Fermeuse Formation

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
Location
Region Newfoundland and Labrador
Country Canada

Occurrence of Fermeuse formation in southeast Newfoundland

The Fermeuse Formation is a fossil-bearing Ediacaran geologic formation in Newfoundland.

Palaeobiological community

1-2 centimetre-wide Aspidella discs (and some smaller mm-sized individuals) on a bedding surface of the Fermeuse Formation near Ferryland, Newfoundland

On Avalon Peninsula[1] there is low diversity, and includes rare trace fossils, [[Palaeopascichnus,[3] and Aspidella discs, sometimes in great concentrations.[4]

On Bonavista Peninsula there is higher diversity, including more fronds (rangeomorphs) and better preserved than on Avalon Peninsula.[1]

Depositional environment

On Bonavista Peninsula the depositional environment was a slope and outer shelf–below photic zone Turbidites probably were the dominant sediment transporters.[4]

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.[4]

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]

See also

References


This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.