Tooth replacement rate can be calculated in extinct animals by counting incremental lines of deposition in tooth dentin. Calculating this rate in several taxa allows for the study of the evolution of tooth replacement rate. Sauropod dinosaurs, the largest terrestrial animals that ever evolved, exhibited a diversity of tooth sizes and shapes, but little is known about their tooth replacement rates.
We present tooth replacement rate, formation time, crown volume, total dentition volume, and enamel thickness for two coexisting but distantly related and morphologically disparate sauropod dinosaurs Camarasaurus and Diplodocus. Individual tooth formation time was determined by counting daily incremental lines in dentin. Tooth replacement rate is calculated as the difference between the number of days recorded in successive replacement teeth. Each tooth family in Camarasaurus has a maximum of three replacement teeth, whereas each Diplodocus tooth family has up to five. Tooth formation times are about 1.7 times longer in Camarasaurus than in Diplodocus (315 vs. 185 days). Average tooth replacement rate in Camarasaurus is about one tooth every 62 days versus about one tooth every 35 days in Diplodocus. Despite slower tooth replacement rates in Camarasaurus, the volumetric rate of Camarasaurus tooth replacement is 10 times faster than in Diplodocus because of its substantially greater tooth volumes. A novel method to estimate replacement rate was developed and applied to several other sauropodomorphs that we were not able to thin section.
Differences in tooth replacement rate among sauropodomorphs likely reflect disparate feeding strategies and/or food choices, which would have facilitated the coexistence of these gigantic herbivores in one ecosystem. Early neosauropods are characterized by high tooth replacement rates (despite their large tooth size), and derived titanosaurs and diplodocoids independently evolved the highest known tooth replacement rates among archosaurs.
Citation: D’Emic MD, Whitlock JA, Smith KM, Fisher DC, Wilson JA (2013) Evolution of High Tooth Replacement Rates in Sauropod Dinosaurs. PLoS ONE 8(7): e69235. https://doi.org/10.1371/journal.pone.0069235
Editor: Alistair Robert Evans, Monash University, Australia
Received: November 9, 2012; Accepted: June 6, 2013; Published: July 17, 2013
Copyright: © 2013 D’Emic et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: Funding was provided by the Scott D. Turner Award (University of Michigan) to MDD. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Large or complex dentitions generally experience attrition through abrasion against food, substrates, or other teeth. In mammals, food intake and tooth use tend to increase with body size, so larger animals tend to exhibit increased tooth wear . During their nearly 300-million-year evolutionary history , vertebrate herbivores evolved numerous mechanisms to cope with increased tooth wear, including changes in the mechanical properties of tooth tissues , , increases in the number of teeth that are functional at one time , , continuous tooth growth and eruption throughout the life of the animal , increases in the number of tooth-bearing bones, changes in crown volume and/or shape –, and increased tooth replacement rate , .
Sauropod dinosaurs achieved the largest adult body sizes of any terrestrial herbivore, and so would have required a large food supply and high levels of tooth use and tooth wear regardless of their inferred physiology –. Evolutionary responses to high tooth wear in sauropods – including changes in tooth volume and tooth replacement rate – are first recorded shortly after their divergence from sauropodomorph ancestors. Early Jurassic sauropods increased tooth size, but decreases in tooth size characterized some later-appearing lineages . The volume of the tooth crown has a demonstrated relationship to its formation time and expected use-life ,  and is inversely related to the number of teeth that can be held at each tooth position . High tooth replacement rates were calculated in one sauropod with up to ten small teeth packed at each tooth position , but neither the relationship between tooth volume and replacement rate nor the relationship between these parameters and the overall rate of replacement of the total functional dentition have been studied for other sauropods.
Here, we measure tooth formation time, replacement rate, crown volume, and enamel thickness in sectioned teeth of Camarasaurus and Diplodocus, two neosauropod dinosaurs from the Late Jurassic Morrison Formation of North America. The largest exemplars of these two genera are similar in body mass (e.g., femur length ca. 1.8 m, sum of femoral and humeral circumference ca. 1.3 m; MDD unpublished data), but they belong to distantly related neosauropod clades that differ substantially in skull morphology, body proportions, and inferred feeding ecology –. The rarity of sauropod craniodental materials that can be sacrificed for histological sampling limits the taxonomic scope across which we can measure these features. We explore the distribution of these features more broadly within Sauropodomorpha by developing a method to estimate tooth replacement rates for several taxa that have craniodental material but cannot be sampled histologically.
