How to define an osteoporotic vertebral fracture?
Editorial

How to define an osteoporotic vertebral fracture?

Daniele Diacinti1, Giuseppe Guglielmi2

1Department of Radiological Sciences, Oncology and Anatomo-Pathology, University Sapienza, Rome, Italy; 2Department of Clinical and Experimental Medicine, University of Foggia, Foggia, Italy

Correspondence to: Giuseppe Guglielmi, MD. Professor of Radiology, Department of Clinical and Experimental Medicine, University of Foggia, Viale Luigi Pinto, 71100 Foggia, Italy. Email: giuseppe.guglielmi@unifg.it.

Abstract: A vertebral deformity (VD) is not always a vertebral fracture (VF). Because of lack of a completely satisfactory “gold standard”, there is no consensus on the exact definition of a VF. Therefore, it may sometimes be difficult, especially in mild cases, to discriminate the prevalent VF from a non-fracture deformity or short vertebral height (SVH). A combined standardized approach based on qualitative and semiquantitative (SQ) vertebral assessment may be the most option to correctly identify a VD as a VF. However this visual approach for VF identification is subjective, therefore it is mandatory an adequate training and experience of radiologist to reach a good sensitivity and specificity. Vertebral morphometry, objective and reproducible method, could be used only to evaluate the severity of VFs but requires the availability of reference values of vertebral height ratios. There is actually an evidentiary basis for suggesting that a qualitative approach by expert radiologists to morphological vertebral assessment, combined SQ and morphometric methods seem to be the preferred option for the correct diagnosis of VF as endplate or/and cortex fracture (ECF) or severe vertebral height loss.

Keywords: Vertebral fractures (VFs); vertebral deformities (VDs); endplate or/and cortex fractures (ECFs); semiquantitative vertebral assessment (SQ vertebral assessment); algorithm-based qualitative (ABQ); vertebral morphometry


Submitted Sep 03, 2019. Accepted for publication Sep 06, 2019.

doi: 10.21037/qims.2019.09.10


Introduction

Vertebral fractures (VFs) are the hallmark of osteoporosis. They are the most common of all osteoporotic fractures, occurring in 15% among women 50–59 yrs of age and in 50% among women >85 years of age (1-4). The majority of osteoporotic VFs are asymptomatic and occur in absence of specific trauma (5,6). However, even these mild VFs could have clinical consequences for the patient because of the increased, approximately 5-fold, risk of future fractures that may be symptomatic (7-10). Multiple VFs are associated with an increased mortality rate (11-13) and impaired quality of life (14-17). As a consequence of that, the radiologic report of a VF strongly induces the physician to introduce a full bone fragility assessment, and if necessary, offer proper anti-osteoporotic treatment. Nevertheless, their relevant clinical impact, a high percentage (mean 30%) of the mild VFs remain undiagnosed, and then a proper therapeutic intervention is omitted (18-23). The diagnosis of VFs is usually based on the presence of a deformation of vertebral body on lateral spinal radiographs, but a vertebral deformity (VD) isn’t always a VF (24,25). Because there is no consensus on the exact definition of a VF, it may sometimes be difficult to discriminate the prevalent VF from a normal variant of vertebral shape or from a vertebral deformation that may have occurred long ago especially in mild cases.


VF definition

Osteoporotic VF appears as an alteration in the shape and size of the vertebral body, associated or not to vertebral height loss, resulting as a wedge, end-plate (mono-or biconcave), or collapse VD. There are three approaches for VFs identification on conventional radiographic and dual X-ray absorptiometry (DXA) spine images: a qualitative visual approach, a semiquantitative (SQ) assessment method and morphometric quantitative methods.

