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Assessing Acrodont Dentition in Reptilia, with Special Attention to Replacement and Wear Adaptations

by

Yara Haridy

A thesis submitted in conformity with the requirements for the degree of Master of Science Department of Ecology and Evolutionary Biology University of Toronto

© Copyright by Yara Haridy 2018 Assessing Acrodont Dentition in Reptilia, with special Attention to Replacement as and Wear Adaptations

Yara Haridy

Master of Science

Department of Ecology and Evolutionary Biology University of Toronto

2018 Abstract

Tooth implantation has been conflated with other tooth characteristics, such as replacement, attachment, and morphology. Tooth attachment refers to the tissues that attach teeth, whilst implantation refers to the orientation of the tooth relative to the jaw. There are three main forms of tooth implantation identified in Reptilia: (1) thecodonty, where the tooth in implanted in a socket, (2) pleurodonty, the tooth is implanted against the side of the jaw, and (3) acrodonty the tooth is at the apex of the jaw; this thesis is concerned with the latter. Acrodonty has long been linked with a lack of replacement, which is because all modern acrodont do not replace their teeth; instead, they exhibit derived wear adaptations that help them counteract the loss of replacement. Here in this study, I explore the wear adaptations in extant acrodont reptiles, and analyze forms of acrodonty found within Reptilia in the Permian.

ii Acknowledgments

It has been quite the transition from an undergraduate heading to veterinary college, to the word of academia and paleontology. It would have been impossible to make this leap without the supportive community at University of Toronto Mississauga, I could not have found this path nor completed this thesis without everyone’s help, so I sincerely hope I do not forget anyone. Firstly, I would like to thank my supervisor Professor Robert Reisz, for initially taking me into his lab when I was a lost undergraduate looking to learn anatomy. I would like to especially thank him for putting up with my incessant questioning, stubbornness, and would like to acknowledge all the opportunities he has provided me that have fed and fueled my curiosity.

I would like to extend a special thanks to Diane Scott, whom vouched for me when I first came into the lab with no previous knowledge of paleontology, she fostered my growing curiosity and answered every question I threw her way without fail. She is a consistent and unwavering pillar of support that is the hallmark of the Reisz lab experience. I would like to thank her for all her support over these years, and for all the endless knowledge she enthusiastically shared, from fossil preparation to scientific illustration.

I would like to thank my supervisory committee for their assistance in the direction of these studies. Professor David Evans of the Royal Ontario Museum was a great help with his consistently innovative ideas, and for full access to the Paleohistology lab at the ROM. Professor Luke Mahler who’s extensive knowledge on all things reptilian aided in these studies.

I would extend thanks to Dr. Aaron LeBlanc and Dr. Mark MacDougall, the two of which provided endless entertainment and support in the Reisz lab. Mark put up with me through my first ever publication as an undergrad, and Aaron co-designed the main questions that I addressed in my thesis, and taught me all I know about histology, a skill that I will continue to include in my future work. Aaron and Mark have taught me so much about being a diligent scientist I could not be more thankful for having them as senior students while completing my degree. I would like to extend a special thank you to Bryan Gee, for putting up with my constant attitude, for his valiant attempt at teaching me about amphibians, for being my diligent copy editor, and for being a friend. I would thank Professor Dave Mazierski for teaching me about scientific illustration and for patiently designing the developmental model in chapter 3.

iii A huge thank you to Kevin Seymor who let me scour the collections at the ROM and allowed me to pick and choose from his precious collection to complete my studies, without his endless knowledge on all things living and dead these studies may not have come to fruition. The graduate students, and supports staff at the ROM always made for a welcoming and intellectually stimulating environment, and for that I am thankful.

Finally, I would like to thank my immediate family. My mother Sherine Hafez, and grandmother Nadia El-Enany, without these two strong stubborn women in my life I would not be who I am today. They taught me the value of tenacity, and supported every turn my life took, I could not wish for better role models. I would like to thank my brother Youssef, who made me endless coffees on late nights and took care of my sanity.

It takes an immense support network to be successful and happy in life, and I do not take mine for granted.

iv Table of Contents

Acknowledgements ...... iii Table of Contents ...... v List of Figures ...... ix

Chapter 1 Histological analysis of post-eruption tooth wear adaptations, and ontogenetic changes in tooth implantation in the acrodontan squamate Pogona vitticeps ...... 1

Introduction ...... 1

Materials and Methods ...... 2

2.1 Histology ...... 3

2.2 Confounding factors...... 3

Results ...... 4

3.1 External anatomy ...... 4

3.2 Histology ...... 6

Discussion ...... 18

Conclusion ...... 22

Literature Cited ...... 23

Chapter 2 Histology of the coronoid dentition with evidence of replacement in the Permian parareptile Delorhynchus ...... 32

Abstract ...... 32

Introduction ...... 33

Materials and Methods ...... 34

Results ...... 35

10.1.1 Mandible ...... 35

10.1.2 Coronoids ...... 43

10.1.3 Dentition ...... 44

10.1.4 Histology ...... 45

Discussion ...... 48

v 11.1 Multiple coronoids and coronoid dentition among Palaeozoic reptiles ...... 48

11.2 Taxonomic status of Bolterpeton carrolli ...... 53

Conclusions ...... 55

Literature Cited ...... 56

Chapter 3 Opisthodontosaurus as a model for acrodont tooth replacement and dental ontogeny ...... 60

Abstract ...... 60

Introduction ...... 61

Materials and methods ...... 62

Results ...... 63

17.1 External morphology ...... 63

17.2 Histology ...... 68

Discussion ...... 73

18.1 Opisthodontosaurus as a model for acrodont tooth replacement...... 73

18.2 Opisthodontosaurus as a model for ontogenetic tooth migration ...... 79

18.3 Ontogenetic tooth loss and feeding biomechanics ...... 81

Conclusion ...... 82

Literature Cited ...... 84

vi List of Figures

Figure 1-1: A comparative figure showing the external morphological differences in the dentition and mandibles between a juvenile and an adult specimen of Pogona vitticeps………………….05

Figure 1-2: Longitudinal sections of juvenile mandible of Pogona vitticeps with special focus on tooth histology...... ….08

Figure 1-3: Coronal sections of juvenile mandible of Pogona vitticeps with a special focus on tooth histology……………………………………………………………………………...…..10

Figure 1-4: Longitudinal sections of adult mandible of Pogona vitticeps with special focus on tooth histology...... ….13

Figure 1-5 Coronal sections of adult mandible of Pogona vitticeps with a special focus on tooth histology………………………………………………………………….……………………..15

Figure 2-1: Photographs and associated illustrations of Delorhynchus mandible in lingual and labial view………………………………………………………………………….…………….29

Figure 2-2: Photographs and associated illustrations of Delorhynchus mandible in dorsal and ventral view……………………………………………………………………...... ……………..31

Figure 2-3: Serial histological sections of a Delorhynchus mandible showing the internal anatomy and reinforcement of the mandible…………………………………………...………..33

Figure 2-4: Histological anatomy of the coronoid process and associated dentition in Delorhynchus ……………………………………………………………………………...…….38

Figure 2-5: Strict consensus tree obtained from the 6 optimal trees produced by the phylogenetic analysis, showing the prevalence of multiple coronoids as well as coronoid dentition in amniotes………………………………………………………………………………………….41

Figure 2-6: Preserved replacement teeth in coronoid dentition visualized through photography and a scanning electron microscope…………………………………………………………….44

ix Figure 2-7: Scanning electron microscope dentition comparison between Delorhynchus and the holotype of Bolterpeton carrolli…………………………………………...... ………………….46

Figure 3-1: A sequence portraying the ontogenetic change in tooth count and morphology in Opisthodontosaurus carrolli……………………………………………………………………..56

Figure 3-2: The specimens that exhibit morphology that supports the replacement model in Opisthodontosaurus carrolli………………………..……………………………………………59

Figure 3-3: Histological anatomy of the dentary and associated dentition in Opisthodontosaurus carrolli ………………………………………………………………………………………...... 61

Figure 3-4: Histological evidence of migration of dentition and asymmetrical growth of the jaw in Opisthodontosaurus carrolli …………………………………………………………………64

Figure 3-5: The proposed model of acrodont replacement for Opisthodontosaurus carrolli with stepwise replacement illustrated……………………………………………………………

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Chapter 1 Histological analysis of post-eruption tooth wear adaptations, and ontogenetic changes in tooth implantation in the acrodontan squamate Pogona vitticeps

Introduction

Reptilian dentition has been extensively studied in both extinct and extant taxa, and for the vast majority of these taxa, there is constant replacement of teeth, a condition known as polyphyodonty. However, in a subset of reptiles, there has been an evolutionary cessation of replacement, a condition known as monophyodonty. Among lepidosaurian reptiles, this suppression of replacement is limited to Sphenodontidae (), Chamaeleonidae, and , with the latter two being grouped within the clade () (Pyron et al., 2013). This squamate group is aptly named for the acrodont style implantation of the dentition, and all acrodontians have apically implanted teeth making up the majority of their dentulous surface (Jenkins et al., 2017). This is in contrast to the condition found in most squamates and other reptiles (Zaher and Rippel, 1999; Delgado et al., 2003a; LeBlanc and Reisz, 2015) in which the dentition is implanted to the lingual surface of the jaw bone, a condition known as pleurodonty, exemplified in taxa like Iguana iguana (Throckmorton, 1976; Montanucci, 2008; Kline and Cullum, 2017). The most studied form of implantation is generally identified as thecodonty, where the tooth is implanted in a deep socket; this form of implantation is found in all mammals and also occurs within crocodilians and in many extinct archosaurs (Brown et al., 2015; García and Zurriaguz, 2016). Tooth implantation should not be conflated with tooth attachment which refers to the tissue that attaches the tooth to the dentulous bone.

Acrodonty in Reptilia is largely associated with a lack of tooth replacement (Zaher and Rippel, 1999; Smirina and Ananjeva, 2007), although it is important to note that acrodonty is also found in some extinct reptiles (Simões et al., 2015) and non- vertebrates such as piranhas (Shellis and Berkovitz, 1976), that all replace their dentition. This lack of replacement poses a mechanical dilemma, as the supposed function of constant replacement is to avoid

1 2 excessive wear; accordingly, higher rates of replacement are often seen in herbivorous taxa, as their fibrous diet and often of mastication requires a constant renewal of their dentition. In extreme instances, there are examples of starvation in herbivorous mammals that lack continuous replacement and that have worn their dentition to such a degree such that it is no longer functional (Spencer, 2005). This raises the question: if many acrodontians with no replacement of their dentition are relatively long-lived (Zari, 1999; Smirina and Ananjeva, 2017), how are they able to maintain a viable occlusal surface? Essentially, the question is how do acrodontians adapt to dental wear at a tissue level? This question has been addressed through histology in aegyptia (Throckmorton, 1979) and Chamaeleo calyptratus (Buchtová et al., 2013; Dosedělová et al., 2016a), members of acrodontan Uromastycinae and Chamaeleoninae, respectively (Pyron et al., 2013). There are six other groups within Acrodonta that presumably also lack replacement and have undocumented wear adaptations. This study aims to test if the wear adaptations that have already been documented in the literature indeed extend beyond these two clades; if not, how do these various taxa adapt to dental wear, and what implications does this have for the evolutionary timing of these wear resistant adaptations within acrodontians? This study describes the ontogenetic change in dentition of Pogona vitticeps, with a focus on comparisons of wear adaptations of this member of Agamidinae to those previously described in Uromastycinae and Chamaeleoninae. It has been previously proposed that ichthyosaurs and alligators can change implantation types through ontogeny by growth in the jaw ramus and additional ossification on the lingual side (Motani, 1997). However, this is the first study to document the change in implantation types through ontogeny due to osteological remodeling of the dentary, with evidence of a change from pleurodont implantation to acrodont implantation in a modern squamate. This has implications on how we view implantation categories as they are likely to be more ontogenetically variable than previously thought.

Materials and Methods

The illustrations and diagrams found in the figures were made using Adobe Photoshop CS6 and Adobe Illustrator CS6. All specimens in this study have been photographed prior to sectioning using a Canon EOS40D. To access normally inaccessible anatomical features of the lower jaw and its dentition, several mandibles were sectioned in both coronal and transverse

3 planes. All the Pogona vitticeps specimens belong to the Royal Ontario Museum (ROM) recent osteology collection, and were sectioned with permission. In this study, the genus Pogona was represented by the central bearded dragon (P. vitticeps). P. vitticeps was sectioned at two ontogenetic stages, a juvenile stage ROM R8234 with 16 tooth positions and a snout vent (SV) length of 103mm, and ROM R8507 with 17 tooth positions, and a SV length of 222mm.

2.1 Histology

All thin sections were done following the ROM histology protocol and executed in the ROM vertebrate paleontology thin sectioning facility. Specimens were embedded in AP Castolite acrylic resin, vacuumed and left to cure for a minimum of 24 hours. All specimens were cut using a Buhler Isomet 1000 wafer saw at a low speed of 275rpm. The specimens were mounted on plexiglass slides using Scotch-Weld SF-100 cyanoacrylate. The slides were then mounted on the Hillquist grinding cup and ground down using the grinding cup until optical clarity was achieved; subsequently the specimen was manually ground using progressively finer grit suspensions on glass plates, beginning with a 600-grit silicon carbide powder and working down to a 1-micron aluminum oxide powder. All slides were imaged using a Nikon DS-Fi1 camera mounted to a Nikon AZ 100 microscope fitted with crossed-polarizing and lambda filters and an oblique illumination slider and NIS-Elements software registered to R. R. Reisz of the University of Toronto Mississauga. The images in Figures 6 and 7 were obtained using a Jeol Neoscope JCM-5000 scanning electron microscope (SEM).

2.2 Confounding factors

It is important to note that all squamate specimens examined in this study were donated to the Royal Ontario Museum (ROM) extant osteological collection; as such, all of the specimens examined here, unless indicated otherwise, originated from the pet trade. This is possibly a factor as reptilian husbandry can affect bone growth as well as tooth wear. Furthermore, these reptiles were all likely given tap water, which in North America is fluorinated, possibly affecting the enamel hardness and thereby the wear patterns; the extent of any effect of fluorination on non-mammalian enamel has not been documented.

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Results

3.1 External anatomy

The external mandibular and dental morphology is apparently different between the juvenile and adult specimens of Pogona vitticeps (Figs. 1A, B). The juvenile specimen of P.vitticeps ROM R8234 has fewer tooth positions (16 tooth positions) occupying the space between the symphysis and the coronoid process. There are a few mandibular characters of ROM R8234 that identify it a juvenile: (1) the symphysis is poorly ossified, (2) the mandible is less robust in apparent bone density, as well as in dorsoventral width, and (3) the mandible is relatively short, with the dentulous region making up more than half the total length. It is also important to note that in the juvenile specimen, the wear facets are not as well developed as those seen in the adults. This specimen of P. vitticeps is found to have pleurodont dentition in the first two tooth positions on the rostral portion of the mandible. This pleurodont dentition is conical and tapers to a point; this appears to represent the common condition among many, but not all agamids. Posterior to the pleurodont dentition, the remaining tooth row appears to be acrodont in attachment and maintains a simple triangular morphology, where the tooth body is mediolaterally compressed and does not seem to have the multi-cuspid morphology that other acrodontians, like chameleons and Uromastyx display. Compared to the older anterior teeth, the dentition is larger in overall size posteriorly, likely correlated with the age of the individual teeth, with the youngest dentition added posteriorly being largest. It appears that the new posteriorly added tooth is not ankylosed to the jaw bone prior to the development of the next tooth in the series. Instead, the dentition appears be attached to the jaw only by soft tissue. This is readily recognizable even by external observation, because the last two teeth are not oriented at an angle that is congruent with the rest of the dentition (Fig. 1A). Lastly, the initiation of new dentition seems to be surpassing the rate of jaw growth, as the newest and last tooth position is growing directly against, and partially resorbing (Fig. 1A), the coronoid process, which does not allow sufficient space for the next tooth position.

