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Ingta Formation

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Thicknessup to 312 metres (1,020 ft)
PrimaryInterbedded Shale & Sandstone
OtherSubordinate limestone units
Ingta Formation
Stratigraphic range: Ediacaran–Lower Cambrian[1] (?)
TypeGeological formation
Thicknessup to 312 metres (1,020 ft)
Lithology
PrimaryInterbedded Shale & Sandstone
OtherSubordinate limestone units
Location
Country Canada

The Ingta Formation is a geological unit containing green sandstones and shales; it crops out in the Canadian Mackenzie Mountains.[2] Its age is poorly constrained, though it straddles the Precambrian/Cambrian boundary.[1] Below the boundary its ichnofauna comprises subhorizontal Planolites burrows; above it, Phycodes burrows immediately appear, with Nemakit-Daldyn SSFs appearing soon after.[1]

The formation is overlain by either the Backbone Ranges Formation and the Vampire Formation, depending on the locality. These two formations have a common base with the Ingta formation, and both continue onwards until the base of the Sekwi Formation. [3]

Depositional environment

Palaeontology

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