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. Author manuscript; available in PMC: 2013 Nov 1.
Published in final edited form as: Bone. 2012 Aug 15;51(5):920–928. doi: 10.1016/j.bone.2012.08.110

Comparison of bone tissue properties in mouse models with collagenous and non-collagenous genetic mutations using FTIRI

Rhima M Coleman a,1, Laura Aguilera b, Layla Quinones b, Lyudamila Lukashova a, Christophe Poirier c, Adele Boskey a,*,2
PMCID: PMC3583571  NIHMSID: NIHMS401488  PMID: 22910579

Abstract

Understanding how the material properties of bone tissue from the various forms of osteogenesis imperfecta (OI) differ will allow us to tailor treatment regimens for affected patients. To this end, we characterized the bone structure and material properties of two mouse models of OI, the osteogenesis imperfecta mouse (oim/oim) and fragilitas ossium (fro/fro), in which bone fragility is due to a genetic defect in collagen type I and a defect in osteoblast matrix mineralization, respectively. Bones from 3 to 6 month old animals were examined using Fourier transform infrared spectroscopic imaging (FTIRI), microcomputed tomography (micro-CT), histology, and biochemical analysis. The attributes of oim/oim bone tissue were relatively constant over time when compared to wild type animals. The mineral density in oim/oim cortices and trabecular bone was higher than wild type while the bones had thinner cortices and fewer trabeculae that were thinner and more widely spaced. The fro/fro animals exhibited osteopenic attributes at 3 months. However, by 6 months, their spectroscopic and geometric properties were similar to wild type animals. Despite the lack of a specific collagen defect in fro/fro mice, both fro/fro and oim/oim genotypes exhibited abnormal collagen crosslinking as determined by FTIRI at both time points. These results demonstrate that abnormal extracellular matrix assembly plays a role in the bone fragility in both of these models.

Keywords: Osteogenesis imperfecta, Mouse models, Fourier transform infrared spectroscopy, Microcomputed tomography

Introduction

Osteogenesis imperfecta (OI) is a genetic disease in which sufferers break their bones with minimal trauma [1]. This disease was once thought to involve only malformation of type I collagen (classical OI) caused by dominant negative structural mutations in either of the type I collagen genes [2, 3]. However, recent studies have identified OI forms that are due to genetic defects in accessory proteins that are involved in the post-translational modification of pro-collagen molecules [3]. To effectively treat OI patients, it is important to understand how bone tissue properties diverge in various conditions resulting in bone fragility. Mouse models allow us to examine tissue from multiple genetic defects over time.

Osteogenesis imperfecta mice (oim/oim) have osteopenia, brittle fractures, and progressive skeletal deformities due to a G nucleotide deletion in the α2(I) gene that results in an altered amino acid sequence [4]. This mutation results in the accumulation ofαl(I) homotrimeric collagen in the extracellular matrix and a reduction of collagen production. The end result is increased tissue mineral density in bone tissues [4]. The phenotypic, biochemical, and molecular findings in homozygous oim/oim mice closely duplicate those seen in OI type III patients [4, 5] and have served as a model of OI due to genetic defects in the Col1a1 gene. However, most patients with this type of genetic defect have been shown to have Ehlers/Danlos Syndrome [6] and only one OI patient exhibiting the accumulation of αl(I) homotrimers has been identified [7].

The fragilitis ossium (fro/fro)model of bone fragility was produced by exposing mice to (tris (1-aziridinyl phosphine) sulfide) which results in an autosomal recessive disorder characterized by severe angular deformities of all long bones and numerous fractures [8]. A defect of type I collagen has not been detected and the collagen produced by fro/fro-derived fibroblasts appears normal [9]. Recently, the mutation that causes the fro/fro phenotype was identified as a defect in the sphingomyelin phosphodiesterase 3 (Smpd3) gene [10]. This mutation causes loss of function of neutral sphingomyelinase 2 (nSMase2), a membrane-bound enzyme, which cleaves sphingomyelin to generate the lipid second messenger ceramide. Ceramide generated by sphingomyelinases is involved in the regulation of stress-induced cellular responses, including cell differentiation, proliferation, adhesion, and cell death [11]. In osteoblasts, RUNX-2 has been shown to regulate expression of the Smpd3 gene [12] and ceramide regulates cell apoptosis [13]. In fro/fro mice, the Smpd3 defect results in reduced mineralization of the osteoid [9, 14].

These animal models offer us the unique opportunity to study the tissue-level properties of fragile bones, specifically differences between collagen and mineral structures, with and without a defect on the collagen gene. The goal of this study was to compare the tissue properties of these models in an effort to understand the complex relationship between matrix morphology and progression of mineralization.

Materials and methods

Animal tissue

Homozygous fro/fro were produced by exposing FRA/Pas inbred mice to the chemical mutagen tris (1-aziridinyl) phosphine-sulfide (ThioTEPA®) as previously described [10]. Homozygous oim/oim mice, which were developed on the C57Bl/6 background, were kindly provided by Dr. Mathias Bostrom at the Hospital for Special Surgery. Bones were harvested from 3 and 6 month old males and females from fro/fro (3 months: n=8, 6 months: n=3) and oim/oim (3 months: n=7, 6 months: n=4) mice for the analyses described below. To keep numbers comparable, the number of fro/ fro animals and oim/oim was matched. Bones from age-matched FRA/Pas animals (3 months: n=13, 6 months: n=6) were used as controls for the fro/fro and age-matched C57Bl6 animals (3 months: n=10, 6 months: n=12) were used as controls for oim/oim samples.

