Otterton Point, Budleigh Salterton: Anisian, United Kingdom
collected by Whitaker 1868
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia
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Hyperodapedon sp.
Huxley 1859
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Whitaker 1869 | 1 specimen | ||||||||
GSM 90494, anterior right maxilla | ||||||||||
= Hyperodapedon gordoni
Huxley 1859
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Newton 1905 | |||||||||
Benton 1990 | ||||||||||
see common names |
Geography
Country: | United Kingdom | State/province: | England | County: | Devon |
Coordinates: | 50.6° North, 3.3° West (view map) | ||||
Paleocoordinates: | 27.8° North, 19.4° East (Wright 2013) | ||||
Basis of coordinate: | stated in text | ||||
Geographic resolution: | small collection |
Time
Period: | Triassic | Epoch: | Middle Triassic |
Stage: | Anisian | 10 m.y. bin: | Triassic 2 |
Key time interval: | Anisian | ||
Age range of interval: | 246.7 - 241.464 m.y. ago |
Stratigraphy
Geological group: | Sherwood Sandstone | Formation: | Otter Sandstone | ||
Stratigraphic resolution: | formation | ||||
Stratigraphy comments: lower part of the formation, early-mid Anisian: "The unit is dated as Anisian on the basis of faunal comparisons and matching with palynologically dated units in the English Midlands... This has since been confirmed by magnetostratigraphy (Hounslow and McIntosh 2003), who found that the lower parts of the Otter Sandstone Formation correspond to the early and mid Anisian, and the upper parts, which contain the majority of the macrofossils correlate with late Anisian and latest Anisian magnetozones on the marine standard." |
Lithology and environment
Primary lithology: | "cross stratification",concretionary lithified conglomeratic sandstone |
Includes fossils? | Y |
Lithology description: "At Otterton Point hard, calcite-cemented, cross-bedded sandstone units in the Otter Sandstone Formation contain clacite-cemented rhizoliths and other calcrete formations...the [specimen] came from the zone of breccia and calcite-cemented nodules" | |
Environment: | dry floodplain |
Geology comments: "Purvis and Wright (1991) attributed the large vertical rhizoliths to deep-rooted phreatophytic plants which colonized bars and abandoned channels on a large braidplain" |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Disassociated major elements: | all |
Collection methods and comments
Collection methods: | surface (in situ),field collection | ||
Reason for describing collection: | taxonomic analysis | ||
Collectors: | Whitaker | Collection dates: | 1868 |
Metadata
Database number: | 88984 | ||
Authorizer: | R. Butler, M. Carrano | Enterer: | R. Butler, M. Carrano |
Modifier: | M. Carrano | Research group: | vertebrate |
Created: | 2009-04-27 07:56:56 | Last modified: | 2025-02-22 15:12:02 |
Access level: | the public | Released: | 2009-04-27 07:56:56 |
Creative Commons license: | CC0 |
Reference information
Primary reference:
29827. | T. H. Huxley. 1869. On Hyperodapedon. Quarterly Journal of the Geological Society of London 25:138-152 [R. Butler/R. Butler] |
Secondary references:
28945 | M. J. Benton. 1990. The species of Rhynchosaurus, a rhynchosaur (Reptilia, Diapsida) from the Middle Triassic of England. Philosophical Transactions of the Royal Society of London, Series B 328:213-306 [J. Mueller/T. Liebrecht/R. Butler] | |
15587 | ETE | M. J. Benton and P. S. Spencer. 1995. Fossil Reptiles of Great Britain. Chapman & Hall, London 1-386 [M. Carrano/K. Maguire/J. Tennant] |
69432 | W. J. Harrison. 1882. Geology of the Counties of England and of North and South Wales xxviii-346 [M. Carrano/M. Carrano] | |
51970 | E. T. Newton. 1905. Notes on the Triassic fossils (excluding Rhaetic) in the Museum of the Geological Survey at Jermyn Street, London. Report of the British Association for the Advancement of Science 1904:282-285 [M. Carrano/M. Carrano] | |
29825 | W. Whitaker. 1869. On the succession of beds in the "New Red" on the south coast of Devon, and on the locality of a new specimen of Hyperodapedon. Quarterly Journal of the Geological Society of London 25:152-158 [R. Butler/R. Butler] |