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Hornerstown Formation

From Wikipedia, the free encyclopedia

The Hornerstown Formation is a Paleogene or latest Mesozoic geologic formation in New Jersey.[2] The age of these deposits have been controversial. While most fossils are of animals types known from the earliest Cenozoic era, several fossils of otherwise exclusively Cretaceous age have been found. These include remains of the shark Squalicorax, several types of non-avian dinosaurs, the teleost fish Enchodus, several species of ammonite, and marine lizards referred to the genus Mosasaurus. Some of these remains show signs of severe abrasion and erosion, however, implying that they are probably re-worked from older deposits. Most of these fossils are restricted to the lowest point in the formation, one rich in fossils and known as the Main Fossiliferous Layer, or MFL. Other explanations for the out-of-place fossils in the MFL is that they represent a time-averaged assemblage that built up and remained unburied during a time of low sediment deposition, or that they were stirred up from deeper in the sediment and deposited together during a tsunami.[3]

Vertebrate paleofauna

Birds

Birds of the Hornerstown Formation
Genus Species Location Stratigraphic position Abundance Notes

Anatalavis[4]

A. rex.[4]

Graculavus[4]

G. velox[4]

Laornis[4]

L. edwardsianus[4]

Palaeotringa[4]

P. littoralis[4]

P. vagans[4]

Telmatornis[4]

T. priscus[4]

Tytthostonyx[4]

T. glauconiticus[4]

Non-Avian Dinosaurs

Dinosaurs of the Hornerstown Formation
Genus Species Location Stratigraphic position Abundance Notes

Dryptosaurus[5]

D. aquilunguis

Gloucester County Maastrichtian

Turtles

Testudines of the Hornerstown Formation
Genus Species Location Stratigraphic position Abundance Notes

Osteopygis[1]

O. emarginatus

Maastrichtian-Danian
Euclastes E. wielandi found as a separate genus from the cranial material of Osteopygis

Crocodylomorphs

Crocodylomorphs of the Hornerstown Formation
Genus Species Location Stratigraphic position Abundance Notes

Bottosaurus[6]

B. harlani.

Hyposaurus[7] H. rogersii

Ray-finned Fishes

Actinopterygii of the Hornerstown Formation
Genus Species Location Stratigraphic position Abundance Notes

Iridopristis[8]

I. parrisi[8]

Sewell, New Jersey Danian A stem-lineage member of Holocentridae.

See also

References

  1. ^ a b Gentry, A.D.; Kiernan, C.R.; Parham, J.F. (2022). "A large non-marine turtle from the Upper Cretaceous of Alabama and a review of North American "Macrobaenids"". The Anatomical Record. doi:10.1002/ar.25054.
  2. ^ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  3. ^ Gallagher, W.B. (2005). "Recent mosasaur discoveries from New Jersey and Delaware, USA: stratigraphy, taphonomy and implications for mosasaur extinction." Netherlands Journal of Geosciences — Geologie en Mijnbouw, 84(3): 241-245. [1] Archived 2012-09-04 at the Wayback Machine
  4. ^ a b c d e f g h i j k l m "3.22 New Jersey, United States; 7. Hornerstown Formation," in Weishampel, et al. (2004). Page 586.
  5. ^ Olsson, R.K. (1960). "Foraminifera of latest Cretaceous and earliest Tertiary age in the New Jersey coastal plain". Journal of Paleontology. 34: 1–58.
  6. ^ Cossette, A. P., and C. A. Brochu. 2018. A new specimen of the alligatoroid Bottosaurus harlani and the early history of character evolution in alligatorids. Journal of Vertebrate Paleontology. DOI:10.1080/02724634.2018.1486321.
  7. ^ Morgan, Donald J (December 2018). "PRESENCE OF A DYROSAURID NEOSUCHIAN IN THE SEVERN/BRIGHTSEAT FORMATION OF MARYLAND". The Journal of the Delaware Valley Paleontological Society. X: 91 to 104.
  8. ^ a b Andrews, J. V.; Schein, J. P.; Friedman, M. (2023). "An earliest Paleocene squirrelfish (Teleostei: Beryciformes: Holocentroidea) and its bearing on the timescale of holocentroid evolution". Journal of Systematic Palaeontology. 21 (1). doi:10.1080/14772019.2023.2168571.

Bibliography

  • Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.


This page was last edited on 24 March 2024, at 20:22
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