Abstract
Objectives
Several theories have been proposed regarding the genesis of sialoliths, including the organic core theory, which suggests epithelial or bacterial etiology originating in the central core. Our aim was to use novel methodologies to analyze central areas (the core) of calculi from sialolithiasis patients.
Materials and methods
The structures of the halves of six submandibular salivary stones were analyzed by scanning electron microscopy (SEM). After structural analysis, from the other six halves, samples from the central parts of the core and peripheral parts of the core were digested with trypsin and analyzed by matrix-assisted laser desorption ionization–time of flight mass spectrometry. The peptide mass fingerprints were compared with the results of in silico digestion.
Results
SEM analysis of the sialoliths showed that organic structures (collagen/fibrous-like structures, bacterial fragments) were visible only outside of the core in the concentric layers of external areas, but not in the core area. The mass spectrometry (MS)/MS post-source decay experiments were completed from the four, most intense signals observed in the MS spectrum and human defensin was proven to be present in three of the examined samples, originated from the peripheral region of three cores.
Conclusions
Although proteomic analysis demonstrated defensin protein in the peripheral region of the core in three sialoliths, SEM failed to prove organic structures in the core.
Clinical relevance
New investigation modalities still cannot prove organic structures in the core, henceforward challenging the organic core theory.
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Acknowledgments
We would like to thank Professor László Seress for SEM analysis and Béla Dolgos for the SEM technical assistance. The authors thank the Hungarian Scientific Research Fund (OTKA) PD 76395, PD 78599, and K 81839 for supporting this research.
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The authors declare that they have no conflict of interests.
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Szalma, J., Böddi, K., Lempel, E. et al. Proteomic and scanning electron microscopic analysis of submandibular sialoliths. Clin Oral Invest 17, 1709–1717 (2013). https://doi.org/10.1007/s00784-012-0870-6
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DOI: https://doi.org/10.1007/s00784-012-0870-6