Microcomputed tomography

Right femurs and tibias were placed in 70% ethanol and scanned on a Scanco µCT35 scanner (Scanco Medical, Basserdorf, Switzerland) with a 6 µm voxel size. A 0.36° rotation step (360° angular range), 400 ms exposure and 4 frames per view were used in the scans. The Scanco micro-CT software (HP, DECwindows Motif 1.6) was used for 3D reconstruction and viewing of images. Volumes of interest were defined with a free-hand tool on sequential sections in the metaphyseal and mid-diaphysis of each bone to determine the trabecular and cortical bone parameters, respectively. The trabecular bone parameters calculated were bone volume fraction (BV/TV), tissue mineral density (TMD), the number, thickness, and spacing of the trabeculae (Tb.N, Tb.Th, and Tb.Sp), and the bone surface to bone volume ratio (BS/BV). The cortical bone parameters calculated were BV/TV, TMD, and the thickness of the cortices (Cort.Th).

Fourier transform infrared spectroscopic imaging (FTIRI)

After micro-CT scanning, the right femurs were dehydrated in graded ethanols and embedded in poly methyl methacrylate (PMMA). Undecalcified sections of the whole bone were microtomed at a 2 µm thickness and placed on BaF2 windows (Spectral Systems, Hopewell Junction, NY) for FTIRI. Within each section, three cortical and three trabecular FTIR images over the spectral range 800–2000 cm−1 were collected at a spectral resolution of 8 cm−1 and a spatial resolution of 6.25 µm using an infrared imaging system (Spotlight 300; PerkinElmer Instruments, Waltham, MA). Background (BaF2 window only) and PMMA spectra were also collected for each section and used to correct the sample spectra. Spectra were baseline corrected and the PMMA spectral contribution was subtracted using chemical imaging software (ISys, Malvern Instruments, Worcestershire, UK). The infrared spectrum at each pixel was analyzed to determine four FTIR parameters [15]: the mineral/matrix ratio (area ratio of the phosphate ν1/amide I peaks), which characterizes tissue mineral content; the carbonate:phosphate ratio (area ratio of the carbonate/phosphate ν1 peaks), which characterizes the extent of carbonate substitution into the mineral lattice; the collagen maturity (intensity ratio of 1660 cm−1/1690 cm−1 bands), which is related to the ratio of non-reducible to reducible collagen crosslinks [16]; and the mineral crystallinity (intensity ratio of 1030 cm−1/1020 cm−1 bands), which is related to crystal size as assessed by X-ray diffraction [17]. The FTIR parameter values calculated at each of the bone pixels within each image yielded a distribution of values for each FTIR parameter. Each distribution was characterized by two outcome variables: the mean of the distribution and the full width at half maximum (FWHM) of the Gaussian curve fit to the distribution (300 bins), which provided a measure of tissue compositional heterogeneity. For each parameter, the distribution mean and width for each of the bone tissue regions were averaged to obtain mean and width values for each specimen.

Histology

Sections (7 µm thick) of the right femurs were taken from the undecalcified PMMA blocks of the right femur immediately after FTIRI sections were taken. The sections were mounted on poly-l-lysine/gelatin coated slides and stained with a modified Goldner's Trichrome. Briefly, sections were deplasticized in PMMA monomer, rinsed in 100% ethanol and rehydrated to distilled water through graded alcohols. They were then sequentially stained in Weigart's hematoxylin, Ponceau 2R/Acid Fuchsin, and Light Green. This results in green bone, light pink cartilage, and red or orange osteoid.

For transmission electron microscopic analysis (TEM), tissues were preserved in 2% paraformaldehyde and 0.5% glutaraldehyde in 0.05 M cacodylate buffer, pH 7.4 at 4 °C for 18 h. Following fixation, the tissues were dissected into individual pieces a few millimeters thick. These were treated with reduced osmium tetroxide for 1 h at room temp. This solution consists of 2% (w/v) potassium ferricyanide in distilled water combined 4:1 with 4% osmium tetroxide (EM Sciences, Hatfield, PA.). Following osmication, the samples were dehydrated in graded alcohols and embedded in Spurrs resin. Sections (60–80 nmin thickness) were stained with 2% (w/v) uranyl acetate in 50% ethyl alcohol, followed by Reynolds' lead citrate (3% (w/v) in distilled water with 1% (v/v) 10 N sodium hydroxide). Images were taken using a Philips CM-12 transmission electron microscope at 80 kv accelerating voltage.

Tissue milling

The diaphyses of left femurs and tibias from each animal were combined for all other assays based on previous analysis confirming that there is no difference in any of the biochemical outcome measures between these two bones (unpublished). The marrow was washed from the diaphyses using phosphate buffered saline and then 70% ethanol. They were then defatted in a 50:50 (v:v) chloroform/methanol solution over 3 days. Defatted bones were frozen at −80 °C, lyophilized, and ground in a liquid nitrogen-cooled freezer mill (Spex Industries, Metuchen, NJ). This process yielded approximately 10 mg of powder that was analyzed for crystal size by X-ray diffraction and assayed for collagen, calcium, and phosphate content as described below. Six month old fro/fro animals were not available for these analyses due to the high mortality rate of these animals (~90%).

