Bone strength and management of postmenopausal fracture risk with antiresorptive therapies: considerations for women's health practice.

Bone strength - and, hence, fracture risk - reflects the structural and material properties of the skeleton, which changes with bone turnover during aging and following effective pharmacotherapy. A variety of powerful new techniques (quantitative computed tomography, as well as peripheral quantitative computed tomography and high-resolution peripheral quantitative computed tomography) provide precise images of bone structure and can be used to model the response of specific bones to different types of mechanical load. This review explores the various components of bone strength and the clinical significance of measures, such as bone mineral density, bone turnover markers, and modern imaging data, with regard to fracture risk in women with postmenopausal osteoporosis, before and after initiating antiresorptive therapy. These imaging and related techniques offer an ever-clearer picture of the changes in bone structure and bone mineral metabolism during normal aging and in osteoporosis, as well as in response to treatment. However, because the newer techniques are not yet available in routine practice, validated tools for absolute fracture risk assessment remain essential for clinical decision making. These tools, which are tailored to patient risk data in individual countries, are based on bone mineral density and other readily available clinical data. In addition, bone turnover marker measurements can be useful in assessing risk and guiding treatment decisions for women with postmenopausal osteoporosis. Such tests may be used before starting a patient on antiresorptive therapy and for ongoing monitoring of treatment effectiveness.

Introduction

The human skeleton is well designed to resist physical insults, but bone, like other materials, will break under a sufficiently great load. Bone strength is therefore defined as resistance to fracture, and fracture provides the most clinically meaningful indicator of bone strength in primary care. Fragility fractures – those that occur with minimal trauma, such as in falls from standing height – clearly demonstrate decreased bone strength. Indeed, a history of fragility fractures in peri- and postmenopausal women is strongly associated with a risk of future fractures.1

What is bone strength?

Bones are hard because they consist of hydroxyapatite crystals, set in a matrix of collagen and other connective tissue. They owe their strength not just to their composition (bone mineral density [BMD]), but also to their structure – their overall size and shape, along with their microarchitecture.2 Viewed up close, every bone has a complex microarchitecture, with pores and channels running through the apparently solid cortex (Figure 1). Inside the cortex is the medullary cavity, where bone tissue is not solid, but spongy in appearance, consisting of an extensive cross-linked mesh-work of projections (trabeculae).

Figure 1

Structure of trabecular (spongy) and cortical (compact) bone tissue.

The distribution of trabecular and cortical tissue varies across anatomical sites, with the vertebrae containing >75% trabecular bone and long bones, such as the femur, containing >75% cortical bone.3 At the microarchitectural level, features also differ. Trabecular tissue varies with regard to the number of trabeculae, as well as their length, thickness, and degree of cross-linking. Cortical bone is of variable thickness and porosity (the number and size of pores). Both trabecular and cortical bone may also show microcracks as a result of mechanical loading.

These features, which greatly influence the overall mechanical strength of the bone, are all in a state of flux: bone is constantly being turned over and replaced by resident osteoclasts and osteoblasts.2,4 Because loss of bone strength leads to increased risk of fracture, antiresorptive agents and other interventions that reduce bone turnover can improve bone strength and reduce fracture risk in women with postmenopausal osteoporosis (PMO).5,6

Patterns of age-related bone loss

Women commonly experience some degree of bone loss as they age, particularly as their estrogen levels decline during and after menopause.7 Along with this loss of BMD, bone microarchitecture changes in several ways, including: loss and thinning of trabeculae, which reduce cross-linking between neighboring trabeculae; expansion of the medullary cavity (cortical thinning) as the inner endosteal surface is eroded by an imbalance in bone turnover;8 and increased porosity within the cortex itself.9 Each of these changes will ultimately lead to loss of bone strength and increased fracture risk.

