Temporal range: Early Cretaceous, 123.2–100Ma
|P. meileyingensis cast, Children's Museum of Indianapolis|
Psittacosaurus (// SIT-ə-kə-SOR-əs; "parrot lizard") is a genus of extinct ceratopsian dinosaur from the Early Cretaceous of what is now Asia, existing between 123.2 and 100 million years ago. It is notable for being the most species-rich dinosaur genus. Up to 11 species are known, from across Mongolia, Siberia, China, and possibly Thailand. The species of Psittacosaurus were obligate bipeds at adulthood, with a high skull and a robust beak. One individual was found preserved with long quills on the tail, similar to those of Tianyulong, yet scales of varying sizes and shapes across the rest of the animal. Psittacosaurus probably had complex behaviours, based on the proportions and relative size of the brain. It may have been active for short periods of time during the day and night, and had good smell and well developed vision.
Psittacosaurus was one of the earliest ceratopsians, but closer to Triceratops than Yinlong. Once in its own family, Psittacosauridae, with other genera like Hongshanosaurus, it is now considered to be senior synonym of the latter and an early offshoot of the branch that led to more derived forms. The genera closely related to Psittacosaurus are all from Asia, with the exception of Aquilops, from North America. The first species was either P. lujiatunensis or closely related, and it may have given rise to later forms of Psittacosaurus.
Psittacosaurus is one of the most completely known dinosaur genera. Fossils of over 400 individuals have been collected so far, including many complete skeletons. Most different age classes are represented, from hatchling through to adult, which has allowed several detailed studies of Psittacosaurus growth rates and reproductive biology. The abundance of this dinosaur in the fossil record has led to the labelling of Lower Cretaceous sediments of east Asia the Psittacosaurus biochron.
Different species of Psittacosaurus varied in size and specific features of the skull and skeleton, but shared the same overall body shape. The best-known species, P. mongoliensis, reached 2 meters (6.5 ft) in length. The maximum adult body weight was most likely over 20 kilograms (44 lb) in P. mongoliensis. Several species approached P. mongoliensis in size (P. lujiatunensis, P. neimongoliensis, P. xinjiangensis), while others were somewhat smaller (P. sinensis, P. meileyingensis). P. ordosensis was the smallest known species, 30% smaller than P. mongoliensis. The largest were P. lujiatunensis and P. sibiricus, although neither was significantly larger than P. mongoliensis.
The skull of Psittacosaurus was highly modified compared to other ornithischian dinosaurs of its time. The skull was extremely tall in height and short in length, with an almost round profile in some species. The portion in front of the orbit (eye socket) was only 40% of total skull length, shorter than any other known ornithischian. The lower jaws of psittacosaurs are characterized by a bulbous vertical ridge down the center of each tooth. Both upper and lower jaws sported a pronounced beak, formed from the rostral and predentary bones, respectively. The bony core of the beak may have been sheathed in keratin to provide a sharp cutting surface for cropping plant material. As the generic name suggests, the short skull and beak superficially resembled those of modern parrots. Psittacosaurus skulls shared several adaptations with more derived ceratopsians, such as the unique rostral bone at the tip of the upper jaw, and the flared jugal (cheek) bones. There was still no sign of the bony neck frill or prominent facial horns which would develop in later ceratopsians. Bony horns did protrude from the skull of P. sibiricus, but these are thought to be an example of convergent evolution.
Psittacosaurus postcranial skeletons were more typical of a 'generic' bipedal ornithischian. In P. mongoliensis, similarly to other species, the forelimbs were only 58% as long as the hindlimbs and their range of motion indicates that the hands could neither be rotated at the forearm (pronated) nor used in scrambling fashion, to generate propulsive force, suggesting that these animals were totally bipedal in life. There were only four digits on the manus ('hand'), as opposed to the five found in most other ornithischians (including all other ceratopsians). Overall, the four-toed hindfoot was very similar to many other small ornithischians.
Integumental structures from Psittacosaurus have been discovered to preserve possible quill-like feathers. However, the specimen on which these were identified were illegally exported from China to Germany, where it was described while awaiting repatriation. The specimen, in the Senckenberg Museum, showed integument from most major regions of the skeleton. It has not yet been identified as a specific species, and was referred to as P. sp. by the 2002 study describing it. Various scales were present across the body, including impressions from the shoulder similar to those identified on Chasmosaurus, with irregular rows of larger and rounded scales surrounded by smaller hexagonal ones.