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FIGURE 1. A comparative figure showing the external morphological differences in the dentition and mandibles between a juvenile and an adult specimen of Pogona vitticeps. A) Right mandibular ramus of juvenile specimen ROM R8234. B) Right mandibular ramus of adult specimen ROM R8507. Abbreviations; ad, acrodont dentition; cp, coronoid process; pd, pleurodont dentition; wf, wear facets. Scale bar = 1 cm.

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Several ontogenetic changes can be recognized in the adult specimen of Pogona vitticeps, ROM R8507, including an increase in the number of tooth positions. This specimen has 17 tooth positions, although other specimens have been found to have as many as 19 tooth positions; a definite tooth count was difficult to ascertain by direct examination of the external morphology due to wear, but was later verified in thin section. Wear on the adult mandible is evident on both the acrodont dentition and the jaw bone. Interestingly, the anterior pleurodont dentition was mostly unworn in the adult specimen, or affected to a minimal degree on other adult specimens examined; this is similar to the condition seen in Agama agama, which has been documented to replace its anterior dentition (Cooper et al. 1970). However, the anterior acrodont dentition is all but worn away, making it difficult to differentiate it from the jaw bone; to circumvent this problem, tooth counts were made under a microscope and later confirmed in thin section, when possible. The wear observed on the anterior acrodont dentition was extensive and similar to that seen in Uromastyx, a taxon that can become functionally edentulous in adulthood (Throckmorton, 1979).

The second line of evidence of wear is found on the mandible itself in the form of wear facets, which are only present on the labial side of the dentary where the maxillary dentition occludes, interdigitating between dentary tooth positions. Wear facets have been characteristically found in acrodont squamates as far back as the Cretaceous (Simões et al., 2015), which is due to the maxillary dentition wearing down on the dentary bone during mastication and passive occlusion. These wear facets are present along the posterior two-thirds of the tooth row but are best seen in the posterior dentition of adult specimens of Pogona vitticeps. However, in adult individuals of other acrodontians, like chameleons, the wear facets are found along the entire tooth row. Lastly, it is important to mention that the jaw ontogenetically increases posteriorly in length and dorsoventrally in width, with the articular increasing in robustness and the coronoid process moving posteriorly relative to the tooth row. This ontogenetic change effectively creates more space for the posterior addition of dentition, a feature that is frequently seen in lepidosaurs (Berkovitz and Shellis, 2017).

3.2 Histology

Transverse and coronal sections of the mandible of a juvenile specimen of Pogona vitticeps, ROM 8234 were examined (Fig. 2&3). The juvenile jaw is not as well ossified as the

7 adult (ROM R8507) and has a medial curvature anteriorly; this made obtaining sections of the anterior and posterior dentition within the same sectioning plane difficult, therefore the pleurodont dentition of the juvenile was not included in this study. In transverse section, each tooth is composed of dentine and no other dental tissues, such as cementum or enamel are visible. However, in coronal section all the common dental tissues are identifiable. The dentition itself is not remarkable, with the dentine comprising the bulk of the tooth, with characteristic radiating dentinal tubules. The enamel that should cover the crown portion is not evident in transverse section even in cross polarized light (Fig. 2C), likely because the teeth are mediolaterally compressed in morphology, so a transverse plane of section would only allow us to visualize the anterior and posterior edges, leaving the bulk of the enamel on the lingual and labial surfaces. The enamel is readily visible in the youngest dentition in coronal section (Fig.3B) as this plane of section transects the labial and lingual surfaces of the tooth. The enamel is fairly thick, which has also been reported in Uromastyx (Throckmorton, 1979). Furthermore, the enamel is of equal thickness on the lingual and labial sides of the tooth crown (Fig.3B). On the lingual side of the tooth, the tapering edge of the enamel leads down to a layer of acellular cementum, meeting at the cementoenamel junction which defines the boundary between the anatomical crown and root of the tooth. It is likely that the cementum cannot be visualized on the labial side because the alveolar bone is denser and has grown to meet the cementum, effectively attaching the tooth while obstructing the cementum, or possibly because of resorption of the cementum.

In longitudinal section, the relationship of the dentition to the jawbone is not easily discernable. However, the interaction between the individual tooth and its neighboring teeth is best visualized in this plane (Fig. 2). This plane of section also gives a more complete idea of the incremental maturation of dentition, this is based on the thickness of dentine. There is distinct tissue that attaches the teeth to each other as well as to the jaw bone. This tissue is tentatively identified as alveolar bone (sensu LeBlanc and Reisz, 2015); this identification is based on the position and presumed function of the tissue rather than on its histological appearance which does not conform to the surrounding lamellar bone but is rather woven and slightly trabecular in appearance. This tissue attaches the teeth to each other, as well as to the jaw bone proper, a function that has been attributed to ‘bone of attachment’ (Ananjeva and Smirina, 2007) or to alveolar bone (Budney et al., 2006; Caldwell, 2007; LeBlanc and Reisz, 2013, 2015; LeBlanc et

8 al., 2016a). The alveolar bone in this specimen has a woven appearance that is less organized than the bone that makes up the dentary; however it lacks a trabecular or ‘spongy’ appearance that is found in other squamates, such as snakes (Budney, 2004; Budney et al., 2006). The alveolar bone in Pogona vitticeps is also not distinguished from the jaw bone by a reversal line; this is possibly an effect of the plane of section, or an effect of unequal remodeling (Fig. 2). It is important to note that the dentition in this specimen is not yet fully ankylosed to the jaw bone; however, each tooth seems to ossify to the surrounding dentition, which occurs prior to full ankylosis and which mirrors what has been documented in Chamaeleo calyptratus (Buchtová et al., 2013; Dosedělová et al., 2016a). Another important note is that the pulp cavities remain open in the youngest (posterior most) teeth and progressively infill with dentine (Figs. 2B-D). It is unclear in this section if the pulp cavity has been completely ‘obliterated’ (completely infilled with no sign of vasculature) as previously reported in the agamid Uromastyx (Throckmorton, 1979). The infilling of the pulp cavity with dentine is most extensive in the oldest (anteriormost) teeth and less so posteriorly in the youngest dentition. This phenomena has also been observed in Hadrosaurs, who progressively infill their dentition with dentine as it nears the occlusal surface in their dental batteries, then wear away the entire tooth (LeBlanc et al., 2016b; Bramble et al., 2017).

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FIGURE 2. Longitudinal histological sections of the juvenile mandible of Pogona vitticeps with special focus on the dentition. A) External view of specimen ROM R8234, box outlining the dentition cut. B) A section of the posterior 7 tooth positions. C) A section of the posterior 7 tooth positions in cross polarized light. D) A schematic representation showing the distinct tissues as well as the progressive ankylosis of the teeth. Abbreviations; ab, alveolar bone; de, dentine; jb, jaw bone; pc, pulp cavity.

In the coronal section of the juvenile specimen of Pogona vitticeps, it is evident that both the shape of the dentition, as well as the manner in which the individual teeth are implanted are more in line with the pleurodont condition. In coronal section (Fig. 3A, C) the lingual side of the tooth is markedly greater in length than that of the labial side. Although both ends of the tooth

10 are ankylosed to the jaw, it is clear that there is more contact with the jaw bone as well as more attachment tissues on the labial side, a condition reminiscent of pleurodont implantation. Apart from the obvious labial bias of attachment, alveolar bone can be seen at the base of the tooth, more woven than the rest of the jaw bone, yet apparently still lacking the trabecular structure that is usually associated with alveolar bone. In coronal section (Fig. 3B), the reversal line defining the boundary between the new alveolar bone and the preexisting jaw bone is visible in cross polarized light. The labial side of the tooth (Fig. 3C) is shorter and is attached to the jaw bone with more attachment tissue than the lingual side, and the labial side appears to be actively remodeled by osteoblasts and osteoclasts (Fig. 3D). The osteoclast on the labial side of the tooth is identified on the basis of multiple nuclei, general shape and the resorption bay that is created in the dentine (Witten and Huysseune, 2009). The high density of bone cell lacunae directly posterior to the osteoclast are identified as osteoblasts, indicating that the labial side of the tooth is being resorbed and bone is being deposited in its place. It is also important to note the cancellous bone that makes up the jaw of this juvenile, the ‘strut’ like structures likely give the mandible form and function prior to full ossification and maturity.

Lastly, a coronal section through the coronoid process (Fig. 3E), shows the presence of a developing tooth. Its identification as a developing tooth is based on its general shape, as well as the presence of thick enamel relative to the amount of dentine. The presence of more enamel than dentine denotes an early stage of tooth development (Erickson, 1996; LeBlanc et al., 2016b). The presence of this developing tooth was only discovered by sectioning the specimen since there were no external indicators that this tooth was buried within the bone of the coronoid process. This new tooth is developing within the coronoid process, and visibly resorbing the bone tissues of both the coronoid and the dentary, effectively making space for itself.

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FIGURE 3. Coronal sections of juvenile mandible of Pogona vitticeps with a special focus on tooth histology. A) Coronal section of the jaw and tooth of a juvenile specimen of P.vitticeps ROM R8510 showing minimal ossification of the jaw bone, and pleurodont tooth attachment. B) A close up of the ROM R8510 juvenile specimen dentition, showing unworn morphology. C) A coronal section of a juvenile specimen of P.vitticeps ROM R8234 showing pleurodont implantation, and remodeling. D) A close-up of the attachment site in ROM R8234, showing the labial side of the dentition being resorbed by the osteoclast. E) A coronal section of the coronoid process in a juvenile specimen of P.vitticeps ROM R8234 showing a tooth developing lingually inside the coronoid and dentary. F) a close up of the tooth in the jaw bone, showing the resorption of the jawbone around newly developing tooth. All un-labeled scale bars are 1000m. Abbreviations: ab, alveolar bone; ac, acellular cementum; cb, cancellous bone; cp, coronoid process de, dentine; dt, developing tooth; lb, lamellar bone; en, enamel; ob, osteoblast oc, osteoclast; rb, resorption bay.

In the transverse and coronal sections of the mandible of an adult specimen of Pogona vitticeps, ROM 8057, the lamellar bone makes up the main body of the mandible (Fig. 3). In coronal section, it can be seen that the large cancellous spaces seen in the juvenile have been infilled incrementally by lamellar bone, giving the mandible an osteological density that was not present in early ontogeny. As previously reported in agamids, the bone tissue is not highly vascularized (Ananjeva and Smirina, 2007), and is not highly remodeled, especially in the dentary. This is in line with the findings in the adult jaw, where no reversal lines or large areas of remodeling are found. No primary or secondary osteons can be identified in the transverse sections. In coronal section, an osteon could be identified ventral to the tooth implantation site (Fig. 5A). In transverse section (Fig. 4C), posterior to the most worn dentition, the wear facets become a marked feature of the dentary’s labial surface. The pervasiveness and the depth of the wear facets should not be considered informative in thin section, as the variation of depth is a false impression, and is due to the sectioning plane in combination with the slight curvature of the dentary. The wear facets form pseudo-pedicels for the tooth remnants; these should not be confused for the ‘bony pedicles’ that have been identified developmentally in chameleons (Buchtová et al., 2013). These pseudo-pedicels are formed by the wear facets, as the maxillary teeth wear away lamellar bone between the functional dentition on the jaw, leaving the

13 remaining tooth caps on secondarily formed pedicels of lamellar bone (Fig. 4C-D), this gives the tooth implantation region the distinctly acrodont appearance.

The dentition in the adult specimen seems to have undergone ontogenetic changes, specifically in the region of the acrodont teeth, with the presence of a clearly acrodont implantation with no lingual bias. The anterior pleurodont dentition is shown to maintain its vasculature, which is associated with an open pulp cavity, this is typical of pleurodont dentition among squamates. Perhaps the most interesting feature of the transverse sections is seen in the worn acrodont teeth directly posterior to the pleurodont pair (Fig. 4). The teeth are worn to such an extent that often no dentine or enamel is detectable (Fig. 4B), even in thin section. However, the vasculature is maintained and denotes tooth positions, and the pulp cavity remains open and vascularized for the majority of the functional life of the tooth. The pulp cavity cannot be breached, so it is assumed that at some point the tooth is entirely filled and the vasculature is sealed so the tooth may entirely be worn away, as seen in the adult condition Thus, the teeth appear to remain viable into adulthood (Fig. 4E), which is in contrasted to the condition reported in Chameleo (Dosedělová et al., 2016a) and in Uromastyx (Throckmorton, 1979). The vasculature is best seen in Figures 4 and 5.

The tissues between the tooth and the platform of lamellar bone, when viewed in cross- polarized light (Fig. 5B) are particularly interesting because they are clearly distinct from both the tooth and the jaw bone. These tissues provide evidence of remodeling, and the true extent of remodeling can be seen in coronal section because the orientation of the bone is uneven and rather woven. This indicates the occurrence of relatively fast deposition, and is unlikely to be the original alveolar bone that was identified in the juvenile specimen. The woven appearance identifies this as woven bone, and is tentatively identified here as a remodeling zone (sensu Budney, 2004) (Fig. 4C;5B). In coronal section (Fig. 5B) the remodeling zone is clearly identifiable in cross polarized light, and the distribution of dental tissues and bone is markedly different than that previously described in the juvenile specimen. The coronal sections of the adult also show evidence of secondary dentine that has been growing into the pulp cavity post- ankylosis, clearly identifiable under cross polarized light (Fig 5A,B) where the primary and secondary dentine refract light differentially. Interestingly, enamel is still present, but it is only found on the lingual side (Fig. 5A), and the dentine and pulp cavity are generally maintained.

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However, the overall shape of the tooth is markedly different to that reported in the juvenile, and the implantation here appears more acrodont, like that described in literature (Budney, 2004).

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FIGURE 4. Longitudinal sections of adult mandible of Pogona vitticeps with special focus on tooth histology. A) External view of specimen ROM R8507, box outlining the dentulous area

16 sectioned. B) Broad view showing the variation between the anterior and the posterior dentition. C) A closeup of the worn dentition showing wear facets and remodeling zones; D) broad view showing the variation between the anterior and the posterior dentition, showing the depth of wear facets and arrangement of vasculature. E) A close up of the anterior dentition with open pulp cavities and associated vasculature. Abbreviations: de, dentine; jb, jaw bone; pc, pulp cavity; vc, vascular canal; wf, wear facet. The arrows demarcate the extensive vasculature leading to pulp cavities.

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FIGURE 5: Coronal sections of adult mandible of Pogona vitticeps with a special focus on tooth histology. A) Coronal section of the jaw and tooth of an adult specimen of P. vitticeps ROM R8507 showing the maintained vasculature and worn enamel on the labial side. B) Coronal section of the jaw and tooth of an adult specimen of P. vitticeps ROM R8507 showing the extensive remodeling of the tooth attachment site as well as the tooth. Abbreviations: de, dentine; lb, lamellar bone; en, enamel; vc, vascular canals; rz, remodeling zone.

Discussion

Tooth replacement has been a topic of great interest in recent years in groups ranging from fish to mammals and from extinct to extant, and there have been several studies documenting the presence and the patterns of development of dentition (Westergaard and Ferguson, 1990; Richman and Handrigan, 2011; LeBlanc and Reisz, 2015) . However, there has been relatively little work on the anomalous squamates that has completely ceased tooth replacement, the acrodontians. Acrodonta (Cope, 1864) is aptly named for the form of tooth implantation that this group possesses, namely one where the teeth are attached to the apex of the jaw (acrodonty). Grouping based on tooth implantation has divided squamates between acrodontians and pleurodontians (Cope, 1864; Budney, 2004), the latter of which attach their dentition to the lingual margin of the jaw. The classic categories of acrodonty, pleurodonty, and thecodonty have been used as descriptors, as well as phylogenetic characters(Zaher and Rippel, 1999), and continue to be pervasive in literature (Jenkins et al., 2017) but have been called into question by Estes et al. (1988) who suggested these categories are artificial and are not likely representative of natural groupings.