Materials and Methods
Permission was received to access the relevant specimens from museum collections managers. Specimens were loaned from the Yale Peabody Museum, Utah Museum of Natural History, Staatliches Museum für Naturkunde, and Iziko South African Museum. Computed tomography (CT) images were acquired at the Canton Health Center, University of Michigan, using a General Electric Lightspeed Pro 8 CT scanner, GE Medical systems, Milwaukee, Wisconsin. CT slices were taken using 140 Kv and 325 mA, with 1.250 mm thick slices and 0.625 mm overlap. Incremental lines were counted in thin section. Each tooth was mechanically removed from the jaws. Specimens were embedded in epoxy resin, cut longitudinally on a Buehler Isomet saw with a diamond wafering blade, mounted on a glass slide, cut to a thick section, and hand-sanded and polished until incremental lines were visible. Thin sections were photographed using a Spot CCD camera (Spot Insight 11.2 Color Mosaic, Diagnostic Instruments) mounted on a Nikon SMZ 1500 microscope. Increments were counted in ImageJ ,  using the IncMeas v1.11 plug-in .
Tooth formation time and replacement rate in Diplodocus and Camarasaurus were measured by counting incremental lines of von Ebner (Fig. 1), which have been shown to represent daily fronts of dentin deposition in several groups of extant amniotes , , –. We define tooth replacement rate to be the time required to replace one tooth in a given alveolus. This rate is sometimes expressed in days, with the unit numerator implicit. Replacement rate was calculated by subtracting tooth formation times for successive teeth within one family, following Erickson , . Recently, Scheyer and Moser  questioned the identification of incremental lines of von Ebner in sauropods, suggesting that they could represent longer-period increments (e.g., Andresen lines). We examined our thin sections and did not find smaller increments between the lines spaced ca. 15 microns apart in areas where preservation seems excellent, so we interpret these lines as daily fronts of deposition. The ca. 15-micron spacing of incremental lines of von Ebner observed in Diplodocus and Camarasaurus is close to the mean value observed in labelling studies of adult Alligator .
Thin sections of Camarasaurus (A, C) and Diplodocus (B, D) premaxillary teeth showing incremental lines of von Ebner (white arrowheads) in dentin. Teeth are oriented with their long axis horizontal and the occlusal surface directed to the right. A shows the tip of tooth 3iii of Camarasaurus, and B shows the tip of tooth 4iv of Diplodocus. C and D are enlarged images of one ‘limb’ of tooth 3ii and 4iii, respectively. Abbreviations: edj, enamel-dentin junction; en, enamel; pc, pulp cavity. [planned for page width].
Enamel thickness was measured in ImageJ on photographs of thin sections. Thickness was measured perpendicular to the enamel-dentin junction at seven locations around the tooth crown (three labial, three lingual, and one apical). Fewer measurements were made on teeth for which enamel was chipped or missing in certain locations. Labial and lingual measurements were taken at roughly evenly spaced locations along the apicobasal axis (one near the tooth tip or apex, one near the mid-length of the crown, and one near the crown-root junction). Enamel thickness varies around the tooth crown, so comparison of labial and lingual thicknesses for each tooth was based on the average of three labial measurements and the average of three lingual measurements. An overall average of all measurements taken on a single tooth was also calculated. Raw enamel measurements are presented in Supporting Information (Raw Data S1).
Volumes of both the entire tooth and the crown (i.e., the part of the tooth covered in enamel, including the pulp cavity) were measured by water displacement via suspension three times and averaged (see Raw Data S1) . Total erupted tooth volume (the sum of the volumes of all ‘fresh’ [functional but unworn] teeth in the jaw) and crown volume (the sum of the crown volumes of all fresh teeth in the jaw) were estimated for Camarasaurus and Diplodocus. Tooth crowns are similar in volume for adjacent teeth throughout and among jaw elements for all tooth positions except for the last few in these species. For each species, the antepenultimate and penultimate tooth crown volumes were estimated as 75% of the average measured tooth crown volume, and the last tooth position was estimated as 50% of the average measured tooth crown volume. In contrast to total crown volumes, total functional tooth volumes were more complicated to estimate because the alternating pattern of tooth replacement in these species yields tooth roots of substantially different size in adjacent teeth. The average of total functional tooth volumes for two large teeth was used as the functional individual tooth volume. As with crowns, total functional tooth volumes for the antepenultimate, penultimate, and ultimate tooth positions were estimated as 75%, 75%, and 50% of the volume of the largest teeth, respectively. Finally, in Diplodocus, dentary teeth are about 10% smaller in volume than premaxillary or maxillary teeth , so estimates of the volumes of dentary teeth and crowns were adjusted accordingly.
