The Vardebukta Formation is divided into the Urnetoppen Member and the overlying Wibebreen Member. Both members are of marine origin. They were deposited in a sublittoral to shallow-neritic environment.[2] The Vardebukta Formation represents the oldest Mesozoic formation in Svalbard.[3]
The top of the Urnetoppen Member contains the so-called Brevassfjellet Myalina beds, a 5–6 meter thick, fossiliferous conglomerate.
Wibebreen Member
The Wibebreen Member is ca. 90–100 meter thick in the Hornsund area. It consists of black to light-grey coloured shales, marly shales, arenaceous marls and siltstone. The lower part of this member contains mainly siltsone layers. The locally developed Skilisen Retzia Limestone belongs to the uppermost part of the Wibebreen Member. The Wibebreen Member is overlain by the Smithian (early Olenekian) aged Lusitaniadalen Member (="Sticky Keep Member") of the Vikinghøgda Formation.[2]
The isolated fish teeth of bony and cartilaginous fishes have been described from the Brevassfjellet Myalina Bed (upper Urnetoppen Member of the Vardebukta Formation) of Hyrnefjellet, Hornsund.[2][3][6] The bony fish teeth are mostly tentatively referred to Saurichthys sp.[7]
^ abcdefghijkBirkenmajer, Krzysztof; Jerzmańska, Anna (1979). "Lower Triassic shark and other fish teeth from Hornsund, South Spitsbergen". In K. Birkenmajer (ed.). Results of the Polish Spitsbergen Expeditions, Part 10. Studia Geologica Polonica 60. pp. 7–38.
^Stensiö, Erik (1918). "Notes on some fish remains collected at Hornsund by the Norwegian Spitzbergen expedition in 1917". Norsk Geologisk Tidsskrift. 5 (1): 75–78..