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Passador-Santos F, de Oliveira CRR, Teixeira LN, Turssi CP, de Brito-Junior RB, Soares AB, de Freitas NS, de Araújo NS, de Araújo VC. Adenomatoid odontogenic tumor: Features of ameloblastic-like epithelial cells differentiation, secretion, and the nature of tumor cells products. J Oral Pathol Med 2023. [PMID: 37141592 DOI: 10.1111/jop.13436] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/11/2023] [Revised: 04/10/2023] [Accepted: 04/18/2023] [Indexed: 05/06/2023]
Abstract
BACKGROUND This study aimed to investigate the differentiation of ameloblastic-like cells and the nature of the secreted eosinophilic materials in adenomatoid odontogenic tumors. METHODS We studied histological and immunohistochemical characteristics of 20 cases using: cytokeratins 14 and 19, amelogenin, collagen I, laminin, vimentin, and CD34. RESULTS Rosette cells differentiated into ameloblastic-like cells positioned face-to-face, displaying collagen I-positive material between them. Epithelial cells of the rosettes can differentiate into ameloblastic-like cells. This phenomenon probably occurs due to an induction phenomenon between these cells. The secretion of collagen I is probably a brief event. Amelogenin-positive areas were interspersed by epithelial cells in the lace-like areas, outside the rosettes and distant from the ameloblastic-like cells. CONCLUSIONS There are at least two types of eosinophilic material in different areas within the tumor, one in the rosette and solid areas and another in lace-like areas. The secreted eosinophilic material in the rosettes and solid areas is probably a product of well-differentiated ameloblastic-like cells. It is positive for collagen I and negative for amelogenin, whereas some eosinophilic materials in the lace-like areas are positive for amelogenin. We hypothesize that the latter eosinophilic material could be a product of odontogenic cuboidal epithelial or intermediate stratum-like epithelial cells.
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Affiliation(s)
| | - Catarina Rodrigues Rosa de Oliveira
- Department of Oral Pathology, Faculdade São Leopoldo Mandic, São Paulo, Brazil
- Centro Universitário CESMAC, Faculdade de Odontologia, Maceió, Brazil
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Cook TD, Prothero J, Brudy M, Magraw JA. Complex enameloid microstructure of †Ischyrhiza mira rostral denticles. J Anat 2022; 241:616-627. [PMID: 35445396 DOI: 10.1111/joa.13676] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/23/2022] [Revised: 04/07/2022] [Accepted: 04/07/2022] [Indexed: 11/30/2022] Open
Abstract
Serving in a foraging or self-defense capacity, pristiophorids, pristids, and the extinct sclerorhynchoids independently evolved an elongated rostrum lined with modified dermal denticles called rostral denticles. Isolated rostral denticles of the sclerorhynchoid Ischyrhiza mira are commonly recovered from Late Cretaceous North American marine deposits. Although the external morphology has been thoroughly presented in the literature, very little is known about the histological composition and organization of these curious structures. Using acid-etching techniques and scanning electron microscopy, we show that the microstructure of I. mira rostral denticles are considerably more complex than that of previously described dermal denticles situated elsewhere on the body. The apical cap consists of outer single crystallite enameloid (SCE) and inner bundled crystallite enameloid (BCE) overlying a region of orthodentine. The BCE has distinct parallel bundled enameloid (PBE), tangled bundled enameloid (TBE), and radial bundled enameloid (RBE) components. Additionally, the cutting edge of the rostral denticle is produced by a superficial layer of SCE and a deeper ridges/cutting edge layer (RCEL) of the BCE. The highly organized enameloid observed in the rostral denticles of this batomorph resembles that of the multifaceted tissue architecture observed in the oral teeth of selachimorphs and demonstrates that dermal scales have the capacity to evolve histologically similar complex tooth-like structures both inside and outside the oropharyngeal cavity.
