) bones suggest that adult bones experience more prevalent/
predominant torsion. Alternatively, this relationship may reflect differences in growth rates. High positive correlations
between LI and predominant CFO (subadults:
r
= 0.735; adults:
r
= 0.866;
P
< 0.001) suggest that primary
bone can exhibit potentially adaptive material variations that are independent of secondary osteon formation
Keywords :
Osteons , laminar bone , bone vascularity , Cortical bone , Bone adaptation
Journal title :
Journal of Anatomy Wily
Journal title :
Journal of Anatomy Wily