Structural patterns of enamel in the superfamily Ceboidea

A fundamental enamel structure was found in the superfamily Ceboidea, and tentatively named the nonserial pattern, as distinguished from the multiserial and uniserial patterns. In the nonserial pattern, almost all rows of enamel prisms are straight to slightly curved from the enameldentin junction to the surface of the tooth, and are nearly uniformly oriented. Accordingly, Schreger's band is definitely lacking throughout the length and width of enamel. The interprismatic bundles between both adjacent rows are well developed. The nonserial pattern has so far been found to be limited to some genera of which the molars preserve rather primitive external features; i.e.,Saimiri, Callicebus, Aotus, Alouatta, Saguinus andLeontopithecus. On the other hand, the multiserial pattern is fairly common in many genera of the Ceboidea. The nonserial pattern, which corresponds to the pattern I described byBoyde (1964), is the most primitive, judging from its occurrence, structural simplicity and other factors. The multiserial and uniserial patterns are assumed to be independently evolved from the nonserial pattern.     

Expression of ameloblastin during enamel formation in a crocodile

Ameloblastin is an enamel-specific protein that plays critical roles in enamel formation, as well as adhesion between ameloblasts and the enamel matrix, as shown by analyses of ameloblastin-null mice. In the present study, we produced two distinct antibodies that recognize the N-terminus and C-terminus regions of caiman ameloblastin, in order to elucidate the fate of ameloblastin peptides during tooth development. An immunohistochemical study using the antibodies showed that caiman ameloblastin was a tooth-specific matrix protein that may initially be cleaved into two groups, N- and C-terminal peptides, as shown in mammals. The distribution of the N-terminal peptides was much different from that of the C-terminal peptides during enamel formation; however, it was similar to that of mammalian ameloblastin. Although ameloblastin is thought to have a relationship with the enamel prismatic structure in mammals, in the caiman, which has non-prismatic enamel, functional ameloblastin has no relationship with any enamel structure. Consequently, it is suggested that ameloblastin has kept its original functions during the evolutionary transition from reptiles to mammals and that it has been conserved in both lineages during more than 200 million years of evolution. Our results support the notion that ameloblastin acts as a factor for ameloblast adhesion to enamel matrix, because distribution of the C-terminal peptides was consistently restricted on the surface layers of enamel matrix specimens ranging from immature to nearly completely mature. The principal molecules that provide the adhesive function are presumably C-terminal peptides.     

Mineral-organic-matrix relations in tooth enamel

X-ray and electron diffraction patterns show that β-pleated-sheet polypeptide chains are predominantly oriented approximately perpendicular to the c-axes of developing enamel apatite crystallites. This spatial relation suggests a specific role for enamelins in controlling crystal growth.     

Variation in enamel thickness within the genus Homo

Recent humans and their fossil relatives are classified as having thick molar enamel, one of very few dental traits that distinguish hominins from living African apes. However, little is known about enamel thickness in the earliest members of the genus Homo, and recent studies of later Homo report considerable intra- and inter-specific variation. In order to assess taxonomic, geographic, and temporal trends in enamel thickness, we applied micro-computed tomographic imaging to 150 fossil Homo teeth spanning two million years. Early Homo postcanine teeth from Africa and Asia show highly variable average and relative enamel thickness (AET and RET) values. Three molars from South Africa exceed Homo AET and RET ranges, resembling the hyper thick Paranthropus condition. Most later Homo groups (archaic European and north African Homo, and fossil and recent Homo sapiens) possess absolutely and relatively thick enamel across the entire dentition. In contrast, Neanderthals show relatively thin enamel in their incisors, canines, premolars, and molars, although incisor AET values are similar to H. sapiens. Comparisons of recent and fossil H. sapiens reveal that dental size reduction has led to a disproportionate decrease in coronal dentine compared with enamel (although both are reduced), leading to relatively thicker enamel in recent humans. General characterizations of hominins as having ‘thick enamel’ thus oversimplify a surprisingly variable craniodental trait with limited taxonomic utility within a genus. Moreover, estimates of dental attrition rates employed in paleodemographic reconstruction may be biased when this variation is not considered. Additional research is necessary to reconstruct hominin dietary ecology since thick enamel is not a prerequisite for hard-object feeding, and it is present in most later Homo species despite advances in technology and food processing.     

