New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age.
Accepted manuscript version. Published version available at https://doi.org/10.1139/cjes-2018-0035 . Copyright NRC Research Press. We report on new occurrences of the late Ediacaran problematicum Palaeopascichnus (Protista?) from the Stáhpogieddi Formation, Arctic Norway. The stratigraphically lowes...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
NRC Research Press
2018
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/14748 https://doi.org/10.1139/cjes-2018-0035 |
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author | Jensen, Sören Högström, Anette Høyberget, Magne Meinhold, Guido McIlroy, Duncan Ebbestad, Jan Ove R. Taylor, Wendy L. Agic, Heda Palacios, Teodoro |
author_facet | Jensen, Sören Högström, Anette Høyberget, Magne Meinhold, Guido McIlroy, Duncan Ebbestad, Jan Ove R. Taylor, Wendy L. Agic, Heda Palacios, Teodoro |
author_sort | Jensen, Sören |
collection | University of Tromsø: Munin Open Research Archive |
container_issue | 11 |
container_start_page | 1253 |
container_title | Canadian Journal of Earth Sciences |
container_volume | 55 |
description | Accepted manuscript version. Published version available at https://doi.org/10.1139/cjes-2018-0035 . Copyright NRC Research Press. 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. |
format | Article in Journal/Newspaper |
genre | Arctic Newfoundland Varanger |
genre_facet | Arctic Newfoundland Varanger |
geographic | Arctic Norway Digermulen Mortensnes Stáhpogieddi Indreelva Lillevannet |
geographic_facet | Arctic Norway Digermulen Mortensnes Stáhpogieddi Indreelva Lillevannet |
id | ftunivtroemsoe:oai:munin.uit.no:10037/14748 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(11.560,11.560,64.731,64.731) ENVELOPE(20.269,20.269,69.581,69.581) ENVELOPE(28.018,28.018,70.543,70.543) ENVELOPE(19.187,19.187,69.957,69.957) ENVELOPE(19.683,19.683,70.215,70.215) |
op_collection_id | ftunivtroemsoe |
op_container_end_page | 1261 |
op_doi | https://doi.org/10.1139/cjes-2018-0035 |
op_relation | Canadian journal of earth sciences (Print) info:eu-repo/grantAgreement/RCN/FRINATEK/231103/Norway/The Digermul Peninsula - a window into the early diversification of animal life// FRIDAID 1581517 https://hdl.handle.net/10037/14748 |
op_rights | openAccess |
publishDate | 2018 |
publisher | NRC Research Press |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/14748 2025-04-13T14:14:02+00:00 New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. Jensen, Sören Högström, Anette Høyberget, Magne Meinhold, Guido McIlroy, Duncan Ebbestad, Jan Ove R. Taylor, Wendy L. Agic, Heda Palacios, Teodoro 2018-09-18 https://hdl.handle.net/10037/14748 https://doi.org/10.1139/cjes-2018-0035 eng eng NRC Research Press Canadian journal of earth sciences (Print) info:eu-repo/grantAgreement/RCN/FRINATEK/231103/Norway/The Digermul Peninsula - a window into the early diversification of animal life// FRIDAID 1581517 https://hdl.handle.net/10037/14748 openAccess VDP::Mathematics and natural science: 400::Zoology and botany: 480 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495 Journal article Tidsskriftartikkel Peer reviewed 2018 ftunivtroemsoe https://doi.org/10.1139/cjes-2018-0035 2025-03-14T05:17:55Z Accepted manuscript version. Published version available at https://doi.org/10.1139/cjes-2018-0035 . Copyright NRC Research Press. 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. Article in Journal/Newspaper Arctic Newfoundland Varanger University of Tromsø: Munin Open Research Archive Arctic Norway Digermulen ENVELOPE(11.560,11.560,64.731,64.731) Mortensnes ENVELOPE(20.269,20.269,69.581,69.581) Stáhpogieddi ENVELOPE(28.018,28.018,70.543,70.543) Indreelva ENVELOPE(19.187,19.187,69.957,69.957) Lillevannet ENVELOPE(19.683,19.683,70.215,70.215) Canadian Journal of Earth Sciences 55 11 1253 1261 |
spellingShingle | VDP::Mathematics and natural science: 400::Zoology and botany: 480 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495 Jensen, Sören Högström, Anette Høyberget, Magne Meinhold, Guido McIlroy, Duncan Ebbestad, Jan Ove R. Taylor, Wendy L. Agic, Heda Palacios, Teodoro New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title | New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title_full | New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title_fullStr | New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title_full_unstemmed | New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title_short | New occurrences of Palaeopascichnus from the Stáhpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age. |
title_sort | new occurrences of palaeopascichnus from the stáhpogieddi formation, arctic norway, and their bearing on the age of the varanger ice age. |
topic | VDP::Mathematics and natural science: 400::Zoology and botany: 480 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495 |
topic_facet | VDP::Mathematics and natural science: 400::Zoology and botany: 480 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480 VDP::Mathematics and natural science: 400::Zoology and botany: 480::Vegetation history: 495 VDP::Matematikk og Naturvitenskap: 400::Zoologiske og botaniske fag: 480::Vegetasjonshistorie: 495 |
url | https://hdl.handle.net/10037/14748 https://doi.org/10.1139/cjes-2018-0035 |