Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation

Pollen analysis of two cores with discontinuous records from a peat bog near Girdwood, in south-central Alaska, provides the basis for reconstructing the first radiocarbon-dated outline of postglacial history of vegetation in the upper Turnagain Arm area of Cook Inlet. Pollen data from clayey silt u...

Full description

Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Authors: Ager, T. A., Carrara, P. E., McGeehin, J. P.
Other Authors: Fisher, Timothy
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2010
Subjects:
Online Access:http://dx.doi.org/10.1139/e10-020
http://www.nrcresearchpress.com/doi/full-xml/10.1139/E10-020
http://www.nrcresearchpress.com/doi/pdf/10.1139/E10-020
id crcansciencepubl:10.1139/e10-020
record_format openpolar
spelling crcansciencepubl:10.1139/e10-020 2024-03-03T08:43:17+00:00 Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation Ager, T. A. Carrara, P. E. McGeehin, J. P. Fisher, Timothy 2010 http://dx.doi.org/10.1139/e10-020 http://www.nrcresearchpress.com/doi/full-xml/10.1139/E10-020 http://www.nrcresearchpress.com/doi/pdf/10.1139/E10-020 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 47, issue 7, page 971-985 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 2010 crcansciencepubl https://doi.org/10.1139/e10-020 2024-02-07T10:53:39Z Pollen analysis of two cores with discontinuous records from a peat bog near Girdwood, in south-central Alaska, provides the basis for reconstructing the first radiocarbon-dated outline of postglacial history of vegetation in the upper Turnagain Arm area of Cook Inlet. Pollen data from clayey silt underlying peat at one site indicate that the earliest known vegetation in the Girdwood area was shrub–herb tundra. Tundra vegetation developed by ∼13 800 cal years BP, soon after local retreat of glacial ice from the maximum position of the Elmendorf glacial advance (∼15 000 – 11 000 cal years BP). By ∼10 900 cal years BP, the tundra vegetation became shrubbier as Betula nana , Salix , and Ericales increased, and scattered Alnus shrubs began to colonize Turnagain Arm. By ∼9600 cal years BP, Alnus thickets with Polypodiaceae ferns became the dominant vegetation. By ∼6600 cal years BP, birch trees ( Betula neoalaskana , B. kenaica ) from the Anchorage and Kenai lowlands began to spread eastward into eastern Turnagain Arm. Mountain hemlock ( Tsuga mertensiana ) began to colonize the Girdwood area by ∼3400 cal years BP, followed soon after by Sitka spruce ( Picea sitchensis ), both Pacific coastal forest species that spread westward from Prince William Sound after a long migration from southeastern Alaska. For at least the past 2700 cal years, Pacific coastal forest composed mostly of Tsuga mertensiana , Picea sitchensis , and Alnus has been the dominant vegetation of eastern Turnagain Arm. Article in Journal/Newspaper Betula nana Tundra Alaska Canadian Science Publishing Anchorage Pacific Canadian Journal of Earth Sciences 47 7 971 985
institution Open Polar
collection Canadian Science Publishing
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Ager, T. A.
Carrara, P. E.
McGeehin, J. P.
Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
topic_facet General Earth and Planetary Sciences
description Pollen analysis of two cores with discontinuous records from a peat bog near Girdwood, in south-central Alaska, provides the basis for reconstructing the first radiocarbon-dated outline of postglacial history of vegetation in the upper Turnagain Arm area of Cook Inlet. Pollen data from clayey silt underlying peat at one site indicate that the earliest known vegetation in the Girdwood area was shrub–herb tundra. Tundra vegetation developed by ∼13 800 cal years BP, soon after local retreat of glacial ice from the maximum position of the Elmendorf glacial advance (∼15 000 – 11 000 cal years BP). By ∼10 900 cal years BP, the tundra vegetation became shrubbier as Betula nana , Salix , and Ericales increased, and scattered Alnus shrubs began to colonize Turnagain Arm. By ∼9600 cal years BP, Alnus thickets with Polypodiaceae ferns became the dominant vegetation. By ∼6600 cal years BP, birch trees ( Betula neoalaskana , B. kenaica ) from the Anchorage and Kenai lowlands began to spread eastward into eastern Turnagain Arm. Mountain hemlock ( Tsuga mertensiana ) began to colonize the Girdwood area by ∼3400 cal years BP, followed soon after by Sitka spruce ( Picea sitchensis ), both Pacific coastal forest species that spread westward from Prince William Sound after a long migration from southeastern Alaska. For at least the past 2700 cal years, Pacific coastal forest composed mostly of Tsuga mertensiana , Picea sitchensis , and Alnus has been the dominant vegetation of eastern Turnagain Arm.
author2 Fisher, Timothy
format Article in Journal/Newspaper
author Ager, T. A.
Carrara, P. E.
McGeehin, J. P.
author_facet Ager, T. A.
Carrara, P. E.
McGeehin, J. P.
author_sort Ager, T. A.
title Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
title_short Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
title_full Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
title_fullStr Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
title_full_unstemmed Ecosystem development in the Girdwood area, south-central Alaska, following late Wisconsin glaciation
title_sort ecosystem development in the girdwood area, south-central alaska, following late wisconsin glaciation
publisher Canadian Science Publishing
publishDate 2010
url http://dx.doi.org/10.1139/e10-020
http://www.nrcresearchpress.com/doi/full-xml/10.1139/E10-020
http://www.nrcresearchpress.com/doi/pdf/10.1139/E10-020
geographic Anchorage
Pacific
geographic_facet Anchorage
Pacific
genre Betula nana
Tundra
Alaska
genre_facet Betula nana
Tundra
Alaska
op_source Canadian Journal of Earth Sciences
volume 47, issue 7, page 971-985
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e10-020
container_title Canadian Journal of Earth Sciences
container_volume 47
container_issue 7
container_start_page 971
op_container_end_page 985
_version_ 1792498707677052928