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Vertebrate teeth are attached to jaws by a variety of mechanisms, including acrodont, pleurodont, and thecodont modes of attachment. Recent studies have suggested that various modes of attachment exist within each sub-category. Especially squamates feature a broad diversity of modes of attachment. Here we have investigated tooth attachment tissues in the late cretaceous mosasaur Clidastes and compared mosasaur tooth attachment with modes of attachment found in other extant reptiles. Using histologic analysis of ultrathin ground sections, four distinct mineralized tissues that anchor mosasaur teeth to the jaw were identified: (i) an acellular cementum layer at the interface between root and cellular cementum, (ii) a massive cone consisting of trabecular cellular cementum, (iii) the mineralized periodontal ligament containing mineralized Sharpey’s fibers, and (iv) the interdental ridges connecting adjacent teeth. The complex, multilayered attachment apparatus in mosasaurs was compared with attachment tissues in extant reptiles, including Iguana and Caiman. Based on our comparative analysis we postulate the presence of a quadruple-layer tissue architecture underlying reptilian tooth attachment, comprised of acellular cementum, cellular cementum, mineralized periodontal ligament, and interdental ridge (alveolar bone). We propose that the mineralization status of the periodontal ligament is a dynamic feature in vertebrate evolution subject to functional adaptation.
The anchorage of teeth in jaws is one of the great architectural masterpieces in the design of the vertebrate body plan. Teeth commonly provide pointy tips, sharp incisal edges, or massive masticatory plateaus that allow them to exert their function related to capturing, biting, and chewing. However, for an efficient capture and partitioning of prey, tooth function is greatly enhanced through the connection with a rigid base as it is established by the load-bearing jaw bones. This connection between teeth and jaws is maintained by the periodontal attachment apparatus. The anchorage of teeth to jaws is also unique from a developmental point of view since vertebrate teeth develop essentially independent from the adjacent jaw bone through interactions between oral epithelium and migratory cranial ectomesenchyme. Only after tooth formation has begun, tooth-bound migratory tissues extend toward the jaw bone and form a connective tissue attachment that structurally and mechanically integrates the teeth with the jaw (Diekwisch 2002). The nature of this attachment greatly differs between vertebrate lineages and varies between rigid ankylosis and flexible fiber-mediated attachment.
Three basic types of tooth attachment are observed in extant reptiles (Osborn, 1984; Gaengler, 2000). The acrodont type of tooth attachment, characteristic of the Tuatara (Sphenodon punctatus) as well as agamid lizards and chameleons, is characterized by ankylosis of the tooth to the crest of the tooth-bearing element. The squamate condition is pleurodont, the tooth being ankylosed to the pleura (lingually sloping inner surface) of the tooth-bearing element (Lessman, 1952). Crocodiles feature a thecodont dentition, where the teeth are set in sockets but do not ankylose to the tooth-bearing elements. Instead, crocodile teeth show a fibrous attachment (Osborn, 1984) to the wall of the alveolus by means of the periodontal ligament. These distinctions of tooth implantation become blurred if fossil reptiles are taken into account. Acrodonty and pleurodonty can be seen as parts of the same transformation series (Estes et al., 1988), while other fossil reptiles show subthecodont or thecodont tooth implantation that involves ankylosis (Motani, 1997). The debate over the interpretation of tooth implantation and attachment has resulted in a debate over the affinities between mosasaurs and snakes, which were claimed to uniquely share a thecodont mode of tooth implantation among squamates (Lee, 1997a, b, 1998; Zaher and Rieppel, 1999). In an attempt to clarify and better characterize the nature of tooth implantation and ankylosis in mosasaurs, Caldwell et al. (2003) subjected mosasaur jaw fragments to histological analysis (see also Caldwell, 2007).