Some observations on enamel thickness and enamel prism packing in the miocene hominoid Otavipithecus namibiensis

Otavipithecus namibiensis is currently the sole representative of a Miocene hominoid radiation in subequatorial Africa. Several nondestructive techniques, such as computed tomography (CT) and confocal microscopy (CFM), can provide useful information about dental characteristics in this southern African Miocene hominoid. Our studies suggest that the molars of Otavipithecus are characterized by (1) thin enamel and (2) a predominance of pattern 1 enamel prism. Together, these findings provide little support for the recent suggestion of an Afropithecini clade consisting of Otavipithecus, Heliopithecus, and Afropithecus. Instead, they lend some (though not conclusive) support to the suggestion of an Otavipithecus/African ape clade distinct from Afropithecus. © 1995 Wiley-Liss, Inc.     

Fine structure of the dental enamel in the Family Callitrichidae (Ceboidea,primates)

The fine structure of the dental enamel was intensively examined in the Family Callitrichidae.Leontopithecus rosalia has the nonserial pattern, butCallimico goeldii andSaguinus midas appear more or less modified from the typical nonserial pattern asSaimiri sciureus has (see Figs. 1 & 5). On the other hand,Callithrix jacchus andCebuella pygmaea attain to the primitive stage of the multiserial pattern (see Figs. 4 & 6). So far as the structural patterns of the dental enamel are concerned, a serial trend is confirmed in the Callitrichidae; extending from the genusLeontopithecus through the generaCallimico andSaguinus to the generaCallithrix andCebuella. The genusSaguinus shows extremely wide interspecific variation in the fine structure of the dental enamel, ranging fromS. leucopus with the most primitive features toS. bicolor with the most advanced (see Figs. 2 & 3). The rows of enamel prisms are slightly twisted mesiodistally in the former species, but strongly folded in the latter. This reflects transitional stages from the nonserial pattern to the multiserial. As a whole, however, the genusSaguinus is still regarded as nonserial. Thus, there is a slight, but important gap between the genusSaguinus andCallithrix, as shown by the decussation of clusters (see Fig. 5), as well as by other characters.     

The evolution of dinosaur tooth enamel microstructure

The evolution of tooth enamel microstructure in both extinct and extant mammalian groups has been extensively documented, but is poorly known in reptiles, including dinosaurs. Previous intensive sampling of dinosaur tooth enamel microstructure revealed that: (1) the three‐dimensional arrangement of enamel types and features within a tooth—the schmelzmuster—is most useful in diagnosing dinosaur clades at or around the family level; (2) enamel microstructure complexity is correlated with tooth morphology complexity and not necessarily with phylogenetic position; and (3) there is a large amount of homoplasy within Theropoda but much less within Ornithischia. In this study, the examination of the enamel microstructure of 28 additional dinosaur taxa fills in taxonomic gaps of previous studies and reinforces the aforementioned conclusions. Additionally, these new specimens reveal that within clades such as Sauropodomorpha, Neotheropoda, and Euornithopoda, the more basal taxa have simpler enamel that is a precursor to the more complex enamel of more derived taxa and that schmelzmusters evolve in a stepwise fashion. In the particularly well‐sampled clade of Euornithopoda, correlations between the evolution of dental and enamel characters could be drawn. The ancestral schmelzmuster for Genasauria remains ambiguous due to the dearth of basal ornithischian teeth available for study. These new specimens provide new insights into the evolution of tooth enamel microstructure in dinosaurs, emphasizing the importance of thorough sampling within broadly inclusive clades, especially among their more basal members.     

