Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory

The pollen record of a 240 cm peat profile in the Ittlemit Lake area in southwest Yukon Territory presents a vegetation development history of the last 9000 radiocarbon years. Spruce migrated into the area at least 9000 radiocarbon years ago. From 9000 yr BP to approximately 5000 yr BP the area supp...

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Published in:ARCTIC
Main Authors: Wang, Xia-Cheng, Geurts, Marie-Anne
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1991
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64568 2023-05-15T14:19:12+02:00 Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory Wang, Xia-Cheng Geurts, Marie-Anne 1991-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568/48482 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568 ARCTIC; Vol. 44 No. 1 (1991): March: 1–93; 23-30 1923-1245 0004-0843 Cores Frozen ground Palaeoclimatology Palaeoecology Palynology Peat Plant distribution Plants (Biology) Pollen Radiocarbon dating Soil profiles Ittlemit Lake region Yukon info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1991 ftunivcalgaryojs 2022-03-22T21:21:42Z The pollen record of a 240 cm peat profile in the Ittlemit Lake area in southwest Yukon Territory presents a vegetation development history of the last 9000 radiocarbon years. Spruce migrated into the area at least 9000 radiocarbon years ago. From 9000 yr BP to approximately 5000 yr BP the area supported a sparse Picea-Salix-Betula forest-tundra vegetation. By 5000 yr BP local environmental change created a different habitat primarily affecting the local taxa. Alnus invaded the general area shortly after 5000 yr BP. A local Betula-dominated community replaced the previous Cyperaceae-dominated one at about 3000 yr BP. A Cyperaceae-dominated community again occupied the area at about 1900 yr BP. Although the local community changed several times, the present regional forest-tundra vegetation has had little change during the last 9000 radiocarbon years.Key words: pollen analysis, paleovegetation, southwest Yukon Mots clés: analyse pollinique, paléovégétation, sud-ouest du Yukon Article in Journal/Newspaper Arctic Tundra Yukon University of Calgary Journal Hosting Ittlemit Lake ENVELOPE(-137.178,-137.178,61.201,61.201) Yukon ARCTIC 44 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Cores
Frozen ground
Palaeoclimatology
Palaeoecology
Palynology
Peat
Plant distribution
Plants (Biology)
Pollen
Radiocarbon dating
Soil profiles
Ittlemit Lake region
Yukon
spellingShingle Cores
Frozen ground
Palaeoclimatology
Palaeoecology
Palynology
Peat
Plant distribution
Plants (Biology)
Pollen
Radiocarbon dating
Soil profiles
Ittlemit Lake region
Yukon
Wang, Xia-Cheng
Geurts, Marie-Anne
Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
topic_facet Cores
Frozen ground
Palaeoclimatology
Palaeoecology
Palynology
Peat
Plant distribution
Plants (Biology)
Pollen
Radiocarbon dating
Soil profiles
Ittlemit Lake region
Yukon
description The pollen record of a 240 cm peat profile in the Ittlemit Lake area in southwest Yukon Territory presents a vegetation development history of the last 9000 radiocarbon years. Spruce migrated into the area at least 9000 radiocarbon years ago. From 9000 yr BP to approximately 5000 yr BP the area supported a sparse Picea-Salix-Betula forest-tundra vegetation. By 5000 yr BP local environmental change created a different habitat primarily affecting the local taxa. Alnus invaded the general area shortly after 5000 yr BP. A local Betula-dominated community replaced the previous Cyperaceae-dominated one at about 3000 yr BP. A Cyperaceae-dominated community again occupied the area at about 1900 yr BP. Although the local community changed several times, the present regional forest-tundra vegetation has had little change during the last 9000 radiocarbon years.Key words: pollen analysis, paleovegetation, southwest Yukon Mots clés: analyse pollinique, paléovégétation, sud-ouest du Yukon
format Article in Journal/Newspaper
author Wang, Xia-Cheng
Geurts, Marie-Anne
author_facet Wang, Xia-Cheng
Geurts, Marie-Anne
author_sort Wang, Xia-Cheng
title Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
title_short Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
title_full Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
title_fullStr Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
title_full_unstemmed Post-Glacial Vegetation History of the Ittlemit Lake Basin, Southwest Yukon Territory
title_sort post-glacial vegetation history of the ittlemit lake basin, southwest yukon territory
publisher The Arctic Institute of North America
publishDate 1991
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568
long_lat ENVELOPE(-137.178,-137.178,61.201,61.201)
geographic Ittlemit Lake
Yukon
geographic_facet Ittlemit Lake
Yukon
genre Arctic
Tundra
Yukon
genre_facet Arctic
Tundra
Yukon
op_source ARCTIC; Vol. 44 No. 1 (1991): March: 1–93; 23-30
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568/48482
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64568
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