The timing of increased fracture risk varies among different women, reflecting both the peak bone mass they reached in their youth and the rate at which they lose BMD during the years around menopause.10 In addition, the relative timing of mineral loss from the cortical and trabecular compartments can vary among different bones, due to differences in bone architecture and load.11

In general, trabecular bone loss occurs first, largely affecting the spine and resulting in compression fractures. Although often unnoticed clinically, these fractures can lead to height loss.12 Trabecular bone loss begins by age 40, when women still produce substantial levels of estrogen; approximately a third of a woman’s lifetime loss of trabecular bone occurs in the decades before menopause. Trabecular bone loss accelerates with estrogen deficiency for the first 4–8 years of menopause, after which it continues at a lower rate.13

Because the vertebrae contain a large proportion of trabecular bone, it is expected that vertebral fracture risk begins to rise relatively early in life, as trabecular BMD declines.14 However, the large majority (80%) of osteoporotic fractures are nonvertebral, occurring in bones, such as the wrist and the hip, where cortical thickness is a key predictor of bone strength and stiffness.15 In Canada and the US, the majority of these nonvertebral fractures occur in the wrist.16,17

As postmenopausal women age, BMD loss moves from trabecular bone to the inner cortex, where loss of mechanical strength appears to drive the growing risk of nonvertebral fractures.14,18,19 Changes in the cortex occur by cortical thinning and increased cortical porosity – that is, erosion of the bone tissue on the inner (endosteal) surface and also within the cortical compartment. Endosteal resorption produces porous structures resembling trabeculae.7,18 This process is observed in the earlier years of menopause and accelerates after age 65,18 and continues at a lower rate even into extreme old age.18,20 Likewise, cortical porosity appears to increase in a woman during her 40s to 50s in different bones and continues indefinitely (Figure 2A).9,19 Cortical bone loss is strongly related to estrogen deficiency7 and accelerates after menopause,18 playing a major role in nonvertebral fractures later in a woman’s life.

Figure 2

Postmenopausal changes in bone architecture.

Notes: (A) Micrographs of femur sections from two women, aged 78 and 90 years. The inner surface of the 78-year old’s femur shows ongoing erosion (“endocortical trabecularization”) and also increasing porosity within the cortex. In the 90-year old’s femur, cortical porosity is extensive and the inner compartment has expanded, leaving a thin cortex. Reprinted from Lancet, 375/9727, Zebaze RM, Ghasem-Zadeh A, Bohte A, et al, Intracortical remodelling and porosity in the distal radius and post-mortem femurs of women: a cross-sectional study, 1729–1736,18 copyright 2015, with permission from Elsevier. (B) Progressive expansion of the medullary space (dotted arrows) occurring during and after menopause is accompanied and partially offset by deposition of new mineralized tissue on the outer surface of the periosteal apposition (solid arrows). Bar charts show the effects of endocortical resorption and periosteal apposition before (Pre), during (Peri) and after (Post) menopause. Because appositional growth slows over time, while endocortical resorption accelerates, there is a progressive thinning of the cortex, decreasing bone strength. Reproduced from Szulc P, Seeman E, Duboeuf F, Sornay-Rendu E, Delmas PD. Bone fragility: failure of periosteal apposition to compensate for increased endocortical resorption in postmenopausal women. J Bone Miner Res. 2006;21(12):1856–1863.23 Copyright ©2006, with permission from John Wiley and Sons.

Aging is also associated with an adaptative expansion of the outer diameter of bones (periosteal apposition),20–22 which occurs throughout adult life. As a result of appositional growth on the outer (periosteal) surface, along with erosion on the inner (endosteal) surface, the cortex is gradually displaced outward. At the same time, the cortex thins, because periosteal growth does not keep up with endosteal resorption (Figure 2B). Following menopause, cortical loss accelerates and periosteal appositional growth declines. In long bones, these changes lead to substantial loss of bending strength.13,23

