| Fermeuse Formation | |
|---|---|
| Stratigraphic range: Ediacaran | |
| Beds of the Fermeuse Formation near Ferryland, NL; note Aspidella discs | |
| Type | Formation |
| Unit of | St John's Group [1] |
| Underlies | Renews Head Formation [2] |
| Overlies | Trepassey Formation |
| Thickness | 1400 m (4,593 ft) [3] |
| Lithology | |
| Primary | Gray Shale [4] |
| Other | Sandstone, Siltstone [4] |
| Location | |
| Region | Newfoundland and Labrador |
| Country | Canada |
| Occurrence of Fermeuse formation in southeast Newfoundland | |
The Fermeuse Formation is an Ediacaran aged geologic formation in Newfoundland and Labrador, Canada.
It is known to outcrop on both the Avalon and Bonavista Peninsulas, both of which preserve fossils.
On Bonavista Peninsula the depositional environment was a slope and outer shelf–below photic zone Turbidites probably were the dominant sediment transporters. [5]
It is predominantly silts and sands, in contrast to underlying Trepassey Formation, which is mostly dark grey shales. There is a coarsening up sequence throughout the two formations, such that the top of the Fermeuse is predominantly sandstones. [5]
On Avalon Peninsula there were much shallower waters, particularly than in underlying Mistaken Point Formation and Trepassey Formation. [1] It is indicated by sandy channel fills, slumping, occasional silts. [1] There is a possible delta front and shallow slope setting. [1]
On Avalon Peninsula [1] there is low diversity, and includes rare agglutinating organisms, Palaeopascichnus , [6] and Aspidella discs, [7] sometimes in great concentrations. [5]
On Bonavista Peninsula there is higher diversity, including more fronds (rangeomorphs) and better preserved than on Avalon Peninsula. [1]
Color key
| Notes Uncertain or tentative taxa are in small text; |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Aninoides [8] |
| Sessile frondose organism. | |
| Arborea [9] |
| Sessile frondose organism, A. spinosa was previously described as a species of Charniodiscus. A. arborea may be considered belonging to Charniodiscus. [9] | |
| Bradgatia [7] |
| Sessile frondose organism. | |
| Charnia [7] |
| Sessile frondose organism. | |
| Charniodiscus [7] |
| Sessile frondose organism. C. arboreus may be considered belonging to Arborea. [9] | |
| Fractofusus [7] |
| Sessile spindle-like frondose organism. | |
| Primocandelabrum [7] |
| Sessile frondose organism. | |
| Vinlandia [10] |
| Sessile frondose organism, previously reported as a species of Charnia. [7] | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Haootia [11] |
| Staurozoan cnidarian. | |
| Hiemalora [7] |
| Discoid organism, possibly holdfasts of petalonamids. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Aspidella [7] [3] |
| Enigmatic discoidal fossil. | |
| Hadrynichorde [7] |
| Sea Whip-like frondose organism. | |
| Palaeopascichnus [1] [12] |
| Palaeopascichnid organism. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Ivesheadia [7] |
| Poorly preserved organism. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Neonereites [12] |
| Burrows. | |