X-ray diffraction

The entire mass of bone milled as described above was analyzed by wide-angle X-ray diffraction using a Bruker AX-8 diffractometer (Bruker, Madison, WI) with Cu Kα radiation. Scans were recorded from 20° to 40° 2θ, the line-width of the 002 peak measured, and c-axis crystallite size determined using manufacturer-supplied software (AXS Topas P, version 2; Bruker).

Collagen content

Approximately 4 mg of each milled sample was decalcified with 0.5 N HCl. The supernatant was retained, neutralized with NaOH, recombined with the washed pellet, and dialyzed against distilled/deionized water using dialysis tubing with a 10,000–12,000 MW cutoff. The samples were then frozen and lyophilized. Lyophilized samples were reconstituted with NaOH and hydrolyzed over night at 110 °C. The hydroxyproline content was determined using the colorimetric assay described by Martin et al. [18]. The concentrations were determined by comparison to a standard curve created from of cis-4-Hydroxy-D-proline (Sigma, St. Louis, MO). Total proline content was normalized by the weight of bone used for the assay.

Calcium/phosphate measurement

Approximately 0.5 mg of milled bone was mixed with 10 ml 1 N HCl and hydrolyzed overnight at 110 °C. To measure total calcium, triplicate aliquots of each sample were mixed with lanthanum hydrochloride as described by Montford et al. [19]. The calcium content was measured using atomic absorption and the concentration determined from CaCO3, HNO3 calcium standards (Sigma, St. Louis, MO).

Triplicate aliquots of the hydrolyzed solution were used to measure the phosphate content by means of the Fiske–Subbarow method with modifications developed by Heinonen et al. [20]. Briefly, 1 part of the samples was mixed with 8 parts of a solution containing 5 N H2SO4, 10 mM ammonium molybdate, and acetone. The reaction was then stabilized by adding citric acid. The spectroscopic absorbance was measured at 355 nm and the phosphate concentration calculated from a standard curve created with a phosphorus atomic absorption standard solution (Sigma, St. Louis, MO).

Statistics

A general linear model (ANOVA) was performed for all data sets after the test for normality was satisfied with significance set at p<0.05. Since the background (wild type) strains for fro/fro and oim/oim animals were different, the baseline bone tissue properties for all parameters measured were not identical. Therefore, the statistical analysis was performed as follows: when comparing values from defect animals to wild type, the raw values of the genetically impaired animals were compared directly to its respective wild type. For comparisons between ages or between oim/oim and fro/frothe defect animals' values were normalized to their respective wild type and then the ANOVA tests were performed. In the figures, only the normalized data is presented for clarity. In each figure, the star above a bar indicates a significant difference from wild type and a bracket indicates a significant difference between the groups under the ends of the brackets.

Results

Microcomputed tomography

Differences in tissue geometry were evident between the genotypes and were predominantly manifested in the trabecular bone (Table 1 and Figs. 1A and C). All of the data and p-values listed below are from analysis of the femurs. Tibia samples followed identical trends.

Table 1.

Mean trabecular micro-CT values (stand. dev.).

BV/TV (mm3/mm3)
Tb.N (1/mm)
Tb.Th (mm)
Tb.Sp (mm)
BS/BV (mm2/mm3)
TMD (mg HA/cm3)
3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo.
fro 0.191b 0.125b,c 5.39b 2.60a,c 0.043 0.058a,b,c 0.18b 0.42a,c 60.54b 45.90b,c 940.8b 992.26a,b,c
(0.06) (0.06) (1.2) (0.74) (0.004) (0.017) (0.04) (0.11) (6.36) (11.08) (15.33) (51.88)
F/P 0.172 0.173 4.98 4.88 0.044 0.042 0.20 0.20 61.15 60.21 945.12 905.94
(0.05) (0.04) (0.89) (0.57) (0.005) (0.004) (0.04) (0.03) (8.11) (6.40) (41.31) (7.62)
oim 0.063a 0.032a 3.45a 2.33a 0.037a 0.035a 0.30a 0.46a 77.82a 84.54a 927.84 956.42a
(0.03) (0.02) (0.78) (0.71) (0.003) (0.003) (0.06) (0.13) (7.07) (11.74) (17.12) (7.25)
Bl/6 0.178 0.122 5.32 3.63 0.044 0.045 0.18 0.28 61.21 59.25 909.57 921.35
(0.05) (0.06) (0.49) (0.71) (0.005) (0.005) (0.02) (0.06) (7.60) (9.78) (18.96) (17.19)
a

Different from WT of the same age.

b

Different from oim/WT of the same age.

c

Different from 3 months of same genotype.

Fig. 1.

Fig. 1

Micro-CT parameters of (A) trabecular and (B) cortical bone. (C) Representative 3D images rendered from micro-CT analysis of trabecular and cortical bone morphology. The values shown are of each genotype normalized by its respective wild type control. The line indicates the level of the wild types for each parameter. A star above a bar indicates that a significant difference was found between mutant and wild type by performing a general linear model on the raw data. To compare between mutant genotypes and ages, the mutant values were normalized by the wild type values and then a GLM was performed. A bracket indicates significant differences that were found between the groups under the ends of the bracket. Differences in tissue geometry between the genotypes were predominantly manifested in the trabecular bone. The geometric properties of the oim/oim tissue remained constant with time. In fro/fro tissue, the volume fraction and surface of the trabecular bone decreased with time due to an increase in thickness and spacing of the trabeculae, while the mineral density increased.

