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North Horn Formation

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Coordinates: 39°00′N 111°00′W / 39.0°N 111.0°W / 39.0; -111.0
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North Horn Formation
Stratigraphic range: Maastrichtian-Danian
~71–64 Ma
Type locality for the North Horn Formation on North Horn Mountain, Emery County, Utah
TypeGeological formation
UnderliesFlagstaff Formation
OverliesPrice River & Tuscher Formations
Thickness>1,100 m (3,600 ft)
Lithology
PrimarySandstone, shale, conglomerate
OtherSiltstone, limestone, coal
Location
Coordinates39°00′N 111°00′W / 39.0°N 111.0°W / 39.0; -111.0
Approximate paleocoordinates46°48′N 88°00′W / 46.8°N 88.0°W / 46.8; -88.0
RegionUtah
Country United States
Extent~140 km (87 mi)
Type section
Named forNorth Horn Mountain
North Horn Formation is located in the United States
North Horn Formation
North Horn Formation (the United States)
North Horn Formation is located in Utah
North Horn Formation
North Horn Formation (Utah)
North Horn Formation on the west face of North Horn Mountain, Emery County, Utah.

The North Horn Formation is a widespread non-marine sedimentary unit with extensive outcrops exposed in central and eastern Utah. The formation locally exceeds 3,600 feet (1,100 m) in thickness and is characterized by fluvial, lacustrine, and floodplain dominated systems, representing a terrestrial, high energy, depositional environment.[1][2][3] The sediments date from Late Cretaceous (Maastrichtian) to early Paleocene in age and include the K-Pg extinction event boundary; however, this boundary is extremely difficult to locate and there is no strong stratigraphic evidence available that indicates a specific marker bed such as an iridium rich clay layer.[4][5] Thus far, the only visible evidence is represented in the form of faunal turnover from dinosaur to mammal-dominated fossil assemblages. Taxa from the Cretaceous part of the formation include squamates, testudines, choristoderes, crocodyliforms, sharks, bony fishes, amphibians, mammals, dinosaurs, eggshell fragments, trace fossils, mollusks, plant macrofossils, such as wood fragments, and palynomorphs.[6][7][8][9]

Stratigraphy

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Type locality for the North Horn Formation on North Horn Mountain, Emery County, Utah

The North Horn Formation is a non-marine, stratigraphic unit located in east and central Utah which unconformably overlies the Late Cretaceous Price River Formation west of the San Rafael Swell, and the Tuscher Formation east of the swell.[2] The formation is overlain by the late Paleocene-early Eocene Flagstaff Formation, also called the Flagstaff Limestone.[1][2] The North Horn type section is located on North Horn Mountain in Emery County, Utah.[10] Laterally, the North Horn Formation nearly spans an 87-mile (140 km) long east–west transect that extends from the Wasatch Plateau on the west and the Book Cliffs, near Green River, on the east, separated in the middle by the San Rafael Swell.[3] The North Horn Formation varies greatly in thickness and lithology, representing a time transgressive stratigraphic sequence,[clarification needed] which means that the age of the base and top of the formation changes as one moves laterally. West of the San Rafael Swell, near Price Canyon, Utah, the basal contact for the North Horn Formation is Maastrichtian (latest Cretaceous) in age,[1][2][3] whereas its base is Paleocene in age on the eastern side of the swell.[2] Some of the most complete sections of the North Horn Formation are exposed west of the San Rafael Swell at North Horn Mountain in which the local stratigraphy sometimes exceeds 3,600 ft (1,100 m) in thickness. Further to the east, towards Green River, Utah, stratigraphic sections are significantly thinner compared to sections in the west with thicknesses varying between as little as 50 to 130 ft (15 to 40 m).[2][4]

