CERATOPSIA

THE HORNED AND FRILLED DINOSAURS

(Related to Chapter 9 in Fastovsky and Weishampel)


A sketch of Triceratops made by E. L. Crisp, 1995 (reconstruction based on a 1:40 model from The Carnegie Museum).

INDRODUCTION

     We will now turn our attention to the other clade of the Marginocephalia, the Ceratopsia.


Cladogram of the Ornithischia.  The Ceratopsia are outlined in blue (Slightly modified from Dingus and Rowe, 1997).

     The horned dinosaurs are some of the ones that are most familiar to us.  For example, Triceratops in combat with Tyrannosaurus rex is a favorite scene in movies.


A Late Cretaceous scene showing Tyrannosaurus rex with his bounty, a Triceratops that he has "bagged". This picture was photographed by E. L. Crisp at The Carnegie Museum of Natural History.
 

CERATOPSIA

Cladogram of the GenasauriaLecture 18: Early Cretaceous II
From: http://rainbow.ldeo.columbia.edu/courses/v1001/liaoning16.html
     1. cheeks
     2. armor
     3. armor as plates covering back
     4. armor as spikes or plates
     5. uneven enamel
     6. back part of skull makes shelf
     7. rostral bone
     8. frill
     9. reduced hands
     10. domed head
     11. jaw joint below tooth row
     12. elongate hands
     13. prepubic process well developed
     14. ridge on teeth
     15. reduction in manus digits I and V (and large nares)
     16. manus digit 1 spike-like
 

     The Ceratopsia are exclusively Cretaceous in age and have a very large fossil record.  Ceratopsians are one of the most diverse groups of plant eating dinosaurs of the Cretaceous.  They were very abundant during the last 35 million years of the Cretaceous and only from Asia and North America.  The fossil evidence indicates that Ceratopsia arose in Asia during the early Cretaceous and later migrated to North America.

     The key derived characters of Ceratopsia include the following:


GENUS Psittacosaurus

      The most primitive (least derived) member of the Ceratopsia is the genus Psittacosaurus of the Lower Cretaceous of eastern Asia.  Psittacosaurus is often referred to as the "Parrot dinosaur".  It is known from many complete skeletons from the Lower Cretaceous of eastern Asia.

Psittacosaurus skull and skeleton (From Lucas, 1997)

     The skull had only a rudimentary frill.  This was a small dinosaur of less than 2 meters in length.  The skeleton is of the primitive ornithischian type with hind limbs longer than fore limbs, fore limbs with only three functional digits (5 gone and 4 greatly reduced), short neck, and a long tail.  It probably walked on two legs most of the time (bipedal), but when eating may have moved on all four limbs.  Psittacosaurus was widespread and fairly common in Asia during the Early Cretaceous.  It is perhaps very similar to the ancestral stock for all of the Ceratopsia.
    Psittacosaurus (The Natural History Museum, London)Psittacosaurus
 

NEOCERATOPSIA

     The distribution of the Neoceratopsia suggests that the group originated in Asia and then spread to North America.  This group includes some of the most diverse and abundant dinosaurs of the Late Cretaceous of North America.

     The following derived characters separate Neoceratopsia from Psittacosaurus:

     The Neoceratopsia has traditionally been divided into two families, the Protoceratopsidae (primarily from Asia) and the Ceratopsidae (from western North America).  However, fairly recently, Paul Sereno of the University of Chicago (see Paul Sereno's Biography  http://dinosaur.uchicago.edu/biography.html)  has questioned the monophyletic nature of the Protoceratopsidae.  He has suggested that the traditional members of Protoceratopsidae show a sequentially  more closely aligned relationship to the Ceratopsidae.  In other words, he suggests that the Protoceratopsidae are not a monophyletic group (see discussion in Fastovsky and Weishampel).
 
 

PROTOCERATOPSIDAE

     With Sereno's objection to a monophyletic Protoceratopsidae aptly noted, we will continue with a discussion of the primitive ceratopsians that have traditionally been placed in the family Protoceratopsidae.

