Fruitland Formation

Coordinates: 36°45′07″N 108°26′31″W / 36.752°N 108.442°W / 36.752; -108.442
Source: Wikipedia, the free encyclopedia.
Fruitland Formation
Ma
Approximate paleocoordinates
43°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)

The Fruitland Formation is a

age of the late Cretaceous.[2]

The Fruitland Formation shares its name with Fruitland, New Mexico. That city is on what was the western shore of the Western Interior Seaway.[3]

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

Baculites scotti, therefore placing the base of the Fruitland Formation at ~76.3 Ma.[4]

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.[5] Intermediate[5] Fossil Forest[5] One print[5] Giant hadrosaur track, indicating an individual larger than Shantungosaurus, the largest known hadrosaur.[5]
Parasaurolophus
Pentaceratops
Stegoceras
Titanoceratops
Parasaurolophus[6] P. cyrtocristatus[6] Fossil Forest[6] A partial skull associated with a mostly complete postcranial skeleton, and a partial skull and fragmentary ribs of a juvenile individual.[6] A lambeosaurine hadrosaurid also known from the Kaiparowits Formation.[6]
Pentaceratops[7] P. sternbergii[7] Fossil Forest[7] [Two] nearly complete skulls and a nearly complete frill.[7] A chasmosaurine ceratopsid also known from the Kirtland Formation.[7]
Stegoceras[8] S. novomexicanum[8] Fossil Forest[8] Partial remains of [three] frontals and nearly complete frontoparietal.[8] A basal
pachycephalosaurid also known from the lower Kirtland Formation.[8]
Titanoceratops[9] T. ouranos[9] A partial skull, syncervical vertebrae, cervical vertebrae, dorsal vertebrae, sacral vertebrae, caudal vertebrae, ribs, humeri, radius, femora, tibiae, fibula, ilia, ischia, and ossified tendons.[9] Possibly represents a junior synonym of Pentaceratops, holotype may possibly have come from the Kirtland Formation.[9]

Saurischians

Some remains (OMNH 10131) of Bistahieversor may actually have originated in the upper Fruitland Formation.[10]

Saurischians
of the Fruitland Formation
Genus Species Member Abundance Notes Images
Bistahieversor[11] B. sealeyi[11] Fossil Forest[11] A rostral ramus of a lacrimal, and a partial skull and postcranial skeleton of an adult individual.[11] A eutyrannosaur tyrannosauroid also known from the Kirtland Formation.[11]
Bistahieversor
Ornithomimus
Dromaeosauridae[12] Indeterminate[12] Fossil Forest[12] Numerous isolated teeth.[12] Indeterminate dromaeosaurid remains.[12]
Ornithomimidae[12] Indeterminate[12] Fossil Forest[12] Distal end of metatarsals, distal end of a phalanx, and foot-bone fragments.[12] Indeterminate ornithomimid ornithomimosaur remains.[12]
cf. Ornithomimus[12] cf. O edmontonicus[12] Fossil Forest[12] A manual ungual.[12] Material possibly referable to Ornithomimus.[12]
?Troodontidae[13] Indeterminate[13] Fossil Forest[13] Isolated teeth.[14] Formerly identified as Paronychodon sp., referral to Troodontidae doubtful.[15]
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.[16]

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.[17][18]

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. ^ National Geographic Map of the Day, published in May 2014, depicting North America about 77 million years ago; https://twitter.com/natgeomaps/status/1129816543251054592
  4. PMID 29166406
    .
  5. ^ 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.
  6. ^
    PMID 33552721
    .
  7. ^ .
  8. ^ a b c d e Steven E. Jasinski; 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.
  9. ^ .
  10. ^ .
  11. ^ .
  12. ^ . 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. .
  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.