Subdivisions

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The formation is divided into three informal units based on broad but distinct lithological characteristics. These units include the lower variegated unit at the base, a middle coal unit (in which the K-Pg boundary is located), and the upper variegated unit at the top. The units themselves are further divided into a total of eight sub-units, or lithofacies, based on facies scale lithological features.[1][3][4] A detailed sedimentary study of the North Horn Formation was conducted by Lawton et al.[2] These units, from oldest to youngest, include a 330 ft (100 m) thick basal conglomerate unit that consists of an upward fining conglomerates and sandstone and lacks any interbedded shale, followed by the lower redbed unit, a 790 ft (240 m) thick sequence dominated by red sandy siltstone, conglomerate, and pebbly sandstone. The third unit is the sheet sandstone unit and is composed of sheetlike sandstone beds that are interbedded with gray and carbonaceous siltstones. Some limestone beds are present but are uncommon. The fourth unit is characterized by 131 to 374 ft (40 to 114 m) thick coal beds and coal-streaked siltstone deposits and are referred to as the coal-bearing unit. This unit is overlain by a 833 ft (254 m) thick sequence of primarily calcareous siltstone beds, called the calcareous siltstone unit. The big mountain unit consists of nearly 750 feet (230 m) of interbedded conglomerates and trough cross bedded sandstones, followed by a 200 ft (60 m) thick set of strata composed of sandstone, pebbly sandstone, and conglomerates which make up the coal canyon unit. The uppermost unit is the upper redbed unit, which is nearly a 390 ft (120 m) thick and is composed of red brown mottled siltstone and sandy siltstone.

Paleontology

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Characteristic dinosaur taxa include the ceratopsian Torosaurus utahensis, the titanosaurid sauropod Alamosaurus sanjuanensis, and the theropod Tyrannosaurus;[11][12][13][14] however, the most frequently occurring taxon in the Cretaceous strata of the North Horn Formation is the Polyglyphanodont squamate Polyglyphanodon.[6] Fauna recorded from Paleocene strata within the formation appear to be far more diverse and over 70 different taxa have been identified, including frogs, numerous multituberculate, protoeutherians, periptychids, arctocyonids and phenacodontid mammals, crocodyliforms, choristoderes, trace fossils, and palynomorphs.[4][7][8][6] Marsupial remains similar to Alphadon and Eodelphis have also been found here as well.[15]

Pterodactyloid tracks present at an unnamed site. The specimens are kept at the Dinosaur Tracks Museum, of the University of Colorado at Denver.[16] Bird and dinosaur eggs have also been found at the site, along with unidentified hadrosaur fossils (possibly from Edmontosaurus or Kritosaurus).[6]

Fossil content

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Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Vertebrates of the North Horn Formation
Genus Species Location Time[8] Abundance Notes Image
Adocus[6] A. sp.[6] Maastrichtian Adocus
Alamosaurus[17] A. sanjuanensis[18] Maastrichtian Alamosaurus
Alphadon[8] A. sp.[8] Maastrichtian Alphadon
Amiidae[8] Indeterminate[8] Maastrichtian
Anura[8] Indeterminate[8] Maastrichtian
Aspideretes[8] "A." sp.[8] Maastrichtian
Atoposauridae[8] Indeterminate[8] Maastrichtian
Basilemys[6] B. sp.[6] Maastrichtian Basilemys
Champsosaurus[6] C. sp.[6] Maastrichtian-Danian Champsosaurus
Cimolomys[8] C. sp.[8] Maastrichtian
Compsemys[8] C. victa & C. sp.[8] Maastrichtian-Danian
Eutheria[8] Indeterminate[8] Maastrichtian
Ischyrhiza[8] I. sp.[8] Maastrichtian Ischyrhiza
Hadrosauridae[8] Indeterminate[8] Maastrichtian
Lepisosteus[6] L. sp.[6] Maastrichtian-Danian Lepisosteus
Leptochamops[8] cf. L. sp.[8] Maastrichtian
Mesodma[8] M. sp. (cf. M. hensleighi)[8] Maastrichtian
Myledaphus[8] M. bipartitus[8] Maastrichtian Myledaphus
Paracimexomys[8] P. sp.[8] Maastrichtian
Paraglyphanodon[8] P. utahensis & P. gazini[8] Maastrichtian
Pediomys[8] P. sp.[8] Maastrichtian
Pinacosuchus[8] P. mantiensis[8] Maastrichtian
Pholidosauridae[8] Indeterminate[8] Maastrichtian
Polyglyphanodon[6] P. sternbergi[6] Maastrichtian Polyglyphanodon
Protolambda P. hatcheri[8][19] Maastrichtian Previously identified as a species of Pediomys
Pteraichnus[16]   Found at an unnamed site.[16] Maastrichtian   Specimens kept at the Dinosaur Tracks Museum, of the University of Colorado at Denver.[16]  
Pycnodontidae[8] Indeterminate[8] Maastrichtian Pycnodus
Squatirhina[8] S. americana[8] Maastrichtian
Torosaurus[20] T. utahensis[20] Maastrichtian Torosaurus
Troodontidae[8] Indeterminate[8] Maastrichtian Troodon
Tyrannosaurus[21][17] T. rex [21][17] Maastrichtian Tyrannosaurus

