FCU is a forearm muscle that proximally fastens at the medial epicondyle and distally attaches to the palmar surface of the pisiform, and then inserts into the hamate and fifth metacarpal bones as the pisohamate and pisometacarpal ligaments, respectively. FCU acts as the wrist flexor and adductor and such as a palmaris longus tendon, has no sheath, and therefore, does not cause tenovaginitis and stenosing tendon disorders. Calcific tendinitis also known as calcific periarthritis, peritendinitis calcarea, periarthritis calcarea, calcific bursitis, calcareous tendinitis and bursitis and hydroxyapatite rheumatism of the hand and wrist has been reported in the literature. The first description of acute calcific tendinitis of the wrist goes back to 1924 by Cohen and since then, several reports have been published.
Two large series including 209 patients with calcific tendinitis of the hand and wrist have been assessed by Carroll et al. (
9) and Yelton and Dickey (
10). They revealed that this entity is much more common than previously thought and the wrist is more affected than fingers. The most common site of calcification at the wrist is the distal insertion of FCU tendon on the pisiform.
Most cases of calcific tendinitis commonly occur between the ages of 30 and 60; however, no age is spared (
11). Men and women are equally involved (
10). Although calcific tendinitis is frequently asymptomatic in the shoulder, it is almost always symptomatic in the hand and wrist (
2,
9,
10). The exact cascade of events that results in calcific deposition is not fully understood and still under question. Several authors have attributed this condition to tendon degeneration, hypoxia caused by poor blood supply, and trauma, while others have proposed that the calcifications are a cell-mediated reactive process. Uhthoff et al. explained local hypoxia induced by mechanical, metabolic, or other factors that lead to degeneration and metaplasia of the tendon to the fibrocartilage that results in calcification by chondrocytes (
12).
Repetitive strain injuries and trauma cause stress necrosis and chronic inflammation, which have been postulated by Carroll et al. (
9) as an etiology of such calcifications. Certain types of activity, such as sudden repeated motions and certain occupations such as typing, golfing or violin playing are more associated with this entity (
13). Moyer et al. (
14) presented cases of calcific tendonitis of the hand and wrist without a history of repetitive trauma or strain which considered to be idiopathic.
Calcific tendinitis is much more common at few conditions such as gout and rheumatoid arthritis (RA). Metabolic abnormalities could be associated with soft tissue calcification in hypervitaminosis D, hyperparathyroidism, and chronic renal failure. Hormonal disorders such as estrogen and thyroid hormones by Harvie et al. (
15) and adult-onset diabetes mellitus by Mavrikakis et al. (
16) are postulated as other possibilities that lead to calcific tendinitis. Gartner (
17) and Sengar et al. (
18) described an HLA-A1 gene predisposition with calcific tendinitis and Gohr et al. (
19) suggested matrix vesicles could be the origin of the pathologic calcification.
Some researchers suggest that calcifications occur due to tendon degeneration, but most others believe that these are two distinct entities and have several differences. The age of inception of calcific tendinitis is earlier than that of degenerative tendinopathy (
20). Calcific tendinitis may resolve, unlike degenerative tendinopathy. Calcific tendinitis occurs in viable tissue, but degenerative tendinopathy occurs in necrotic tissue (
21). Deposits at calcific tendinitis are hydroxyapatite and have a different chemical composition compared to degenerative tendinopathy (
22).
Seldom, calcific tendinitis may be seen before the onset of symptoms. Symptoms of calcific tendinitis are not due to the calcification itself and appear to happen when the calcific deposit rupture to adjacent soft tissue and result in acute inflammatory response consequently (
23,
24).
On clinical examination, the disease is presented by tenderness over the distal tendon at the wrist which could be worsened by wrist flexion or ulnar deviation against resistance. Typically, the symptoms begin abruptly and initially are localized at the volar aspect of the ulnar side of the distal forearm and wrist but eventually are limited directly over the pisiform and distal of FCU within few days. Other symptoms such as swelling and erythema may be present as well.
Due to the rarity of calcific tendinitis at the distal insertion of FCU, and nonspecific symptoms, imaging has a fundamental role in the diagnosis of tendinopathy and calcific tendinitis.
