Bone modeling, remodeling, and skeletal health in children and adolescents: mineral accrual, assessment and treatment

Article information

Ann Pediatr Endocrinol Metab. 2017;22(1):1-5

Publication date (electronic) : 2017 March 31

doi : https://doi.org/10.6065/apem.2017.22.1.1

Chiara Maggioli, MD, Stefano Stagi, MD

Department of Health Sciences, University of Florence, Anna Meyer Children's University Hospital, Florence, Italy.

Address for correspondence: Stefano Stagi, MD. Department of Health Sciences, University of Florence, Anna Meyer Children's University Hospital, viale Pieraccini 24, Florence, Italy. Tel: +39-055-5662405, Fax: +39-055-5662400, stefano.stagi@yahoo.it

Received 2017 March 22; Revised 2017 March 31; Accepted 2017 March 31.

Abstract

Introduction

Osteoporosis in adults is one of the major causes of morbidity and mortality because of its association with fragility fractures1). The peak bone mass (PBM) is well known as a key determinant of the lifetime risk of osteoporosis. In fact, childhood and adolescence are a critical time for bone development, mineralization, and the attainment of a PBM2). Therefore, osteoporosis prevention begins by optimizing bone mineral gains over an individual's growing years3).

During childhood and adolescence, bone linear growth and bone mineral accrual proceed in different ways and velocities in various skeletal sites2). In particular, the growth of the appendicular skeleton is prevalent before puberty, whereas that of the spine mostly occurs later. During peripuberty, the areal bone mineral content (BMC) and bone mineral density (BMD) in the lumbar spine and proximal femur increase fourfold to sixfold. At the same time, the diaphyses of the long bone increase twofold4).

Puberty is also the time of major gender differences in bone growth, particularly in terms of bone size and bone mass content. The bone mass accrual rate usually follows sex-specific patterns that are similar to those of height velocity but are delayed by about 6–12 months (Fig. 1). Therefore, the peripubertal period is characterized by relatively undermineralized bones and a higher risk of fractures until the PBM is achieved. In fact, the increase in bone mass and density carries on for several years after the end of linear growth. The exact time when bone accrual ceases is unknown, but it is estimated to be during the young adult age. In particular, it is specific for different sites: it ranges from 16 to 18 years for the spine and femoral neck, and up to 35 years for the skull4).

Fig. 1

(A) Growth of bone mass in relation to height growth velocity and difference in peak bone mass between males (♂) and females (♀). (B) Difference in peak bone mass between males (♂) and females (♀) and factors and diseases that influence the peak bone mass and the risk of osteopenia/osteoporosis in adulthood.

Among many factors that drive skeletal growth, the genetic factor plays a key role in the variability of PBM5). Genome-wide association studies have discovered numerous genes involved in this process. Polymorphisms in the genes encoding the vitamin D receptor, estrogen receptor, insulin-like growth factor-I, type I collagen, transforming growth factor beta, and interleukin 6 are the most intensively studied, but recently, some genes that also seem to influence BMD in children and osteoporosis in adults have been recognized. Aside from heritable factors, environmental factors, such as diet, physical activity6), and hormonal status, modify the complex mechanism of cellular interactions leading to bone accrual.

Multiple hormonal signals regulate bone growth and turnover. In addition to the well-known parathyroid hormone (PTH), calcitonin, thyroid hormones, the growth hormone, and sexual steroids, other hormones, cytokines, and growth factors with endocrine, paracrine, and autocrine actions have been the focus in an increasing number of studies. Bone cells and the skeletal matrix itself produce and contain many signals that influence bone growth; furthermore, neighboring muscle and adipose tissue exert significant 2-way interactions, with the skeleton contributing significantly to the final adult bone density7). Particularly, as shown by recent studies, a higher muscle mass and greater brown adipose tissue volume are associated with a greater cortical bone density and thickness8).

Definition

Osteoporosis in childhood and adolescence is a condition characterized by a low BMD or BMC (z-score ≤-2.0, adjusted for age and gender) and the presence of a clinically significant fracture history9).

Causes

Pediatric osteoporosis recognizes 2 pathogenetic pathways that can contribute to the development of this condition—defects in bone accrual and mineralization, and excessive bone resorption. The causes of osteoporosis are included into 2 large groups, which identify primary and secondary osteoporosis. Primary osteoporosis is a rare disease that is mainly related to genetic defects leading to an intrinsic bone abnormality10). Osteogenesis imperfecta, through its various clinical phenotypes, is the most common genetic disease. Fractures, blue sclera, a short stature, joint laxity, and hearing loss are typical features of osteogenesis imperfecta. Other genetic defects include some rickets, calcium and phosphorus metabolism alterations, and genetic syndromes, such as Marfan syndrome, Paget disease, and Ehler-Danlos syndrome (Table 1). Secondary osteoporosis in childhood is more frequent than primary osteoporosis (Table 2). Systemic chronic inflammatory diseases, malabsorption disorders, endocrinopathies, neoplastic diseases, and medications are the most common causes of secondary osteoporosis. Furthermore, prolonged immobilization can lead to a decrease in BMD, determining the reduction of mechanical stress on the bone. Among medications, many drugs can interfere with calcium and vitamin D absorption and metabolism, or adversely work directly on bone metabolism. Glucocorticoid-associated osteoporosis (GAO) is an iatrogenic condition that leads to an impaired BMD. Glucocorticoids work both on calcium metabolism and directly on bone cells. Particularly, calcium gastrointestinal absorption is impaired, and urinary excretion is increased. The effect on bone cells is characterized by a transient early phase of increased bone resorption through stimulation of osteoclasts. Conversely, in the long term, the major determinant of damage is impaired bone formation. Osteoblastogenesis is reduced, and apoptosis of osteoblasts and osteocytes is increased11). The osteoblastic function to stimulate the synthesis of type 1 collagen is also impaired. Moreover, glucocorticoid can alter bone metabolism through extra skeletal actions. Altered growth hormone synthesis and hypothalamic-pituitary-gonadal function are frequently involved in GAO. Because of accelerated muscle catabolism, glucocorticoid myopathy can have a role in bone damage. Furthermore, glucocorticoids can worsen bone damage, induced by an underlying inflammatory disease, and result in an increased risk of fractures. Prolonged inflammation indeed alters bone metabolism, which favors bone resorption in different ways. Interleukin 1 and interleukin 6 stimulate osteoclastogenesis through receptor activator of nuclear factor kappa-B ligand; therefore, collagen synthesis and osteoblast differentiation are impaired, and osteoblast apoptosis is increased1213).

