Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland

The Cape Cormorant Formation of the Table Head Group exposed on the Port au Port Peninsula, western Newfoundland, is composed of dark-brown to black shales with interbeds of thin calcareous silty and sandy distal turbidites. Distinctive carbonate conglomerates and breccias derived from the founderin...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Albani, R., Bagnoli, G., Maletz, J., Stouge, S.
Format: Article in Journal/Newspaper
Language:English
Published: 2001
Subjects:
Online Access:https://curis.ku.dk/portal/da/publications/integrated-chitinozoan-conodont-and-graptolite-biostratigraphy-from-the-upper-part-of-the-cape-cormorant-formation-middle-ordovician-western-newfoundland(30ed0ba2-3410-441d-9542-5a3c982b47e6).html
https://doi.org/10.1139/e00-081
http://www.scopus.com/inward/record.url?scp=57249085628&partnerID=8YFLogxK
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spelling ftcopenhagenunip:oai:pure.atira.dk:publications/30ed0ba2-3410-441d-9542-5a3c982b47e6 2024-06-09T07:47:50+00:00 Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland Albani, R. Bagnoli, G. Maletz, J. Stouge, S. 2001 https://curis.ku.dk/portal/da/publications/integrated-chitinozoan-conodont-and-graptolite-biostratigraphy-from-the-upper-part-of-the-cape-cormorant-formation-middle-ordovician-western-newfoundland(30ed0ba2-3410-441d-9542-5a3c982b47e6).html https://doi.org/10.1139/e00-081 http://www.scopus.com/inward/record.url?scp=57249085628&partnerID=8YFLogxK eng eng info:eu-repo/semantics/restrictedAccess Albani , R , Bagnoli , G , Maletz , J & Stouge , S 2001 , ' Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland ' , Canadian Journal of Earth Sciences , vol. 38 , no. 3 , pp. 387-409 . https://doi.org/10.1139/e00-081 article 2001 ftcopenhagenunip https://doi.org/10.1139/e00-081 2024-05-16T11:29:30Z The Cape Cormorant Formation of the Table Head Group exposed on the Port au Port Peninsula, western Newfoundland, is composed of dark-brown to black shales with interbeds of thin calcareous silty and sandy distal turbidites. Distinctive carbonate conglomerates and breccias derived from the foundering shelf are occasionally found in the formation. The sediments accumulated in the foreland basin formed during the early stage of the Taconic orogeny. The faunas from the upper part of the Cape Cormorant Formation include graptolites, conodonts, and chitinozoans. The graptolites are well preserved, but are of low diversity and are referred to the Darriwil Pterograptus elegans Zone. Conodonts recorded from the distal turbidites are rare and fragmented. The faunas include taxa that are known from the St. George and Table Head groups. The conodont fauna is tentatively assigned to the Histiodella kristinae Phylozone and to the younger, unzoned interval. The chitinozoans are well preserved and the yield is high. The fauna is assigned to the Cyathochitina jenkinsi Zone and to an undefined interval. The abundance and diversity of the chitinozoan assemblages display a cyclic pattern, which is related to changes of the oceanic watermass in the foreland basin. The new chitinozoan species Belonechitina nevillensis n. sp., Belonechitina uniformipunctata n. sp., and Cyathochitina cormorani n. sp. are described. Article in Journal/Newspaper Newfoundland University of Copenhagen: Research Table Head ENVELOPE(-55.698,-55.698,52.083,52.083) Canadian Journal of Earth Sciences 38 3 387 409
institution Open Polar
collection University of Copenhagen: Research
op_collection_id ftcopenhagenunip
language English
description The Cape Cormorant Formation of the Table Head Group exposed on the Port au Port Peninsula, western Newfoundland, is composed of dark-brown to black shales with interbeds of thin calcareous silty and sandy distal turbidites. Distinctive carbonate conglomerates and breccias derived from the foundering shelf are occasionally found in the formation. The sediments accumulated in the foreland basin formed during the early stage of the Taconic orogeny. The faunas from the upper part of the Cape Cormorant Formation include graptolites, conodonts, and chitinozoans. The graptolites are well preserved, but are of low diversity and are referred to the Darriwil Pterograptus elegans Zone. Conodonts recorded from the distal turbidites are rare and fragmented. The faunas include taxa that are known from the St. George and Table Head groups. The conodont fauna is tentatively assigned to the Histiodella kristinae Phylozone and to the younger, unzoned interval. The chitinozoans are well preserved and the yield is high. The fauna is assigned to the Cyathochitina jenkinsi Zone and to an undefined interval. The abundance and diversity of the chitinozoan assemblages display a cyclic pattern, which is related to changes of the oceanic watermass in the foreland basin. The new chitinozoan species Belonechitina nevillensis n. sp., Belonechitina uniformipunctata n. sp., and Cyathochitina cormorani n. sp. are described.
format Article in Journal/Newspaper
author Albani, R.
Bagnoli, G.
Maletz, J.
Stouge, S.
spellingShingle Albani, R.
Bagnoli, G.
Maletz, J.
Stouge, S.
Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
author_facet Albani, R.
Bagnoli, G.
Maletz, J.
Stouge, S.
author_sort Albani, R.
title Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
title_short Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
title_full Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
title_fullStr Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
title_full_unstemmed Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland
title_sort integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the cape cormorant formation (middle ordovician), western newfoundland
publishDate 2001
url https://curis.ku.dk/portal/da/publications/integrated-chitinozoan-conodont-and-graptolite-biostratigraphy-from-the-upper-part-of-the-cape-cormorant-formation-middle-ordovician-western-newfoundland(30ed0ba2-3410-441d-9542-5a3c982b47e6).html
https://doi.org/10.1139/e00-081
http://www.scopus.com/inward/record.url?scp=57249085628&partnerID=8YFLogxK
long_lat ENVELOPE(-55.698,-55.698,52.083,52.083)
geographic Table Head
geographic_facet Table Head
genre Newfoundland
genre_facet Newfoundland
op_source Albani , R , Bagnoli , G , Maletz , J & Stouge , S 2001 , ' Integrated chitinozoan, conodont, and graptolite biostratigraphy from the upper part of the Cape Cormorant Formation (Middle Ordovician), western Newfoundland ' , Canadian Journal of Earth Sciences , vol. 38 , no. 3 , pp. 387-409 . https://doi.org/10.1139/e00-081
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op_doi https://doi.org/10.1139/e00-081
container_title Canadian Journal of Earth Sciences
container_volume 38
container_issue 3
container_start_page 387
op_container_end_page 409
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