Radiography is the primary and most used modality for evaluating calcific tendinitis (
25). It is cost-effective and calcium deposits and their extension and density could be easily detected. Characteristically, degenerative joint evidence is usually absent (
26).
Calcifications have been classified into two groups based on the shape and border on radiography (
21,
26). In most cases, heterogeneous deposits with the fluffy appearance and ill-defined contour correlate with the acute symptomatic phase of calcific tendinitis, while the discrete homogeneous calcifications with well-defined edges are mostly seen in asymptomatic patients. Calcifications are usually amorphous and have varying shapes and sizes with irregular borders. Localized obliteration of fascial planes over the pisiform secondary to edema could be seen in the acute phase of calcific tendinitis (
4). Over time, calcifications become less well-defined or hazy and may fragment and eventually disappear or markedly decrease in size (
9). Rarely, calcifications are not visible on plain radiographs as in this case and may need other modalities for confirmation (
21).
Computerized tomography (CT) is not routinely used for the diagnosis of calcific tendinitis. On CT, the appearance of calcification mirrors the radiographs (
27). CT is the best modality for evaluating osseous involvement and cortical erosion and intramedullary extension of calcifications which is most often seen inside the femur and humerus and is very rare in the wrist and hand (
28). CT is also helpful for localizing the disease to a tendon and confirming calcific tendinitis (
27).
MRI is the second most commonly used modality after radiographs, performed for evaluation of calcific tendinitis, as it shows the presence of calcification and helps to characterize the extent of the inflammation and exclude other causes of joint pain. Sagittal plane provides a better diagnostic view for evaluating the full length of FCU tendon attachment on the pisiform. On MRI, the degree of soft tissue inflammation depends on the stage of the calcification.
Fluid sensitive MR images show soft tissue edema typically surrounding the region of calcification in the symptomatic phase. Calcifications present as focal areas of low signal on all pulse sequences located within or near the tendon insertion, although small deposits may be difficult to see by MRI and need radiography or ultrasonography for confirmation (
29).
Ultrasonography is less expensive, easily accessible and the most-useful modality for the evaluation of hand and wrist tendons. Ultrasound is not routinely used for the diagnosis of calcific tendinitis, but it is useful particularly when calcification happens at shoulder tendons and is commonly used in image-guided therapeutic procedures. Longitudinal views of FCU tendon are obtained at the parasagittal plane while the wrist is mildly dorsiflexed. Within normal tendon, smooth tangential fibers are visible as echo-bright parallel thin lines that taper distally to attach on the pisiform. Tendinopathy causes loss of normal fibrillar pattern, hypoechogenicity, hypervascularity, and tendon thickening. Farin et al. (
27) believe that although sonography is reliable in the recognition and localization of calcifications but it is unable to classify the pathophysiologic stage of calcifications in hand and wrist tendons. Because of this restriction and for evaluating bony abnormalities, they postulated that radiographs should be obtained in combination with ultrasound examination in calcific tendinitis for further confirmation. Increased flow on color Doppler is seen in symptomatic phases but is present in only about one-third of cases and is not necessary for diagnosis (
30).
The acute calcific tendinitis has a very good prognosis. Carroll et al. (
9) and Strandell (
24) reported resolution of symptoms in untreated patients takes a long time, approximately three weeks. Immobilization by splinting and treatment with NSAIDs shortens the symptomatic period to 7 - 9 days (
9). The success rate of nonsurgical interventions is high. Invasive treatment including local injection of anesthetic or steroid agents, aspiration of calcium deposits, surgical excision of calcific deposition and lysis of peritendinous adhesions are also available but are usually kept for severe cases that have not responded to conventional treatments and when symptoms last for more than several weeks (
8).
In conclusion, due to the rapid clinical course, it is important to make the diagnosis early to prevent unnecessary interventions. The initial diagnosis is almost always incorrect. Infection and fractures must be included in the initial differential diagnosis to avoid terrible misdiagnosis. If a patient has erythema, localized pain, restricted motion and ectopic calcification on radiographs over the tender point, without a history of trauma or findings in favor of infection, acute calcific tendinitis must be considered in the differential diagnosis. Sonography and MRI could be employed for an accurate diagnosis. Increasing knowledge and awareness about this condition lead to an earlier diagnosis without exposing the patient to unnecessary interventions.