Palynological study of the continental shelf sediments of the Labrador Sea ...
A detailed palynological examination was made of Tertiary pollen and spore assemblages from six exploratory wells located along the continental margins of the Labrador Sea. From north to south, the study wells are Kangamiut 1, Hekja 0-71, Karlsefni A-13, Herjolf M-92, Roberval K-92 and Cartier D-70....
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University of British Columbia
2010
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ftdatacite:10.14288/1.0052419 2024-04-28T08:27:37+00:00 Palynological study of the continental shelf sediments of the Labrador Sea ... Williams, V. Eileen 2010 https://dx.doi.org/10.14288/1.0052419 https://doi.library.ubc.ca/10.14288/1.0052419 en eng University of British Columbia article-journal Text ScholarlyArticle 2010 ftdatacite https://doi.org/10.14288/1.0052419 2024-04-02T09:38:34Z A detailed palynological examination was made of Tertiary pollen and spore assemblages from six exploratory wells located along the continental margins of the Labrador Sea. From north to south, the study wells are Kangamiut 1, Hekja 0-71, Karlsefni A-13, Herjolf M-92, Roberval K-92 and Cartier D-70. Using local extinction events of zonally diagnostic species to define the tops of intervals, eight provisional pollen and spore zones were established. The zones and their relative ages are as follows: Tsuga igniculus (middle to late Miocene); Fagus granulata (early to middle Miocene); Parviprojectus sp. A (early Oligocene); Araliaceoipollenites megaporifer (latest Eocene/earliest Oligocene); Rhoipites latus (middle to late Eocene); Pistillipollenites mcgregorii (early to middle Eocene); Tricolpites sp. A (middle to late Paleocene); and Paraalnipollenites alterniporus (early to middle Paleocene). The middle and upper Oligocene is apparently absent in the study welIs. When used in conjunction with dinoflagellate ... Text Labrador Sea DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
description |
A detailed palynological examination was made of Tertiary pollen and spore assemblages from six exploratory wells located along the continental margins of the Labrador Sea. From north to south, the study wells are Kangamiut 1, Hekja 0-71, Karlsefni A-13, Herjolf M-92, Roberval K-92 and Cartier D-70. Using local extinction events of zonally diagnostic species to define the tops of intervals, eight provisional pollen and spore zones were established. The zones and their relative ages are as follows: Tsuga igniculus (middle to late Miocene); Fagus granulata (early to middle Miocene); Parviprojectus sp. A (early Oligocene); Araliaceoipollenites megaporifer (latest Eocene/earliest Oligocene); Rhoipites latus (middle to late Eocene); Pistillipollenites mcgregorii (early to middle Eocene); Tricolpites sp. A (middle to late Paleocene); and Paraalnipollenites alterniporus (early to middle Paleocene). The middle and upper Oligocene is apparently absent in the study welIs. When used in conjunction with dinoflagellate ... |
format |
Text |
author |
Williams, V. Eileen |
spellingShingle |
Williams, V. Eileen Palynological study of the continental shelf sediments of the Labrador Sea ... |
author_facet |
Williams, V. Eileen |
author_sort |
Williams, V. Eileen |
title |
Palynological study of the continental shelf sediments of the Labrador Sea ... |
title_short |
Palynological study of the continental shelf sediments of the Labrador Sea ... |
title_full |
Palynological study of the continental shelf sediments of the Labrador Sea ... |
title_fullStr |
Palynological study of the continental shelf sediments of the Labrador Sea ... |
title_full_unstemmed |
Palynological study of the continental shelf sediments of the Labrador Sea ... |
title_sort |
palynological study of the continental shelf sediments of the labrador sea ... |
publisher |
University of British Columbia |
publishDate |
2010 |
url |
https://dx.doi.org/10.14288/1.0052419 https://doi.library.ubc.ca/10.14288/1.0052419 |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_doi |
https://doi.org/10.14288/1.0052419 |
_version_ |
1797586476041502720 |