Measures of bone strength

Bone strength assessment in clinical practice generally relies on standard radiological (eg, dual-energy X-ray absorptiometry [DXA]) and laboratory tests (eg, serum bone turnover markers [BTMs]). Validated prognostic tools incorporate patient history and clinical observations, along with DXA findings, to estimate an individual’s absolute risk of fracture over the following 10 years (eg, the Canadian Association of Radiologists and Osteoporosis Canada Tool [CAROC] and the WHO Fracture Risk Assessment Tool [FRAX]). However, some newer mechanical modeling approaches that use high-resolution imaging data have had impressive success predicting whether and how a bone will fracture in a fall. Insights from these studies are important for primary care and fracture prevention, because they confirm that available treatments improve bone strength and reduce fracture risk by reversing some of the microarchitectural changes associated with aging bone.

Here, we discuss a variety of tools and measurements used to assess bone strength and fracture risk. We consider how these tools demonstrate different components of bone strength and the effects of pharmacotherapy on fracture risk in women with PMO.

Measuring bone strength: tools of the trade and what they tell us

Clinical measures of bone strength provide clues to a patient’s risk of suffering a fracture. As shown in Table 1, not all of these tools are widely used in clinical practice. However, all offer insights into the loss of BMD with aging, as well as the material and structural changes to the bone that occur during effective pharmacotherapy.

Table 1

Clinical and experimental evaluation of bone strength: some common approaches

Technique	Outcome	Used in clinical practice?	Advantages	Limitations
Imaging
DXA	Areal (2D) BMD	Yes, widely accessible	Validated in peri- and postmenopausal population; used in conjunction with medical history and clinical findings to estimate absolute 10-year fracture risk	Low precision, hence provides no insight into bone microarchitecture; trabecular and cortical BMD viewed collectively
QCT	Low-resolution (~500 μm) volumetric (3D) BMD (vBMD), which can be further analyzed by mathematical modeling	No; typically used in a research setting	Resolves trabecular and cortical compartment BMD in hip and spine	No insight into microarchitecture; not validated as a prognostic tool in osteoporosis
pQCT	Low-resolution (300–500 μm) vBMD, which can be further analyzed by mathematical modeling	No; typically used in a research setting	Resolves trabecular and cortical compartment BMD in tibia and radius	Not validated as a prognostic tool in osteoporosis; not used for imaging vertebral bone
HR-pQCT	High-resolution (~60–82 μm) vBMD, which can be further analyzed by mathematical modeling	No; research tool only	Detailed microarchitecture of peripheral bones, particularly radius and tibia. Low radiation dose per exposure (0.003 mSv vs 0.13 mSv for standard HR-pQCT use)43,79	Not validated as a prognostic tool in osteoporosis; not used for imaging vertebral or hip bone
Mathematical modeling
FEA	Estimate of whole bone strength	No; typically used in a research setting	Allows modeling of outcomes following falls or other specific types of mechanical load	Not validated as a prognostic tool
Polar moment of inertia	Bone’s ability to resist torsion	No
Biochemistry
Bone turnover markers	Analysis of blood or urine to identify products of osteoclast (resorption) or osteoblast (formation) activity	Yes	Inexpensive, safe, and noninvasive; rapid response following treatment; changes may be maintained during treatment	Not standardized Not validated as prognostic tools

Abbreviations: BMD, bone mineral density; vBMD, volumetric bone mineral density; DXA, dual-energy X-ray absorptiometry; FEA, finite element analysis; mSv, milliSievert; pQCT, peripheral quantitative computed tomography; QCT, quantitative computed tomography; HR-pQCT, High Resolution-peripheral quantitative computed tomography.

DXA

DXA is used to assess the “areal” BMD, meaning the mass of bone mineral per unit area when this mass is projected onto a 2D surface, as in an X-ray image. By definition, a reduction in BMD indicates the extent of mineral loss from the bone, but it measures the mineral mass of cortical and trabecular bone collectively and does not identify the compartment where mineral is lost.