CRAC channels in dental enamel cells

Enamel mineralization relies on Ca²⁺ availability provided by Ca²⁺ release activated Ca²⁺ (CRAC) channels. CRAC channels are modulated by the endoplasmic reticulum Ca²⁺ sensor STIM1 which gates the pore subunit of the channel known as ORAI1, found the in plasma membrane, to enable sustained Ca²⁺ influx. Mutations in the STIM1 and ORAI1 genes result in CRAC channelopathy, an ensemble of diseases including immunodeficiency, muscular hypotonia, ectodermal dysplasia with defects in sweat gland function and abnormal enamel mineralization similar to amelogenesis imperfecta (AI). In some reports, the chief medical complain has been the patient’s dental health, highlighting the direct and important link between CRAC channels and enamel. The reported enamel defects are apparent in both the deciduous and in permanent teeth and often require extensive dental treatment to provide the patient with a functional dentition. Among the dental phenotypes observed in the patients, discoloration, increased wear, hypoplasias (thinning of enamel) and chipping has been reported. These findings are not universal in all patients. Here we review the mutations in STIM1 and ORAI1 causing AI-like phenotype, and evaluate the enamel defects in CRAC channel deficient mice. We also provide a brief overview of the role of CRAC channels in other mineralizing systems such as dentine and bone.     

Sulphur dioxide and fluoride co-exposure cause enamel damage by disrupting the Cl-/HCO3- ion transport

ObjectiveAlthough there is growing evidence linking the exposure to sulphur dioxide (SO₂) and fluoride to human diseases, there is little data on the co-exposure of SO₂ and fluoride. Moreover, literature on SO₂ and fluoride co-exposure to enamel damage is insufficient. In this work, we concentrate on the concurrent environmental issues of excessive SO₂ and fluoride in several coal-consuming regions.MethodTo identify the toxicity of SO₂ and fluoride exposure either separately or together, we used both ICR mice and LS8 cells, and factorial design was employed to assess the type of potential combined action.ResultIn this study, co-exposure to SO₂ and fluoride exacerbated enamel damage, resulting in more severe enamel defects of incisor and the damage occurred earlier. Cl^-/HCO₃^- exchanger expression is increased by SO₂ and fluoride in mouse incisor. Consistent with in vivo results, co-exposure of SO₂ and fluoride decreased pHi and increased [Cl^-]i level by increasing the expression of the Cl^-/HCO₃^- exchanger in LS8 cells. Furthermore, SO₂ and F may increase merlin protein expression, and merlin deficiency causes AE2 expression to decrease in vitro.ConclusionOverall, these results indicate that co-exposure to SO₂ and fluoride may result in more toxicity both in vitro and in vivo than a single exposure to SO₂ and fluoride, suggesting that residents in areas contaminated with SO₂ and fluoride may be more likely to suffer enamel damage.     

Ameloblastic secretion and calcification of the enamel layer in shark teeth

Tooth primordia at early stages of mineralization in the sharks Negaprion brevirostris and Triaenodon obesus were examined electron microscopically for evidence of ameloblastic secretion and its relation to calcification of the enamel (enameloid) layer. Ameloblasts are polarized with most of the mitochondria and all of the Golgi dictyosomes localized in the infranuclear end of the cell toward the squamous outer cells of the enamel organ. Endoplasmic reticular membranes and ribosomes are also abundant in this region. Ameloblastic vesicles bud from the Golgi membranes and evidently move through perinuclear and supranuclear zones to accumulate at the apical end of the cell. The vesicles secrete their contents through the apical cell membrane in merocrine fashion and appear to contribute precursor material both for the basal lamina and the enameline matrix. The enamel layer consists of four zones: a juxta-laminar zone containing newly polymerized mineralizing fibrils (tubules); a pre-enamel zone of assembly of matrix constituents; palisadal zones of mineralizing fibrils (tubules); and interpalisadal zones containing granular amorphous matrix, fine unit fibrils, and giant cross-banded fibers with a periodicity of 17.9 nm. It seems probable that amorphous, non-mineralizing fibrillar and mineralizing fibrillar constituents of the matrix are all products of ameloblastic secretion. Odontoblastic processes are tightly embedded in the matrix of the palisadal zones and do not appear to be secretory at the stages investigated. The shark tooth enamel layer is considered homologous with that of other vertebrates with respect to origin of its mineralizing fibrils from the innerental epithelium. The term enameloid is appropriate to connote the histological distinction that the enamel layer contains odontoblastic processes but should not signify that shark tooth enamel is a modified type of dentine. How amelogenins and/or enamelins secreted by amelo- blasts in the shark and other vertebrates are related to nucleation and growth of enamel crystallites is still not known.     

