Vardebukta Formation
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| Vardebukta Formation | |
|---|---|
| Stratigraphic range: Induan ~ | |
| Type | Formation |
| Lithology | |
| Primary | Conglomerate |
| Other | Sandstone, lime mudstone, packstone |
| Location | |
| Coordinates | 77°00′N 16°12′E / 77°N 16.2°E |
| Approximate paleocoordinates | 41°00′N 9°24′E / 41.0°N 9.4°E |
| Region | Svalbard |
| Country | Norway |
  Vardebukta Formation (Svalbard) | |
The Vardebukta Formation is a geologic formation in Norway. It preserves fossils dating back to the Induan stage (early Early Triassic).[1] Outcrops are known from the Hornsund area but also from Bellsund and Isfjorden areas.[2]
Urnetoppen Member
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 Urnetoppen Member, which is approximately 30 meter thick in the Hornsund area, consists of greenish shales, siltstone and fine-grained sandstone, occasionally with clay-ironstone nodules. In the Hornsund area, it rests paraconformably on the Permian Kapp Starostin Formation. The Urnetoppen Member is correlated with the Deltadalen Member of the Vikinghøgda Formation, which is of Dienerian (late Induan) age.[2][4]
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]
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