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Affiliation(s)
- Todd D Cook
- Penn State Behrend, School of Science, Erie, Pennsylvania, USA
| | - Jack Prothero
- Penn State Behrend, School of Science, Erie, Pennsylvania, USA
| | - Michael Brudy
- Penn State Behrend, School of Science, Erie, Pennsylvania, USA
| | - Jerome A Magraw
- Penn State Behrend, School of Science, Erie, Pennsylvania, USA
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Wilmers J, Waldron M, Bargmann S. Hierarchical Microstructure of Tooth Enameloid in Two Lamniform Shark Species, Carcharias taurus and Isurus oxyrinchus. Nanomaterials (Basel) 2021; 11:nano11040969. [PMID: 33918809 PMCID: PMC8070439 DOI: 10.3390/nano11040969] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 03/16/2021] [Revised: 04/02/2021] [Accepted: 04/06/2021] [Indexed: 12/22/2022]
Abstract
Shark tooth enameloid is a hard tissue made up of nanoscale fluorapatite crystallites arranged in a unique hierarchical pattern. This microstructural design results in a macroscopic material that is stiff, strong, and tough, despite consisting almost completely of brittle mineral. In this contribution, we characterize and compare the enameloid microstructure of two modern lamniform sharks, Isurus oxyrinchus (shortfin mako shark) and Carcharias taurus (spotted ragged-tooth shark), based on scanning electron microscopy images. The hierarchical microstructure of shark enameloid is discussed in comparison with amniote enamel. Striking similarities in the microstructures of the two hard tissues are found. Identical structural motifs have developed on different levels of the hierarchy in response to similar biomechanical requirements in enameloid and enamel. Analyzing these structural patterns allows the identification of general microstructural design principles and their biomechanical function, thus paving the way for the design of bioinspired composite materials with superior properties such as high strength combined with high fracture resistance.
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Affiliation(s)
- Jana Wilmers
- Chair of Solid Mechanics, University of Wuppertal, 42119 Wuppertal, Germany;
- Correspondence: ; Tel.: +49-202-439-2086
| | - Miranda Waldron
- Electron Microscope Unit, University of Cape Town, Cape Town 7701, South Africa;
| | - Swantje Bargmann
- Chair of Solid Mechanics, University of Wuppertal, 42119 Wuppertal, Germany;
- Wuppertal Center for Smart Materials, University of Wuppertal, 42119 Wuppertal, Germany
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Moyer JK, Finucci B, Riccio ML, Irschick DJ. Dental morphology and microstructure of the Prickly Dogfish Oxynotus bruniensis (Squaliformes: Oxynotidae). J Anat 2020; 237:916-932. [PMID: 32539172 DOI: 10.1111/joa.13251] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/24/2020] [Revised: 05/19/2020] [Accepted: 05/20/2020] [Indexed: 11/25/2022] Open
Abstract
This study describes and illustrates the jaws, teeth, and tooth microstructure of the Prickly Dogfish Oxynotus bruniensis. Detailed accounts of the dental morphology of O. bruniensis are rare and have not addressed the tissue arrangement or microstructure of the teeth. These features are documented and discussed in the contexts of interspecific comparisons with other elasmobranchs and the dietary specialization of O. bruniensis. The overall tooth morphology of O. bruniensis is similar to those of other closely related members in the order Squaliformes, as is the tissue arrangement, or histotype. Oxynotus bruniensis exhibits a simplified enameloid microstructure, which we compare with previously documented enameloid microstructures of other elasmobranchs. Though subtle interspecific differences in dental characters are documented, neither overall tooth morphology nor histotype and microstructure are unique to O. bruniensis. We conclude that in the case of O. bruniensis, dietary specialization is facilitated by behavioral rather than morphological specialization.
