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Timeline of ceratopsian research

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Skeletal mount of Titanoceratops

This timeline of ceratopsian research is a chronological listing of events in the history of paleontology focused on the ceratopsians, a group of herbivorous marginocephalian dinosaurs that evolved parrot-like beaks, bony frills, and, later, spectacular horns. The first scientifically documented ceratopsian fossils were described by Edward Drinker Cope starting in the 1870s; however, the remains were poorly preserved and their true nature was not recognized. Over the next several decades, Cope named several such genera and species. Cope's hated rival, Othniel Charles Marsh, also described ceratopsian remains. In 1887, Marsh mistook a Triceratops horn for one belonging to a new species of prehistoric Bison.[1] Marsh also named the eponymous genus Ceratops in 1888.[2] The next year, he named the most famous ceratopsian, Triceratops horridus. It was the discovery of Triceratops that illuminated the ceratopsian body plan,[1] and he formally named the Ceratopsia in 1890.[3]

The early 20th century was a fruitful time for ceratopsian research. In 1907, Hatcher and others published a monograph on ceratopsid anatomy that is still considered the single most significant publication on the topic to date.[1] Many new species were being described, including Centrosaurus, Styracosaurus, and Chasmosaurus.[4] Not long after, the Central Asiatic Expedition led by Roy Chapman Andrews of the American Museum of Natural History discovered the primitive ceratopsians Psittacosaurus and Protoceratops in Mongolia. Protoceratops gained notoriety as the supposed parent of the first fossil dinosaur eggs known to science.[5] One of these supposed Protoceratops nests preserved the skeleton of a new kind of theropod dinosaur, Oviraptor. It was thought to have been preserved after being killed in the act of raiding the Protoceratops nest. This narrative would last until the 1990s, when the "Protoceratops" eggs were determined to belong to Oviraptor itself.[6]

Throughout the rest of the century, paleontologists would be occupied with several controversies regarding ceratopsian paleobiology. One concerned the stance of the ceratopsid forelimbs. When Marsh first reconstructed the ceratopsid forelimb, he portrayed it in an erect posture. However, when later researchers like Sternberg and Osborn tried to mount the skeletons, they found that the forelimb bones apparently sprawled despite the hindlimbs standing straight up and down. Later researchers like Robert T. Bakker and Gregory S. Paul attempted to revive the erect reconstruction, but continuing research in the 1990s by researchers like John Ostrom, Peter Dodson, and James Farlow found an intermediate value to be better supported.[7]

The original use of the ceratopsids' horns and frills was another long-running controversy in ceratopsian paleontology. Early researchers like Richard Swann Lull thought that bony frills served as the attachment site for enlarged jaw muscles. This explanation was followed by researchers like Russell, Haas, and Ostrom. Sternberg thought the horns of ceratopsians helped defend against predators. In 1961, Davitashvili proposed that ceratopsids used their horns and frills to compete over mates. Farlow and Dodson arrived at the same conclusion in the 1970s, and were followed by Ralph Molnar. Ostrom, who had previously followed the jaw musculature interpretation, came to support this view in 1986. The idea gained further support in the 1990s from researchers like Forster and Sampson.[8]

19th century

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1870s

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Charles Knight's restoration of "Agathaumas sphenocerus" (a dubious species originally described as Monoclonius sphenocerus)

1872

1876

1878

1880s

[edit]
Marsh's reconstruction of Triceratops

1887

  • Despite the description of several ceratopsid taxa by Cope, science still had no concept of what these animals were like due to the scrappy quality of the fossils. Othniel Charles Marsh described the new species Bison alticornis based on horn cores from the animal he would later name Triceratops, not recognizing their dinosaurian origins.[1]

1888

1889

1890s

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1890

Skull from the type specimen of Torosaurus (top). Skull of a young adult below.

1891

1896

  • Barnum Brown discovered a Triceratops skull in Wyoming. It was the first dinosaur fossil Brown ever discovered.[10]

1898

20th century

[edit]

1900s

[edit]
Centrosaurus apertus specimen ROM 767 on exhibit in the Royal Ontario Museum, Toronto, Canada

1901

  • William Temple Hornaday discovered some Triceratops fossils in Montana. These were the first Triceratops fossils to ever be discovered in the Hell Creek Formation.[11]

1902

1904

1905

1907

  • Hatcher and others published a monograph on ceratopsids. This publication has been regarded as the first comprehensive study on ceratopsids and was still regarded as "the most valuable single reference on ceratopsid anatomy" nearly a century later. The researchers classified ceratopsids into two main groups. One consisted of Monoclonius, Triceratops, and their relatives and the other consisted of Ceratops, Torosaurus and their relatives.[12]

1908

  • Lull interpreted ceratopsid frills as sites for the attachment of enlarged jaw muscles.[8]

1910s

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Holotype skeleton of Styracosaurus albertensis

1910

  • An expedition led by Barnum Brown on behalf of the American Museum of Natural History discovered an isolated brainscase in the Horseshoe Canyon Formation. This find represented the first non-ceratopsid neoceratopsian remains discovered in the unit.[13] Field photos suggest that the discovery occurred near the AMNH 5245 "Ankylosaurus" quarry.[14]

1913

  • Lambe described the new genus and species Styracosaurus albertensis.[3] The frill of Styracosaurus bore three pairs of long, bony spikes, giving it a spectacular and formidable appearance.[15]

