Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”

In a recent article, Narbonne et al. (1991) documented that the stratigraphic range of the chondrophorine Kullingia delicata continues above the the uppermost Precambrian (Vendian) into the lowermost Cambrian (Placentian Series) of the Avalonian faunal province. The revised text published in the Jou...

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Published in:Journal of Paleontology
Main Authors: Landing, Ed, Narbonne, Guy M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1992
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022336000033837
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033837
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spelling crcambridgeupr:10.1017/s0022336000033837 2024-03-03T08:46:42+00:00 Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland” Landing, Ed Narbonne, Guy M. 1992 http://dx.doi.org/10.1017/s0022336000033837 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033837 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 66, issue 2, page 338-338 ISSN 0022-3360 1937-2337 Paleontology journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0022336000033837 2024-02-08T08:33:51Z In a recent article, Narbonne et al. (1991) documented that the stratigraphic range of the chondrophorine Kullingia delicata continues above the the uppermost Precambrian (Vendian) into the lowermost Cambrian (Placentian Series) of the Avalonian faunal province. The revised text published in the Journal of Paleontology includes several references to Scenella Billings, 1872, as a Cambrian chondrophorine. This classification is in error and unfortunately serves to reinforce several recent reports that conclude that Scenella is a chondrophorine rather than a helcionacean mollusk. Article in Journal/Newspaper Newfoundland Cambridge University Press Journal of Paleontology 66 2 338 338
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Paleontology
spellingShingle Paleontology
Landing, Ed
Narbonne, Guy M.
Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
topic_facet Paleontology
description In a recent article, Narbonne et al. (1991) documented that the stratigraphic range of the chondrophorine Kullingia delicata continues above the the uppermost Precambrian (Vendian) into the lowermost Cambrian (Placentian Series) of the Avalonian faunal province. The revised text published in the Journal of Paleontology includes several references to Scenella Billings, 1872, as a Cambrian chondrophorine. This classification is in error and unfortunately serves to reinforce several recent reports that conclude that Scenella is a chondrophorine rather than a helcionacean mollusk.
format Article in Journal/Newspaper
author Landing, Ed
Narbonne, Guy M.
author_facet Landing, Ed
Narbonne, Guy M.
author_sort Landing, Ed
title Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
title_short Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
title_full Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
title_fullStr Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
title_full_unstemmed Scenella and “a chondrophorine (medusoid hydrozoan) from the basal Cambrian (Placentian) of Newfoundland”
title_sort scenella and “a chondrophorine (medusoid hydrozoan) from the basal cambrian (placentian) of newfoundland”
publisher Cambridge University Press (CUP)
publishDate 1992
url http://dx.doi.org/10.1017/s0022336000033837
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000033837
genre Newfoundland
genre_facet Newfoundland
op_source Journal of Paleontology
volume 66, issue 2, page 338-338
ISSN 0022-3360 1937-2337
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0022336000033837
container_title Journal of Paleontology
container_volume 66
container_issue 2
container_start_page 338
op_container_end_page 338
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