True teeth in lower vertebrates are well known for their extensive patterns of development and replacement through their life (Zaher and Rieppel, 1999; Delgado et al., 2003b; LeBlanc and Reisz, 2015; LeBlanc et al., 2016b), this is why any condition that deviates from polyphyodonty is unusual and worthy of study. An important example of non-polyphyodont dentition is seen in mammals, in which there are only two generations of dentition, the deciduous teeth and the permanent teeth. Some mammals such as shrews have even forgone the deciduous phase by resorbing the dentition prior to eruption, giving them one tooth generation proper

19

(Järvinen et al., 2009). Other than mammals, most fish (but see ratfish, e.g., Huber et al., 2008), amphibians, reptiles and even pre-mammalian synapsids have continuous tooth replacement through life, making acrodontian squamates an anomaly amongst toothed vertebrates. The lack of replacement comes with a set of challenges, two of which are addressed here. The first challenge is how does and organism grow the jaw whilst having permanently ankylosed dentition and whilst maintaining occlusion with the maxillary dentition? The second challenge is how to maintain a single set of functional teeth through the lifetime of an , which essentially is a problem of combating or adapting to wear. These two obstacles are also faced by mammals, which have one primary set of teeth throughout most of their life. In mammals, the issue of maintaining occlusion appears to be solved by maintaining a ligamentous tooth attachment, which remains mobile as the mandible grows and remodels (Lumsden and Osborn, 1977; LeBlanc and Reisz, 2013). The issue of wear is at least partially addressed by having much thicker prismatic enamel than that found in most reptiles (Dauphin and Williams, 2008; Kieser et al., 2009). However, the question remains how reptiles that permanently ankylose their dentition to the jaw and those with reptilian enamel adapt to growth and wear.

This study found that the agamid Pogona vitticeps has a fairly uniform layer of enamel on both the lingual and labial sides on their mandibular teeth, and the layer is relatively thick for reptilian dentition. The thick enamel also seems to occur in two other acrodontians, the chameleon of (Buchtová et al., 2013; Dosedělová et al., 2016b) but is not explicitly commented on, while the enamel of Uromastyx has been documented as ‘thickened’ (Cooper and Poole, 1973; Throckmorton, 1979). This is interesting because this shows that thickening of the enamel is a convergent adaption in both some squamates and in mammals. Furthermore, Uromastyx, a herbivorous acrodontian, has been reported to have thickened prismatic enamel (Throckmorton, 1979), similar to mammalian enamel, although this has not been confirmed subsequently.

Enamel thickening is not the only adaptation that acrodontians appear to have evolved in order combat wear. Previous studies of chameleons and Uromastyx have shown that their pulp cavities were infilled with ‘mineralized tissue’ (Dosedělová et al., 2016b) or ‘bone’ (Throckmorton, 1979). The likely purpose of this infilling is to prevent the pulp cavity from being exposed as the external surface of the tooth is worn away. Both studies also reported either disappearance or significant restriction of vasculature that initially supplied the dentition in early ontogeny. Dosedělová et al. (2016) also showed increased mineralization in the bone

20 underlying the tooth-bone junction, and Throckmorton (1979) found that the bone below the teeth had become more compact in appearance rather than cancellous. These findings are quite comparable with one another, even though Uromastyx and chameleons are on two disparate branches of Acrodonta (Pyron et al., 2013). These results then beg the question, is pattern more widespread across acrodontians.

In Pogona vitticeps, the pulp cavity is also greatly diminished through ontogeny, but is not completely ‘obliterated’, as seen in Uromastyx. It remains unclear what tissue infills this cavity, although preliminary data suggest that it is secondary dentine. This is contrast to the condition seen in Uromastyx (Thockmorton, 1979), although secondary dentine has also been reported in Uromastyx, the bulk of the infilling is done by ingrowth of bone. In all the sampled sections of P. vitticeps, the teeth fail to show the bone infilling reported in Uromastyx. The matrix that infills the pulp cavity does not seem to have any of the cellular spaces reported in Uromastyx, instead it is completely acellular. Additionally, this mineralized material at the base of the dentition has a woven appearance in cross-polarized light, differentiating it from the primary dentine that makes up the body of the tooth (Fig. 5B). This is also different from the secondary dentine that has in-filled the majority of the pulp cavity, their woven appearance indicates extensive remodeling at the base of the tooth, especially when compared to the juvenile dentition.

The dentine and enamel on the labial side of the mandible are worn in the older specimens of P. vitticeps, which is compatible with the findings in Uromastyx (Throckmorton, 1979) , where depending on the tooth position, the enamel and dentine were either completely worn away or worn to such a degree that the lingual side of the tooth retained a much thicker layer of these two tissues. This pattern is likely caused by the combination of extensive wear from feeding and passive occlusion with the maxillary dentition, as well as the complete lack of tooth replacement. Interestingly, the vasculature that leads to the pulp cavities is still present in the adult specimens of Pogona vitticeps indicating that even the most worn teeth probably remained viable until they were eventually entirely filled, killing the tooth then subsequently wearing it away.

Continuous growth of the mandible throughout ontogeny is concurrent with the increased size of the skull and could not be interpreted exclusively as a functional adaptation for increasing

21 the available dentulous space. This study of Pogona vitticeps has shown that the growth of the jaw and the initiation of additional tooth development are decoupled processes. This is most evident in the juvenile specimen where the dentition is growing into or within the coronoid process (Fig. 3E,F), where the youngest un-erupted tooth is resorbing the ventral portion of the coronoid process in order to continue developing. This indicates that in the early stages of ontogeny tooth development likely happens at a rate faster than dentary growth. This is reinforced by comparing the juvenile specimen (103mm SV length) which has 16 tooth positions whereas the adult, which is more than twice as long (222 mm SV length) only has 17 tooth positions. This shows that attaining the maximum number of teeth likely happens relatively early in ontogeny, well before attaining maximum adult size, indicating that tooth development slows, and likely stops later in ontogeny, while the jaw bones continue to grow. The mandible of Pogona vitticeps undergoes many changes through ontogeny, but there seems to be little distortion of the tooth row during growth. This is likely achieved by growth of the jaw appositionally, with deposition of parallel-fibered bone both internally and externally to achieve the increase in internal ossification, width and length that is seen in the adult without remodeling or migration of the ankylosed dentition.

Lastly, it is important to note that acrodont implantation is defined rather ambiguously, identifying it as attachment to the ‘edge’ of a jaw (Peyer, 1968), as teeth ankylosed to the ‘apex’ of the jaw by cement (Edmund 1969), or even as the fusion of dentition to the ‘margin’ of the jaw (Motani, 1997). Eventually, the lack of replacement also became a character of acrodont tooth implantation (Zaher and Rippel, 1999) because of the condition being present in acrodont squamates. These definitions tend to imply an evolutionary progression of tooth implantation (Budney et al., 2006), when in reality, the traditional categories of acrodonty, pleurodonty, and thecodonty are, at best, descriptive characters. As seen in P. vitticeps, morphology can change through ontogeny. The teeth in the juvenile P. vitticeps are unequal in shape, with the lingual side being much longer than that of the labial side (Fig. 3), and early in ontogeny the implantation is also pleurodont, with the attachment only occurring on the labial side. This unequal attachment, favoring the labial side is typically found in taxa with pleurodont implantation. Implantation becomes acrodont in later stages of ontogeny through wear of both the dentition and the underlying bone, as well as with basal remodeling (Fig. 3D) of the teeth. Thus, at least in the agamid P.vitticeps, the dentition changes from pleurodont to acrodont in

22 implantation. This is significant because it implies that we should not use implantation categories as phylogenetic characters if the ontogenetic stage of the specimen is unknown.

Conclusion

The dentition of acrodontians has long been an area of interest in the context of dental development and implantation because this group is known to lack tooth replacement (monophyodonty), whereas intermittent to continuous replacement (polyphyodonty) is the primitive condition for toothed vertebrates, including most fish, amphibians, and amniotes. A lack of replacement has also been associated with a particular type of implantation (acrodonty), which has resulted in the lack of replacement becoming a formal characteristic of acrodont implantation. However, this study shows here that even some modern acrodont reptiles do not have acrodont implantation early in ontogeny, and that there is a distinct ontogenetic change in the morphology and implantation of dentition of Pogona vitticeps. The youngest teeth in juvenile specimens exhibit features of pleurodont implantation with a greater lingual contribution of tooth tissues and an attachment biased towards the labial side. These tissues are secondarily remodeled through a step-wise process of: resorption of dentine, deposition of bone, wear of the tooth surface, and finally wear of the jaw bone proper, effectively changing the morphology to the full acrodont pattern. These processes give the agamid Pogona vitticeps the appearance of acrodont dentition in adulthood.

This raises the question as to how we should code acrodont dentition in squamate phylogenies; is it true acrodonty if this implantation mode is only achieved through secondary remodeling of the teeth and dentary? Finally, another important consideration is that if all acrodontians share these ontogenetic changes and wear adaptations, then what is the significance of the convergence seen between acrodontian squamates and the rhynchocephalian Sphenodon, which is also reported to have acrodont dentition with undocumented wear adaptations?

23

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25

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26

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Richman, J. M., and G. R. Handrigan. 2011. Reptilian tooth development. Genesis 49:247–260.

Shellis, R. P., and B. K. B. Berkovitz. 1976. Observations on the dental anatomy of piranhas (Characidae) with special reference to tooth structure. Journal of Zoology 180:69–84.

Simões, T. R., E. Wilner, M. W. Caldwell, L. C. Weinschütz, and A. W. A. Kellner. 2015. A stem acrodontan lizard in the Cretaceous of Brazil revises early lizard evolution in Gondwana. Nature Communications 6:8149.

Smirina, E., and N. Ananjeva. 2017. On the longevity, growth and reproductive characteristics of Lichtenstein’s Toadhead Agama, Phrynocephalus interscapularis Lichtenstein, 1856 (Agamidae, Sauria). Amphibia-Reptilia 38:31–39.

Smirina, E. M., and N. B. Ananjeva. 2007. Growth layers in bones and acrodont teeth of the agamid lizard Laudakia stoliczkana (Blanford, 1875)(Agamidae, Sauria). Amphibia-Reptilia 28:193–204.

Spencer, M. A. 2005. Dental functional morphology: How teeth work. American Journal of Human Biology 17:384–385.

Throckmorton, G. S. 1979. The effect of wear on the cheek teeth and associated dental tissues of the lizard Uromastix aegyptius (Agamidae). Journal of Morphology 160:195–207.

Throckmorton, G. Y. S. 1976. Oral food processing in two herbivorous lizards, Iguana iguana (Iguanidae) and Uromastix aegyptius (Agarnidae). Journal of Morphology 148:363–390.

Westergaard, B., and M. W. J. Ferguson. 1990. Development of the dentition in Alligator mississippiensis: Upper jaw dental and craniofacial development in embryos, hatchlings, and young juveniles, with a comparison to lower jaw development. American Journal of Anatomy 187:393–421.

27

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Ananjeva, N., and E. Smirina. 2007. Growth layers in bones and acrodont teeth of the agamid lizard Laudakia stoliczkana (Blanford, 1875) (Agamidae, Sauria). Amphibia-Reptilia 28:193–204.

Berkovitz, B., and P. Shellis. 2017. Reptiles 1: Tuatara and Lizards; pp. 153–200 in The Teeth of Non-Mammalian Vertebrates.

Bramble, K., A. R. H. LeBlanc, D. O. Lamoureux, M. Wosik, and P. J. Currie. 2017. Histological evidence for a dynamic dental battery in hadrosaurid dinosaurs. Scientific Reports 7:15787.

Brown, C. M., C. S. Vanburen, D. W. Larson, K. S. Brink, N. E. Campione, M. J. Vavrek, and D. C. Evans. 2015. Tooth counts through growth in diapsid reptiles: Implications for interpreting individual and size-related variation in the fossil record. Journal of Anatomy 226:322–333.

Buchtová, M., O. Zahradníček, S. Balková, and A. S. Tucker. 2013. Odontogenesis in the Veiled Chameleon (Chamaeleo calyptratus). Archives of Oral Biology 58:118–133.

28

Budney, L. 2004. A survey of tooth attatchment histology in squamata: The evaluation of tooth attatchment classiciation and characters. University of Alerta pp.

Budney, L. A., M. W. Caldwell, and A. Albino. 2006. Tooth socket histology in the Cretaceous snake Dinilysia, with a review of amniote dental attachment tissues. Journal of Vertebrate Paleontology 26:138–145.

Caldwell, M. W. 2007. Ontogeny, anatomy and attachment of the dentition in mosasaurs (Mosasauridae: Squamata). Zoological Journal of the Linnean Society 149:687–700.

Cooper, J. S., and D. F. G. Poole. 1973. The dentition and dental tissues of the agamid lizard , Uromastyx The dentition. 85–100.

Cope, E. D. 1864. On the Characters of the Higher Groups of Reptilia Squamata: And Especially of the Diploglossa. Academy of Natural Sciences 16:224–231.

Dauphin, Y., and C. T. Williams. 2008. Chemical composition of enamel and dentine in modern reptile teeth. Mineral Mag 72:247–250.

Delgado, S., T. Davit-Beal, and J. Y. Sire. 2003a. Dentition and tooth replacement pattern in Chalcides (Squamata; Scincidae). Journal of Morphology 256:146–159.

Delgado, S., T. Davit-Beal, and J.-Y. Sire. 2003b. Dentition and tooth replacement pattern inChalcides (Squamata; Scincidae). Journal of Morphology 256:146–159.

Dosedělová, H., K. Štěpánková, T. Zikmund, H. Lesot, J. Kaiser, K. Novotný, J. Štembírek, Z. Knotek, O. Zahradníček, and M. Buchtová. 2016a. Age-related changes in the tooth–bone interface area of acrodont dentition in the chameleon. Journal of Anatomy 229:356–368.

Dosedělová, H., K. Štěpánková, T. Zikmund, H. Lesot, J. Kaiser, K. Novotný, J. Štembírek, Z. Knotek, O. Zahradníček, and M. Buchtová. 2016b. Age-related changes in the tooth-bone interface area of acrodont dentition in the chameleon. Journal of Anatomy 229:356–368.

Erickson, G. M. 1996. Incremental lines of von Ebner in dinosaurs and the assessment of tooth replacement rates using growth line counts. Proceedings of the National Academy of Sciences of the United States of America 93:14623–14627.

29

Estes, R., and C. Charles. 1988. Phylogenetic Relationships of the Lizard Families: Essays Commemorating Charles L. Camp, illustrate. (Gregory K. Pregill (ed.)). Stanford University Press, 631 pp.

García, R. A., and V. Zurriaguz. 2016. Histology of teeth and tooth attachment in titanosaurs (Dinosauria; Sauropoda). Cretaceous Research 57:248–256.

Huber, D. R., M. N. Dean, and A. P. Summers. 2008. Hard prey, soft jaws and the ontogeny of feeding mechanics in the spotted ratfish Hydrolagus colliei. Journal of The Royal Society Interface 5:941–953.

Hugall, A. F., R. Foster, M. Hutchinson, and M. S. Y. Lee. 2008. Phylogeny of Australasian agamid lizards based on nuclear and mitochondrial genes : implications for morphological evolution and biogeography. 343–358.

Järvinen, E., M. Tummers, and I. Thesleff. 2009. The role of the dental lamina in mammalian tooth replacement. Journal of Experimental Zoology Part B: Molecular and Developmental Evolution 312:281–291.

Jenkins, K. M., M. E. H. Jones, T. Zikmund, A. Boyde, and J. D. Daza. 2017. A Review of Tooth Implantation Among Rhynchocephalians (Lepidosauria). Journal of Herpetology 51:300–306.

Kieser, J. A., T. Tkatchenko, M. C. Dean, M. E. H. Jones, W. Duncan, and N. J. Nelson. 2009. Microstructure of dental hard tissues and bone in the Tuatara Dentary, Sphenodon punctatus (Diapsida: Lepidosauria: Rhynchocephalia). Frontiers of Oral Biology 13:80–85.

Kline, A. L. W., and D. Cullum. 2017. A Long Term Study of the Tooth Replacement Phenomenon in the Young Green Iguana , Iguana iguana. Society for the Study of Amphibians and Reptiles 18:176–185.

LeBlanc, A. R. H., and R. R. Reisz. 2013. Periodontal Ligament, Cementum, and Alveolar Bone in the Oldest Herbivorous Tetrapods, and Their Evolutionary Significance. PLoS ONE 8.

