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...
Published in: | Science |
---|---|
Main Authors: | , |
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 |
id |
craaas:10.1126/science.202.4373.1181 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1810482266081591296 |