The BV/TV, Tb.N, Tb.Th in the oim/oim were all lower than WT at 3 months (BV/TV — p=0.00001; Tb.N — p=0.00001; Tb.Th — p= 0.05) and 6 months (BV/TV — p=0.003; Tb.N — p=0.0247; Tb.Th — p=0.004), while Tb.Sp and BS/BV were greater in oim/oim than WT at both time points (3 mo.: Tb.Sp — p=0.0006; BS/BV — p=0.0004; 6 mo.: Tb.Sp — p=0.00001; BS/BV — p=0.00001).

At 3 months, there was no significant difference in any of the trabecular parameters between the fro/fro and wild type controls. By 6 months, Tb.Th and Tb.Sp increased significantly from 3 months in the fro/fro bone (Tb.Th — p=0.002; Tb.Sp — p=0.0001) to become greater than WT (Tb.Th — p=0.005; Tb.Sp — p=0.0009). Thus, by 6 months, fro/fro Tb.Th is greater than oim/oim (p=0.00001), and the Tb.Sp of fro/fro and oim/oim bones are similar. Tb.N decreased in the fro/fro animals with time (p=0.00001), so that it became lower than WT (p=0.006) and comparable to oim/oim at 6 months. Accordingly, BV/TV and BS/BV also decreased in the fro/fro animals with time (BV/TV — p=0.008; BS/BV — p=0.001). Despite the decrease in BV/TV of fro/fro trabecular bone with time, it was higher than oim/oim at both time points (3 mo. — p=0.00001; 6 mo. — p=0.008). The BS/BV was lower in the fro/fro than in the oim/oim at both time points (3 mo. — p=0.002; 6 mo. — p=0.00001).

The cortical properties were not as varied as the trabecular properties (Table 2 and Figs. 1B and C). The only difference in the cortices was that the Cort.Th was less in the oim/oim than in the WT at both time points (3 mo. — p=0.005; 6 mo. — p=0.0001).

Table 2.

Mean cortical micro-CT values (stand. dev.).

3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo.
fro 0.922 0.925 0.189 0.197 1108.77b 1218.11a,b,c
(0.01) (0.01) (0.02) (0.02) (29.63) (29.82)
F/P 0.929 0.920 0.210 0.214 1149.69 1086.79
(0.01) (0.01) (0.01) (0.01) (53.47) (10.95)
oim 0.469 0.457 0.159a 0.159a 1126.31 1170.92
(0.07) (0.04) (0.03) (0.02) (25.81) (19.38)
Bl/6 0.510 0.515 0.199 0.218 1130.42 1176.05
(0.03) (0.05) (0.01) (0.03) (12.98) (27.03)
a

Different from WT of the same age.

b

Different from oim/WT of the same age.

c

Different from 3 months of same genotype.

The change in TMD with time was similar for both trabecular and cortical bone tissues or just bone in both genotypes. Specifically, TMD was greater in the oim/oim compared to fro/fro at 3 months (Trab. — p=0.003; Cort. — p=0.046). TMD increased from 3 to 6 months in both the trabecular and cortical fro/fro bone tissues (Trab. — p= 0.00001; Cort. — p=0.00001) so that it became greater than WT (Trab. — p=0.0002; Cort. — p=0.00001) and oim/oim (Trab. — p= 0.007; Cort. — p=0.00001) by 6 months of age.

Fourier transform infrared spectroscopic imaging (FTIRI)

The means (Table 3) and distribution widths (FWHM, Table 4) of the mineral properties in the defect animals' bone tissue varied with age and between genotypes (Fig. 2). These changes were also dependent on the bone tissue type (cortical or trabecular). At 3 months of age, the distribution mean and width of the mineral/matrix ratio in the fro/fro cortices were lower than their WT counterparts (p=0.013 and p=0.005, respectively). There were no significant differences in the trabecular tissue. In contrast, the mean mineral/matrix was higher in oim/oim than their WT in both bone tissue types in the younger animals (Cort. — p=0.05; Trab. — p=0.002) while the distribution width of this parameter was not different from WT. Therefore, when the genotypes were compared in younger animals, we found that the mean mineral/matrix ratio of fro/fro tissue was significantly lower than oim/oim tissue (p=0.0001) and the distribution width of the mineral/matrix data was wider in the oim/oim tissue than in fro/fro tissue (p=0.0009).

Table 3.

Mean FTIRI values (stand. dev.).

