Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance

Two previously known species of stromatoporoids are reported from Nevada: Stromatoporella perannulata, from the Bartine Member of the McColley Canyon Formation (middle Emsian); and Stictostroma moosense, from the Oxyoke Canyon Sandstone (uppermost Emsian). A new species, Syringodictyon nevadense n....

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Published in:Journal of Paleontology
Main Author: Carl W. Stock
Format: Text
Language:English
Published: The Paleontological Society 2022
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Online Access:https://doi.org/10.1017/jpa.2022.18
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spelling ftbioone:10.1017/jpa.2022.18 2024-06-02T08:01:48+00:00 Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance Carl W. Stock Carl W. Stock world 2022-09-07 text/HTML https://doi.org/10.1017/jpa.2022.18 en eng The Paleontological Society doi:10.1017/jpa.2022.18 All rights reserved. https://doi.org/10.1017/jpa.2022.18 Text 2022 ftbioone https://doi.org/10.1017/jpa.2022.18 2024-05-07T00:48:07Z Two previously known species of stromatoporoids are reported from Nevada: Stromatoporella perannulata, from the Bartine Member of the McColley Canyon Formation (middle Emsian); and Stictostroma moosense, from the Oxyoke Canyon Sandstone (uppermost Emsian). A new species, Syringodictyon nevadense n. sp., is described from the Coils Creek Member of the McColley Canyon Formation (upper Emsian). Stromatoporella perannulata also occurs in Emsian-age strata on Ellesmere Island, arctic Canada, and in strata of Emsian and/or Eifelian age in Ontario, New York, Ohio, and Kentucky. Outside Nevada, Syringodictyon is confined to the Emsian of Ellesmere Island, and Emsian/Eifelian of Ontario and New York. Stictostroma moosense is known from only the Emsian/Eifelian of Ontario. It is concluded that the three Nevada specimens are Emsian in age. This implies that in other localities where two of the species, S. perannulata and S. moosense, occur in strata where the placement of the Emsian-Eifelian boundary is in question, it might be higher than previously thought. The presence of the two species, plus Syringodictyon, in both the Old World Realm (Nevada, arctic Canada) and the Eastern Americas Realm (Ontario, New York, Ohio, Kentucky), infers a selective marine connection between the two realms that was not available to other taxa. The breach in the inter-realm barrier most likely occurred as a shallow seaway across the Canadian Shield. Text Arctic Ellesmere Island BioOne Online Journals Arctic Canada Ellesmere Island Journal of Paleontology 96 5 979 990
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description Two previously known species of stromatoporoids are reported from Nevada: Stromatoporella perannulata, from the Bartine Member of the McColley Canyon Formation (middle Emsian); and Stictostroma moosense, from the Oxyoke Canyon Sandstone (uppermost Emsian). A new species, Syringodictyon nevadense n. sp., is described from the Coils Creek Member of the McColley Canyon Formation (upper Emsian). Stromatoporella perannulata also occurs in Emsian-age strata on Ellesmere Island, arctic Canada, and in strata of Emsian and/or Eifelian age in Ontario, New York, Ohio, and Kentucky. Outside Nevada, Syringodictyon is confined to the Emsian of Ellesmere Island, and Emsian/Eifelian of Ontario and New York. Stictostroma moosense is known from only the Emsian/Eifelian of Ontario. It is concluded that the three Nevada specimens are Emsian in age. This implies that in other localities where two of the species, S. perannulata and S. moosense, occur in strata where the placement of the Emsian-Eifelian boundary is in question, it might be higher than previously thought. The presence of the two species, plus Syringodictyon, in both the Old World Realm (Nevada, arctic Canada) and the Eastern Americas Realm (Ontario, New York, Ohio, Kentucky), infers a selective marine connection between the two realms that was not available to other taxa. The breach in the inter-realm barrier most likely occurred as a shallow seaway across the Canadian Shield.
author2 Carl W. Stock
format Text
author Carl W. Stock
spellingShingle Carl W. Stock
Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
author_facet Carl W. Stock
author_sort Carl W. Stock
title Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
title_short Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
title_full Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
title_fullStr Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
title_full_unstemmed Rare stromatoporoids from the Lower Devonian (Emsian) of Nevada, and their biostratigraphic and paleobiogeographic significance
title_sort rare stromatoporoids from the lower devonian (emsian) of nevada, and their biostratigraphic and paleobiogeographic significance
publisher The Paleontological Society
publishDate 2022
url https://doi.org/10.1017/jpa.2022.18
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Canada
Ellesmere Island
geographic_facet Arctic
Canada
Ellesmere Island
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Ellesmere Island
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Ellesmere Island
op_source https://doi.org/10.1017/jpa.2022.18
op_relation doi:10.1017/jpa.2022.18
op_rights All rights reserved.
op_doi https://doi.org/10.1017/jpa.2022.18
container_title Journal of Paleontology
container_volume 96
container_issue 5
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