Kanguk Formation
| Kanguk Formation | |
|---|---|
| Stratigraphic range: Cenomanian-Maastrichtian ~ | |
| Type | Geological formation |
| Sub-units | Eglinton Member |
| Underlies | Expedition Formation |
| Overlies | Hassel Formation |
| Thickness | up to 365 metres (1,200 ft)[1] |
| Lithology | |
| Primary | Shale, siltstone |
| Other | Sandstone, tuff |
| Location | |
| Coordinates | Lua error: callParserFunction: function "#coordinates" was not found. |
| Region | Northwest Territories, Nunavut |
| Country | Canada |
| Type section | |
| Named for | Kanguk Peninsula |
| Named by | Souther |
| Year defined | 1963 |
Kanguk Formation (Canada) | |
The Kanguk Formation is a geological formation in the Northwest Territories and Nunavut, Canada whose strata date back to the Late Cretaceous.[2] Dinosaur remains are among the fossils that have been recovered from the formation.[3]
It was first described in the Kanguk Peninsula of the Axel Heiberg Island, along the shore of the Stand Fiord by Souther in 1963.[4] The formation occurs throughout the Sverdrup Basin and the southern Queen Elizabeth Islands.
Lithology
[edit | edit source]The Kanguk Formation is composed of dark shale and siltstone with interbeds of sandstone, bentonite and tuff.[1] Thicker sandstone and conglomerate beds occur in the western reaches in Eglinton Island.
Fossil content
[edit | edit source]The Kanguk Formation preserves an extensive record of shelf assemblages rich in benthic foraminifera that reveal numerous pulses of local hypoxia.[5] Fish fossils have been unearthed here.[6]
| Dinosaurs of the Kanguk Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Abundance | Description | Images |
| Canadaga | C. arctica | A Hesperomithes | ||||
| Hesperornis[3] | Indeterminate[3] | |||||
| Hadrosauridae[7][8][9] | Indeterminate | |||||
| Lambeosaurinae[10][11] | Indeterminate | |||||
| Tyrannosauroidea[10] | Indeterminate | |||||
| Ornithomimidae[12] | Indeterminate | |||||
| Plesiosauroidea[13] | Indeterminate | |||||
| Aurorachelys[14][15] | A. gaffneyi | |||||
| Champsosaurus[16][17] | Champsosaurus sp. | |||||
See also
[edit | edit source]References
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- ^ a b c Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, North America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 574-588. Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value)..
- ^ Geological Survey of Canada Map 36-1959
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Further reading
[edit | edit source]- A. T. Pugh, C. J. Schröder-Adams, E. S. Carter, J. OHerrle, J. Galloway, J. W. Haggart, J. L. Andrews and K. Hatsukanoc. 2014. Cenomanian to Santonian radiolarian biostratigraphy, carbon isotope stratigraphy and paleoenvironments of the Sverdrup Basin, Ellef Ringnes Island, Nunavut, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology 413:101-122
- J. A. Tarduno, D. B. Brinkman, P. R. Renne, R. D. Cottrell, H. Scher and P. Castillo. 1998. Evidence for extreme climatic warmth from Late Cretaceous Arctic vertebrates. Science 282:2241-2244
- Geologic formations of the Northwest Territories
- Geologic formations of Nunavut
- Upper Cretaceous Series of North America
- Maastrichtian Stage of North America
- Campanian Stage
- Cenomanian Stage
- Coniacian Stage
- Santonian Stage
- Turonian Stage
- Sandstone formations of Canada
- Shale formations of Canada
- Siltstone formations of Canada
- Tuff formations of Canada