Evolution of high tooth replacement rates in theropod dinosaurs
Authors:
Michael D. D’Emic aff001; Patrick M. O’Connor aff003; Thomas R. Pascucci aff001; Joanna N. Gavras aff001; Elizabeth Mardakhayava aff001; Eric K. Lund aff003
Authors place of work:
Department of Biology, Adelphi University, Garden City, New York, United States of America
aff001; Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York, United States of America
aff002; Department of Biomedical Sciences, Ohio University, Athens, Ohio, United States of America
aff003; Ohio Center for Ecology and Evolutionary Studies, Athens, Ohio, United States of America
aff004; Department of Biological Sciences, North Carolina Museum of Natural Sciences, Raleigh, North Carolina, United States of America
aff005
Published in the journal:
PLoS ONE 14(11)
Category:
Research Article
doi:
https://doi.org/10.1371/journal.pone.0224734
Summary
Tooth replacement rate is an important contributor to feeding ecology for polyphyodont animals. Dinosaurs exhibit a wide range of tooth replacement rates, mirroring their diverse craniofacial specializations, but little is known about broad-scale allometric or evolutionary patterns within the group. In the current broad but sparse dinosaurian sample, only three non-avian theropod tooth replacement rates have been estimated. We estimated tooth formation and replacement rates in three additional non-avian theropod dinosaurs, the derived latest Cretaceous abelisaurid Majungasaurus and the more generalized Late Jurassic Allosaurus and Ceratosaurus. We created the largest dental histological and CT dataset for any theropod dinosaur, sectioning and scanning over a dozen toothed elements of Majungasaurus and several additional elements from the other two genera. Using this large sample, we created models of tooth formation time that allow for theropod replacement rates to be estimated non-destructively. In contrast to previous results for theropods, we found high tooth replacement rates in all three genera, with Allosaurus and Ceratosaurus rates of ~100 days and 56 days for Majungasaurus. The latter rate is on par with those of derived herbivorous dinosaurs including some neosauropods, hadrosaurids, and ceratopsians. This elevated rate may be a response to high rates of tooth wear in Majungasaurus. Within Dinosauria, there is no relationship between body mass and tooth replacement rate and no trends in replacement rate over time. Rather, tooth replacement rate is clade-specific, with elevated rates in abelisaurids and diplodocoids and lower rates in coelurosaurs.
Keywords:
Phylogenetics – Teeth – Computed axial tomography – Dentition – Theropoda – Herbivory – Dinosaurs – Sauropoda
Introduction
Tooth formation time and replacement rate are related to feeding mechanics and diet and can help reconstruct paleoecology and paleodemography [1–3]. Controls on tooth formation and replacement rates in relation to body mass, feeding ecology, and phylogeny, especially regarding the loss of teeth on the lineage leading to birds, remain debated [4,5]. Tooth formation and replacement rates have been measured empirically in a variety of extant taxa; in these groups, counts of incremental lines of von Ebner within dentine of successive teeth in a tooth socket can be used to estimate such rates ([1,6]. Based on data from nine species, Erickson [1] found that both tooth formation time in Dinosauria, and tooth replacement rate in Theropoda, were negatively correlated with tooth volume, suggesting that structural or physiological limits on odontoblast activity constrained the rate of tooth growth regardless of tooth size or body mass. Erickson [1] also estimated that the three carnivorous (theropod) dinosaurs in his sample had tooth replacement rates on the order of several months to years, whereas the herbivorous dinosaurs had tooth replacement rates on the order of 2–3 months.
An explosion in the number of described dinosaur taxa over the last two decades has expanded the range of dental and craniofacial morphologies known in the clade, prompting reevaluation of hypotheses explaining tooth formation and replacement times with a larger sample size and increased taxonomic breadth. To do this, we established a rich histological and tomographic dental and craniofacial dataset of the carnivorous dinosaur Majungasaurus crenatissimus, which has an apomorphic anteroposteriorly short and dorsoventrally tall skull with abbreviated tooth crowns relative to most other theropods ([7]. This is the largest such dataset for a Mesozoic dinosaur, allowing us to also investigate allometric and intraspecific variation within Majungasaurus. We also collected similar but smaller datasets for the non-avian theropods Allosaurus and Ceratosaurus to both contextualize our findings in Majungasaurus and better examine phylogenetic and allometric trends and possible constraints on odontogenesis across Dinosauria. By examining these trends, we test the hypothesis that carnivorous dinosaurs had lower tooth replacement rates than herbivorous ones as found by Erickson [1].
