Pollen diagrams from interior Labrador
Six pollen zones can be distinguished in interior Labrador. The earlier zones represent the primary succession of vegetation from bare ground to boreal woodland or forest, which occupied about 500 years between 5700 and 5200 B.P. There have been only minor fluctuations in the nature of the vegetatio...
Published in: | Canadian Journal of Botany |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Canadian Science Publishing
1970
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Online Access: | http://dx.doi.org/10.1139/b70-287 http://www.nrcresearchpress.com/doi/pdf/10.1139/b70-287 |
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crcansciencepubl:10.1139/b70-287 2023-12-17T10:28:52+01:00 Pollen diagrams from interior Labrador Morrison, Alastair 1970 http://dx.doi.org/10.1139/b70-287 http://www.nrcresearchpress.com/doi/pdf/10.1139/b70-287 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Botany volume 48, issue 11, page 1957-1975 ISSN 0008-4026 Plant Science journal-article 1970 crcansciencepubl https://doi.org/10.1139/b70-287 2023-11-19T13:38:29Z Six pollen zones can be distinguished in interior Labrador. The earlier zones represent the primary succession of vegetation from bare ground to boreal woodland or forest, which occupied about 500 years between 5700 and 5200 B.P. There have been only minor fluctuations in the nature of the vegetation since 5200 B.P. Radiocarbon dates show that the zones are contemporaneous over that part of the Lake Plateau within the Churchill River watershed, but similar vegetation changes occurred 1000 years earlier in the Kaniapiskau basin, further north, in New Quebec. These two areas must have been freed of a cover of glacier ice or lake waters immediately before 5700 B.P. and 6700 B.P. respectively. Article in Journal/Newspaper Churchill River Canadian Science Publishing (via Crossref) Freed ENVELOPE(164.333,164.333,-71.483,-71.483) Canadian Journal of Botany 48 11 1957 1975 |
institution |
Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
Plant Science |
spellingShingle |
Plant Science Morrison, Alastair Pollen diagrams from interior Labrador |
topic_facet |
Plant Science |
description |
Six pollen zones can be distinguished in interior Labrador. The earlier zones represent the primary succession of vegetation from bare ground to boreal woodland or forest, which occupied about 500 years between 5700 and 5200 B.P. There have been only minor fluctuations in the nature of the vegetation since 5200 B.P. Radiocarbon dates show that the zones are contemporaneous over that part of the Lake Plateau within the Churchill River watershed, but similar vegetation changes occurred 1000 years earlier in the Kaniapiskau basin, further north, in New Quebec. These two areas must have been freed of a cover of glacier ice or lake waters immediately before 5700 B.P. and 6700 B.P. respectively. |
format |
Article in Journal/Newspaper |
author |
Morrison, Alastair |
author_facet |
Morrison, Alastair |
author_sort |
Morrison, Alastair |
title |
Pollen diagrams from interior Labrador |
title_short |
Pollen diagrams from interior Labrador |
title_full |
Pollen diagrams from interior Labrador |
title_fullStr |
Pollen diagrams from interior Labrador |
title_full_unstemmed |
Pollen diagrams from interior Labrador |
title_sort |
pollen diagrams from interior labrador |
publisher |
Canadian Science Publishing |
publishDate |
1970 |
url |
http://dx.doi.org/10.1139/b70-287 http://www.nrcresearchpress.com/doi/pdf/10.1139/b70-287 |
long_lat |
ENVELOPE(164.333,164.333,-71.483,-71.483) |
geographic |
Freed |
geographic_facet |
Freed |
genre |
Churchill River |
genre_facet |
Churchill River |
op_source |
Canadian Journal of Botany volume 48, issue 11, page 1957-1975 ISSN 0008-4026 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/b70-287 |
container_title |
Canadian Journal of Botany |
container_volume |
48 |
container_issue |
11 |
container_start_page |
1957 |
op_container_end_page |
1975 |
_version_ |
1785581067223171072 |