Mineral/matrix
Collagen maturity
Carbonate/PO4 (×1000)
Crystallinity
Cortical
Trabecular
Cortical
Trabecular
Cortical
Trabecular
Cortical
Trabecular
3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo.
fro 6.56a,b 8.34γ 4.89b 5.90 3.41b 4.09α, γ 3.74b 3.85 5.89 6.96 4.78 6.67 1.21 1.17 1.14 1.13
(0.44) (0.26) (0.34) (0.49) (0.69) (0.49) (1.3) (0.75) (0.53) (0.07) (1.4) (0.58) (0.03) (0.00) (0.02) (0.01)
F/P 7.74 7.93 5.56 5.40 3.60 3.29 4.03 3.69 6.59 7.58 6.51 8.26 1.18 1.18 1.11 1.07
(0.84) (0.38) (0.81) (1.04) (0.64) (0.36) (0.96) (0.99) (0.83) (0.76) (1.7) (2.1) (0.02) (0.03) (0.03) (0.04)
oim 9.30a 8.52 7.45a 7.29a 3.98 4.59a,c 5.11α 5.26 5.90 5.05a 5.04 4.09a 1.14 1.14 1.10 1.12
(1.2) (0.85) (1.3) (0.64) (0.48) (0.34) (1.03) (0.31) (1.2) (0.96) (1.4) (0.76) (0.04) (0.01) (0.04) (0.02)
Bl/6 7.91 7.95 5.71 5.48 3.70 3.96 4.33 4.57 6.75 7.00 6.23 5.91 1.15 1.16 1.08 1.11
(1.4) (1.1) (0.93) (0.82) (0.42) (0.32) (0.70) (0.45) (0.86) (0.87) (0.93) (1.0) (0.05) (0.04) (0.02) (0.03)

Raw values from the analysis of fro/fro and its wild type (F/P) and oim/oim and its wild type (Bl/6). For statistical comparison between the mutant genotype and wild type, the raw values were used. For comparison between fro/fro and oim/oim or across ages, the values of the mutant animal are normalized by its respective wild type counterpart and then the ANOVA tests were performed as described in the Materials and methods section.

a

Different from WT of the same age.

b

Different from oim/WT of the same age.

c

Different from 3 months of same genotype.

α

Trend different from WT p ≤ 0.1.

γ

Trend different from 3 months p ≤ 0.1.

Table 4.

FWHM of FTIRI distributions (stand. dev.).

Mineral/matrix
Collagen maturity
Carbonate/PO4 (×1000)
Crystallinity (×10)
Cortical
Trabecular
Cortical
Trabecular
Cortical
Trabecular
Cortical
Trabecular
3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo.
fro 1.80a,b 3.01c 3.04 2.52 0.34 0.77c 0.51 0.74 1.91b 1.44b 3.16 1.44 1.51 1.48b 1.23 1.27
(0.20) (0.27) (0.52) (0.96) (0.17) (0.35) (0.24) (0.16) (0.46) (0.11) (1.0) (0.11) (0.48) (0.33) (0.23) (0.12)
F/P 2.77 2.40 3.00 2.44 0.54 0.31 0.87 0.43 2.37 2.09 3.65 3.42 1.38 1.33 1.26 1.41
(0.61) (0.40) (0.54) (0.44) (0.29) (0.14) (0.53) (0.11) (0.59) (0.23) (1.5) (0.68) (0.32) (0.36) (0.16) (0.64)
oim 4.21 4.09 3.68 4.57α 0.99a 1.34 1.83 1.78 2.74 3.24 3.41 3.89 1.16 1.19α 1.20 1.10
(1.3) (0.32) (1.2) (1.1) (0.47) (0.32) (1.11) (0.50) (0.88) (0.69) (1.0) (0.90) (0.19) (0.13) (0.47) (0.01)
Bl/6 3.22 3.27 3.39 3.36 0.56 0.60 0.94 1.12 2.1 2.57 3.45 4.71 1.31 1.49 1.21 1.09
(1.0) (1.0) (0.95) (0.76) (0.37) (0.12) (0.27) (0.40) (0.53) (0.44) (1.5) (1.5) (0.23) (0.27) (0.15) (0.20)

Raw values from the analysis of fro/fro and its wild type (F/P) and oim/oim and its wild type (Bl/6). For statistical comparison between the mutant genotype and wild type, the raw values were used. For comparison between fro/fro and oim/oim or across ages, the values of the mutant animal were normalized by its respective wild type counterpart and then the ANOVA was performed as described in the Materials and methods section.

a

Different from WT of the same age.

b

Different from oim/WT of the same age.

c

Different from 3 months of same genotype.

α

Trend different from WT p ≤ 0.1.

Fig. 2.

Fig. 2

FTIRI color maps and histogram distributions (70 bins for clarity) of the mineral/matrix ratio (phosphate/amide I peak area ratio) in cortical bone tissue. fro/fro mice were created on the FRA/Pas background and oim/oim on the C57Bl6 background. Graphs on the right show the mean (top) and widths (bottom) of the distributions of each genotype normalized by its respective wild type control for both cortical and trabecular tissues. The line indicates the level of the wild types for each parameter. A star above a bar indicates that a significant difference was found between mutant and wild type by performing a general linear model on the raw data. To compare between mutant genotypes and ages, the mutant values were normalized by the wild type values and then a GLM was performed. A bracket indicates significant differences that were found between the groups under the ends of the bracket. The fro/fro cortical tissue has significantly less mineral that was less heterogeneously distributed than WT and oim/oim tissues at 3 months, but both the mineral content and heterogeneity are normal by 6 months. The oim/oim tissue has higher mineral content than WT and remains constant over time.

When the effect of age was examined, a trend was found suggesting that the mineral/matrix mean and distribution width of cortical bone increased in fro/fro tissue to the level of WT from 3 to 6 months (p= 0.10 and p=0.035, respectively). Similar age-related trends in mineral to matrix content were seen in fro/fro trabecular bone, but these were not significant. At 6 months, the mean mineral/matrix ratio of the oim/oim cortical bone tissue was similar to WT while it remained higher than WT in trabecular bone (p=0.007). There were no differences in the mean or distribution width of this parameter between the fro/fro and oim/oim tissue in the older animals.