LeBlanc, A. R. H., and R. R. Reisz. 2015. Patterns of tooth development and replacement in captorhinid reptiles: a comparative approach for understanding the origin of multiple tooth

30

rows. Journal of Vertebrate Paleontology 4634:e919928.

LeBlanc, A. R. H., R. R. Reisz, K. S. Brink, and F. Abdala. 2016a. Mineralized periodontia in extinct relatives of mammals shed light on the evolutionary history of mineral homeostasis in periodontal tissue maintenance. Journal of Clinical Periodontology 43:323–332.

LeBlanc, A. R. H., R. R. Reisz, D. C. Evans, and A. M. Bailleul. 2016b. Ontogeny reveals function and evolution of the hadrosaurid dinosaur dental battery. BMC Evolutionary Biology 16:152.

Lumsden, A. G. S., and J. W. Osborn. 1977. The evolution of chewing: A dentist’s view of palaeontology. Journal of Dentistry 5:269–287.

Montanucci, R. 2008. Comparative Dentition in Four Iguanid Lizards. Herpetologica 24:305– 315.

Motani, R. 1997. Temporal and Spatial Distribution of Tooth Implantation in Icthyosaurs; pp. 81–103 in Ancient marine reptiles. San Diego : Academic Press, c1997.

Pyron, R., F. T. Burbrink, and J. J. Wiens. 2013. A phylogeny and revised classification of Squamata, including 4161 species of lizards and snakes. BMC Evolutionary Biology 13:93.

Richman, J. M., and G. R. Handrigan. 2011. Reptilian tooth development. Genesis 49:247–260.

Shellis, R. P., and B. K. B. Berkovitz. 1976. Observations on the dental anatomy of piranhas (Characidae) with special reference to tooth structure. Journal of Zoology 180:69–84.

Simões, T. R., E. Wilner, M. W. Caldwell, L. C. Weinschütz, and A. W. A. Kellner. 2015. A stem acrodontan lizard in the Cretaceous of Brazil revises early lizard evolution in Gondwana. Nature Communications 6:8149.

Smirina, E., and N. Ananjeva. 2017. On the longevity, growth and reproductive characteristics of Lichtenstein’s Toadhead Agama, Phrynocephalus interscapularis Lichtenstein, 1856 (Agamidae, Sauria). Amphibia-Reptilia 38:31–39.

Smirina, E. M., and N. B. Ananjeva. 2007. Growth layers in bones and acrodont teeth of the

31

agamid lizard Laudakia stoliczkana (Blanford, 1875)(Agamidae, Sauria). Amphibia-Reptilia 28:193–204.

Spencer, M. A. 2005. Dental functional morphology: How teeth work. American Journal of Human Biology 17:384–385.

Throckmorton, G. S. 1979. The effect of wear on the cheek teeth and associated dental tissues of the lizard Uromastix aegyptius (Agamidae). Journal of Morphology 160:195–207.

Throckmorton, G. Y. S. 1976. Oral food processing in two herbivorous lizards, Iguana iguana (Iguanidae) and Uromastix aegyptius (Agarnidae). Journal of Morphology 148:363–390.

Westergaard, B., and M. W. J. Ferguson. 1990. Development of the dentition in Alligator mississippiensis: Upper jaw dental and craniofacial development in embryos, hatchlings, and young juveniles, with a comparison to lower jaw development. American Journal of Anatomy 187:393–421.

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Chapter 2 Histology of the coronoid dentition with evidence of replacement in the Permian parareptile Delorhynchus

The co-authors of this paper are Mark MacDougall whom preformed the phylogenetic analysis and assisted with manuscript editing, and Robert Reisz who created the initial project and provided specimens for sectioning, as well as assisted in the direction of the study.

Citation: Haridy, Y., MacDougall, M.J. and Reisz, R.R., 2017. The lower jaw of the Early Permian parareptile Delorhynchus, first evidence of multiple denticulate coronoids in a reptile. Zoological Journal of the Linnean Society. Abstract

We describe the lower jaw of the parareptile Delorhynchus cifellii from the Early Permian of Oklahoma on the basis of a complete, isolated right ramus and histological thin sections. The lower jaw of Palaeozoic amniotes is generally less well known than other parts of the cranium, largely because they are often preserved in articulation with the skull and are partially obscured. Thus, complete information about the dentition and other features of the lower jaw are rarely available. The completeness of these specimens allows us to recognize, for the first time, the presence of two coronoid ossifications in a Palaeozoic reptile. In addition, both coronoids bear numerous small teeth, a feature that is commonly found in anamniotes but that is rare in amniotes. The distribution of these two features among amniotes reveals that they represent a reversal and a synapomorphy of the parareptile clade Lanthanosuchoidea that is possibly associated with specialized feeding behaviour among these small predators. In addition, Delorhynchus has a coronoid process that is anatomically distinct from those in other parareptiles, indicating multiple independent origins of this feature within Parareptilia. Furthermore, our increased knowledge of the mandible of Delorhynchus allows us to recognize that Bolterpeton carrolli, known from fragmentary jaw material, is a junior synonym of Delorhynchus.

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Introduction

The immense taxonomic diversity and exceptional preservation found at the Richards Spur locality, Oklahoma, have greatly increased our understanding of upland terrestrial vertebrate communities of the Early Permian. In addition to yielding one of the richest and most diverse faunal assemblages of the Palaeozoic, this locality has preserved many taxa that are currently considered to be endemic (MacDougall and Reisz, 2012). Although this endemism is likely related to the unprecedented taxonomic diversity found at this locality, the fossils from Richards Spur provide unique insights into the initial stages of amniote diversification. Here we provide a description of the lower jaw of the parareptile Delorhynchus, which not only shows critical information on early parareptilian anatomy but which also offers a basis for comparison with that of the coeval eureptile Captorhinus, which has the only other well-known, histologically characterized reptilian lower jaw of this period.

The Richards Spur locality has recently yielded many articulated and pristinely preserved specimens, allowing us to reevaluate the taxonomic identity and relationships of previously described fragments. These recent discoveries have shown that several parareptile species are present at this locality: Bolosaurus grandis Reisz et al., 2002, Feeserpeton oklahomensis (MacDougall and Reisz, 2012), Microleter mckinzieorum (Tsuji et al., 2010), Abyssomedon williamsi (MacDougall and Reisz, 2014), Colobomycter pholeter ((Modesto, 1999)), Colobomycter vaughni (MacDougall et al., 2016), Delorhynchus cifelli (Reisz et al., 2014), and Delorhynchus priscus (Reisz et al., 2014). Delorhynchus was previously known only through the fragmentary holotype of Delorhynchus priscus (KU 11117), which was initially described as pelycosaur material ((Fox, 1962) before being reassigned to Parareptilia (Modesto, 1999). The holotype of Delorhynchus cifellii (OMNH 73515) and other specimens of this species show features that are comparable with those of Bolterpeton carrolli, a taxon that was previously described on the basis of fragmentary remains and identified as a ‘microsaur.’ This is of particular interest, as the lower jaw of Delorhynchus, described here in detail, is indistinguishable from the holotype of Bolterpeton carrolli (Anderson and Reisz, 2003).

Herein we describe the anatomy and histology of the lower jaw and associated dentition of Delorhynchus in detail, which has only been previously done in Captorhinus (Heaton, 1979). This was facilitated through a series of coronal sections of the lower jaw, allowing us to

34 determine the exact contribution of each element to the morphology of the mandible. The preservation of this jaw has also allowed for the identification of two coronoid ossifications and their associated dentition, which were referred to previously as denticles (Anderson and Reisz, 2003). The coronoid and its associated dentition were also examined histologically, revealing that the coronoid dentition is indistinguishable from that of the marginal dentition on a microanatomical basis, therefore we refer to the coronoid dentition as true teeth rather than the problematic term denticles.

Institutional abbreviations—OMNH, Sam Noble Oklahoma Museum of Natural History, Norman, Oklahoma, USA; KU and KUMNH, University of Kansas, Museum of Natural History, Lawrence, Kansas, USA; ROM, Royal Ontario museum, Toronto, Ontario, Canada.

Materials and Methods

The illustrations found in Figures 1 and 2 were made using Adobe Photoshop CS6 to create outlines, and detailed shape was added to the illustrations using charcoal pencils and coquille paper. The diagrams for figures 3 and 4 were made using Adobe Illustrator CS6. To access normally inaccesible anatomy of the lower jaw and its dentition, a near complete right mandible was serially sectioned along a coronal plane, both thin and thick sections were made. The coronoid region was thin sectioned and used in figure 3, while the remaining thick sections were photographed and then outlined to make the schematic diagram found in figure 4. All specimens in this study have been photographed using a Canon EOS40D, prior to sectioning. All sectioning was done following the ROM histology protocol. Specimens were embedded in AP Castolite acrylic resin, vacuumed and left to cure for a minimum of 24 hours. All resin embedded specimens were cut using a Buhler Isomet 1000 wafer saw at a low speed of 275rpm. The specimens were then mounted on plexiglass slides using Scotch-Weld SF-100 cyanoacrylate. The slides were then mounted on the Hillquist and ground down using the grinding cup until optical clarity was achieved, subsequently the specimen was then ground by hand using progressively finer grit, beginning with a 600-grit silicon carbide powder and working down to a 1-micron aluminum oxide powder. All slides produced were imaged using Nikon DS-Fi1camera mounted to a Nikon AZ 100 microscope fitted with crossed-polarizing and lambda filters, and an

35 oblique illumination slider, image processing was done through NIS-Elements registered to R. R. Reisz of the University of Toronto Mississauga. The photographs in figures 6 and 7 were obtained using a Jeol Neoscope JCM-5000 scanning electron microscope (SEM).

The phylogenetic analysis was performed in PAUP 4.0a152 (Swofford, 2017) using the methodology of MacDougall and Reisz (2014). The data matrix used was the MacDougall et al. (2017) matrix.

Referred Specimens—ROM 76624, partial right mandibular ramus; OMNH 73363, complete right mandibular ramus; OMNH 52364, holotype of Bolterpeton carrolli, partial right mandibular ramus; OMNH 71111, Bolterpeton carrolli, partial right dentary; KU 11117, holotype of Delorhynchus priscus, a partial right maxilla.

Results

These isolated mandibles of Delorhynchus present a relatively rare opportunity to study in detail the anatomy of the lower jaw of a Palaeozoic amniote. The most common mode of preservation of early amniote jaws is either as fragmentary remains or in close association with skulls. In the latter case, the lower jaw tends to be tightly appressed against the palate, obscuring critical aspects of its anatomy, as is the case in other lanthanosuchoids, such as Feeserpeton oklahomensis (MacDougall and Reisz, 2012) and Acleistorhinus pteroticus (deBraga and Reisz, 1996). We are therefore fortunate in finding isolated, completely preserved mandibular rami, which allow us to study and to illustrate most aspects of their anatomy in detail. The mandible of the holotype of Delorhynchus cifelli (OMNH 73363) is indistinguishable from that of the specimens described here (OMNH 71111, OMNH 52364, and ROM 76624); OMNH 73363 was previously briefly mentioned and described by Reisz et al. (2014).

10.1.1 Mandible

The mandible of Delorhynchus is an elongate structure subdivided into three distinct regions: a slender anterior tooth bearing region, a tall coronoid region immediately posterior to the tooth row, and a broad posterior region that includes the articular cotyles for the jaw articulation. The

36 mandible is most robust in the region of the articular bone, which forms not only the articular surfaces with the skull, but which also maintains well-developed medial and posterior processes. As noted in Reisz et al. (2014), the mandible is characterized by the presence of a well- developed coronoid process; however, what is more striking is the occurrence of two denticulate coronoid ossifications which can be observed on the medial surface (Fig. 1).

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FIGURE 1. Delorhynchus mandible, OMNH 72363. A, photograph of lingual view; B, photograph of labial view; C, illustration of lingual view; D, illustration of labial view. Abbreviations: an, angular; ar, articular; cr1, anterior coronoid; cr2; posterior coronoid; d, dentary; f int or, foramen intermandibularis oralis; f int ca, foramen intermandibularis caudalis; pr, prearticular; sp, splenial; sur, surangular. Scale bar = 1 cm. Illustrations by Steven Leduc.

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The dentary is a long element, forming most of the lateral surface of the mandible in the region of the tooth row, and extends from the mandibular symphysis to slightly beyond the coronoid process. The lateral surface of the dentary lacks the type of ornamentation found on the skull roof of Delorhynchus, but the anteriormost portion of the bone exhibits a series of mental foramina. This pattern of clustered anterolateral foramina near the symphysis is present in all Richards Spur lanthanosuchoids and is prominent in all Delorhynchus cifellii specimens (Reisz et al., 2014). Ventrally, most of the dentary is overlain by the splenial, forming a linear suture best observed in lateral and ventral views (Figs. 1D, 2C). Posterodorsally, the dentary overlies the surangular bone; a slender process of the dentary extends between the lateral exposure of that bone and the coronoid process. The dentary contacts the angular posteroventrally, forming a highly interdigitated suture that continues dorsally to form a similar suture with the surangular. Lingually, the dentary forms the lateral wall of the Meckelian fossa and contacts the dorsal edge of the medial portion of the splenial and the anterior coronoid.

The splenial is a large, smooth superficial element that forms much of the lingual and ventral surfaces of the lower jaw, spanning more than half the length of the mandible (Fig. 2). Only a small portion of the splenial, directly under the dentary and angular bones, is visible in labial view. The splenial contributes to the anterior margin of the large intermandibular caudalis foramen, as is the case in other parareptiles, such as Macroleter poezicus (Tsuji, 2006). The foramen intermandibularis oralis, as described in the eureptile Captorhinus laticeps (Heaton, 1979), is not present. Instead, there is a large uncovered region of the Meckelian canal, as the splenial does not continue anteriorly to contact the mandibular symphysis, and therefore does not create a foramen proper, as in C. laticeps (Heaton, 1979). Most parareptiles have a mandibular symphysis that is formed entirely by the dentary bone, and a similar pattern where the most anterior part of the dentary is uncovered by the splenial is also observed in the procolophonid Scoloparia glyphanodon (Sues and Baird, 1998). Anteriorly, the splenial has two tongue-like processes that attach to the dorsal and ventral edges of the dentary

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FIGURE 2. Delorhynchus mandible, OMNH 72363. A, photograph of ventral view; B, photograph of dorsal view; C, illustration of ventral view; D, illustration of dorsal view. Abbreviations: an, angular; ar, articular; cr1, anterior coronoid; cr2; posterior coronoid; d,

40 dentary; pr, prearticular; sp, splenial; sur, surangular. Scale bar = 1 cm. Illustrations by Steven Leduc.

The angular is a large, dorsally curved element that forms the posterior portion of the labial and ventral surfaces of the mandible. This element is bordered anteroventrally by the splenial, anterodorsally by the dentary, dorsally by the surangular, and extends posteriorly to meet the articular. In lingual view, the angular extends dorsally from the ventral ridge to form much of the medial wall and floor of the adductor fossa, and underlies the splenial anteriorly, forming an elongate anteriorly slanted suture. Dorsally, the angular contacts the prearticular bone and, together with the splenial and the prearticular, contributes to the large intermandibular caudalis foramen. Thin sections have allowed us to determine that a process of the angular underlies the splenial anteriorly (Fig. 3B); this internal anterior process of the bone extends to the level of the suture between the two coronoids. The angular bone extends even farther anteriorly as a relatively thin sheet of bone that appears to brace the internal surfaces of the dentary and splenial, at least to the level of the 12th tooth position. Comparison with Captorhinus indicates that the anterior, internally located process of the angular is much shorter in the eureptile (Heaton, 1979) than in Delorhynchus, and it does not appear to extend anteriorly beyond the level of the foramen intermandibularis caudalis. The angular shows the presence of a distinct pattern of rugosities posteroventrally that can be best viewed labially (Figs. 1D, 2C). The rugosity on the labial surface of the mandible likely represents dermal sculpturing, although it differs from the pattern of round pits found on the skull roof or the tuberosities present along the edges of the orbit (Reisz et al., 2014). It is unlikely that this pattern of rugosities is related to muscle attachments, such as the pterygoideus muscles, because a sharp ventral ridge separates the labial and lingual surfaces of the bone (Fig. 2C). This ventral ridge has an un-even edge, and slight rugosities are present on either side. It is possible that this ventral ridge may have been the origination for muscles that extended posteriorly, possibly to the hyoid apparatus (equivalent to mandibulohyoideus mm. in squamates).