In many cases, destructive sampling of a specimen was not possible. For these taxa, we developed a non-invasive approach for estimating replacement rate, based on use of Camarasaurus as a model for taxa with broad-crowned teeth (Patagosaurus, Mamenchisaurus) and Diplodocus as a model for taxa with narrow-crowned teeth (Nigersaurus, Río Negro titanosaur). Both models were used for estimation of replacement rate in Massospondylus, which has an intermediate crown breadth. Tooth length was measured for teeth of Camarasaurus and Diplodocus for which ages were already known via counts of incremental lines of von Ebner. For each genus, regression of tooth formation time on tooth length generated an equation that was used to estimate tooth formation time in teeth that were not sampled histologically.
We estimated volumetric tooth replacement rate (the time required to replace the total dentition-in-use) by dividing total erupted tooth volume by average tooth replacement rate. We made a similar estimate using only tooth crown volumes (volumetric crown replacement rate). We make the assumption that tooth replacement rate was constant throughout and among jaw elements due to similarities in the shape, number of replacement teeth, and depth of alveoli in all but the distal-most few teeth in each jaw element. Our simplification would tend to inflate the volumetric replacement rates, but would affect each species similarly, thus keeping results for each comparable to one another.
Histology-based tooth replacement rates and estimated replacement rates are summarized in Tables 1–2. The dentary of the basal sauropodomorph Plateosaurus did not show any replacement teeth in CT images, so no further analysis was undertaken. CT scans of a maxilla and dentary of the basal sauropodomorph Massospondylus revealed only a single replacement tooth (in one alveolus of the dentary). Although we did thin section teeth of Massospondylus, tooth replacement rate for that genus was estimated because incremental lines were poorly preserved.
CT scans reveal that each premaxillary tooth family of Camarasaurus (Fig. 2a, Movies S1 and S2) includes one functional and up to three replacement teeth, whereas each premaxillary tooth family of Diplodocus (Fig. 2d, Movie S3) includes up to one functional and five replacement teeth. Incremental lines of von Ebner visible in thin section (Figs. 1–2; Table 1) indicate that each premaxillary tooth of Camarasaurus took over ten months to form (ca. 1 tooth/315 days), whereas each Diplodocus tooth took only six months to form (ca. 1 tooth/185 days). Average tooth replacement rate in Camarasaurus was one tooth per two months (ca. 1 tooth/62 days), whereas it was about one tooth per month in Diplodocus (ca. 1 tooth/35 days).
Reconstructed skulls (A, D) and premaxillary teeth (B, C) of Camarasaurus (A, B) and Diplodocus (C, D). B and C include CT-generated sagittal and transverse sections of premaxillary alveoli and photographs of thin sections of Camarasaurus (UMNH 5527) and Diplodocus (YMP 4677). Premaxillae show replacement teeth in each of the four alveoli adjacent to the symphysis labelled by their position along the tooth row (1–4) and their position in the replacement sequence at each tooth position (i–v). Sagittal sections in B and C were taken at premaxillary tooth position 4 in Camarasaurus and premaxillary tooth position 1 in Diplodocus. The symphysis faces the bottom of the page in transverse sections. Photographs of thin sections of Diplodocus and Camarasaurus teeth show enamel (en), the pulp cavity (pc), daily-deposited incremental lines of von Ebner (arrowheads mark every other line) in the dentin (den), and the crown-root junction (crj). The 20 mm scale bar is for the premaxilla and tooth images in (B); 10 mm scale bar is for premaxilla and tooth images in (C). Skull reconstructions are from , [planned for page width].
