Viséan limestones front the Newfoundland Shelf
Three short cores of Windsor Group carbonates from the northeast Newfoundland Shelf yielded Late Viséan foraminifers of Zones 15 and 16 Inf . This most northeastward occurrence of the marine Lower Carboniferous on the American continent has foraminifers identical to those reported from Windsor carbo...
Published in: | Canadian Journal of Earth Sciences |
---|---|
Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1978
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e78-149 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-149 |
id |
crcansciencepubl:10.1139/e78-149 |
---|---|
record_format |
openpolar |
spelling |
crcansciencepubl:10.1139/e78-149 2024-09-15T18:19:39+00:00 Viséan limestones front the Newfoundland Shelf Jansa, L. F. Mamet, B. Roux, A. 1978 http://dx.doi.org/10.1139/e78-149 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-149 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 15, issue 9, page 1422-1436 ISSN 0008-4077 1480-3313 journal-article 1978 crcansciencepubl https://doi.org/10.1139/e78-149 2024-07-25T04:10:06Z Three short cores of Windsor Group carbonates from the northeast Newfoundland Shelf yielded Late Viséan foraminifers of Zones 15 and 16 Inf . This most northeastward occurrence of the marine Lower Carboniferous on the American continent has foraminifers identical to those reported from Windsor carbonates exposed in southwestern Newfoundland and Nova Scotia. The foraminifera belong to the North American realm and not to the Tethyan realm. The algae are exceptionally well preserved. Except for a single species, they are also 'American' and not Tethyan. This confirms that the proto-Atlantic effectively separates the North American and Euro–African continental blocks in Early Carboniferous time. Article in Journal/Newspaper Newfoundland Canadian Science Publishing Canadian Journal of Earth Sciences 15 9 1422 1436 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
description |
Three short cores of Windsor Group carbonates from the northeast Newfoundland Shelf yielded Late Viséan foraminifers of Zones 15 and 16 Inf . This most northeastward occurrence of the marine Lower Carboniferous on the American continent has foraminifers identical to those reported from Windsor carbonates exposed in southwestern Newfoundland and Nova Scotia. The foraminifera belong to the North American realm and not to the Tethyan realm. The algae are exceptionally well preserved. Except for a single species, they are also 'American' and not Tethyan. This confirms that the proto-Atlantic effectively separates the North American and Euro–African continental blocks in Early Carboniferous time. |
format |
Article in Journal/Newspaper |
author |
Jansa, L. F. Mamet, B. Roux, A. |
spellingShingle |
Jansa, L. F. Mamet, B. Roux, A. Viséan limestones front the Newfoundland Shelf |
author_facet |
Jansa, L. F. Mamet, B. Roux, A. |
author_sort |
Jansa, L. F. |
title |
Viséan limestones front the Newfoundland Shelf |
title_short |
Viséan limestones front the Newfoundland Shelf |
title_full |
Viséan limestones front the Newfoundland Shelf |
title_fullStr |
Viséan limestones front the Newfoundland Shelf |
title_full_unstemmed |
Viséan limestones front the Newfoundland Shelf |
title_sort |
viséan limestones front the newfoundland shelf |
publisher |
Canadian Science Publishing |
publishDate |
1978 |
url |
http://dx.doi.org/10.1139/e78-149 http://www.nrcresearchpress.com/doi/pdf/10.1139/e78-149 |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_source |
Canadian Journal of Earth Sciences volume 15, issue 9, page 1422-1436 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e78-149 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
15 |
container_issue |
9 |
container_start_page |
1422 |
op_container_end_page |
1436 |
_version_ |
1810457999956770816 |