Cedar Mountain Formation

Cedar Mountain Formation
Stratigraphic range: Early Cretaceous
Type Geological formation
Underlies Naturita Formation
Overlies Morrison Formation
Thickness 0–410 feet (0–125 m)
Location
Region Utah
Country United States
Type section
Named for Cedar Mountain

The Cedar Mountain Formation is the name given to a distinctive sedimentary geologic formation in eastern Utah.

The formation was named for Cedar Mountain in northern Emery County, Utah, where William Lee Stokes first studied the exposures in 1944.[1]

Geology

The drab-colored lower portion of the Cedar Mountain Formation, overlying the brighter Morrison Formation.

The formation occurs between the underlying Morrison Formation and overlying Naturita Formation (sometimes formerly called the Dakota Formation).

It is composed of non-marine sediments, that is, sediments deposited in rivers, lakes and on flood plains. Based on various fossils and radiometric dates, the Cedar Mountain Formation was deposited during the last half of the Early Cretaceous Epoch, about 127 - 98 million years ago (mya).

It has lithography similar to the Burro Canyon Formation in the region.

Dinosaurs occur throughout the formation, but their study has only occurred since the early 1990s. The dinosaurs in the lower part of the formation differ from those in the upper part. These two dinosaur assemblages, characterized by distinct dinosaurs, show the replacement of older, European-like dinosaurs with younger, Asian-like dinosaurs as the North American Continental Plate drifted westward. A middle dinosaur assemblage may be present, but the fossil record is not clear.

Stratigraphy

The Cedar Mountain Formation is sandwiched between the Morrison Formation below and the Naturita Formation and Mancos Shale above. The youngest date for Morrison just below the Cedar Mountain Formation is 148.1 ± 0.5 Ma .[2] or lower Tithonian. Typically, the Jurassic-Cretaceous boundary in western North America is marked by an unconformity of variable length, and typically signifies 10-49 million years of missing geologic time.[2] This boundary between the Morrison and Cedar Mountain is commonly marked by a horizon of carbonate nodules[3][4] or by highly polished pebbles that are allegedly gastroliths.

Although not part of the Cedar Mountain Formation, the Naturita Formation immediately overlies the Cedar Mountain and marks the encroaching Western Interior Seaway. The Naturita is not uniformly distributed and was eroded away in places by the advancing Seaway so that the marine shales of the Mancos Formation lay directly on the Mussentuchit or its equivalent. The name Dakota Formation has been improperly used for these strata.

Stratigraphic column showing the various members that make up the Cedar Mountain Formation and their approximate geologic age.
Missing strata either were not deposited or were deposited, but later eroded.

Formation members

Only recently did the 125 m (410 ft) thick formation get subdivided into smaller, distinctive beds called members. There is a debate as to whether there are five members[5] or four[6] depending whether the Buckhorn Conglomerate is considered to be at the top of the Morrison Formation or at the base of the Cedar Mountain Formation; most geologists and paleontologists consider it part of the Cedar Mountain Formation. In ascending order the remaining members are the Yellow Cat Member, Poison Strip Sandstone, Ruby Ranch Member, and the Mussentuchit Member. Each of these members are named after a geographic area where they were first studied.

Dinosaurs

Example of dinosaurs from the Cedar Mountain Formation include the polacanthid ankylosaur Gastonia from the Yellow Cat Member (upper left), Utahraptor from the Yellow Cat Member (upper right), a large theropod represented by a tooth from the Ruby Ranch Member (lower left), and Tenontosaurus from the base of the Mussentuchit (lower right).

The Cedar Mountain Formation is one of the last major dinosaur-bearing formations to be studied in the United States. Although sporadic bone fragments were known prior to 1990, serious research did not begin until that year. Since then, several organizations have conducted field work collecting dinosaurs, chiefly the Oklahoma Museum of Natural History, the Denver Museum of Nature & Science, the College of Eastern Utah, the Utah Geological Survey, Brigham Young University, and Dinosaur National Monument staff. This research indicates that at least two, possibly three dinosaur assemblages are contained within the formation.

