Fruitland Formation

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Fruitland Formation
Stratigraphic range: Campanian[1]
~76.3–75 Ma
↓
Fruitland Formation at type.jpg
Fruitland Formation at its type location north of Fruitland, New Mexico
TypeGeological formation
Sub-unitsFossil Forest Member
Ne-nah-ne-zad Member
UnderliesKirtland Formation
OverliesPictured Cliffs Sandstone
Lithology
PrimarySandstone
OtherShale, coal
Location
Coordinates36°45′07″N 108°26′31″W / 36.752°N 108.442°W / 36.752; -108.442Coordinates: 36°45′07″N 108°26′31″W / 36.752°N 108.442°W / 36.752; -108.442
Approximate paleocoordinates43°30′N 79°36′W / 43.5°N 79.6°W / 43.5; -79.6
Region New Mexico
 Colorado
Country USA
Fruitland Formation is located in the United States
Fruitland Formation
Fruitland Formation (the United States)
Fruitland Formation is located in New Mexico
Fruitland Formation
Fruitland Formation (New Mexico)

The Fruitland Formation is a geologic formation found in the San Juan Basin in the states of New Mexico and Colorado, in the United States of America. It contains fossils dating it to the Campanian age of the late Cretaceous.[2]

Description[]

The Fruitland Formation is a sedimentary geological formation containing layers of sandstone, shale, and coal. It was laid down in marshy delta conditions, with poor drainage and frequent flooding, under a warm, humid and seasonal climate.

San Juan Basin Upper Cretaceous stratigraphy

The Fruitland is underlain by the Pictured Cliffs Sandstone, and overlain by the more recent Kirtland Formation. The sequence of rocks represents the final filling of the Cretaceous seaway. The underlying Pictured Cliffs is a marginal marine sandstone, deposited in an environment similar to offshore barrier islands of the southeast United States. As the seaway retreated, the Pictured Cliffs was covered by the Fruitland Formation, which was deposited in near-shore swampy lowlands. The formation is dated to the late Campanian (part of the Cretaceous period), and was deposited over a period of about a million years. Radiometric dating from 23 meters above the base of the formation has yielded an age of 76.03 ± 0.41 Ma ago. An ash bed lying above the upper boundary with the Kirtland Formation has been dated to 75.02 ± 0.13 Ma ago. The underlying Pictured Cliffs Sandstone would be dated 76.94 - 76.27 Ma, based on the presence of the ammonite Baculites scotti, therefore placing the base of the Fruitland Formation at ~76.3 Ma.[3]

The formation is subdivided into the upper Fossil Forrest Member (deposited between about 75.5-75 million years ago) and the lower Ne-nah-ne-zad Member (deposited from 76.3-75.5 million years ago). The Fossil Forrest member is considered to be part of the Hunter Wash, fauna shared with the overlying lower Kirtland Formation.[1]

Paleofauna[]

Ornithischians[]

Ornithischians of the Fruitland Formation
Genus Species Member Abundance Notes Images
Hadrosauridae indet.[4] Intermediate[4] Fossil Forest[4] One print[4] Giant hadrosaur track, indicating an individual larger than Shantungosaurus, the largest known hadrosaur.[4]
Parasaurolophus
Pentaceratops
Stegoceras
Titanoceratops
Parasaurolophus[5] P. cyrtocristatus[5] Fossil Forest[5] A partial skull associated with a mostly complete postcranial skeleton, and a partial skull and fragmentary ribs of a juvenile individual.[5] A lambeosaurine hadrosaurid also known from the Kaiparowits Formation.[5]
Pentaceratops[6] P. sternbergii[6] Fossil Forest[6] [Two] nearly complete skulls and a nearly complete frill.[6] A chasmosaurine ceratopsid also known from the Kirtland Formation.[6]
Stegoceras[7] S. novomexicanum[7] Fossil Forest[7] Partial remains of [three] frontals and nearly complete frontoparietal.[7] A basal pachycephalosaurid also known from the lower Kirtland Formation.[7]
Titanoceratops[8] T. ouranos[8] A partial skull, syncervical vertebrae, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, ribs, humeri, radius, femora, tibiae, fibula, ilia, ischia, and ossified tendons.[8] Possibly represents a junior synonym of Pentaceratops, holotype may possibly have come from the Kirtland Formation.[8]

Saurischians[]

Some remains (OMNH 10131) of Bistahieversor may actually have originated in the upper Fruitland Formation.[9]

Saurischians of the Fruitland Formation
Genus Species Member Abundance Notes Images
Bistahieversor[10] B. sealeyi[10] Fossil Forest[10] A rostral ramus of a lacrimal, and a partial skull and postcranial skeleton of an adult individual.[10] A eutyrannosaur tyrannosauroid also known from the Kirtland Formation.[10]
Bistahieversor
Ornithomimus
Dromaeosauridae[11] Indeterminate[11] Fossil Forest[11] Numerous isolated teeth.[11] Indeterminate dromaeosaurid remains.[11]
Ornithomimidae[11] Indeterminate[11] Fossil Forest[11] Distal end of metatarsals, distal end of a phalanx, and foot-bone fragments.[11] Indeterminate ornithomimid ornithomimosaur remains.[11]
cf. Ornithomimus[11] cf. O edmontonicus[11] Fossil Forest[11] A manual ungual.[11] Material possibly referable to Ornithomimus.[11]
?Troodontidae[12] Indeterminate[12] Fossil Forest[12] Isolated teeth.[13] Formerly identified as Paronychodon sp., referral to Troodontidae doubtful.[14]
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.