SQ method

The visual SQ method proposed by Genant et al. (26) is more commonly used for identifying VF for vertebrae T4 to L4. Visualization of vertebrae T1–T3 and L5 is often limited due to overlying of the shoulders and of the pelvis, respectively. Anyway, osteoporotic VF above T4 is also very rare. Vertebra L5 is also subject to considerable morphologic variation between individuals, such that very often vertebral Ha measurement is much larger than posterior height (Hp). VF assessment (VFA) according to SQ method is based on vertebral height reduction. So, a vertebra is graded on visual inspection of the Ha, middle, or Hps as normal (grade-0), mildly deformed (grade-1, a 20–25% reduction in one of the three heights and a reduction of area 10–20%), moderately deformed (grade-2, a 25–40% reduction in any height and a reduction in area of 20–40%), and severely deformed (grade-3, a 40% or more reduction in height and area). Congenital or acquired non-osteoporotic VDs, which may mimic osteoporotic VD (oVD) in appearances, are systemically excluded (27). Though it has been suggested that SQ method provides a good performance for the diagnosis of prevalent and incident VFs, when utilized by expert and trained radiologist (28). More recently, some authors (29,30) noted that consistently and precisely estimating the extent of height loss according to Genant’s criteria is difficult. In particular, Lentle et al. (31) and Wáng (30) suggested that the narrow range of Genant’s SQ grade-1 height loss, i.e., 20–25%, can cause much inconsistency and difficulties for population studies, and many reported epidemiological differences between regions and ethnic groups could be largely due to methodology imprecision and inconsistency. Since an osteoporotic VF does not necessarily have a height loss, or does not necessarily have a height loss ≥20%, Wáng (30) further proposed a modified SQ criteria, i.e., mild VF with <20% vertebral height loss; moderate mild VF with 20–34% vertebral height loss; severe VF with >34% vertebral height loss. Deng et al. (32) and Wáng et al. (27) reported that vertebrae with >34% height loss always showed radiographical sign of endplate or/and cortex fracture (ECF). Thus severe grade would be always ECF (+). This modified SQ criteria may be more practical daily clinics, such as, if height loss is more than 1/3 of the vertebra, then it is severe grade (approximately >34%); if height loss is less than 1/5 of the vertebra, then it is mild grade (<20%) (33). Worsening of a VF, e.g., progression from grade-1 to -2, has been commonly considered to be equivalent to an incident fracture. In a recent study, Wáng et al. (27) used the criteria that an incident fracture is defined as a qualitative VF occurred in a vertebra that was not deformed at baseline [i.e., standard deviation (SD) grade-0], which could be either a change from grade-0 at baseline to grade-2 or grade-3 VD at follow-up, or a change from grade-0 at baseline to grade-1 VD with at least 10% height loss during the follow-up period. If a normal vertebra (grade-0) progressed to grade-1 is considered a new VF without such height loss requirement, then there is a theoretical possibility that a qualitative VF with 18% height loss (may be graded as grade-0.5) progressed to SQ grade-1 VF with only 2% further height loss during the 4-year follow-up. This may lead to “overcall” of incident new VFs. For an existing VF at baseline, a further vertebral height loss at follow-up of at least 15% or 20% is considered as a VF worsening (27,34), it was suggested that a threshold of >15% further height loss may be more sensitive for epidemiological follow-up studies (27).

Vertebral wedging

VF is more frequent at midthoracic and thoracolumbar levels that are the most biomechanically compromised locations within the vertebral column (35,36).

Vertebral wedging is one of the characteristic features in osteoporotic compression fractures, but may occur in healthy subjects or in developmental abnormalities with or without degenerative changes. The vertebrae bodies changes as size and as shape at different levels of the spine for the construction of thoracic-lumbar curvatures, that reduces bending moments created by upright posture and so provides stability during motion (37). So the spine normally appears with physiological wedging of the thoracolumbar vertebral bodies in healthy subjects. MRI study in asymptomatic healthy subjects, demonstrated that at the thoracolumbar junction (T11–L2 levels) the vertebral bodies are wedge-shaped with A/P ratio of 0.92±0.08 at T10, 0.92±0.08 at T11, 0.90±0.06 at T12, 0.89±0.06 at L1, and 0.90±0.07 at L2 (38).

On aging, anterior vertebral thoracic wedging increases, so the spine bends forward, resulting in spinal deformity (kyphosis) and height loss. An anatomic study on aged cadaveric thoracic and lumbar dissected vertebrae (T1–L5), demonstrated that the vertebral bodies are anteriorly wedged from T1 through L2 (peak at T7), non-wedged at L3, and posteriorly wedged at L4–L5 (peak at L5) (39). In other studies, the vertebral Ha/Hp ratios measured by DXA technique are resulted in women aged 70–82 years as mean of 0.90±0.04 at thoracic level with lower A/P value at T6 as 0.83±0.05 (40).

