Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary

The type species of Parastrophinella, P. reversa, a pentamerid brachiopod from the uppermost Ordovician (Hirnantian) Ellis Bay Formation of Anticosti Island, Quebec, shows that the genus is characterized by three features: 1) a ventral median septum apically buried in a thickened valve floor, but an...

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Published in:Journal of Paleontology
Main Authors: Jin, Jisuo, Copper, Paul
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1997
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022336000039391
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039391
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spelling crcambridgeupr:10.1017/s0022336000039391 2024-09-15T17:57:05+00:00 Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary Jin, Jisuo Copper, Paul 1997 http://dx.doi.org/10.1017/s0022336000039391 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039391 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Paleontology volume 71, issue 3, page 369-380 ISSN 0022-3360 1937-2337 journal-article 1997 crcambridgeupr https://doi.org/10.1017/s0022336000039391 2024-07-10T04:04:08Z The type species of Parastrophinella, P. reversa, a pentamerid brachiopod from the uppermost Ordovician (Hirnantian) Ellis Bay Formation of Anticosti Island, Quebec, shows that the genus is characterized by three features: 1) a ventral median septum apically buried in a thickened valve floor, but anteriorly rising above valve floor; 2) prominent alate plates, which are homologous to brachial processes; and, 3) a pseudocruralium consisting of a dorsal median septum, which is largely buried in the valve floor posteriorly, and outer plates that are connected to the median septum via prismatic substance (with poorly developed lamellar layer at the junctions) at, or slightly above, the valve floor. These constitute criteria by which many species previously assigned to Parastrophinella are excluded from the genus. Late Ordovician species that fit the redefinition of Parastrophinella are now confined to eastern North America. The genus crosses the Ordovician/Silurian boundary without major morphologic change, and Early Silurian species of Parastrophinella occur in both eastern North America and Great Britain. In the Late Ordovician, the pentamerid fauna of North America (Laurentia) contrasted sharply with that of Baltica and Kazakhstan, where the Holorhynchus fauna was dominant. Typical elements of the Holorhynchus fauna, such as the large-shelled Holorhynchus and Proconchidium, are known only in the northern parts of Laurentia (Baffin Island, Greenland, and Kolyma), and are absent in the Hudson Bay and Williston basins and southwards. Article in Journal/Newspaper Baffin Island Baffin Greenland Hudson Bay Cambridge University Press Journal of Paleontology 71 3 369 380
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description The type species of Parastrophinella, P. reversa, a pentamerid brachiopod from the uppermost Ordovician (Hirnantian) Ellis Bay Formation of Anticosti Island, Quebec, shows that the genus is characterized by three features: 1) a ventral median septum apically buried in a thickened valve floor, but anteriorly rising above valve floor; 2) prominent alate plates, which are homologous to brachial processes; and, 3) a pseudocruralium consisting of a dorsal median septum, which is largely buried in the valve floor posteriorly, and outer plates that are connected to the median septum via prismatic substance (with poorly developed lamellar layer at the junctions) at, or slightly above, the valve floor. These constitute criteria by which many species previously assigned to Parastrophinella are excluded from the genus. Late Ordovician species that fit the redefinition of Parastrophinella are now confined to eastern North America. The genus crosses the Ordovician/Silurian boundary without major morphologic change, and Early Silurian species of Parastrophinella occur in both eastern North America and Great Britain. In the Late Ordovician, the pentamerid fauna of North America (Laurentia) contrasted sharply with that of Baltica and Kazakhstan, where the Holorhynchus fauna was dominant. Typical elements of the Holorhynchus fauna, such as the large-shelled Holorhynchus and Proconchidium, are known only in the northern parts of Laurentia (Baffin Island, Greenland, and Kolyma), and are absent in the Hudson Bay and Williston basins and southwards.
format Article in Journal/Newspaper
author Jin, Jisuo
Copper, Paul
spellingShingle Jin, Jisuo
Copper, Paul
Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
author_facet Jin, Jisuo
Copper, Paul
author_sort Jin, Jisuo
title Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
title_short Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
title_full Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
title_fullStr Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
title_full_unstemmed Parastrophinella (Brachiopoda): Its paleogeographic significance at the Ordovician/Silurian boundary
title_sort parastrophinella (brachiopoda): its paleogeographic significance at the ordovician/silurian boundary
publisher Cambridge University Press (CUP)
publishDate 1997
url http://dx.doi.org/10.1017/s0022336000039391
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022336000039391
genre Baffin Island
Baffin
Greenland
Hudson Bay
genre_facet Baffin Island
Baffin
Greenland
Hudson Bay
op_source Journal of Paleontology
volume 71, issue 3, page 369-380
ISSN 0022-3360 1937-2337
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0022336000039391
container_title Journal of Paleontology
container_volume 71
container_issue 3
container_start_page 369
op_container_end_page 380
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