Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada
Abstract Two radiocarbon-dated cores from small lakes located approximately 25 km north of the mapped boundary between forest-tundra and tundra provide records of postglacial vegetation change at the treeline near Yellowknife, NWT, Canada. Basal radiocarbon dates of 6180 and 7470 yr B.P. were obtain...
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Cambridge University Press (CUP)
1990
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Online Access: | http://dx.doi.org/10.1016/0033-5894(90)90033-h http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/xml http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400020950 |
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crcambridgeupr:10.1016/0033-5894(90)90033-h 2024-09-15T18:26:38+00:00 Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada Moser, K. A. MacDonald, G. M. 1990 http://dx.doi.org/10.1016/0033-5894(90)90033-h http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/xml http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400020950 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Quaternary Research volume 34, issue 2, page 227-239 ISSN 0033-5894 1096-0287 journal-article 1990 crcambridgeupr https://doi.org/10.1016/0033-5894(90)90033-h 2024-08-07T04:04:39Z Abstract Two radiocarbon-dated cores from small lakes located approximately 25 km north of the mapped boundary between forest-tundra and tundra provide records of postglacial vegetation change at the treeline near Yellowknife, NWT, Canada. Basal radiocarbon dates of 6180 and 7470 yr B.P. were obtained from the cores. The fossil pollen evidence suggests that the initial vegetation was Betula tundra with a peatland component. Alnus became an important constituent of the pollen assemblages between 6900 and 5500 yr B.P. Both lakes record sharp increases in Picea cf. mariana pollen at approximately 5000 yr B.P., suggesting the establishment of forest-tundra. By 3500 yr B.P. Picea mariana forest-tundra had withdrawn. The proportion of organic to inorganic sediment in the cores was at a maximum between 5000 and 3500 yr B.P. Tundra has dominated the region since 3500 yr B.P. In northwestern Canada, the maximum northward advance of treeline occurred between 9000 and 5000 yr B.P. The asynchrony in treeline advance in central and northwestern Canada may reflect that glacial ice persisted in the interior NWT longer than previously believed. Alternatively, the asynchronous history of the treeline may be a result of the geometric properties of the long-wave westerly disturbance that is manifest in the median summer position of the arctic front and ultimately controls the geographic location of the treeline. Article in Journal/Newspaper Northwest Territories Tundra Yellowknife Cambridge University Press Quaternary Research 34 2 227 239 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Two radiocarbon-dated cores from small lakes located approximately 25 km north of the mapped boundary between forest-tundra and tundra provide records of postglacial vegetation change at the treeline near Yellowknife, NWT, Canada. Basal radiocarbon dates of 6180 and 7470 yr B.P. were obtained from the cores. The fossil pollen evidence suggests that the initial vegetation was Betula tundra with a peatland component. Alnus became an important constituent of the pollen assemblages between 6900 and 5500 yr B.P. Both lakes record sharp increases in Picea cf. mariana pollen at approximately 5000 yr B.P., suggesting the establishment of forest-tundra. By 3500 yr B.P. Picea mariana forest-tundra had withdrawn. The proportion of organic to inorganic sediment in the cores was at a maximum between 5000 and 3500 yr B.P. Tundra has dominated the region since 3500 yr B.P. In northwestern Canada, the maximum northward advance of treeline occurred between 9000 and 5000 yr B.P. The asynchrony in treeline advance in central and northwestern Canada may reflect that glacial ice persisted in the interior NWT longer than previously believed. Alternatively, the asynchronous history of the treeline may be a result of the geometric properties of the long-wave westerly disturbance that is manifest in the median summer position of the arctic front and ultimately controls the geographic location of the treeline. |
format |
Article in Journal/Newspaper |
author |
Moser, K. A. MacDonald, G. M. |
spellingShingle |
Moser, K. A. MacDonald, G. M. Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
author_facet |
Moser, K. A. MacDonald, G. M. |
author_sort |
Moser, K. A. |
title |
Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
title_short |
Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
title_full |
Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
title_fullStr |
Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
title_full_unstemmed |
Holocene Vegetation Change at Treeline North of Yellowknife, Northwest Territories, Canada |
title_sort |
holocene vegetation change at treeline north of yellowknife, northwest territories, canada |
publisher |
Cambridge University Press (CUP) |
publishDate |
1990 |
url |
http://dx.doi.org/10.1016/0033-5894(90)90033-h http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/xml http://api.elsevier.com/content/article/PII:003358949090033H?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033589400020950 |
genre |
Northwest Territories Tundra Yellowknife |
genre_facet |
Northwest Territories Tundra Yellowknife |
op_source |
Quaternary Research volume 34, issue 2, page 227-239 ISSN 0033-5894 1096-0287 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1016/0033-5894(90)90033-h |
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Quaternary Research |
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34 |
container_issue |
2 |
container_start_page |
227 |
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239 |
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1810467155189170176 |