From Wikipedia, the free encyclopedia
Jump to: navigation, search
Temporal range: Late Cretaceous, 79 Ma
Acristavus Skull.png
Diagram of skull
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Ornithischia
Family: Hadrosauridae
Subfamily: Saurolophinae
Tribe: Brachylophosaurini
Genus: Acristavus
Gates et al., 2011

A. gagslarsoni Gates et al., 2011 (type)

Acristavus is a genus of saurolophine dinosaur. Fossils have been found from the Campanian Two Medicine Formation in Montana and Wahweap Formation in Utah, United States. The type species A. gagslarsoni was named in 2011. Unlike nearly all hadrosaurids except Edmontosaurus, Acristavus lacked ornamentation on its skull. The discovery of Acristavus is paleontologically significant because it supports the position that the ancestor of all hadrosaurids did not possess cranial ornamentation, and that ornamentation was an adaptation that later arose interdependently in the subfamilies Saurolophinae and Lambeosaurinae. It is closely related to Brachylophosaurus and Maiasaura, and was assigned to a new clade called Brachylophosaurini.[1]

Discovery and occurrence[edit]

The holotype specimen of Acristavus, MOR 1155, was recovered at the Two Medicine Formation, in Teton County, Montana. The specimen was collected in 1999 by C. Riley Nelson in well-indurated tan colored calcareous sandstone that was deposited during the Campanian stage of the Cretaceous period, approximately 79 million years ago.[2] MOR 1155 consists of an almost complete skull with associated postcrania including eleven cervical vertebrae, three incomplete dorsal vertebrae, a proximal caudal vertebra, several dorsal ribs, the left humerus, the left ulna, the right sternal, the left pubis, the left femur, the left tibia, two left metatarsals, five left pedal phalanges and one right pedal phalanx. A second specimen UMNHVP 16607 assigned to Acristavus in 2011, was excavated from the Smokey Mountain Road locality in Middle Mudstone Member of the Wahweap Formation in Utah. It was collected by C. R. Nelson in 2000, in lithified, yellow sandstone believed to be from the same time period as the type specimen. UMNHVP 16607 consists of a partial articulated skull, including both lacrimals, a complete braincase, and a cervical vertebra.


Acristavus was first assigned to the Brachylophosaurini, in a basal position, by Gates et al. (2011). All subsequent phylogenetic analyses have confirmed this assignment. Brachylophosaurines are derived members of the group Saurolophinae. Other brachylophosaurins include Maiasaura, Brachylophosaurus, and potentially Wulagasaurus. Gates concluded that Acristavus and Maiasaura shared a sister-taxon relationship but more recent analysis by Prieto-Márquez (2013) shows that Maiasaura is more closely related to the more derived Brachylophosaurus.

The following cladogram is based on the 2013 phylogenetic analysis by Prieto-Márquez (the relationships within Lambeosaurinae and between basal hadrosauroids are not shown):[3]















Edmontosaurus annectens

Edmontosaurus regalis

PASAC-1 (Unnamed Sabinas species)



Saurolophus morrisi

Saurolophus osborni

Saurolophus angustirostris



Kritosaurus horneri

Kritosaurus navajovius

Gryposaurus latidens

Gryposaurus notabilis

Gryposaurus monumentensis

UTEP 37.7 (Unnamed Big Bend species)



Distinguishing anatomical features[edit]

A diagnosis is a statement of the anatomical features of an organism (or group) that collectively distinguish it from all other organisms. Some, but not all, of the features in a diagnosis are also autapomorphies. An autapomorphy is a distinctive anatomical feature that is unique to a given organism.

According to Gates (2011), Acristavus can be distinguished based on the following characteristics:

  • an enlarged caudodorsal brow of the postorbital and the basioccipital, which extends caudally well beyond the dorsal border of the foremen magnum to a greater extent than in other hadrosaurine species
  • a deep laterally squared frontonasal suture
  • swelling of the interdigitate suture between the prefrontal and frontal
  • a deep depression is present on the lateral surface of the postorbital jugal process



The Wahweap Formation has been radiometrically dated as being between 81 and 76 million years old.[4] During the time that Acristavus lived, the Western Interior Seaway was at its widest extent, almost completely isolating southern Laramidia off from the rest of North America. The area where dinosaurs lived included lakes, floodplains, and east-flowing rivers. The Wahweap Formation is part of the Grand Staircase region, an immense sequence of sedimentary rock layers that stretch south from Bryce Canyon National Park through Zion National Park and into the Grand Canyon. The presence of rapid sedimentation and other evidence suggests a wet, seasonal climate.[5]