However, over the tail were exciting discoveries of tall bristles. These were confirmed by the authors, as well as an independent scientist, to not represent plant material. The bristles extend into the skin nearly to the vertebrae, farther in closer to the proximal end of the tail. All quills were on the proximal third of the tail, and were likely circular or tubular before being preserved. Under ultraviolet light, the quills gave off the same fluorescence as scales, providing the possibility they were keratinized. As the authors of the study said, "At present, there is no convincing evidence which shows these structures to be homologous to the structurally different integumentary filaments of theropod dinosaurs", however, they did state that all other feathery integument from the Yixian Formation is indeed feathers.
In 2008, another study was published describing the integument and dermis of Psittacosaurus sp., from two different specimens. The skin was cross-sectioned to compare to modern animals, showing dinosaurian dermal layers evolved parallel to those in many other large vertebrates. The tissue fibres in Psittacosaurus are complex, virtually identical to all other vertebrates. As the sections of dermis were collected from the abdomen, where the scales were worn away, the tissue may have assisted with the musculature of the stomach and intestines.
The brain of P. lujiatunensis is well known, a 2007 study published on the anatomy and functionality of three specimens all clearly of the species. Generally thought until the study, the brain of Psittacosaurus would have been similar to other ceratosians with low Encephalization Quotients. Russell & Zhao (1996) believed “the small brain size of psittacosaurs implies a very restrictive behavioural repertoire relative to that of modern mammals of similar body size”. However, the 2007 study disposed of this misbelief, finding the brain more advanced. Generally negative allometry for brain size with development in vertebrates, but it was shown that in Psittacosaurus this was not true. The EQ score for P. lujiatunensis is 0.31, significantly higher than genera such as Triceratops.
Based on the EQ, Psittacosaurus was behaviourally complex, as a higher EQ influences the behaviour of animals. Various dinosaurs have high EQs, similar to birds, which range from 0.36 to 2.98. Thus, Psittacosaurus behaved complexly, even as complex as Tyrannosaurus, whose EQ ranges from 0.30 to 0.38. Behaviours influenced by high EQs include nest-building, parental care, and bird-like sleeping, some of which have been shown to be present in Psittacosaurus and others of which may have occurred. Based on the 2007 study, these may come from the high EQ in Psittacosaurus.
The senses of Psittacosaurus can be inferred from the endocast. Large olfactory bulbs are present, indicating the genus had an acute sense of smell. The size of these bulbs are comparable to large predatory theropods, although they likely evolved to avoid predators instead of seek out prey. The sclerotic rings in reptiles directly show the size of the eyeball. The rings are not well preserved in Psittacosaurus, with one individual preserving them likely contracted postmortem, but if they are similar to those of Protoceratops, Psittacosaurus would have had large eyes and acute vision. The curvature of the semicircular canals are in effect to the agility of reptiles, and the large curved canals in Psittacosaurus show that the genus was much more agile than later ceratopsians. Comparisons between the scleral rings of Psittacosaurus and modern birds and reptiles suggest that it may have been cathemeral, active throughout the day and night at short intervals.
Ford and Martin (2010) proposed that Psittacosaurus was semi-aquatic, swimming with its tail like a crocodile, and paddling and kicking. They based their interpretation on evidence including: the lacustrine (lake) depositional setting of many specimens; the position of the nostrils and eyes; interpretations of the motions of the arms and legs; tails with long chevrons (and with the bristles on the tail interpreted as possibly skin-covered, forming a fin), providing a propulsive surface; and the presence of gastroliths, interpreted as ballast. They further suggested that some species of Psittacosaurus were more terrestrial than others.
Psittacosaurs had self-sharpening teeth that would have been useful for cropping and slicing tough plant material. Unlike later ceratopsians, they did not have teeth suitable for grinding or chewing their food. Instead, they used gastroliths, stones swallowed to wear down food as it passed through the digestive system. Gastroliths, sometimes numbering more than fifty, are occasionally found in the abdominal cavities of psittacosaurs, and may have been stored in a gizzard, as in modern birds.
