In the collective imagination derived from scientific and popular literature, Triceratops often faced each other in combat. Thus, from the second half of the twentieth century, these ceratopsids were described as pugnacious animals. This arises primarily from the interpretation of extracranial fenestrae in ceratopsids being the result of combat trauma. However, the diagnosis of the traumatic nature of these anatomical variants of their neck frill requires evidence of bone healing and remodelling by microscopy analysis. Here, we present the case of the Triceratops horridus known as Big John, which is one of the largest specimens discovered in the Hell Creek Formation (Upper Cretaceous; South Dakota, USA). Its right squamosal bone shows an extrafenestra with irregular margins and signs of inflammation. Microscopy analysis revealed newly formed and healing bone, with histological signs typical of the bone remodelling phase. Chemical analysis revealed sulphur that was derived from glycosaminoglycan’s and sulphated glycoproteins of the preosseous osteoid substance present in the healing phases of a bone trauma. Histological and microanalytical analyses confirm that the squamosal fenestra of Big John is the result of a traumatic event, which might indeed have occurred during combat with another Triceratops.
The Late Cretaceous dinosaur Triceratops was characterised by its large neck frill, which predominantly consisted of the hyperelongated parietal and squamosal bones. It also had two large supraorbital horns and a smaller nasal horn. This cranial ornamentation of Triceratops probably served several functions. The evolutionary predecessors of ceratopsids had a relatively developed frill, while the horns, if present, were reduced to simple protuberances. The primitive function of the frill, therefore, was that of visual display and/or species recognition1.
The development of the solid frill and the long supraorbital horns during the evolution of ceratopsids such as Triceratops suggests that their function was to protect the cervical region of the skull from blows inflicted by individuals of the same species. Farke et al. stated that in Triceratops the horns not only had a visual function, but were also used in intraspecific combat2,3. Therefore, the cranial ornaments in Triceratops were used not only as a display, but also as a means of attack and defence against conspecifics3.
The specimen of Triceratops horridus known as Big John (due to its large size) was discovered in 2014 in the Upper Cretaceous Hell Creek Formation (South Dakota, USA), from where numerous remains of Ceratopsidae (Chasmosaurinae) have been recovered4,5,6 (see Supplementary Information). Big John has a fenestra on the right squamosal that completely perforates the bone (Fig. 1a,b). The presence of squamosal fenestrae has been documented for the chasmosaurines, which are usually unilateral and with variable shapes, from oval to circular. Their aetiology stimulated a debate that generated two hypotheses. The first hypothesis claims that squamosal fenestrae are of traumatic origin, probably as the result of intraspecific fighting or attacks by predators, such as Tyrannosaurus7,8. The second hypothesis argues that the squamosal fenestrae are not pathological, but are the result of bone resorption related to aging, or of bone removal for bone that was no longer necessary from a biomechanical and structural point of view9.
Macroscopic evidence of associated traumatic injuries, such as bone calli, radial fracture lines and displacement of bone fragments, should contribute to our understanding of whether these fenestrae are indeed traumatic lesions or are the outcome of other pathologies (e.g., infectious diseases). Histological analysis of the affected areas is a valuable tool for ascertaining the pathological nature of such lesions, to potentially exclude the fenestrae as taphonomic lesions or an anatomical variant linked to aging.
In modern mammals and reptiles, post-traumatic bone remodelling involves recruitment of osteogenic cells and activation of the molecular and chemical mechanisms that control the formation of soft calli that are rich in procollagen and proteoglycans, and their subsequent calcification10,11,12,13,14. The composition and distribution of the biochemical elements in the healing bone also changes during the healing process14,15,16,17. Consequently, the study of these factors can also provide useful information for diagnosis of the possible traumatic nature of these lesions.
Macroscopic and microscopic analyses of the squamosal fenestra of Big John
The fenestra on the right squamosal bone of Big John is shaped like a ‘keyhole’, with the widest part positioned caudally. The rostrocaudal length of the squamosal bone is 112 cm; the distance of the caudal border of the fenestra from the caudal apex of the squamosal is 75 cm; its rostrocaudal diameter and mediolateral width are 20 cm and 5 cm, respectively.
