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 paleoenviroments 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. | ![]() |