Unlike many other dinosaurs, psittacosaurs had akinetic skulls: that is to say, the upper and lower jaws each behaved as a single unit, without internal joints. The only joint was the jaw joint itself, and psittacosaurs could slide their lower jaws forward and backward on the joint, permitting a shearing action. Unlike most ceratopsians, their beaks did not form curved tips, but were instead rounded and flattened. If the jaws were aligned, the beaks could be used to crop objects, but if the lower jaw was retracted so that the lower beak was inside the upper beak, the jaws may have served a nutcracking function. A nut- or seed-rich diet would also match well with the gastroliths often seen in well-preserved psittacosaur skeletons.
Studies by Phil Senter in 2007 conducted on Psittacosaurus neimongoliensis and Psittacosaurus mongoliensis concluded that the forelimbs of these taxa (and likely those of other Psittacosaurus species) were too short to reach the ground and could neither be pronated nor generate propulsive force for locomotion, suggesting that Psittacosaurus was entirely bipedal. The forelimbs were also too short to be used in digging or bringing food to the mouth, and Senter suggested that if Psittacosaurus needed to dig depressions in the ground it may have used its hindlimbs instead. The forelimbs could be used for two-handed grasping of objects or scratching the body, but due to their extremely limited flexibility and reach, they could have only been used to grasp objects very close to the belly or sides of the animal and could have scratched only the belly, flank and knees. Even though the hands could not reach the mouth, Psittacosaurus could have still used them to carry nesting material or food to a desired location. New findings may dispute the hypothesis of Psittacosaurus being entirely bipedal thanks to the studies of Qi Zhao from the University of Bristol. Taking sections from the limb bones from 16 specimens of Psittacosaurus, ranging in age from less than a year old to ten-year old adults, Zhao found that Psittacosaurus was probably secondarily bipedal. The infants' front limbs grew at faster rates than the hind limbs at between birth and three years of age. At the age of between four and six years, arm growth slowed and leg growth accelerated as the animal became mature. At this stage, Psittacosaurs would switch to a bipedal stance. These findings further reveal that the ancestor of Psittacosaurus was likely quadrupedal and eventually gained the ability to become bipedal as it evolved, with the young retaining the quadrupedal gait of the ancestor in question. These findings also lead to the hypothesis that many such dinosaur families may have evolved along this path at some point in their evolution.
Several juvenile Psittacosaurus have been found. The smallest is a P. mongoliensis hatchling conserved in the American Museum of Natural History (AMNH), which is only 11 to 13 centimeters (4–5 inches) long, with a skull 2.8 centimeters (1 in) in length. Another hatchling skull at the AMNH is only 4.6 centimeters (1.8 inches) long. Both specimens are from Mongolia. Juveniles discovered in the Yixian Formation are approximately the same age as the larger AMNH specimen.
A histological examination of P. mongoliensis has determined the growth rate of these animals. The smallest specimens in the study were estimated at three years old and less than 1 kilogram (2.2 lb), while the largest were nine years old and weighed almost 20 kilograms (44 lb). This indicates relatively rapid growth compared to most reptiles and marsupial mammals, but slower than modern birds and placental mammals. An age determination study performed on the fossilized remains of Psittacosaurus mongoliensis by using growth ring counts suggest that the longevity of the basal ceratopsian was 10 to 11 years.
The find of a herd of six Psittacosaurus individuals killed and buried by a volcanic mudflow indicates the presence of at least two age groups from two distinct clutches gathered together. This find has been taken as evidence for group fidelity and gregariousness extending beyond the nest; the earliest such evidence for any ceratopsian. Even very young psittacosaur teeth appear worn, indicating they chewed their own food and may have been precocial. Another juvenile-only cluster shows that specimens of different ages grouped together. These juveniles may have associated together as a close knit, mixed-age herd either for protection, to enhance their foraging, or as putative helpers at the parental nest. There is no evidence for parental care.