Mosasauroids are an extinct clade of marine squamates generally thought to be related to extant monitor lizards and their fossil relatives (e.g., Lee, 1997a, 1998; Rieppel et al., 2007). The clade makes its first appearance in the Fossil Record with the poorly known taxon Proaigialosaurus from the Upper Jurassic Solnhofen deposits in Southern Germany (Kuhn, 1958; referred to Aigialosauridae by Carroll, 1988), and it went extinct at the end of the Cretaceous. A first significant radiation of the clade is documented for mid-Cretaceous (Cenomanian) times, when aigialosaurs, adriosaurs, acetosaurs, coniasaurs, dolichosaurs, and pontosaurs populated coastal stretches of the neo-Tethys, predominantly in areas that today correspond to southeastern Europe and the Middle East (see Caldwell, 2006, for a recent review). During the Upper Cretaceous, with global sea level at a peak and ichthyosaurs facing extinction, the mosasaurs invaded the open sea, initiating a second rapid radiation of the clade as they adapted to numerous ecological niches offered throughout the oceans (Bell, 1997). Pelagic animals with limbs transformed to form flippers, mosasaurs include gigantic species, some attaining 14 meters (Prognathodon saturator: Dortangs et al., 2002) to 17.6 meters (Mosasaurus hoffmanni: Lingham-Soliar, 1995) in total length, thus establishing themselves at the top of the marine food chain during that time. The mosasaur feeding apparatus was indeed adapted to large prey, as is indicated by the high degree of mobility achieved by their lower jaws. The mandibular rami did not meet anteriorly in a syndesmotic symphysis, but remained independent from one another as is indicated by the smooth and rounded surface of their anterior tips. The lower jaws could thus separate at their anterior ends during feeding, and gape could be further enlarged by the presence of an intramandibular joint between the dentary and postdentary bones. Similar features are known for snakes feeding on large prey, such as boas and pythons. It is in recognition of this similarity that Cope (1869) introduced Pythonomorpha as a group that would include what he considered the two major families of mosasaurs. Although not initially part of his project, Cope (1872) later defended relationships of mosasaurs with snakes against Owen’s (1877, 1878) criticism by proposing a gradualistic scenario that would link the feeding mechanics of mosasaurs with those of macrostomatan snakes (see Rieppel et al., 2003, for further comments).
The present paper serves two functions, one to perform a detailed histological and comparative analysis of the mosasaurian attachment apparatus, and second to conduct a more generalized study of reptilian attachment tissues, comparing a mosasaur (Halisaurus sternbergi), a Green Iguana (Iguana iguana) and a Spectacled Caiman (Caiman crocodylus). The purpose of this second study is to identify similarities and differences between reptilian attachment tissues in order to identify possibly scenarios involved in the evolution of the reptilian feeding apparatus. Here we review the histology of reptilian tooth attachment in light of the findings of McIntosh et al. (2002). This study showed the crocodile (Caiman) tooth attachment to be histologically intermediate between a squamate type ankylosis (e.g. in the gecko Hemidactylus), and the mouse gomphosis, where the tooth is attached to the alveolus by the periodontal ligament. In the present paper, we have identified the mineralized periodontal ligament as an attachment tissue at the interface between mosasaur root cementum and interdental ridge, a concept that is no longer extravagant in light of the findings of McIntosh et al. (2002). This finding may have important consequences for the interpretation of the periodontium of mosasaurs, to which we now turn.
The jaw fragments sectioned for the present study come from two different specimens of mosasaurs, both held in the collections of the Field Museum of Natural History, Chicago. Specimen FMNH PR 186 represents Halisaurus sternbergi, specimen FMNH PR 484 represents an unidentified individual (Mosasauridae gen. et spec. indet.).
Samples were infiltrated in Exakt Technovit 7200 VLC according to the manufacturer’s instructions. Samples were cut using an Exakt 300 parallel band saw system and an Exakt 400CS grinding and polishing device. Samples were then mounted on plastic slide holders. Surfaces were ground and polished using a graded series of Exact polishing papers with a smallest size of P2500. Thickness of ground sections was between 5 and 20μm in average.
For this study, ultrathin ground sections were subjected to polarized light and analyzed using an analyzing polarization filter at 120°, 240°, and 360° rotation. Micrographs were recorded digitally. An identical region in each micrograph was chosen and the distribution of birefringend tissue elements was compared between micrographs from all three angles of rotation.
One Green Iguana (Iguana iguana) and an infant Spectacled Caiman (Caiman crocodylus) were obtained and sacrificed in accordance with Baylor College of Dentistry and UIC animal care regulations. Mandibles were prepared, fixed in formalin, decalcified and processed for paraffin sections. Sections measuring 5μm in thickness were then stained in Paragon-Epoxy stain (Paragon C. & C., Bronx, New York). Paragon-Epoxy is a polychromatic toluidine blue/basic fuchsin stain that has been proven particularly suitable for the demonstration of cement lines in tooth attachment tissues. Alternatively, ground sections were subjected to von Kossa’s procedure for the identification of mineralized calcium deposits.
Electron microprobe analysis was conducted using a Hitachi S-3000N scanning electron microscope with an Oxford Inca EDX system and a light element X-ray detector (15mm WD). Elemental composition was determined as weight % and Ca/P ratios were calculated from five measurements per area selected.