Functional premaxillary teeth of the Camarasaurus and Diplodocus individuals are 26.5 cm3 and 1.7 cm3 in volume, respectively. Tooth crowns of the Camarasaurus and Diplodocus individuals are 15.7 cm3 and 1.5 cm3 in volume, respectively. We estimate total functional (i.e., erupted) tooth volume across the dentition to be 1,272 cm3 in Camarasaurus and 69 cm3 in Diplodocus. When measuring only tooth crowns, these values are 754 cm3 and 63 cm3, respectively. The volumetric tooth replacement rate was about 10 times greater in Camarasaurus (1272 cm3/62 days = 20.5 cm3/day) than in Diplodocus (69 cm3/35 days = 2.0 cm3/day). The volumetric crown replacement rate was about seven times greater in Camarasaurus (754 cm3/62 days = 12.2 cm3/day) than in Diplodocus (63 cm3/35 days = 1.8 cm3/day).
Premaxillary tooth crowns of Camarasaurus individuals have ca. 1.0 mm-thick enamel on both the labial and lingual surfaces of the teeth; in contrast, the enamel of Diplodocus is thinner overall (ca. 0.5 mm) and is slightly asymmetrical, with the enamel on the labial face of the tooth about 125–150% the enamel thickness on the lingual face (Figs. 1–2, Table 3).
Our non-invasive approach to estimating tooth replacement rate allowed us to evaluate a broader spectrum of sauropodomorphs. Tooth length and age are strongly related in both Camarasaurus and Diplodocus (R2>0.95), but the equations describing these relationships differed between the taxa (see Raw Data S1). We evaluated the performance of our estimation method by estimating tooth replacement rate in Camarasaurus and Diplodocus, taxa for which replacement rate is known. For a given tooth and its successor, our method of estimating both formation time and replacement rate was generally accurate to within one week. When successive replacement estimates are averaged for several teeth in a single jaw element, the estimates are off by one day at most. Because we were only able to measure the length of one tooth and its successor for each of the non-histologically sampled taxa (aside from the case of Nigersaurus), we expect that our estimates are accurate for those taxa to within one week.
The initial increase in tooth size and crown breadth that occurred near the base of Sauropoda was accompanied by a reduction in tooth replacement rate (as estimated by replacement tooth length). The much smaller teeth of basal sauropodomorphs like Massospondylus and Patagosaurus formed and replaced faster than did the larger teeth of basal sauropods like Mamenchisaurus (Fig. 3; Table 2). Derived broad-crowned taxa (e.g., Camarasaurus) exhibited a higher replacement rate than non-neosauropods like Mamenchisaurus and matched the rate in the much smaller-toothed Patagosaurus, but did not achieve rates as high as those observed in the smaller-toothed Massospondylus. Non-neosauropods exhibit a maximum of two replacement teeth per alveolus, whereas neosauropods exhibit three to nine (, , Fig. 3). Within Neosauropoda, diplodocoids and titanosaurs independently achieved higher tooth replacement rates than basal neosauropods (Fig. 3). The highly specialized diplodocoid Nigersaurus is estimated to have replaced each tooth as often as once every 14 days, twice as fast as previous estimates [30 days, ] and by far the highest rate for any dinosaur. The discrepancy between our estimate and a previous one for Nigersaurus is potentially explainable by the fact that the histology-based replacement rate previously reported for Nigersaurus  was based on transverse thin sections of teeth. Transverse sections likely yield inaccurate replacement rates due to the limited number of incremental lines of von Ebner exposed in any given transverse plane.
The light gray field indicates taxa that have at least three replacement teeth at each tooth position; dark gray field encapsulates taxa that have narrow tooth crowns. Silhouettes along the top of the cladogram show the number and size of replacement teeth in one tooth position. These include (from left to right): Patagosaurus (MPEF-PV 1670), Mamenchisaurus , Diplodocus (this study), Nigersaurus [Sereno, Wilson, Witmer, Whitlock, Maga, Ide and Rowe, unpublished data], Camarasaurus (this study), and the Río Negro titanosaur (MPCA-79) . Number of replacement teeth is unknown in Brachiosauridae, but the taxon is optimized to have had at least three. Cladogram based on  with the addition of Tazoudasaurus  and Bonitasaura . [planned for column width].