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Affiliation(s)
- Joshua K Moyer
- Graduate Program in Organismic and Evolutionary Biology, University of Massachusetts Amherst, Amherst, MA, USA
| | - Brittany Finucci
- National Institute of Water and Atmospheric Research, Wellington, New Zealand
| | | | - Duncan J Irschick
- Graduate Program in Organismic and Evolutionary Biology, University of Massachusetts Amherst, Amherst, MA, USA.,Department of Biology, University of Massachusetts Amherst, Amherst, MA, USA
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Sasagawa I, Ishiyama M, Yokosuka H, Mikami M, Oka S, Shimokawa H, Uchida T. Immunolocalization of enamel matrix protein-like proteins in the tooth enameloid of spotted gar, Lepisosteus oculatus, an actinopterygian bony fish. Connect Tissue Res 2019; 60:291-303. [PMID: 30063414 DOI: 10.1080/03008207.2018.1506446] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Submit a Manuscript] [Subscribe] [Scholar Register] [Indexed: 02/03/2023]
Abstract
Enameloid is a well-mineralized tissue covering the tooth surface in fish and it corresponds to the outer-most layer of dentin. It was reported that both dental epithelial cells and odontoblasts are involved in the formation of enameloid. Nevertheless, the localization and timing of secretion of ectodermal enamel matrix proteins in enameloid are unclear. In the present study, the enameloid matrix during the stages of enameloid formation in spotted gar, Lepisosteus oculatus, an actinopterygian, was examined mainly by transmission electron microscopy-based immunohistochemistry using an anti-mammalian amelogenin antibody and antiserum. Positive immunoreactivity with the antibody and antiserum was found in enameloid from the surface to the dentin-enameloid junction just before the formation of crystallites. This immunoreactivity disappeared rapidly before the full appearance of crystallites in the enameloid during the stage of mineralization. Immunolabelling was usually found along the collagen fibrils but was not seen on the electron-dense fibrous structures, which were probably derived from matrix vesicles in the previous stage. In inner dental epithelial cells, the granules in the distal cytoplasm often showed positive immunoreactivity, suggesting that the enamel matrix protein-like proteins originated from inner dental epithelial cells. Enamel matrix protein-like proteins in the enameloid matrix might be common to the enamel matrix protein-like proteins previously reported in the collar enamel of teeth and ganoine of ganoid scales, because they exhibited marked immunoreactivity with the same anti-mammalian amelogenin antibodies. It is likely that enamel matrix protein-like proteins are involved in the formation of crystallites along collagen fibrils in enameloid.
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Affiliation(s)
- Ichiro Sasagawa
- a Advanced Research Center, The Nippon Dental University , Niigata Japan
| | - Mikio Ishiyama
- b Department of Histology , The Nippon Dental University , Niigata Japan
| | - Hiroyuki Yokosuka
- b Department of Histology , The Nippon Dental University , Niigata Japan
| | - Masato Mikami
- c Department of Microbiology , The Nippon Dental University , Niigata , Japan
| | - Shunya Oka
- d Department of Biology , School of Life Dentistry at Niigata, The Nippon Dental University , Niigata Japan
| | - Hitoyata Shimokawa
- e Pediatric Dentistry, Department of Oral Health Sciences , Graduate School, Tokyo Medical and Dental University , Tokyo Japan
| | - Takashi Uchida
- f Department of Oral Biology , Graduate School of Biomedical Sciences, Hiroshima University , Hiroshima Japan
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Marcus MA, Amini S, Stifler CA, Sun CY, Tamura N, Bechtel HA, Parkinson DY, Barnard HS, Zhang XXX, Chua JQI, Miserez A, Gilbert PUPA. Parrotfish Teeth: Stiff Biominerals Whose Microstructure Makes Them Tough and Abrasion-Resistant To Bite Stony Corals. ACS Nano 2017; 11:11856-11865. [PMID: 29053258 DOI: 10.1021/acsnano.7b05044] [Citation(s) in RCA: 19] [Impact Index Per Article: 2.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/07/2023]
Abstract
Parrotfish (Scaridae) feed by biting stony corals. To investigate how their teeth endure the associated contact stresses, we examine the chemical composition, nano- and microscale structure, and the mechanical properties of the steephead parrotfish Chlorurus microrhinos tooth. Its enameloid is a fluorapatite (Ca5(PO4)3F) biomineral with outstanding mechanical characteristics: the mean elastic modulus is 124 GPa, and the mean hardness near the biting surface is 7.3 GPa, making this one of the stiffest and hardest biominerals measured; the mean indentation yield strength is above 6 GPa, and the mean fracture toughness is ∼2.5 MPa·m1/2, relatively high for a highly mineralized material. This combination of properties results in high abrasion resistance. Fluorapatite X-ray absorption spectroscopy exhibits linear dichroism at the Ca L-edge, an effect that makes peak intensities vary with crystal orientation, under linearly polarized X-ray illumination. This observation enables polarization-dependent imaging contrast mapping of apatite, a method to quantitatively measure and display nanocrystal orientations in large, pristine arrays of nano- and microcrystalline structures. Parrotfish enameloid consists of 100 nm-wide, microns long crystals co-oriented and assembled into bundles interwoven as the warp and the weave in fabric and therefore termed fibers here. These fibers gradually decrease in average diameter from 5 μm at the back to 2 μm at the tip of the tooth. Intriguingly, this size decrease is spatially correlated with an increase in hardness.
