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New occurrences of ...
New occurrences of Palaeopascichnus from the Stahpogieddi Formation, Arctic Norway, and their bearing on the age of the Varanger Ice Age
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- Jensen, Soren (author)
- Univ Extremadura, Area Paleontol, E-06006 Badajoz, Spain
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- Hogstrom, Anette E. S. (author)
- UiT Arctic Univ Norway, Tromso Univ Museum, N-9037 Tromso, Norway
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- Hoyberget, Magne (author)
- Rennesveien 14, N-4513 Mandal, Norway
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- Meinhold, Guido (author)
- Univ Gottingen, Geosci Ctr, Goldschmidtstr 3, D-37077 Gottingen, Germany;Keele Univ, Sch Geog Geol & Environm, Keele ST5 5BG, Staffs, England
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- McIlroy, Duncan (author)
- Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada
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- Ebbestad, Jan Ove R., 1967- (author)
- Uppsala universitet,Evolutionsmuseet
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- Taylor, Wendy L. (author)
- Univ Cape Town, Dept Geol Sci, ZA-7701 Cape Town, South Africa
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- Agic, Heda (author)
- Univ Calif Santa Barbara, Dept Earth Sci, 1006 Webb Hall, Santa Barbara, CA 93106 USA
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- Palacios, Teodoro (author)
- Univ Extremadura, Area Paleontol, E-06006 Badajoz, Spain
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(creator_code:org_t)
- CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS, 2018
- 2018
- English.
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In: Canadian journal of earth sciences (Print). - : CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS. - 0008-4077 .- 1480-3313. ; 55:11, s. 1253-1261
- Related links:
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http://eprints.keele...
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https://urn.kb.se/re...
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https://doi.org/10.1...
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Abstract
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- We report on new occurrences of the late Ediacaran problematicum Palaeopascichnus (Protista?) from the Stahpogieddi 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 similar to 565 to 541 Ma. Since the transition from the Mortensnes Formation to the Stahpogieddi 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.
Subject headings
- NATURVETENSKAP -- Geovetenskap och miljövetenskap -- Annan geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences -- Other Earth and Related Environmental Sciences (hsv//eng)
Publication and Content Type
- ref (subject category)
- art (subject category)
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