The mean values of mature collagen crosslinks in both mutant genotypes followed similar trends to the mineral/matrix parameter (Tables 3 and 4, Fig. 3). The mean values of this parameter in the cortices of oim/oim animals were 7.6% higher than WT at 3 months (NS) and increased to 15% higher than WT at 6 months (p=0.042). The collagen maturity in the trabecular tissue of oim/oim bones was also greater than WT and fairly constant over time (3 mo.: 18% greater, p=0.09; 6 mo.: 15% greater, NS). The collagen maturity in the cortices of the fro/fro was 5.3% lower than WT in younger animals (NS). In contrast to oim/oim cortical tissue, the collagen maturity of fro/fro cortical tissue increased significantly with age (3 vs. 6 months, p= 0.003) to become 24% higher in the mutant bones compared to WT. In trabecular bone, the trends were similar to cortical tissue (3 mo.: 7% lower than WT, NS; 6 mo.: 4% higher than WT, NS). When comparing the genotypes relative to their respective WT, we found that the mean values of this parameter tended to be higher in oim/oim than in fro/fro tissue at 3 months (Cort.: p=0.06; Trab.: p=0.03) and their means comparable at 6 months.

Fig. 3.

Fig. 3

FTIRI color maps and histogram distributions (70 bins for clarity) of non-reducible collagen/reducible collagen crosslinks (1660 cm−1/1690 cm−1 peak heights) in cortical bone tissue. fro/fro mice were created on the FRA/Pas background and oim/oim mice on the C57Bl6 background. Graphs on the right show the mean (top) and widths (bottom) of the distributions of each genotype normalized by its respective wild type control for both cortical and trabecular tissues. The line indicates the level of the wild types for each parameter. A star above a bar indicates that a significant difference was found between mutant and wild type by performing a general linear model on the raw data. To compare between mutant genotypes and ages, the mutant values were normalized by the wild type values and then a GLM was performed. A bracket indicates significant differences that were found between the groups under the ends of the bracket. The mean and distribution width of mature collagen crosslinks in the fro/fro was 5.3% lower than WT in younger animals (NS) and increased significantly to 24% higher in the mutant bones. The mean and distribution width of mature collagen crosslinks in the oim/oim tissue was greater than WT at both time points. The mean and distribution of this parameter tended to be higher in oim/oim than fro/fro at 3 months and comparable at 6 months.

The width of the distribution of the collagen maturity data in oim/oim was greater than WT in both tissue types and did not vary from 3 months to 6 months (Cort.: from 80% to 123% greater with time, NS; Trab.: from 95% to 60% greater with time, NS), which indicates greater heterogeneity in the concentration of mature collagen crosslinks throughout the oim/oim tissue in adolescent and adult animals. In the fro/frothe distribution widths were lower than WT at 3 months (Cort.: 37% less than WT; Trab.: 41% less than WT) and increased to greater than WT (Cort.: 148% greater than WT; Trab.: 72% greater than WT). Due to our small sample size, these differences were not significant. The change over time of the distribution width was significant in the cortices of fro/fro bones (p=0.005), but not in the trabecular tissue. The mature collagen crosslinks in the cortical tissue of fro/fro animals were less heterogeneously distributed than oim/oim at 3 months (adolescence) (Cort.: p=0.007; Trab.: p=0.05). By 6 months, the heterogeneity of collagen maturity was equivalent in both genotypes.

The mean and distribution values of the carbonate content and crystallinity are shown in Tables 3 and 4, respectively. The mean carbonate/phosphate ratio of cortical and trabecular bones was not different from WT at 3 months in either phenotype. The carbonate/ phosphate ratio remains constant with age in the fro/fro animals, while it decreases in oim/oim tissue to lower than WT by 6 months (p=0.008). The distribution width of this parameter in the fro/fro cortices was less than oim/oim at 3 months (p=0.016) with a similar trend at 6 month (p=0.1). There was no difference in the mean crystallinity compared to WT or between genotypes. At 6 months, there was a trend suggesting that the distribution width of this parameter was narrower in oim/oim than WT (p=0.07) and narrower than fro/fro (p=0.06) in cortical bone.

Histology

At 3 months, the oim/oim trabecular tissue appears to have less osteoid than their WT controls (Fig. 4). The fro/fro tissue appears to have a higher amount of osteoid in the trabecular bone while there is no difference in the cortical bone. The differences in trabecular osteoid levels in both genotypes appear to correct themselves by 6 months. The growth plates in all animals appear to be normal with no change to cellular organization or height (not shown).

Fig. 4.

Fig. 4

Trichrome staining of fro/fro (top) and oim/oim (bottom) and their respective wild type controls at 3 and 6 months. The fro/fro animals have more osteoid surface than WT at 3 months whereas oim/oim trabecular tissue has less osteoid. Both genotypes appear to have normal amounts of osteoid by 6 months. Original magnification 10×. Green = bone and red or orange = osteoid.

The collagen fibrils in the mutant genotypes are highly disorganized as seen in TEM images of 3 month old cortical tissue (Fig. 5). The fibrils also appear to be smaller than in the control tissue at this age.

Fig. 5.

Fig. 5

TEM images of 3-month-old control, oim/oim, and fro/fro cortical tissue demonstrating abnormal collagen fiber size and organization in the mutant animals. Scale bar= 200 nm.