The lumen of this fenestra is partially filled with a ring of brownish material, which is particularly evident on the caudal and inferior edges (Fig. 1c). The bone surface around the fenestra is irregular and characterised by plaquelike depositions of reactive bone that could resulted from periostitis; i.e., a non-specific inflammatory process, which can be triggered by different stimuli (e.g., trauma, infection)18.
The histological analyses of a sample taken from the lower margin of the fenestra (Supplementary Fig. S1) provided information on the characteristics of the bone tissue near and distant from the edge of the squamosal opening. The optical and scanning electron miroscopy (SEM) images show that the bone tissue that delimits the fenestra was well vascularised, with primary osteons and osteocytic lacunae visible (Figs. 2, 3). At high magnification (× 400), the border shows areas of bone resorption, the morphology and dimensions of which are compatible with Howship lacunae, which are seen as eroded depressions of the bone surface due to the activity of osteoclasts (Howship lacunae mean diameter, 19.38 ± 2.25 μm) (Fig. 2b). Conversely, the bone tissue distant from the fenestra is characterised by its compact structure, with little vascularisation.
The dominant chemical elements in the bone sample seen under the electronic scanning field emission microscope equipped with a microanalysis system were oxygen (O), calcium (Ca) and phosphorus (P) (Supplementary Figs. S2, S3). The other elements seen were iron (Fe), sulphur (S), potassium (K), sodium (Na) and aluminium (Al), in smaller quantities and variously distributed, as well as traces of barium (Ba), strontium (Sr) and manganese (Mn). By focusing the microanalysis on the margin of the lesion, the presence of S was noted in the area that delimits the fenestra, with a distribution superimposable on that of Ca. The S is almost completely absent in the bone tissue distant from the lesion, where P, O and Na are the predominant elements (Fig. 4).
Macroscopy analysis of the bone surface that delimits the fenestra on the right squamosal bone of Big John show alterations that could be consequent to inflammatory processes18. In anatomical region where the periosteum is close to the skin surface, localized ossifying periostitis, sometimes accompanied by a lytic response, can be observed secondary to trauma12.
Histological and chemical analyses of the bone sample from the margin of the fenestra demonstrate that it consists of newly formed bone tissue that appears porous and disorganised, with numerous vascular canals and osteocytic lacunae (Figs. 2a, 3a), where layers of bone matrix that were undergoing mineralisation tend to fill the opening (Fig. 3b). At higher magnification, the margin of the bone tissue facing the lumen of the fenestra shows resorption areas, with morphology and dimensions that correspond to the Howship lacunae that are characteristic of the remodelling of human bone tissue (Fig. 2b)19. All of these histological characteristics are compatible with previously metabolically active and remodelling bone.
The specific cellular and molecular processes that occur during bone remodelling in modern reptiles and dinosaurs are not known in detail. Therefore, the reference interpretative models here are the physiology and biochemistry of healing bone tissue in mammals (including humans). Bone remodelling begins with a phase of bone resorption by osteoclasts. Through a combination of acid dissolution of the mineralised matrix and digestion of the organic matrix by proteolytic enzymes, small areas of bone resorption are formed (the so-called Howship lacunae); these are concave in shape and a few microns in diameter18,19. The bone resorption is followed by a phase of apposition of osteoid substance by the osteoblasts, which undergoes mineralisation through precipitation of calcium phosphate.
The main constituents of the mineralised bone matrix in new bone are Ca, O and P (which are typically present in calcium hydroxyapatite), and also S (Fig. 4). The phases of bone resorption and neoformation are separated by a transition phase, during which macrophage-like mononuclear cells deposit an initial layer of bone matrix that forms the cementing line that delimits the osteons20. This cementing line is rich in sulphated proteins21, which explains the presence of S among the elements that constitute bone during the mineralisation phase.
