Temporal range: Late Cretaceous,80–75Ma
Pinacosaurus ("plank lizard") is a genus of medium-sized ankylosaur dinosaurs that lived from the late Santonian to the late Campanian stages of the late Cretaceous Period (roughly 80–75 million years ago), in Mongolia and China.
The type species Pinacosaurus grangeri was named in 1933. Pinacosaurus mephistocephalus named in 1999, is a second possibly valid species, differing from the type species in details of the skull armour. Of Pinacosaurus grangeri over a hundred skeletons have been found, more than of any other ankylosaur. These mostly consists of juveniles that perhaps lived in herds roaming the desert landscape of their habitat.
Pinacosaurus was about five metres long and weighed up to two tonnes. Its body was flat and low-slung but not as heavily built as in other members of the Ankylosaurinae. The head was protected by rather flat bone tiles, hence its name. Each nostril was formed as a large depression pierced by between three and five smaller holes, the purpose of which is uncertain. A smooth beak bit off low-growing plants that were sliced by rows of small teeth and then swallowed to be processed by the enormous hind gut. Neck, back and tail were protected by an armour of keeled osteoderms. The animal could also actively defend itself by means of a tail club.
The American Museum of Natural History sponsored several Central Asiatic Expeditions to the Gobi Desert in Mongolia in the 1920s. Among the many paleontological finds from the "Flaming Cliffs" of the Djadokhta Formation in Shabarakh Usu were the original specimens of Pinacosaurus, found by Walter Wallis Granger in 1923. In 1933, Charles Whitney Gilmore described a right ilium and a tail vertebra, without yet naming the animal. In a later publication of the same year, he named and described the type species Pinacosaurus grangeri. The generic name is derived from Greek πίναξ, pinax, "plank", in reference to the small rectangular scutes covering the head. The specific name honours Granger, who accompanied the 1923 expedition as a paleontologist.
The holotype, AMNH 6523, was found in a layer of the Djadochta Formation, dating from the Campanian. It consists of a partially transversely crushed skull, lower jaws, the first two neck vertebrae, and dermal bones collected in 1923. The skull is still the largest known of the genus.
Pinacosaurus is the best known Asian or worldwide ankylosaur with numerous specimens having been discovered. From the original Flamimg Cliffs or Shabarakh Usu several other fossils have been reported including ZPAL MgD II/1: a nearly complete skeleton; ZPAL MgD II/9: a postcranial skeleton; ZPAL MgD II/31: the handle of a tail club; PIN 614: a nearly complete postcranial skeleton (= Syrmosaurus viminocaudus); PIN 3780/3: a skull; and MPC 100/1305, a postcranial skeleton erroneously described in 2011 as belonging to Saichania. At another site, Alag Teeg, entire bonebeds have been uncovered of juvenile animals. Soviet-Mongolian expeditions in 1969 and 1970 reported thirty skeletons. Mongolian-Japanese expeditions added another thirty between 1993 and 1998. Forty were reported by Canadian expeditions between 2001 and 2006. The remains have not been all dug up and it is possible the reports partly pertain to the same material. In Inner Mongolia at Bayan Mandahu, the Canada−China Dinosaur Project in 1987, 1988, and 1990 found specimens IVPP V16853: a skull with cervical halfrings; IVPP V16283: a partial skull, IVPP V16854: a nearly complete skeleton; IVPP V16346: a partial skull; and IVPP V16855: a skeleton. Other, as yet undescribed material included two finds of several juveniles huddled together, evidently killed by a sandstorm (Jerzykiewicz, 1993; Burns et al., 2011). Whereas ankylosaur skeletons have often been preserved laying on their back, most Pinacosaurus juveniles are found on their belly in a resting position, with the legs tucked in.