Five tissue sections per specimen and 10 randomly determined areas per section were selected using a Leica light microscope, a 100x lens, and a Leica digital camera system. All objects within one area were measured and their diameter was determined using our image analysis software. Mean values and standard deviation were calculated and used for comparison.
In the present study, a number of different methods of investigation were used to determine structural differences between tissue compartments of the mosasaur attachment apparatus, including transmission and incident lighting techniques of ultrathin mosasaur ground sections as well as histological examination of mosasaur attachment tissue thin sections at high magnification. Histological analysis of ultrathin ground sections by transmitted light revealed the following clearly distinguishable tissue layers contributing to tooth attachment in mosasaurs (Figs. 1–3,,7):7): (i) a thin layer of acellular cementum between root orthodentin and the remainder of the periodontium (Figs. 3A,B), (ii) the cellular cementum cone as a trabecular tissue providing the major portion of the tooth anchorage (Figs. 3A,D,E), (iii) the mineralized periodontal ligament as a fibrous mineralized tissue between the cellular cementum and the tooth bearing element/interdental ridge (Figs. 3A,F,G), (iv) the interdental ridge containing lamellar osteons (Figs. 3A,H,I), and (v) the tooth-bearing element featuring compact bone as the basic bony element of the jaw bone (Figs. 3A,J,K). These separate tissues were also delineated on the polished section of another mosasaur tooth (Fig. 2A) and following polarized light application (Fig. 4). Cellular cementum and mineralized periodontal ligament microstructure were remarkably similar (Fig. 3D-G). However, the mineralized periodontal ligament layer contained thick bundles of Sharpey’s fibers measuring 9.06+/−3.35μm in diameter, while fibers were less pronounced in the cellular cementum layer and measured only 4.35+/−1.9μm in thickness (Figs. 3B,D).
Polarized light analysis at three angles of inclination revealed significant changes in tissue birefringence between rotated planes of polarization (120, 240, and 360 degrees)(Fig. 4). Birefringence in fossilized mineralized tissues is an indicator for the presence of collagen fibers in the tissue prior to fossilization (Shackelford et al. 1964, Wojtowicz et al. 1998). Birefringence was most obvious in the fibrous cellular cementum bulb immediate surrounding the root orthodentin, followed by the surrounding mineralized periodontal ligament (Fig. 4). There was little or no birefringence in the interdental ridge coinciding with a low density of fiber bundles. Levels of birefringence in the tooth bearing element were low and depended on the polarizer/analyzer angle of rotation (Fig. 4). The mosasaur used for this analysis was Halisaurus sternbergi.
Calculations of calcium phosphate ratios obtained from electron microprobe analysis of mosasaur dental tissues, including interdental ridge, cellular cementum, tooth bearing element, root dentin, and enamel, resulted in values close to 2.0 (Table 1). There was no significant difference between the Ca/P ratios of those five tissues investigated and overall values were significantly higher than those of naturally occurring hydroxyapatite. Standard deviation values were higher in the cellular cementum (1.2, CEM) compared to other tissues investigated (below 0.1), indicative of varying degrees of mineralization in the cellular cementum layer. There is a possibility that Ca/P ratios were influenced by diagenetic changes caused by infiltrating fossil matrix. However, control measurements of the surrounding embedment resulted in Ca/P ratios close to infinity due to the absence of phosphorus outside of the embedded tissues, enhancing confidence in our microprobe analysis.
In order to identify mosasaur tooth attachment tissues and compare them with the histology of attachment tissues in other reptilians, a comparative study between mosasaur (Halisaurus sternbergi) and caiman (Caiman crocodylus) attachment tissues was performed (Figs. 2A,B). The massive mosasaur cellular cementum layer revealed an underlying fibrous structure using transmitted light analysis of thin ground sections (Figs. 1,3A,B) while it displayed a typical mineralized tissue morphology when a polished sample was photographed in incident light (Fig. 2A). Similarly, von Kossa’s staining of caiman cementum revealed pronounced mineralized fiber bundles as part of the cementum layer (Figs. 5A,B,C) while a routine ground section dye such as Paragon emphasized the cellular structure of the cementum layer in comparison to other tissue layers (Figs. 5J,K). Nevertheless, fiber bundles were also identified in Caiman cementum stained with Paragon (Fig. 5D). Together, this analysis indicates that the bulbous cone of mineralized attachment tissues surrounding the mosasaur root orthodentin consists of a fiber-rich tissue that closely resembles cellular cementum.