The distribution of S in repaired bone tissue might also be linked to glycosaminoglycan’s and glycoproteins in the osteoid substance, which is the preosseous substance found in ossification centres. Glycosaminoglycan’s contain sulphate and are essential for osteogenesis22,23,24. Baylink et al. demonstrated that the concentration of glycosaminoglycan’s and S are elevated in the osteoid substance, and then are reduced during the mineralisation process, as a result of enzymatic digestion10. The results of the studies carried out by Baylink were confirmed by Takagi et al., who showed a reduction in S in areas undergoing mineralisation and in the calcified matrix25. The removal of glycosaminoglycan’s and their sulphate compounds might be the prerequisite to the start of the calcification process of the osteoid substance. The SEM images in the present study showed the mineralisation front of the bone tissue in the remodelling phase, whereby the distribution map of the elements highlighted the presence of S in the areas that had still been occupied by the osteoid substance that had not yet calcified (Fig. 4).
The bone that was more distant from the margins of the lesion was mainly made up of bone matrix with few vascular channels and reduced numbers of osteocytic lacunae. These are histological characteristics that are compatible with compact bone tissue that has completed or almost completed the remodelling phase. In this region, moreover, there were lower amounts of S, which confirms the hypothesis of a gradual reduction in S during deposition of hydroxyapatite in the osteoid substance.
The edge of the lesion thus appeared to be made up of remodelling bone tissue undergoing mineralisation, as seen for both the light and dark areas of the histological preparations. Conversely, the innermost region that was more distant from the fenestra showed well mineralised bone or bone that was in an advanced state of mineralisation.
The results of the histological and chemical analyses show that the bone that circumscribed and partially filled the lesion had been made up of metabolically active and remodelling tissue (Figs. 2, 4). The fenestra is therefore of traumatic origin, and at the time of the death of Big John, the lesion was still healing.
The presence of newly formed bone and the histological characteristics of bone remodelling that was in progress excludes the possibilities that the lesion occurred post mortem (i.e., that it is of a taphonomic nature) and that the fenestra represented an anatomical variant. This conclusion is supported by the lack of regular, sharp and blunt margins for the lesion. Furthermore, although congenital squamosal fenestrae have been described for the subfamily of Chamsmosaurinae, they have not been found in Triceratops or Anchiceratops to date9. Instead, the lesion was possibly caused by the horn of another Triceratops. The mediolateral diameter (equal to 5 cm) and shape of the caudal region of the fenestra coincide with those of the apex of the supraorbital horns. Furthermore, the Triceratops used their horns in intraspecific combat3.
Farke hypothesised three models of engagement in the intraspecific combat of Triceratops2. The “single horn contact position” defines the contact that occurs between only one postorbital horn of each combatant, where lesions of the squamosal bone are inflicted by the nasal horn. In the “oblique horn locking position”, the skulls come into contact when they are slightly rotated with respect to each other, and contact occurs between both postorbital horns of both individuals. This model predicts lesions inflicted by the nasal horn in the rostral portion of both the parietals and squamosal’s. The third model of engagement is defined as “full horn locking”, which consists of the collision between the skulls when tilted at about 45° with respect to the horizontal plane, and involves contact between both postorbital horns of the opponents. This combat mode will result in injuries in the region of the temporal fenestra. The location of the lesion analysed here on the squamosal bone of Big John does not respect these predictive models of Farke for horn use in Triceratops2. It appears likely that the wound was instead inflicted from behind Big John (Supplementary Fig. S4), whereby the rival’s horn would have penetrated the frill and then slipped towards the rostrum, giving this lesion the shape of a keyhole. According to Aufderheide and Rodrìguez-Martìn26 pointed weapons could generate a perforating lesion with sharply-defined edges. The blow may also have caused comminution and loss of fragments and radiating fissures, that were hidden by bone remodelling in the months following the trauma. In describing his models on the trauma inflicted by the horns in the fighting between Triceratops, Farke did not exclude that there might also be other engagement dynamics besides those he hypothesised2.
Big John appears to have survived this trauma for some time. Two cases have been described in the literature where adult specimens of Centrosaurus survived extensive traumatic lesions to the skull9. However, it remains difficult to establish how long Big John survived following this trauma. Although the bone remodelling process can be first recognized in the third to fourth weeks after the trauma11, the healing times vary according to the species and to the extent of the trauma. Considering the healing times of traumatic injuries in modern reptiles, along with the size of the traumatic injury and the amount of bone repair, it is likely that the death of Big John occurred at least 6 months after this traumatic event27,28.