In both Camarasaurus and Diplodocus, a volume equivalent to approximately one tooth is replaced across the dentition every 1–2 days (20.5 cm3/day and 2.0 cm3/day, respectively). These taxa are characterized by different styles of forming and replacing dentition: Camarasaurus has larger teeth that are replaced less frequently, whereas Diplodocus has smaller teeth that are replaced more frequently. Even with Camarasaurus’ lower tooth replacement rates, both sauropods exhibit tooth replacement rates on par with or higher than those of non-sauropod dinosaurian herbivores (i.e., hadrosauroid and ceratopsian ornithischians at 50–83 days; Table 4).
The enamel of Camarasaurus is roughly symmetrical labiolingually, in contrast to the slightly asymmetrical enamel of Diplodocus. The enamel of the diplodocoid Nigersaurus is highly asymmetrical, with enamel on the labial side up to ten times thicker than on the lingual side , , . Labiolingually asymmetrical enamel appears to characterize several diplodocoids, and extremely asymmetric enamel characterizes Nigersaurus or a slightly more inclusive clade . Labiolingually asymmetrical enamel, reduced crown volume, increased replacement rate, and the development of tooth batteries evolved independently in two other dinosaur clades: iguanodontian ornithopods  and ceratopsian marginocephalians . The repeated evolution of these features together may represent an adaptation to herbivory at large body size and within the context of polyphyodonty, though several important differences in the evolution of these features exist as well .
Sauropods were obligate herbivores, but their antecedents were omnivorous –. The origin and early evolution of sauropods involved increases in tooth volume  and body size . Although herbivory and extremely large body size persisted among the vast majority of sauropods, multiple lineages drastically reduced the volume of functional crowns . The repeated independent evolution of narrow crowns suggests that they conferred an adaptive advantage over broad crowns during the second half of sauropod evolution. By the Late Cretaceous, only narrow-crowned sauropod taxa remained , . Additionally, following the disappearance of diplodocoids from the fossil record in the early Late Cretaceous, tooth crowns in titanosauriforms decreased in volume and breadth until they were similar in size and shape to those of diplodocoids . Sauropods with broad-crowned teeth (e.g., Camarasaurus) evolved tooth replacement rates on par with those of ornithischian herbivores that persisted into the latest Cretaceous, and each Camarasaurus tooth was more resistant to wear than smaller teeth by virtue of their larger volume and thicker enamel. Why then did several neosauropod lineages develop narrow-crowned teeth?
One explanation is that fresh teeth are more effective than worn teeth. Replacing a tooth every month reduces the number of excessively worn crowns in the functional dentition, which prolongs contact with opposing teeth and with food. Additionally, although individual teeth were being replaced more frequently, the smaller crown volume results in a lower rate of mineralized tissue production and loss – narrow-crowned taxa had to recoup around 10% of the crown volume of dental tissue that was required in their larger-crowned relatives per tooth replaced. Furthermore, the narrow crowns of Diplodocus are made up of a larger proportion of enamel to dentin than the broad crowns of Camarasaurus. The advent of narrow-crowned dentition therefore enabled the animal to have many more fresh teeth at any given time, while losing far less mineralized tissue. Furthermore, smaller, more slender teeth would have allowed for smaller tooth roots (Fig. 2) and smaller and lighter cranial bones, resulting in a lighter skull overall. A small head-to-body volume ratio sets sauropods apart from other dinosaurian herbivores .
In a finite element analysis of the skull of Diplodocus, Young et al.  identified high stresses at the bases of teeth that would have been incurred during branch stripping or other feeding strategies. In the context of those results, they interpreted high tooth replacement rates in Diplodocus as an adaptation that would have accommodated increased levels of tooth breakage. Aside from concerns that tooth breakage is maladaptive, producing ineffective and infection-prone teeth, we briefly discuss one testable consequence of the Young et al. hypothesis. If Diplodocus and other narrow-crowned sauropods experienced tooth breakage as a result of branch stripping or static biting, then the fossil record should bear evidence of such failure. Although the record of cranial remains is sparse for sauropods, it is relatively good for Diplodocus and other narrow-crowned sauropods, and we know of no evidence of jaws preserving teeth broken in life.
Rather than being related to high levels of tooth breakage, we propose that increased replacement rates are related to increased wear rates that may have been a consequence of a shift in diet , . Some narrow-crowned taxa (e.g., Diplodocus) were likely low-browsers , , , , , a behavior that leads to increased ingestion of abrasive exogenous grit . The sauropod most highly specialized for low browsing, Nigersaurus, also has the highest known replacement rate of any dinosaur. In contrast, sauropods with broader tooth crowns and slower replacement rates, such as Mamenchisaurus and Camarasaurus, are thought to have been mid- to upper-canopy browsers , , , , , , , where exogenous grit levels are expected to be lowest.