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FIGURE 3. Interior view of Delorhynchus mandible, ROM 76624. A, anterior portion of the mandible; B, anterior portion of the first coronoid; C, posterior portion of the first coronoid; D, anterior portion of the second coronoid; E, maximum height of the coronoid process; F, posterior adductor foramen. Abbreviations: add for, adductor foramen; an, angular; ar, articular; cr1, anterior coronoid; cr2; posterior coronoid; d, dentary; f int or, foramen

42 intermandibularis oralis; f int ca, foramen intermandibularis caudalis; pr, prearticular; sp, splenial; sur, surangular. Scale bar = 1 cm.

The surangular is a complex element that contributes to several features of the lower jaw. Anterodorsally, the surangular contributes to the prominent coronoid process, forming a rugose eminence that meets the coronoid bone to form the labial component of the coronoid process proper. Extending posteriorly from this eminence, the dorsal edge of the surangular has a wide, flattened surface that forms a shelf, as in numerous other parareptiles (Reisz and Scott, 2002; Tsuji et al., 2010). This is in strong contrast to the plesiomorphic condition present in eureptiles and synapsids where the dorsal edge of the surangular is rounded (Heaton, 1979; Reisz and Berman, 1986). The presence of this enlarged dorsal shelf is likely related to the modified pattern of adductor muscle attachment that may have evolved in parareptiles (Reisz and Scott, 2002). Posteriorly, the surangular is broadened labiolingually, and abuts against the body of the articular bone; a thin posteriorly oriented sheet of bone extends from the main body of surangular and wraps around the articular bone. The posterior sheet of bone of the surangular covers much of the articular cotyle in labial view. Lastly, the surangular, along with the angular form the internal wall of the adductor fossa, which can be observed lingually (Figs. 1, 2). Thin sections of the mandible indicate that the surangular has a long internal anterior process, one that underlies the dentary bone, well anterior to the coronoid process, almost to the level of the anterior edge of the posterior coronoid bone (Fig. 3D), which is in contrast to the condition that is observed in the eureptile Captorhinus.

The prearticular is another complex element of the lower jaw; it is exposed in lingual, ventral, and dorsal views. It is a relatively slender, elongate bone that is wedged anteriorly between the splenial and the posterior coronoid, and reaches far anteriorly beneath the splenial as a thin sliver of bone, extending to the midpoint of the anterior coronoid (Fig. 3C). Ventrally, it borders the splenial, the large intermandibularis foramen caudalis, and the angular and underlies the articular posteriorly. The dorsal edge of the prearticular forms the lingual margin of the adductor fossa. Furthermore, along this dorsal edge there is a sharp ridge that runs the length of the element, moving posteriorly this ridge twists ventrally and forms a lingually slanted shelf.

The articular is a large bodied and robust element that is composed of two cotyles and a retroarticular process that makes up the posterior portion of the mandible. Labially, the articular

43 contacts the angular and surangular, whereas it contacts the prearticular lingually. The mandibular fossa of the articular is large and located dorsally, and is characterized by the porous unfinished bone that would have likely been capped with cartilage to aid in articulation with the condyle of the quadrate. The articular surface of the fossa is surrounded by rugose areas of thicker bone that give the bone its robustness, and includes a particularly rugose medioventrally projecting pterygoideus process. The retroarticular process projects posteriorly beneath the main body of the articular, and its rounded circumference is marked by rugosities that were probably areas of origin for jaw opening musculature (depressor mandibularis).

10.1.2 Coronoids

Perhaps the most interesting aspect of the mandible of Delorhynchus is the distinctive coronoid complex. It is composed of two separate bones, a simple, sheet-like anterior coronoid bone, and a more complex posterior coronoid. Both coronoid elements bear numerous small teeth, all of which are on elevated pads of bone that are distinct from the coronoid element itself. Histological thin sections of this region have shown that the dentigerous pads are composed of several generations of alveolar bone similar to that observed in (LeBlanc and Reisz, 2013), this is best illustrated in figure 4. These pads are more distinct and occupy less of the total coronoid area in the smaller and presumably younger specimen (ROM 76624), whereas in the larger specimen (OMNH 72363), the pads occupy the majority of the surface area of the individual coronoid elements. The larger mandibular ramus (OMNH 72363) has dentigerous pads essentially forming a continuous field of teeth on the dorsolingual surface of the lower jaw, which extends over most of the anterior coronoid and covers the anterior half of the posterior coronoid.

The posterior coronoid differs from the anterior coronoid in having an edentulous posterior region that meets dorsally with the surangular; together they form the coronoid process. The coronoid process is rather rugose in appearance with a number of tuberosities on the lingual surface. This is complimented by the rugose surface of the underlying surangular, together making up a robust muscle attachment site at the apex of the coronoid process. This is in contrast to some other parareptiles like Belebey vegrandis where the coronoid process has a tripartite composition of dentary, coronoid, and surangular (Reisz et al., 2007) or to the condition in Owenetta, where it is composed of the dentary alone (Reisz and Scott, 2002).

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10.1.3 Dentition

10.1.3.1 Marginal

The morphology of the marginal dentition associated with the mandibular ramus described by Reisz et al. (2014) is indistinguishable to the maxillary dentition of Delorhynchus priscus, Delorhynchus cifellii, and Bolterpeton carrolli. The general morphology of the mandibular dentition can be described as moderately recurved and distinctly monocuspid with an uneven apex that leads to a cutting blade running labiolingually down the body of the tooth. Delorhynchus marginal dentition also consistently shows fluting crownward, which is a feature that is also found among eureptiles (Reisz et al., 2015), other parareptiles (Modesto, 1999), and anamniotes (Fröbisch and Reisz, 2012), indicating that this feature is likely primitive for tetrapods. In the specimens attributed to Delorhynchus, the teeth have a characteristic, slightly recurved outline, and rootwards, there are external plications, which are formed by the infolding of dentine (MacDougall et al., 2014). The shape and the presence of plicidentine near the root of the teeth are a feature found not only within the genus Delorhynchus, but also other closely related parareptiles, such as Colobomycter, Feeserpeton, and Microleter (MacDougall et al., 2014).

10.1.3.2 Coronoid

Interestingly, all lanthanosuchoid taxa that have exposed coronoids exhibit dentition on these elements. Re-examination of computed tomography (CT) scans of the holotype and only know specimen of Feeserpeton oklahomensis (MacDougall and Reisz, 2012) revealed the presence of coronoid teeth; their disposition and the size of the dental pads could only be determined by CT scans because that part of the mandible was not visible externally. Coronoid teeth have also been found to be present in Colobomycter pholeter (MacDougall et al., 2017).

It should be noted that the coronoid dentition mirrors that of the marginal teeth in external and internal morphology. Externally there is a color variation on the crown portion of the coronoid dentition, this is also found in the marginal dentition, and likely indicates the portion of the crown that is covered by enamel. Additionally, there is the same fluting of the enamel on the coronoid teeth as there is in the marginal dentition. Internally we see other

45 similarities between coronoid and marginal dentition, for instance the amount of enamel, dentine and alveolar bone are proportionately the same between the coronoid and marginal dentition.

There seems to be a larger disparity in the size range of the individual teeth on the dentulous pads, with the more labial dentition being larger. This is more evident on the larger specimen (OMNH 72363) than on the smaller ramus (ROM 76624). The size of these dental pads and therefore the number and size of coronoid teeth appears to vary between individual specimens of Delorhynchus, and this variation may be related to ontogeny with the larger specimens having larger coronoids, hence more teeth.

10.1.4 Histology

The mandibular ramus ROM 76624 was serially sectioned to better understand the internal morphology of the element; particular interest was paid to the coronoids and their associated dentition. Two thin sections were made of (ROM 76624); these thin sections were located in the center of the anterior and posterior coronoid respectively. The thin sections allowed for histological analysis of the marginal and coronoid dentition, as well as of the underlying bone.

The marginal dentition is implanted in a pleuroacrodont fashion with a bias towards acrodonty; we assign the term pleuroacrodonty to this specimen due to the unequal geometry of the dentary underlying the marginal dentition. It should also be noted that although there is a bias towards a higher labial wall, the labial wall is mostly composed of alveolar bone rather than true jawbone. The marginal dentition of Delorhynchus has been previously sectioned and interpreted (MacDougall et al., 2014), for this reason the histological description of the marginal dentition will remain brief as the focus of this study is the coronoid dentition.

The coronoid dentition is similar in attachment to that of marginal dentition of multiple rowed captorhinids (LeBlanc and Reisz, 2015), where alveolar bone ankylosis the dentition to the underlying bone; furthermore there seems to be secondary attachment via alveolar bone to the neighbouring teeth as well as resorption of the neighbouring teeth (Fig. 4).

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FIGURE 4. Histology of coronoid dentition in Delorhynchus, ROM 76624. A, Lingual view of Delorhynchus mandible, ROM 76624 with thin cut section indicated; B, thin section showing both the marginal and coronoid dentition; C, a close up of the coronoid dentition; D, a close up of the coronoid dentition under cross polarized light. Scale bar equals 500 μm.

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The enamel found on the coronoid dentition is uneven favoring the lingual side; this is likely due to wear or taphonomic damage. The enamel covered crown makes up about one third of the total height of the tooth. The dentine underlying the enamel is characterized by radiating dentine tubules that terminate at the pulp cavity. In the dentine, lines of von Ebner can be observed; these are much more prominent towards the crown, they are unevenly spaced, eventually becoming indistinct towards the root portion of the tooth. Rootwards, there does not seem to be any plicidentine infolding, which is clearly visible in the marginal dentition; this is likely a character of scale, supporting the idea that smaller dentition may need less infolding to properly attach to the underlying tissues (MacDougall et al., 2014). The dentition is attached to the coronoid by a fibrous mineralized tissue that contains trabeculae that we here identify as alveolar bone (LeBlanc and Reisz, 2013, 2015). This attachment tissue is present at the base of the dentition as well as between where the teeth come in contact with one another. The alveolar bone is parallel-fibered in appearance under cross-polarized light, which is distinguishable from the lamellar bone making up the coronoid and the dentary. There are also two reversal lines separating the alveolar bone and the underlying layers, the layers are composed of alveolar bone super imposed on one another, this is likely a remnant of tooth replacement at this location. The reversal lines not only show separation between the various generations of alveolar bone, but also mark the boundary between the fibrous alveolar bone and the underlying lamellar coronoid bone (Fig. 4).

In thin section the coronoid is made up of lamellar bone that is highly organized with few vascular spaces. There are incremental growth lines that are evenly distributed along the coronoid, indicating even growth and slow bone deposition through ontogeny. Unlike the captorhinid condition in which fast growing jaw bone is highly vascularized and continuously remodeled (LeBlanc and Reisz, 2015), here the coronoid and dentary bone are made of evenly deposited lamellar bone, where the only resorption and remodeling are done at the dentulous surfaces (Fig. 4).

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Discussion

11.1 Multiple coronoids and coronoid dentition among Palaeozoic reptiles

Multiple coronoids have been used often as a character in analyses of microsaurs (Carroll and Currie, 1975; Anderson and Reisz, 2003) and other anamniotes (Gregory, 1948; Carroll and Currie, 1975), and the presence of two coronoids have been reported in synapsid amniotes such as Haptodus garnettensis (Laurin, 1993). However, the presence of multiple coronoids in Reptilia has not been previously noted. A single coronoid element is present in many well- known eureptiles: the captorhinids Captorhinus aguti (Fox and Bowman, 1966; Heaton, 1979), Captorhinus laticeps (Heaton and Reisz, 1980), and Labidosaurus hamatus (Modesto et al., 2007); the basal captorhinomorphs Paleothyris acadiana (Carroll, 1969) and Protorothyris (Clark and Carroll, 1973); the basal diapsids Petrolacosaurus (Reisz, 1977) and Araeoscelis (Reisz et al., 1984; Reisz, 2017). It was therefore assumed that Reptilia lost the anterior coronoid, or that the two elements fused. This latter hypothesis was supported by the presence of an elongate anterior process of the coronoid in captorhinids (Heaton, 1979). The presence of a single coronoid in Late Permian pareiasaurs (Tsuji, 2013) and Early Triassic owenettids (Modesto et al., 2003) suggests that reduction in the number of coronoid ossifications occurred independently in parareptiles (Fig. 5). Although we seem to have evidence of multiple cases of loss of the anterior coronoid as a separate ossification in all amniote lineages (Synapsida, Eureptilia, and Parareptilia), the absence of information about the condition of the coronoids in such critical reptiles as Hylonomus (Carroll, 1964), Cephalerpeton (Gregory, 1948; Carroll and Baird, 1972), and Macroleter (Tsuji, 2006), makes a comprehensive evaluation of this evolutionary event difficult. Nevertheless, when the presence of one or two coronoids is mapped onto a cladogram of Palaeozoic amniotes (Fig. 5), the overall pattern supports the hypothesis that the presence of a single coronoid is a synapomorphy of Reptilia. Thus, the fusion of the coronoids into a single element, or the loss of the anterior coronoid, appears to have occurred at the base of Reptilia. The occurrence of two coronoids in the lanthanosuchoids Feeserpeton and Delorhynchus appears to represent a reversal to the primitive tetrapod condition, or an independent acquisition of this condition. The association between the presence of two coronoids

49 and the presence of coronoid dentition may suggest that these two character states are linked in lanthanosuchoids.

FIGURE 5: Strict consensus tree obtained from the 6 optimal trees produced by the phylogenetic analysis. Solid blue squares indicate the presence of coronoid dentition, whereas

50 empty blue squares indicate the absence of coronoid dentition. Solid red squares indicate the presence of two coronoids, whereas empty blue squares indicate the presence of a single coronoid. Nodes of clades of interest are labeled: A, Amniota; B, Reptilia; C, Eureptilia; D, Parareptilia; E, Lanthanosuchoidea.

Coronoid dentition is rare among amniotes (Laurin, 1993), but has been found to be widely distributed among anamniotes (Carroll and Currie, 1975; Fröbisch and Reisz, 2012), furthermore it is often referred to as denticles in literature. Here we show that this character now extends into reptiles, and that coronoid denticles are in fact true teeth. The two-coronoid elements in Delorhynchus exhibit a large number of teeth, a feature that appears to characterize lanthanosuchoids. Two coronoids and coronoid dentition is occasionally present in other amniotes, like the synapsid Haptodus garnettensis (Laurin, 1993). The presence of two coronoids with dentition in Delorhynchus and Feeserpeton, as well as at least one dentulous coronoid in Colobomycter (MacDougall et al., 2017), is in strong contrast to the condition observed in other parareptiles. This can be most parsimoniously interpreted as support for the hypothesis that the primitive condition for this clade is the presence of a single, edentulous coronoid. Mesosaurs, millerettids, and bolosaurids have only one edentulous coronoid, as do Microleter, Nyctiphruretus, procolophonids, and pareiasaurs (Fig. 5).

As previously noted, the coronoid dentition mirrors that of the marginal dentition in external and internal morphology; therefore, it is reasonable to assume that the replacement mode for these teeth would follow that of the pleurodont marginal dentition. This, however, would be difficult to prove without further histological sampling; the material examined for this study shows that it is likely that multiple generations of teeth occupied the coronoids on the basis of several generations of alveolar bone being present, and super imposed (Fig. 4). Each layer of alveolar bone demarcates a tooth attachment site, and prominent reversal lines show that these layers were deposited sequentially with minimal resorption between generations. External evidence of replacement is visible in the larger specimen (OMNH 72363); there are several empty sockets that show no outward damage due to attritional processes. Furthermore, a small compete enamel cap is present in the matrix on the posterior coronoid amongst ankylosed dentition (Fig. 7). This enamel cap (Fig. 7) is positioned in an area that largely lacks dentition, and there seems to be a depression in neighbouring tooth as well as the surrounding bone, suggesting resorption of the adjacent tooth as well as the surrounding bone prior to deposition of

51 new alveolar bone and subsequent ankylosis of this new tooth, making it reasonable to deduce that this is a replacement tooth that would have been in soft tissue. As previously noted the coronoid teeth vary in size which cannot be attributed to replacement rate, with the largest of them being positioned labial to the smallest, this is best observed in (OMNH 72363), this heterodonty likely becomes more pronounced through ontogeny as it is harder to visualize in the smaller specimen (ROM 76624).