Therefore, the SQ method assumption that the vertebra body shape is rectangular it is incorrect.

The physiological wedging of vertebral bodies, more evident at T6–T9 spine level, should be taken into account when performing VFA using the criteria of SQ method. So, SQ approach based on vertebral heights reduction may bring equivocal diagnosis for grade-1 VFs that are often either false positive or deformities related to non-osteoporotic diseases of the spine. The assessment of the overall aspect of the spine may help in the identifying the VFs among VDs. Wedging of the vertebral bodies has been reported to occur in patients with disorders of intervertebral disc cartilage endplates including a Schmorl’s node and irregularity of the endplates as Scheuermann’s disease (41). Moreover in aging population anterior vertebral wedging may be due to both underlying VF and osteoarthritis changes (42). For these reasons is particularly difficult to accurately diagnose mild wedge fractures in the mid-thoracic region using only SQ method based on vertebral height reduction (Figure 1).

Figure 1 Radiographs shows VDs anterior wedged-shaped. (A) Moderate VDs (SQ2) anterior wedged-shaped at vertebrae T6, T7 and T8 with central endplate integrity and anterior osteophytes: wedging in osteoarthritis; (B) moderate VDs (SQ2) anterior wedged-shaped at vertebrae T12 with central endplate collapse: VF. VD, vertebral deformity; VF, vertebral fracture; SQ, semiquantitative.

Vertebral endplate collapse: algorithm-based qualitative (ABQ)

In old study (43) it was demonstrated that for differentiation between osteoporotic and osteoarthritis wedging should be evaluated, in addition to Ha/Hp ratio, also the middle/Hp ratio that is exaggerated lower in osteoporotic fracture. Next studies highlighted that there is a relationship between vertebral body deformity and disc degeneration in the aging spine. The central region of the vertebra endplate adjacent to the nucleus pulpous is the weakest area and it is exposed to greater vertical stress than other regions resulting in biconcave deformity (44,45). Genant et al. (46) suggested that for VFA, in addition to vertebral height reductions, the expert and reader have to identify the vertebral shape alterations (as buckling of cortices, the lack of parallelism of endplates, etc.). However, SQ criteria do not require the presence of these radiographic fracture sign to diagnose VF. In order to improve the specificity of VF diagnosis, it has been developed an ABQ with a focus on the appearance of endplate rather than height reduction (47). On a true lateral projection, the superior (or inferior) surface of the normal vertebra exhibits two lines; one line represents one side of the vertebral ring, and the second (more dense) line represents the central endplate superimposed on the opposite vertebral ring. The ABQ assumes that all osteoporotic VFs initially involve concave depression of the center of the endplate within the vertebral ring, that is considered the weakest area. Thus, by definition, wedge and crush fractures are initially concave fractures. If the vertebral ring is displaced with fracture of the lateral or anterior cortex of the vertebral body, will be wedge or crush fracture. The non-fracture deformities with apparent “reduction” in vertebral height without endplate depression are categorized by Ferrar et al. (48) as non-osteoporotic short vertebral height (SVH), as degenerative change and Scheuermann’s disease (Figure 2). Patients with SVH had similar bone mineral density (BMD) values to patients with normal vertebral heights; otherwise patients with concave or biconcave VDs identified by ABQ had BMD values significantly lower. ABQ approach had interobserver agreement for radiographic diagnosis of VFs significantly better than SQ method (49). It has been demonstrated that vertebrae classified as grade-1 VF by ABQ were associated with higher risk of VFs as well as non-vertebral major osteoporotic fracture, while SQ1-VF was not associated with higher non-VF (50). Really, also ABQ method has some limits. Genant et al. assumed that endplate fracture is 100% sensitive for osteoporotic fracture (46), but ABQ approach not include anterior cortex buckling which is quite common as VF sign (Figure 3) (51). Furthermore, endplate fracture does not always occur at the center of endplate (52). Finally, the ABQ do not take account for grading the extent of vertebral height loss.