Tooth replacement rate, size, and shape data indicate that despite their somewhat stereotyped body plan and large body size, sauropod dinosaurs exhibited varied approaches to feeding. The coexisting but morphologically disparate and distantly related Late Jurassic sauropods Camarasaurus and Diplodocus differed greatly in their anatomy related to food acquisition: Camarasaurus had a large volume of broad-crowned teeth that were replaced relatively slowly, whereas Diplodocus had a small volume of narrow-crowned teeth that were replaced very quickly. This variety represents a potential factor that allowed multiple gigantic species such as Camarasaurus and Diplodocus to partition the same ecosystem. The repeated evolution of narrow-crowned teeth in sauropods appears to have been accompanied by an increase in tooth replacement rate, which would have equipped these forms with less worn teeth over their lifetimes and allowed their skulls to be lighter.
Microsoft Excel spreadsheet containing tooth volumes, crown volumes, enamel thicknesses, tooth lengths, and estimation method for tooth replacement rate for various sauropodomorphs investigated in this study.
CT-generated movie of the premaxilla of Camarasaurus (UMNH 5527) in mesiodistal view (see separate.mov file)
CT-generated movie of the premaxilla of Camarasaurus (UMNH 5527) in apicobasal view (see separate.mov file).
CT-generated movie of the premaxilla of Diplodocus (YPM 4677), with bone rendered transparent and teeth opaque (see separate.avi file).
We thank J. Gauthier, W. Joyce, D. Brinkman (YPM), M. Getty (UMNH), P. M. Sander (U. Bonn), R. Schoch (Staatliches Museum für Naturkunde) and R. Smith (Iziko South African Museum) for loan assistance and permission to sample specimens. Thanks to W. Sanders (University of Michigan Museum of Paleontology) for preparation, Dr. C. Blane, K. Schwarz, and K. Barber (Department of Radiology, University of Michigan Medical Center) for access and assistance with CT scanning. We thank Paul Upchurch (University College London) and Paul Tafforeau (European Synchrotron Radiation Facility) for critical comments that improved the manuscript.
Conceived and designed the experiments: MDD J. A. Whitlock J. A. Wilson. Performed the experiments: MDD J. A. Whitlock KMS. Analyzed the data: MDD J. A. Whitlock KMS DCF J. A. Wilson. Contributed reagents/materials/analysis tools: MDD KMS DCF J. A. Wilson. Wrote the paper: MDD J. A. Whitlock KMS DCF J. A. Wilson.
- 1. Owen-Smith RN (1992) Megaherbivores: the influence of very large body size on ecology. Cambridge: Cambridge University Press. 388 p.
- 2. Sues H-D, Reisz RR (1998) Origins and early evolution of herbivory in tetrapods. Trends in Ecology and Evolution 13: 141–145.
- 3. Erickson GM, Krick BA, Hamilton M, Bourne GR, Norell MA, et al. (2012) Complex dental structure and wear biomechanics in hadrosaurid dinosaurs. Science 338: 98–101.
- 4. Teaford FT, Smith MM, Ferguson MWJ (2000) Development, Function and Evolution of Teeth. Cambridge, UK: Cambridge University Press. 314 p.
- 5. Sereno PC, Wilson JA (2005) Structure and evolution of a sauropod tooth battery. In: Curry Rogers KA, Wilson JA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. 157–177.
- 6. Sereno PC, Wilson JA, Witmer LM, Whitlock JA, Maga A, et al. (2007) Structural extremes in a Cretaceous dinosaur. PLoS ONE 2: e1230.
- 7. Richman JM, Whitlock JA, Abramyan J (2013) Regeneration of reptile teeth. In: Huang GT-J, Thesleff I, editors. Stem cells in craniofacial development, regeneration and repair. Hoboken: Wiley-Blackwell. 135–151.
- 8. White TE (1959) The endocrine glands and evolution, no. 3: os cementum, hypsodonty, and diet. Contributions from the Museum of Paleontology, University of Michigan 13: 211–265.