1914

Artist's restoration of Leptoceratops
G. F. Sternberg preparing the skull of Chasmosaurus belli

1915

1917

1918

1920s

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Skeletal reconstruction of Pentaceratops

1922

1923

Skeletal reconstruction of two Protoceratops and a nest

1924

  • Osborn described the new non-ceratopsian theropod dinosaur genus and species Oviraptor philoceratops.[22] Since a specimen was found preserved on top of a nest of eggs presumed to belong to Protoceratops and its short toothless beak seemed adapted to cracking open eggs, Osborn thought that it was smothered by a sandstorm while in the act of raiding the nest.[6]

1925

Skull of Anchiceratops
  • Charles Mortram Sternberg described the fossilized skin of Chasmosaurus belli. The skin was preserved as an impression of skin covering the right side of the animal's pelvic region. C. belli had skin covered in small "nonimbricating" polygonal scales interspersed with rows of larger rounded plates up to 5.5 cm across spaced between 5 and 10 cm across.[17]

1928

  • Tait and Barnum Brown interpreted ceratopsids as low browsers than fed on herbaceous plants.[23]

1927

  • A Chasmosaurus skeletal mount was created for the National Museum of Canada. It was the first skeletal mount of Chasmosaurus ever created and the third skeletal mount of any ceratopsid.[7]
  • Sternberg argued that while the hindlimbs of Triceratops stood straight up and down, its forelimbs sprawled.[7]

1929

1930s

[edit]
Henry Fairfield Osborn lent his support to reconstructing Triceratops with sprawling forelimbs.

1930

1931

1933

  • Brown described the species Chasmosaurus kaiseni.[3]
  • Brown described the species Triceratops maximus.[2]
  • Lull described the species Chasmosaurus brevirostris.[3]
  • Lull described the fossilized skin of Monoclonius cutleri. The skin was preserved as an impression of skin near the far end of the animal's thigh. The skin of M. cutleri was similar to that of Chasmosaurus belli, which had skin covered in small "nonimbricating" polygonal scales interspersed with rows of larger rounded plates up to 5.5 cm across. The larger plate-like scales of M. cutleri, however, were more widely spaced than the 5–10 cm intervals seen in C. belli.[17]
  • Lull classified ceratopsids into two groups based on frill length in a scheme similar to that devised by Hatcher and others in 1907. Ceratopsids which he regarded as short-frilled forms include Centrosaurus, Styracosaurus, and Triceratops. Long-frilled taxa included Anchiceratops, Arrhinoceratops, Chasmosaurus, Pentaceratops, and Torosaurus.[12]
Skeleton of Styracosaurus "parksi"
  • Osborn concurred with Sternberg's opinion that the forelimbs of Triceratops sprawled despite the erect posture of the hindlimb.[7]

1935

1937

1940s

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Skeletal mount of Chasmosaurus russelli

1940

1942

1946

1947

  • Colbert and Bump observed that ceratopsids like Pentaceratops and Torosaurus had the largest skulls on any terrestrial vertebrate.[1]

1949

  • Sternberg described the species Triceratops albertensis.[2]
  • Sternberg followed the division of the Ceratopsidae into short-frilled and long-frilled forms, but regarded Triceratops as an unusually short-frilled member of the long-frilled group.[12]

1950s

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Pachyrhinosaurus canadensis skull on display at the Royal Tyrrell Museum

1950

1951

1953

1955

  • Haas interpreted ceratopsid frills as sites for the attachment of enlarged jaw muscles.[8]

1958

1959

1960s

[edit]
Davitashvili and others have argued that ceratopsids used their spectacular horns and frills in competitions over mates.

1960

  • Murray and others reported ceratopsid remains from Mexico.[1]

1961

  • Davitashvili proposed that ceratopsids used their horns and frills in intraspecific competition over mates or territory. This hypothesis is supported by the observation that the horns and frills of ceratopsids are the primary source of variation between species within the family.[8]

1962

1964:

  • John Ostrom described the functional morphology of ceratopsid jaws for the first time. He concluded that they fed on tough gymnosperms with significant fiber contents like palms and cycads.[23] He also interpreted ceratopsid frills as sites for the attachment of enlarged jaw muscles.[8]
  • Don Taylor of the Provincial Museum of Alberta (now called the Royal Alberta Museum) found evidence of another Centrosaurus bonebed near Hilda, Alberta.[25]

1966

  • Ostrom further described the functional morphology of ceratopsid jaws. He observed that the ceratopsian beak was probably not designed for biting but was better suited for "grasping and plucking".[23] He also interpreted ceratopsid frills as sites for the attachment of enlarged jaw muscles.[8]
  • Taylor's work on the second apparent Centrosaurus bonebed near Hilda, Alberta concluded.[25]

1967

  • Langston found additional support for Sternberg's reclassification of Triceratops among the long-frilled ceratopsids among the anatomical characteristics of its premaxilla. He also classified Pachyrhinosaurus among the short-frilled ceratopsids.[12]

1969

  • Steel followed Lull's division of the Ceratopsidae into short-frilled and long-frilled forms.[12]

1970s

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The fighting dinosaurs specimen of Protoceratops and Velociraptor

1971

  • Richard Thulborn followed Lull's division of the Ceratopsidae into short-frilled and long-frilled forms.[12]