Economic geology[]

Fruitland Formation at the Bisti Wilderness

The Fruitland Formation contains beds of bituminous coal that are mined in places along the outcrop. Original reserves of coal in the formation have been estimated at 200 billion tons.[15]

Since the 1980s, the coal beds of the Fruitland Formation have yielded large quantities of coalbed methane. The productive area for coalbed methane straddles the Colorado-New Mexico state line, and is one of the most productive areas for coalbed methane in the United States. The methane released from the Fruitland Formation, through oil and gas production and a bit of natural seepage, contributes to the Four Corners Methane Hot Spot.[16][17]

See also[]

References[]

  1. ^ a b Sullivan, R.M.; Lucas, S.G. (2006). "The Kirtlandian land-vertebrate "age" – faunal composition, temporal position and biostratigraphic correlation in the nonmarine Upper Cretaceous of western North America". New Mexico Museum of Natural History and Science Bulletin. 35: 7–29. Retrieved 1 September 2021.
  2. ^ Fruitland Formation at Fossilworks.org
  3. ^ Fowler, Denver Warwick (2017-11-22). "Revised geochronology, correlation, and dinosaur stratigraphic ranges of the Santonian-Maastrichtian (Late Cretaceous) formations of the Western Interior of North America". PLOS ONE. 12 (11): e0188426. Bibcode:2017PLoSO..1288426F. doi:10.1371/journal.pone.0188426. ISSN 1932-6203. PMC 5699823. PMID 29166406.
  4. ^ a b c d e Hunt, Adrian P.; Lucas, Spencer G. (2003). "A New Hadrosaur Track from the Upper Cretaceous Fruitland Formation of Northwestern New Mexico" (PDF). New Mexico Geological Society Field Conference Series. 54: 379–381. Retrieved 1 September 2021.
  5. ^ a b c d e Gates, Terry A.; Evans, David C.; Sertich, Joseph J. W. (2021-01-25). "Description and rediagnosis of the crested hadrosaurid (Ornithopoda) dinosaur Parasaurolophus cyrtocristatus on the basis of new cranial remains". PeerJ. 9: e10669. doi:10.7717/peerj.10669. ISSN 2167-8359. PMC 7842145. PMID 33552721.
  6. ^ a b c d e 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. PMID 32547873.
  7. ^ a b c d e Steven E. Jasinski and Robert M. Sullivan (2011). "Re-evaluation of pachycephalosaurids from the Fruitland-Kirtland transition (Kirtlandian, late Campanian), San Juan Basin, New Mexico, with a description of a new species of Stegoceras and a reassessment of Texascephale langstoni" (PDF). Fossil Record 3. New Mexico Museum of Natural History and Science, Bulletin. 53: 202–215. Archived from the original (PDF) on 2015-09-24. Retrieved 2011-08-25.{{cite journal}}: CS1 maint: uses authors parameter (link)
  8. ^ a b c d Longrich, N.R. (2011). "Titanoceratops ouranos, a giant horned dinosaur from the Late Campanian of New Mexico". Cretaceous Research. 32 (3): 264–276. doi:10.1016/j.cretres.2010.12.007.
  9. ^ Carr, T.D. and Williamson, T.E. (2010). "Bistahieversor sealeyi, gen. et sp. nov., a new tyrannosauroid from New Mexico and the origin of deep snouts in Tyrannosauroidea." Journal of Vertebrate Paleontology, 30(1): 1-16. doi:10.1080/02724630903413032
  10. ^ a b c d e Carr, Thomas D.; Williamson, Thomas E. (2010). "Bistahieversor sealeyi, gen. et sp. nov., a new tyrannosauroid from New Mexico and the origin of deep snouts in Tyrannosauroidea". Journal of Vertebrate Paleontology. 30 (1): 1–16. doi:10.1080/02724630903413032. S2CID 54029279.
  11. ^ a b c d e f g h i j k l m n o Lucas, Spencer G.; Mateer, Niall J.; Hunt, Adrian P.; O'Neill, F. Michael (1987). Dinosaurs, the age of the Fruitland and Kirtland Formations, and the Cretaceous-Tertiary boundary in the San Juan Basin, New Mexico.
  12. ^ a b c Weishampel, David B.; Dodson, Peter; Osmólska, Halszka, eds. (2004). The Dinosauria, 2nd edition. Berkeley: University of California Press. p. 580. ISBN 0-520-24209-2. Retrieved 2019-02-21.
  13. ^ David C. Evans, Derek William Larson, Thomas Michael Cullen & Robert M Sullivan (2014) ‘Saurornitholestes’ robustus is a troodontid (Dinosauria: Theropoda). Canadian Journal of Earth Sciences 51: (7): 730-734. doi: 10.1139/cjes-2014-0073 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2014-0073
  14. ^ David C. Evans, Derek William Larson, Thomas Michael Cullen & Robert M Sullivan (2014) ‘Saurornitholestes’ robustus is a troodontid (Dinosauria: Theropoda). Canadian Journal of Earth Sciences 51: (7): 730-734. doi: 10.1139/cjes-2014-0073 http://www.nrcresearchpress.com/doi/abs/10.1139/cjes-2014-0073
  15. ^ Fassett, James E.; Hinds, Jim S. (1971). "Geology and Fuel Resources of the Fruitland Formation and Kirtland Shale of the San Juan Basin, New Mexico and Colorado". U.S. Geological Survey Professional Paper. Professional Paper. 676. doi:10.3133/pp676.
  16. ^ Fenton, James (May 12, 2016). "Geologist: Coal outcrops cause methane hot spot". Farmington Daily Times. Retrieved 2019-12-21.
  17. ^ Elliott, Dan (2016-08-15). "Methane "hot spot" over Four Corners linked to oil, gas production sites". The Denver Post. Retrieved 2019-12-21.
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