In 2004, a specimen found in the Yixian Formation of Liaoning Province, China was claimed as evidence for parental care in dinosaurs. The specimen DNHM D2156 consists of 34 articulated juvenile Psittacosaurus skeletons, closely associated with the skull of an adult. The juveniles, all approximately the same age, are intertwined in a group underneath the adult, although all 34 skulls are positioned above the mass of bodies, as they would have been in life. This suggests that the animals were alive at the time of burial, which must have been extremely rapid, perhaps due to the collapse of a burrow. However, a 2013 paper pointed out that the adult specimen did not belong with the nest, its skull having no sedimentary connection to the main slab where the juveniles occurred, but had been glued onto it. This artificial association led to the inference that the skull belonged to an individual, possibly a "mother", that was providing parental care for the 34 juveniles - a claim that is unfounded. Furthermore, the adult was also shown to be six years old, whereas histological studies have shown P. mongoliensis was unable to breed until it reached ten years of age. It is also unlikely that a single female would have so many offspring at one time.
A 2014 analysis of the same specimen concluded that the proximity of the six-year-old specimen to the post-hatchlings may indicate post-hatchling cooperation, making the six-year-old specimen a possible caretaker. Such behavior is also found in cooperative breeding modern birds.
Out of over 400 known Psittacosaurus specimens, only one has been described to possess any sort of pathology. The specimen in question, consisting of a complete adult skeleton and tentatively assigned to P. mongoliensis, was found in the lower beds of the Yixian Formation. There is no sign of a bone fracture, but very clear signs of an infection can be seen near the midpoint of the right fibula. The bone exhibits a large round pit, evidence of necrosis due to a lack of blood supply to the region. The pit is surrounded by a massive amount of swelling along the lower third of the bone. This large amount of bone deposited around the injury indicates that the animal survived for quite a while despite the injury and subsequent infection. As psittacosaurids were bipedal animals, a similar injury to a weight bearing bone in the leg would likely have been fatal. Unlike the femur and tibia, the fibula is not a weight-bearing bone, so this animal would still have been able to walk to some extent. The source of the injury remains unknown.
Psittacosaurus is known from over 400 individual specimens, of which over 75 have been assigned to the type species, P. mongoliensis. All Psittacosaurus fossils discovered so far have been found in Early Cretaceous sediments in Asia, from southern Siberia to northern China, or possibly as far south as Thailand. The most common age of geologic formations bearing Psittacosaurus fossils is from the late Barremian through Albian stages of the Early Cretaceous, or approximately 123 to 100 mya (million years ago). Many terrestrial sedimentary formations of this age in Mongolia and northern China have produced fossils of Psittacosaurus, leading its use as in defining the Psittacosaurus biochron for this time period in the region.
The earliest known species is P. lujiatunensis, found in the lowest beds of the Yixian Formation. Over 200 specimens attributed to this genus have been recovered from these and other beds of the Yixian, the age of which is the subject of much debate. Although many early studies using radiometric dating put the Yixian in the Jurassic Period, tens of millions of years outside of the expected temporal range of Psittacosaurus, most recent work dates it to the Early Cretaceous. Using argon-argon dating, a team of Chinese scientists dated the lowest beds in the formation to about 128 Ma, and the highest to approximately 122 mya. A more recent Chinese study, using uranium-lead dating, suggests that the lower beds are younger, approximately 123.2 mya, while agreeing with an age of 122 mya for the upper beds.
Another fossil from the Yixian Formation provides direct evidence of Psittacosaurus as a prey animal. One skeleton of Repenomamus robustus, a large triconodont mammal, is preserved with the remains of a juvenile Psittacosaurus in its abdominal cavity. Several of the juvenile's bones are still articulated, indicating that the carnivorous mammal swallowed its prey in large chunks. This specimen is notable in that it is the first known example of Mesozoic mammals preying on live dinosaurs. Heavy predation on juvenile Psittacosaurus may have resulted in R-selection, the production of more numerous offspring to counteract this loss.
Discovery and naming
Psittacosaurus was first described as a genus in 1923, by Henry Fairfield Osborn. He named the type species P. mongoliensis, for the location of its discovery in Mongolia. The holotype, American Museum of Natural History 6254, preserved a nearly complete skull, as well as a post cranial skeleton lacking sections of the limbs. In the same article, Osborn named another new binomial, a subfamily and new family for the taxa, Protiguanodon mongoliense, Protiguanodontinae, and Psittacosauridae, respectively. Protiguanodon mongoliense, AMNH 6523, measured 1.35 m (4.4 ft) long, and was known from much of the skeleton, although at the time of description the neck vertebrae were still covered by matrix. Osborn diagnosed his taxa on the basis of features of the teeth and snout. However, modern taxonomists find these features insignificant, instead placing Protiguanodon mongoliense within Psittacosaurus mongoliensis.
