Old Church Formation
Appearance
Old Church Formation | |
---|---|
Stratigraphic range: Oligocene | |
Type | Formation |
Unit of | Chesapeake Group |
Underlies | Calvert Formation, Popes Creek Sand |
Overlies | Pamunkey Group, Piney Point Formation |
Location | |
Region | Virginia |
Country | United 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.
Species
[edit]Some of the species known from the Old Church Formation are included below. Further study will likely reveal a more diverse fauna.[1]
Chondrichthyans
[edit]Cetaceans
[edit]- Xenorophidae sp.
- Micromysticetus sp.[2]
- cf. Ankylorhiza sp.[2]
- cf. Xenorophus sloani[2]
- aff. Coronodon sp.[2]
- aff. Cotylocara sp. and Echovenator sp.[2]
- aff. Eosqualodon sp.[2]
Chelonians
[edit]- Mercenaria gardnerae
- Anomia ruffini
- "Pectin" seabeensis
- "Pectin" sp.
- Lucina sp.
- Plicatula sp.
- Epitonium sp.
- Panopea sp.
- Cyclocardia sp.
- Astarte sp.
- Pycnodonte sp.
- Isognomon sp.
- "Cardium" sp.
- Bicorbula idonea
- Macrocallista sp.
- Diadora sp.
- Ecphora sp.
- Trophon sp.
- Calypttaea sp.
See also
[edit]References
[edit]- ^ Weems, Robert (2014). "Paleogene chelonians from Maryland and Virginia" (PDF). PaleoBios. 31 (1).
- ^ 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.
- ^ 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.
- Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.