[A PhD completed. More insight into the origin and composition of salivary stones]. / Serie: Hora est. Meer inzicht in het ontstaan en de samenstelling van speekselstenen.

Salivary stones are hardened, stony calcifications that primarily develop in the drainage duct of a salivary gland. They can lead to obstruction of the saliva flow, resulting in swelling and pain. Since the aetiology of salivary stones remains largely unclear, this was further investigated in this PhD study. A case-control review of patient records showed that systemic diseases and lifestyle factors most likely do not play a role in their occurrence. The biochemical composition of salivary stones removed by oral-maxillofacial surgeons was examined, revealing that large salivary stones have a different inorganic composition than small salivary stones. Several salivary proteins were detected in submandibular salivary stones, including lysozyme, s-IgA, and -amylase. Clumping together of these proteins may play a role in the initial formation of salivary stones.

Microbiomic association between the saliva and salivary stone in patients with sialolithiasis.

Salivary stones, known as sialoliths, form within the salivary ducts due to abnormal salivary composition and cause painful symptoms, for which surgical removal is the primary treatment. This study explored the role of the salivary microbial communities in the formation of sialoliths. We conducted a comparative analysis of microbial communities present in the saliva and salivary stones, and sequenced the 16S rRNA gene in samples obtained from patients with sialoliths and from healthy individuals. Although the diversity in the saliva was high, the essential features of the microbial environment in sialoliths were low diversity and evenness. The association of microbial abundance between stones and saliva revealed a positive correlation between Peptostreptococcus and Porphyromonas, and a negative correlation for Pseudomonas in saliva. The functional potential differences between saliva and stones Bacterial chemotaxis and the citrate cycle were negatively correlated with most genera found in salivary stone samples. However, the functions required for organic compound degradation did not differ between the saliva samples. Although some microbes were shared between the sialoliths and saliva, their compositions differed significantly. Our study presents a novel comparison between salivary stones and salivary microbiomes, suggesting potential preventive strategies against sialolithiasis.

Rapid development of a salivary calculus in submandibular gland and its potential causes in a young victim following Russell's viper bite.

Russell's viper bites are known to cause a range of haemotoxic, neurotoxic, myotoxic, cytotoxic and nephrotoxic complications. However, the impact of Russell's viper bites as well as bites from other venomous snakes on sialolithiasis has not been previously reported. Here, we present an interesting case where a Russell's viper bite induced the rapid development of a calculus in submandibular gland in a 10-year-old boy. Upon admission, the victim did not show any symptoms of swelling and/or pain around his oral cavity. He received antivenom treatment to normalise his coagulation parameters, however, on day three he developed swelling and extreme pain around his right mandibular region. An ultrasound investigation revealed the presence of a calculus in his submandibular gland, which was removed using a minor surgical procedure. The histopathological examination revealed this as a poorly calcified salivary calculus, which is composed of cell debris, mucopolysaccharides and lipids. The mechanisms behind its rapid development following a snakebite are unclear although this could be linked to excessive inflammation or modifications to the composition of saliva induced by venom toxins or other unknown factors. This report reveals an unusual complication induced by a Russell's viper bite and alerts clinicians who treat snakebites to be aware of such envenomation effects. Moreover, this will lead to novel research to explore the relationship between venom toxins and functions of salivary glands.

Patient Outcomes After Unsuccessful Endoscopic Sialolith Extraction.

OBJECTIVE/HYPOTHESIS: To evaluate clinical outcomes following failed endoscopic extraction of salivary calculi and to assess any relation between clinical outcome and calculi location, number, size, and mobility. If sialendoscopy fails to extract the calculus, subsequent spontaneous passage of the calculus out of the ductoglandular system or secondary effects of sialendoscopy could mitigate the clinical impact of a residual sialolithiasis. STUDY DESIGN: Prospective observational study. METHODS: Prospective comparative study of endoscopic procedures for sialolithiasis performed in the Manukau Surgery Center, in Auckland, New Zealand, from 2010 to 2020. The recurrent symptoms and the variables related to the need for additional surgical intervention for salivary calculi were analyzed. RESULTS: Among the 465 sialendoscopy procedures, 154 (33.1%) were for obstructive sialolithiasis. Among these, there were 30 (19.4%) with unsuccessful stone extraction with re-operation for these failures performed in 14 of the 27 failed submandibular cases (52%) and 2 of the 3 parotids (66.7%). Location of calculi was a significant factor in predicting the need of further surgery. Patients with perihilar stones were 5 times more likely to have a failed procedure (P = .001). If the stone was intraglandular, the likelihood increased to 8.5 times (P = .005). The likelihood for a revision procedure increased almost 11 times if the stone was intraglandular (P = .004). Calculi size, mobility, multiple calculi, and presence of concurrent stenosis did not correlate with need for further surgery. CONCLUSIONS: A significant proportion of "failed" sialendoscopy did not require further intervention. Stone location was a significant factor in predicting a failed procedure and the need for re-intervention. Laryngoscope, 132:1029-1033, 2022.

