Polarized Fourier transform infrared microscopy (FT-IRM) was used to a
ssess the orientation of mineral and matrix components of the normally
calcified turkey leg tendon. Two groups of tendon, <16 weeks of age (
young) and >60 weeks of age (old), were analyzed, Linear sequences fro
m calcified, non-calcified, and transitional regions of the tendons we
re examined. Spectra collected in the ''parallel polarization'' mode w
ere acquired with the electric vector of the infrared radiation parall
el to the collagen fiber axis whereas spectra collected in the ''perpe
ndicular polarization'' mode were acquired with the electric vector of
the infrared radiation perpendicular to this axis. The nu(2) carbonat
e (850-890 cm(-1)) and nu(1), nu(3) phosphate (900-1180 cm(-1)) contou
rs of the tendon mineral as well as the collagen amide I, II, and III
bands of the extracellular matrix all displayed marked dichroism. The
CO32- ions substituted for PO43- (878 cm(-1), type B substitution) in
the tendon mineral displayed parallel dichroism while the CO32- ions s
ubstituted for OH (871 cm(-1), type A substitution) in the tendon mine
ral displayed perpendicular dichroism. These orientational effects for
both sites of carbonate substitution were greater in the older animal
s. The polarization properties of the nu(1), nu(3) phosphate contour w
ere analyzed by use of an empirical anisotropy parameter (A), the valu
e of which monitors the degree of orientation. This index significantl
y increased in the other animals indicating that aging produces a more
highly oriented mineral. The amide I, II, and III contours of the col
lagen extracellular matrix also exhibited marked dichroism, The amide
I component exhibits perpendicular dichroism while the amide II and II
I components exhibit parallel dichroism. The current study demonstrate
s the ability of polarized FT-IRM to assess the orientation of the min
eral and matrix components of calcified tissue at the microscopic leve
l.