Early Deglaciation of the Labrador Shelf

Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters. The pollen record indicate...

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Published in:Science
Main Authors: Vilks, Gustavs, Mudie, Peta J.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1978
Subjects:
Online Access:http://dx.doi.org/10.1126/science.202.4373.1181
https://www.science.org/doi/pdf/10.1126/science.202.4373.1181
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spelling craaas:10.1126/science.202.4373.1181 2024-09-15T18:37:55+00:00 Early Deglaciation of the Labrador Shelf Vilks, Gustavs Mudie, Peta J. 1978 http://dx.doi.org/10.1126/science.202.4373.1181 https://www.science.org/doi/pdf/10.1126/science.202.4373.1181 en eng American Association for the Advancement of Science (AAAS) Science volume 202, issue 4373, page 1181-1183 ISSN 0036-8075 1095-9203 journal-article 1978 craaas https://doi.org/10.1126/science.202.4373.1181 2024-07-25T04:01:04Z Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters. The pollen record indicates the presence of a sedge-shrub tundra in eastern Labrador as early as 21,000 years B.P. Both sources of evidence suggest less extensive continental ice than has previously been reported for this subarctic region. Article in Journal/Newspaper Subarctic Tundra AAAS Resource Center (American Association for the Advancement of Science) Science 202 4373 1181 1183
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Two marine sediment cores from a basin on the southeastern Labrador Shelf penetrate a mud sequence extending back to 21,000 carbon-14 years before the present (B.P.). The benthic foraminifera are dominated by subartic nearshore species indicative of ice-free summer waters. The pollen record indicates the presence of a sedge-shrub tundra in eastern Labrador as early as 21,000 years B.P. Both sources of evidence suggest less extensive continental ice than has previously been reported for this subarctic region.
format Article in Journal/Newspaper
author Vilks, Gustavs
Mudie, Peta J.
spellingShingle Vilks, Gustavs
Mudie, Peta J.
Early Deglaciation of the Labrador Shelf
author_facet Vilks, Gustavs
Mudie, Peta J.
author_sort Vilks, Gustavs
title Early Deglaciation of the Labrador Shelf
title_short Early Deglaciation of the Labrador Shelf
title_full Early Deglaciation of the Labrador Shelf
title_fullStr Early Deglaciation of the Labrador Shelf
title_full_unstemmed Early Deglaciation of the Labrador Shelf
title_sort early deglaciation of the labrador shelf
publisher American Association for the Advancement of Science (AAAS)
publishDate 1978
url http://dx.doi.org/10.1126/science.202.4373.1181
https://www.science.org/doi/pdf/10.1126/science.202.4373.1181
genre Subarctic
Tundra
genre_facet Subarctic
Tundra
op_source Science
volume 202, issue 4373, page 1181-1183
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.202.4373.1181
container_title Science
container_volume 202
container_issue 4373
container_start_page 1181
op_container_end_page 1183
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