1972

1975

Skull of Bagaceratops
Artistic restoration of Bagaceratops

1976

  • Dodson published research on the sexual dimorphism present in the skull of Protoceratops.[26] He found the sexes to vary based on the size of the ridge on the nose and the shape of the frill.[12]

1977

  • Ralph Molnar supported the hypothesis that ceratopsids used their horns and frills in competition over mates. This hypothesis is supported by the observation that the horns and frills of ceratopsids are the primary source of variation between species within the family.[8]
  • A Centrosaurus bone bed was discovered in Dinosaur Provincial Park. The site was later become known as Quarry 143.[27]

1978

  • Wheeler suggested that the horns and frills of ceratopsids primarily helped the animal regulate its body temperature based on these organs' large surface area and abundance of blood vessels.[8]

1979

  • Spassov supported the hypothesis that ceratopsids used their horns and frills in competition over mates.[8]
  • Paleontologists began excavating the Quarry 143 Centrosaurus bonebed.[27]

1980s

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Artist's restoration of Centrosaurus

1981

  • Colbert followed Lull's division of the Ceratopsidae into short-frilled and long-frilled forms.[12]

1983

1984

Skeletal mount of Triceratops "elatus", one of many species synonymized with Triceratops horridus in the 1980s

1985

  • David Norman followed Lull's division of the Ceratopsidae into short-frilled and long-frilled forms.[12]

1986

  • Paul Sereno named the Neoceratopsia.[19]
  • Dodson described the new genus and species Avaceratops lammersi.[3]
  • Ostrom supported the hypothesis that ceratopsids used their horns and frills in competition over mates.[8]
  • Ostrom and Peter Wellnhofer argued that the various described species of Triceratops showed no more anatomical variation between each other than can be observed between individuals of any given species of modern horned mammal. Consequently, they considered all 16 named species to be synonymous, leaving T. horridus as the only valid Triceratops species.[29] They supported the hypothesis that ceratopsids used their horns and frills in competition over mates.[8]
  • Robert T. Bakker supported the interpretation of ceratopsid horns and frills hypothesizing their use in defense against predators like tyrannosaurids.[8]

1987

  • Bakker illustrated ceratopsids with upright forelimbs.[7]
Artist's restoration of Turanoceratops
  • Gregory S. Paul illustrated ceratopsids with upright forelimbs.[7]
  • Brouwers and others reported ceratopsid remains from a site that would have been located at a latitude of 85 degrees North during the Cretaceous.[30]
  • Cobabe and Fastovsky described the new genus and species Ugrosaurus olsoni.[2]
  • Lehman reported that 61–71% of the fossils found in deposits dating to the end of the Cretaceous period belong to a few ceratopsids, like Torosaurus and Triceratops.[1]
  • Lehman argued that ceratopsids preferred coastal habitats over more inland regions.[28]
  • Parrish and others reported ceratopsid remains from the North Slope of Alaska.[1]
  • Farlow studied the diet and digestive physiology of herbivorous dinosaurs and concluded that ceratopsids probably had slow metabolisms for their body size and used gut microbes to break-down low quality plant material during digestion.[23]
  • Coe and others argued that ferns were probably a major food source for herbivorous dinosaurs like ceratopsids and may have grown in vast "prairies" that could feed large numbers of dinosaurs.[31]
Artist's restorations of "Chasmosaurus" (now Agujaceratops) mariscalensis
  • Coombs recognized some Asian fossils purported to be isolated ceratopsid horns as actually belonging to armored ankylosaurs.[1]

1988

1989

1990s

[edit]
The status of Triceratops as a "long-frilled" ceratopsid became a consensus view in the early 1990s.

1990

  • Brinkman argued that ceratopsids preferred coastal habitats over more inland regions.[28]
  • Kurzanov erected the new genus Breviceratops for the species Protoceratops kozlowskii that had been described by Maryanska and Osmolska in 1975.[19]
  • Dodson osberved that psittacosaurs are among the most common dinosaurs in the fossil record.[26]
  • Dodson claimed to have found evidence for sexual dimorphism in the horns and frills of centrosaurines.[12] Dodson performed a cladistic analysis of the centrosaurines.[12] He observed that Triceratops is one of the most common dinosaurs in the fossil record.[28]
  • Dodson and Currie performed a cladistic analysis of the ceratopsids found further support for regarding Triceratops as a "long-frilled" ceratopsid.[12]
  • Lehman supported Ostrom and Wellnhofer's conclusion that there was only one valid species of Triceratops.[29] He divided the Ceratopsidae into two subfamilies originally named by Lambe, the Centrosaurinae and the Chasmosaurinae. This has been the accepted classification scheme for ceratopsids ever since.[12]
  • Lehman performed a cladistic analysis of the Chasmosaurines.[12]
  • Sereno reported the association of 50 gastroliths associate with two psittacosaurid skeletons. These gastroliths probably helped break down the plants it ate. He also noticed that the first toe of the front foot was offset from the others and could probably be used to grasp vegetation.[26]
  • Catherine Forster argued that there was no satisfactory evidence for sexual dimorphism in ceratopsids.[12] She also joined the growing consensus that Triceratops should be classified among the long-frilled ceratopsids.[12] Forster performed a cladistic analysis of the ceratopsids. She argued against the idea that ceratopsid frills served as attachment sites for large jaw muscles. She observed that the opening in the skull above the animal's temple seems to show the physical location extent of the jaw muscle attachment point. She supported the hypothesis that ceratopsids used their horns and frills in competition over mates.[8]
  • Rogers observed that ceratopsid bonebeds are associated with signs that the local ancient climate had seasonal or semiarid levels of precipitation and speculated that drought was likely responsible for the deaths of these dinosaurs.[28]

