Abstract

Salivary gland stones, or sialoliths, are the most common cause of the obstruction of salivary glands. The mechanism behind the formation of sialoliths has been elusive. Symptomatic sialolithiasis has a prevalence of 0.45% in the general population, is characterized by recurrent painful periprandial swelling of the affected gland, and often results in sialadenitis with the need for surgical intervention. Here, we show by the use of immunohistochemistry, immunofluorescence, computed tomography (CT) scans and reconstructions, special dye techniques, bacterial genotyping, and enzyme activity analyses that neutrophil extracellular traps (NETs) initiate the formation and growth of sialoliths in humans. The deposition of neutrophil granulocyte extracellular DNA around small crystals results in the dense aggregation of the latter, and the subsequent mineralization creates alternating layers of dense mineral, which are predominantly calcium salt deposits and DNA. The further agglomeration and appositional growth of these structures promotes the development of macroscopic sialoliths that finally occlude the efferent ducts of the salivary glands, causing clinical symptoms and salivary gland dysfunction. These findings provide an entirely novel insight into the mechanism of sialolithogenesis, in which an immune system-mediated response essentially participates in the physicochemical process of concrement formation and growth.

Highlights

  • IntroductionSialoliths, are the most common cause for the obstruction of the salivary glands [1,2]

  • Salivary gland stones, or sialoliths, are the most common cause for the obstruction of the salivary glands [1,2]

  • Our study shows that neutrophil extracellular trap (NET) formation is an essential step for sialolith development

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Summary

Introduction

Sialoliths, are the most common cause for the obstruction of the salivary glands [1,2]. 20% of patients with sialolithiasis, the stones affect the excretory duct system of the submandibular and parotid glands, respectively [5]. Postmortem investigations in humans detected small concrements even in asymptomatic patients, in the submandibular glands [6,7]. These small concrements may provide a basis for the development of larger stones, which become clinically symptomatic. Ultrasound imaging and sialendoscopy are preferentially employed to detect the concrements [11,12,13,14] The latter often need to be removed by sialendoscopy-assisted interventions such as basket extractions, mechanical fragmentation, or transoral or endoscopic–transcutaneous surgical approaches [15,16,17,18,19,20]

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