Seventeen species have been referred to the genus Psittacosaurus, although only nine to eleven are considered valid today. This is the highest number of valid species currently assigned to any single dinosaur genus (not including birds). In contrast, most other dinosaur genera are monospecific, containing only a single known species. The difference is most likely due to quirks of the fossil record. While Psittacosaurus is known from hundreds of fossil specimens, most other dinosaur species are known from far fewer, and many are represented by only a single specimen. With a very high sample size, the diversity of Psittacosaurus can be analyzed more completely than that of most dinosaur genera, resulting in the recognition of more species. Most extant animal genera are represented by multiple species, suggesting that this may have been the case for extinct dinosaur genera as well, although most of these species may not have been preserved. In addition, most dinosaurs are known solely from bones and can only be evaluated from a morphological standpoint, whereas extant species often have very similar skeletal morphology but differ in other ways which would not normally be preserved in the fossil record, such as behavior, or coloration. Therefore actual species diversity may be much higher than currently recognized in this and other dinosaur genera.
- Valid Psittacosaurus species
- Psittacosaurus mongoliensis – Mongolia, northern China
- Psittacosaurus sinensis – northeastern China
- Psittacosaurus meileyingensis – north-central China
- Psittacosaurus xinjiangensis – northwestern China
- Psittacosaurus neimongoliensis – north-central China
- Psittacosaurus ordosensis – north-central China
- Psittacosaurus mazongshanensis – northwestern China
- Psittacosaurus sibiricus – Russia (southern Siberia)
- Psittacosaurus lujiatunensis – northeastern China
- Psittacosaurus gobiensis – Inner Mongolia
- Possible Psittacosaurus species
Although many species of Psittacosaurus have been named, their relationships to each other have not yet been fully explored and no scientific consensus exists on the subject. Several phylogenetic analyses have been published, with the most detailed being those by Alexander Averianov and colleagues in 2006, Hai-Lu You and colleagues in 2008, and Paul Sereno in 2010. The middle one is shown below.
It has been suggested that P. lujiatunensis is basal to all other species. This would be consistent with its earlier appearance in the fossil record.
Psittacosaurus is the type genus of the family Psittacosauridae, which was also named by Osborn in 1923. Psittacosaurids were basal to almost all known ceratopsians except Yinlong and perhaps the Chaoyangsauridae. While Psittacosauridae was an early branch of the ceratopsian family tree, Psittacosaurus itself was probably not directly ancestral to any other groups of ceratopsians. All other ceratopsians retained the fifth digit of the hand, a plesiomorphy or primitive trait, whereas all species of Psittacosaurus had only four digits on the hand. In addition, the antorbital fenestra, an opening in the skull between the eye socket and nostril, was lost during the evolution of Psittacosauridae, but is still found in most other ceratopsians and in fact most other archosaurs. It is considered highly unlikely that the fifth digit or antorbital fenestra would evolve a second time.
In 2014, the describers of a new taxon of basal ceratopsian published a phylogenetic analysis encompassing Psittacosaurus. The below cladogram is from their analysis, placing the genus as one of the most primitive ceratopsians. The authors (Farke et al.) noted that all taxa outside of Leptoceratopsidae and Coronosauria with the exception of their genus Aquilops are from Asia, meaning the group likely originated there.
- Sereno, P.C. (1997). "Psittacosauridae". In Currie, Philip J.; Padian, Kevin P. The Encyclopedia of Dinosaurs. Academic Press. pp. 611–613.
- Erickson, G.M.†; Tumanova, T.A. (2000). "Growth curve of Psittacosaurus mongoliensis Osborn (Ceratopsia: Psittacosauridae) inferred from long bone histology". Zoological Journal of the Linnean Society 130 (4): 551–566. doi:10.1111/j.1096-3642.2000.tb02201.x.