1991

  • Paul illustrated ceratopsids with upright forelimbs.[7]

1992

Fossil eggs like these were actually laid by the bird-like theropod Oviraptor, not Protoceratops.
  • Kurzanov described the new genus and species Udanoceratops tschizhovi.[16]
  • Horner and others observed that ceratopsid horns and frills are only fully developed at sexual maturity. They hypothesized that since ceratopsid bodies were generally fairly similar, changes in cranial adornments played a major role in ceratopsid evolution.[33]

1993

  • Dong and Currie reported Protoceratops embryos from Bayan Mandhu in China.[26]
  • Osmolska challenged Kielan-Jawarowska and Barsbold's 1972 interpretation of an associated skeleton of Velociraptor and Protoceratops as being of two animals killed and preserved while locked in mortal combat. She reinterpreted the association as a Velociraptor that had been killed while scavenging an already dead Protoceratops.[34]
  • Clemens and Nelms reported centrosaurine remains from Alaska.[32]
  • Dodson supported the intraspecific competition over mates interpretation of ceratopsid horns and frills with the observation that the horns and frills of ceratopsids are the primary source of variation between species within the family.[8]

1994

1995

  • Nessov described the new genus and species Kulceratops kulensis.[16]
  • Nessov argued that Turanoceratops was a ceratopsid because it had horns and teeth with two roots.[32]
Skull of Einiosaurus procurvicornis
  • Scott D. Sampson described the new genus and species Achelousaurus horneri.[3] Sampson described the new genus and species Einiosaurus procurvicornis.[3]
  • Sampson performed a cladistic analysis of the centrosaurines.[12]
  • Sampson supported the intraspecific competition over mates interpretation of ceratopsid horns and frills with the observation that the horns and frills of ceratopsids are the primary source of variation between species within the family.[33]
  • Sampson observed that ceratopsid horns and frills are only fully developed at sexual maturity.[33]
  • Godfrey and Holmes examined variability within Chasmosaurus and concluded that it contained two valid species; C. russelli and C. belli.[29] Godfrey and Holmes performed a cladistic analysis of Chasmosaurus.[12]
  • Johnson and Ostrom studied the anatomy of the ceratopsid forelimb and concluded that it was inconsistent with a fully erect stance despite the tendency of artists to draw them that way. Instead they concluded that ceratopsids stood with the front limbs in a semi-erect posture.[7]
  • Martin Lockley and Adrian Hunt named the new ichnogenus and ichnospecies Ceratopsipes goldenensis, interpreting it as fossilized ceratopsid footprints. They argued that the narrow width of the foreprints were evidence for the upright forelimb hypothesis and inconsistent with sprawling reconstructions.[7]

1996

Artistic restoration of Achelousaurus horneri
  • Forster used cladistics and morphometrics to determine, which, if any of the species referred to Triceratops are valid. She found that Triceratops came in two varieties, both found in the same rocks in the same places. One corresponded with the type species T. horridus, and the other with the referred species T. prorsus. She concluded that these were probably both valid species, although admitted the possibility that these forms were males and females of the same species. She also considered Diceratops hatcheri to be a valid genus and species.[29]
  • She argued against the idea that ceratopsid frills served as attachment sites for large jaw muscles.[8]
  • Eberth estimated a ceratopsid bonebed to preserve more than a thousand individuals.[28]
  • Dodson studied the anatomy of the ceratopsid forelimb and concluded that it was inconsistent with a fully erect stance despite the tendency of artists to draw them that way. Instead they concluded that ceratopsids stood with the front limbs in a semi-erect posture. He argued against the interpretation Lockley and Hunt made of the forprints left behind by the trackmaker of their 1995 ichnospecies Ceratopsipes goldenensis as supporting the erect-forelimb hypothesis, instead Dodson suggested that the width of the Ceratopsipes foreprints were still consistent with the sprawling reconstruction supported by the actual limb anatomy.[7]
  • Dodson disagreed with Ostrom's suggestion that ceratopsids fed on ferns and cycads because the flora of the late Cretaceous environments of Alberta were largely made up of other kinds of plants and this is the time and place in earth's history where ceratopsids were at their most diverse.[31]
  • Dodson argued against the idea that ceratopsid frills served as attachment sites for enlarged jaw muscles.[8]
  • Dodson supported the hypothesis that ceratopsids used their horns and frills in competition over mates. Dodson supported the intraspecific competition over mates interpretation of ceratopsid horns and frills with the observation that the horns and frills of ceratopsids are the primary source of variation between species within the family. Dodson also observed that in modern animals horns are primarily used to acquire mates.[8]
  • Barrick and others found evidence for a temperature gradient across the horns and frills of ceratopsids. This is consistent with Wheeler's 1978 hypothesis that these organs evolved to help regulate the animals' temperatures.[8]
  • Dong and Currie reported the discovery of an oviraptorid from the Djadokhta Formation of northern China preserved on top of a nest of eggs. This overturned more than 60 years of interpreting the Oviraptor of the Central Asiatic Expeditions as a rapacious egg-thief in favor of it likely being a faithful mother at her nest.[6]
  • The Royal Tyrell Museum finally performed a preliminary survey of the bonebeds studied by Langston and Taylor in the 1950s and 1960s. The survey discovered entire new bonebeds in the area.[35]