Relationship between volume of submandibular salivary stones in vivo determined with Cone-Beam Computer Tomography and in vitro with micro-Computer Tomography / Relación entre el volumen de cálculos salivales submandibulares in vivo determinado con tomografía computarizada de haz cónico e in vitro con microtomografía computarizada

Background: Successful removal of salivary stones depends on exact pretreatment information of the location, thesize and shape of the stones. This study aimed to compare the volume of submandibular sialoliths determined bypreoperative Cone-Beam Computer Tomography (CBCT) scans with the volume of the removed stones on micro-Computer Tomography (micro-CT) scans.Material and Methods: In this study, using twenty-one submandibular sialoliths, the pretreatment volumes in-vivomeasured on CBCT were compared to the volumes of removed stones determined by micro-CT scans. The volumemeasured on micro-CT scans served as the gold standard. Pre-operative CBCT’s and in-vitro micro-CT’s wereconverted into standard tessellation language models (STL-models) using an image segmentation software pack-age. The CBCT and micro-CT images of the stones were subsequently metrologically assessed and compared toeach other using reverse engineering software.Results: Volumes of submandibular sialoliths determined by CBCT’s correlated significantly with volumes mea-sured on micro-CT’s (Spearman’s coefficient r = 0.916). The interquartile range (IQR) for the volume measuredwith micro-CT was 117.23. The median is 26.41. For the volume measured with CBCT the IQR was 141.3 and themedian 36.61. The average volume on micro-CT is smaller than on CBCT.Conclusions: When using CBCT-scans for the detection of submandibular sialoliths one should realize that in-vivothose stones are actually a fraction smaller than assessed on the preoperative scan. This is important when cut-offvalues of sizes of stones are used in the pretreatment planning of stone removal.(AU)

Salivary calculi microbiota: new insights into microbial networks and pathogens reservoir.

Sialolithiasis represents the most common disorders of salivary glands in middle-aged patients. It has been hypothesized that the retrograde migration of bacteria from the oral cavity to gland ducts may facilitate the formation of stones. Thus, in the present study, a microbiome characterization of salivary calculi was performed to evaluate the abundance and the potential correlations between microorganisms constituting the salivary calculi microbiota. Our data supported the presence of a core microbiota of sialoliths constituted principally by Streptococcus spp., Fusobacterium spp. and Eikenella spp., along with the presence of important pathogens commonly involved in infective sialoadenitis.

Biochemical composition of salivary stones in relation to stone- and patient-related factors

BACKGROUND: Salivary stones are calcified structures most often found in the main duct of the submandibular or parotid salivary gland. They contain of a core surrounded by laminated layers of organic and inorganic material. MATERIAL AND METHODS: Submandibular and parotid sialoliths (n=155) were collected at the department of Oral and Maxillofacial surgery of a general hospital between February 1982 and September 2012. The weight of the sialo-liths was determined and the consistency was subjectively classified. Subsequently, the biochemical composition of the stones was determined by wet chemical methods or FT-IR spectrometry. Age and gender of the patients were retrieved from their medical records. Data were statistically analyzed using Fisher's exact tests. RESULTS: Sialoliths are mainly composed of inorganic material. Carbonate apatite was identified in 99% of the stones, phosphate in 88%, calcium in 87%, magnesium in 68%, struvite in 44%, oxalate in 38% and carbonate in 35%. Solid salivary stones contain more frequently struvite than stones with a soft consistency (p = 0.05). Larger stones (> 100 mg) contain more frequently carbonate (p = 0.05). Stones from older patients (≥ 38 years) showed an almost significant trend towards more frequent presence of phosphate (p = 0.083). CONCLUSIONS: The biochemical composition of submandibular and parotid sialoliths is related to stone-related factors, probably to age but not to the gender of the patient

No disponible

Sialólito Gigante em Ducto de Wharton: um caso incomum / Giant Sialolith in the Wharton Duct: An Unusual Case

A obstrução das glândulas salivares por cálculos acomete 90% dessas estruturas, apresentando geralmente tamanho menor que 1 cm. É encontrada, principalmente, nas glândulas submandibulares. Clinicamente, o paciente apresenta um aumento de volume na região referente à glândula salivar envolvida, podendo apresentar sintomatologia dolorosa e drenagem purulenta. O presente artigo relata um caso de sialólito gigante com 2,5 cm de diâmetro, em glândula submandibular, removido cirurgicamente, com preservação funcional da glândula submandibular. O tratamento pode variar de acordo com o tamanho, a forma e localização do cálculo... (AU)

The obstruction of the salivary glands by calculations affects 90% of these structures, usually exhibiting a size smaller than 1 cm. It is mainly found in the submandibular glands. Clinically, the patient presents an increase in volume in the region related to the salivary gland involved and may present painful symptoms and purulent drainage. The present article reports a case of giant sialolith with a diameter of 2.5 cm in the submandibular gland, which was removed surgically with functional preservation of the submandibular gland. The treatment may vary according to the size, shape and location of the calculus... (AU)