This study confirms the existence of intraspecific fighting in Triceratops. Furthermore, although the physiological and cellular mechanisms underlying the healing process in dinosaurs are still largely unknown, it would appear to be similar to those described in humans and mammals. Further histological and microanalytical investigations on fossil remains with traumatic lesions might shed light on the bone physiopathology of these reptiles.
Materials and methods
The histological sample of Triceratops horridus known as Big John is housed at Museum of the University “G. D’Annunzio” (Chieti, Italy) (access number 23751). The microscopy and histological analyses were performed on a bone sample taken from the inferior margin of the fenestra (Supplementary Data Fig. S1). The sample was analysed under stereo microscopy (Wild M8; Leica). The 30-μm-thick histological sections were made using a diamond-edged circular blade microtome (RMS-16G3; Reha-Tech Engineering). It was not possible to make thinner sections as the fossilized bone tissue tended to fracture and fragment excessively. The sample was cut directly from the edge of the fenestra, without any pre-treatment. The histological sections were analysed under a transmitted light optical microscopy (BX41; Olympus). The observations were conducted under white and polarised light. Both the sample and the histological sections were examined under electronic scanning field emission microscope (GeminiSEM 500; Zeiss) equipped with a microanalysis system (Oxford Aztec Live Microanalysis system, version 5.0; EDS OXFORD) and a detector (Ultim Max 100). The analyses were carried out in ‘analytical’ mode (15 kV; working distance, 8.5 mm; variable pressure); this allowed analysis of the samples directly, without any preliminary treatments with glues or surface metallisation.
Farlow, J. O. & Dodson, P. The behavioral significance of frill and horn morphology in ceratopsian dinosaurs. Evolution 29, 353–361 (1975).
Farke, A. A. Horn use in Triceratops (Dinosauria: Ceratopsidae): Testing behavioral hypotheses using scale models. Palaeontol. Electron. 7, 10 (2004).
Farke, A. A., Wolff, E. D. S. & Tanke, D. H. Evidence of combat in Triceratops. PLoS ONE 4(1), e4252. https://doi.org/10.1371/journal.pone.0004252 (2009).
Hicks, J. F., Johnson, K. R., Obradovich, J. D., Tauxe, L. & Clark, D. Magnetostratigraphy and geochronology of the Hell Creek and basal Fort Union formations of southwestern North Dakota and a recalibration of the age of Cretaceous-Terziary boundary. In The Hell Creek Formation and the Cretaceous-Tertiary Boundary in the Northern Great Plains: An Integrated Continental Record of the End of the Cretaceous (eds Hartman, J. H. et al.) 35–55 (Geological Society of America, 2002).
Horner, J. R., Goodwin, M. B. & Myhrvold, N. Dinosaur census reveals abundant Tyrannosaurus and rare ontogenetic stages in the Upper Cretaceous Hell Creek formation (Maastrichtian), Montana, USA. PLoS ONE 6(2), e16574. https://doi.org/10.1371/journal.pone.0016574 (2011).
Scannella, J. B., Fowler, D. W., Goodwin, M. B. & Horner, J. R. Evolutionary trends in Triceratops from the Hell Creek formation, Montana. Proc. Natl. Acad. Sci. U.S.A. 111(28), 10245–10250 (2014).
Lull, R. S. A revision of the Ceratopsia or horned dinosaurs. Mem. Peabody Mus. Nat. Hist. 3, 1–175 (1933).
Molnar, R. E. Analogies in the evolution of combat and display structures in ornithopods and ungulates. Evol. Theory 3, 165–190 (1977).
Tanke, D. H. & Farke, A. A. Bone resorption, bone lesions, and extracranial fenestrae in ceratopsid dinosaurs: A preliminary assessment. In Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs (ed. Carpenter, K.) 319–347 (Indiana University Press, 2006).