1997

  • Dodson and Farlow studied the anatomy of the ceratopsid forelimb and concluded that it was inconsistent with a fully erect stance despite the tendency of artists to draw them that way. Instead they concluded that ceratopsids stood with the front limbs in a semi-erect posture. They also concluded that Lockley and Hunt had overextended themselves by trying to infer limb posture from the Ceratopsipes footprints, which they felt was impossible.[7]
The Alaskan Pachyrhinosaurus species P. perotorum
  • Xu described the species Psittacosaurus mazongshanensis.[19]
  • Dong and Azuma described the new genus and species Archaeoceratops oshimai.[19]
  • Matsumoto found the limb posture of Protoceratops to be typical of neither reptiles, nor mammals.[26]
  • Rich and others reported the presence of Pachyrhinosaurus remains in Alaska.[1]
  • Williamson reported centrosaurine remains from the Menefee Formation in New Mexico.[1]
  • Lehman argued that the two supposedly distinct species of Chasmosaurus were really just variant individuals of a single species.[29]

Sampson and others studied centrosaurine bonebeds and found that the individuals preserved therein could be categorized into three broad phases of developments; juveniles, subadults, and adults. The researchers defined these age groups based on specimens' body size, the surface texture of their bones, and how completely closed the sutures between their bones were.[36] They observed that the juveniles and subadults of different centrosaurine species are practically indistinguishable and can only be told apart upon reaching adulthood when their horns and frills were fully developed.[12]

The ontogeny of Centrosaurus skulls

Sampson and the other researchers interpreted the delay of ceratopsid horn and frill development to sexual maturity as further evidence for the hypothesis that these traits evolved primarily for competition over mates. They disagreed with more functional explanations for these structures, like the idea that the frills served as attachment points for enlarged jaw muscles. The researchers also marshalled support from the fact that the horns and frills of ceratopsids are the primary source of variation between species within the family and observations of modern animals, whose horns are also primarily used to acquire mates.[8] Nevertheless, they argued that there was still no evidence for sexual dimorphism in ceratopsids.[12]

The researchers argued that the anatomical variation in horns and frills and their delayed development had taxonomic implications. They concluded that species based on immature type specimens like Brachyceratops montanensis and Monoclonius crassus were dubious because immature individuals would not yet have developed the primary traits paleontologists rely on to distinguish one kind of ceratopsid from another. Likewise, they dismissed Avaceratops as just a juvenile rather than a small adult from a distinct taxon. Sampson and the other researchers noted that bonebeds differing in location and age all preserved "Monoclonius-like" fossils left behind by immature animals, which is consistent with the idea that these remains are actually the juveniles of a variety of species from different times and places rather than a unique kind of animal in their own right.[12]

  • Sampson supported the hypothesis that ceratopsids used their horns and frills in competition over mates.[8]
  • Sereno disagreed with Nessov's claim that Turanoceratops was a ceratopsid. Instead, Sereno found Turanoceratops to be the closest known relative of the family without technically being a member itself. Its position at the base of the ceratopsid family tree suggests that the family originated in Asia.[32]
  • White and others observed that remains of Triceratops have been found in every kind of depositional environment preserved by the Hell Creek Formation. They also noticed that even though Triceratops remains are widespread and common, they are not found in bonebeds like many ceratopsids are.
  • Carrano studied dinosaur locomotion. He concluded that ceratopsids were highly graviportal and may not have been able to gallop.[7]
  • Barrick and others found additional evidence for a temperature gradient across the horns and frills of ceratopsids. This is consistent with Wheeler's 1978 hypothesis that these organs evolved to help regulate the animals' temperatures.[8]
  • The Royal Tyrell Museum intensified its investigation of the bonebeds near Hilda, Alberta. In only two days, researchers discovered 14 separate bonebeds in one mudstone bed that extended for at least 7 km, with 3.7 km worth of visible outcrops.[37]

1998

1999

Artistic restoration of Chaoyangsaurus youngi
  • Zhao, Cheng, and Xu described the new genus and species Chaoyangsaurus youngi.[16] They contended that the presence of such an early, primitive ceratopsian in Asia suggested that this continent was where the ceratopsians first originated.[30]
  • Swisher and others dated the Psittacosaurus fossils of the Yixian Formation to near the Barremian-Aptian boundary based on Argon-Argon radiometric dating.[26]
  • Chinsamy and Trexler noted that the fossil record of basal neoceratopsians is actually of relatively high quality. They found that complete skulls were known for about half of the genera named up to this point and many had good postcranial remains and/or multiple specimens.[26]
  • Clark and others argued that it was impossible to know whether or not Velociraptor was a predator of Protoceratops based on the famous "fighting dinosaurs" specimen, since this was only one specimen.[34]
  • Penkalski and Dodson argued that Avaceratops was not a true ceratopsid after all. It was, however, the family's nearest known evolutionary relative. They performed a cladistic analysis of the centrosaurines.[12]
  • Andersen and others used computers to model the kinetics of the Triceratops skeleton curated by the Smithsonian Institution.[7]
  • Chapman and others used computers to model the kinetics of the Triceratops skeleton curated by the Smithsonian Institution.[7]
  • Jabo and others used computers to model the kinetics of the Triceratops skeleton curated by the Smithsonian Institution.[7]
  • Sampson hypothesized that since ceratopsid bodies were generally fairly similar, changes in cranial adornments played a major role in ceratopsid evolution.[38]