Uses and limitations of DXA

While DXA correlates with incident fracture rate, in the postmenopausal years 60% of nonvertebral fractures occur in women who have nonosteoporotic BMD,24 highlighting a limitation of using this measure on its own as an indicator of fracture risk.2 DXA scans can also be used to calculate a Trabecular Bone Score (TBS). This approach, which uses grayscale variations in the scanning data to quantify trabecular bone density, is broadly predictive of incident fractures in postmenopausal women. In some at-risk populations, such as individuals with diabetes or primary hyperparathyroidism or those receiving long-term glucocorticoid therapy, it has been suggested that the TBS can improve fracture prediction, relative to DXA alone. Conversely, in postmenopausal women, TBS so far has not proved superior to standard DXA measurements of the hip (reviewed in Bousson et al25).

For practical purposes, estimates of 10-year absolute fracture risk (AFR) overcome some of the limitations of DXA by incorporating other patient data, including age, medical history, and prior fracture.26,27 Comorbidities that affect bone strength without necessarily changing BMD in a predictable way, such as glucocorticoid-induced osteoporosis,28,29 are included in these AFR tools. Canadian guidelines recommend AFR estimated by the Canadian FRAX30 or CAROC tools (which are ~90% concordant) be used in preference to DXA alone to identify patients who will most benefit from pharmacotherapy.26,31 Recent updates of the FRAX tool for some jurisdictions now allow the user to include the TBS, if available, as a component of AFR evaluation.32

Use of BMD in treatment monitoring

At the population level, antiresorptive treatment clearly reduces vertebral and nonvertebral fracture risk in PMO.5,6 To monitor the effectiveness of therapy, DXA scans are usually repeated every 1–3 years, with a decrease in testing once the patient appears to have responded.26,31

In clinical practice, maintenance or increase in BMD is traditionally taken as evidence of decreased fracture risk in patients treated with antiresorptives, such as oral bisphosphonates. However, the optimal frequency of testing and the most useful target BMD have not been established.33–35 Moreover, it is common in many areas to restrict follow-up DXA to a single scan unless the patient’s risk factors for fracture change.

Ongoing DXA monitoring would be justified by clear evidence showing that BMD predicts incident fracture in women on therapy, as it does in treatment-naïve women. Indeed, one study of women on antiresorptives showed that a DXA T-score that remains in the osteoporotic range (≤−2.5) predicts continued high risk of incident fracture.36 In addition, prospective, placebo-controlled trials using potent antiresorptive agents have shown good correlations between BMD change and incident fracture rate.5,6

The clearest evidence of such link in women with PMO comes from a study of denosumab, an inhibitor of the receptor activator of nuclear factor kappa B ligand, which is essential for the formation, function, and survival of osteoclasts. Austin et al reported strong correlations between changes in total hip BMD and the incidences of vertebral and nonvertebral fracture over 3 years.37 As shown in Figure 3, total hip BMD increased in most subjects on denosumab, while declining or remaining unchanged in most placebo-treated subjects. For every 1% increase in total hip BMD, there was a 3% decrease in nonvertebral fractures (Figure 3A) and a 4.9% decrease in new vertebral fractures (Figure 3B). This relationship between the increase in total hip BMD and reduced fractures persists out to 6 years of treatment.38

Figure 3

Improvement in total hip BMD with 3 years of denosumab treatment predicts incident of nonvertebral (A) and vertebral (B) fractures in women.

Note: Reprinted from Austin M, Yang YC, Vittinghoff E, et al. Relationship between bone mineral density changes with denosumab treatment and risk reduction for vertebral and nonvertebral fractures. J Bone Miner Res. 2012;27(3):687–693,37 with permission from John Wiley and Sons.

Abbreviation: BMD, bone mineral density.