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FIGURE 6: Replacement in coronoid dentition of Delorhynchus. A, photograph of the denticulate region of the coronoid of Delorhynchus OMNH 72363; B, scanning electron microscope (SEM) photograph of replacement tooth in matrix and surrounding reabsorption.

New evidence regarding the internal anatomy of the mandible in Delorhynchus indicates not only that the dentary and angular are surprisingly robust when viewed in transverse section, but also that the superficial elements are extensively reinforced through the anterior extension of

53 the angular, surangular and prearticular bones (Fig. 3). This is a particularly interesting phenomenon because the anterior extension of these bones provides additional internal reinforcement of the region where the tooth covered coronoids are found. This raises the possibility that these anatomical features are related to the presence of coronoid dentition in that have unusually large number of palatal teeth, likely related to their lifestyle. This is in contrast to the condition observed in coeval captorhinid eureptiles, where there is no coronoid dentition, palatal dentition is reduced, and the marginal chewing surface is expanded via multiple rows of teeth or large bulbous dentition (LeBlanc and Reisz, 2015; LeBlanc et al., 2015; Reisz et al., 2015). Furthermore, in captorhinids the angular, surangular, and prearticular are not anteriorly extended as in Delorhynchus, likely because further reinforcement to the interior of the mandible is not necessary for captorhinids. Future work will allow us to expand these types of comparisons, by including parareptiles and other eureptiles that lack coronoid dentition.

11.2 Taxonomic status of Bolterpeton carrolli

Anderson and Reisz (2003) erected the taxon Bolterpeton carrolli on the basis of a few morphological features of a fragmentary lower jaw (OMNH 71111), but mainly on the presence of the two coronoids, as well as some apparently unique features of its dentition. Since the discovery of the fragmentary jaw of Bolterpeton, many new parareptiles from Richards Spur, as well as more complete specimens of previously known taxa, have been described (Modesto, 1999; Tsuji et al., 2010; MacDougall and Reisz, 2012; Reisz et al., 2014; MacDougall et al., 2017). Many of these taxa share dental and mandibular features that were assumed to only belong to anamniotes like Cardiocephalus and Euryodus (Anderson and Reisz, 2003). For instance, the delicate fluting on the enamel that is present on the lingual side of the crown is commonly found in parareptiles, including Colobomycter, Microleter, and Delorhynchus (Fig. 6). Similarly, the anterior and posterior cutting edges or ridges, misinterpreted as ‘weakly bicuspid’ (Anderson and Reisz 2003, pg. 503, fig. 3) because they lack a sulcus that would separate the lingual and labial cusps, this term was originally used by (Bolt, 1977) to describe the amphibamids Doleserpeton and Tersomius, are also clearly present in Delorhynchus (Fig. 6).

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FIGURE 7. Scanning electron microscope dentition comparison between the holotype of Bolterpeton carrolli, OMNH 71111, and Delorhynchus mandible, OMNH 72363. A, scanning electron microscope (SEM) photograph of the Bolterpeton carrolli holotype showing coronoids and marginal dentition; B, SEM photograph of the Delorhynchus mandible showing coronoids and marginal dentition; C, close up SEM photograph of the marginal and coronoid dentition of Bolterpeton; D, close up SEM photograph of the marginal and coronoid dentition of Delorhynchus.

However, upon reexamination of the holotype of Bolterpeton, the original observation of ‘weakly bicuspid’ morphology can be attributed to uneven wear of the teeth on the lingual side. In fact, the tooth morphology of Bolterpeton carrolli is indistinguishable from that observed in Delorhynchus cifellii (OMNH 73363). Finally, the presence of two coronoids that are covered

55 with dentition is clearly present in both the holotype of Bolterpeton carrolli and Delorhynchus cifellii. The anatomy of the preserved portion of the posterior coronoid, with its anterior region being covered by teeth, and the posterior edentulous portion, where the base of the coronoid process is preserved, is also identical to that in Delorhynchus cifellii. Therefore, we have no hesitation in declaring that Bolterpeton is a junior synonym of Delorhynchus.

Conclusions

The Dolese Brothers Limestone Quarry, near Richards Spur continues to provide a wealth of information on the anatomy and evolution of Early Permian terrestrial vertebrates, notably parareptiles. New material of the parareptile Delorhynchus reveals the presence of multiple coronoids on the mandibular ramus, as well as dentition on these coronoids. The multiple coronoids in Delorhynchus have led to a more detailed look at the coronoids of lanthanosuchoids; although there are some critical species on which we have no coronoid data, there is still compelling evidence that lanthanosuchoids either independently acquired denticulate multiple coronoids, or that they show a reversal to the condition found in anamniotes.

This study has also shown how the reinforced internal anatomy of the jaw of Delorhynchus is likely linked to the dentition found on the coronoids, and the purpose of this re- enforcement is to cope with the physiological stresses put on the element during feeding. The discovery of the multiple coronoids and associated dentition has furthered our understanding of the evolution of morphology of the parareptilian jaw and their adaptations to hypercarnivory. The histological data presented has shown unambiguous parallels between the coronoid and marginal dentition in that they are histologically identical when it comes to the tissues that form these structures, and by that logic, we promote the term ‘teeth’ rather than ‘denticles’ for the coronoid dentition. Lastly, through the analysis of the lower jaw of Delorhynchus, all of the anatomical features that were initially assigned to Bolterpeton carrolli can now be attributed to the genus Delorhynchus, effectively making Bolterpeton a junior synonym of Delorhynchus.

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Fröbisch, N. B., and R. R. Reisz. 2012. A new species of dissorophid (Cacops woehri) from the Lower Permian Dolese Quarry, near Richards Spur, Oklahoma. Journal of Vertebrate Paleontology 32:35–44.

Gregory, J. T. 1948. The structure of Cephalerpeton and affinities of the Microsauria. American Journal of Science 246:550–568.

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Laurin, M. 1993. Anatomy and relationships of Haptodus garnettensis, a Pennsylvanian synapsid from Kansas. Journal of Vertebrate Paleontology 13:200–229.

LeBlanc, A. R. H., and R. R. Reisz. 2013. Periodontal ligament, cementum, and alveolar bone in the oldest herbivorous tetrapods, and their evolutionary significance. PLoS ONE 8.

LeBlanc, A. R. H., and R. R. Reisz. 2015. Patterns of tooth development and replacement in captorhinid reptiles: a comparative approach for understanding the origin of multiple tooth rows. Journal of Vertebrate Paleontology 4634:e919928.

LeBlanc, A. R. H., A. K. Brar, W. J. May, and R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the Early Permian fissure fills of the Bally Mountain locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35.

MacDougall, M., and R. Reisz. 2012. A new parareptile (parareptila Lanthanosuchoidia) From the Early Permian. Journal of Vertebrate Paleontology 32:1018–1026.

MacDougall, M. J., and R. R. Reisz. 2014. The first record of a nyctiphruretid parareptile from the Early Permian of North America, with a discussion of parareptilian temporal fenestration. Zoological Journal of the Linnean Society 172:616–630.

MacDougall, M. J., A. R. H. LeBlanc, and R. R. Reisz. 2014. Plicidentine in the Early Permian parareptile Colobomycter pholeter, and its phylogenetic and functional significance among coeval members of the clade. PLoS ONE 9.

MacDougall, M. J., S. P. Modesto, D. Scott, and R. R. Reisz. 2017. New material of the reptile Colobomycter pholeter (Lanthanosuchoidiea; Parareptilia) and the diversity of the reptilies of the Early Permian (Cisularian). Zoological Journal of the Linnean Society.

Modesto, S. P. 1999. Colobomycter pholeter from the Lower Permian of Oklahoma: a parareptile, not a protorothyridid. Journal of Vertebrate Paleontology 19:466–472.

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Modesto, S. P., R. J. Damiani, J. Neveling, and A. M. Yates. 2003. A new Triassic owenettid parareptile and the Mother of Mass Extinctions. Journal of Vertebrate Paleontology 23:715–719.

Modesto, S. P., D. M. Scott, D. S. Berman, J. Müeller, and R. R. Reisz. 2007. The skull and the palaeoecological significance of Labidosaurus hamatus, a captorhinid reptile from the Lower Permian of Texas. Zoological Journal of the Linnean Society 149:237–262.

Reisz, R. R. 2017. Petrolacosaurus , the Oldest Known Diapsid Reptile. Science 196:1091–1093.

Reisz, R. R., and D. S. Berman. 1986. Lanthasaurus hardestii m. sp. , a primitive edaphosaur (Reptilia, Pelycosauria) from the Upper Pennsylvanian Rock Lake Shale near Garnett, Kansas. Can.J.Earth Sci. 23:77–91.

Reisz, R. R., and D. Scott. 2002. Owenetta kitchingorum , sp. nov., a small parareptile (Procolophonia: Owenettidae) from the Lower Triassic of South Africa. Journal of Vertebrate Paleontology 22:244–256.

Reisz, R. R., D. S. Berman, and D. Scott. 1984. The anatomy and relationships of the Lower Permian reptile Araeoscelis. Journal of Vertebrate Paleontology 4634:57–67.

Reisz, R. R., M. J. MacDougall, and S. P. Modesto. 2014. A new species of the parareptile genus Delorhynchus, based on articulated skeletal remains from Richards Spur, Lower Permian of Oklahoma. Journal of Vertebrate Paleontology 34:1033–1043.

Reisz, R. R., J. Müller, L. Tsuji, and D. Scott. 2007. The cranial osteology of Belebey vegrandis (Parareptilia: Bolosauridae), from the Middle Permian of Russia, and its bearing on reptilian evolution. Zoological Journal of the Linnean Society 151:191–214.

Reisz, R. R., A. R. H. LeBlanc, C. A. Sidor, D. Scott, and W. May. 2015. A new captorhinid reptile from the Lower Permian of Oklahoma showing remarkable dental and mandibular convergence with microsaurian tetrapods. Naturwissenschaften 102:50.

Suesi, H.-D., and D. Baird. 1998. Procolophonidae (Reptilia: Parareptilia) From the Upper Triassic Wolfville Formation of Nova Scotia, Canada. Journal of Vertebrate Paleontology 18:525–532.

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Tsuji, L. A. 2006. Cranial anatomy and phylogenetic affinities of the Permian parareptile Macroleter poezicus. Journal of Vertebrate Paleontology 26:849–865.

Tsuji, L. A. 2013. Anatomy, cranial ontogeny and phylogenetic relationships of the pareiasaur Deltavjatia rossicus from the Late Permian of central Russia. Earth and Environmental Science Transactions of the Royal Society of Edinburgh 104:81–122.

Tsuji, L. A., J. Müller, and R. R. Reisz. 2010. Microleter mckinzieorum gen. et sp. nov. from the Lower Permian of Oklahoma: the basalmost parareptile from Laurasia. Journal of Systematic Palaeontology 8:245–255.

Chapter 3 Opisthodontosaurus as a model for acrodont tooth replacement and dental ontogeny

The co-authors of this paper are Aaron LeBlanc, and Robert Reisz who together created the initial project and provided specimens for sectioning. Aaron Leblanc assisted in the drafts of the manuscript as well as the general direction of the study.

Citation: Haridy, Y., LeBlanc, A.R. and Reisz, R.R., 2017. The Permian reptile Opisthodontosaurus carrolli: a model for acrodont tooth replacement and dental ontogeny. Journal of anatomy.

Abstract

Continuous tooth replacement is common for tetrapods, but some groups of acrodont lepidosaurs have lost the ability to replace their dentition (monophyodonty). Acrodonty, where the tooth attaches to the apex of the jawbone, is an unusual form of tooth attachment that has been associated with the highly autapomorphic condition of monophyodonty. Beyond Lepidosauria, very little is known about the relationship between acrodonty and monophyodonty in other amniotes. We test for this association with a detailed study of the dentition of Opisthodontosaurus, an unusual Early Permian captorhinid eureptile with acrodont dentition. We provide clear evidence, both histological and morphological, that there were regular tooth replacement events in the lower jaw of Opisthodontosaurus, similar to its captorhinid relatives. Thus, our study of the oldest known amniote with an acrodont dentition shows that acrodonty does not inhibit tooth replacement, and that many of the characteristics assigned to lepidosaurian acrodonty are actually highly derived features of lepidosaurs that have resulted secondarily from a lack of tooth replacement. In the context of reptilian dental evolution, we propose the retention of the simple definition of acrodonty, which only pertains to the relative position of the tooth at the apex of the jaw, where the jaw possesses equal lingual and labial walls. This definition of implantation therefore focuses solely on the spatial relationship between the tooth and the jawbone and separates this relationship from tooth development and replacement.

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Introduction

Tooth implantation has been frequently used as a diagnostic feature and phylogenetic character in analyses of major squamate and other amniote groups (e.g., Zaher & Rieppel, 1999). Cope (1864) first used tooth implantation to divide modern Squamata into two distinct groups, Pleurodonta and Acrodonta. Tooth implantation should not be confused with tooth attachment; the former refers to the placement of the tooth in relation to the tooth-bearing element, whereas the latter refers to the nature of the attachment tissues that unite the tooth with the bone. However, categories of tooth implantation (acrodonty, pleurodonty, thecodonty) have often been incorrectly linked with tooth attachment (LeBlanc et al., in press), so much so that the presence or absence of certain tooth attachment tissues has become one of the defining features of certain implantation categories (Zaher & Rieppel, 1999). Additionally, the categories of ‘thecodont,’ ‘pleurodont,’ and ‘acrodont’ persist throughout the literature although they are problematic because of discrepancies in definitions.

Acrodonty is an understudied form of tooth implantation where the tooth is attached via hard tissue (ankylosed) to the apex of the jaw; this differs from mammalian or crocodilian thecodonty, where the tooth sits within a socket (LeBlanc & Reisz, 2013; LeBlanc et al., 2016), and from reptilian pleurodonty, where the tooth is attached to the labial wall of the jaw (Zaher & Rieppel, 1999). The acrodont condition in amniotes has been continually redefined throughout its historical use, often with conflicting anatomical interpretations. For example, acrodonty is associated with a reduction or loss of tooth replacement and is linked to other lepidosaur adaptations for heavy tooth wear. These associations are supported by the diversity of extant acrodont lepidosaurs, where the convergent reduction in tooth replacement has resulted in an association between oligophyodonty (reduced tooth replacement) and the evolution of acrodont implantation (Zaher & Rieppel, 1999; Smirina & Ananjeva, 2007). It is unknown if the association between a lack of replacement and implantation mode persists when considering dental diversity in extinct reptiles with acrodont dentitions, which are found in eureptilian groups outside of Lepidosauria.

The Early Permian eureptile Opisthodontosaurus carrolli is ideally suited to address the evolutionary link between acrodonty and oligophyodonty, because it is the oldest known acrodont reptile. Material of O. carrolli, known only from the Dolese Brothers Limestone Quarry

62 near Richards Spur, Oklahoma, was originally attributed to the gymnarthrid ‘microsaur’ Euryodus primus (e.g., Peyer, 1968; Reisz et al., 2015), but was recognized to be a captorhinid reptile, based on more complete material, with an unusual dentition that was convergent with that of some ‘microsaurs’ (Reisz et al., 2015). Opisthodontosaurus is also unique among acrodont reptiles in exhibiting very little tooth wear, while also showing very little evidence of tooth replacement (replacement teeth and resorption pits). The rarity of resorption pits or replacement teeth led Bolt and DeMar (1983) to hypothesize that this animal replaced its teeth simultaneously in each jaw quadrant, similar to the extant piranha (Shellis & Berkovitz, 1976). The presence of the oldest known acrodont dentition in an Early Permian reptile, coupled with controversy related to the mode or frequency of tooth replacement led us to study Opisthodontosaurus as a unique case in early reptilian dental evolution.

