Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas

Conodont faunas are described from the type sections of Lower Triassic stages in the Canadian Arctic. The collections come largely from ammonoid-bearing strata of the Strigatus (upper Griesbachian), Candidus (lower Dienerian), Romunduri and Tardus (lower and upper Smithian), and Subrobustus (upper S...

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Published in:Polar Research
Main Author: Orchard, Michael J.
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2008
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/2897
https://doi.org/10.3402/polar.v27i3.6187
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spelling ftjpolarres:oai:journals.openacademia.net:article/2897 2023-05-15T14:36:56+02:00 Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas Orchard, Michael J. 2008-12-01 application/pdf https://polarresearch.net/index.php/polar/article/view/2897 https://doi.org/10.3402/polar.v27i3.6187 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/2897/6524 https://polarresearch.net/index.php/polar/article/view/2897 doi:10.3402/polar.v27i3.6187 Copyright (c) 2018 Polar Research Polar Research; Vol. 27 No. 3 (2008): Special issue: The Boreal Triassic; 393-412 1751-8369 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2008 ftjpolarres https://doi.org/10.3402/polar.v27i3.6187 2021-11-11T19:13:21Z Conodont faunas are described from the type sections of Lower Triassic stages in the Canadian Arctic. The collections come largely from ammonoid-bearing strata of the Strigatus (upper Griesbachian), Candidus (lower Dienerian), Romunduri and Tardus (lower and upper Smithian), and Subrobustus (upper Spathian) zones. These demonstrate that diverse late Griesbachian conodont faunas included the first species of Borinella, Neospathodus and Scythogondolella, accompanied by several species of Neogondolella. Dienerian faunas are dominated by Neospathodus, but explosive radiation led to several Smithian Scythogondolella species and diverse cosmopolitan “neospathodid” species of Conservatella, Discretella and Neospathodus. Smithian Paullella (nomen novum) and Wapitiodus are recorded here for the first time in the Arctic collections, and emphasize the correlation with successions in the Western Canada Sedimentary Basin (WCSB) and in the western USA. Conodonts from the Romunduri Zone differ in the three regions: Conservatella, Discretella and Paullella are rare in the Arctic, are more common in WCSB and are most common in the USA; Scythogondolella species are common in the Arctic, less so in WCSB and are virtually absent in the USA. Conodonts from the Tardus Zone, both in the Arctic and elsewhere, contain cosmopolitan Borinella buurensis, Neospathodus waageni, Scythogondolella mosheri and Scythogondolella milleri. Spathian conodont faunas from the Subrobustus Zone are dominated by Neogondolella species, which also occur in the WCSB associated with Triassospathodus. These two genera have an inverse relationship: Triassospathodus dominates the USA successions, and is virtually absent in the Arctic. Scythogondolella ellesmerensis sp. nov. and Scythogondolella lachrymiformis sp. nov. are described. Article in Journal/Newspaper Arctic Polar Research Polar Research (E-Journal) Arctic Canada Polar Research 27 3
institution Open Polar
collection Polar Research (E-Journal)
op_collection_id ftjpolarres
language English
description Conodont faunas are described from the type sections of Lower Triassic stages in the Canadian Arctic. The collections come largely from ammonoid-bearing strata of the Strigatus (upper Griesbachian), Candidus (lower Dienerian), Romunduri and Tardus (lower and upper Smithian), and Subrobustus (upper Spathian) zones. These demonstrate that diverse late Griesbachian conodont faunas included the first species of Borinella, Neospathodus and Scythogondolella, accompanied by several species of Neogondolella. Dienerian faunas are dominated by Neospathodus, but explosive radiation led to several Smithian Scythogondolella species and diverse cosmopolitan “neospathodid” species of Conservatella, Discretella and Neospathodus. Smithian Paullella (nomen novum) and Wapitiodus are recorded here for the first time in the Arctic collections, and emphasize the correlation with successions in the Western Canada Sedimentary Basin (WCSB) and in the western USA. Conodonts from the Romunduri Zone differ in the three regions: Conservatella, Discretella and Paullella are rare in the Arctic, are more common in WCSB and are most common in the USA; Scythogondolella species are common in the Arctic, less so in WCSB and are virtually absent in the USA. Conodonts from the Tardus Zone, both in the Arctic and elsewhere, contain cosmopolitan Borinella buurensis, Neospathodus waageni, Scythogondolella mosheri and Scythogondolella milleri. Spathian conodont faunas from the Subrobustus Zone are dominated by Neogondolella species, which also occur in the WCSB associated with Triassospathodus. These two genera have an inverse relationship: Triassospathodus dominates the USA successions, and is virtually absent in the Arctic. Scythogondolella ellesmerensis sp. nov. and Scythogondolella lachrymiformis sp. nov. are described.
format Article in Journal/Newspaper
author Orchard, Michael J.
spellingShingle Orchard, Michael J.
Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
author_facet Orchard, Michael J.
author_sort Orchard, Michael J.
title Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
title_short Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
title_full Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
title_fullStr Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
title_full_unstemmed Lower Triassic conodonts from the Canadian Arctic, their intercalibration with ammonoid-based stages and a comparison with other North American Olenekian faunas
title_sort lower triassic conodonts from the canadian arctic, their intercalibration with ammonoid-based stages and a comparison with other north american olenekian faunas
publisher Norwegian Polar Institute
publishDate 2008
url https://polarresearch.net/index.php/polar/article/view/2897
https://doi.org/10.3402/polar.v27i3.6187
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Polar Research
genre_facet Arctic
Polar Research
op_source Polar Research; Vol. 27 No. 3 (2008): Special issue: The Boreal Triassic; 393-412
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/2897/6524
https://polarresearch.net/index.php/polar/article/view/2897
doi:10.3402/polar.v27i3.6187
op_rights Copyright (c) 2018 Polar Research
op_doi https://doi.org/10.3402/polar.v27i3.6187
container_title Polar Research
container_volume 27
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