Fermeuse Formation
| Fermeuse Formation | |
|---|---|
| Stratigraphic range: Ediacaran | |
| File:Fermeuse Formation photo.jpg 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 |
| File:Fermeuse Formation map.svg Occurrence of Fermeuse formation in southeast Newfoundland | |
The Fermeuse Formation is a fossil-bearing Ediacaran geologic formation in Newfoundland.
Depositional environment
[edit | edit source]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]
Paleobiota
[edit | edit source]On Avalon Peninsula[1] there is low diversity, and includes rare trace fossils, 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; |
Petalonamae
[edit | edit source]| Genus | Species | Notes | Images |
|---|---|---|---|
| Arborea[8] |
|
Sessile frondose organism, A. spinosa was previously described as a species of Charniodiscus. A. arborea may be considered belonging to Charniodiscus.[8] | |
| Bradgatia[7] |
|
Sessile frondose organism. | |
| Charnia[7] |
|
Sessile frondose organism. | |
| Charniodiscus[7] |
|
Sessile frondose organism. C. arboreus may be considered belonging to Arborea.[8] | |
| Fractofusus[7] |
|
Sessile spindle-like frondose organism. | |
| Primocandelabrum[7] |
|
Sessile frondose organism. | |
| Vinlandia[9] |
|
Sessile frondose organism, previously reported as a species of Charnia.[7] |
Cnidaria
[edit | edit source]| Genus | Species | Notes | Images |
|---|---|---|---|
| Haootia[10] |
|
Staurozoan cnidarian. | |
| Hiemalora[7] |
|
Discoid organism, possibly holdfasts of petalonamids. |
incertae sedis
[edit | edit source]| Genus | Species | Notes | Images |
|---|---|---|---|
| Aspidella[7][3] |
|
Enigmatic discoidal fossil. | |
| Hadrynichorde[7] |
|
Sea Whip-like frondose organism. | |
| Palaeopascichnus[1][11] |
|
Palaeopascichnid organism. |
Ivesheadiomorphs
[edit | edit source]| Genus | Species | Notes | Images |
|---|---|---|---|
| Ivesheadia[7] |
|
Poorly preserved organism. |
Ichnogenera
[edit | edit source]| Genus | Species | Notes | Images |
|---|---|---|---|
| Neonereites[11] |
|
Burrows. |
See also
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References
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