While our comparative histology analysis revealed similarities between mosasaur and caiman cellular cementum, there were differences in the morphology and appearance of the other two major mosasaur attachment tissues with other reptilian attachment tissues. One of the other two distinct mosasaur attachment tissues we refer to as mineralized periodontal ligament as it consists of a mineralized support tissue that forms the interface between cellular cementum on one side and interdental ridge/tooth bearing element on the other side (Figs. 2A; 3A,D; ;7).7). On both sides, the mineralized periodontal ligament was delineated by a layer of bundle bone (Figs. 1, ,3A).3A). In mosasaurs, the mineralized periodontal ligament displayed the trabecular histology characteristic for cellular cementum, but contained fiber bundles that were parallel oriented and more than double as thick (Fig. 3D vs. Fig. 3B). As a fiber-rich tissue that forms the interface between cementum and tooth bearing element/interdental ridge, the mineralized periodontal ligament might be equivalent to the fiber-rich periodontal ligament, especially since earlier studies showed remaining levels of calcification in the caiman periodontium (McIntosh et al. 2002).
The third major mosasaur attachment tissue is the interdental ridge (Zaher and Rieppel 1999). The mosasaur interdental ridge mostly consisted of osteons of lamellar bone (Figs. 3F,G). In comparison to the Caiman alveolar bone, the border to adjacent tissues was less delineated, and Sharpey’s fibers from the mineralized periodontal ligament infiltrated the coronal margin of the interdental ridge (Fig. 3F).
For comparison, we performed a histological analysis of the attachment tissues of an extant squamate, the Green Iguana (Iguana iguana)(Figs. 2C, ,6).6). Our analysis revealed several layers of mostly acellular cementum covering the surface of the root dentin and a cell-rich bone of attachment connecting adjacent teeth, while anchoring teeth to the tooth bearing element (Figs. 6A,F). The bone of attachment contained enlarged cellular lacunae, differentiating bone of attachment from other mineralized tissues of the periodontal apparatus (Fig. 2C, 6C–D). In addition, we did not observe any osteons in the iguana bone of attachment. Root cementum and bone of attachment were ankylosed with the tooth bearing element or the interdental ridge (Figs. 6A,E,F). In order to distinguish tooth attachment tissues from each other, diameters of lacunae in cross-section were compared. Lacunae within bone of attachment measured 9.75+/−1.75μm in diameter, and those in cellular cementum were slightly smaller (7.55+/−1.55μm diameter). In contrast, the tooth bearing element contained oval-shaped lacunae measuring 21.65+/−4.25μm in length and 6.1+/−0.95μm in thickness.
In the present study we have subjected mosasaur jaw fragments to a number of mineralized tissue histology techniques to understand the mineralized tissue microarchitecture involved in mosasaur tooth anchorage. Mosasaur tooth attachment was compared with the attachment apparatus of Caiman and Iguana in order to identify the basic tissue architecture underlying reptilian tooth attachment. Both the extinct Mosasaurs and the extant Iguanas are grouped as squamates while the Caiman belongs to the Archosaur clade (Fig. 8). Using ultrathin ground sections, electron microprobe analysis, semi-thin sections, and polarized light microscopy, five unique layers of mosasaurian tooth attachment were identified: (i) a thin layer of acellular cementum between root orthodentin and the remainder of the periodontium, (ii) a trabecular cellular cementum providing the major portion of the tooth anchorage, (iii) the mineralized periodontal ligament between the cellular cementum and the interdental ridge/tooth bearing element, (iv) the interdental ridge containing lamellar osteons, and (v) the tooth-bearing element featuring compact bone as the basic bony element of the jaw bone (Table 2, Fig. 7). It appears that our cellular cementum largely corresponds to the ‘osteocementum’ of Caldwell et al. (2003), and to the “aligned cellular cementum” of Caldwell (2007), our ‘interdental ridge’ is a re-classification of Caldwell’s alveolar bone (Caldwell et al. 2003), and while we have identified an extensive mineralized fiber layer between interdental ridge and cellular cementum, the ‘mineralized periodontal ligament’, Caldwell et al. (2003) report that the non-ossified component of the periodontal ligament is unrecognizable. Instead, they find morphologies of a cribriform plate-like structure and remnants of Sharpey’s fibers, which they believe to support the presence of a periodontal membrane (Caldwell et al. 2003). However, Caldwell et al. (2003) fall short of identifying a distinct periodontal ligament tissue layer between cellular cementum and interdental ridge.
