Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada
Sediment from Eildun Lake, located at 63°8.6′N, 122°46.5′W in the northern boreal forest, was cored to a depth of 268 cm and analyzed for pollen content. Pollen percentages and 14 C dates suggest a vegetational sequence extending back over 11 000 years. The sequence begins with a discontinuous herb...
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1985
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crcansciencepubl:10.1139/e85-073 2023-12-17T10:29:31+01:00 Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada Slater, Donald S. 1985 http://dx.doi.org/10.1139/e85-073 http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-073 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 22, issue 5, page 663-674 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1985 crcansciencepubl https://doi.org/10.1139/e85-073 2023-11-19T13:38:21Z Sediment from Eildun Lake, located at 63°8.6′N, 122°46.5′W in the northern boreal forest, was cored to a depth of 268 cm and analyzed for pollen content. Pollen percentages and 14 C dates suggest a vegetational sequence extending back over 11 000 years. The sequence begins with a discontinuous herb tundra dominated by Artemisia and Gramineae. This was succeeded by a shrub tundra dominated by dwarf birch and willow. Poplar had invaded by approximately 10 700 BP to form a dwarf birch – poplar groveland or forest tundra. Between approximately 10 300 and 7510 BP spruce replaced poplar as the dominant tree, although still forming a forest tundra. Boreal forest, including tree birch and alder, became established shortly after 7510 BP and has persisted since then with very little change. Pinus pollen has increased in percentage, particularly during the last 2400 years, reaching its Holocene maximum at the present day. The percentages attained indicate the presence of pine trees regionally though not in the near vicinity of Eildun Lake. Article in Journal/Newspaper Dwarf birch Tundra Canadian Science Publishing (via Crossref) Canada Canadian Journal of Earth Sciences 22 5 663 674 |
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Open Polar |
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Canadian Science Publishing (via Crossref) |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Slater, Donald S. Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
topic_facet |
General Earth and Planetary Sciences |
description |
Sediment from Eildun Lake, located at 63°8.6′N, 122°46.5′W in the northern boreal forest, was cored to a depth of 268 cm and analyzed for pollen content. Pollen percentages and 14 C dates suggest a vegetational sequence extending back over 11 000 years. The sequence begins with a discontinuous herb tundra dominated by Artemisia and Gramineae. This was succeeded by a shrub tundra dominated by dwarf birch and willow. Poplar had invaded by approximately 10 700 BP to form a dwarf birch – poplar groveland or forest tundra. Between approximately 10 300 and 7510 BP spruce replaced poplar as the dominant tree, although still forming a forest tundra. Boreal forest, including tree birch and alder, became established shortly after 7510 BP and has persisted since then with very little change. Pinus pollen has increased in percentage, particularly during the last 2400 years, reaching its Holocene maximum at the present day. The percentages attained indicate the presence of pine trees regionally though not in the near vicinity of Eildun Lake. |
format |
Article in Journal/Newspaper |
author |
Slater, Donald S. |
author_facet |
Slater, Donald S. |
author_sort |
Slater, Donald S. |
title |
Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
title_short |
Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
title_full |
Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
title_fullStr |
Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
title_full_unstemmed |
Pollen analysis of postglacial sediments from Eildun Lake, District of Mackenzie, N.W.T., Canada |
title_sort |
pollen analysis of postglacial sediments from eildun lake, district of mackenzie, n.w.t., canada |
publisher |
Canadian Science Publishing |
publishDate |
1985 |
url |
http://dx.doi.org/10.1139/e85-073 http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-073 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Dwarf birch Tundra |
genre_facet |
Dwarf birch Tundra |
op_source |
Canadian Journal of Earth Sciences volume 22, issue 5, page 663-674 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e85-073 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
22 |
container_issue |
5 |
container_start_page |
663 |
op_container_end_page |
674 |
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1785581912995135488 |