Sutherland Pit: Late/Upper Pleistocene, Canada

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia - Proboscidea - Elephantidae
Mammuthus sp. Brookes 1828
"mammoth" teeth: listed as Proboscidea by SwaraWoolf 1981
Mammalia - Carnivora - Mustelidae
? Taxidea sp. Waterhouse 1839
SkwaraWoolf 1981
Mammalia - Cervidae
Cervus sp. Linnaeus 1758
SkwaraWoolf 1981
Mammalia - Bovidae
Bison sp. Hamilton-Smith 1827
Mammalia - Perissodactyla - Equidae
Equus niobrarensis Hay 1913
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]