- 9. Damuth J, Janis CM (2011) On the relationship between hypsodonty and feeding ecology in ungulate mammals, and its utility in palaeoecology. Biological Reviews 86: 733–758.
- 10. Chure DJ, Britt BB, Whitlock JA, Wilson JA (2010) First complete sauropod dinosaur skull from the Cretaceous of the Americas and the evolution of sauropod dentition. Naturwissenschaften 97: 379–391.
- 11. Strömberg CAE (2006) Evolution of hypsodonty in equids: testing a hypothesis of adaptation. Paleobiology 32: 236–258.
- 12. Erickson GM (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 93: 14623–14627.
- 13. Erickson GM (1996) Daily deposition of dentine in juvenile Alligator and assessment of tooth replacement rates using incremental line counts. Journal of Morphology 228: 189–194.
- 14. Ganse B, Stahn A, Stoinski S, Suthau T, Gunga HC (2011) Body mass estimation, thermoregulation and cardiovascualr physiology of large sauropods. In: Klein N, Remes K, Sander PM, editors. Biology of the sauropod dinosaurs: understanding the life of giants. Bloomington: Indiana University Press. 105–115.
- 15. Paladino FV, Spotila JR, Dodson P (1997) A blueprint for giants: modeling the physology of large dinosaurs. In: Farlow JO, Brett-Surman MK, editors. The Complete Dinosaur. Bloomington: Indiana University Press. 491–504.
- 16. Spotila JR, Lommen PW, Bakken GS, Gates DM (1973) A mathematical model for body temperatures of large reptiles: implications for dinosaur biology. The American Naturalist 107: 391–404.
- 17. Upchurch P, Barrett PM, Dodson P (2004) Sauropoda. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. 259–324.
- 18. Upchurch P, Barrett PM (2000) The evolution of sauropod feeding mechanisms. In: Sues HD, editor. Evolution of Herbivory in Terrestrial Vertebrates – Perspectives from the Fossil Record. Cambridge: Cambridge University Press. 79–122.
- 19. Wilson JA, Sereno PC (1998) Early evolution and higher-level phylogeny of sauropod dinosaurs. Journal of Vertebrate Paleontology Society of Vertebrate Paleontology Memoir 1–68.
- 20. Whitlock JA (2011) Inferences of diplodocoid (Sauropoda: Dinosauria) feeding behavior from snout shape and microwear analyses. PLoS ONE 6(4): e18304.
- 21. Rasband WS (1997–2009) ImageJ. Bethesda: US National Institutes of Health.
- 22. Abramoff M, Magelhaes P, Ram S (2004) Image processing with ImageJ. Biophotonics International 11: 36–42.
- 23. Rountrey A (2009) Life histories of juvenile wooly mammoths from Siberia: stable isotope and elemental analyses of tooth dentin. Ann Arbor: University of Michigan.
- 24. Carlson SJ (1990) Vertebrate dental structures. In: Carter J, editor. Skeletal Biomineralization: Patterns, Processes and Evolutionary Trends. New York: Van Nostrand Reinhold. 531–536.
- 25. Smith T, Reid DJ, Sirianni J (2006) The accuracy of histological assessments of dental development and age at death. Journal of Anatomy 208: 125–138.
- 26. Fitzgerald C (1998) Do enamel microstructures have regular time dependencies? Conclusions from the literature and a large scale study. Journal of Human Evolution 35: 371–386.
- 27. Scheyer TM, Moser M (2011) Survival of the thinnest: rediscovery of Bauer’s (1898) ichthyosaur tooth sections from Upper Jurassic lithographic limestone quarries, south Germany. Swiss Journal of Geosciences 104 (Suppl 1)S147–S157.
- 28. Hughes SW (2006) Archimedes revisited: a faster, better, cheaper method of accurately measuring the volume of small objects. Physics Teacher 40: 468–474.
- 29. Holland WJ (1924) The skull of Diplodocus. Memoirs of the Carnegie Museum 9: 379–403.
- 30. Wilson JA (2002) Sauropod dinosaur phylogeny: critique and cladistic analysis. Zoological Journal of the Linnean Society 136: 217–276.
- 31. Sereno PC, Beck AL, Dutheil DB, Larsson HCE, Lyon GH, et al. (1999) Cretaceous sauropods from the Sahara and the uneven rate of skeletal evolution among dinosaurs. Science 286: 1342–1347.