Biochemistry

Biochemical analysis of pulverized pooled bone (Table 5) shows that collagen levels per unit mass of bone is lower in the oim/oim animals compared to WT (p=0.005) and fro/fro bones (p=0.0001). There was also a trend suggesting that the phosphate levels in the oim/oim bones were higher than fro/fro (p=0.09). The overall effect is that the phosphate/collagen ratio that is lower in the fro/fro and higher in oim/oim bone tissue compared to their respective WT controls (fro/WT — 0.83±0.30 vs. oim/WT — 2.30±0.79). This is in agreement with the FTIRI results. Also identical to the FTIRI data was the crystal size which showed no significant differences between fro/fro and oim/oim bone tissue at 3 months of age.

Table 5.

Bioassay results of long bone diaphyses (stand. dev.).

Calcium (µM/mg)
PO4 (µM/mg)
Hydroxyproline (µg/mg)
Crystal size (nm)
3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo. 3 mo. 6 mo.
fro 535.78 266.36β 9.34b 23.83
(85.8) (40.42) (3.9) (6.2)
F/P 712.25 316.04 9.56 20.13
(100.7) (37.61) (4.7) (4.5)
oim 705.09 687.81 431.44a 341.79 3.41 5.15 23.40 18.31
(245.2) (262.2) (164.6) (73.9) (1.1) (1.4) (9.1) (6.4)
Bl/6 708.33 768.74 349.59 377.52 7.01 5.28 19.88 21.94
(163.3) (114.5) (69.4) (45.9) (2.0) (1.3) (4.1) (4.7)
a

Different from WT of the same age.

b

Different from oim/WT of the same age.

β

Trend different from oim/WT of the same age p ≤ 0.1.

Discussion

There are 2 major components of bone that determine the strength of the tissue: type I collagen and the hydroxyapatitic mineral [21]. The overall goal of this study was to better understand the interrelationship between these components in bone fragility. Therefore, we compared the tissue level and geometric properties of mouse models of bone fragility to elucidate the specific tissue level differences between these models. The defect in the fro/fro mouse has been identified as deficient mineralization of the osteoid by osteoblasts with normal collagen production while the oim/oim mouse possesses a mutation in the collagen type I gene resulting in reduced collagen production and misalignment of collagen fibrils [22]. We found in this study that the bone tissue of the oim/oim and fro/fro mice differed in the amount, distribution, and type of mineral. The relative mineral content and heterogeneity (distribution width) in young fro/fro animals are less than those in age-matched oim/oim bones, which may reflect a defect in bone turnover as well as mineral deposition. The degree of carbonate substitution of fro/fro cortical hydroxyapatite was also more homogeneous than oim/oim at both time points. This can be due to either stoichiometric differences in how carbonate substitution occurs in these animals or a difference in the age of the bone tissue. It has also been suggested that the stoichiometry of non-collagenous proteins (NCP) may also be abnormal in OI bones [23], which may contribute to abnormal mineral deposition and crystal growth. For instance, previous studies in our lab have shown that the NCP osteopontin [2426] and the proteoglycan biglycan [27] both regulated apatite growth and proliferation.

In previous studies, a more homogeneous mineral/matrix distribution was found in osteoporotic human bone [15, 28] and in dogs with reduced bone turnover due to bisphophonate treatment [29]. Accordingly, fro/fro bone, which has both decreased mineral density and decreased mineral heterogeneity, is more easily fractured than oim/oim bone in young animals, as demonstrated from the increased rib deformities that greatly decrease postnatal survival in this model [5]. As both genotypes age, their mean mineral density becomes similar to wild type bone while the distribution width increases to normal levels in the fro/fro tissue and remains high in oim/oim tissue. How the above tendencies in mineral content and composition relate to the age-related changes in tissue level and whole bone mechanical properties between the genotypes has yet to be elucidated.

Like oim/oim animals, the defect in fro/fro animals appears to result in deposition of a malformed ECM in addition to decreased matrix mineralization by fro/fro osteoblasts. It has long been held that the anomalous mineral phenotype of oim/oim bones is due to the abnormal collagen packing [22, 30] and higher levels of mature collagen crosslinks have been found in OI patients [31]. Even though there is no genetic defect in the collagen of fro/fro animals, we found trends indicating that heterogeneity of the collagen crosslinking parameter was very different the mutant animals compared to WT, though this result was not significant due to our small sample size. The heterogeneity of mature collagen crosslinks was reduced in young animals, while, at 6 months, the distribution width of this parameter in fro/fro animals increased 17% compared to a 9% decrease in WT. This indicates that the range of mature collagen crosslinks becomes more heterogeneously distributed in the fro/fro animals by 6 months. In contrast, oim/oim mice have increased amounts of collagen crosslinking at 6 months, and a consistently more heterogeneous distribution of this parameter over time. In both genotypes, the increased collagen crosslinking may be due to abnormal packing of the collagen fibers, which has been documented for oim/oim [32] and also observed in electron microscopic images of fro/fro tissue in this study.

