Sialolithiasis develops from salivary gland calculi and leads to salivary gland obstruction and recurrent painful swelling of the involved gland. A 54-year-old Japanese man had experienced right submandibular swelling since 1995, but he left it untouched because there were no severe symptoms. Eventually, he noticed an increase in swelling and pain, and thus he was referred to our clinic in October 2018. Computed tomography revealed hard tissue of about 30 × 20 mm located in the gland body. The patient underwent surgical extraction of the submandibular salivary gland under general anesthesia in December 2018. Energy dispersive x-ray fluorescence analysis revealed that the main components of the sialolithiasis were Ca: 78.6% and P: 21%. Histological analysis showed atrophy and fibrosis of the submandibular salivary gland. In this report, we present this case of an asymptomatic submandibular giant calculus left untreated for 24 years.
sialolithiasis, submandibular gland
Sialolithiasis is calculus formation that occurs due to mineralization within the duct lumen of debris such as bacterial colonies, epithelial cells, and/or mucus buffers. It often occurs in the submandibular gland, and it is more common in middle age [1]. Typical symptoms are colic pain and swelling in the lower jaw when eating, and the size of the calculus is usually several mm. The pathological condition is characterized by the obstruction of a salivary gland or its excretory duct due to the formation of calculi, resulting in salivary ectasia and even determining the subsequent dilatation of the salivary gland [2]. Pain and swelling occur in occasional cases, and may be localized or diffuse. When present, symptoms are more severe in cases in which the duct is blocked for a long time, and they may be intensified during meals [3]. Pain may gradually decrease with salivary flow and may also be related to infection [4]. The occurrence of fever and local reactive lymphadenopathy is thus highly likely [5]. However, less frequently, the patient may be asymptomatic, regardless of the size of the calculus [1] Calculi tend to develop in the submandibular gland and can vary in size from less than one millimeter to a few centimeters at their largest diameter, but they are typically less than 10 mm in diameter. Giant calculi are defined a those exceeding 15 mm in any one dimension [6]. Here we report the case of a 54-year-old Japanese male with asymptomatic giant right submandibular calculi left untreated for 24 years.
A 54-year-old Japanese male was referred to our clinic with a chief complaint of swelling and pain in the right submandibular region. He had experienced the swelling in 1995 but he left it untouched because there were no severe symptoms. He noticed an increase in the swelling and pain, and thus he was referred to our clinic in October 2018. According to his history, the patient was under treatment for hypertension. His blood pressure was 120/96 mmHg, and he was diagnosed with old myocardial infarction and atrioventricular block leading to bradycardia on the basis of an electrical cardiograph; however, neither of these conditions has pathological significance. A clinical examination found obvious swelling in his right submandibular area (Figure 1). The mass-like swelling was palpable and was the size of walnut. The mass had an elastic soft texture, mobility, and was painful when touched. Intraorally, the right mouth floor mucosa was reddened, mildly swollen, and tender. Yellow-white viscous liquid spilled out from the sublingual salivary papilla. A panoramic X-ray examination revealed a curved, elliptical radiopaque mass in the right submandibular salivary gland region (Figure 2A). Evaluation of the bone window on Computed tomography (CT) revealed a hard tissue about 30 × 20 mm in size located in the gland body (Figure 2B). No neurological disturbance of the facial, lingual, or sublingual nerve was evident. Based on the examinations, a clinical diagnosis of right submandibular sialolithiasis resulting in submandibular sialadenitis was made. To reduce inflammation, amoxicillin 750 mg/day was orally administered for 4 days. In December 2018, the patient underwent surgical extraction of the submandibular salivary gland under general anesthesia after the inflammation was reduced. Figure 3 shows the facets of the submandibular gland and the internal calculi. The calculi were flexed in line with the mylohyoid muscle, and the surface was rough and grayish-yellow in color. Figure 4 shows the hematoxylin-eosin staining of the extracted submandibular gland, and the main composition of the region was inflammatory saliva tissue. Mild-to-severe migration of lymphocytes and plasmacytes, which are chronic inflammatory cells, was observed around the salivary tissue. Some salivary tissue degenerated into adipo-tissue. Acinic cells had atrophied, and the saliva duct was extended as a result of migration of the inflammatory cells. The pathological diagnosis was chronic sialadentitis and sialolithiasis. The calculi were analyzed using energy dispersive x-ray fluorescence (EDX-7000, Shimadzu, Tokyo, Japan) (Figures 1-3). The main components of the sialolithiasis were Ca: 78.6%, P: 21%, S: 0.25%, Fe: 0.07%, and Cu: 0.04% (Figure 5). The patient has remained in good condition since the surgery.