- Sereno, P.C.; Zhao, X.; Brown, L.; Tan, L. (2007). "New psittacosaurid highlights skull enlargement in horned dinosaurs" (PDF). Acta Palaeontologica Polonica 52 (2): 275–284.
- Russell, D.A.; Zhao, X. (1996). "New psittacosaur occurrences in Inner Mongolia". Canadian Journal of Earth Sciences 33 (4): 637–648. doi:10.1139/e96-047.
- Brinkman, D.B.; Eberth, D.A.; Ryan, M.J.; Chen, P. (2001). "The occurrence of Psittacosaurus xinjiangensis Sereno and Chow, 1988 in the Urho area, Junggar basin, Xinjiang". Canadian Journal of Earth Sciences 38 (12): 1781–1786. doi:10.1139/e01-049.
- Sereno, Paul C.; Xijin, Zhao; Zhengwu, Chang; Chenggang, Rao (1988). "Psittacosaurus meileyingensis (Ornithischia: Ceratopsia), a new psittacosaur from the Lower Cretaceous of northeastern China". Journal of Vertebrate Paleontology 8: 366–377. doi:10.1080/02724634.1988.10011725.
- Changfu, Zhou; Keqin, Gao; Fox, Richard C.; Shuihua, Chen (2006). "A new species of Psittacosaurus (Dinosauria: Ceratopsia) from the Early Cretaceous Yixian Formation, Liaoning, China". Palaeoworld 15: 100–114.
- Averianov, Alexander O.; Voronkevich, Alexei V.; Leshchinskiy, Sergei V.; Fayngertz, Alexei V. (2006). "A ceratopsian dinosaur Psittacosaurus sibiricus from the Early Cretaceous of West Siberia, Russia and its phylogenetic relationships". Journal of Systematic Paleontology 4 (4): 359–395. doi:10.1017/s1477201906001933.
- You Hailu & Dodson, Peter. (2004). Basal Ceratopsia. In: Weishampel, David B., Dodson, Peter, & Osmolska, Halszka (Eds.). The Dinosauria (2nd Edition). Berkeley: University of California Press. Pp. 478–493.
- Senter, P (2007). "Analysis of forelimb function in basal ceratopsians". Journal of Zoology 273: 305–314. doi:10.1111/j.1469-7998.2007.00329.x.
- Mayr, G.; Peters, S.D.; Plodowski, G.; Vogel, O. (2002). "Bristle-like integumentary structures at the tail of the horned dinosaur Psittacosaurus" (PDF). Naturwissenschaften 89: 361–365. doi:10.1007/s00114-002-0339-6.
- Lingham-Soliar, T. (2008). "A unique cross section through the skin of the dinosaur Psittacosaurus from China showing a complex fibre architecture". Proceedings of the Royal Society B: Biological Sciences 275 (1636): 775. doi:10.1098/rspb.2007.1342.
- Zhou, C. F.; Gao, K. Q.; Fox, R. C.; Du, X. K. (2007). "Endocranial morphology of psittacosaurs (Dinosauria: Ceratopsia) based on CT scans of new fossils from the Lower Cretaceous, China". Palaeoworld 16 (4): 285. doi:10.1016/j.palwor.2007.07.002.
- Schmitz, L.; Motani, R. (2011). "Nocturnality in Dinosaurs Inferred from Scleral Ring and Orbit Morphology". Science 332 (6030): 705–8. doi:10.1126/science.1200043. PMID 21493820.
- Ford, Tracy L.; Martin, Larry D. (2010). "A semi-aquatic life habit for Psittacosaurus". In Ryan, Michael J.; Chinnery-Allgeier, Brenda J.; and Eberth, David A. (editors.). New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium. Bloomington and Indianapolis: Indiana University Press. pp. 328–339. ISBN 978-0-253-35358-0.
- Sereno, Paul C.; Xijin, Zhao; Lin, Tan (2010). "A new psittacosaur from Inner Mongolia and the parrot-like structure and function of the psittacosaur skull" (PDF). Proceedings of the Royal Society B 277 (1679): 199–209. doi:10.1098/rspb.2009.0691.