The discussion over the condition of the mineralized tissue separating individual teeth from each other is not only of importance for the development and structure of mosasaur tooth attachment, but is also intimately linked to the debate over the presence of ‘true’ sockets and thecodonty of mosasaurian teeth. Lee (1997) classified the mosasaurian socket wall as a non-dental tissue, Zaher and Rieppel (1999) noted that tooth sockets of mosasaurs were merely apparent sockets, and Caldwell et al. (2003) thought of the mosasaurian sockets as real sockets that remain in place through multiple replacement events, similar to those found in crococilians. Our analysis revealed that the mosasaurian interdental ridge was intimately linked to the adjacent mineralized periodontal ligament by mineralized fibers and mechanical integration through ankylosis while the alveolar bone of mammals formed a stand-alone structural entity in conjunction with the jaw bone and separated from the tooth root by a non- or semi-mineralized periodontal ligament. We therefore retained Zaher and Rieppel’s nomenclature of the interdental ridge in contrast to the mammalian alveolar bone. The concept of ‘true’ thecodonty implies the presence of deep sockets which in depth exceed the length of the tooth crown, a lack of ankylosis, and the presence of genuine alveoli (Romer 1956, Motani 1997, Zaher and Rieppel 1999). In contrast, sockets of the mosasaur Halisaurus sternbergi studied here were shallow compared to the length of the crown, and teeth were ankylosed to the socket walls by means of a mineralized periodontal ligament. We noted that in many Crocodiliae, the distal regions of the jaw do not contain much alveolar bone in the midline zone, while the mesial portion of the jaw feature fairly prominent alveolar bone, suggesting that even in squamates, the alveolar bone is a variable structural element susceptible to functional evolutionary pressures. Nevertheless, histological similarities between the interdental ridge and alveolar bone such as the organization into osteons (Caldwell et al. 2003) appear to suggest that the mosasaurian interdental ridge might be an early step in the evolution of thecodont modes of tooth attachment in vertebrates.
Our comparitive analysis of mosasaurian and crocodilian attachment apparatus histology suggests that the large bulbous tissue mass surrounding the mosasaurian tooth root orthodentin is likely to consist of cellular cementum, in support of a classification first introduced by Caldwell et al. (2003). Depending on the type of analysis, transmitted light or incident light illumination of mosasaur ground sections versus von Kossa’s or Epoxy-Paragon stain for Caiman cementum, micrographs either highlighted a bone-like mineralized tissue layer or emphasized an underlying sub-structure of fiber bundles. The presence of mineralized fiber bundles in the cellular cementum of mosasaurs was especially prominent following transmitted light illumination, while in the Caiman, von Kossa’s procedure caused silver precipitates to outline mineralized fiber bundles, emphasizing the trabecular organization of crocodilian cellular cementum. Polarizing microscopy confirmed the presence of highly birefringent fiber bundles in the mosasaurian cellular cementum, indicative of the presence of collagen prior to fossilization, while electron microprobe analysis revealed high calcium/phosphate ratios. This cementum layer may be classified as intrinsic and extrinsic because of the strong presence of fibers within the cementum layer and the insertion of Sharpey’s fibers from the mineralized periodontal ligament. Together, these findings are consistent with the interpretation of the bulk of the mosasaurian attachment tissue surrounding the tooth root orthodentin as a cellular, trabecular fiber cementum.
In earlier studies (McIntosh et al. 2002) it has been proposed that the partially mineralized Caiman periodontal ligament was an evolutionary interface between the non-mineralized mammalian periodontal ligament and the rigid ankylosis that characterizes amphibians and reptilians. Here we suggest that the mosasaur ‘mineralized periodontal ligament’ represents yet another way to modularize the interface tissue between the root of the tooth and the tooth-bearing element. We have chosen the term ‘mineralized periodontal ligament’ to identify the separate mineralized tissue layer between the tooth-bearing element/interdental ridge and the cellular cementum. From a functional perspective, we expect that the mosasaurian mineralized periodontal ligament mostly functions as an attachment interface while the amphibian mineralized periodontal ligament mostly serves the purpose of elevation, but these functions are not well understood as of yet. Our electron microprobe analysis revealed that the mosasaurian mineralized periodontal ligament is highly mineralized in comparison to the periodontal ligament of crocodilians and mammals. The mineralized phase accounts for approximately 50% of its volume, the remainder consists of interstitial spaces. Moreover, the high fiber content of the mosasaurian mineralized periodontal ligament prior to fossilization as suggested by its birefringence in tandem with its trabecular structure points to highly flexible mechanical properties. In functional terms, the ‘mineralized periodontal ligament’ of mosasaurs provides a resilient mode of attachment, as does the partially mineralized periodontal ligament of Caiman, or the non-mineralized periodontal ligament of mammals.