     Perhaps the best known of the Protoceratopsidae is the small dinosaur Protoceratops from Upper Cretaceous rocks of the Gobi Desert in Mongolia.  In addition to Protoceratops,Bagaceratops is also known from the Upper Cretaceous of Mongolia, and Leptoceratops and Montanoceratops are known from Upper Cretaceous rocks of western North America.  The protoceratops are all of Late Cretaceous age and represent a stage of evolution intermediate between Psittacosaurus and Ceratopsidae (Lucas, 1997).

     The first specimens of Protoceratops (also Psittacosaurus) were found in the Gobi desert as a result of the Central Asiatic Expeditions led by Roy Chapman Andrews ( American Museum of Natural History: Roy Chapman Andrews at http://www.amnh.org/Exhibition/Fossil_Halls/Personalities/andrews.html) of the American Museum of Natural History in the early 1920s.

Discovery Online -- Dinosaurs in the Dunes, Protoceratops andrewsi (From: http://icarus.online.discovery.com/area/specials/gobi/bonezonepages/dino.06.html).

     Protoceratopsids had a large skull and much larger frill than Psittacosaurus (which had only an incipient frill).  The protoceratopsids had no horns, as in later neoceratopsians.

LIFESTYLE OF PROTOCERATOPSIDS

     The Late Cretaceous of eastern Asia was characterized by an arid climate with desert dune fields and intermittant lakes and streams.  Of course, this type of environment is ideal for preserving fossils.  It is thought that protoceratopsids lived in small herds and possible nested communally (somewhat speculative).  Although large numbers of Protoceratops skeletons (dozens) have been found, no eggs of Protoceratops are known.  The large number of eggs found by the Central Asiatic Expeditions (an latter expeditions) as ring-shaped clusters in shallow depressions in dune sand are now known to be eggs of the small, strange looking theropod dinosaur, Oviraptor (Click this site:AMNH Dino News | Headlines | The Baby That Changed a Theory (http://www.amnh.org/enews/headl/e2_h3.html).

     Well documented growth sequences, from young to adult, have been found for Protoceratops.  Onset of the frill growth is associated with sexual maturity.  Thus, the frill may have been important for display.  The frill is highly vascularized and perhaps may have served some function in thermoregulation.  For adults, there are two sizes of skulls, suggesting sexual dimorphism.  The larger skull with more prominent nose bumps have been interpreted as males.


 From Lucas, 1997.

CERATOPSIDAE

     Members of the Ceratopsidae are relatively large (4 to 8 meters long) and are obligate quadrapeds.
Derived characters include:

     The Ceratopsidae are divided into two subfamilies, 1) the Centrosaurinae and 2) the Chasmosaurinae.


     Cladogram showing the relaionships among the Ceratopsia (From: Dodson, Peter and Philip J. Currie; 1990; Neoceratopsia, p. 609; in The Dinosauria; Weishampel, David B., Peter Dodson, and Halszda Osmolska (eds.); 1990; University of California Press; Berkely, Los Angeles, London; 733 p.

CENTROSAURINAE

     The Centrosaurinae are the more primitive (least derived) of the Ceratopsidae.  They are known primarily from Upper Cretaceous rocks of Montana, Alberta, and Alaska.

CHASMOSAURINAE

     This is the group that contains Triceratops.  These dinosaurs have very large skulls, some as large as 2.8 meters.  They are also fairly long of body, some with bodies as long as 8 meters (about 26 feet).  A typical Triceratops would weigh from 5 to 7 tons.  As with the Centrosaurinae, they are only known from western North America.  The Chasmosaurinae ranged across western North America from Alberta to Texas.


TRICERATOPS

     Triceratops is a typical representative of the Chasmosaurinae, so let's look at the characteristics of this dinosaur.


LIFESTYLE OF CERATOPSIDAE


  A herd of Torosaurus feeding in a wash descending into a distant
  lake (From: DeCourten, Frank; 1998; Dinosaurs of Utah; The University
  of Utah Press; Salt Lake City; 300 p.).

CERATOPSIAN EVOLUTION AND BIOGEOGRAPHY