Baylink, D., Wergedal, J. & Thompson, E. Loss of proteinpolysaccharides at sites where bone mineralization is initiated. J. Histochem. Cytochem. 20, 279–292 (1972).
Marsell, R. & Einhorn, T. A. The biology of fracture healing. Injury 42(6), 551–555 (2011).
Anné, J. et al. Synchrotron imaging reveals bone healing and remodelling strategies in extinct and extant vertebrates. J. R. Soc. Interface 11, 20140277. https://doi.org/10.1098/rsif.2014.0277 (2014).
Anné, J., Garwood, R. J., Lowe, T., Withers, P. J. & Manning, P. L. Interpreting pathologies in extant and extinct archosaurs using micro-CT. PeerJ 3, e1130. https://doi.org/10.7717/peerj.1130 (2015).
Bonucci, E. Bone mineralization. Front. Biosci. 17, 100–128 (2012).
Wise, E. R. et al. The organic-mineral interface in bone is predominantly polysaccharide. Chem. Mater. 19, 5055–5057 (2007).
Herrmann, M. et al. Different kinetics of bone markers in normal and delayed fracture healing of long bones. Clin. Chem. 48, 2263–2266 (2002).
Muljačić, A. et al. The changes of bone-specific alkaline phosphatase (BsALP) associated with callus formation and rate of bone healing. Croat. Chem. Acta 83, 315–321 (2010).
Ortner, D. J. Infectious diseases: Introduction, biology, osteomyelitis, periostitis, brucellosis, glanders, and septic arthritis. In Identification of Pathological Conditions in Human Skeletal Remains 2nd edn (ed. Ortner, D.) 179–224 (Academic Press, 2003).
Schultz, M. Paleohistopathology of bone: A new approach to the study of ancient diseases. Yearb. Phys. Anthropol. 44, 106–147 (2001).
Ortner, D. J. & Turner-Walker, G. The biology of skeletal tissues. In Identification of Pathological Conditions in Human Skeletal Remains 2nd edn (ed. Ortner, D. J.) 11–35 (Academic Press, 2003).
Burr, D. B., Schaffler, M. B. & Frederickson, R. G. Composition of the cement line and its possible mechanical role as a local interface in human compact bone. J. Biomech. 21(11), 939–945 (1988).
Campo, R. D. Protein-polysaccharides of cartilage and bone in health and disease. Clin. Orthop. 68, 182–209 (1970).
Herring, G. M. The organic matrix of bone. In The Biochemistry and Physiology of Bone Vol. 1 (ed. Bourne, G. H.) 127–189 (Academic Press, 1972).
Urist, M. R. Biochemistry of calcification. In The Biochemistry and Physiology of Bone Vol. 4 (ed. Bourne, G. H.) 1–59 (Academic Press, 1976).
Takagi, M., Parmley, R. T., Toda, Y. & Denys, F. R. Ultrastructural cytochemistry of complex carbohydrates in osteoblasts, osteoid, and bone matrix. Calcif. Tissue Int. 35, 309–319 (1983).
Aufderheide, A. C. & Rodrìguez-Martìn, C. The Cambridge Encyclopedia of Human Paleopathology (Cambridge University Press, 1998).
DiGeronimo, P. M. & Brandão, J. Orthopedics in reptiles and amphibians. Vet. Clin. Exot. Anim. 22, 285–300 (2019).
McGavin, M. D. & Zachary, J. F. Pathologic Basis of Veterinary Disease 4th edn. (Elsevier, 2006).
We thank Maria Del Cimmuto for assistance in preparing the figures.
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The original online version of this Article was revised: The original version of this Article contained errors, where the place of discovery of Triceratops horridus, known as Big John, was incorrectly stated as ‘Hell Creek Formation (Upper Cretaceous; MT, USA).” in the Abstract and Introduction. Full information regarding the corrections made can be found in the correction for this Article.
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D’Anastasio, R., Cilli, J., Bacchia, F. et al. Histological and chemical diagnosis of a combat lesion in Triceratops. Sci Rep 12, 3941 (2022). https://doi.org/10.1038/s41598-022-08033-2