Early Devonian Spores from Central Ellesmere Island, Canadian Arctic

The Vendom Fiord Formation near the head of Cañon Fiord, central Ellesmere Island, hitherto thought to be unfossiliferous, contains mid to late Emsian trilete spores. Strata below the Vendom Fiord Formation, separated from it by an unconformity, contain a less diverse assemblage of spores that sugge...

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Published in:Canadian Journal of Earth Sciences
Main Author: McGregor, D. C.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1974
Subjects:
Online Access:http://dx.doi.org/10.1139/e74-006
http://www.nrcresearchpress.com/doi/pdf/10.1139/e74-006
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spelling crcansciencepubl:10.1139/e74-006 2024-09-15T18:04:45+00:00 Early Devonian Spores from Central Ellesmere Island, Canadian Arctic McGregor, D. C. 1974 http://dx.doi.org/10.1139/e74-006 http://www.nrcresearchpress.com/doi/pdf/10.1139/e74-006 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 11, issue 1, page 70-78 ISSN 0008-4077 1480-3313 journal-article 1974 crcansciencepubl https://doi.org/10.1139/e74-006 2024-07-25T04:10:08Z The Vendom Fiord Formation near the head of Cañon Fiord, central Ellesmere Island, hitherto thought to be unfossiliferous, contains mid to late Emsian trilete spores. Strata below the Vendom Fiord Formation, separated from it by an unconformity, contain a less diverse assemblage of spores that suggests a mid to late Gedinnian age. The spores are the only fossils known from these beds, and the first palynomorphs to be reported from the Early Devonian rocks of Ellesmere Island. Article in Journal/Newspaper Ellesmere Island Canadian Science Publishing Canadian Journal of Earth Sciences 11 1 70 78
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
description The Vendom Fiord Formation near the head of Cañon Fiord, central Ellesmere Island, hitherto thought to be unfossiliferous, contains mid to late Emsian trilete spores. Strata below the Vendom Fiord Formation, separated from it by an unconformity, contain a less diverse assemblage of spores that suggests a mid to late Gedinnian age. The spores are the only fossils known from these beds, and the first palynomorphs to be reported from the Early Devonian rocks of Ellesmere Island.
format Article in Journal/Newspaper
author McGregor, D. C.
spellingShingle McGregor, D. C.
Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
author_facet McGregor, D. C.
author_sort McGregor, D. C.
title Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
title_short Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
title_full Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
title_fullStr Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
title_full_unstemmed Early Devonian Spores from Central Ellesmere Island, Canadian Arctic
title_sort early devonian spores from central ellesmere island, canadian arctic
publisher Canadian Science Publishing
publishDate 1974
url http://dx.doi.org/10.1139/e74-006
http://www.nrcresearchpress.com/doi/pdf/10.1139/e74-006
genre Ellesmere Island
genre_facet Ellesmere Island
op_source Canadian Journal of Earth Sciences
volume 11, issue 1, page 70-78
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e74-006
container_title Canadian Journal of Earth Sciences
container_volume 11
container_issue 1
container_start_page 70
op_container_end_page 78
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