Table 1

Causes of primacy osteoporosis in children and adolescents

Table 2

Main conditions potentially causing an altered bone density and/or quality in childhood

Malabsorption and celiac disease are the most common causes of bone damage. A low BMD and impaired bone growth in childhood are caused by reduced calcium and vitamin D absorption, as well as secondary hyperparathyroidism. In these patients, a strictly gluten-free diet significantly improves bone mineralization14).

Many endocrinopathies affect bone health. Alterations in PTH metabolism, as well as thyroid hormones, the growth hormone, cortisol, and sex steroids, influence bone growth and accrual. Furthermore, type 1 diabetes impairs the attainment of the PBM, which increases the long-life risk of fractures1516).

The main mechanism underlying this association is a defect in osteoblast differentiation and activity because of many contributing factors, such as insulinopenia and pro-inflammatory cytokine production. Moreover, other mechanisms involved include hyperglycemia, oxidative stress, and the accumulation of advanced glycation end products that compromise collagen properties17).

Diagnosis

A diagnosis of bone disease requires clinical assessment, laboratory, and imaging. Some conditions, such as primary osteoporosis, also need genetic investigation and bone biopsy. In this section, I describe the specific tools that are currently used in the diagnosis of osteoporosis.

Dual-energy X-ray absorptiometry (DXA) is a widely available technique that is used to investigate BMC and BMD918). In association with a history of fractures, BMD evaluation is required to make a diagnosis of osteoporosis in children and adolescents. However, in pediatric patients, the correct reading of DXA is affected by several limitations. The T-score parameter is not applicable to children because it refers to the BMD value upon PBM achievement. The z-score is the index used in childhood and adolescence up to 20 years. It is adjusted for age, gender, and ethnic group, but it does not consider weight and height variability19). Therefore, in children with a short stature or delayed puberty, their BMD is underestimated. In fact, these patients have smaller bones compared with their peers. Unlike the T-score, the z-score without a fracture history cannot be used to characterize “osteoporosis,” whereas the term “reduced bone density according to chronological age” should be used if the z-score is below -2.0 standard deviation, according to the International Society for Clinical Densitometry20).

Quantitative computed tomography (QCT) is an excellent alternative to DXA because it can evaluate cortical and trabecular compartments, as well as volumetric bone density. High-resolution QCT also assesses the microarchitecture of the bone and is useful in evaluating bone strength. However, the use of QCT is limited by its high cost and higher radiation than that of DXA21).

Quantitative bone ultrasonometry (QUS) is a radiation-free approach to investigate bone mineral status in childhood. This method is fast to execute and cheap. Through measurements of the speed of sound, broadband ultrasound attenuation, stiffness factor, and bone transmission time, QUS can give information on not only density but also elasticity, microarchitecture, and thickness2223). However, at present, no evidence on the diagnostic accuracy of QUS in the pediatric population is available, although several studies have demonstrated its correlation with densitometric parameters. Therefore, in consideration of its characteristics, QUS cannot replace DXA, but it can be integrated to it.

Therapeutical approaches

The first approach to pediatric osteoporosis is prevention, if possible. This approach consists of identifying those patients at risk of bone disease and counseling them about lifestyle and dietary calcium and vitamin D supplementations. Several studies suggest that physical activity in childhood is an effective strategy to achieve the optimal PBM24). Secondary osteoporosis is treated by removing the underlying specific cause. The drugs approved for pediatric use in osteoporosis are limited. When the main mechanism of osteoporosis is bone resorption, treatment with an antiresorptive agent is the appropriate choice. Several studies demonstrated bisphosphonate utility in severe osteoporosis and in primary prevention in some conditions as glucocorticoid-induced osteoporosis, although this practice is not yet recommended25). Therefore, bisphosphonates are used in some genetic forms, such as osteogenesis imperfecta. The recombinant human parathyroid hormone, an anabolic agent that is effective in adults, is unavailable for children because of the risk of osteosarcoma. Indeed, this association with osteosarcoma is well demonstrated in rats in many studies, but it remains theoretical for humans26).

Conclusions

Osteoporosis in childhood and adolescence is characterized by reduced bone density (z-score≤2) associated with fragility fractures. This condition during an individual's growth years can alter bone mineral accrual, which leads to insufficient bone peak mass. It is a well-recognized risk factor for adult bone fragility. Primary osteoporosis is caused by genetic defects that lead to bone abnormality, whereas secondary osteoporosis results from multisystemic, often chronic, diseases, or their treatments. Prevention consists of a healthy lifestyle, physical activity, and optimal calcium and vitamin D intake. Therapy depends on the pathogenesis involved; in severe osteoporosis, bisphosphonates are recommended.

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