The oldest of these assemblages is from the Yellow Cat, Poison Strip and basal Ruby Ranch members. The small, Ornitholestes-like theropod Nedcolbertia and the brachiosaurid sauropod Cedarosaurus may be considered as relics, with their closest relatives in the Morrison Formation. In contrast, the polacanthid ankylosaur Gastonia and a yet unnamed iguanodontid are similar to related forms from the Lower Cretaceous of southern England. These dinosaurs show that the connection between North America and Europe still existed during the Barremian. All of this changes, however, with the upper dinosaur assemblage from the top of the Ruby Ranch and Mussentuchit members. This upper assemblage shows greater similarities with Asian dinosaur assemblages from the same time. For example, the primitive ankylosaurid Cedarpelta is related to Gobisaurus and Shamosaurus from Mongolia, but is more primitive than either because it has teeth in the premaxilla. The upper assemblage also has a tyrannosaurid, a ceratopsian, and a pachycephalosaur. Although not a dinosaur, the primitive mammal Gobiconodon is known from both Mongolia and the Mussentuchit Member. Evidence for a middle dinosaur assemblage between the older and younger ones is controversial because the evidence mostly depends on a single specimen of the ornithopod Tenontosaurus from high in the Ruby Ranch Member and the sauropod Astrodon from low in the Ruby Ranch. Regardless, the upper and lower dinosaur assemblages in the Cedar Mountain Formation document the separation of North America and Europe, the westward drift of North America, and its connection with Asia 10 to 15 million years later.[14]

Data from Carpenter (2006),[14] Cifelli et al. (1999),[15] Kirkland and Madsen (2007), and The Paleobiology Database.

Ankylosaurs

Ankylosaurs reported from the Cedar Mountain Formation
Genus Species Location Member Material Notes Images
Animantarx Animantarx ramaljonesi * Mussentuchit Member "Partial skull [and] skeleton."[16]
Cedarpelta[17] Cedarpelta bilbeyhallorum[17] * Mussentuchit Member[17] "Skull [and] postcranium."[18] Cedarpelta bilbeyhallorum was not from the Ruby Ranch Member as initially described.[17]
Gastonia Gastonia burgei * Yellow Cat Member "[Two] skulls, [two] partial skulls, [and four] or [five] partial skeletons."[19]
G. lorriemcwhinneyae[20] * Ruby Ranch Member
Peloroplites Peloroplites cedrimontanus * Mussentuchit Member

Marginocephalians

Indeterminate neoceratopsian present in the Mussentuchit Member. Indeterminate pachycephalosaurid present in the Mussentuchit Member.

Ornithopods

New genus and species of iguanodont present in the Ruby Ranch and Yellow Cat members.

Ornithopods reported from the Cedar Mountain Formation
Genus Species Location Member Material Notes Images

Cedrorestes

Cedrorestes crichtoni

  • Yellow Cat Member.

Eolambia

Eolambia caroljonesa

  • Mussentuchit Member.

Hippodraco

Hippodraco scutodens

  • Yellow Cat Member.

Iguanacolossus

Iguanacolossus fortis

  • Yellow Cat Member.

Iguanodon

I. ottingeri

"Teeth."[21]

Dubious.

Planicoxa

Planicoxa venenica

  • Poison Strip Member.

"Associated postcranium." [22]

Tenontosaurus[12]

Tenontosaurus sp.

  • Mussentuchit Member[12]
  • Ruby Ranch Member

Zephyrosaurus

cf. Zephyrosaurus sp.

  • Mussentuchit Member.

Sauropods

New titanosaurid genus and species present in the Yellow Cat Member. Indeterminate brachiosaurid remains present in the Mussentuchit Member.

Sauropods reported from the Cedar Mountain Formation
Genus Species Location Member Material Notes Images

Abydosaurus

  • Mussentuchit Member

cf. Astrodon

Indeterminate

  • Ruby Ranch Member.

Brontomerus

Brontomerus mcintoshi

  • Ruby Ranch Member.

Cedarosaurus

Cedarosaurus weiskopfae

  • Yellow Cat Member.

"Postcranial skeleton."[23]

Venenosaurus

Venenosaurus dicrocei

  • Poison Strip Member.

"Partial postcranial skeleton."[24]

Theropods

Indeterminate dromaeosaurine present in the Mussentuchit Member. Indeterminate velociraptorine remains present in the Mussentuchit Member. Possible indeterminate tyrannosaurid remains present in the Mussentuchit Member. Indeterminate troodontid remains present in the Mussentuchit Member. Indeterminate therizinosaurid remains present in the Mussentuchit Member. Indeterminate dromaeosaurine remains present in the Mussentuchit Member. Possible new allosaurid species present in the Ruby Ranch Member. Possible indeterminate hesperornithiformes present in the Mussentuchit Member.

Theropods reported from the Cedar Mountain Formation
Genus Species Location Member Material Notes Images

cf. Acrocanthosaurus

Indeterminate

  • Ruby Ranch Member.

Deinonychus

Indeterminate

  • Mussentuchit Member.

Falcarius

Falcarius utahensis

  • Yellow Cat Member.

Geminiraptor

Geminiraptor suarezarum

  • Yellow Cat Member.

Martharaptor

Martharaptor greenriverensis

  • Yellow Cat Member.

Nedcolbertia

Nedcolbertia justinhofmanni

  • Yellow Cat Member.

"Partial skeletons of [three] individuals."[25]

cf. Richardoestesia

Indeterminate

  • Mussentuchit Member.