21st century

[edit]

2000s

[edit]
Artistic restoration of Graciliceratops mongoliensis

2000

  • Paul and Christiansen studied ceratopsid forelimbs and concluded that in life the animal probably stood with its elbows slightly everted but with its forelimbs otherwise erect. They also concluded that ceratopsians had faster running speeds than modern elephants and were able to gallop.[7]
  • Sereno described the new genus and species Graciliceratops mongoliensis.[16]
  • Lambert and others described the new species Protoceratops hellenikorhinus.[16]
  • Shuvalov reported Psittacosaurus fossils from near the Berriasian-Valanginian boundary in the Sangiin Dala Nuur depression. Most Psittacosaurus fossils date to an age closer to the Barremian-Aptian boundary.[26]
  • Erickson and Tumanova reported Psittacosaurus mongoliensis fossils from Khamaryn Us in Mongolia that ranged from 0.9 kg juveniles to 19.9 kg adults. They found that it took 9 years for a Psittacosaurus to become fully grown. To reach that size in that time frame it must have grown at a rate of 12.5 grams per day. This is four times faster than modern reptiles and 25% faster than modern marsupials. However it is only three to twenty times as slow as modern eutherian mammals and birds.[26]
  • Weishampel and others reported the presence of fifteen Protoceratops hatchlings from a single nest in an Aeolian sandstone deposit in the central Gobi Desert.[26]

2001

  • Tang and others dated Psittacosaurus mazongshanensis to near the Barremian-Aptian boundary based on fossil pollen and spores.[26]
  • Witmer studied the nasal passages of ceratopsids. He found that the nasal vestibule of cerastopsids is complex and may have helped regulate the animal's body temperature through its effect on inhaled air.[31]
Skull of Protoceratops hellenikorhinus
  • Tereshchenko reported that Protoceratops andrewsi had sexual dimorphism in its body in addition to its head.[26]
  • Lambert and others reported sexual dimorphism in Protoceratops hellenikorhinus.[26]
  • Holmes and others found that the two Chasmosaurus species argued to be valid by Godfrey and Holmes are found at different positions within the stratigraphic column of the Dinosaur Park Formation. This finding bolstered the idea that these species were distinct after all. They also described a new species, Chasmosaurus irvinensis, which was discovered in Dinosaur Park Formation rocks deposited more recently than either previously described Chasmosaurus species.[29]
  • Peter J. Makovicky formally described the braincase attributed to the small ceratopsian dinosaur Montanoceratops cerorhynchus.[13] This specimen is currently cataloged as AMNH 5244.[39] Makovicky found that it shares anatomical features with Leptoceratops gracilis.[13] The shared features between the two taxa's braincases contradicts previous phylogenetic studies which had suggested that they were not closeley related.[40] M. cerorhynchus had been previously known from the contemporary St. Mary River Formation and Makovicky's referral of AMNH 5224 to the species expanded its known paleobiogeographic range.[13] Makovicky performed a phylogenetic analysis to clarify the relationship between ceratopsian in the light of the new braincase data.[41] Makovicky concluded from his analysis that at least three dispersal events from Asia to North America are required to explain the paleobiogeography of neoceratopsians. The patterns of distribution and dispersal are similar to those found in other contemporary taxa like oviraptorosaurs, troodonts, and multituberculate mammals.[42]

2002

Artistic restoration of Liaoceratops
  • Swisher and others dated the Psittacosaurus fossils of the Yixian Formation to near the Barremian-Aptian boundary based on Argon-Argon radiometric dating.[26]
  • Xu and others described the new genus and species Liaoceratops yangzigouensis.[16]
  • Makovicky re-examined the type specimen of Turanoceratops. Nessov had claimed that this genus was a ceratopsid because it had horns and teeth with two roots, but Makovicky found that the teeth were single rooted after all and the supposed eye-horn may actually have come from and armored dinosaur. Since it had no good distinguishing traits, Makovicky regarded the genus as dubious.[32]

2003

2004

Skeletal mount of Prenoceratops

2005

2006

Artistic restoration of Agujaceratops

2007

Skull of Eotriceratops

2008

2009

2010s

[edit]
Skull of Diabloceratops eatoni

2010

Artistic restoration of Sinoceratops

2011

Pachyrhinosaurus perotorum pair

2012

2013

2014

2015

2016

2017

  • Rivera-Sylva and others described the new genus and species Yehuecauhceratops mudei.
  • Andrew Farke and George Philips described evidence of ceratopsidae in Appalachia.

