Pollen Diagrams from Sub-Arctic Central Canada

Peat from Keewatin and Manitoba contained macrofossil and palynological evidence of former latitudinal movements of the forest-tundra boundary in response to the changing location of the mean summer position of the Arctic front. Radiocarbon dating demonstrates the synchroneity of these climatic chan...

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Bibliographic Details
Published in:Science
Main Author: Nichols, Harvey
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1967
Subjects:
Arctic
Canada
Keewatin
Tundra
Online Access:http://dx.doi.org/10.1126/science.155.3770.1665
https://www.science.org/doi/pdf/10.1126/science.155.3770.1665
id craaas:10.1126/science.155.3770.1665
record_format openpolar
spelling craaas:10.1126/science.155.3770.1665 2024-06-09T07:43:08+00:00 Pollen Diagrams from Sub-Arctic Central Canada Nichols, Harvey 1967 http://dx.doi.org/10.1126/science.155.3770.1665 https://www.science.org/doi/pdf/10.1126/science.155.3770.1665 en eng American Association for the Advancement of Science (AAAS) Science volume 155, issue 3770, page 1665-1668 ISSN 0036-8075 1095-9203 journal-article 1967 craaas https://doi.org/10.1126/science.155.3770.1665 2024-05-16T12:55:40Z Peat from Keewatin and Manitoba contained macrofossil and palynological evidence of former latitudinal movements of the forest-tundra boundary in response to the changing location of the mean summer position of the Arctic front. Radiocarbon dating demonstrates the synchroneity of these climatic changes with those registered in northwest Europe during the past 6000 years. Article in Journal/Newspaper Arctic Keewatin Tundra AAAS Resource Center (American Association for the Advancement of Science) Arctic Canada Science 155 3770 1665 1668
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Peat from Keewatin and Manitoba contained macrofossil and palynological evidence of former latitudinal movements of the forest-tundra boundary in response to the changing location of the mean summer position of the Arctic front. Radiocarbon dating demonstrates the synchroneity of these climatic changes with those registered in northwest Europe during the past 6000 years.
format Article in Journal/Newspaper
author Nichols, Harvey
spellingShingle Nichols, Harvey
Pollen Diagrams from Sub-Arctic Central Canada
author_facet Nichols, Harvey
author_sort Nichols, Harvey
title Pollen Diagrams from Sub-Arctic Central Canada
title_short Pollen Diagrams from Sub-Arctic Central Canada
title_full Pollen Diagrams from Sub-Arctic Central Canada
title_fullStr Pollen Diagrams from Sub-Arctic Central Canada
title_full_unstemmed Pollen Diagrams from Sub-Arctic Central Canada
title_sort pollen diagrams from sub-arctic central canada
publisher American Association for the Advancement of Science (AAAS)
publishDate 1967
url http://dx.doi.org/10.1126/science.155.3770.1665
https://www.science.org/doi/pdf/10.1126/science.155.3770.1665
geographic Arctic
Canada
geographic_facet Arctic
Canada
genre Arctic
Keewatin
Tundra
genre_facet Arctic
Keewatin
Tundra
op_source Science
volume 155, issue 3770, page 1665-1668
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.155.3770.1665
container_title Science
container_volume 155
container_issue 3770
container_start_page 1665
op_container_end_page 1668
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