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The Belgrade Formation is a limestone geologic formation in North Carolina characterized by limestone coquina mixed with sand, and thinly laminated clays.[2] It preserves fossils dating back to the Paleogene period.
Description
The Belgrade Formation is composed of two subunits: the Pollocksville member and the Haywood Landing member. The Pollocksville member is composed of unconsolidated oyster shells and sand. It was deposited in the Oligocene and early Miocene. The Haywood Landing member is composed of shelly sands and thinly laminated clays. The Belgrade Formation was originally considered part of an Eocene formation called the Trent Marl before it was identified as being deposited in the Miocene and split off.[2]
Strontium isotope dating suggests that the marine invertebrates in the formation primarily originate from an older Late Oligocene-aged facies, while the vertebrates (including the land mammals and sharks) date to a younger, earliest Miocene-aged facies.[3]
Fossil content
Mammals
A small but diverse land mammal fauna is known from the formation.[3]
Rodents
Lagomorphs
| Genus |
Species |
Presence
|
Material |
Notes |
Images
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| cf. Megalagus
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cf. M. sp.
|
Jones County[3]
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A leporid.
|
|
Carnivorans
Perissodactyls
Artiodactyls
Cetaceans
Sirenians
Reptiles
| Reptiles
|
| Genus |
Species |
Presence
|
Material |
Notes |
Images
|
| Chelonioidea
|
|
Belgrade Quarry.[5]
|
|
Indeterminate sea turtle remains.
|
|
| Crocodilia
|
|
Belgrade Quarry.[5]
|
|
Indeterminate crocodilian remains.
|
|
Fish
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|
|
|
Color key
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Notes Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
|
Invertebrates
See also
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References
- ^ Page Module:Citation/CS1/styles.css has no content.Ward, L. W.; Lawrence, D. R.; Blackwelder, B. W. (1978). "Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina". Bulletin. doi:10.3133/b1457F.
- ^ a b c Page Module:Citation/CS1/styles.css has no content.Ward, Lauck W.; Lawrence, David R.; Blackwelder, Blake W. (1979). "Stratigraphic revision of the middle Eocene, Oligocene, and lower Miocene; Atlantic Coastal Plain of North Carolina" (PDF). U.S. Geological Survey Bulletin. 1457-F: 3–10. Retrieved 26 June 2018.
- ^ a b c d e f Page Module:Citation/CS1/styles.css has no content.MacFadden, Bruce J.; Bohaska, David J.; Cone, Lee; Killingsworth, Stephanie R.; Zbinden, Samantha P.; Pirlo, Jeanette; Moran, Sean M.; Baskin, Jon; Perez, Victor J. (2025). "Early Miocene land mammals and chronology of the Belgrade Formation, eastern North Carolina". Journal of Paleontology. 99 (1): 241–261. doi:10.1017/jpa.2024.68. ISSN 0022-3360.
- ^ a b Page Module:Citation/CS1/styles.css has no content.Baskin, Jon; Dickinson, Edward; Hartstone-Rose, Adam (2020-07-08). "?Amphictis (Carnivora, Ailuridae) from the Belgrade Formation of North Carolina, USA". PeerJ. 8: e9284. doi:10.7287/peerj.9284v0.1/reviews/2. PMC 7353912. PMID 32714653.
- ^ a b c d e f g h i j k l m n o p q r s t u v w Page Module:Citation/CS1/styles.css has no content.Boessenecker, Robert W.; Ahmed, Erum; Geisler, Jonathan H. (2017-11-08). "New records of the dolphin Albertocetus meffordorum (Odontoceti: Xenorophidae) from the lower Oligocene of South Carolina: Encephalization, sensory anatomy, postcranial morphology, and ontogeny of early odontocetes". PLOS ONE. 12 (11) e0186476. Bibcode:2017PLoSO..1286476B. doi:10.1371/journal.pone.0186476. ISSN 1932-6203. PMC 5695589. PMID 29117197.
- ^ a b c d e f g h i j k l m n o p q r s t u v w Page Module:Citation/CS1/styles.css has no content.Boessenecker, Robert W. (2022-09-03). "Oligocene-Miocene marine mammals from Belgrade Quarry, North Carolina". Geobios. 74: 1–19. Bibcode:2022Geobi..74....1B. doi:10.1016/j.geobios.2022.08.002. ISSN 0016-6995. S2CID 252077178.
- ^ Page Module:Citation/CS1/styles.css has no content."Late Oligocene sharks and rays from the Chandler Bridge Formation, Dorchester County, South Carolina, USA - Acta Palaeontologica Polonica". www.app.pan.pl. Retrieved 2022-09-06.
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