Siats

Siats meekerorum

  • Mussentuchit Member.
"Partial postcranial skeleton of immature individual."

Utahraptor

Utahraptor ostrommaysorum

  • Yellow Cat Member.

"Skull and postcranial fragments."[26]

Indeterminate

  • Poison Strip Member.

Yurgovuchia

Yurgovuchia doellingi

  • Yellow Cat Member.

Other fossils

Besides dinosaurs, the Cedar Mountain Formation has produced a wealth of small fossils (a.k.a. microfossils), mostly teeth from a variety of vertebrates. Most of these specimens have been found in the Mussentuchit Member where they are collected by washing the rock through fine window screen. The teeth and other small fossils are picked from the residue.[15]

Map of Utah showing the location of the Cedar Mountain Formation (red). The San Rafael Swell is the dome-like structure that the formation jogs around. Base map data courtesy of geodata.gov

The various vertebrates are listed by member in the list below.

Non-vertebrate fossils are more widely distributed in the Cedar Mountain Formation. These include the distinctive reproductive structures of fresh water algae that are called charophytes. Charophytes are so distinctive that they are used to correlate strata of similar age, and thus were used to show that the Yellow Cat Member was time equivalent to Barremian age strata in England.[5] Ostracods, small crustaceans with clam-like shells, also occur in fresh water deposits, along with "finger-clams" or chonchostracans. Pollen have been found in the Mussentuchit Member and are important for reconstructing the environment. In a few places, large petrified logs are known, especially from the Poison Strip. These conifer logs are over a meter in diameter and indicate the presence of trees over 30 m (100 feet). The distinct wood of the tree fern Tempskya is occasional found as well.

Data from Carpenter (2006),[14] Cifelli et al. (1999),[15] Kirkland and Madsen (2007), and The Paleobiology Database.

Amphibians

Indeterminate anuran remains present in the Mussentuchit Member.

Amphibians of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Albanerpeton

Albanerpeton cf. A. nexuosus

  • Mussentuchit Member.

Bony fish

Indeterminate amiiform present in the Yellow Cat and Mussentuchit Members. Indeterminate neopterygion remains present in the Mussentuchit Member. Possible indeterminate pycnodontid remains present in the Mussentuchit Member. Possible indeterminate lepisosteid remains present in the Mussentuchit Member.

Bony Fishes of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Semionotus?

Semionotus? sp.

  • Yellow Cat Member.

Ceratodus

kempae[27]

  • Yellow Cat Member.

kirklandi

  • Yellow Cat Member.

molossus

  • Mussentuchit Member.

Cartilaginous fish

A new genus and species of orectolobid present in the Mussentuchit Member.

Cartilaginous Fishes of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Hybodus

Hybodus sp.

  • Ruby Ranch Member
  • Mussentuchit Member

Polyacrodus

Polyacrodus parvidens

  • Mussentuchit Member.

Lissodus

Lissodus spp.

  • Mussentuchit Member.

Ischyrhiza

Ischyrhiza sp.

  • Mussentuchit Member.

Pseudohypolophus

Pseudohypolophus sp.

  • Mussentuchit Member.

cf. Baibisha

New species

  • Mussentuchit Member.

Cretorectolobus

Indeterminate

  • Mussentuchit Member.

Mammals

New genus and species of pappotheriid present in the Mussentuchit Member. Indeterminant genus and species of picopsid present in the Mussentuchit Member.

Mammals of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Ameribaatar

Ameribaatar zofiae

  • Mussentuchit Member.

Astroconodon

Astroconodon delicatus

  • Mussentuchit Member.

Bryceomys

Bryceomys intermedius

  • Mussentuchit Member.

Cedaromys

Cedaromys bestia

  • Mussentuchit Member.

Cedaromys parvus

  • Mussentuchit Member.

Corviconodon

Corviconodon utahensis

  • Mussentuchit Member.

Dakotadens[28]

Dakotadens pertritus

  • Mussentuchit Member.

Janumys

Janumys erebos

  • Mussentuchit Member.

Jugulator

Jugulator amplissimus

  • Mussentuchit Member.

Kokopellia

Kokopellia juddi

  • Mussentuchit Member.

Possible metatherian.

Paracimexomys

Paracimexomys perplexus

  • Mussentuchit Member.

Paracimexomys robisoni

  • Mussentuchit Member.

Spalacolestes

Spalacolestes cretulablatta

  • Mussentuchit Member.

Spalacolestes inconcinnus

  • Mussentuchit Member.

Spalacotheridium

Spalacotheridium noblei

  • Mussentuchit Member.

Other reptiles

Indeterminate pterosaur remains in the Mussentuchit Member.