2018

2019

2020s

[edit]

2020

2022

See also

[edit]

Footnotes

[edit]
  1. ^ a b c d e f g h i j k l m Dodson, Forster, and Sampson (2004); "Introduction", page 494.
  2. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac ad ae af ag Dodson, Forster, and Sampson (2004); "Table 23.1: Ceratopsidae", page 496.
  3. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab ac Dodson, Forster, and Sampson (2004); "Table 23.1: Ceratopsidae", page 495.
  4. ^ Dodson, Forster, and Sampson (2004); "Table 23.1: Ceratopsidae", pages 495–496.
  5. ^ Lavas (1999); "American Museum Expeditions to the Gobi," pages 35–37.
  6. ^ a b c d Osmolska, Currie, and Barsbold (2004); "Paleoecology", page 183.
  7. ^ a b c d e f g h i j k l m n o p q r s Dodson, Forster, and Sampson (2004); "Posture and Locomotion", page 511.
  8. ^ a b c d e f g h i j k l m n o p q r s t u v w x Dodson, Forster, and Sampson (2004); "Horns and Frills", page 512.
  9. ^ Tanke (2010); "Background and Collection History," page 541.
  10. ^ Moore (2014); "1896" (3), page 109.
  11. ^ a b Moore (2014); "1901" (4), page 124.
  12. ^ a b c d e f g h i j k l m n o p q r s t u v w x Dodson, Forster, and Sampson (2004); "Phylogeny and Evolution", page 508.
  13. ^ a b c d Makovicky (2001); "Abstract," page 243.
  14. ^ Makovicky (2001); "Introduction," page 245.
  15. ^ Dodson (1996); "Styracosaurus- The Spear-Bearer", page 165.
  16. ^ a b c d e f g h i j k l m n o You and Dodson (2004); "Table 22.1: Basal Ceratopsia", page 480.
  17. ^ a b c d Dodson, Forster, and Sampson (2004); "Integument", page 506.
  18. ^ Carpenter (1999); "First Discoveries," page 2.
  19. ^ a b c d e f g h i j k l You and Dodson (2004); "Table 22.1: Basal Ceratopsia", page 479.
  20. ^ Carpenter (1999); "First Discoveries," page 4.
  21. ^ Lavas (1999); "American Museum Expeditions to the Gobi," pages 35–36.
  22. ^ Osmolska, Currie, and Barsbold (2004); "Table 8.1: Oviraptorosauria", page 166.
  23. ^ a b c d e Dodson, Forster, and Sampson (2004); "Feeding, Diet, and Respiration", page 511.
  24. ^ Moore (2014); "1929" (7), page 182.
  25. ^ a b c Eberth, Brinkman, and Barkas (2010); "Introduction", page 496 and "The Site", Eberth.
  26. ^ a b c d e f g h i j k l m n o p q r You and Dodson (2004); "Biostratigraphy, Taphonomy, Paleoecology, and Biogeography", page 492.
  27. ^ a b Moore (2014); "1977" (5), page 272.
  28. ^ a b c d e f g Dodson, Forster, and Sampson (2004); "Taphonomy and Paleoecology", page 510.
  29. ^ a b c d e f Dodson, Forster, and Sampson (2004); "Phylogeny and Evolution", page 507.
  30. ^ a b You and Dodson (2004); "Biostratigraphy, Taphonomy, Paleoecology, and Biogeography", page 493.
  31. ^ a b c Dodson, Forster, and Sampson (2004); "Feeding, Diet, and Respiration", page 512.
  32. ^ a b c d e Dodson, Forster, and Sampson (2004); "Historical Biogeography", page 510.
  33. ^ a b c Dodson, Forster, and Sampson (2004); "Evolution within Ceratopsidae", page 512.
  34. ^ a b Norell and Makovicky (2004); "Paleoecology", page 209.
  35. ^ Eberth, Brinkman, and Barkas (2010); "Introduction", page 496.
  36. ^ Dodson, Forster, and Sampson (2004); pages "Phylogeny and Evolution", 507–508.
  37. ^ Eberth, Brinkman, and Barkas (2010); "Introduction", page 497 and "The Site", Eberth.
  38. ^ Dodson, Forster, and Sampson (2004); "Evolution within Ceratopsidae", page 513.
  39. ^ Makovicky (2001); "Introduction," page 244.
  40. ^ Makovicky (2001); "Abstract," pages 243–244.
  41. ^ Makovicky (2001); "Discussion," page 253.
  42. ^ Makovicky (2001); "Discussion," page 255.
  43. ^ Tereschenko and Alifanov (2003); "Abstract," page 293.
  44. ^ a b Alifanov (2003); "Abstract," page 524.
  45. ^ You and Dong (2003); "Abstract," page 299.
  46. ^ You, Xu, and Wang (2003); "Abstract," page 15.
  47. ^ Rich and Vickers-Rich (2003); "Abstract," page 1.
  48. ^ Chinnery (2004); "Abstract," page 572.
  49. ^ You et al. (2005); "Abstract," page 593.
  50. ^ Lucas, Sullivan, and Hunt (2006); "Abstract," page 367.
  51. ^ Zhao et al. (2006); "Abstract," page 467.
  52. ^ Makovicky and Norell (2006); "Abstract," page 1.
  53. ^ Xu et al. (2006); "Abstract," page 2135.
  54. ^ Ryan (2007); "Abstract," page 376.
  55. ^ Chinnery and Horner (2007); "Abstract," page 625.
  56. ^ Wu et al. (2007); "Abstract," page 1243.
  57. ^ a b Mateus (2008); "Abstract," page 423.
  58. ^ Alifanov (2008); "Abstract," page 621.
  59. ^ Ohashi and Barrett (2009); "Abstract," page 748.