Methods
We CT scanned 52 isolated Majungasaurus teeth and 15 Majungasaurus tooth-bearing elements at Stony Brook University Hospital that are accessioned at the Field Museum of Natural History, Chicago, USA (FMNH), Université d’Antananarivo, Antananarivo, Madagascar (UA), Stony Brook University (MAD, Madagascar Collection), or Denver Museum of Nature and Science (DMNH) (see S1 Fig and Morphobank project P322 or Morphosource project 848 for specimen numbers). We scanned 11 Allosaurus (Museum of Paleontology, Brigham Young University, Provo, Utah (BYU), BYU 8901, 2028) and one Ceratosaurus (BYU 12893) tooth-bearing element(s) at Orem Community Hospital. We measured 104, 32, and 6 apicobasal tooth lengths based on these CT data for Majungasaurus, Allosaurus, and Ceratosaurus, respectively. Linear measurements of the Majungasaurus teeth were taken according to the approach utilized in Smith [8]; volumes of isolated teeth were measured by water displacement (S1 File).
We thin sectioned 19 of the CT scanned Majungasaurus teeth, one Ceratosaurus tooth (Museum of Western Colorado, Grand Junction, Colorado (MWC), MWC 1), and one Allosaurus tooth (BYU 2028) according to standard paleohistological techniques [9]. Specimens were embedded in epoxy resin, bisected in the mesiodistal plane, ground with 600 grit sandpaper, mounted to glass slides with cyanoacrylate, cut to ca. 0.5 mm, and sanded again using 600 and then 1200 grit sandpaper to a thickness of ca. 100 μm. Poor preservation of incremental lines left us able to only measure incremental line thicknesses in 13 Majungasaurus teeth and estimate tooth age in only five. Thin sections were stitched at 5x or 20x using a Zeiss Axioimager Z2 system running Zen2 software. We measured incremental line thicknesses and counted incremental lines on these stitched images to obtain individual tooth formation times (interpolating for lines that were diagenetically altered; see Morphobank Project 3222, Morphosource Project 848 and S1 File).
Some studies [10,11] have questioned previous interpretation of incremental lines of von Ebner in dinosaurs, instead suggesting that they represent higher-order increments with implied absence of daily lines due to preservation issues. We refute this hypothesis with two lines of evidence: first, the ca. 10–20 μm mean thicknesses of the dinosaurian daily incremental lines is on par with those found via labeling studies of extant archosaurs [6,12]; second, if these were higher order increments such as Andresen lines, they would imply tooth formation and replacement times 7–14 times longer than those previously estimated based on body mass [13]. These augmented times would be biologically unreasonable (e.g., 3.5–7 years to form a single Diplodocus tooth or 15–30 years to replace a single T. rex tooth). Therefore, we continue to interpret ca. 10–20 μm thick increments in dentine as daily incremental lines of von Ebner in archosaurs.
For Majungasaurus, we regressed total tooth length (measured parallel to the distal margin) versus tooth formation time to allow for prediction of formation time in teeth that could not be thin sectioned. We used PAST3 [14] to compare the fit of nine regression models to Majungasaurus data collected herein using Akaike’s information criterion corrected for small sample size (AICc; see S1 File for values). We also fit these nine models and compared AICc scores for previously published Diplodocus and Camarasaurus data [2]. A power model fit the data best for Majungasaurus, a Gaussian model fit the data best for Camarasaurus, and both quadratic and Logistic models fit equally well for Diplodocus (AICc values only differed by ~1). We follow D’Emic et al. [2] in using a quadratic model to describe tooth age-length relationships on theoretical grounds: tooth growth should be rapid in the apicobasal direction at first, as odontoblast apposition is more parallel to the direction of tooth extension, and then slow as the direction of apposition becomes more perpendicular to the overall direction of tooth growth. Furthermore, the Camarasaurus and Majungasaurus data overlap (see Results below), suggesting that a single model should describe their growth–length relationship. However, AICc values favor different models of tooth growth, which is more likely a statistical artifact related to the limited sample sizes involved. The quadratic Majungasaurus regression model was used to estimate tooth age based on the CT data of dentigerous elements for Majungasaurus, Ceratosaurus, and Allosaurus, justified by the similar proportions of these teeth.