Figure 1. Clinical picture of the patient. Arrow head, right submandibular gland swelling
Figure 2. Panoramic X-ray (A), 3-D CT image (B)
Figure 3. Photo of the calculus in divided submandibular gland
Figure 4. Histology of the submandibular gland. The acinic cells atrophied and the saliva duct was extended as a result of the migration of inflammatory cells (×100)
Figure 5. Energy dispersive x-ray fluorescence spectrum and the components of the calculus. A-C: Spectrum (cps/uA) of the energy dispersive x-ray fluorescence. D: Components of the calculus
Most salivary calculi are about 10 mm in diameter, and those 10 mm in diameter or smaller account for about 70 to 90% of the total, but this case was estimated to have increased to 30 x 20 mm over a long period of time [7]. Although most giant glandular calculi are associated with pain, particularly when located within ducts [8], this patient was completely asymptomatic. This absence of symptoms may have been related to the incomplete obstruction of the duct, which enabled the secretion of some amount of saliva and thus allowed the calculus to develop without symptoms, as has been suggested in other cases [9]. Due to the absence of symptoms, the patient did not seek dental care, allowing the calculus to increase in size over a long period of time. It is important to point out that even in asymptomatic cases; giant calculi should be removed as soon as possible to avoid the potential for complications such as atrophy of the gland, parenchymal fibrosis, sialadenitis, or even extra-oral fistula [10]. In this case, the extracted submandibular gland was contained inflammatory and degenerated saliva tissue. Although the exact etiology is unknown, calculi are thought to occur as a result of the deposition of mineral salts around an initial nidus consisting of salivary mucin, bacteria, or desquamated epithelial cells [11]. Salivary stagnation, increased alkalinity and calcium content of the saliva, inflammation or infection of the salivary duct or gland, and physical trauma to the salivary duct or gland may predispose an individual to calculus formation [12]. Calculi are believed to be more common in the submandibular duct system for the following reasons: (1) the submandibular excretory duct is wider in diameter and longer; (2) the salivary flow in the submandibular gland goes against gravity; (3) the submandibular salivary secretion is more alkaline than the parotid saliva; (4) the submandibular saliva contains a greater quantity of mucin proteins [13]. As in this case, the calculus might increase in size, becoming a giant calculus, and remain asymptomatic for a long period if the calculus is located in a duct that is able to dilate, thus allowing normal secretion of the salivary flow around the calculus [8].
In general, the components of salivary calculi are mainly inorganic substances, with small amounts of organic substances. About 80% of the components are inorganic substances, including about 70% calcium phosphate and about 10% calcium carbonate, magnesium phosphate, iron oxide, etc [14]. The constituents of the submandibular salivary calculus are Ca and P as the main components, and also Mg, Na, Cl, Si, Fe and K [15]. The constituents of the parotid salivary calculus also include Ca, P, Mg, S, Cl, and K. [16]. The constituent elements of the salivary calculus in this case were mainly Ca (78.6%) and P (21.4%), and S, Fe, and Cu were also observed. On the other hand, Ca, P, S, Mg, Na, K, and Cl have been detected as constituents of a small salivary gland calculus[17]. Calcium oxalate and phosphocalcium were found in a component analysis of a kidney calculus [18]. These findings suggest that Ca and P are common as the main components of salivary calculi and other calculi in the body.
The symptoms begin whenever the lumen of the Wharton duct is obstructed by a salivary calculus, with the resultant accumulation of saliva causing pain and swelling of the involved gland. Although our patient had been asymptomatic for 24 years, salivary stasis may have resulted in a rise of bacteria into the glandular parenchyma, and thus may eventually have caused recurrent infections. Long-term obstruction of the saliva flow and recurrent infections may have resulted in salivary tissue degenerating into adipo-tissue and ultimately fibrosis [19].
Most submandibular calculi are detected as radiopaque formations in plain radiographs and as radiolucent filling defects in sialography. Approximately 20% of calculi are not radiopaque, and sialography or sialendoscopy may be required to diagnose them. Salivary calculi are usually unilateral and do not cause dry mouth [20]. Bodner evaluated various imaging modalities for the diagnosis of giant calculi and found that panoramic radiograph and axial CT were comparable in their precise preoperative estimation of calculus size [6]. CT is very accurate at detecting and defining the location of salivary calculi. Sialography is rarely indicated and should be restricted to cases of sialadenitis related to radiolucent calculi [21]. CT scans have become the preferred modality for detecting gland salivary calculus, because they are not invasive like sialography [2]. The 3D-CT image analysis in this case showed that the salivary calculus was bent at a right angle by the mylohyoid muscle and had a shape that matched the shape of the submandibular gland.
The ultimate objective of giant calculus treatment is to restore a normal salivary flow. Whenever the calculus can be palpated intraorally, the best option is to remove it through an intraoral approach [22]. Sialadenoscopy, which is a non-invasive technique, can be used to manage large calculi as well as ductal obliteration. The CO2 laser, because of its advantages of minimal bleeding, less scarring, clear vision, and minimal post-operative complications, is gaining its popularity in the treatment of sialolithiasis [21]. However, removal of the submandibular gland is indicated for submandibular gland calculi with recurrent infections, as in this case.
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Informed consent was taken.
All authors have contributed equally in the treatment, data collection, data analysis or interpretation and writing this paper.
None of the authors have any conflict of interest.
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