Crurotarsans

Indeterminate crocodilian remains present in the Yellow Cat and Ruby Ranch Members. Indeterminate pholidosaurid remains present in the Mussentuchit Member. Indeterminate atoposaurid remains present in the Mussentuchit Member.

Crurotarsans of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

cf. Bernissartia

cf. Bernissartia sp.

  • Mussentuchit Member.

cf. Dakotasuchus

cf. Dakotasuchus sp.

  • Mussentuchit Member.

Lepidosaurs

Lepidosaurs of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Toxolophosaurus

Toxolophosaurus sp.

  • Yellow Cat Member.

Harmodontosaurus

Harmodontosaurus emeryensis

  • Mussentuchit Member.

Dimekodontosaurus

Dimekodontosaurus masdeni

  • Mussentuchit Member.

Dicothodon

Dicothodon moorensis

  • Mussentuchit Member.

Bothriagenys

Bothriagenys mysterion

  • Mussentuchit Member.

Pseudosaurillus

Pseudosaurillus sp.

  • Mussentuchit Member.

Primaderma

Primaderma nessovi

  • Mussentuchit Member.

Coniophis

Coniophis sp.

  • Mussentuchit Member.

Turtles

Indeterminate baenid remains present in the Mussentuchit Member.

Turtles of the Cedar Mountain Formation
Genus Species Location Member Abundance Description Images

Glyptops

Glyptops sp.

  • Yellow Cat Member
  • Mussentuchit Member

Naomichelys

Naomichelys sp.

  • Mussentuchit Member.

Conclusions

The Cedar Mountain Formation is proving to contain one of the richest and most diverse Early Cretaceous dinosaur faunas in the world. The discoveries to date have revealed that the origin of some of the later Cretaceous dinosaurs may lie in the Cedar Mountain, but further work is needed to understand the timing and effects the changing position of the North American Plate had on dinosaurian evolution. Also needed is a better understanding of the effects that the changing North American Plate had on the non-dinosaur vertebrates.

See also

References

  1. Stokes (1944).
  2. 1 2 Kowallis, et al. (1998).
  3. 1 2 Stokes (1952).
  4. Aubrey (1998).
  5. 1 2 3 Kirkland, et al. (1997b).
  6. Roca-Argemi and Nadon (2003).
  7. Kirkland and Madsen (2007).
  8. "Geological and Taphonomic Setting," DiCroce and Carpenter (2001). Page 186.
  9. "Depositional Setting," Tidwell, Carpenter, and Meyer (2001). Page 140.
  10. "Introduction," DiCroce and Carpenter (2001). Page 186.
  11. "Introduction," DiCroce and Carpenter (2001). Page 185.
  12. 1 2 3 "Geological and Taphonomic Setting," DiCroce and Carpenter (2001). Page 187.
  13. Chure, et al. (2010).
  14. 1 2 3 Carpenter (2006).
  15. 1 2 3 4 Cifelli, et al. (1999).
  16. "Table 17.1," in Weishampel, et al. (2004). Page 366.
  17. 1 2 3 4 Carpenter, et al. (2008).
  18. "Table 17.1," in Weishampel, et al. (2004). Page 365.
  19. "Table 17.1," in Weishampel, et al. (2004). Page 364.
  20. Billy Kinneer; Kenneth Carpenter; Allen Shaw (2016). "Redescription of Gastonia burgei (Dinosauria: Ankylosauria, Polacanthidae), and description of a new species". Neues Jahrbuch für Geologie und Paläontologie – Abhandlungen. 282 (1): 37–80. doi:10.1127/njgpa/2016/0605.
  21. "Table 19.1," in Weishampel, et al. (2004). Page 417.
  22. "Table 19.1," in Weishampel, et al. (2004). Page 414.
  23. "Table 13.1," in Weishampel, et al. (2004). Page 267.
  24. "Table 13.1," in Weishampel, et al. (2004). Page 268.
  25. "Table 4.1," in Weishampel, et al. (2004). Page 76.
  26. "Table 10.1," in Weishampel, et al. (2004). Page 198.
  27. Frederickson J.A. and Cifelli R.L. (2016) New Cretaceous lungfishes (Dipnoi, Ceratodontidae) from western North America. Journal of Paleontology.
  28. Richard L. Cifelli; Joshua E. Cohen; Brian M. Davis (2016). "New tribosphenic mammals from the Mussentuchit Local Fauna (Cedar Mountain Formation, Cenomanian), Utah, USA" (PDF). Palaeontologia Polonica 67: 67–81. doi:10.4202/pp.2016.67_067.

Further reading and literary references

External links

Cretaceous Period
Lower/Early Cretaceous Upper/Late Cretaceous
Berriasian | Valanginian | Hauterivian
Barremian| Aptian | Albian
Cenomanian | Turonian | Coniacian
Santonian |Campanian | Maastrichtian
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