See also

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References

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  1. ^ a b c d Fouch, T. D., Lawton, T. F., Nichols, D. J., Cashion, W. B., Cobban, W. A. (1983). Patterns and timing of synorogenic sedimentation in Upper Cretaceous rocks of central and northeast Utah. In Reynolds, M. W., and Dolly, E. D., eds., Mesozoic paleogeography of west central United States. Society of Economic Paleontologists and Mineralogists. Pp. 305-336.
  2. ^ a b c d e f g Lawton, T. F. (1986). Fluvial systems of the Upper Cretaceous Mesaverde Group and Paleocene North Horn Formation, central Utah: A record of transition from thin-skinned to thick-skinned deformation in the foreland region. Paleotectonics and Sedimentatio in the Rocky Mountain Region, United States. AAPG Special Volumes, M 41. Pp. 423-442.
  3. ^ a b c d Lawton, T. F., Talling, P. J., Hobbs, R. S., Trexler, J. H. Jr, Weiss, M. P., Burbank, D. W. (1993). Structure and stratigraphy of Upper Cretaceous and Paleocene strata (North Horn Formation), eastern San Pitch Mountains, Utah – sedimentation at the front of the Sevier orogenic belt. United States Geological Survey, Bulletin 1787-II, Pp. 1-33.
  4. ^ a b c d Difley, R., Ekdale, A. A. (2002). Faunal implications of an environmental change before the Cretaceous-Tertiary (K-T) transition in central Utah. Cretaceous Research, 23:315-331.
  5. ^ Myung-Suk, Y., Cross, A.T. (1997). Palynostratigraphy of Upper Cretaceous-Lower Tertiary strata, Price Canyon, Utah. Review of Palaeobotany and Palynology 97, p.53-66
  6. ^ a b c d e f g h i j k l m n Gilmore, Charles W. (1946). Reptilian fauna of the North Horn Formation of central Utah (Vol. 210). Washington, D.C.: US Government Printing Office. pp. 29–53. doi:10.3133/PP210C. S2CID 128849169.
  7. ^ a b Cifelli, R.L., Czaplewski, N.J., Rose, K.D. (1995). Knowledge of Paleocene Mammals from the North Horn Formation, Central Utah. The Great Basin Naturalist. Vol. 55:4. Pp. 304-314
  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 y z aa ab ac ad ae af ag ah ai aj ak al am an ao ap aq ar as at Cifelli, Richard L.; Nydam, Randall L.; Eaton, Jeffrey G.; Gardner, James D.; Kirkland, James I. (1999). "Vertebrate faunas of the North Horn Formation (Upper Cretaceous–Lower Paleocene), Emery and Sanpete Counties, Utah". In Gillette, David D. (ed.). Vertebrate Paleontology in Utah. Salt Lake City: Utah Geological Survey. pp. 377–388. ISBN 1-55791-634-9.
  9. ^ Difley, Rose L.; Ekdale, Allan A. (August 2002). "Footprints of Utah's Last Dinosaurs: Track Beds in the Upper Cretaceous (Maastrichtian) North Horn Formation of the Wasatch Plateau, Central Utah". PALAIOS. 17 (4): 327–346. Bibcode:2002Palai..17..327D. doi:10.1669/0883-1351(2002)017<0327:FOUSLD>2.0.CO;2. JSTOR 3515759. S2CID 130309439. Retrieved 18 October 2020.