Acristavus shared its paleoenvironment with other dinosaurs, such as the lambeosaur Adelolophus hutchisoni,[6] the ceratopsian Diabloceratops eatoni,[7][8] unnamed ankylosaurs and pachycephalosaurs, and the theropod Lythronax argestes, which was likely the apex predator in its ecosystem.[9] Vertebrates present in the Wahweap Formation at the time of Acristavus included freshwater fish, bowfins, abundant rays and sharks, turtles like Compsemys, crocodilians,[10] and lungfish.[11] A fair number of mammals lived in this region, which included several genera of multituberculates, cladotherians, marsupials, and placental insectivores.[12] These mammals were more primitive than those that lived in the area that is now the Kaiparowits Formation. Trace fossils are relatively abundant in the Wahweap Formation, and suggest the presence of crocodylomorphs, as well as ornithischian and theropod dinosaurs.[13] In 2010 a unique trace fossil was discovered that suggests a predator-prey relationship between dinosaurs and primitive mammals. The trace fossil includes at least two fossilized mammalian den complexes as well as associated digging grooves presumably caused by a maniraptoran dinosaur. The proximity indicates a case of probable active predation of the burrow inhabitants by the animals that made the claw marks.[14] Invertebrate activity in this formation ranged from fossilized insect burrows in petrified logs[15] to various mollusks, large crabs,[16] and a wide diversity of gastropods and ostracods.[17]

See also[edit]


  1. ^ Gates, T.A.; Horner, J.R.; Hanna, R.R.; Nelson, C.R. (2011). "New unadorned hadrosaurine hadrosaurid (Dinosauria, Ornithopoda) from the Campanian of North America". Journal of Vertebrate Paleontology. 31 (4): 798–811. doi:10.1080/02724634.2011.577854. 
  2. ^ Jinnah, Z.A., Roberts, E.M., Deino, A.L., Larsen, J.S., Link, P.K. and Fanning, C.M. (2009). New 40Ar-39Ar and detrital zircon U-Pb ages for the Upper Cretaceous Wahweap and Kaiparowits formations on the Kaiparowits Plateau, Utah: implications for regional correlation, provenance and biostratigraphy. Cretaceous Research 30, 287-299.
  3. ^ Prieto-Márquez, A. (2013). "Skeletal morphology of Kritosaurus navajovius (Dinosauria:Hadrosauridae) from the Late Cretaceous of the North American south-west, with an evaluation of the phylogenetic systematics and biogeography of Kritosaurini". Journal of Systematic Palaeontology. in press. doi:10.1080/14772019.2013.77041
  4. ^ Introduction: Kaiparowits Basin Project Overview," Getty, et al. (2010); page 479.
  5. ^ Zubair A. Jinnah, #30088 (2009)Sequence Stratigraphic Control from Alluvial Architecture of Upper Cretaceous Fluvial System - Wahweap Formation, Southern Utah, U.S.A. Search and Discovery Article #30088. Posted June 16, 2009.
  6. ^ Terry A. Gates; Zubair Jinnah; Carolyn Levitt; Michael A. Getty (2014). "New hadrosaurid specimens from the lower-middle Campanian Wahweap Formation of Utah". In David A. Eberth; David C. Evans. Hadrosaurs: Proceedings of the International Hadrosaur Symposium. Indiana University Press. pp. 156–173. ISBN 978-0-253-01385-9. 
  7. ^ "Diabloceratops eatoni". Natural History Museum of Utah. Retrieved 16 November 2013. 
  8. ^
  9. ^ John Wesley Powell Memorial Museum display, visited April 30th, 2009
  10. ^ Thompson, Cameron R. "A preliminary report on biostratigraphy of Cretaceous freshwater rays, Wahweap Formation and John Henry Member of the Straight Cliffs Formation, southern Utah." Abstracts with Programs - Geological Society of America, vol.36, no.4, pp.91, Apr 2004
  11. ^ Orsulak, Megan et al. "A lungfish burrow in late Cretaceous upper capping sandstone member of the Wahweap Formation Cockscomb area, Grand Staircase-Escalante National Monument, Utah." Abstracts with Programs - Geological Society of America, vol. 39, no. 5, pp.43, May 2007
  12. ^ Eaton, Jeffrey G; Cifelli, Richard L. "Review of Cretaceous mammalian paleontology; Grand Staircase-Escalante National Monument, Utah. Abstracts with Programs - Geological Society of America, vol.37, no.7, pp.115, Oct 2005
  13. ^ Tester, Edward et al. Isolated vertebrate tracks from the Upper Cretaceous capping sandstone member of the Wahweap Formation; Grand Staircase-Escalante National Monument, UtahAbstracts with Programs - Geological Society of America, vol. 39, no. 5, pp.42, May 2007
  14. ^
  15. ^ De Blieux, Donald D. "Analysis of Jim's hadrosaur site; a dinosaur site in the middle Campanian (Cretaceous) Wahweap Formation of Grand Staircase-Escalante National Monument (GSENM), southern Utah." Abstracts with Programs - Geological Society of America, vol. 39, no. 5, pp.6, May 2007
  16. ^ Kirkland, James Ian. "An inventory of paleontological resources in the lower Wahweap Formation (lower Campanian), southern Kaiparowits Plateau, Grand Staircase-Escalante National Monument, Utah." Abstracts with Programs - Geological Society of America, vol.37, no.7, pp.114, Oct 2005.
  17. ^ Williams, Jessica A J; Lohrengel, C Frederick. Preliminary study of freshwater gastropods in the Wahweap Formation, Bryce Canyon National Park, Utah. Abstracts with Programs - Geological Society of America, vol. 39, no. 5, pp.43, May 2007