Duntulm Formation

Duntulm Formation
Stratigraphic range: Bathonian
Exposures of limestone of the Duntulm Formation on the foreshore near Duntulm, Skye
TypeFormation
Unit ofGreat Estuarine Group
UnderliesKilmaluag Formation
OverliesValtos Sandstone Formation
ThicknessUp to 55 m
Lithology
PrimaryOyster beds
OtherSandstone, Siltstone, Shale
Location
RegionScotland
CountryUnited Kingdom
Type section
Named forDuntulm

The Duntulm Formation is a sedimentary geologic formation deposited in the Inner Hebrides, Scotland. The formation was previously known as the 'Lower Ostrea Beds', and dates to the Bathonian stage of the Middle Jurassic. [1][2] The formation is noted for its highly fossiliferous oyster beds, which compose of the species Praeexogyra hebridica. [1] The sedimentary sequence also forms part of the Great Estuarine Group.

  1. ^ a b Andrews, Julian E.; Walton, William (1990). "Depositional environments within Middle Jurassic oyster-dominated lagoons: an integrated litho-, bio- and palynofacies study of the Duntulm Formation (Great Estuarine Group, Inner Hebrides)". Transactions of the Royal Society of Edinburgh: Earth Sciences. 81 (1): 1–22. doi:10.1017/s0263593300005095. ISSN 0263-5933.
  2. ^ Anderson, F.W (1948). "Algal beds in the great estuarine series of Skye". Proceedings of the Royal Physical Society of Edinburgh. 23: 'pp.123-141'.