Old Church Formation

Geologic formation in Virginia, U.S.
Old Church Formation
Stratigraphic range: Oligocene
Xenorophid(?) Cetacean tooth from the Old Church formation of Virginia
TypeFormation
Unit ofTrent Supergroup
UnderliesCalvert Formation, Popes Creek Sand
OverliesPamunkey Group, Piney Point Formation
Location
RegionVirginia, Maryland
CountryUnited States

The Old Church Formation is a geologic formation in Virginia and possibly Maryland. It preserves fossils dating back to the Oligocene epoch of the Paleogene period. It rarely exposes on land and is under-studied. However, deposits from this period are rare and the Old Church Formation likely contains many scientifically significant taxa. Ward (1985) recommended placing this formation in the Chesapeake Group.[1]

Species

Some of the species known from the Old Church Formation are included below. Further study will likely reveal a more diverse fauna.[2]

Chondrichthyans

  • Otodus angustidens
  • Hemipristis serra
  • Alopias vulpinus
  • Squatina prima?

Cetaceans

  • Xenorophidae sp.
  • Micromysticetus sp.[3]
  • cf. Ankylorhiza sp.[3]
  • cf. Xenorophus sloani[3]
  • aff. Coronodon sp.[3]
  • aff. Cotylocara sp. and Echovenator sp.[3]
  • aff. Eosqualodon sp.[3]

Chelonians

Invertebrates[1]

See also

  • Earth sciences portal
  • flagVirginia portal
  • iconPaleontology portal

References

  1. ^ a b Ward, Lauck W. (1985). "Stratigraphy and characteristic mollusks of the Pamunkey Group (lower Tertiary) and the Old Church Formation of the Chesapeake Group; Virginia Coastal Plain". Professional Paper. doi:10.3133/pp1346. ISSN 2330-7102.
  2. ^ Weems, Robert (2014). "Paleogene chelonians from Maryland and Virginia" (PDF). PaleoBios. 31 (1).
  3. ^ a b c d e f Weems, Robert E; Boessnecker, Robert W; Sanders, Albert E (2022). "Cetacean remains from the Lower Oligocene Old Church Formation of Virginia". The Mosasaur. 12: 29–44.
  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.


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