Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen

Seven samplcs from the Limcstonc and Boulder Conglomerate Members of the Bulltinden Formation have yicldcd poorly prcscrvcd conodonts. On tentative identifications Periodon aculeatus Hadding and Prioniodus cf. P. alobatus Bergstrom at the basc of thc formation suggest an Ordovician lower Caradoc, or...

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Published in:Polar Research
Main Authors: Armstrong, Howard A., Nakrem, Hans A., Ohta, Yoshihide
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 1986
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2487
https://doi.org/10.3402/polar.v4i1.6915
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spelling ftjpolarres:oai:journals.openacademia.net:article/2487 2023-05-15T17:31:28+02:00 Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen Armstrong, Howard A. Nakrem, Hans A. Ohta, Yoshihide 1986-01-05 application/pdf https://polarresearch.net/index.php/polar/article/view/2487 https://doi.org/10.3402/polar.v4i1.6915 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2487/5738 https://polarresearch.net/index.php/polar/article/view/2487 doi:10.3402/polar.v4i1.6915 Copyright (c) 2018 Polar Research Polar Research; Vol. 4 No. 1 (1986); 17-23 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1986 ftjpolarres https://doi.org/10.3402/polar.v4i1.6915 2021-11-11T19:12:43Z Seven samplcs from the Limcstonc and Boulder Conglomerate Members of the Bulltinden Formation have yicldcd poorly prcscrvcd conodonts. On tentative identifications Periodon aculeatus Hadding and Prioniodus cf. P. alobatus Bergstrom at the basc of thc formation suggest an Ordovician lower Caradoc, or older agc. This confirms that the Vcstgotabrccn Formation unconformably beneath underwent highpressure metamorphism during the Taconic and/or Finmarkian phases of the Caledonian orogeny. The conodonts show affinity to the North Atlantic Province suggesting a deeper water marine depositional cnvironmcnt. Conodont colour alteration indiccs of five indicate that the Bulltinden Formation was heated to tcmpcraturcs in cxcess of 3°K. probably during thc middle-upper Silurian main Caledonian uplift cvcnt. Article in Journal/Newspaper North Atlantic Polar Research Spitsbergen Polar Research (E-Journal) Bulltinden ENVELOPE(12.583,12.583,78.483,78.483) Motalafjella ENVELOPE(12.967,12.967,78.450,78.450) Polar Research 4 1 17 23
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description Seven samplcs from the Limcstonc and Boulder Conglomerate Members of the Bulltinden Formation have yicldcd poorly prcscrvcd conodonts. On tentative identifications Periodon aculeatus Hadding and Prioniodus cf. P. alobatus Bergstrom at the basc of thc formation suggest an Ordovician lower Caradoc, or older agc. This confirms that the Vcstgotabrccn Formation unconformably beneath underwent highpressure metamorphism during the Taconic and/or Finmarkian phases of the Caledonian orogeny. The conodonts show affinity to the North Atlantic Province suggesting a deeper water marine depositional cnvironmcnt. Conodont colour alteration indiccs of five indicate that the Bulltinden Formation was heated to tcmpcraturcs in cxcess of 3°K. probably during thc middle-upper Silurian main Caledonian uplift cvcnt.
format Article in Journal/Newspaper
author Armstrong, Howard A.
Nakrem, Hans A.
Ohta, Yoshihide
spellingShingle Armstrong, Howard A.
Nakrem, Hans A.
Ohta, Yoshihide
Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
author_facet Armstrong, Howard A.
Nakrem, Hans A.
Ohta, Yoshihide
author_sort Armstrong, Howard A.
title Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
title_short Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
title_full Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
title_fullStr Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
title_full_unstemmed Ordovician conodonts from the Bulltinden Formation, Motalafjella, central-western Spitsbergen
title_sort ordovician conodonts from the bulltinden formation, motalafjella, central-western spitsbergen
publisher Norwegian Polar Institute
publishDate 1986
url https://polarresearch.net/index.php/polar/article/view/2487
https://doi.org/10.3402/polar.v4i1.6915
long_lat ENVELOPE(12.583,12.583,78.483,78.483)
ENVELOPE(12.967,12.967,78.450,78.450)
geographic Bulltinden
Motalafjella
geographic_facet Bulltinden
Motalafjella
genre North Atlantic
Polar Research
Spitsbergen
genre_facet North Atlantic
Polar Research
Spitsbergen
op_source Polar Research; Vol. 4 No. 1 (1986); 17-23
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2487/5738
https://polarresearch.net/index.php/polar/article/view/2487
doi:10.3402/polar.v4i1.6915
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v4i1.6915
container_title Polar Research
container_volume 4
container_issue 1
container_start_page 17
op_container_end_page 23
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