The mineralized tissue involved in reptile tooth ankylosis has historically been referred to as ‘bone of attachment’ (Tomes, 1874), the nature of which remained notoriously elusive. In previous studies, we have compared the spongy cell mass immediately surrounding the mosasaur root orthodentin with ‘bone of attachment’ of other squamates (e.g., Zaher and Rieppel, 1999; Rieppel and Kearney, 2005). However, our histological analysis allows us now to reclassify this tissue layer as trabecular fiber cementum (cellular cementum, osteocementum). Moreover, we found significant differences between the trabecular organization of the mosasaur fiber cementum and the structure of the ‘bone of attachment’ of Iguana, featuring numerous enlarged lacunae that contain osteocytes.
Recent studies in mammals have shed light on potential underlying mechanisms of reptilian attachment tissue diversity. Wnt1/Rosa26 molecular marker studies, fluorescent and radioactive labeling experiments have confirmed the common origin of root cementum, alveolar bone, and periodontal ligament from migratory neural crest and a tooth-bound intermediary, the dental follicle (Ten Cate et al., 1971; Chai et al., 2000; Diekwisch, 2001, 2002). The dental follicle in turn consists of at least three distinct progenitor cell populations (Luan et al. 2006a) that may contribute to attachment tissue diversity through changes in composition and gene expression. At least two specific gene products have been identified that directly affect the mineralization status of the periodontal ligament, ank1 and ameloblastin (Ho et al. 2000, Fukumoto et al. 2004). In addition, the non-mineralized status of the periodontium may be controlled by Hertwig’s Epithelial Root Sheath (HERS), an epithelial cell layer that extends to the tooth apex of crocodylians and mammals (Luan et al. 2006b). These molecular and cellular mechanisms may specifically define the mineralized tissue interface involved in tooth attachment, from the ankylosis of many squamates to the fibrous mineralized periodontal ligament of mosasaurs or to the submicroscopically mineralized state of crocodilian ligaments, and eventually to the non-mineralized periodontal ligament that provides the basis of resilient tooth anchorage in mammals. Such concept is also featured in the exoskeletal building block theory of Smith and Hall (1993) which introduces a morphogenetic system consisting of a dental cap epithelium in conjunction with dental papillary and follicular ecomesenchyme as the underlying theme of gnathostome tooth structure diversification.
The history of vertebrate tooth attachment is characterized by an evolutionary transition from teleosts and amphibian ankylosis over various reptilian modes of attachment to the thecodont gomphosis of mammals, even though some teleost teeth are also attached by ligaments (reviewed in Peyer 1968, Gaengler 2000). A number of potential evolutionary benefits of thecodont attachment modes of attachment can be thought of, including a reduced chance of tooth breakage and a mechanical adaptability to antagonistic occlusal surface loads, especially in multi-cusped teeth. The studies presented here suggest that the modulation of the static or elastic state of the vertebrate attachment apparatus might be accomplished to a large extend through changes in the mineralized state of the periodontal ligament tissue layer. As shown in the previous paragraph, such changes may have been the result of changes in gene expression or caused by varying degrees of Hertwig’s Root Sheath (HERS) invasion into the mineralized attachment apparatus. Such a functional modification of a periodontal attachment tissue would be just one example for a functional reorganization of an ancestral phenotype in tandem with genetic accommodation (Luan and Diekwisch 2007). Evidence for the likelihood of such a scenario is provided by the presence of intermediates such as the semi-mineralized crocodilian attachment, in the ankylosis of the periodontium following removal of HERS, and in the change of the mineralized state of the periodontium following changes in ank1 and AMBN gene expression. In reptilians, the diversity in attachment structures indicates a significant evolutionary adaptability of reptilian taxa to various food environments. The resilient attachment apparatus in mosasaurs, maintained by a fibrous mineralized periodontal ligament and a highly trabecular cellular cementum, undoubtedly will allow the mosasaur to cope with various loads and degrees of hardness of prey encountered in Cretaceous oceans.
Funding for these studies by NIH grants DE18075 and DE19155 to XL as well as DE15425 and NSF grant MCB-0236226 to TGHD is gratefully acknowledged.