Enamel microarchitecture of a tribosphenic molar

The tribosphenic molar is a dental apomorphy of mammals and the molar type from which all derived types originated. Its enamel coat is expected to be ancestral: a thin, evenly distributed layer of radial prismatic enamel. In the bat Myotis myotis, we reinvestigated the 3D architecture of the dental enamel using serial sectioning combined with scanning electron microscopy analyses, biometrics of enamel prisms and crystallites, and X‐ray diffraction. We found distinct heterotopies in enamel thickness (thick enamel on the convex sides of the crests, thin on the concave ones), angularity of enamel prisms, and in distribution of particular enamel types (prismatic, interprismatic, aprismatic) and demonstrated structural relations of these heterotopies to the cusp and crest organization of the tribosphenic molar. X‐ray diffraction demonstrated that the crystallites composing the enamel are actually the aggregates of much smaller primary crystallites. The differences among particular enamel types in degree of crystallite aggregation and the variation in structural microstrain of the primary crystallites (depending upon the duration and the mechanical context of mineralization) represent factors not fully understood as yet that may contribute to the complexity of enamel microarchitecture in a significant way. J. Morphol., 2010. © 2010 Wiley‐Liss, Inc.     

In vitro histological and tetracycline staining properties of surface layer rat incisor enamel also reflect the cyclical nature of the maturation process

Summary Rat incisors cleaned of overlying enamel organ cells stain unevenly with several common histological stains producing two kinds of banding pattern. In one a pattern of widely spaced stained bands run in an oblique to transverse direction from a more apical level on the medial side to a more incisal level on the lateral side of each tooth. The pattern correlated directly with that produced by both in vivo and in vitro short-term tetracycline labelling in the same teeth: it also resembled the patterns previously demonstrated in a) horseradish peroxidase penetration into lateral intercellular spaces between maturation ameloblasts, b) the distribution of enamel labelling in vivo with ⁴⁵Ca, c) of etching of enamel surfaces demineralized with EDTA with the glutaraldehyde fixed enamel organ in situ and d) in the distribution of smoothended and ruffled border types of cell specialisations. We conclude that these bands demonstrate further and previously unrecognised aspects of the cyclical phenomena in enamel maturation-mineralization and show cyclical differences in the physico-chemical status of the organic matrix in the maturation process. A second, incremental growth type of banding pattern occurred at 200–225 m intervals in the lower incisors and had the same distribution at the beginning and end of the maturation zone.     

Sheath configurations in human cuspal enamel

To determine the prism sheath configurations in human cuspal enamel 80 teeth were initially ground to produce flat surfaces through the following planes: a horizontal series at successively greater distances from the dentinoenamel junction and longitudinally through the center of the cusps. Individual teeth were suspended in an acid-alcohol solution (1 cm³ conc. HCl in 100 cm³ 95% ethanol) at 37°C for seven to ten days. The treatment “softened” the enamel to a depth of approximately 1 mm. The teeth were embedded in Epon and sectioned at 0.5 to 10 μm with a diamond knife. Thick and thin ground sections for phase contrast microscopy and acid-etched ground sections for Nomarski differential interference microscopy were prepared through the same regions. In thicker longitudinal sections, the prisms in gnarled enamel formed a zig-zag pattern which was unlike the twisting pattern generally observed in ground sections. The thinnest transverse sections showed the sheath outlines to be dramatically different from those seen elsewhere in the enamel. Some prism sheaths were circular, others were in the form of spirals. What could be described as sheaths within sheaths were also seen. In the thinnest longitudinal sections the prisms were seen to be elongated and discontinuous. Sheath outlines in enamel adjacent to the central core of gnarled enamel were similar to those described elsewhere in the body of the enamel. Keyhole, modified keyhole patterns and arcade forms were the dominant sheath patterns. Other atypical sheath configurations were seen scattered throughout this region.     