  10. ^ Spieker, E. M. (1946). Late Mesozoic and early Cenozoic history of central Utah. United States Geological Survey. Professional Paper 205-D, 117-159
  11. ^ Black, Riley (2005). "When Tyrannosaurus Chomped Sauropods". Smithsonian Magazine. 25. Smithsonian Institution: 469. doi:10.1671/0272-4634(2005)025[0469:TRFTUC]2.0.CO;2. ISSN 0272-4634. S2CID 131583311. Retrieved 13 April 2012.
  12. ^ Black, Riley. "Tyrannosaurus vs. Alamosaurus". Smithsonian Magazine. Smithsonian Institution. Retrieved 23 March 2009.
  13. ^ Sampson, Scott D.; Loewon, Mark A. (27 June 2005). "Tyrannosaurus rex from the Upper Cretaceous (Maastrichtian) North Horn Formation of Utah: Biogeographic and Paleoecologic Implications". Journal of Vertebrate Paleontology. 25 (2): 469–472. doi:10.1671/0272-4634(2005)025[0469:TRFTUC]2.0.CO;2. JSTOR 4524461. S2CID 131583311. Retrieved 18 October 2020.
  14. ^ Sampson, S.D., Loewen, M.A.(2005). Tyrannosaurus from the Upper Cretaceous (Maastrichtian) North Horn Formation of Utah: biogeographic and paleoecologic implications. Journal of Vertebrate Paleontology 25:2, 469-472
  15. ^ Cifelli, Richard L.; de Muizon, Christian (May 1998). "Marsupial mammal from the Upper Cretaceous North Horn Formation, Central Utah". Journal of Paleontology. 72 (3). Cambridge University Press: 532–637. Bibcode:1998JPal...72..532C. doi:10.1017/S0022336000024306. S2CID 130086187. Retrieved 19 November 2020.
  16. ^ a b c d Lockley, M.; Harris, J.D.; and Mitchell, L. 2008. "A global overview of pterosaur ichnology: tracksite distribution in space and time." Zitteliana. B28. p. 187-198. ISSN 1612-4138.
  17. ^ a b c Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. ISBN 0-520-24209-2.
  18. ^ Lehman, T.M.; Coulson, A.B. (2002). "A juvenile specimen of the sauropod Alamosaurus sanjuanensis from the Upper Cretaceous of Big Bend National Park, Texas" (PDF). Journal of Paleontology. 76 (1): 156–172. doi:10.1017/s0022336000017431. S2CID 232345559.
  19. ^ Davis, B. M. (2007). "A revision of 'pediomyid' marsupials from the Late Cretaceous of North America" (PDF). Acta Palaeontologica Polonica. 52 (2): 217–256.
  20. ^ a b Sullivan, R.M.; Boere, A.C.; Lucas, S.G. (2005). "Redescription of the ceratopsid dinosaur Torosaurus utahensis (Gilmore, 1946) and a revision of the genus". Journal of Paleontology. 79 (3): 564–582. Bibcode:2005JPal...79..564S. doi:10.1666/0022-3360(2005)079<0564:ROTCDT>2.0.CO;2.
  21. ^ a b Sampson, Scott D.; Loewon, Mark A. (27 June 2005). "Tyrannosaurus rex from the Upper Cretaceous (Maastrichtian) North Horn Formation of Utah: Biogeographic and Paleoecologic Implications". Journal of Vertebrate Paleontology. 25 (2): 469–472. doi:10.1671/0272-4634(2005)025[0469:TRFTUC]2.0.CO;2. JSTOR 4524461. S2CID 131583311. Retrieved 18 October 2020.
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