Tooth formation time, replacement rate, and incremental line thicknesses for other dinosaurian taxa were gathered from the literature [1,2,15,16]. We plotted tooth replacement rates on a phylogeny with branch lengths compiled from the literature [17]; only adult values were used because tooth replacement rates change over ontogeny [1,6]. Branch lengths were based on specimen geologic ages and assigned using the R code provided by Graeme Lloyd (http://www.graemetlloyd.com/methdpf.html). No geologic age was available for the titanosaur premaxilla included in the dataset; for our analysis it was estimated as 83 Ma based on its reported “Upper Cretaceous” provenance [18]. This specimen was omitted from regressions because it was not possible to estimate its body mass, so sensitivity analysis surrounding its geologic age was unnecessary. We regressed incremental line width and then tooth replacement rate on ln(body mass), both with and without accounting for phylogenetic influence following the methods and using the R code provided in D’Emic et al. [19]. The R code, raw data, phylogenetic tree, and branch lengths used herein are provided in S2–S6 Files. Again, only adult values were used to avoid confounding ontogenetic factors. Body masses were estimated using stylopodial limb circumferences and the equations presented in Campione and Evans [20] and Campione et al. [21]; circumferences were sourced from Benson et al. [17] or personally measured by the first author. Because a humeral circumference is not available for Patagosaurus, we estimated its humeral circumference as 578 mm based on the ratio in the closely related Cetiosaurus oxoniensis, yielding an estimated body mass of 27,221 kg. We assessed the sensitivity of our regressions to this coarse estimate by re-running the analysis with 50% larger and smaller values for Patagosaurus (i.e., using 13,612 kg or 40,832 kg as its body mass estimate).
Results
New theropod data
The total volume of the sectioned Ceratosaurus tooth (MWC 1, a posterior maxillary or dentary tooth) is 1.1 ml, its preserved length is 40 mm, and its mesiodistal dimension is 13 mm. The Allosaurus tooth was incomplete and so these measurements are not available. The crown height and mesiodistal length of a mid-dentary crown of Majungasaurus are 26 and 13.5 mm, respectively [8]. We take this as an approximate mean size for the functional dentition following Erickson [1,6]. Isolated Majungasaurus teeth similar in size to this have volumes of about 3 ml as measured by water displacement (Electronic Supplementary Material), which we use for our mean Majungasaurus tooth volume.
Majungasaurus has incremental line thicknesses (mean and standard deviation: 18 +/- 5 μm) within the range of those reported by Erickson [1] and D’Emic et al. [2] for other archosaurs, whereas those of Allosaurus were slightly thicker (23 +/-1 μm) and those of Ceratosaurus were slightly thinner (14 +/- 3 μm; Fig 1). The largest estimated tooth formation times for these three genera are estimated as 293 (Majungasaurus), 359 (Allosaurus), and 337 days (Ceratosaurus), which is on par with tooth formation times in sauropod dinosaurs with similar tooth size [2]. CT data reveal that successive generations of replacement teeth are more similar in size in Majungasaurus than in Allosaurus or Ceratosaurus. Using the length-tooth age model developed below to predict tooth age from tooth length measured in CT slices, replacement rates for these three genera are estimated at 56, 104, and 107 days, respectively.
Models of tooth formation time
Thin sections of Majungasaurus teeth reveal a tight relationship between tooth apicobasal length and tooth age as measured by counting daily deposited incremental lines of von Ebner (Fig 2; r2 = 0.95; p = 0.05). Interestingly, the relationship is nearly identical to that obtained for Camarasaurus [2]; however, it is substantially different than the relationship for Diplodocus (Fig 2). This is likely because Majungasaurus and Camarasaurus have teeth of similar aspect ratio (slenderness index [SI] = crown length:crown mesiodistal length ca. 1.9; Electronic Supplementary Material; [22]), whereas Diplodocus has much narrower crowns (SI = 5.2; [22]).