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Affiliation(s)
- Matthew A Marcus
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - Shahrouz Amini
- Biological and Biomimetic Material Laboratory, School of Materials Science and Engineering, Nanyang Technological University , 637553 Singapore
| | - Cayla A Stifler
- Department of Physics, University of Wisconsin-Madison , Madison, Wisconsin 53706, United States
| | - Chang-Yu Sun
- Department of Physics, University of Wisconsin-Madison , Madison, Wisconsin 53706, United States
| | - Nobumichi Tamura
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - Hans A Bechtel
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - Dilworth Y Parkinson
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - Harold S Barnard
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - Xiyue X X Zhang
- Advanced Light Source, Lawrence Berkeley Laboratory , Berkeley, California 94720, United States
| | - J Q Isaiah Chua
- Biological and Biomimetic Material Laboratory, School of Materials Science and Engineering, Nanyang Technological University , 637553 Singapore
| | - Ali Miserez
- Biological and Biomimetic Material Laboratory, School of Materials Science and Engineering, Nanyang Technological University , 637553 Singapore
- School of Biological Sciences, Nanyang Technological University , 637551 Singapore
| | - Pupa U P A Gilbert
- Department of Physics, University of Wisconsin-Madison , Madison, Wisconsin 53706, United States
- Departments of Chemistry, Geoscience, Materials Science Program, University of Wisconsin-Madison , Madison, Wisconsin 53706, United States
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Keating JN, Marquart CL, Donoghue PCJ. Histology of the heterostracan dermal skeleton: Insight into the origin of the vertebrate mineralised skeleton. J Morphol 2015; 276:657-80. [PMID: 25829358 PMCID: PMC4979667 DOI: 10.1002/jmor.20370] [Citation(s) in RCA: 22] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 08/15/2014] [Revised: 12/10/2014] [Accepted: 01/08/2015] [Indexed: 11/17/2022]
Abstract
Living vertebrates are divided into those that possess a fully formed and fully mineralised skeleton (gnathostomes) versus those that possess only unmineralised cartilaginous rudiments (cyclostomes). As such, extinct phylogenetic intermediates of these living lineages afford unique insights into the evolutionary assembly of the vertebrate mineralised skeleton and its canonical tissue types. Extinct jawless and jawed fishes assigned to the gnathostome stem evidence the piecemeal assembly of skeletal systems, revealing that the dermal skeleton is the earliest manifestation of a homologous mineralised skeleton. Yet the nature of the primitive dermal skeleton, itself, is poorly understood. This is principally because previous histological studies of early vertebrates lacked a phylogenetic framework required to derive evolutionary hypotheses. Nowhere is this more apparent than within Heterostraci, a diverse clade of primitive jawless vertebrates. To this end, we surveyed the dermal skeletal histology of heterostracans, inferred the plesiomorphic heterostracan skeleton and, through histological comparison to other skeletonising vertebrate clades, deduced the ancestral nature of the vertebrate dermal skeleton. Heterostracans primitively possess a four‐layered skeleton, comprising a superficial layer of odontodes composed of dentine and enameloid; a compact layer of acellular parallel‐fibred bone containing a network of vascular canals that supply the pulp canals (L1); a trabecular layer consisting of intersecting radial walls composed of acellular parallel‐fibred bone, showing osteon‐like development (L2); and a basal layer of isopedin (L3). A three layered skeleton, equivalent to the superficial layer L2 and L3 and composed of enameloid, dentine and acellular bone, is possessed by the ancestor of heterostracans + jawed vertebrates. We conclude that an osteogenic component is plesiomorphic with respect to the vertebrate dermal skeleton. Consequently, we interpret the dermal skeleton of denticles in chondrichthyans and jawless thelodonts as independently and secondarily simplified. J. Morphol. 276:657–680, 2015. © 2015 The Authors Journal of Morphology Published by Wiley Periodicals, Inc.
