RTMP L2000, Horsethief Canyon: Early/Lower Maastrichtian, Canada
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Mammalia
|
||||||||||
Mammalia indet.
Linnaeus 1758
|
4 specimens | |||||||||
Mammalia
- Pediomyidae
|
||||||||||
Pediomys sp.
Marsh 1889
|
1 specimen | |||||||||
= Pediomyidae indet.
Simpson 1927
|
Alroy 2007 | |||||||||
Reptilia
- Tyrannosauridae
|
||||||||||
Tyrannosauridae indet.
Osborn 1906
|
25 specimens | |||||||||
Reptilia
- Troodontidae
|
||||||||||
Troodon sp.
Leidy 1856
|
65 specimens | |||||||||
= Albertavenator curriei
Evans et al. 2017
|
Funston and Currie 2018 | |||||||||
Reptilia
- Dromaeosauridae
|
||||||||||
Richardoestesia sp.
Currie et al. 1990
|
11 specimens | |||||||||
cf. Saurornitholestes sp.
Sues 1978
|
8 specimens | |||||||||
= Dromaeosaurinae indet.
Matthew and Brown 1922
|
Larson and Currie 2013 | |||||||||
TMP 1998.084.0003 | ||||||||||
Reptilia
|
||||||||||
Paronychodon sp.
Cope 1876
|
1 specimen | |||||||||
Reptilia
- Hadrosauridae
|
||||||||||
Hadrosauridae indet.
Cope 1869
|
224 specimens | |||||||||
see common names |
Geography
Country: | Canada | State/province: | Alberta |
Coordinates: | 51.5° North, 112.9° West (view map) | ||
Paleocoordinates: | 59.2° North, 84.6° West | ||
Basis of coordinate: | estimated from map | ||
Altitude: | 2397 feet | ||
Geographic resolution: | small collection |
Time
Period: | Cretaceous | Epoch: | Late/Upper Cretaceous |
Stage: | Maastrichtian | 10 m.y. bin: | Cretaceous 8 |
Key time interval: | Early/Lower Maastrichtian | ||
Age range of interval: | 72.10000 - 66.00000 m.y. ago |
Stratigraphy
Geological group: | Edmonton | Formation: | Horseshoe Canyon |
Stratigraphic resolution: | bed |
Lithology and environment
Primary lithology: | sideritic silty,carbonaceous "shale" |
Secondary lithology: | ironstone |
Includes fossils? | Y |
Lithology description: "3.5 m thick, olive-coloured, silty shale that contains a prominent ironstone layer, abundant small siderite nodules and rare sideritized rhizoliths" | |
Environment: | "channel" |
Geology comments: meandering channel deposits interpreted as having been deposited in an overbank setting during a flood event; scattered fossils are interpreted to represent a modern deflational lag formed by winnowing away of fine-grained sediments |
Taphonomy
Modes of preservation: | body |
Degree of concentration: | dispersed |
Size of fossils: | macrofossils,mesofossils |
Spatial orientation: | random |
Preservation of anatomical detail: | variable |
Articulated whole bodies: | none |
Associated major elements: | none |
Fragmentation: | frequent |
Collection methods and comments
Collection methods: | surface (float),surface (in situ),sieve,field collection |
Reason for describing collection: | taxonomic analysis |
Metadata
Database number: | 60563 | ||
Authorizer: | M. Carrano, J. Alroy | Enterer: | K. Maguire, J. Alroy, M. Carrano |
Modifier: | M. Carrano | Research group: | vertebrate |
Created: | 2006-05-17 11:45:59 | Last modified: | 2023-04-07 15:54:57 |
Access level: | the public | Released: | 2006-05-17 11:45:59 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
17404. | ETE | M. J. Ryan, P. J. Currie, J. D. Gardner, M. K. Vickaryous, and J. M. Lavigne. 2000. Baby hadrosaurid material associated with an unusually high abundance of Troodon teeth from the Horseshoe Canyon Formation, Upper Cretaceous, Alberta, Cananda. Gaia 15:123-133 [M. Carrano/K. Maguire/M. Carrano] |
Secondary references:
19636 | J. Alroy. 2007. Synonymies and reidentifications of North American fossil vertebrates and so forth. [J. Alroy/J. Alroy] | |
84397 | G. F. Funston and P. J. Currie. 2018. The first record of dinosaur eggshell from the Horseshoe Canyon Formation (Maastrichtian) of Alberta, Canada. Canadian Journal of Earth Sciences 55(4):436-441 [M. Carrano/M. Carrano] | |
48570 | D. W. Larson and P. J. Currie. 2013. Multivariate analyses of small theropod dinosaur teeth and implications for paleoecological turnover through time. PLoS ONE 8(1):e54329:1-14 [M. Carrano/M. Carrano/M. Carrano] |