Allometric and Phylogenetic patterns
In dinosaurs, incremental line width is unrelated to body mass (OLS regression: r2 = 0.28; p = 0.07), as is tooth formation time (r2 = 0.008; p = 0.72). No relationship between body mass and tooth replacement rate was detected whether or not phylogenetic information was included in the regression (Fig 3; OLS regression: r2 = 0.024; p = 0.54; PGLS regression: lambda ~ 1). This relationship was still not significant when only herbivores were included in the regression (OLS: r2 = 0.53; p = 0.07). Uncertainly surrounding our body mass estimate for Patagosaurus is immaterial to the results: increasing or decreasing its body mass estimate by 50% does not meaningfully alter the significance, strength (i.e., r value) or direction of any of our regression results.
We infer approximately monthly tooth replacement rates as the ancestral dinosaurian condition (Fig 3B), though this should be viewed as a preliminary estimate until better sampling is conducted near the base of the tree. Coelurosaurs and diplodocoids have unusually slow and fast replacement rates, respectively (Fig 3). Even excluding these two groups, there is no relationship between body mass and replacement rate (r2 = 0.12; p = 0.27). Carnivores have significantly lower absolute tooth replacement rates than do herbivores (t test: p < 0.001; Mann-Whitney U test: p = 0.001). In dinosaurs, feeding ecology is a better predictor of tooth replacement rate than is body mass.
Discussion and conclusions
We established a novel dataset to address relationships among tooth formation time, tooth replacement rate, and body mass in an expanded dinosaurian sample, including the largest sample of individuals for any single dinosaur species (Majungasaurus). This allowed us to develop tooth age-length models in an aim to estimate tooth formation and replacement rates in a non-destructive way. In the future, novel CT data for additional dinosaur species can be used with our models to estimate tooth formation and replacement rates, refining when, where, and in precisely which clades elevated tooth replacement rates evolved. Increased histological sampling is necessary to test that the tooth age-length models developed for Camarasaurus, Majungasaurus, and Diplodocus are valid for a wide variety of dinosaurs with teeth of similar aspect ratio to those of these genera.
Our expanded sample supports the finding of Erickson [1] that structural or physiological limitations on dentine production rate by odontoblasts affect both tooth generation and replacement rates. Incremental line thickness does not increase with body mass, instead hovering around a relatively consistent ~10–20 μm. This further supports the concept that there may indeed be a biological limit on odontogenesis that requires other evolutionary innovations to overcome increased selection pressures imposed by faster rates of tooth wear, such as the development of tooth batteries in some ornithischian and sauropod dinosaurs [1,23] or the evolution of ever-growing teeth as in some groups of mammals [24].
All carnivorous dinosaurs in our sample replaced their teeth more slowly than the herbivorous dinosaurs with the exception of Majungasaurus, which has tooth replacement rates comparable to those of broad-toothed sauropods and dental-battery bearing ceratopsians and hadrosaurids. Tooth replacement rate is intrinsically controlled at the individual level and does not respond to increased wear or breakage [25]; instead, tooth replacement rate is a general reflection of dietary specialization [1,3,6]. The generally slower replacement rate for theropods versus herbivores likely reflects their softer foodstuffs and/or release from the necessity of fast tooth replacement via adaptations against tooth breakage or rapid wear [3]. In contrast, the elevated, herbivore-like rate for the carnivorous Majungasaurus perhaps reflects its osteophageous behavior, evidenced by extensive tooth markings on both herbivores and conspecifics in the Maevarano Formation [26]. We hypothesize that elevated tooth replacement rates characterize at least some other abelisaurids, which have maxillae “packed with replacement teeth” (Sereno and Brusatte [27]:20); by extension, perhaps osteophageous behavior also applies to these species. Tyrannosaurus rex likely exhibited osteophageous behavior, but likely took a different evolutionary approach compared to Majungasaurus and perhaps other abelisaurids, evolving exceedingly robust teeth and slow replacement rates [1,28]. These disparate approaches to increased consumption of harder foodstuffs in theropods seem to mirror the evolution of broad-crowned, faster replacing, vs. narrow-crowned, slower-replacing teeth in sauropods [1].
