Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland

A diverse and well-preserved fauna of shelly fossils from the upper Lower Cambrian Bastion and Ella Island Formations of North-East Greenland contains more than 90 species. The fauna is the most diverse shelly fauna yet discovered in the Lower Cambrian of Laurentia and includes many fossils previous...

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Bibliographic Details
Main Author: Skovsted, Christian B.
Format: Article in Journal/Newspaper
Language:English
Published: 2006
Subjects:
Online Access:https://researchers.mq.edu.au/en/publications/ebc9b8d3-2d15-4bfc-8e17-1e0a0843c4e8
https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2
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author Skovsted, Christian B.
author_facet Skovsted, Christian B.
author_sort Skovsted, Christian B.
collection Unknown
description A diverse and well-preserved fauna of shelly fossils from the upper Lower Cambrian Bastion and Ella Island Formations of North-East Greenland contains more than 90 species. The fauna is the most diverse shelly fauna yet discovered in the Lower Cambrian of Laurentia and includes many fossils previously known only from other continental blocks. It enhances correlation of the North-East Greenland succession into Laurentia, most notably with the Browns Pond Formation of New York State, but also with other important Early Cambrian continents, in particular with Australia, Antarctica, and Siberia. A middle Dyeran age is most probable for both the Bastion and Ella Island Formation, and the rich fossil assemblage facilitates correlation with the Botoman Stage of Siberia and its equivalents. One new taxon is described, the disc-shaped problematicum Tunudiscus duovittarius n. gen. and sp.
format Article in Journal/Newspaper
genre Antarc*
Antarctica
East Greenland
Greenland
Siberia
genre_facet Antarc*
Antarctica
East Greenland
Greenland
Siberia
geographic Browns
Browns Pond
Greenland
The Bastion
geographic_facet Browns
Browns Pond
Greenland
The Bastion
id ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/ebc9b8d3-2d15-4bfc-8e17-1e0a0843c4e8
institution Open Polar
language English
long_lat ENVELOPE(-44.583,-44.583,-60.700,-60.700)
ENVELOPE(-56.081,-56.081,49.617,49.617)
ENVELOPE(-136.705,-136.705,67.655,67.655)
op_collection_id ftmacquarieunicr
op_doi https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2
op_rights info:eu-repo/semantics/restrictedAccess
op_source Skovsted , C B 2006 , ' Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland ' , Journal of Paleontology , vol. 80 , no. 6 , pp. 1087-1112 . https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2
publishDate 2006
record_format openpolar
spelling ftmacquarieunicr:oai:https://researchers.mq.edu.au:publications/ebc9b8d3-2d15-4bfc-8e17-1e0a0843c4e8 2025-06-15T14:12:26+00:00 Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland Skovsted, Christian B. 2006 https://researchers.mq.edu.au/en/publications/ebc9b8d3-2d15-4bfc-8e17-1e0a0843c4e8 https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2 eng eng info:eu-repo/semantics/restrictedAccess Skovsted , C B 2006 , ' Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland ' , Journal of Paleontology , vol. 80 , no. 6 , pp. 1087-1112 . https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2 shelly fauna fossils Lower Cambrian Bastion Ella Island Formation North-East Greenland Tunudiscus duovittarius article 2006 ftmacquarieunicr https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2 2025-06-02T00:02:24Z A diverse and well-preserved fauna of shelly fossils from the upper Lower Cambrian Bastion and Ella Island Formations of North-East Greenland contains more than 90 species. The fauna is the most diverse shelly fauna yet discovered in the Lower Cambrian of Laurentia and includes many fossils previously known only from other continental blocks. It enhances correlation of the North-East Greenland succession into Laurentia, most notably with the Browns Pond Formation of New York State, but also with other important Early Cambrian continents, in particular with Australia, Antarctica, and Siberia. A middle Dyeran age is most probable for both the Bastion and Ella Island Formation, and the rich fossil assemblage facilitates correlation with the Botoman Stage of Siberia and its equivalents. One new taxon is described, the disc-shaped problematicum Tunudiscus duovittarius n. gen. and sp. Article in Journal/Newspaper Antarc* Antarctica East Greenland Greenland Siberia Unknown Browns ENVELOPE(-44.583,-44.583,-60.700,-60.700) Browns Pond ENVELOPE(-56.081,-56.081,49.617,49.617) Greenland The Bastion ENVELOPE(-136.705,-136.705,67.655,67.655)
spellingShingle shelly fauna fossils
Lower Cambrian Bastion
Ella Island Formation
North-East Greenland
Tunudiscus duovittarius
Skovsted, Christian B.
Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title_full Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title_fullStr Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title_full_unstemmed Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title_short Small shelly fauna from the upper Lower Cambrian Bastion and Ella Island Formations, North-East Greenland
title_sort small shelly fauna from the upper lower cambrian bastion and ella island formations, north-east greenland
topic shelly fauna fossils
Lower Cambrian Bastion
Ella Island Formation
North-East Greenland
Tunudiscus duovittarius
topic_facet shelly fauna fossils
Lower Cambrian Bastion
Ella Island Formation
North-East Greenland
Tunudiscus duovittarius
url https://researchers.mq.edu.au/en/publications/ebc9b8d3-2d15-4bfc-8e17-1e0a0843c4e8
https://doi.org/10.1666/0022-3360(2006)80[1087:SSFFTU]2.0.CO;2