Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec

Successive Tremadocian planktic dendroid graptolite assemblages from continental slope sequences in Quebec can be correlated with North American platform biozonations on the basis of conodonts. Anisograptid-bearing (Assemblage 2), middle Tremadocian "Matane faunas" are associated with Earl...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Landing, Ed, Barnes, Christopher R., Stevens, Robert K.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1986
Subjects:
Online Access:http://dx.doi.org/10.1139/e86-180
http://www.nrcresearchpress.com/doi/pdf/10.1139/e86-180
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spelling crcansciencepubl:10.1139/e86-180 2024-09-15T18:20:12+00:00 Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec Landing, Ed Barnes, Christopher R. Stevens, Robert K. 1986 http://dx.doi.org/10.1139/e86-180 http://www.nrcresearchpress.com/doi/pdf/10.1139/e86-180 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 23, issue 12, page 1928-1949 ISSN 0008-4077 1480-3313 journal-article 1986 crcansciencepubl https://doi.org/10.1139/e86-180 2024-07-25T04:10:07Z Successive Tremadocian planktic dendroid graptolite assemblages from continental slope sequences in Quebec can be correlated with North American platform biozonations on the basis of conodonts. Anisograptid-bearing (Assemblage 2), middle Tremadocian "Matane faunas" are associated with Early Ordovician Rossodus manitouensis Zone (new designation) conodonts. Younger middle Tremadocian faunas with adelograptids (Assemblage 3) are no younger than the Rossodus manitouensis Zone. Key dendroid evolutionary–immigration events take place within the lower conodont Fauna B interval. Rooted dendroids near Cap des Rosiers, Quebec, and in eastern New York State occur with lower Fauna B conodonts and the trilobites Pareuloma and Borthaspidella. However, the earliest Tremadocian (and earliest Ordovician) dendroid immigration event, represented by the local lowest occurrence of faunas with Dictyonema flabelliforme s.l. at localities in western Newfoundland, eastern New York State, Norway, and eastern China, also lies within the lower Fauna B interval. Finally, the lowest occurrence of key Assemblage 2 dendroid taxa falls within the lower Fauna B interval at the latter localities.The Rossodus manitouensis Zone is proposed as a new designation for a biostratigraphic unit that is appropriate for North American marginal and open shelf sequences. This zone is approximately equivalent to the "Loxodus bransoni Interval" of other authors and is characterized by Fauna C conodonts. Newly described taxa include Rossodus? highgatensis n. sp., Scolopodus? praecornuformis n. sp., and Variabiloconus n. gen. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 23 12 1928 1949
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description Successive Tremadocian planktic dendroid graptolite assemblages from continental slope sequences in Quebec can be correlated with North American platform biozonations on the basis of conodonts. Anisograptid-bearing (Assemblage 2), middle Tremadocian "Matane faunas" are associated with Early Ordovician Rossodus manitouensis Zone (new designation) conodonts. Younger middle Tremadocian faunas with adelograptids (Assemblage 3) are no younger than the Rossodus manitouensis Zone. Key dendroid evolutionary–immigration events take place within the lower conodont Fauna B interval. Rooted dendroids near Cap des Rosiers, Quebec, and in eastern New York State occur with lower Fauna B conodonts and the trilobites Pareuloma and Borthaspidella. However, the earliest Tremadocian (and earliest Ordovician) dendroid immigration event, represented by the local lowest occurrence of faunas with Dictyonema flabelliforme s.l. at localities in western Newfoundland, eastern New York State, Norway, and eastern China, also lies within the lower Fauna B interval. Finally, the lowest occurrence of key Assemblage 2 dendroid taxa falls within the lower Fauna B interval at the latter localities.The Rossodus manitouensis Zone is proposed as a new designation for a biostratigraphic unit that is appropriate for North American marginal and open shelf sequences. This zone is approximately equivalent to the "Loxodus bransoni Interval" of other authors and is characterized by Fauna C conodonts. Newly described taxa include Rossodus? highgatensis n. sp., Scolopodus? praecornuformis n. sp., and Variabiloconus n. gen.
format Article in Journal/Newspaper
author Landing, Ed
Barnes, Christopher R.
Stevens, Robert K.
spellingShingle Landing, Ed
Barnes, Christopher R.
Stevens, Robert K.
Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
author_facet Landing, Ed
Barnes, Christopher R.
Stevens, Robert K.
author_sort Landing, Ed
title Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
title_short Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
title_full Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
title_fullStr Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
title_full_unstemmed Tempo of earliest Ordovician graptolite faunal succession: conodont-based correlations from the Tremadocian of Quebec
title_sort tempo of earliest ordovician graptolite faunal succession: conodont-based correlations from the tremadocian of quebec
publisher Canadian Science Publishing
publishDate 1986
url http://dx.doi.org/10.1139/e86-180
http://www.nrcresearchpress.com/doi/pdf/10.1139/e86-180
genre Newfoundland
genre_facet Newfoundland
op_source Canadian Journal of Earth Sciences
volume 23, issue 12, page 1928-1949
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e86-180
container_title Canadian Journal of Earth Sciences
container_volume 23
container_issue 12
container_start_page 1928
op_container_end_page 1949
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