Supporting information
S1 Fig [tif]
Labeled image of surface models showing specimen numbers for CT scanned isolated teeth.
S1 File [xlsx]
Excel spreadsheet with gross tooth measurements for , dinosaur incremental line thicknesses, input data for the tooth age-length model, estimated tooth formation times and replacement rates, and regression data.
S2 File [r]
R code to perform analyses.
S3 File [csv]
ln(tooth replacement rates) in several dinosaurs.
S4 File [txt]
Branch lengths (in millions of years) for calibrating phylogeny.
S5 File [txt]
ln(body mass) and ln(tooth replacement rates) in several dinosaurs (.txt file) for regression.
S6 File [nex]
Phylogenetic tree (.nex file) for use in R code.
Zdroje
1. Erickson GM. Incremental lines of von Ebner in dinosaurs and the assessment of tooth replacement rates using growth line counts. Proc Nat Acad Sci. 1996a;93: 14623–14627.
2. D’Emic MD, Whitlock JA, Smith KM, Fisher DC, Wilson JA. Evolution of high tooth replacement rates in sauropod dinosaurs. PLoS ONE 2013a;8: e69235.
3. Brink KS, Reisz RR, LeBlanc ARH, Chang RS, Lee YC, Chiang CC, Huang T, Evans DC. Developmental and evolutionary novelty in the serrated teeth of theropod dinosaurs. Sci Rep. 2015;5: 12338 doi: 10.1038/srep12338 26216577
4. Button K, You H, Kirkland J, Zanno L. Incremental growth of therizinosaurian dental tissues: implications for dietary transitions in Theropoda. PeerJ. 2017;5: e4129. doi: 10.7717/peerj.4129 29250467
5. Zhou YC, Sullivan C, Zhang FC. Negligible effect of tooth reduction on body mass in Mesozoic birds. Vert. PalAs.; 2019: 57: 38–50.
6. Erickson GM. Daily deposition of dentine in juvenile Alligator and assessment of tooth replacement rates using incremental line counts. J Morph. 1996b;228: 189–194.
7. Sampson SD, Witmer LM. Craniofacial anatomy of Majungasaurus crenatissimus (Theropoda: Abelisauridae) from the Late Cretaceous of Madagascar. J Vert Paleo. Mem. 2007;8: 32–102.
8. Smith JB. Dental morphology and variation in Majungasaurus crenatissimus (Theropoda: Abelisauridae) from the Late Cretaceous of Madagascar. J Vert Paleo Mem. 2007;8: 103–126.
9. Padian K, Lamm ET. Bone Histology of Fossil Tetrapods: Advancing Methods, Analysis and Interpretations. University of California Press; 2013.
10. Scheyer TM, Moser M. Survival of the thinnest: rediscovery of Bauer’s (1898) ichthyosaur tooth sections from Upper Jurassic lithographic limestone quarries, south Germany. Swiss J Geosci. 2011;104 (Suppl 1), S147–S157.
11. Dumont M, Tafforeau P, Bertin T, Bhullar B.-A. Field D, Schulp A, Strilisky B, Thivichon-Prince B, Viriot L, Louchart A. 2016 Synchrotron imaging of dentition provides insights into the biology of Hesperornis and Ichthyornis, the “last” toothed birds. BMC Evo Bio. 2016;16: 1–28.
12. Mishima H, Iwasa Y, Yokota R, Elsey RM. The short-period incremental lines in dentin of Alligatoridae teeth. In: Kobayaski I, Ozawa H, editors. Biomineralization (BIOM2001): formation, diversity, evolution and application, Proceedings of the 8th International Symposium on Biomineralization Tokai University Press, Kanagawa, 2003. pp. 317–320.
13. Bromage TG, Lacruz RS, Hogg R, Goldman HM, McFarlin SC, Warshaw J, Dirks W, Perez-Ochoa A, Smolyar I, Enlow DH, Boyde A. Lamellar bone is an incremental tissue reconciling enamel rhythms, body size, and organismal life history. Calcif Tiss Int. 2009;84: 388–404.
14. Hammer Ø., Harper DAT, Ryan PD. 2001. PAST: Paleontological statistics software package for education and data analysis. Palaeont Elect 2001;4: 1–9.