Another study, which followed women on zoledronic acid in a prospective manner over 3 years, found a similar relationship between change in BMD and fracture risk.39 Based on these two studies, it appears that BMD increase can serve as a surrogate for improved bone strength in the treatment setting, at least in patients receiving relatively potent antiresorptive drugs. Thus, ongoing monitoring with DXA may provide helpful guidance in deciding whether to maintain or switch therapy.

QCT, pQCT, and HR-pQCT

Quantitative computed tomography (QCT) and related techniques use X-ray tomography to generate an average BMD for a whole bone or a specified volume within the bone.40,41 This volumetric BMD measurement differs from the standard (areal) BMD reported by DXA scanning, because it calculates the mass of mineral within a volume of the bone tissue, rather than a 2D projection of the bone.

Structural changes affecting bone strength can be seen using each of these imaging technologies.40,42–44 QCT and peripheral QCT (pQCT) can show internal bone structure with a resolution of 300–500 μm.40,41 These techniques separate a bone’s trabecular and cortical compartments, allowing the average BMD to be determined separately for each compartment. With high-resolution pQCT (HR-pQCT), the resolution is generally ~60–82 μm.45,46 Thus, while pQCT is generally not able to resolve internal structures within the compartments,47 HR-pQCT shows this structure with considerable detail.48 Using HR-pQCT, researchers can observe and quantify specific microarchitecture changes, such as thinning of the bone cortex and the specific location (eg, the inner cortex), an increase in the size or number of cortical pores, or the loss of trabecular cross-links.43

Uses and limitations of QCT, pQCT, and HR-pQCT

As shown in Figure 4, different classes of bone mineral loss (endosteal cortical thinning, increased cortical porosity, and loss of trabeculae) may have essentially identical effects on BMD but different effects on bone strength.40,49,50 Using HR-pQCT imaging, it is possible to improve estimates of fracture risk, particularly in women who are not in the “osteoporotic” range by DXA but have low BMD (T-scores between −1 and −2.5).51

Figure 4

Identical T-scores in bones with different structural features.

Notes: All four images are of the distal radius. Despite having the same BMD, the microarchitecture and biomechanical properties of the bone vary substantially. The images on the right show loss in the trabecular compartment; those on the right have lower cortical vBMD and greater cortical porosity. Reproduced from J Biomech, 44/2, Kazakia GJ, Burghardt AJ, Link TM, Majumdar S, Variations in morphological and biomechanical indices at the distal radius in subjects with identical BMD, 257–266,50 copyright 2015, with permission from Elsevier.

Abbreviations: BMD, bone mineral density; vBMD, volumetric bone mineral density; aBMD, areal bone mineral density.

Complementing the material and structural data from HR-pQCT and pQCT measurements are several mathematical models for estimating bone strength. These analytic tools, such as finite element analysis (FEA, which models bone strength and the bone’s ability to resist fracture under different kinds of mechanical load) and polar moment of inertia (PMI, reflecting the bone’s ability to resist torsion), are adapted from engineering, where they are used to analyze the mechanical strength of various structures.

FEA has been used successfully even with low-resolution structural data from DXA scans, leading to improved prediction of hip fractures, relative to DXA alone.49 However, FEA and PMI are most powerful when applied to data from higher-resolution QCT and related methods that capture cortical and trabecular structure.40,41,43,52 Using FEA to model the strength of the imaged bone, researchers can model the outcomes of specific kinds of impact, such as a femoral neck fracture resulting from an unprotected sideways fall, and the changes in these parameters when patients are treated for osteoporosis.52–54

In a study of older adults (average age 75 years), femoral neck BMD proved to be a good surrogate for hip strength measured by QCT FEA. This finding is significant for clinical practice because it helps confirm the value in fracture risk assessment of the femoral neck BMD T-score, which is central to the CAROC and FRAX tools.55

Limitations of HR-pQCT and pQCT include motion artifacts (particularly for the distal forearm with HR-pQCT), and the inability to image clinically important sites, such as spine and hip. HR-pQCT is generally used for just two sites in the peripheral skeleton, the distal tibia and distal radius43 while pQCT can image mid-shaft tibia and occasionally mid-femur. Conversely, QCT can be used for imaging central skeletal sites, such as the spine and hip, although with its limited resolution, it provides less precise information about changes in bone microarchitecture. Another limitation is that these techniques cannot inform us regarding the nonmineral aspects of the bone matrix, such as cells and collagen, which provide toughness to the bone. Turnover of these nonmineral components is not evaluated by imaging in the clinical setting but may be assessed biochemically.