Here we present additional material of Opisthodontosaurus that allows us to further characterize the relationship between its acrodont dentition and the apparent lack of replacement. The larger data set in this study now represents a developmental series through which we can see that simultaneous replacement likely did not occur. This developmental series allows us to identify, and to model tooth replacement in an acrodont reptile for the first time. The replacement in Opisthodontosaurus is characterized by increased tooth size and reduced tooth count, the mechanism of reduction being of particular interest as it is poorly documented in non- mammalian amniotes. Furthermore, this increase in sample size allowed for the identification of an ontogenetic series that shows a peculiar reduction in tooth count through ontogeny.

Materials and methods

The sampled material consisted of 32 specimens, 13 of which were histologically sectioned, and 12 of which were measured (Sup. Table 1 & Sup. Table 2). The remainder of the specimens were too incomplete be accurately measured and were only used for external examination. All specimens in this study were photographed using a Canon EOS40D prior to any sectioning. All sectioning was done at the Royal Ontario Museum. Specimens were embedded in AP Castolite acrylic resin, vacuumed, and left to cure for a minimum of 24 hours. All embedded specimens were cut using a Buehler IsoMet 1000 wafer saw at low speed (200–300 rpm). The

63 specimens were mounted on plexiglass slides using Scotch-Weld SF-100 cyanoacrylate. The slides were then mounted on a Hillquist 1010 and ground down until near-optical clarity was achieved. The specimens were subsequently polished by hand on glass plates using progressively finer grit, beginning with a 600-mesh silicon carbide powder and working down to a 1-micron aluminum oxide powder, until optimal clarity was achieved. All slides were imaged using a Nikon DS-Fi1camera mounted to a Nikon AZ 100 microscope fitted with polarizing and lambda filters and an oblique illumination slider. Image processing was performed through NIS- Elements registered to R. R. Reisz of the University of Toronto Mississauga. All figures were compiled using Adobe Photoshop and Adobe Illustrator CS6 software.

Results

17.1 External morphology

Cranial material of Opisthodontosaurus carrolli from the Dolese Brothers Quarry are relatively rare, which is why this study focuses on the dentaries, which are more frequently preserved as relatively complete elements (Fig. 1). As briefly described by Reisz et al. (2015), the mandibular dentition of O. carrolli comprises as few as ten and as many as thirteen teeth ankylosed to the apex of the dentary (Fig. 1A-E, I). The anterior three teeth are comparatively slender, with the first two teeth being slightly procumbent. The next group of teeth gradually increase in diameter and height posteriorly. Each tooth consists of a wide circular base that tapers to a blunt point. The largest tooth in the dental series is positioned at the mid-length of the dentary but posterior to the midpoint of the tooth row. The posteriormost region of the tooth row contains two to three short, bulbous teeth that are approximately a third of the size of the largest dentary tooth (Fig.1H). These teeth are usually of a similar size to each other, but, in some dentaries, these teeth decrease slightly in size posteriorly (Fig. 1A-H).

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FIGURE 1: A sequence portraying the ontogenetic change in tooth count and morphology. A, ROM77328 an incomplete dentary with 13 tooth positions; B, ROM77329 an incomplete dentary with 12 tooth positions; C, ROM77311 an incomplete dentary with variation in tooth morphology and 11 tooth positions; D, ROM77309 an incomplete dentary showing enamel boundary color differentiation, with 11 tooth positions; E, ROM77310 a complete dentary with 10 tooth positions; F, a close up of ROM77328 showing equal lingual and labial walls of the dentary; G, a close up of ROM77310 showing external morphology of the attachment site; H, OMNH43300 a complete dentary with 10 tooth positions (1-3) demarking the anterior, mid dentary and posterior regions of the marginal dentition; I, a graphical representation of the relationship between tooth counts and symphysis height. Red line = indicates where symphysis height was measured. Scale bar = 1 cm. Abbreviations; ab, alveolar bone; la, labial wall; li, lingual wall; pld, plicidentine.

The external morphology of the teeth allows us to differentiate the crown from the root because there is a notable change in color and contrast on each tooth. The enamel-covered crown is glossy and darker in colour than the base in lighter-coloured (hydrocarbon-poor) dentaries and is slightly lighter than the base in black (hydrocarbon-enriched) specimens (Fig. 1G). This variation is present in all of the Opisthodontosaurus material sampled in this study. Another feature that characterizes the teeth of this taxon is the marked fluting towards the crown tips (Reisz et al., 2014:fig. 1c). This fluting and color variation is also found in Captorhinus (Heaton, 1979; Heaton & Reisz, 1980; de Ricqlès & Bolt, 1983; LeBlanc & Reisz, 2015) and in more distantly related taxa from the Dolese Brothers Quarry, including the parareptiles Delorhynchus cifellii (Reisz et al., 2014) and Colobomycter pholeter (Modesto, 1999; MacDougall et al., 2017)

We identified seven specimens that are particularly relevant to the mode of tooth replacement in Opisthodontosaurus, representing a developmental series (Fig. 2). The first specimens are two small enamel and dentine caps (ROM 77313, ROM77314) which were assigned to Opisthodontosaurus based on their unique tooth morphology and size (Reisz et al., 2015). The tapered edges of these caps are clear evidence that they are replacement dentition (Fig. 2A-C) rather than jagged, sharp edges that would have been found in a broken tooth. The next two specimens (ROM77306, ROM77308) are the only two examples with resorption pits; ROM 77306 is a complete dentary that shows a single resorption pit at the ninth tooth position that penetrated into the pulp cavity, while ROM77308 is an incomplete dentary with a resorption

66 pit that does not penetrate the pulp cavity. Another specimen (ROM77307) is a complete dentary that lacks any dentition, but the dentary preserves the vascular canals that supplied each tooth position (Fig. 2J-K). In addition, there is scarring on the bone, showing that the vascular canals were previously situated more anteriorly than their current position and appear to have shifted posteriorly by as much as half of a tooth position between replacement events (Fig. 2L). This specimen shows two sets of tooth positions, the currently occupied positions and the developing tooth positions, the latter of which are indicated by the clear resorption bays on the dentary posterior to functional tooth positions. The last specimen, a partial right dentary (ROM77334), preserves the entire tooth row with only minor damage to the anterior teeth. The damaged teeth consist of broken dentine bases that are still ankylosed to the jaw; however, the eighth tooth position shows no damage to the jaw bone, nor is there a tooth present (Fig. 2H-I). For these reasons, we determine this to be a naturally shed tooth position, showing that the teeth were not simultaneously replaced contrary to Bolt and Demar’s (1983) findings. The final dentary (KU9922) shows late stages of tooth replacement at several positions, where dentine fragments of the older tooth generations remain on the labial edges of the newly ankylosed dentition (Fig.2M,N).

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FIGURE 2: External morphology that support the replacement model. A, ROM77313 an enamel covered replacement tooth; B, ROM77314 an enamel covered replacement tooth; C, SEM of replacement tooth ROM 77314 showing a tapered edge; D, ROM77308 an incomplete dentary showing resorption pit; E, ROM77306 an almost complete dentary with a resorption pit that enters the pulp cavity; F, a close up of ROM77308 showing extent of resorption; G, a close up of ROM77306 showing the extent of resorption; H, ROM77334 a mostly complete dentary with the largest tooth missing; I, a close up of ROM77334 showing the shed tooth location ROM77334; J, ROM77307 an almost complete dentary showing vascular migration; K, a close up of ROM77307; L, a diagram showing the extent of migration within one tooth replacement cycle; M, KU9922 an almost complete dentary with dentine remnants around existing tooth positions; N, a close up of KU9922 showing the dentine remaining from a previous tooth generation. Abbreviations; ode, old dentine; rp, resorption pit; vc, vascular canal.

17.2 Histology

The teeth of Opisthodontosaurus were first analyzed histologically by Peyer (1968) when they were attributed to Euryodus primus. Reisz et al. (2015) examined a single jaw in coronal section in order to identify enamel and dentine and the relative proportions of the crown and the root. The enamel-covered crown constitutes one half to one third of the overall height of each tooth (Fig. 3) (Reisz et al., 2015). The enamel is thickest at the apex of the tooth and tapers rootwards where it meets a covering of acellular cementum. Acellular cementum is a light, uniform-coloured band that coats the root of the tooth, making up the remaining one half to two thirds of the overall tooth height (Fig. 3A-C).

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FIGURE 3: Histological anatomy of the dentary and associated dentition. A, a cross section of ROM77312, TS00303, showing the dentary with associated dentition, tooth is in 2nd position; B, close up of the attachment tissues on the labial side of TS00303; C, the attachment tissues on lingual side TS00303; D, a close up of the lamellar bone structure of the dentary in TS00303; E, incomplete ankylosis shown in TS01110, ROM77323; F, a longitudinal section of the dentary and associated dentition showing plicidentine ROM77317 TS01108; G, close up of plicidentine structure showing canals and infoldings TS01108. Abbreviations; ab, alveolar bone; ac, acellular cementum; c, canal; cr, crown; de, dentine; en, enamel; jb, jaw bone; ia, incomplete ankylosis; lb, lamellar bone; rl, reversal line; rt, root.

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Each tooth is implanted on the dentary bone in an acrodont fashion where the tooth is placed at the apex of the jaw, and the attachment tissues are restricted to the base of the tooth where it contacts the dentary. The dentine forms the bulk of the tooth; it is thickest towards the tip of the crown, and thins towards the root base. The dentine is characterized by radiating tubules that housed odontoblast processes in life (Arana-Chavez and Massa, 2004) that sequentially deposited dentine matrix inwards. The sampled specimens have plicidentine (folded dentine layers) that is restricted to the basal portion of the dentine that contacts the dentary (Fig. 3F-G). The plicidentine is not as complex as that found in some coeval parareptiles (MacDougall et al., 2014) and certainly is not as complex as that found in temnospondyls; rather, it is a much more loosely organized and contains spaces within the dentine infoldings. The pulp cavity of all sampled Opisthodontosaurus dentition remains open throughout ontogeny, unlike that seen in extant acrodont animals.

The alveolar bone (LeBlanc and Reisz, 2013, 2015) is found at the base of the tooth, covering the most root-ward section of cementum as well as a part of the dentary. In coronal section, it can contain several vascular spaces between its contacts to the cementum and to the dentary, giving it a fibrous and often trabecular appearance (Fig. 3B-C). Under cross-polarized light, the alveolar bone shows a parallel-fibered microtexture at the base of the root, under the pulp cavity. The alveolar bone is more disorganized along the peripheries of the tooth base. Another series of mineralized tissue layers are visible in both longitudinal and cross-sectional profiles (Figs. 3-4) within the jawbone of Opisthodontosaurus. Several layers of this tissue may be superimposed on one another at a single tooth position. These layers of mineralized tissue are interpreted as previous alveolar bone generations because the tissues resemble the alveolar bone at the bases of the functional teeth. These multiple generations are best defined by the reversal lines that separate them from the organized bone that makes up the jaw, as well as from the underlying layers. The series of superimposed alveolar bone layers are likely remnants of previous tooth generations that occupied this tooth position. In some specimens, there is a gradual size increase in the number of generations of alveolar bone, with the widest layer being the most external (Fig. 4). It should also be noted that the anterior portion of the jaw shows multiple generations of alveolar bone vertically stacked upon one another, which is best seen in longitudinal section (Fig. 4A, C-D). In comparison, the posterior portion of the jaw shows major posterior displacement of the alveolar bone layers (Fig. 4E-F), with the newest alveolar bone

71 layers being deposited backwards. The alveolar bone displacement is most evident at the posterior end of the dentary (Fig. 4).

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FIGURE 4: Migration of dentition and asymmetrical growth of the jaw. A, a longitudinal section of the anterior portion of ROM77330 TS00280; B, a longitudinal section of the posterior portion of ROM77315 TS00266; C, TS00280 a close up of the alveolar bone on the 3rd tooth position; D, TS00280 a close up of the alveolar bone on the 5th tooth position; E, TS00266 a close up of the alveolar bone layers below an unknown tooth position; F, TS00266 a close up of the alveolar bone layers below an unknown tooth position; G, an longitudinal section of anterior portion of ROM77316 TS01105; H, a close up of TS01105 showing migrating vasculature; I, a cross section of ROM77312 TS00302; J, a close up of the alveolar bone at base of the tooth position TS00302. The bicolored arrows demarcate generation of alveolar bone. Abbreviations; ab, alveolar bone; de, dentine; ode, old dentine vc, vascular canal.

The lamellar bone of the dentary contains numerous distinct growth lines that are visible in both coronal and transverse sections (Fig. 3A, E, 4). These lines show the directionality of growth across the jaw bone and indicate that the jaw grew in width roughly symmetrically and at a relatively slow rate, unlike the condition in other captorhinids (Fig. 2; LeBlanc and Reisz, 2015). The slow rate of jawbone growth can be inferred by a lack of vascularity compared to that seen in the dentaries of C. aguti (LeBlanc and Reisz, 2015). Secondary osteons are concentrated in the center of the dentary in coronal and transverse sections (Fig. 3A, 4G-H). Layers of secondary lamellar bone that were deposited anteriorly to migrating vasculature indicate that posterior migration of teeth and vasculature was most pronounced in the middle to posterior regions of the dentary (Fig. 4A-H). Lastly, it is important to note that the growth lines are more spaced apart in the posterior end of the jaw, best seen at the right ventral edge (Fig. 4B), whereas the growth lines are deposited close to one another at the anterior portion of the jaw (Fig. 4A).

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Discussion

18.1 Opisthodontosaurus as a model for acrodont tooth replacement

Whereas some acrodont fishes show evidence of replacement (e.g., Berkovitz and Shellis, 1978), acrodonty in reptiles is universally associated with a loss of tooth replacement. Tooth implantation and development have been studied in chameleons, sphenodontians, and some agamids, taxa that show apically positioned teeth and lack of tooth replacement (Cooper et al., 1970; Throckmorton, 1979; Smirina & Ananjeva, 2007; Buchtová et al., 2013; Dosedělová et al., 2016). These extant taxa exhibit many adaptations to extreme wear, making them excellent developmental models for studies of wear resistance and how a dentition can remain functional for an extended period of time in spite of a lack of replacement (Cooper et al., 1970; Throckmorton, 1979; Buchtová et al., 2013; Dosedělová et al., 2016). These wear adaptations have also become intimately linked with the acrodont condition, just as the lack of replacement has become a part of the definition of acrodonty (Zaher & Rieppel, 1999; Smirina & Ananjeva, 2007). The definitions by Romer (1956) and Peyer (1968) mention fusion of the tooth to the apex of the jaw as acrodonty, and Motani (1997) and Shellis (1982) both mention ankylosis to the apex of the jaw as a defining feature. Edmund (1969) also defined acrodonty as a tooth that is ankylosed via cement to the apex of the jaw, but he was also the first to mention that reduced replacement is associated with this mode of tooth implantation, which has then been perpetuated through reptilian literature as the standard characteristic for the acrodont condition.

Although acrodont tooth replacement is undocumented in extant amniotes, the mode and pattern of replacement in pleurodont teeth is well studied (e.g., Cooper, 1966; Rieppel, 1978; de Ricqlès and Bolt, 1983; Zaher and Rieppel, 1999; Delgado et al., 2003; Handrigan et al., 2010; LeBlanc and Reisz, 2015) and is likely the ancestral condition for amniotes. Pleurodonty is also the dominant form of implantation in anamniotes, both extinct and extant (e.g., Kline, 1983; Smith et al., 2009), providing an informative basis for comparisons and for developing a model of tooth replacement for acrodont reptiles. Tooth replacement in pleurodont dentitions begins with the formation of a new tooth lingual to the functional tooth, which through continued growth, encroaches on the lingual surface of the functional tooth base. The resorption of the

74 older tooth results in the onset of a resorption pit, and as the new tooth continues to grow and to migrate into position, it either induces resorption of the entire functional tooth or the dislocation and shedding of the old tooth, allowing the new tooth to become situated and ankylosed in the vacated position.

