Vampire Formation | |
---|---|
Stratigraphic range: | |
Type | Geological formation |
Underlies | Sekwi Formation |
Overlies | Ingta Formation |
Thickness | up to |
Location | |
Location | Mackenzie Mountains |
Region | ![]() |
Country | ![]() |
The Vampire Formation is a formation of delta-front siliciclastics deposited in the early Cambrian. The upper unit is trilobitic Cambrian. [1] Some authors place the underlying Ingta formation at least partially in the Cambrian; in places it overlies the sub-Cambrian unconformity. [2]
It contains a rich array of trace fossils spanning the pre-trilobitic Cambrian, [3] including some found only there (once interpreted as sponge-like forms); [4] its uppermost strata contain Fallotaspis-zone trilobites, whereas its lower levels come above Protohertzina and Anabarites-bearing shelly layers in the Ingta formation; as such, it spans much of the Fortunian. [5]