| Wynniatt Formation | |
|---|---|
| Stratigraphic range: Tonian [1] | |
| Type | Geological Formation |
| Sub-units | Member 1, 2, 3 and 4 |
| Underlies | Kilian Formation [2] |
| Overlies | Boot Inlet Formation [2] |
| Thickness | 500 - 800 m (1,640 - 2,624 ft) |
| Lithology | |
| Primary | Dolomite |
| Other | Mudstone, Siltstone, Quartz arenite, Sandstone, Limestone, Gabbro |
| Location | |
| Region | Nunavut |
| Country | Canada |
The Wynniatt Formation is a geologic formation in Nunavut. It preserves enigmatic fossils dating back to the Middle to Late Tonian period, around 850 Ma - 760 Ma. [3]
Due to the large thickness of the Wynniatt Formation, it is broken up into 4 Members, simply named "Member" 1 - 4, and from the rocks contained within these 4 members, a rough idea of what the paleoenvironments may have looked across the formation are as follows: [2]
- Member 1 : Periodically exposed inter-tidal mudflat.
- Member 2 : Shallow sub-tidal to inter-tidal with layers of microbial mat, and is also the fossil bearing member. [3]
- Member 3 : Extensive shelf-marginal reef complex, which itself is overlain by deposits of lagoons and a back-reef agal flat.
- Member 4 : Cycles of shallow sub-tidal to inter-tidal.
After Butterfield, 2005. [3]
Color key
| Notes Uncertain or tentative taxa are in small text; |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Cheilofilum |
| Enigmatic 1.2mm long filamentous organism. | |
| Chuaria |
| Enigmatic fossil, possibly synonymous with Tawuia. | |
| Clavitrichoides |
| Enigmatic filamentous organism, most material from this formation are possibly less well preserved Cheilofilum. | |
| Osculosphaera |
| Enigmatic filamentous organism. | |
| Plicatosphaeridium |
| Enigmatic filamentous organism. | |
| Tappania |
| Acanthomorph acritarch. | |
| Tawuia |
| Enigmatic fossil, possibly an alga. | |