New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada
Brachiopods are common in the lower part of the late Early to Middle Devonian Bird Fiord Formation that is a carbonate-clastic transition succession found in Arctic Canada. These brachiopods, which lived in a shallow, near-shore, marine environment, includes three new genera: Borealistrophia, Arctic...
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Online Access: | http://dx.doi.org/10.1017/s0022336000041925 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000041925 |
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crcambridgeupr:10.1017/s0022336000041925 2024-03-03T08:41:43+00:00 New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada Rong-Yu, Li Jones, Brian 2002 http://dx.doi.org/10.1017/s0022336000041925 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000041925 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 76, issue 4, page 648-658 ISSN 0022-3360 1937-2337 Paleontology journal-article 2002 crcambridgeupr https://doi.org/10.1017/s0022336000041925 2024-02-08T08:38:26Z Brachiopods are common in the lower part of the late Early to Middle Devonian Bird Fiord Formation that is a carbonate-clastic transition succession found in Arctic Canada. These brachiopods, which lived in a shallow, near-shore, marine environment, includes three new genera: Borealistrophia, Arcticastrophia, and Grinnellathyis. The strophomenid Borealistrophia, which is characterized by two pairs of straight side septa, prominent and thick socket ridges, a thick but short median septum, and a cordate ventral muscle field, is found in the Baad Fiord, Blubber Point, and Norwegian members on Bathurst, Devon, North Kent, and Ellesmere islands. The strophomenid Arcticastrophia, which is distinctive because of its stout transmuscle septa, its narrow and low medium septum, and elevated ventral muscle field, is found in the Baad Fiord Member on Bathurst and Devon islands. The athyridid Grinnellathyris, which is characterized by an imperforated cardinal plate and inverted U-shaped jugum, is found in the Baad Fiord Member on Bathurst, North Kent, and Devon islands. The similarities between Grinnellathyris and Johnsonathyris Savage, Eberlein, and Churkin, 1978, in terms of their shell size and internal structures, may indicate that the latter evolved from the former. Article in Journal/Newspaper Arctic Cambridge University Press Arctic Canada Bird Fiord ENVELOPE(-87.000,-87.000,77.168,77.168) Baad Fiord ENVELOPE(-86.500,-86.500,76.468,76.468) Blubber Point ENVELOPE(-89.600,-89.600,76.618,76.618) Journal of Paleontology 76 4 648 658 |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
Paleontology |
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Paleontology Rong-Yu, Li Jones, Brian New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
topic_facet |
Paleontology |
description |
Brachiopods are common in the lower part of the late Early to Middle Devonian Bird Fiord Formation that is a carbonate-clastic transition succession found in Arctic Canada. These brachiopods, which lived in a shallow, near-shore, marine environment, includes three new genera: Borealistrophia, Arcticastrophia, and Grinnellathyis. The strophomenid Borealistrophia, which is characterized by two pairs of straight side septa, prominent and thick socket ridges, a thick but short median septum, and a cordate ventral muscle field, is found in the Baad Fiord, Blubber Point, and Norwegian members on Bathurst, Devon, North Kent, and Ellesmere islands. The strophomenid Arcticastrophia, which is distinctive because of its stout transmuscle septa, its narrow and low medium septum, and elevated ventral muscle field, is found in the Baad Fiord Member on Bathurst and Devon islands. The athyridid Grinnellathyris, which is characterized by an imperforated cardinal plate and inverted U-shaped jugum, is found in the Baad Fiord Member on Bathurst, North Kent, and Devon islands. The similarities between Grinnellathyris and Johnsonathyris Savage, Eberlein, and Churkin, 1978, in terms of their shell size and internal structures, may indicate that the latter evolved from the former. |
format |
Article in Journal/Newspaper |
author |
Rong-Yu, Li Jones, Brian |
author_facet |
Rong-Yu, Li Jones, Brian |
author_sort |
Rong-Yu, Li |
title |
New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
title_short |
New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
title_full |
New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
title_fullStr |
New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
title_full_unstemmed |
New brachiopod genera from Bird Fiord Formation (Devonian), arctic Canada |
title_sort |
new brachiopod genera from bird fiord formation (devonian), arctic canada |
publisher |
Cambridge University Press (CUP) |
publishDate |
2002 |
url |
http://dx.doi.org/10.1017/s0022336000041925 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000041925 |
long_lat |
ENVELOPE(-87.000,-87.000,77.168,77.168) ENVELOPE(-86.500,-86.500,76.468,76.468) ENVELOPE(-89.600,-89.600,76.618,76.618) |
geographic |
Arctic Canada Bird Fiord Baad Fiord Blubber Point |
geographic_facet |
Arctic Canada Bird Fiord Baad Fiord Blubber Point |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
Journal of Paleontology volume 76, issue 4, page 648-658 ISSN 0022-3360 1937-2337 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0022336000041925 |
container_title |
Journal of Paleontology |
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76 |
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4 |
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648 |
op_container_end_page |
658 |
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1792497341920444416 |