BTMs

Complementing the insights of medical imaging, BTMs are biochemical markers that can be assayed in the serum or urine to follow changes in bone remodeling. BTMs measure either bone resorption by osteoclasts (eg, the cross-linked collagen telopeptides CTX and NTX) or bone formation by osteoblasts (eg, serum procollagen type 1 N-terminal propeptide; bone-specific alkaline phosphatase; and serum osteocalcin).

Markers of bone resorption and formation tend to rise or fall together; most commonly, both are high, as in PMO; more rarely, both are low in certain “low-turnover” states, such as adynamic bone disease.56,57 This is because bone resorption and bone formation are tightly coupled, with osteoclasts and osteoblasts acting together on the bone surface.58 However, coupling does not mean that resorption and formation always remain in balance. On the contrary, in postmenopausal women, increased bone remodeling is associated with excess bone resorption, and high BTM levels (resorption or formation markers) correlate loosely with lower BMD and reduced bone strength.5,59

Uses and limitations of BTMs

BTMs offer a rapid and inexpensive test for changes in bone remodeling, commonly responding within days to weeks of the initial treatment with an osteoporosis agent,35,58,60–62 much sooner than BMD changes can be measured. For this reason, they offer an early indication that the patient is responding to therapy as expected.35

This reassurance may be helpful for managing patients with high AFR and high BTMs at baseline. For instance, one study followed outcomes in high-risk women on bisphosphonates (alendronate or risedronate) and found that about a fourth experienced an inadequate treatment response, defined as multiple incident fractures and/or significant BMD loss over 3 years. This outcome was significantly associated with elevated levels of the BTM bone-specific alkaline phosphatase, both at baseline and the end of the study period.63

BTM responses seem to be maintained over the course of treatment, at least in clinical trials. At the population level, elevated BTMs are associated with increased fracture rates, an effect that seems to be independent of BMD in older women.14,35,58,62 In principle, these findings suggest that BTM testing could be incorporated into routine fracture risk assessment. However, validated risk assessment tools, such as FRAX, so far have not included BTMs. This is due in part to a lack of standardization of BTM assays, and in part to the substantial intra- and inter-individual variability seen with these markers, including dietary and circadian effects.35,58,62

BTMs in treatment monitoring

BTM changes associated with treatment vary among different antiresorptive therapies, due to differences in their mechanisms and duration of action and potency.26,64,65 No standardized set of BTM tests has been validated in women undergoing treatment for PMO.33,58,66 Thus, it has been suggested that the primary benefit of BTM monitoring is to encourage treatment adherence.59

For physicians wishing to use BTMs to monitor response to therapy, Canadian guidance suggests that serum CTX be examined before and 3–6 months after the onset of antiresorptive treatment; patients who show a <35% decrease in serum CTX should be asked about their adherence and any side effects that might be limiting their use of the therapeutic agent. Conversely, those who respond may be maintained on therapy, with regular but infrequent monitoring of serum CTX to detect changes in bone remodeling.66