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Affiliation(s)
- Joseph N Keating
- School of Earth Sciences, University of Bristol, Life Science Building, 24 Tyndall Avenue, Bristol, BS8 1TQ, UK
| | - Chloe L Marquart
- School of Earth Sciences, University of Bristol, Life Science Building, 24 Tyndall Avenue, Bristol, BS8 1TQ, UK
| | - Philip C J Donoghue
- School of Earth Sciences, University of Bristol, Life Science Building, 24 Tyndall Avenue, Bristol, BS8 1TQ, UK
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Affiliation(s)
- J D Bartlett
- Department of Mineralized Tissue Biology, The Forsyth Institute, Cambridge, MA, USA
| | - J P Simmer
- Department of Biologic and Materials Sciences, University of Michigan School of Dentistry, Ann Arbor, MI, USA
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Abstract
Enamel and enameloid, the highly mineralized tooth-covering tissues in living vertebrates, are different in their matrix composition. Enamel, a unique product of ameloblasts, principally contains enamel matrix proteins (EMPs), while enameloid possesses collagen fibrils and probably receives contributions from both odontoblasts and ameloblasts. Here we focused on type I collagen (COL1A1) and amelogenin (AMEL) gene expression during enameloid and enamel formation throughout ontogeny in the caudate amphibian, Pleurodeles waltl. In this model, pre-metamorphic teeth possess enameloid and enamel, while post-metamorphic teeth possess enamel only. In first-generation teeth, qPCR and in situ hybridization (ISH) on sections revealed that ameloblasts weakly expressed AMEL during late-stage enameloid formation, while expression strongly increased during enamel deposition. Using ISH, we identified COL1A1 transcripts in ameloblasts and odontoblasts during enameloid formation. COL1A1 expression in ameloblasts gradually decreased and was no longer detected after metamorphosis. The transition from enameloid-rich to enamel-rich teeth could be related to a switch in ameloblast activity from COL1A1 to AMEL synthesis. P. waltl therefore appears to be an appropriate animal model for the study of the processes involved during enameloid-to-enamel transition, especially because similar events probably occurred in various lineages during vertebrate evolution.
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Affiliation(s)
- N Assaraf-Weill
- UMR 7138-SAE, Research Group "Evolution & Development of the Skeleton", Université Pierre et Marie Curie, 7 quai St-Bernard, Case 5, 75005 Paris, France
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Sasagawa I. Fine structure of the cap enameloid and of the dental epithelial cells during enameloid mineralisation and early maturation stages in the tilapia, a teleost. J Anat 1997; 190 ( Pt 4):589-600. [PMID: 9183681 PMCID: PMC1467643 DOI: 10.1046/j.1469-7580.1997.19040589.x] [Citation(s) in RCA: 36] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 02/04/2023] Open
Abstract
Morphological features of the cap enameloid and dental epithelial cells were investigated by light and transmission electron microscopy during the various stages of enameloid mineralisation and early maturation in the tilapia. The pattern of mineralisation along collagen fibrils in the enameloid differed from that in the dentine. Many matrix vesicles were found in the predentine and in the enameloid, suggesting that they may be involved in the initial mineralisation in both regions. Most of the organic matrix disappeared from the cap enameloid during mineralisation and maturation. The disappearance of the organic matrix could be divided into 2 stages. Initially a fine network-like matrix, which probably consisted of glycosaminoglycans and extended between collagen fibrils, began to disappear. At the same time, fine crystallites and electron-dense, fine granular material covered the collagen fibrils as mineralisation of the enameloid began. In the second stage, the maturation of the enameloid, the collagen fibrils degenerated completely and disappeared from the cap enameloid, being replaced by large numbers of large crystals. At the mineralisation stage, the numbers of lysosomal bodies tended to increase in the inner dental epithelial (IDE) cells, which contained a well developed Golgi apparatus and rough endoplasmic reticulum (rER). At the early stage of maturation, a ruffled border was noted at the distal ends of the IDE cells, which contained many mitochondria and lysosomal bodies, but less rER. These features suggest that the cells actively absorb the organic matrix, which includes collagen fibrils, in the cap enameloid. The outer dental epithelial (ODE) cells were translucent cells that contained well developed labyrinthine canalicular spaces from the onset of the mineralisation stage to the middle stage of maturation. The IDE and ODE cells were clearly involved in the mineralisation of the cap enameloid at the mineralisation and maturation stages.
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Affiliation(s)
- I Sasagawa
- Department of Anatomy, Nippon Dental University, Niigata, Japan
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