Chandler Formation
| Chandler Formation Stratigraphic range: Early Jurassic (Hettangian) |
|
|---|---|
| Type | Geological formation |
| Underlies | Bravo Lake Formation |
| Location | |
| Region | Baffin Island (Crimmins Island) |
| Country | Canada  Canada |
The Chandler Formation is a Mesozoic geologic formation. Dinosaur remains are among the fossils that have been recovered from the formation, although none have yet been referred to a specific genus.[1]
Contents
Vertebrate fauna
Crinoidea
Color key
|
Notes Uncertain or tentative taxa are in small text; |
| Crinoidea of the Chandler Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
|
P. dargniesi |
|
"Some indeterminate Fossils." |
||||
Bony Fish
Color key
|
Notes Uncertain or tentative taxa are in small text; |
| Ray-finned fish of the Chandler Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
|
P. sacidus |
|
"Partal Skeleton." |
The Antecesor of Lepidotus |
|||
|
T. magnificus |
|
"Scales and skull bones." |
||||
Synapsids
| Synapsids of the Chandler Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
|
A. parvidens |
A cynodont. |
|||||
Dinosaurs
Color key
|
Notes Uncertain or tentative taxa are in small text; |
| Dinosaurs of the Chandler Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
|
Indeterminate |
|
"Tibia." |
Actually indeterminate ceratosaur remains. |
|||
See also
- List of volcanoes in Canada
- Volcanism of Canada
- Volcanism of Northern Canada
- Geography of Nunavut
- List of dinosaur-bearing rock formations
Footnotes
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- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.
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- ↑ Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