- Qi Zhao, Michael J. Benton, Corwin Sullivan, P. Martin Sander, Xing Xu. "Histology and postural change during the growth of the ceratopsian dinosaur Psittacosaurus lujiatunensis. Nature Communications 2013; 4 doi:10.1038/ncomms3079
- Coombs, Walter P (1982). "Juvenile specimens of the ornithischian dinosaur Psittacosaurus". Palaeontology 25: 89–107.
- Qingjin, Meng; Jinyuan, Liu; Varrichio, David J.; Huang, Timothy; Chunling, Gao (2004). "Parental care in an ornithischian dinosaur". Nature 431: 145–146.
- Zhao, Q.; Barrett, P.M.; Eberth, D.A. (2007). "Social behaviour and mass mortality in the basal ceratopsian dinosaur Psittacosaurus (Early Cretaceous, People's Republic of China)".". Palaeontology 50 (5): 1023–1029. doi:10.1111/j.1475-4983.2007.00709.x.
- Alexander, R.D. (1974). "The evolution of social behavior". Annual Review of Ecology and Systematics 5: 325–383. doi:10.1146/annurev.es.05.110174.001545.
- Zhao, Q. (2013). "Juvenile-only clusters and behaviour of the Early Cretaceous dinosaur Psittacosaurus". Acta Palaeontologica Polonica. doi:10.4202/app.2012.0128.
- "Paleontologists describe a possible dinosaur nest and young 'babysitter'". phys.org. Retrieved 27 August 2014.
- Hedrick, B. P.; Gao Chunling; Omar, G. I.; Zhang Fengjiao; Shen Caizhi; Dodson, P. (2014). "The osteology and taphonomy of a Psittacosaurus bonebed assemblage of the Yixian Formation (Lower Cretaceous), Liaoning, China". Cretaceous Research 51: 321–340. doi:10.1016/j.cretres.2014.06.015.
- Brown, David. "Birds' Cooperative Breeding Sheds Light on Altruism". washingtonpost.com. The Washington Post. Retrieved 28 August 2014.
- Lü Junchang, Kobayashi, Yoshitsugu, Lee Yuong-Nam & Ji Qiang. (2007). A new Psittacosaurus (Dinosauria: Ceratopsia) specimen from the Yixian Formation of western Liaoning, China: the first pathological psittacosaurid. Cretaceous Research. doi:10.1016/j.cretres.2006.08.005 [published online]
- Boswell, Evelyn. (13 September 2006). "MSU, Mongolian paleontologists find 67 dinosaurs in one week." Montana State University News Service. Accessed 5 May 2007.
- Yang, W.; Li, S.; Jiang, B. (2007). "New evidence for Cretaceous age of the feathered dinosaurs of Liaoning: Zircon U-Pb SHRIMP dating of the Yixian Formation in Sihetun, northeast China". Cretaceous Research 28 (2): 177. doi:10.1016/j.cretres.2006.05.011.
- Lucas, Spencer G (2006). "The Psittacosaurus biochron, Early Cretaceous of Asia". Cretaceous Research 27: 189–198. doi:10.1016/j.cretres.2005.11.011.
- Lucas, Spencer G. (2001). Chinese Fossil Vertebrates, pp. 168-170.
- Wang, S; Hu, H; Li, P; Wang, Y (2001). "Further discussion on the geologic age of Sihetun vertebrate assemblage in western Liaoning, China: evidence from Ar-Ar dating". Acta Petrologica Sinica 17: 663–668.
- Yaoming, Hu; Jin, Meng; Yuanqing, Wang; Chuankui, Li (2005). "Large Mesozoic mammals fed on dinosaurs". Nature 433: 149–152.
- Zhao, Q; Benton, M.J.; Xu, X.; Sander, M.J. (2012). "Juvenile-only clusters and the behaviour of the Early Cretaceous dinosaur Psittacosaurus" (PDF). Acta Palaeontologica Polonica.
- Osborn, H.F. (1923). "Two Lower Cretaceous dinosaurs of Mongolia". American Museum Novitates 95 (13): 1–10.
- Sereno, Paul C. (2010). Taxonomy, cranial morphology, and relationships of parrot-beaked dinosaurs (Ceratopsia:Psittacosaurus). In: Ryan, Michael J., Chinnery-Allgeier, Brenda J. & Eberth, David A. (Eds.). New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium. Bloomington and Indianapolis: Indiana University Press. Pp. 21–58.