  60. ^ Jin et al. (2009); "Abstract," page 200.
  61. ^ Ősi, Butler, and Weishampel (2010); "Abstract," page 466.
  62. ^ You, Tanque, and Dodson (2010); "Abstract," page 59.
  63. ^ Loewen et al. (2010); "Abstract," page 99.
  64. ^ Kirkland and DeBlieux (2010); "Abstract," page 117.
  65. ^ a b c Sampson et al. (2010); "Abstract," page 1.
  66. ^ Ryan, Russell and Hartman (2010); "Abstract," page 505.
  67. ^ Longrich (2010); "Abstract," page 681.
  68. ^ Sullivan and Lucas (2010); "Abstract," page 169.
  69. ^ Sereno, Zhao and Lin (2010); "Abstract," page 199.
  70. ^ McDonald and Horner (2010); "Abstract," page 156.
  71. ^ Xu et al. (2010); "Abstract," page 1631.
  72. ^ Ott and Larson (2010); "Abstract," page 203.
  73. ^ Xu et al. (2010); "Abstract," page 1.
  74. ^ Lee, Ryan and Kobayashi (2011); "Abstract," page 39.
  75. ^ Farke et al. (2011); "Abstract," page 691.
  76. ^ Longrich (2011); "Abstract," page 264.
  77. ^ a b Ryan, Evans and Shepherd (2012); "Abstract," page 1251.
  78. ^ Ryan et al. (2012); "Abstract," page 69.
  79. ^ Fiorillo and Tykoski (2012); "Abstract," page 561.
  80. ^ Wick and Lehman (2013); "Abstract," page 667.
  81. ^ Longrich (2013); "Abstract," page 51.
  82. ^ Sampson et al. (2013); "Abstract," page 1.
  83. ^ Ryan et al. (2014); "Abstract," page 505.
  84. ^ Longrich (2014); "Abstract," page 292.
  85. ^ Farke et al. (2014); "Abstract," page 1.
  86. ^ Brown and Henderson (2015); "Abstract," page 1641.
  87. ^ Zheng, Jin, and Xu (2015); "Abstract," page 1.
  88. ^ Evans and Ryan (2015); "Abstract," page 1.
  89. ^ Han et al. (2015); in passim.
  90. ^ He et al. (2015); in passim.
  91. ^ Mallon et al. (2016); in passim.
  92. ^ Lund et al. (2016); in passim.
  93. ^ Sebastian G. Dalman; John-Paul M. Hodnett; Asher J. Lichtig; Spencer G. Lucas (2018). "A new ceratopsid dinosaur (Centrosaurinae: Nasutoceratopsini) from the Fort Crittenden Formation, Upper Cretaceous (Campanian) of Arizona". New Mexico Museum of Natural History and Science Bulletin. 79: 141–164.
  94. ^ Qi Zhao; Michael J. Benton; Shoji Hayashi; Xing Xu (2019). "Ontogenetic stages of ceratopsian dinosaur Psittacosaurus in bone histology". Acta Palaeontologica Polonica. 64. doi:10.4202/app.00559.2018.
  95. ^ Qian-Nan Zhang; James L. King; Da-Qing Li; Ye-Mao Hou; Hai-Lu You (2019). "Endocranial morphology of Auroraceratops sp. (Dinosauria: Ceratopsia) from the Early Cretaceous of Gansu Province, China". Historical Biology: An International Journal of Paleobiology. 32 (10): 1–6. doi:10.1080/08912963.2019.1588893. S2CID 91650220.
  96. ^ Łukasz Czepiński (2019). "Ontogeny and variation of a protoceratopsid dinosaur Bagaceratops rozhdestvenskyi from the Late Cretaceous of the Gobi Desert". Historical Biology: An International Journal of Paleobiology. 32 (10): 1–28. doi:10.1080/08912963.2019.1593404. S2CID 132780322.
  97. ^ Brandon P. Hedrick; Erika Goldsmith; Hector Rivera‐Sylva; Anthony R. Fiorillo; Allison R. Tumarkin‐Deratzian; Peter Dodson (2019). "Filling in gaps in the ceratopsid histologic database: Histology of two basal centrosaurines and an assessment of the utility of rib histology in the Ceratopsidae". The Anatomical Record. 303 (4): 935–948. doi:10.1002/ar.24099. PMID 30773832.
  98. ^ Ronald S. Tykoski; Anthony R. Fiorillo; Kentaro Chiba (2019). "New data and diagnosis for the Arctic ceratopsid dinosaur Pachyrhinosaurus perotorum". Journal of Systematic Palaeontology. 17 (16): 1177–1196. Bibcode:2019JSPal..17.1397T. doi:10.1080/14772019.2018.1532464. S2CID 92034503.
  99. ^ Arbour, Victoria; Evans, David (2019). "A new leptoceratopsid dinosaur from Maastrichtian-aged deposits of the Sustut Basin, northern British Columbia, Canada". PeerJ. 7: e7926. doi:10.7717/peerj.7926. PMC 6842559. PMID 31720103.
  100. ^ Fowler, D.W.; Freedman Fowler, E.A. (2020). "Transitional evolutionary forms in chasmosaurine ceratopsid dinosaurs: evidence from the Campanian of New Mexico". PeerJ. 8: e9251. doi:10.7717/peerj.9251. PMC 7278894. PMID 32547873.
  101. ^ Dalman, S.G.; Lucas, S.G.; Jasinski, S.E.; Longrich, N.R. (2022). "Sierraceratops turneri, a new chasmosaurine ceratopsid from the Hall Lake Formation (Upper Cretaceous) of south-central New Mexico". Cretaceous Research. 130: Article 105034. Bibcode:2022CrRes.13005034D. doi:10.1016/j.cretres.2021.105034. S2CID 244210664.

References

[edit]
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