New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils
Journal home page at https://njg.geologi.no/ . The Vestertana Group on the Digermul Peninsula, Finnmark, northern Norway, presents one of the few, potentially continuous Ediacaran– Cambrian sections in Scandinavia. Trace fossils provide the main age constraint, with the boundary traditionally placed...
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ftunivtroemsoe:oai:munin.uit.no:10037/18954 2023-05-15T16:13:36+02:00 New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils Högström, Anette Jensen, Sören Palacios, Teodoro Ebbestad, Jan Ove R. 2013 https://hdl.handle.net/10037/18954 eng eng Geological Society of Norway Norsk Geologisk Tidsskrift Högström A, Jensen S, Palacios T, Ebbestad JOR. New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils. Norsk Geologisk Tidsskrift. 2013;93:95-106 FRIDAID 1085035 0029-196X 1502-5322 https://hdl.handle.net/10037/18954 openAccess Copyright 2013 The Author(s) VDP::Mathematics and natural science: 400::Geosciences: 450::Stratigraphy and paleontology: 461 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Stratigrafi og paleontologi: 461 Journal article Tidsskriftartikkel Peer reviewed publishedVersion 2013 ftunivtroemsoe 2021-06-25T17:57:11Z Journal home page at https://njg.geologi.no/ . The Vestertana Group on the Digermul Peninsula, Finnmark, northern Norway, presents one of the few, potentially continuous Ediacaran– Cambrian sections in Scandinavia. Trace fossils provide the main age constraint, with the boundary traditionally placed at the base of the Breidvika Formation. Here, we provide trace-fossil evidence to show that this boundary is at least as low as the third cycle of the Manndraperelva Member, Stáhpogieddi Formation, where Treptichnus pedum is associated with trilobed trace fossils. Organic-walled microfossils from the same stratigraphic interval include Granomarginata prima and the first report from Scandinavia of Cochleatina . The second cycle of the Manndraperelva Member contains trace fossils, including treptichnids and ?Cochlichnus isp. tentatively interpreted as latest Ediacaran. Reports of palaeopascichnids suggest a late Ediacaran age for the first cycle. The age of lower parts of the Stáhpogieddi Formation is poorly constrained but discoidal Ediacara-type fossils, vendotaenids, and possible simple trace fossils, suggest that the middle part of the Innerelva Member is younger than c. 560 Ma. Article in Journal/Newspaper Finnmark Northern Norway Finnmark University of Tromsø: Munin Open Research Archive Norway Vestertana ENVELOPE(27.868,27.868,70.424,70.424) Stáhpogieddi ENVELOPE(28.018,28.018,70.543,70.543) Breidvika ENVELOPE(24.083,24.083,-70.250,-70.250) Innerelva ENVELOPE(15.115,15.115,67.457,67.457) |
institution |
Open Polar |
collection |
University of Tromsø: Munin Open Research Archive |
op_collection_id |
ftunivtroemsoe |
language |
English |
topic |
VDP::Mathematics and natural science: 400::Geosciences: 450::Stratigraphy and paleontology: 461 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Stratigrafi og paleontologi: 461 |
spellingShingle |
VDP::Mathematics and natural science: 400::Geosciences: 450::Stratigraphy and paleontology: 461 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Stratigrafi og paleontologi: 461 Högström, Anette Jensen, Sören Palacios, Teodoro Ebbestad, Jan Ove R. New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
topic_facet |
VDP::Mathematics and natural science: 400::Geosciences: 450::Stratigraphy and paleontology: 461 VDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Stratigrafi og paleontologi: 461 |
description |
Journal home page at https://njg.geologi.no/ . The Vestertana Group on the Digermul Peninsula, Finnmark, northern Norway, presents one of the few, potentially continuous Ediacaran– Cambrian sections in Scandinavia. Trace fossils provide the main age constraint, with the boundary traditionally placed at the base of the Breidvika Formation. Here, we provide trace-fossil evidence to show that this boundary is at least as low as the third cycle of the Manndraperelva Member, Stáhpogieddi Formation, where Treptichnus pedum is associated with trilobed trace fossils. Organic-walled microfossils from the same stratigraphic interval include Granomarginata prima and the first report from Scandinavia of Cochleatina . The second cycle of the Manndraperelva Member contains trace fossils, including treptichnids and ?Cochlichnus isp. tentatively interpreted as latest Ediacaran. Reports of palaeopascichnids suggest a late Ediacaran age for the first cycle. The age of lower parts of the Stáhpogieddi Formation is poorly constrained but discoidal Ediacara-type fossils, vendotaenids, and possible simple trace fossils, suggest that the middle part of the Innerelva Member is younger than c. 560 Ma. |
format |
Article in Journal/Newspaper |
author |
Högström, Anette Jensen, Sören Palacios, Teodoro Ebbestad, Jan Ove R. |
author_facet |
Högström, Anette Jensen, Sören Palacios, Teodoro Ebbestad, Jan Ove R. |
author_sort |
Högström, Anette |
title |
New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
title_short |
New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
title_full |
New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
title_fullStr |
New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
title_full_unstemmed |
New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils |
title_sort |
new information on the ediacaran-cambrian transition in the vestertana group, finnmark, northern norway, from trace fossils and organic-walled microfossils |
publisher |
Geological Society of Norway |
publishDate |
2013 |
url |
https://hdl.handle.net/10037/18954 |
long_lat |
ENVELOPE(27.868,27.868,70.424,70.424) ENVELOPE(28.018,28.018,70.543,70.543) ENVELOPE(24.083,24.083,-70.250,-70.250) ENVELOPE(15.115,15.115,67.457,67.457) |
geographic |
Norway Vestertana Stáhpogieddi Breidvika Innerelva |
geographic_facet |
Norway Vestertana Stáhpogieddi Breidvika Innerelva |
genre |
Finnmark Northern Norway Finnmark |
genre_facet |
Finnmark Northern Norway Finnmark |
op_relation |
Norsk Geologisk Tidsskrift Högström A, Jensen S, Palacios T, Ebbestad JOR. New information on the Ediacaran-Cambrian transition in the Vestertana Group, Finnmark, northern Norway, from trace fossils and organic-walled microfossils. Norsk Geologisk Tidsskrift. 2013;93:95-106 FRIDAID 1085035 0029-196X 1502-5322 https://hdl.handle.net/10037/18954 |
op_rights |
openAccess Copyright 2013 The Author(s) |
_version_ |
1765999383445241856 |