Figure 2 Vertebral wedge deformities on VFA images. (A) Mild wedge deformities (SQ1) at vertebrae T6 through T11 with undulated endplates, multiple Schmorl’s nodes and disc space narrowing: Scheuermann’s disease; (B) moderate wedge deformity (SQ2) at vertebra T11 with endplate integrity: wedging in osteoarthritis; (C) severe wedge deformity (SQ3) at vertebra T5; mild wedge deformity (SQ1) at vertebrae T11 and L2 with endplate and cortex fracture: VFs. VF, vertebral fracture; VFA, VF assessment; SQ, semiquantitative.
Figure 3 Vertebra T7 deformity (SQ2), with both upper and lower endplate fracture as well as anterior cortex fracture [reproduced with permission from reference (51)] (51). SQ, semiquantitative.

In a recent review (53) are summarized the radiographic morphological signs of osteoporotic VF detectable by an expert reader: (I) anatomic discordance between adjacent vertebrae; (II) loss of parallelism between adjacent end-plates; (III) end-plate disruption as they are impacted into the vertebral body; (IV) fractures of the vertebral anterior cortex or end-plate characterized by cortical discontinuities (ECF); (V) buckling of the vertebral cortex, especially anteriorly. Compared with subjects without ECF subjects with ECF are at a higher risk of short-term (4-year period) deformity progression and new incident deformity (27). It also possible that vertebrae may fracture with pain but without measurable changes in radiographic height or area or endplate disruption and therefore in the absence of any appreciable radiographic VD (54). Furthermore, in a histologic study vertebrae radiographically classified as normal, adjacent to osteoporotic VFs, had histological evidence of endplate fracture and anterior cortical fracture (55). In these cases it is necessary to perform MR exam which may show transient vertebral marrow edema. The altered MR vertebral marrow signal reflects trabecular microcracks and repair of “occult fracture” in “unfractured” osteoporotic vertebrae (53).

Vertebral morphometry: normative data

To reduce the subjectivity of qualitative readings has been introduced vertebral morphometry, method objective and reproducible based on measurements of vertebral height and their ratios (56,57). The SQ method has been enclosed for VFA in the software for computerized vertebral morphometry performed on conventional radiographs or on images obtained by DXA. Last technique perform VFA with a lower radiation exposure dose (<20 µSv) than conventional radiography (600 µSv) (58). VFA results to be reliable and accurate in detecting VFs in adults (59-61) and children (62) with sensitivity and specificity ranging from 62% to 97% and 94% to 99% respectively (63). However, as it is a quantitative method, vertebral morphometry is unable to differentiate between osteoporotic VFs non-fracture VDs, considering also the variability of the normal radiologic appearance of the vertebrae is both among and within individuals (64). A recent study demonstrated the wide difference in osteoporotic VF prevalence when we use qualitative or morphometric radiological approaches (65). To reduce the rate of false positives among the VFs resulted by morphometric methods, normative data for vertebral body height ratios have been established, specific to the technique used (conventional plain radiographs or DXA) and to the population under study.

Some authors obtained means and SDs of vertebral bodies heights from premenopausal women, assuming that the prevalence of VFs is zero (66,67). This approach involves radiation exposure for fertile women and considers nothing effect of age on vertebral morphometry, even if the results are conflicting. The prospective studies following women from pre- to post-menopause did not find a significant decrease in vertebral heights and ratios with age (68,69). Conversely, all the cross-sectional studies reported vertebral heights and also Ha/Hp ratio values significantly lower in older women compared with younger women (70-72). Understanding whether vertebral heights vary with age is necessary because it influences the choice of the normative data. In fact, if it is accepted that vertebral heights change with age, we must derive normal values from a sample of age-matched women, since a VD which may be in excess of 2SD from the mean in younger subjects may be well within this limit 20 years later. So, have been obtained reference values from postmenopausal women both excluding women with VFs (73,74) and including women with VFs using trimming procedures remove the extreme values from the Gaussian distribution (75). To reduce the variation caused by the larger number of deformities has been recommended the use of median and percentile (76) or the use of a modified quantitative approach based on the calculation of standardized vertebral height, referred as standardized quantitative morphometry (SQM) (77). In a multicentric study, we derived reference data for vertebral morphometry by DXA technique (78) as means (± SD) of raw and trimmed data and medians [± interquartile range (IQR)] of vertebral heights and ratios split into decades. The 1,254 Italian consecutive pre- and postmenopausal women, (mean age 63.7±11.3; range, 26–88 years), enrolled in the study had the vertebral heights significantly different to UK and US women, suggesting the need to have reference data specific to the population under study.

