Sutherland Pit: Late/Upper Pleistocene, Canada
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia
- Proboscidea
- Elephantidae
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Mammuthus sp.
Brookes 1828
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"mammoth" teeth: listed as Proboscidea by SwaraWoolf 1981 | ||||||||||
Mammalia
- Carnivora
- Mustelidae
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? Taxidea sp.
Waterhouse 1839
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SkwaraWoolf 1981 | |||||||||
Mammalia
- Cervidae
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Cervus sp.
Linnaeus 1758
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SkwaraWoolf 1981 | |||||||||
Mammalia
- Bovidae
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Bison sp.
Hamilton-Smith 1827
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Mammalia
- Perissodactyla
- Equidae
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Equus niobrarensis
Hay 1913
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listed as Equus sp. by SwaraWoolf 1981 | ||||||||||
see common names |
Geography
Country: | Canada | State/province: | Saskatchewan |
Coordinates: | 52.2° North, 106.6° West (view map) | ||
Paleocoordinates: | 52.2° North, 106.6° West | ||
Basis of coordinate: | stated in text | ||
Geographic resolution: | outcrop |
Time
Period: | Quaternary | Epoch: | Pleistocene |
Stage: | Late/Upper Pleistocene | 10 m.y. bin: | Cenozoic 6 |
Key time interval: | Late/Upper Pleistocene | ||
Age range of interval: | 0.12900 - 0.01170 m.y. ago |
Stratigraphy
Formation: | Floral | ||||
Stratigraphic resolution: | group of beds | ||||
Stratigraphy comments: from throughout a section about 12 feet thick thought to be of "late Pleistocene age, dating from the time of withdrawal of the Wisconsin ice" based on superposition above a till the hardpan is believed by SkwaraWoolf (1981) to possibly represent the Floral Formation, but the overlying sequence (called by her a "gravel") that yielded most of the fossils does not |
Lithology and environment
Primary lithology: | coarse conglomeratic sandstone |
Lithology description: "Coarse angular sand with pebbles and boulders; imperfectly stratified; bones and teeth at base" above and sometimes within a "basal layer of sand, about 0.5 inch in thickness, that has been cemented by calcareous material into a hardpan" and is immediately above a glacial till | |
Environment: | fluvial indet. |
Glacial or sequence phase: | late glacial |
Geology comments: thought to have been deposited "in or near the lake that formed in this area while the ice lay not very far to the northeast" but lithology is only consistent with a fluvial environment |
Taphonomy
Modes of preservation: | body |
Size of fossils: | macrofossils |
Temporal resolution: | time-averaged |
Spatial resolution: | allochthonous |
Collection methods and comments
Collection methods: | salvage,survey of museum collection |
Reason for describing collection: | general faunal/floral analysis |
Museum repositories: | ROM |
Collection method comments: ROM and University of Saskatchewan collections
discovered by "employees of the Dominion Forest Nursery Station... while excavating for sand" and visited by "the writer and his wife" in 1940, although it is not clear whether material was collected during this visit | |
Taxonomic list comments:fossils may derive from gravel overlying Floral Fm. and therefore may be Wisconsinan or younger (SkwaraWoolf 1981) |
Metadata
Also known as: | Duh | ||
Database number: | 20317 | ||
Authorizer: | J. Alroy | Enterer: | J. Alroy |
Modifier: | J. Alroy | Research group: | vertebrate |
Created: | 1995-03-26 00:00:00 | Last modified: | 2010-01-27 23:30:42 |
Access level: | the public | Released: | 1995-03-26 00:00:00 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
31770. | L. S. Russell. 1943. Pleistocene horse teeth from Saskatchewan. Journal of Paleontology 17(1):110-114 [J. Alroy/J. Alroy] |
Secondary references:
3182 | T. SkwaraWoolf. 1981. Biostratigraphy and paleoecology of Pleistocene deposits (Riddell Member, Floral Formation, Late Rancholabrean), Saskatoon, Canada. Canadian Journal of Earth Sciences 18 [J. Alroy/J. Alroy/J. Ju] |