Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes
Abstract The Kenai Peninsula of south‐central Alaska is a region of high topographic diversity with a complex glacial history. The sedimentary record of two small lakes [Sunken Island (SIL; 76 m a.s.l.) in the Kenai Lowlands; Choquette (CL; 527 m a.s.l.) in the Caribou Hills upland] exemplifies the...
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crwiley:10.1002/jqs.3102 2024-09-15T18:04:07+00:00 Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes Scott Anderson, R. Berg, Edward Williams, Chris Clark, Tami 2019 http://dx.doi.org/10.1002/jqs.3102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3102 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3102 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 34, issue 4-5, page 309-322 ISSN 0267-8179 1099-1417 journal-article 2019 crwiley https://doi.org/10.1002/jqs.3102 2024-07-30T04:18:42Z Abstract The Kenai Peninsula of south‐central Alaska is a region of high topographic diversity with a complex glacial history. The sedimentary record of two small lakes [Sunken Island (SIL; 76 m a.s.l.) in the Kenai Lowlands; Choquette (CL; 527 m a.s.l.) in the Caribou Hills upland] exemplifies the postglacial development of the conifer–hardwood forest over an elevational range there. A herb–shrub tundra was established at both sites after deglaciation. By ~10.7 ka, poplar ( Populus sp.) and alder ( Alnus ) dominated the lowland forest, while alder with minor poplar occurred at the upland site. Lake levels lower than today occurred during the early Holocene until ~8 ka. Subsequently at SIL, the near‐modern Kenai birch ( Betula kenaica ) – white spruce ( Picea glauca ) forest maintained prominence throughout the Holocene. However, at CL, alder dominated with dwarf birch and other subshrubs; small amounts of white spruce arrived ~5.2 ka. Black spruce ( Picea mariana ) grew around SIL by ~4 ka, but never gained prominence at CL. Fire, a prominent agent of disturbance in the Kenai Lowlands since ~8 ka, was essentially absent at the hardwood‐dominated upland site before ~6 ka, and rare thereafter. This suggests an important link between fire and spruce in Kenai forests. Article in Journal/Newspaper Dwarf birch Tundra Alaska Wiley Online Library Journal of Quaternary Science 34 4-5 309 322 |
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Wiley Online Library |
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crwiley |
language |
English |
description |
Abstract The Kenai Peninsula of south‐central Alaska is a region of high topographic diversity with a complex glacial history. The sedimentary record of two small lakes [Sunken Island (SIL; 76 m a.s.l.) in the Kenai Lowlands; Choquette (CL; 527 m a.s.l.) in the Caribou Hills upland] exemplifies the postglacial development of the conifer–hardwood forest over an elevational range there. A herb–shrub tundra was established at both sites after deglaciation. By ~10.7 ka, poplar ( Populus sp.) and alder ( Alnus ) dominated the lowland forest, while alder with minor poplar occurred at the upland site. Lake levels lower than today occurred during the early Holocene until ~8 ka. Subsequently at SIL, the near‐modern Kenai birch ( Betula kenaica ) – white spruce ( Picea glauca ) forest maintained prominence throughout the Holocene. However, at CL, alder dominated with dwarf birch and other subshrubs; small amounts of white spruce arrived ~5.2 ka. Black spruce ( Picea mariana ) grew around SIL by ~4 ka, but never gained prominence at CL. Fire, a prominent agent of disturbance in the Kenai Lowlands since ~8 ka, was essentially absent at the hardwood‐dominated upland site before ~6 ka, and rare thereafter. This suggests an important link between fire and spruce in Kenai forests. |
format |
Article in Journal/Newspaper |
author |
Scott Anderson, R. Berg, Edward Williams, Chris Clark, Tami |
spellingShingle |
Scott Anderson, R. Berg, Edward Williams, Chris Clark, Tami Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
author_facet |
Scott Anderson, R. Berg, Edward Williams, Chris Clark, Tami |
author_sort |
Scott Anderson, R. |
title |
Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
title_short |
Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
title_full |
Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
title_fullStr |
Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
title_full_unstemmed |
Postglacial vegetation community change over an elevational gradient on the western Kenai Peninsula, Alaska: pollen records from Sunken Island and Choquette Lakes |
title_sort |
postglacial vegetation community change over an elevational gradient on the western kenai peninsula, alaska: pollen records from sunken island and choquette lakes |
publisher |
Wiley |
publishDate |
2019 |
url |
http://dx.doi.org/10.1002/jqs.3102 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.3102 https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3102 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/jqs.3102 |
genre |
Dwarf birch Tundra Alaska |
genre_facet |
Dwarf birch Tundra Alaska |
op_source |
Journal of Quaternary Science volume 34, issue 4-5, page 309-322 ISSN 0267-8179 1099-1417 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jqs.3102 |
container_title |
Journal of Quaternary Science |
container_volume |
34 |
container_issue |
4-5 |
container_start_page |
309 |
op_container_end_page |
322 |
_version_ |
1810441607105740800 |