Acrodont replacement in Opisthodontosaurus, although more difficult to detect for taphonomic reasons, follows the same sequential pattern as that of pleurodont teeth in progressing through tooth initiation, growth, resorption, shedding, and ankylosis (Fig. 2). Here, we provide a developmental and replacement model for the dentition of Opisthodontosaurus based on our anatomical and histological data, which we supplement with soft tissue interpretations from the previously mentioned modern pleurodont squamates (Fig. 5). The earliest-forming teeth in Opisthodontosaurus likely formed from the free end of the dental lamina, lingual to the functional tooth and completely surrounded by soft tissue (Fig. 5A). The evidence to support this hypothesis is three-fold. First, there is no histological evidence of teeth developing within the jaw bone, as seen in thecodont taxa (Zaher & Rieppel, 1999; LeBlanc & Reisz, 2013; Cerda et al., 2015; LeBlanc et al., 2016). Second, resorption pits, although rare, are identified at a position lingual to the functional marginal dentition in Opisthodontosaurus, highlighting the position of early-forming replacement teeth; in some cases the newly forming tooth is lingual and slightly posterior to the functional tooth. Third, the hypothesized positions of the replacement teeth in Opisthodontosaurus are consistent with their placement along the dental lamina in extant squamates (Fig. 5A). This interpretation also provides an explanation for the paucity of in situ replacement teeth in Opisthodontosaurus and potentially other extinct acrodont and pleurodont amniotes.

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FIGURE 5. The proposed model of acrodont replacement for Opisthodontosaurus carrolli. A, initiation of tooth replacement where the dental lamina is in the lingual potion of the soft tissue; B, initial stages of resorption; C, advanced resorption; D, shedding and migration of new tooth into position; E, complete ankylosis of new functional tooth. Abbreviations; ab, alveolar bone; de, dentine; dl, dental lamina; en, enamel; jb, jaw bone; od, old dentine; oe, oral epithelium;

76 oab, old alveolar bone; rp, resorption pit; rt, replacement tooth; vc, vascular canal. Illustration by Dave Mazierski.

Here we present the step-wise model of replacement (Fig. 5) based on extinct and extant pleurodont reptiles as reported in the literature (Zaher & Rieppel, 1999; Kline, 1983; Smith et al., 2009). In stage A (Fig.5A), after initiation of the tooth bud from the dental lamina, the developing tooth would reach a sufficiently large size to encroach on the space occupied by the existing ankylosed tooth. This leads to stage B: resorption of the lingual surface of the functional tooth (Fig. 5B). Resorption pits are a hallmark of continuous replacement in many polyphyodont taxa (e.g., Bolt & Demar, 1983; Delgado et al., 2003; LeBlanc & Reisz, 2015) and capture an early stage in the dynamic process of tooth replacement. In material of Opisthodontosaurus that was examined in this study, these pits are quite rare. The paucity of these pits indicates that the replacement in this eureptile was probably less frequent than in most other amniotes, but when replacement did occur, the window of time during which these teeth were being resorbed was short relative to the lifespan of the individual tooth. This was first noted by Bolt & DeMar (1983) when originally describing the pattern of replacement in Opisthodontosaurus when it was identified as Euryodus primus, a feature we can confirm in our sample. Two specimens (ROM77306 and ROM77308) show evidence of resorption. ROM77306 shows resorption of the lingual wall without the pulp cavity being invaded, whereas ROM77308 shows a more significant resorption of the lingual wall with a breach of the pulp cavity (Fig. 2D-G). However, it is likely that there was an additional level of resorption, as shown in stage C (Fig. 5C), where ~30% or more of the tooth base has been resorbed. This particular stage has not been found in any known specimen, probably because by this stage the tooth would have been sufficiently compromised such that it would have been shed in life, or broken off by taphonomic processes.

After the functional tooth has been shed in stage D, the new tooth would quickly become attached to the jaw as represented by stage E. However, if ankylosis does not occur prematurely, prior to migration, it is likely that fossils would only show a tooth position devoid of dentition at this stage, as the replacement tooth would have been only attached via soft tissue. This stage is difficult to document as this lack of dentition is common in the sampled specimens, although often the surrounding tissue is damaged. This leads us to believe that the loss was due to a taphonomic process rather than to subsequent shedding because all of the specimens in this sample have been completely disassociated from the rest of the skull. This shedding stage prior to ankylosis of the replacement tooth is best seen in ROM77334 (Fig 2H-I) where only one tooth

77 78 is missing in an otherwise complete tooth row. This leads us to conclude that this tooth was either ligamentously attached or was still within soft tissue.

Following the resorption events in stages B and C (Fig. 5B-C) the new tooth moves into position prior to full ankylosis in stage D (Fig. 5D). At this stage, if ankylosis occurs prematurely, or if the alignment of the dentition is distorted, as seen in KU9922, fragments of the previous tooth generation are retained labial to the new teeth. Another possible explanation for the incomplete resorption of the remnants of old teeth seen in this specimen is asymmetrical growth of the jaw labio-lingually at the time of replacement, effectively moving the functional tooth away from the area that would have been affected by resorption. This asymmetry would leave more alveolar bone remnants of the previous tooth generation, as found in Captorhinus aguti (LeBlanc & Reisz, 2015). We believe that specimens like KU9922 that show a large amount of dentine and alveolar bone from previous generations represent the exception rather than the rule due to their paucity in the fossil record.

Stage D also includes asymmetrical ankylosis, which is best seen in coronal section (Fig. 3D). In specimens that have incompletely ankylosed teeth, they consistently show either incompletely developed attachment tissue or no attachment tissue at all on the lingual side, providing evidence that ankylosis would have first occurred on the labial side of the dentary. The final step in the replacement cycle is complete ankylosis by alveolar bone to the dentary as represented by stage E (Fig. 5E). Although the old tooth has been partly resorbed and then shed, and a new tooth has ankylosed to the dentary, evidently not all of the alveolar bone was resorbed in Opisthodontosaurus, leaving vital clues regarding the number of replacement events that occurred at each locus. The outlined indicators of replacement as well as the proposed replacement model here can be used to detect replacement in other acrodont reptiles, including stem acrodontians.

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18.2 Opisthodontosaurus as a model for ontogenetic tooth migration

Histological thin sections provide clear evidence of repeated tooth replacement in Opisthodontosaurus, but unexpectedly also revealed the presence of a high degree of posterior tooth migration throughout ontogeny. Most reptiles exhibit minimal change in tooth position and tooth count, with a few documented exceptions (e.g., Brown et al., 2015). Reptilian dentitions tend to be homodont (Montanucci, 1968) readily masking any external anatomical evidence of a change in tooth position that would be associated with tooth replacement, as the new tooth would look very similar in size and shape to its predecessor. An exception is Alligator mississipiensis, where there is modest heterodonty, and an ontogenetic sequence has been constructed (Westergaard & Ferguson, 1990) to show tooth position migration. The heterodonty in Opisthodontosaurus facilitates identification of discrete regions of the dental row, which then facilitates the identification of tooth loss through ontogeny and migration of tooth positions. In Opisthodontosaurus, the change in tooth positions is not only coupled with a reduction in tooth count (Fig.1I & Sup. Fig.1) and changes in tooth size but also with uneven growth along the jaw, which is the likely cause of the migration seen in this taxa.

The migration of tooth positions is best seen in longitudinal section (Fig. 4) where both the anterior and posterior parts of the dentary were sampled from two different specimens. The preservation of multiple remnants of old teeth (Fig. 4C-E), along with generations of alveolar bone provides vital clues for tooth replacement and migration. The anterior part of the jaw features minimal migration, resulting in multiple generations of alveolar bone being vertically stacked upon one another, showing that each tooth position was vertically overlaying a previous generation of tooth positions. By comparison, more posterior tooth positions show major migration of tooth positions between tooth generations (Fig. 4D-F). In the posterior half of the dentary, new tooth positions are more posteriorly placed than their predecessors, again indicated by the displacement of alveolar bone layers, with the newest layers being more posteriorly placed than the previous generation. Moreover, one dentary (ROM77307) shows external evidence of tooth migration within a single replacement event; tooth replacement and subsequent migration in this specimen seem to be occurring at a rapid rate (Fig. 2J-L). The newest tooth position is set about a half tooth position posteriorly from the previous tooth position. As with other specimens, the anterior tooth positions do not experience the same dramatic migration

80 posteriorly as seen in the most posterior dentition. The attachment tissues (alveolar bone) support this conclusion, not only seen histologically, but also in the build-up of alveolar bone in the old tooth position location prior to migration in ROM 77307. It is important to note that this tooth migration is most pronounced in the posterior end of the dentary (Fig. 2J-L, 4).

The migration of tooth positions cannot be accomplished by the dentition alone, as this would require a ligamentous tooth attachment to facilitate migration of a tooth across the jaw (Saffar et al., 1997). As in other captorhinids (LeBlanc and Reisz, 2015), the teeth of Opisthodontosaurus were fused to the jaws and were thus immobile once ankylosed. This pattern of posterior tooth migration is most likely explained by the growth of the dentary along with the change in position of the dental lamina. It appears that the rate of anteroposterior growth of the dentary is uneven, with the most pronounced deposition of lamellar bone occurring posteriorly, resulting in tooth migration occurring at the middle and posterior regions of the bone. We hypothesize that the jaw grew at a rate that was independent of tooth replacement, resulting in tooth migration. As the lamellar bone was being deposited on the surface of the dentary during growth, there was a disproportionate amount of deposition towards the posterior end of the dentary. This is supported by the difference in the width between the growth lines that is seen in the anterior and posterior portions of the jaw (Fig. 4). The larger intervals between growth marks in the posterior end of the jaw indicate that there was more tissue being deposited at each growth event, in comparison to the anterior region. This unequal deposition of tissue would result in more posterior growth of the dentary, while new teeth were being initiated at the same spatial position relative to the jaw, as tooth initiation is constrained by the location of the developing tooth buds along the dental lamina. As the dentary grew posteriorly, the soft tissue including the dental lamina would grow in conjunction. Therefore, relative to the developing tooth, the bone below the developing replacement tooth positions would have shifted anteriorly through growth, predominantly in the mid and posterior region of the dentary. Finally, we also hypothesize that the reason why the anteriormost dentition did not experience any migration is that as the jaw grows posteriorly, and the dental lamina moves along with it, the anterior portion of the jaw and the first tooth-position initiation site of the dental lamina would not shift posteriorly. This results in changes in the middle to posterior tooth positions along the dentary bone that appear as posterior migration. It is known that bones do not grow evenly (e.g., Smirina & Ananjeva, 2007), and the dentary of Opisthodontosaurus is no exception.

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18.3 Ontogenetic tooth loss and feeding biomechanics

Our analysis of 32 specimens has shown a pattern of ontogenetic tooth loss through the reduction of overall tooth counts from 13 to 10 tooth positions (Fig. 1I). This is rare among most acrodont reptiles, which add tooth positions posteriorly through life, with cases of tooth loss being limited to Alligator mississippiensis (Brown et al., 2015). The ontogenetic reduction in tooth count in Opisthodontosaurus is difficult to quantify statistically because most of the dentaries are incomplete, making jaw length an ineffective metric by which to approximate size or age of the individual. We decided to use the height of the mandibular symphysis as a proxy for jaw size relative to tooth count (Fig. 1I). The two largest and most complete dentaries available in this sample (ROM77310, OMNH 43300) have the fewer tooth positions (10). This is in contrast to the smallest complete dentary, which has 13 positions (Fig. 1A). The tooth loss is likely due to a developmental mechanism that determines if the amount of vacant space is sufficient for the developing tooth. Each replacement tooth is larger than its predecessor and therefore requires more of the surface area. Although the jaw is growing wider and longer through ontogeny, it appears that the size of the developing teeth is increasing at a rate that surpasses that of the jaw, thereby resulting in a decrease in the number of teeth present in the dentary. It is also worth noting that Opisthodontosaurus appears to exhibit variation in tooth count that is confined to the region anterior to the largest tooth (Fig. 1A-H). There is no pattern that predicts whether two or three teeth are found posterior to the largest tooth in the dentary; no correlation with size or the tooth count in the anterior part of the dentary is evident. Furthermore, some partially articulated individuals (Reisz et al., 2015) can maintain varying tooth counts on either mandibular ramus.

The dentary appears to become more robust through ontogeny (Fig. 1), increasing in size dorsoventrally and becoming more bowed ventrally. As part of this ontogenetic change, there appears to be a proportional decrease in the length of the dentulous region in the durophagous reptile Opisthodontosaurus (Reisz et al., 2015). This has been seen in other durophagous reptiles, such as the squamate Varanus niloticus (Rieppel & Labhardt, 1979), which exhibit a shift in dental morphology coupled with a proportional shortening of the tooth row, increased depth of the jaw, and the development of a bowed appearance. Varanus niloticus, Amphisbanea ridley and

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Opisthodontosaurus carrolli all have their primary crushing site associated with a large tooth near the posterior end of the tooth row, or exhibit a shift towards that morphology through ontogeny. This large tooth is closer to the adductor jaw musculature, potentially increasing their mechanical advantage (Rieppel & Labhardt, 1979; Pregill, 1984). In V. niloticus, this shift is closely related to an ontogenetic shift in diet from insectivorous juveniles to molluscivorous adults (Rieppel & Labhardt, 1979), whereas in A. ridley there is no such shift; instead the development of durophagous adaptations is attributed to expansion of the feeding repertoire of an animal not limited by predators (Pregill, 1984). This raises the possibility that there may be an ontogenetic shift in diet in Opisthodontosaurus carrolli or that mature individuals simply increase their mechanical advantage in order to consume larger, possibly tougher prey items. However, it is important to note that Opisthodontosaurus is unlike any modern acrodont reptile. Modern acrodont reptiles lack replacement, and therefore have adaptations to combat wear of their dentition, namely infilling their pulp cavities with dentine and bone (Cooper et al., 1970; Throckmorton, 1979; Smirina & Ananjeva, 2007; Buchtová et al., 2013; Dosedělová et al., 2016). This in-filling of the pulp cavity through ontogeny is absent in Opisthodontosaurus. The large open pulp chambers in the teeth of O. carrolli show that, unlike modern acrodontians, this early reptile replaced its teeth frequently enough that pulp breach (due to extensive tooth wear) was unlikely to occur.

Conclusion

This analysis of the dentition of Opisthodontosaurus adds to our understanding of how tooth implantation can affect where and how we find evidence of tooth replacement. In the case of Opisthodontosaurus, the acrodont mode of implantation does not impede the traditional form of lingual replacement. Although the evidence for replacement (resorption pit) is not easily found, histological analysis of the jaws provides a much clearer understanding of the dynamic process of tooth replacement in this taxon. Histological analysis has revealed a surprisingly complex and dynamic dentition in Opisthodontosaurus that shows previously unrecognized ontogenetic changes. These changes arise from a combination of (1) the growth of the jaw; (2) the disproportionate size increase of the dentition, in particular the larger posterior teeth; and (3) the changing spatiotemporal patterns of the replacement events. Two intriguing issues requiring further work arise from this study. Firstly, how does the vasculature that fed the developing tooth

83 before implantation relate to the vasculature that fed the implanted, fully ankylosed tooth? Secondly, how are the apparent differences between the growth rates of the tooth bearing elements (and hence the skull) and that of the marginal dentition related to ontogenetic changes in feeding behaviour? Both of these issues can be addressed only by using extant model organisms where these developmental and ontogenetic phenomena can be studied further. Through the use of the histological indicators identified in this study, future studies can identify tooth replacement, migration and loss in other amniotes.

The acrodont replacement model proposed here reflects the primitive pattern seen period of amniote diversification, the predominant pattern of implantation is pleurodont, and the pattern of tooth development and replacement are well known. Despite being an acrodont reptile, Opisthodontosaurus demonstrates that this type of implantation can also be found in amniotes that replace their teeth in a typical fashion, similar to any pleurodont taxon. This study also allows for discussions of the traditional tooth implantation definitions and how the characters that are attached to them may ultimately be caused by other factors rather than the mode of implantation. The evidence of repeated tooth replacement within the jaws in Opisthodontosaurus shows that tooth implantation alone is not a reliable external indicator of major differences in dental development. In fact, the recognized stages of tooth development and replacement are highly conserved, and tooth implantation simply describes a geometric relationship between the dentition and its tooth-bearing element. It is this high degree of developmental conservation that makes tooth implantation a poor phylogenetic character, as these implantation modes can be highly plastic and do not necessarily reflect an evolutionary trajectory.

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