- Xu Xing & Zhao Xijin. (1999). Psittacosaur fossils and their stratigraphical implications. In: Wang Y. & Deng T. (Eds.). Proceedings of the Seventh Annual Meeting of the Chinese Society of Vertebrate Paleontology. Beijing: China Ocean Press. Pp. 75–80.
- Sereno, Paul C. (2000). The fossil record, systematics and evolution of pachycephalosaurs and ceratopsians from Asia. In: Benton, Michael J., Shishkin, Mikhail A., Unwin, David M. & Kurochkin, Evgeny N. (Eds.). The Age of Dinosaurs in Russia and Mongolia. Cambridge: Cambridge University Press. Pp. 480–516.
- Archibald, J. David. (1997). Species. In: Currie, Philip J. & Padian, Kevin. The Encyclopedia of Dinosaurs San Diego: Academic Press. Pp. 695–699.
- You, Hai-Lu; Tanoue, Kyo; Dodson, Peter (2008). "New data on cranial anatomy of the ceratopsian dinosaur Psittacosaurus major" (PDF). Acta Palaeontologica Polonica 53 (2): 183–196. doi:10.4202/app.2008.0202.
- Sereno, Paul C. (1990). New data on parrot-beaked dinosaurs (Psittacosaurus). In: Carpenter, Ken & Currie, Philip J. (Eds.). Dinosaur Systematics: Perspectives and Approaches. Cambridge: Cambridge University Press. Pp. 203–210.
- Young, C.C. (1958). "The dinosaur remains of Laiyang, Shantung". Palaeontologia Sinica Series C 16: 53–159.
- Sereno, Paul C.; Xijin, Zhao (1988). "Psittacosaurus xinjiangensis (Ornithischia: Ceratopsia), a new psittacosaur from the Lower Cretaceous of northwestern China". Journal of Vertebrate Paleontology 8: 353–365. doi:10.1080/02724634.1988.10011724.
- Xu Xing. (1997). A new psittacosaur (Psittacosaurus mazongshanensis sp. nov.) from Mazongshan area, Gansu Province, China. In: Dong Z. (Ed.). Sino-Japanese Silk Road Dinosaur Expedition. Beijing: China Ocean Press. Pp. 48–67.
- Leshchinskiy, Sergei V., Fayngertz, Alexei V., Voronkevich, Alexei V., Maschenko, E.N. & Averianov, Alexander O. (2000). Preliminary results of the investigation of the Shestakovo localities of Early Cretaceous vertebrates. In: Komarov, A.V. (Ed.). Materials of the Regional Conference of the Geologists of Siberia, Far East and North East of Russia. Tomsk: GalaPress. Pp. 363–366. [In Russian]
- Buffetaut, Eric; Suteethorn, Varavudh (1992). "A new species of the ornithischian dinosaur Psittacosaurus from the Early Cretaceous of Thailand". Palaeontology 35: 801–812.
- Buffetaut, Eric; Suteethorn, Varavudh (2002). "Remarks on Psittacosaurus sattayaraki Buffetaut & Suteethorn, 1992, a ceratopsian dinosaur from the Lower Cretaceous of Thailand". Oryctos 4: 71–73.
- You Hailu, Xu Xing & Wang Xiaolin. (2003). A new genus of Psittacosauridae (Dinosauria: Ornithopoda) and the origin and early evolution of marginocephalian dinosaurs. Acta Geologica Sinica (English edition) 77(1): 15–20.
- Xing, Xu; Forster, Catherine A.; Clark, James M.; Jinyou, Mo (2006). "A basal ceratopsian with transitional features from the Late Jurassic of northwestern China". Proceedings of the Royal Society of London: Biological Sciences 273: 2135–2140. doi:10.1098/rspb.2006.3566.
- Farke, A. A.; Maxwell, W. D.; Cifelli, R. L.; Wedel, M. J. (2014). "A Ceratopsian Dinosaur from the Lower Cretaceous of Western North America, and the Biogeography of Neoceratopsia". PLoS ONE 9 (12): e112055. doi:10.1371/journal.pone.0112055.