Variation in the prismatic arrangement of dental enamel surfaces

Slightly etched prisms of human dental enamel surfaces were examined in the scanning electron microscope. The crystals in the central region of prisms showed a denser arrangement, similar to the crystals on the periphery, which determine their form here. A crevice-like space could be observed between the central and the peripheral region of a prism. The prisms on the enamel surface showed a wide variety in shape being either of fish-scale or key-hole form, in other places fully irregular. There was no uniform prism on a single tooth, and an interprismatic substance was never found. On the surface of a deciduous tooth a prismless enamel surface was observed consisting of edges of crystallites, which did not unite to prism formation.     

On thick and thin enamel in hominoids

Martin (1983, 1985) reviewed the significance of enamel thickness in hominoid evolution. He studied cut faces of hominoid teeth using the scanning electron microscope and related enamel prism packing patterns to both enamel formation rates and enamel thickness, although he did not present primary data on formation rates, which he summarised as being either “fast” or “slow.” Martin concluded that thick enamel formed at a fast rate represented the ancestral condition in the human and great ape clade. Thin enamel in African apes reflected a secondary reduction in secretion rates, with outer enamel being formed at a slow rate. The present study on ground sections of great ape and human teeth, using polarised light microscopy, was designed to measure the spacing between incremental growth lines in enamel, including striae of Retzius and prism cross striations, to determine rates of enamel formation in hominoids. Measurements on stria spacing showed that striae generally diverged as they passed outwards through enamel in all taxa. Cross-striation spacings also increased from inner to outer enamel. Secretion rates did not fall into two exclusive categories but varied, giving a spectrum of values generally increasing from within outwards at any one crown level and reducing in cervical enamel. There was no evidence for a reduction in enamel formation rates in outer enamel among African apes. These findings cast doubt on the proposition that the common ancestor of great apes and man had thick enamel formed at a fast rate. It is possible that thin enamel was the primitive condition, in which case thick enamel in humans and in Sivapithecus is derived, suggesting that thick enamel on low cusped teeth evolved on more than one occasion.     

Morphological and structural studies of early mineral formation in enamel of rat incisors by electron spectroscopic imaging (ESI) and electron spectroscopic diffraction (ESD)

Morphological and structural analysis of the earliest stage of crystal formation in enamel of rat incisors, by use of energy filtering transmission electron microscopy (EFTEM), has shown needlelike crystallites with a dotlike substructure. We conclude that these dots (nanometer-sized particles) have developed at nucleating, active sites along the non-collagenous matrix proteins in enamel. Calcium and phosphate groups are bound at such active sites and develop to nuclei, which grow to these stable dots (nanometer-sized particles). The dots coalesce rapidly in longitudinal direction, along the matrix proteins, with neighbouring dots to form parallel arranged needlelike crystallites. These needles grow and coalesce in lateral directions to ribbon-platelike crystallites. In enamel most of the organic substance becomes decomposed and transported to the ameloblasts. Consequently, the ribbon-platelike crystallites can coalesce to form much thicker (hydroxy)-apatite crystals than in dentine. Already in the earliest stage of crystal formation the mineral chains of dots (nanometer-sized particles) and the needlelike crystallites show a parallel orientation in the direction of the c-axis of hydroxyapatite. This is supported by the texture of the 002 reflections in the corresponding electron spectroscopic diffraction patterns (ESD), which appear as the first Bragg reflections.     

Cyclical phenomena occurring during the maturation of the enamel of rat incisor teeth

Summary A pattern of obliquely oriented bands has been demonstrated at the surface of the maturation zone enamel of freshly dissected rat incisor teeth as they dry. This pattern, of which there is no evidence in the fresh, wet, or completely dry teeth, consists of up to 4 or 5 pale grey, translucent linesseparated by wider, whiter, more opaque bands and has been shown to correlate directly with a similar pattern seen on the same teeth after staining with toluidine blue and previously described as the maturation cycle banding pattern (Boyde and Reith 1982). A second pattern comprised of much more closely spaced bands is also described. In this pattern, which again correlates with a similar pattern seen after toluidine blue staining, translucent and opaque bands cross the maturation zone more transversely and have a width of about 200 microns, approximating to 8h tooth growth. It is postulated that these banding patterns reflect alternately different drying rates of the maturation zone enamel and that they may correspond to cyclical changes in the hydrophobicity and hydrophilicity of enamel matrix both on a daily basis and on a larger time scale.