15. Kosch JCD, Schwarz-Wings D, Fritsch G, Issever AS. Tooth replacement and dentition in Giraffatitan brancai. J Vert Paleo, Programs and Abstracts, 2014; 162.
16. Schwarz D, Kosch JCD, Fritsch G, Hildebrandt T. Dentition and tooth replacement of Dicraeosaurus hansemanni (Dinosauria, Sauropoda, Diplodocoidea) from the Tendaguru Formation of Tanzania, J Vert Paleo, 2015;35: e1008134.
17. Benson RBJ, Campione NE, Carrano MT, Mannion PD, Sullivan C, Upchurch P, Evans D. Rates of dinosaur body mass evolution indicate 170 million years of sustained ecological innovation on the avian stem lineage. PLoS Biol. 2014;12, 1001853.
18. Coria RA, Chiappe LM. Tooth replacement in a sauropod premaxilla from the Upper Cretaceous of Patagonia, Argentina. Ameghin. 2001;38: 463–466.
19. D’Emic MD, Mannion PD, Upchurch P, Benson RBJ, Pang Q, Cheng Q. Osteology of Huabeisaurus allocotus (Sauropoda: Titanosauriformes) from the Upper Cretaceous of China. PLoS ONE 2013b;8: e69375.
20. Campione NE, Evans DC. A universal scaling relationship between body mass and proximal limb bone dimensions in quadrupedal terrestrial tetrapods. BMC Biol. 2012;10: 1–21. doi: 10.1186/1741-7007-10-1 22214525
21. Campione NE, Evans DC, Brown CM, Carrano MT. Body mass estimation in non-avian bipeds using a theoretical conversion to quadruped stylopodial proportions. Methods Ecol Evol. 2014;5: 913–923.
22. Chure D, Brooks BB, Whitlock JA, Wilson JA. First complete sauropod dinosaur skull from the Cretaceous of the Americas and the evolution of sauropod dentition. Naturwiss. 2010;97: 379–391. doi: 10.1007/s00114-010-0650-6 20179896
23. Sereno PC, Wilson JA, Witmer LM, Whitlock JA, Maga A, Ide O, Rowe TA. Structural Extremes in a Cretaceous Dinosaur. PLoS ONE 2007; 2: e1230. doi: 10.1371/journal.pone.0001230 18030355
24. Renvoisé E, Michon F. An evo-devo perspective on ever-growing teeth in mammals and dental stem cell maintenance. Fron Phys 2014;5: 1–12.
25. Edmund AG. Tooth replacement phenomena in lower vertebrates. Royal Ontario Museum Life Science Division Contribution 1960;52: 1–190.
26. Rogers R, Krause DWK, Rogers KC. Cannibalism in the Madagascan dinosaur Majungatholus atopus. Nature 2003;422: 515–518. doi: 10.1038/nature01532 12673249
27. Sereno PC, Brusatte S. Basal abelisaurid and carcharodontosaurid theropods from the Lower Cretaceous Elrhaz Formation of Niger. Acta Palaeo Pol. 2008;53: 15–46.
28. Gignac P, Erickson GM. The biomechanics behind extreme osteophagy in Tyrannosaurus rex. J Vert Paleo, Programs and Abstracts, 2018; 134.
Článok vyšiel v časopise
PLOS One
2019 Číslo 11
- Metamizol jako analgetikum první volby: kdy, pro koho, jak a proč?
- Nejasný stín na plicích – kazuistika
- Masturbační chování žen v ČR − dotazníková studie
- Úspěšná resuscitativní thorakotomie v přednemocniční neodkladné péči
- Dlouhodobá recidiva a komplikace spojené s elektivní operací břišní kýly
Najčítanejšie v tomto čísle
- A daily diary study on maladaptive daydreaming, mind wandering, and sleep disturbances: Examining within-person and between-persons relations
- A 3’ UTR SNP rs885863, a cis-eQTL for the circadian gene VIPR2 and lincRNA 689, is associated with opioid addiction
- A substitution mutation in a conserved domain of mammalian acetate-dependent acetyl CoA synthetase 2 results in destabilized protein and impaired HIF-2 signaling
- Molecular validation of clinical Pantoea isolates identified by MALDI-TOF