- 32. Norman DB (2004) Basal Iguanodontia. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, Second Edition. Berkeley: University of California Press. 413–437.
- 33. Dodson P, Currie PJ (1990) Neoceratopsia. In: Weishampel DB, Dodson P, Osmólska H, editors. The Dinosauria, First Edition. Berkeley: University of California Press. 593–618.
- 34. Martínez RN (2009) Adeopapposaurus mognai, gen. et sp. nov (Dinosauria: Sauropodomorpha), with comments on adaptations of basal sauropodomorphs. Journal of Vertebrate Paleontology 29: 142–164.
- 35. Martínez RN, Alcober OA (2009) A basal sauropodomorph (Dinosauria: Saurischia) from the Ischigualasto Formation (Triassic, Carnian) and the early evolution of Sauropodomorpha. PLoS ONE 4: e4397.
- 36. Barrett PM (2000) Prosauropod dinosaurs and iguanas: speculations on the diets of extinct reptiles. In: Sues HD, editor. Evolution of herbivory in terrestrial vertebrates. Cambridge: Cambridge University Press. 42–78.
- 37. Barrett PM, Upchurch P (2007) The evolution of feeding mechanisms in early sauropodomorph dinosaurs. Special Papers in Palaeontology 77: 91–112.
- 38. Yates AM (2004) Anchisaurus polyzelus (Hitchcock): the smallest known sauropod dinosaur and the evolution of gigantism among sauropodomorph dinosaurs. Postilla 230: 1–58.
- 39. Barrett PM, Upchurch P (2005) Sauropodomorph diversity through time: paleoecological and macroevolutionary implications. In: Wilson JA, Curry Rogers KA, editors. The sauropods: evolution and paleobiology. Berkeley: University of California Press. 125–152.
- 40. Young MT, Rayfield E, J., Holliday CM, Witmer LM, Button DJ, et al. (2012) Cranial biomechanics of Diplodocus (Dinosauria, Sauropoda): testing hypotheses of feeding behaviour in an extinct megaherbivore. Naturwissenschaften 99: 637–647.
- 41. Stevens KA, Parrish JM (1999) Neck posture and feeding habits of two Jurassic sauropod dinosaurs. Science 284: 798–800.
- 42. Stevens KA, Parrish JM (2005) Neck posture, dentition, and feeding strategies in Jurassic sauropod dinosaurs. In: Tidwell V, Carpenter K, editors. Thunder–lizards: the sauropodomorph dinosaurs. Bloomington: Indiana University Press. 212–232.
- 43. Ungar PS (1996) Dental microwear of European Miocene catarrhines: evidence for diets and tooth use. Journal of Human Evolution 31: 335–366.
- 44. Fiorillo AR (1991) Dental microwear on the teeth of Camarasaurus and Diplodocus: implications for sauropod paleoecology. In: Kielan–Jaworowska Z, Heintz N, Nakrem H, editors. Fifth Symposium on Mesozoic Terrestrial Ecosystems and Biota. Oslo: Paleontological Museum, University of Oslo. 23–24.
- 45. Fiorillo AR (1998) Dental microwear patterns of the sauropod dinosaurs Camarasaurus and Diplodocus: evidence for resource partitioning in the Late Jurassic of North America. Historical Biology 13: 1–16.
- 46. Whitlock JA (2011) A phylogenetic analysis of the Diplodocoidea (Saurischia: Sauropoda). Zoological Journal of the Linnean Society 161: 872–915.
- 47. Ouyang H, Ye Y (2002) The first mamenchisaurian skeleton with complete skull: Mamenchisaurus youngi. Chengdu: Sichuan Science and Technology Press. 111 pp. p.
- 48. Coria RA, Chiappe LM (2001) Tooth replacement in a sauropod premaxilla from the Upper Cretaceous of Patagonia, Argentina. Ameghiniana 38: 463–466.
- 49. Allain R, Aquesbi N (2008) Anatomy and phylogenetic relationships of Tazoudasaurus naimi (Dinosauria, Sauropoda) from the late Early Jurassic of Morocco. Geodiversitas 30: 345–424.
- 50. Gallina PA, Apesteguía S (2011) Cranial anatomy and phylogenetic position of the titanosaurian sauropod Bonitasaura salgadoi. Acta Palaeontologica Polonica 56: 45–60.