There is still disagreement about establishing a threshold of height reduction, which would allow unequivocal discrimination between VFs, VDs, and normal shape. Various morphometric algorithms to define VFs have been developed comparing the Ha or middle height to the Hp within a vertebra and the Hp to the Hp of the adjacent vertebrae above or below (predict posterior) (79,80). Overall, as described by Eastell-Melton and McCloskey (81,82), a prevalent VF is defined on the baseline spine images (radiographs or VFA) if any of the three ratios, Ha/Hp, central/Hp (Hm/Hp), posterior/predicted Hp (Hp/Hp+1 or Hp/Hp−1), is < 3SD the corresponding reference ratio value obtained from population of normal fertile women. Using this method, if the reference T6 Ha/Hp ratio result, for example, 0.83±0.05 (mean ± SD), the vertebra T6 may be considered as VF when the Ha/Hp is <0.68, that is the same as 32% reduction of anterior vertebral height. Therefore, the vertebral height reduction of 20% proposed in SQ method as threshold for VF cannot applicable to any subject, and in the same subject at any spine level. It is necessary the comparison between the vertebral height ratios of examined patient with reference data using cut-off of <3SD to vertebral level mean value or more stringent morphometric criteria (mean-4SD). When we used vertebral morphometry it is necessary to compare the measured vertebral dimensions with normative data. So, as quantitative computed tomography (QCT) and DXA use specific for race, sex and age reference values to evaluate BMD, we suggest to include in the vertebral morphometry software the reference vertebral height ratios specific for the population and probably even for age groups to identify VFs with better accuracy for both epidemiological studies and clinical practice.

Finally, it should be noted that osteoporotic VFs of elderly men and elderly women have distinctly different features, and the above descriptions are primarily based on research results for women. Deng et al. (83) demonstrated that while the overall oVD prevalence is only slightly lower in elderly men than in elderly women (i.e., 13.2% vs. 16.1%), ECF prevalence is substantially lower in men than women (i.e., 5.88% vs. 11.93%). Moreover, 63.2% of the oVDs in men were Genant’s SQ grade-1, while only 30.5% of the oVDs in women were Genant’s SQ grade-1. Osteoporotic VDs in males with 25–34% height loss rarely have ECF, while it is common for osteoporotic VDs in females with 25–34% height loss to be associated with ECF (32). More recently, MrOS (Hong Kong)’s year-4 follow-up shows (33), for male subjects at baseline without VD and ECF, the VD progression/new VD rate during follow-up was half of the paired MsOS (Hong Kong) study’s results for females. For those with baseline VD or ECF, the VD progression/new VD was less than 1/6 of females’ rate. Therefore, the clinical importance of osteoporotic VF in males remains undefined and further works are necessary. The VF evaluation schemes described in this paper are likely to be valid only for elderly women’s osteoporotic VF evaluation (84).

In conclusion, we analyzed the most commonly used methods to define osteoporotic VFs. There is actually an evidentiary basis for suggesting that a combination of qualitative approach by expert radiologists to VFA seems to be the preferred option for correctly diagnose and graduate a VF (85,86). At first, non-osteoporotic deformities should be ruled out by an expert reader to detect the specific morphologic signs of osteoporotic VFs, particularly ECF (51,53). Once the diagnosis of VF is established, then SQ criteria (26) or modified criteria (31) is recommended to grade the severity of vertebral height loss. We suggest to utilize vertebral morphometry only to graduate more objectively the VFs, once qualitatively diagnosed. In this way the radiologist plays a central role in the management of patients with osteoporosis, but an adequate training is recommended by correctly identifying all of VFs (87).


Acknowledgments

None.


Footnote

Conflicts of Interest: The authors have no conflicts of interest to declare.


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Cite this article as: Diacinti D, Guglielmi G. How to define an osteoporotic vertebral fracture? Quant Imaging Med Surg 2019;9(9):1485-1494. doi: 10.21037/qims.2019.09.10