Because of the many finds, in principle the entire juvenile skeleton is known. Pinacosaurus especially provides information on the build of the ankylosaurian skull, as in the juveniles the head armour has not yet fused with the skull proper and the sutures of the various elements are still visible. Modern studies have not yet fully covered the abundance of data. A well-preserved juvenile skull was described by Teresa Maryańska in 1971 and 1977. In 2003, Robert Hill studied the juvenile specimen IGM 100/1014 (Hill, 2003). In 2011, Currie published a study on the hand and foot, body parts often incompletely known with other ankylosaurs. The same year Michael Burns dedicated an article to four juveniles from the Bayan Mandahu (Burns, 2011). Also in 2011, the postcranial skeleton MPC 100/1305 was described in detail, though at the time referred to Saichania.
Additional species and synonyms
Yang Zhongjian ("C.C. Young") discovered a new specimen in the Ningxia Province at Bayanmandahu, and described it as a new species Pinacosaurus ninghsiensis in 1935. The rather complete skeleton lacks a present inventory number; it is now considered to be the same species as P. grangeri. The same is true of fragmentary remains, specimen PIN 614, described as Syrmosaurus viminocaudus by Evgenii Aleksandrovich Maleev in 1952. Arbour, Burns and Sissons (2009) considered Heishansaurus pachycephalus ("thick-headed Black Mountain lizard") from the Minhe Formation, near Heishan (= "Black Mountain"), Gansu Province, which is known from poorly preserved cranial and postcranial fragments, to be a junior synonym of P. grangeri as well. It was first described in 1953 as a pachycephalosaur and had been usually considered a nomen dubium. In 2014, Arbour again concluded it was a nomen dubium.
In 1996, a Belgian-Chinese expedition discovered a large skeleton in the Bayan Mandahu, specimen IMM 96BM3/1. It was named as Pinacosaurus mephistocephalus by Pascal Godefroit et alii in 1999. Only the skull was described in detail. The specific name is a contraction of Mephistopheles and Greek κεφαλή, kephalè, "head", in reference to the "devilish" squamosal horns. In 2010, Gregory S. Paul suggested that P. mephistopheles were a junior synonym of P. grangeri. It was considered a valid species by Robert Hill in 2012, based on the "secondary dermal" (squamosal) horns and narial characteristics. In 2014, Arbour confirmed that the species was valid.
Size and distinguishing traits
Pinacosaurus was a lightly built, medium-sized ankylosaur that reached a length of five meters (sixteen ft). Paul estimated the weight of a five metres long animal at 1.9 tonnes. The postcranial skeleton PIN 614 measures 366 centimetres from the first neck vertebrae to the end of the tail.
In 2014, Arbour established some distinguishing traits of the genus. The upper snout armour does not consist of distinct tiles, caputegulae, but of a fused mass. Adult individuals have a skull that is longer than wide. This trait is shared with the distant relatives Gobisaurus and Shamosaurus, but Pinacosaurus differs from those in the possession of extra openings in the nostril and a pointy protruding caputegula on the prefrontal, directed to the front. Pinacosaurus differs from Crichtonpelta in the lack of an ornamented rear edge of the skull roof and in the cheek horn not being curved upwards.
Arbour also provided a list of traits in which P. grangeri and P. mephistocephalus differed from each other. P. grangeri has a notch in the snout armour just above the innermost nostril opening. P. mephistocephalus has squamosal horns extending to behind beyond the rear of the skull roof, their points representing the widest point of the skull, instead of the upper rims of the eye sockets. P. mephistocephalus also has a clear transverse narrowing of the skull roof at level of the lacrimals, just in front of the eye sockets. It had been suggested that the rear skull roof of P. mephistocephalus was more convex but Arbour concluded it essentially had the same curvature. The holotype of P. mephistocephalus has very long cheek horns but a juvenile specimen, MPC 100/1344, found as part of a P. grangeri group, shows a similar elongation.
The adult skulls known have a length of about thirty centimetres. Pinacosaurus has exceptionally smooth praemaxillae, front snout bones, forming the bone core of the upper beak, that was in life covered with a horn sheet. The maxilla bears about fourteen teeth.