Increased crosslinking of non-mineralized collagen fibrils may have contributed to the rapid increase in the distribution of mature collagen crosslinks in the fro/fro mouse. The TEM images showed small, widely spaced collagen fibers, which may reduce the number of crosslinks that can occur in young animals. As the tissue matures and the fibers grow, there will be increased collagen packing permitting the increase in collagen crosslinking thereby providing a permissive environment for mineralization. Indeed, we do see a concomitant increase in the heterogeneity of the mineral density in cortical tissues with age. This hypothesis is further supported by evidence from, Sricholpech et al., which demonstrated that inhibition of collagen crosslinking in MC3T3 cells resulted in accelerated collagen fibrillogenesis, large collagen fibers, and delayed mineralization [33]. We have previously shown that decreased collagen maturity was associated with atypical fractures in humans [34] and our current results show that mature crosslinks in the oim mutant are more heterogeneously distributed at both time points. This indicates that there is a normal range of collagen maturity in healthy bone and that falling on either side of it results in fragile bone. The collagen defect in the fro/fro mice may be the result of the disruption of the pathway that regulates collagen generation, which may involve observed abnormalities in proteoglycan expression and other non-collagenous proteins [24, 26, 35, 36]. Smaller collagen bundles have been noted in the periosteum of fro/fro bones using electron microscopy [5] and we see smaller, disorganized collagen fibers in the bone tissue. Opsahl et al. found that, as a consequence of decreased dentin sialoprotein (DSP), mineralization is impaired in the fro/fro teeth, and that the DSP deficiency was correlated with an accumulation of glycosaminoglycans [35]. There is also evidence that an interaction between the core protein of decorin and collagen governs the rate and extent of collagen fibrillogenesis [3739]. Specific staining for chondroitin sulfate/dermatan sulfate glycosaminoglycans was appreciably enhanced in fro/fro dentin [40]. Taken together, these results suggest that the Smpd3 defect impacts the matrix deposited by osteoblasts. Therefore, it appears that the mineralization defect of fro/fro bone tissue is not solely due to a deficiency in cell-regulated mineralization of the osteoid, but due to the deposition of an abnormal matrix that is stoichiometrically insufficient for the progression of normal mineral crystal nucleation and/or growth.

The specific role of ceramide in matrix production remains unclear. In cartilage degradation studies, it was found that the production of collagen and proteoglycans is dependent on the concentration of ceramide, with lower concentrations having an anabolic effect [41]. In the Smpd3−/− mouse, Stoffel et al. found that loss of function resulted in severe chondrodysplasia, but not a mineralization defect [42]. However, they also found that the ceramide levels in these mice were not altered. Khavandgar et al. have demonstrated that the mineralization defect in fro/fro mice is completely rescued in fro/fro;Col1a1-Smpd3 animals where nSMase2 expression is restricted to osteoblasts [14], which supports the role of nSMase2 in the mineralization process. They further found that sphingomyelin expression is normal while ceramide levels are decreased in fro/fro mice. Their work suggests that ceramide deficiency and the loss of downstream signaling pathways are the course by which mineralization is disrupted. Our data suggests that these pathways regulate matrix organization, and their disruption may lead to imbalances in collagen generation and fiber organization as well as proteoglycan synthesis and turnover [40]. Defects in both of these macromolecules may contribute to the defective mineralization of the tissue. Continued analysis of the specific tissue abnormalities resulting from the Smpd3 defect should be undertaken to further elucidate the contribution of specific components of the osteoid to subsequent mineralization of the matrix in this model. More importantly, this model can be used to determine the role of nSMase on matrix organization and bone cell function to potentially identify additional treatment strategies for bone fragility that focus on producing normal osteoid rather than increasing tissue mineral density.

The geometric properties of the bone in both mutant animals changed with age to a greater extent than in the wild types. The defect in tissue properties of the fro/fro bone appears to correct itself with age whereas the makeup of the oim/oim bones remains steady with age in all of the IR parameters measured. Micro-CT results, which were consistent with the small body size and bone lengths [43], indicate that the geometry of the oim/oim mouse bones was also fairly steady with age relative to wild type. However, in fro/fro mice, there were perceptible changes in the bone geometry, especially in the trabecular bone. This redistribution of tissue with age may be an adaptive response to more rapidly changing loading conditions in the fro/fro mice. The change in fro/fro trabecular geometry with time is consistent with models of bone formation showing that increased mineral density of trabecular tissue (stiffer tissue) leads to increased Tb.Th and decreased Tb.N [44, 45] and parallels observed changes in the trabecular bone of OI patients [46]. The observed increase in trabecular thickness may result as trabeculae fuse and contribute to the decrease in the number of trabeculae and increase in Tb.Sp with time.

In summary, our data indicates that, despite the lack of a specific genetic collagen defect in fro/fro mice, the fragility in both oim/oim and fro/fro genotypes is related to the deposition of an abnormal matrix that results in atypical mineralization. It would be interesting to perform similar analyses on human OI tissue to determine the contribution of specific collagen production and processing defects to the organization of the matrix and its subsequent mineralization.

Acknowledgments

The authors would like to thank Dr. Eve Donnelly for her help with FTIRI data processing. The work was supported by NIH #1F32AR057295 (RC), NIH #AR046121 (AB) and NIH #RR024547 (AB).

Footnotes

Disclosures

All authors state that they have no conflicts of interest.

Authors' roles: Study design: RC and AB. Study conduct: RC and AB. Data collection: RC, AL, AQ, and LL. Data analysis: RC. Data interpretation: RC and AB. Drafting manuscript: RC. Revising manuscript content: RC, CP, and AB. Approving final version of manuscript: RC, CP, and AB. RC and AB takes responsibility for the integrity of the data analysis.

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