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Jensen et al., 2018b

New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age

Jensen, S., Högström, A. E., Høyberget, M., Meinhold, G., McIlroy, D., Ebbestad, J. O. R., Taylor, W. L., Agić, H., Palacios, T.
DOI
DOI10.1139/cjes-2018-0035
Aasta2018
AjakiriCanadian Journal of Earth Sciences
Köide55
Number11
Leheküljed1253-1261
Tüüpartikkel ajakirjas
Keelinglise
Id48946

Abstrakt

We report on new occurrences of the late Ediacaran problematicum Palaeopascichnus (Protista?) from the Stáhpogieddi Formation, Arctic Norway. The stratigraphically lowest occurrences are in beds transitional between the Lillevannet and Indreelva members: the highest in the second cycle of the Manndrapselva Member, stratigraphically close to the lowest occurrences of Cambrian-type trace fossils. This establishes a long stratigraphical range of Palaeopascichnus on the Digermulen Peninsula, as has been previously documented from Newfoundland, South Australia, and elsewhere in Baltica. The age range of Palaeopascichnus in Avalonia and Baltica is from ~565 to 541 Ma. Since the transition from the Mortensnes Formation to the Stáhpogieddi Formation is without a major break in sedimentation, this supports the inference that the underlying glacigenic Mortensnes Formation is ca. 580 Ma, and therefore Gaskiers-equivalent, or younger.

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