A typical and remarkable element of ankylosaurine skulls is that the nostril is in the shape of a large "narial vestibule" in which several smaller oval holes are present. With Pinacosaurus there are at least three per side. Gilmore already noticed this configuration in the original specimen. To allow a comparison between the holes of the several ankylosaurine species, they have been dubbed "A", "B" and "C". The top hole A seems to access the main air-passage of the nasal cavity. In P. grangeri this hole is visible in top view through a notch in the snout armour, whereas in P. mephistocephalus the armour overhangs the hole. The opening pattern is characteristic of the genus: in Pinacosaurus the C hole is below the A hole and the B opening is on the lower outer side of the vestibule. In Pinacosaurus juveniles the C hole seems to consist of secondary smaller openings of varying number: Godefroit et al. described four pairs of openings in total in 1999, and in 2003 a juvenile specimen with five pairs of openings was described. The extra C openings have been named C2 and C3. The precise function of this arrangement is unclear. There are several chambers in the praemaxilla and maxilla to which these holes are connected but it has also been suggested that some extra holes are the result of damage. The larger number with juveniles could be explained by cartilage sheets not having been ossified yet.
The visible sutures of the skull elements in juvenile specimens allowed for the first time to determine their precise arrangement. They generally consisted of indistinctly formed simple shapes. Several skull openings like the antorbital fenestra and the temporal fenestrae apparently closed at a very young age for they are no longer visible even in the juveniles found. The squamosal horn does not cover the entire squamosal, creating the illusion that an additional skull bone is present in front of the horn. Maryańska in 1977 thought that this was a tabular bone, otherwise unknown in dinosaurs, proving that the Ankylosauria had independently evolved from the Aetosauria, a hypothesis today entirely discarded. Godefroit in 1999 called it a "secondary dermal squamosal". A real distinctive trait is that the quadratojugal touches the postorbital, whereas in other Thyreophora for which the condition is known, these bones are separated by the jugal. Usually it is assumed that this configuration is not unique for Pinacosaurus but a synapomorphy of the Ankylosauridae as a whole.
The postcranial skeleton of the known fossils is rather lightly built. Most of these represent juveniles, however: even specimen IMM 96BM3/1, the P. mephistocephalus holotype, is no longer than about three metres. Juveniles had four rear back vertebrae fused into a "sacral rod", three true sacrals, and a tail base of seven vertebrae possessing transverse processes. Behind these about eight "free" vertebrae are present, followed by about twenty vertebrae stiffened by projections and forming the "handle" of the tail club. Like all ankylosaurids, Pinacosaurus had a bony club at the end of its tail which it likely used as a defensive weapon against predators. This club was relatively small.
The torso is very flat. The forelimbs are moderately robust; the P. mephistocephalus holotype has a quite robust humerus and ulna, however. The hand is completely known, which is exceptional for ankylosaurids. It has five digits, and the phalangeal formula is 2-3-3-3-2, meaning that the innermost finger of the forelimb has two bones, the next has three, etc. The metatarsals are closely appressed and held vertical. The claws are hoof-shaped.
In the pelvis, the ilia flare strongly outwards to the front. The ischium is thin and curves forwards. The hindlimbs are moderately robust. The shinbone has a wide underside with well-formed condyles. Currie therefore assumed that the lower leg articulated directly with the metatarsus, the inner part of the astragalus and the entire calcaneum being absent or non-ossified cartilage elements. As in all known ankylosaurids, the foot has three toes, not four as Maryańska assumed in 1977, misled by the damaged specimen ZPAL MgD−II/9. The phalangeal formule of the toes is variable: most individuals have 0−3−3−4−0 but some exemplars possess an extra penultimate phalanx in the third toe, resulting in 0-3-4-4-0, while others lack a phalanx in the fourth toe, which causes a 0-3-3-3-0 configuration.
