Mutations That Alter the Carboxy-Terminal-Propeptide Cleavage Site of the Chains of Type I Procollagen Are Associated With a Unique Osteogenesis Imperfecta Phenotype : C-PROPEPTIDE CLEAVAGE SITE MUTATIONS IN OI
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Abstract
<p class="first" id="P1">Osteogenesis imperfecta (OI) is a genetic bone disorder characterized
by fractures,
low bone mass, and skeletal fragility. It most commonly arises from dominantly inherited
mutations in the genes
<i>COL1A1</i> and
<i>COL1A2</i> that encode the chains of type I collagen. A number of recent reports
have suggested
that mutations affecting the carboxyl-terminal propeptide cleavage site in the products
of either
<i>COL1A1</i> or
<i>COL1A2</i> give rise to a form of OI characterized by unusually dense bones. We
have assembled
clinical, biochemical, and molecular data from 29 individuals from 8 families with
7 different mutations affecting the C-propeptide cleavage site. The phenotype was
generally mild: The median height was ~33th centile. Eighty percent of subjects had
their first fracture by the age of 10 years, and one-third had a femoral or tibial
fracture by the age of 25 years. Fractures continued into adulthood, though rates
varied considerably. Healing was normal and rarely resulted in long bone deformity.
One-third of subjects older than 15 years had scoliosis. The teeth and hearing were
normal in most, and blue sclerae were not observed. Other features noted included
fibro-osseous dysplasia of the mandible and Achilles tendon calcification. The mean
spinal bone mineral density
<i>Z</i>-score was +2.9 (SD 2.1) compared with −2.2 (0.7) in subjects with
<i>COL1A1</i> haploinsufficiency mutations. Bone mineral density distribution, assessed
by quantitative
backscattered electron imaging in bone showed higher levels of mineralization than
found in any other disorder. Bone histology showed high trabecular volume and increased
cortical thickness, with hyperosteoidosis and delayed mineralization. In vitro studies
with cultured skin fibroblasts suggested that these mutations interfere with processing
of the chain in which the sequence alteration occurs, but the C-propeptide is eventually
cleaved (and detectable in blood), suggesting there are alternative sites of cleavage.
The precise mechanism of the bony pathology is not yet clear.
</p>
Osteogenesis imperfecta (OI) is a generalized disorder of connective tissue characterized by fragile bones and easy susceptibility to fracture. Most cases of OI are caused by mutations in type I collagen. We have identified and assembled structural mutations in type I collagen genes (COL1A1 and COL1A2, encoding the proalpha1(I) and proalpha2(I) chains, respectively) that result in OI. Quantitative defects causing type I OI were not included. Of these 832 independent mutations, 682 result in substitution for glycine residues in the triple helical domain of the encoded protein and 150 alter splice sites. Distinct genotype-phenotype relationships emerge for each chain. One-third of the mutations that result in glycine substitutions in alpha1(I) are lethal, especially when the substituting residues are charged or have a branched side chain. Substitutions in the first 200 residues are nonlethal and have variable outcome thereafter, unrelated to folding or helix stability domains. Two exclusively lethal regions (helix positions 691-823 and 910-964) align with major ligand binding regions (MLBRs), suggesting crucial interactions of collagen monomers or fibrils with integrins, matrix metalloproteinases (MMPs), fibronectin, and cartilage oligomeric matrix protein (COMP). Mutations in COL1A2 are predominantly nonlethal (80%). Lethal substitutions are located in eight regularly spaced clusters along the chain, supporting a regional model. The lethal regions align with proteoglycan binding sites along the fibril, suggesting a role in fibril-matrix interactions. Recurrences at the same site in alpha2(I) are generally concordant for outcome, unlike alpha1(I). Splice site mutations comprise 20% of helical mutations identified in OI patients, and may lead to exon skipping, intron inclusion, or the activation of cryptic splice sites. Splice site mutations in COL1A1 are rarely lethal; they often lead to frameshifts and the mild type I phenotype. In alpha2(I), lethal exon skipping events are located in the carboxyl half of the chain. Our data on genotype-phenotype relationships indicate that the two collagen chains play very different roles in matrix integrity and that phenotype depends on intracellular and extracellular events.
Human cortical and trabecular bones are formed by individual osteons and bone packets, respectively, which are produced at different time points during the (re)modeling cycle by the coupled activity of bone cells. This leads to a heterogeneously mineralized bone material with a characteristic bone mineralization density distribution (BMDD) reflecting bone turnover, mineralization kinetics and average bone matrix age. In contrast to BMD, which is an estimate of the total amount of mineral in a scanned area of whole bone, BMDD describes the local mineral content of the bone matrix throughout the sample. Moreover, the mineral content of the bone matrix is playing a pivotal role in tuning its stiffness, strength and toughness. BMDD of healthy individuals shows a remarkably small biological variance suggesting the existence of an evolutionary optimum with respect to its biomechanical performance. Hence, any deviations from normal BMDD due to either disease and/or treatment might be of significant biological and clinical relevance. The development of appropriate methods to sensitively measure the BMDD in bone biopsies led to numerous applications of BMDD in the evaluation of diagnosis and treatment of bone diseases, while advancing the understanding of the bone material, concomitantly. For example, transiliacal bone biopsies of postmenopausal osteoporotic women were found to have mostly lower mineralization densities than normal, which were partly associated by an increase of bone turnover, but also caused by calcium and Vit-D deficiency. Antiresorptive therapy causes an increase of degree and homogeneity of mineralization within three years of treatment, while normal mineralization levels are not exceeded. In contrast, anabolic therapy like PTH decreases the degree and homogeneity of matrix mineralization, at least transiently. Osteogenesis imperfecta is generally associated with increased matrix mineralization contributing to the brittleness of bone in this disease, though bone turnover is usually increased suggesting an alteration in the mineralization kinetics. Furthermore, BMDD measurements combined with other scanning techniques like nanoindentation, Fourier transform infrared spectroscopy and small angle X-ray scattering can provide important insights into the structure-function relation of the bone matrix, and ultimately a better prediction of fracture risk in diseases, and after treatment.
[1
]Department of Medicine; Faculty of Medical and Health Sciences; University of Auckland;
Auckland New Zealand
[2
]Histology Department; Waikato Hospital; Hamilton New Zealand
[3
]Department of Medicine; University of Otago; Wellington New Zealand
[4
]Department of Endocrinology and Metabolism; Aarhus University Hospital; Aarhus Denmark
[5
]McMaster University Medical Center; Hamilton Canada
[6
]Department of Clinical Genetics; Guy's Hospital; London UK
[7
]Institute of Health and Biomedical Innovation; Faculty of Health; Queensland University
of Technology; Brisbane Australia
[8
]Translational Genomics Group, Institute of Health and Biomedical Innovation, Woolloongabba;
Queensland University of Technology; Woolloongabba Australia
[9
]Arnold Palmer Hospital for Children; Orlando FL USA
[10
]Ludwig Boltzmann Institute of Osteology at the Hanusch Hospital of WGKK and AUVA Trauma
Centre Meidling, 1st Medical Department; Hanusch Hospital; Vienna Austria
[11
]Department of Orthopaedics and Sports Medicine; University of Washington; Seattle
WA USA
[12
]Department of Pathology; University of Washington; Seattle WA USA
[13
]Department of Medicine; Division of Medical Genetics; University of Washington; Seattle
WA USA
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