Impact of antiresorptive therapy on bone strength

Although both denosumab and bisphosphonates are antiresorptive medications, they differ with regard to compartmental access in the bone. Bisphosphonates are preferentially adsorbed into trabecular bone, which has a high surface area per volume. Once incorporated into the bone mineral matrix exposed during the initial phase of the resorption lacunae, bisphosphonates are taken up by osteoclasts, causing apoptosis and, subsequently, reduced bone resorption. In contrast, because denosumab acts in the extracellular milieu to inhibit osteoclast formation, function, and survival, it inhibits resorption in both trabecular and cortical bone (Figure 5).67 The Osteoporosis Canada Clinical Practice Guidelines recommend denosumab and bisphosphonates (alendronate, risedronate, and zoledronic acid) as first-line antiresorptive therapies to significantly decrease vertebral, hip, and nonvertebral fracture risk.26

Figure 5

In trabecular bone, osteoclasts engulf matrix containing alendronate, whereas denosumab accesses osteoclasts via the extracellular fluid.

Notes: Because cortical bone has a low surface area/mineralized bone matrix volume, alendronate cannot be adsorbed as readily into the cortical compartment. In contrast, denosumab is not adsorbed onto mineralized bone matrix but circulates freely, thus inhibiting resorption of cortical and trabecular bone more equally.

Head-to-head fracture trials comparing fracture outcomes of these agents have not been conducted. However, there have been several head-to-head studies investigating the impact of denosumab compared to bisphosphonates on indices of bone strength.60,68–71 Denosumab significantly increased BMD (by DXA) at all cortical and trabecular sites measured, relative to bisphosphonates, in subjects who were either treatment-naïve60 or transitioning from a prior bisphosphonate treatment.68,69 At the distal 1/3 radius (a highly cortical site),72,73 a novel analysis of images obtained after in an HR-pQCT study showed that 1 year of denosumab treatment resulted in a more rapid and profound reduction in bone resorption, as well as a 1.5–2.0-fold greater reduction in cortical porosity, relative to alendronate (Figure 6).71 These findings complement data from the original 1-year study, which showed that denosumab significantly increased cortical volumetric BMD and calculated bone strength or PMI in the distal radius and distal tibia compared to alendronate.70

Figure 6

Restoration of bone mass over 12 months of antiresorptive therapy in the distal radius of women with PMO.

Notes: (A) Declining porosity in the compact-appearing cortical bone. (B) Increasing trabecular bone mass. Modeling studies show strength in the distal radius is closely tied to cortical structure, including thickness and porosity. Reprinted from Bone, 59, Zebaze RM, Libanati C, Austin M, et al, Differing effects of denosumab and alendronate on cortical and trabecular bone, 173–179.71 Copyright 2015, with permission from Elsevier.

Abbreviations: PMO, postmenopausal osteoporosis; BV/TV, bone volume over total volume.

Recent observational data suggest that continued use of denosumab beyond 3 years of treatment resulted in a further significant reduction in nonvertebral fracture risk,74 presumably reflecting the decreased cortical porosity and the improvement in calculated bone strength associated with this treatment.

Conclusion: goals of therapy and implications for everyday practice

The goal of osteoporosis therapy is to decrease fracture risk by improving bone strength. The available clinical data confirm that bone strength can be improved with antiresorptive treatment and that both trabecular and cortical BMD must be maintained and restored to prevent fracture in older women. Long-term studies of 7 to 10 years’ duration indicate that gains in BMD are either maintained75–77 or continue to increase78 at both cortical and trabecular sites with long-term antiresorptive treatment. Similarly, BTMs decline with the onset of treatment and generally remain suppressed over long-term treatment. As a consequence of improved bone strength, fracture incidence may be suppressed over the course of long-term therapy and may even continue to decline with time.74

The newer imaging technologies complement BMD and may give physicians confidence that their therapies are working as intended. While these technologies offer an extraordinary view of the changes occurring with aging, osteoporosis, and antiresorptive therapy, approaches in common use today (DXA, BTMs, and validated fracture risk assessment tools [ie, CAROC, FRAX]) still suffice for routine clinical decision making. Baseline and postinitiation DXA and BTM measurements may provide reassurance that the patient has responded to therapy and that she maintains reasonable adherence to the intended dosing.