A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin
A 396-cm sediment sequence from SW Lake in the boreal woodland zone near Travaillant Lake, Northwest Territories, Canada, provides a Holocene record of pollen percentages and species interactions. Three local pollen assemblage zones are described: a Betula–Populus–Juniperus zone from 10 500 to 9000...
Published in: | Canadian Journal of Botany |
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Language: | English |
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Canadian Science Publishing
1984
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Online Access: | http://dx.doi.org/10.1139/b84-188 http://www.nrcresearchpress.com/doi/pdf/10.1139/b84-188 |
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crcansciencepubl:10.1139/b84-188 2023-12-17T10:33:16+01:00 A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin Ritchie, J. C. 1984 http://dx.doi.org/10.1139/b84-188 http://www.nrcresearchpress.com/doi/pdf/10.1139/b84-188 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Botany volume 62, issue 7, page 1385-1392 ISSN 0008-4026 Plant Science journal-article 1984 crcansciencepubl https://doi.org/10.1139/b84-188 2023-11-19T13:39:16Z A 396-cm sediment sequence from SW Lake in the boreal woodland zone near Travaillant Lake, Northwest Territories, Canada, provides a Holocene record of pollen percentages and species interactions. Three local pollen assemblage zones are described: a Betula–Populus–Juniperus zone from 10 500 to 9000 years BP, a Picea–Betula zone from 9000 to 5100 years BP, and a Picea–Betula–Alnus zone from 5100 years BP to the present. The earliest vegetation recorded at this site is a mosaic of poplar groves, juniper and Shepherdia shrub, and fragmentary patches of tundra, replaced rapidly by spruce woodland at roughly 8500 years BP, dominated initially by Picea glauca. Picea mariana spread extensively between 8500 and 5000 years BP, probably as a function of increasing paludification. The present spruce-dominated vegetation was in place by 5000 years BP. Some changes in the pollen record can be explained by the Milankovitch early Holocene period of warmer summers followed by a cooling to modern conditions by 5000 years BP. Others require explanations in terms of edaphic factors or biological interactions among the main taxa. Article in Journal/Newspaper Mackenzie river Northwest Territories Tundra Canadian Science Publishing (via Crossref) Northwest Territories Mackenzie River Canada Travaillant Lake ENVELOPE(-131.786,-131.786,67.700,67.700) Canadian Journal of Botany 62 7 1385 1392 |
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Open Polar |
collection |
Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
Plant Science |
spellingShingle |
Plant Science Ritchie, J. C. A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
topic_facet |
Plant Science |
description |
A 396-cm sediment sequence from SW Lake in the boreal woodland zone near Travaillant Lake, Northwest Territories, Canada, provides a Holocene record of pollen percentages and species interactions. Three local pollen assemblage zones are described: a Betula–Populus–Juniperus zone from 10 500 to 9000 years BP, a Picea–Betula zone from 9000 to 5100 years BP, and a Picea–Betula–Alnus zone from 5100 years BP to the present. The earliest vegetation recorded at this site is a mosaic of poplar groves, juniper and Shepherdia shrub, and fragmentary patches of tundra, replaced rapidly by spruce woodland at roughly 8500 years BP, dominated initially by Picea glauca. Picea mariana spread extensively between 8500 and 5000 years BP, probably as a function of increasing paludification. The present spruce-dominated vegetation was in place by 5000 years BP. Some changes in the pollen record can be explained by the Milankovitch early Holocene period of warmer summers followed by a cooling to modern conditions by 5000 years BP. Others require explanations in terms of edaphic factors or biological interactions among the main taxa. |
format |
Article in Journal/Newspaper |
author |
Ritchie, J. C. |
author_facet |
Ritchie, J. C. |
author_sort |
Ritchie, J. C. |
title |
A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
title_short |
A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
title_full |
A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
title_fullStr |
A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
title_full_unstemmed |
A Holocene pollen record of boreal forest history from the Travaillant Lake area, Lower Mackenzie River Basin |
title_sort |
holocene pollen record of boreal forest history from the travaillant lake area, lower mackenzie river basin |
publisher |
Canadian Science Publishing |
publishDate |
1984 |
url |
http://dx.doi.org/10.1139/b84-188 http://www.nrcresearchpress.com/doi/pdf/10.1139/b84-188 |
long_lat |
ENVELOPE(-131.786,-131.786,67.700,67.700) |
geographic |
Northwest Territories Mackenzie River Canada Travaillant Lake |
geographic_facet |
Northwest Territories Mackenzie River Canada Travaillant Lake |
genre |
Mackenzie river Northwest Territories Tundra |
genre_facet |
Mackenzie river Northwest Territories Tundra |
op_source |
Canadian Journal of Botany volume 62, issue 7, page 1385-1392 ISSN 0008-4026 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/b84-188 |
container_title |
Canadian Journal of Botany |
container_volume |
62 |
container_issue |
7 |
container_start_page |
1385 |
op_container_end_page |
1392 |
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1785587194976534528 |