The configuration of the skin ossifications, or osteoderms, of the body is partly known: no single specimen conserves a complete set. Additional information can be gleaned from the larger specimen MPC 100/1305, a possible Pinacosaurus exemplar. The neck is protected by two cervical halfrings, consisting of keeled rectangular segments fused to a underlying bone band. This band is completely ossified even in juvenile individuals. Godefroit assumed Pinacosaurus differed from other species in having three or four segments instead of the usual six, but Arbour concluded that the normal number was in fact present.
The sides of the rump and the tail were occupied by moderately long, flat, recurved, triangular spikes. Parallel rows of smaller oval keeled osteoderms were present on the back. A continuous "sacral shield" on the hip, made of fused plates, is absent.
The difference in the relative position of the two Pinacosaurus species between the respective analyses, is influenced by the fact that the best preserved P. grangeri skulls are from juveniles, while the holotype of P. mephistocephalus is an adult with a skull that is longer than it is wide, which might cause a more basal position of the latter.
The habitat of Pinacosaurus consisted of a semi-desert interspersed with oases. No large theropods are known to have inhabited the ecosystem, though smaller ones like Velociraptor were present. It has been suggested that the relatively light build of Pinacosaurus was an adaptation to gain agility to better fight small theropods, the moderately large club being fast enough to hit these swift targets.
In the group of juveniles found together at Bayan Mandahu, the individuals were all oriented into the same direction, suggesting they represent a travelling true herd simultaneously killed and covered by a sandstorm. It is remarkable that the members of such groups are all of about the same age, having an average length of circa 1.5 metres. This could be explained by the larger individuals being able to extract themselves from the sand, leaving the small members of the herd behind but in that case it is strange that no very young animals were found, the smallest being about one metre in length. The concentration of fossils at Alag Teeg has been explained as caused by a drying pool, but later research showed the sediments were deposited during a flood. During their ontogenetic development, in juveniles at first the ribs fused with their vertebrae. The forelimbs strongly increased in robustness, while the hindlims did not become larger relative to the rest of the skeleton, indicating that the arms bore most of the weight. In the cervical halfrings, the underlying bone band developed outgrowths connecting it with the underlying osteoderms, which simultaneously fused to each other. On the skull, the caputegulae first ossified at the snout and the rear rim; gradually the ossification extended towards the middle regions. On the rest of the body, the ossification process progressed from the neck onwards in the direction of the tail.
- Arbour, V. M.; Burns, M. E.; Sissons, R. L. (2009). "A redescription of the ankylosaurid dinosaur Dyoplosaurus acutosquameus Parks, 1924 (Ornithischia: Ankylosauria) and a revision of the genus". Journal of Vertebrate Paleontology 29 (4): 1117. doi:10.1671/039.029.0405.
- Hill et al. 2003, p. 2–4.
- Gilmore, C.W., 1933, "On the dinosaurian fauna of the Iren Dabasu Formation", Bulletin of the American Museum of Natural History 67: 23–78
- Gilmore 1933
- Gilmore 1933
- Hill et al. 2003, p. 2.
- Currie, P.J., Badamgarav, D., Koppelhus, E.B., Sissons, R., and Vickaryous, M.K., 2011, "Hands, feet, and behaviour in Pinacosaurus (Dinosauria: Ankylosauridae)", Acta Palaeontologica Polonica 56(3): 489–504
- Maryańska T., 1971, "New data on the skull of Pinacosaurus grangeri (Ankylosauria)", Palaeontologia Polonica 25: 45-53
- T. Maryańska, 1977, "Ankylosauridae (Dinosauria) from Mongolia", Palaeontologia Polonica 37: 85-151
- Carpenter, K., Hayashi, S., Kobayashi, Y., Maryanska, T., Barsbold, R., Sato, K., and Obata, I., 2011, "Saichania chulsanensis (Ornithischia, Ankylosauridae) from the Upper Cretaceous of Mongolia", Palaeontographica, Abteilung A, 294(1-3): 1-61
- Young 1935.
- Hill et al., p. 2 refers to Maleev 1952.
- Arbour, Victoria Megan, 2014, Systematics, evolution, and biogeography of the ankylosaurid dinosaurs. Ph.D thesis, University of Alberta
- P. Godefroit, X. Pereda-Suberbiola, H. Li and Z. Dong, 1999, "A new species of the ankylosaurid dinosaur Pinacosaurus from the Late Cretaceous of Inner Mongolia (P.R. China)", Bulletin de l'Institut Royal des Sciences Naturelles de Belgique, Sciences de la Terre 69(supplement): 17-366
- Paul, G.S., 2010, The Princeton Field Guide to Dinosaurs, Princeton University Press p. 232
- Buffetaut, E., 1995, "An ankylosaurid dinosaur from the Upper Cretaceous of Shandong (China)", Geological Magazine 132: 683-692
- Hill et al. 2003, p. 4.
- Gilmore 1933, p. 5 and Fig. 1.
- Hill et al. 2003
- Martin, A.J. (2006). Introduction to the Study of Dinosaurs. Second Edition. Oxford, Blackwell Publishing. 560 pp. ISBN 1–4051–3413–5.
- Gilmore 1933, p. 9.
- Arbour V.M. and Currie P.J., 2013, "Euoplocephalus tutus and the Diversity of Ankylosaurid Dinosaurs in the Late Cretaceous of Alberta, Canada, and Montana, USA", PLoS ONE 8(5): e62421. doi:10.1371/journal.pone.0062421
- Thompson, R. S.; Parish, J. C.; Maidment, S. C. R.; Barrett, P. M. (2012). "Phylogeny of the ankylosaurian dinosaurs (Ornithischia: Thyreophora)". Journal of Systematic Palaeontology 10 (2): 301. doi:10.1080/14772019.2011.569091.
- Michael E. Burns, Tatiana A. Tumanova and Philip J. Currie, 2015, "Postcrania of juvenile Pinacosaurus grangeri (Ornithischia: Ankylosauria) from the Upper Cretaceous Alagteeg Formation, Alag Teeg, Mongolia: implications for ontogenetic allometry in ankylosaurs", Journal of Paleontology 89(1): 168-182
- Dixon, Dougal. 'The Complete Book of Dinosaurs.' Hermes House, 2006.
- Fukui Prefectural Dinosaur Museum : the web site — Pinacosaurus grangeri
- Gilmore, C. W. (December 4, 1933). "Two new dinosaurian reptiles from Mongolia with notes on some fragmentary specimens". American Museum Novitates (679): 1–20.
- Hill, R. V.; Witmer, L. W.; Norell, M. A. (2003). "A New Specimen of Pinacosaurus grangeri (Dinosauria: Ornithischia) from the Late Cretaceous of Mongolia: Ontogeny and Phylogeny of Ankylosaurs". American Museum Novitates (3395): 1–29. doi:10.1206/0003-0082(2003)395<0001:ansopg>2.0.co;2.
- Maleev, E. A. (1952). "Novoe semeystvo pantsirnich dinosavrov is verchnego mela Mongolii" [A new family of armored dinosaurs from the Upper Cretaceous of Mongolia]. Doklady Akademii Nauk SSSR (in Russian) 87: 131–134.
- Young, C. C. (1935). "On a new nodosaurid from Ninghsia.". Palaeontologica Sinica, Series C (11): 5–27.
- Burns, M. B.; Currie, P. J.; Sissons, R. L.; Arbour, V. M. (2011). "Juvenile specimens of Pinacosaurus grangeri Gilmore, 1933 (Ornithischia: Ankylosauria) from the Late Cretaceous of China, with comments on the specific taxonomy of Pinacosaurus.". Cretaceous Research 32 (2): 174–186. doi:10.1016/j.cretres.2010.11.007.