A Postglacial Pollen Record from Western Kodiak Island, Alaska

Excavation of organic deposits in a seasonally dry depression atop a moraine crest near the village of Karluk, on the west side of Kodiak Island, has provided a more detailed paleoenvironmental record than hitherto available for this part of the island. Radiocarbon dating indicates that the base of...

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Published in:ARCTIC
Main Authors: Nelson, Robert E., Jordan, Richard H.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1988
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64747 2023-05-15T14:19:13+02:00 A Postglacial Pollen Record from Western Kodiak Island, Alaska Nelson, Robert E. Jordan, Richard H. 1988-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747/48661 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747 ARCTIC; Vol. 41 No. 1 (1988): March: 1–90; 59-63 1923-1245 0004-0843 Alders Climate change Ferns Palaeogeography Palynology Radiocarbon dating Recent epoch Soils Stratigraphy Pyroclastics Kodiak Island Alaska info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1988 ftunivcalgaryojs 2022-03-22T21:21:53Z Excavation of organic deposits in a seasonally dry depression atop a moraine crest near the village of Karluk, on the west side of Kodiak Island, has provided a more detailed paleoenvironmental record than hitherto available for this part of the island. Radiocarbon dating indicates that the base of the section is approximately 4260 14C years in age. Seven minor volcanic ashes are recognized prior to the onset of seasonal drying of the basin at about 2330 B.P. A major ash fall (2 cm thick in section) is recorded at about 1625 B.P. The only significant woody taxon indicated in the pollen record is alder (Alnus); all other important taxa are herbaceous. This vegetation record indicates alders and ferns dominated the landscape immediately following substrate stabilization, which apparently was delayed in this area until well into the Holocene. Alder became relatively less important as soils matured and other taxa (mostly grasses) invaded. The overall record is one of vegetational and climatic stability since landscape stabilization in this area. Volcanic ashfalls have apparently had no significant long-term impact on the vegetation at the site.Key words: Alaska, Holocene, Karluk, Kodiak Island, Quaternary, geology, glaciation, paleoenvironments, palynology, radiocarbon dating, tephra Mots clés: Alaska, holocène, Karluk, île Kodiak, quaternaire, géologie, glaciation, paléoenvironnements, palynologie, datation au radiocarbone, cendres volcaniques Article in Journal/Newspaper Arctic Kodiak Alaska University of Calgary Journal Hosting ARCTIC 41 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Alders
Climate change
Ferns
Palaeogeography
Palynology
Radiocarbon dating
Recent epoch
Soils
Stratigraphy
Pyroclastics
Kodiak Island
Alaska
spellingShingle Alders
Climate change
Ferns
Palaeogeography
Palynology
Radiocarbon dating
Recent epoch
Soils
Stratigraphy
Pyroclastics
Kodiak Island
Alaska
Nelson, Robert E.
Jordan, Richard H.
A Postglacial Pollen Record from Western Kodiak Island, Alaska
topic_facet Alders
Climate change
Ferns
Palaeogeography
Palynology
Radiocarbon dating
Recent epoch
Soils
Stratigraphy
Pyroclastics
Kodiak Island
Alaska
description Excavation of organic deposits in a seasonally dry depression atop a moraine crest near the village of Karluk, on the west side of Kodiak Island, has provided a more detailed paleoenvironmental record than hitherto available for this part of the island. Radiocarbon dating indicates that the base of the section is approximately 4260 14C years in age. Seven minor volcanic ashes are recognized prior to the onset of seasonal drying of the basin at about 2330 B.P. A major ash fall (2 cm thick in section) is recorded at about 1625 B.P. The only significant woody taxon indicated in the pollen record is alder (Alnus); all other important taxa are herbaceous. This vegetation record indicates alders and ferns dominated the landscape immediately following substrate stabilization, which apparently was delayed in this area until well into the Holocene. Alder became relatively less important as soils matured and other taxa (mostly grasses) invaded. The overall record is one of vegetational and climatic stability since landscape stabilization in this area. Volcanic ashfalls have apparently had no significant long-term impact on the vegetation at the site.Key words: Alaska, Holocene, Karluk, Kodiak Island, Quaternary, geology, glaciation, paleoenvironments, palynology, radiocarbon dating, tephra Mots clés: Alaska, holocène, Karluk, île Kodiak, quaternaire, géologie, glaciation, paléoenvironnements, palynologie, datation au radiocarbone, cendres volcaniques
format Article in Journal/Newspaper
author Nelson, Robert E.
Jordan, Richard H.
author_facet Nelson, Robert E.
Jordan, Richard H.
author_sort Nelson, Robert E.
title A Postglacial Pollen Record from Western Kodiak Island, Alaska
title_short A Postglacial Pollen Record from Western Kodiak Island, Alaska
title_full A Postglacial Pollen Record from Western Kodiak Island, Alaska
title_fullStr A Postglacial Pollen Record from Western Kodiak Island, Alaska
title_full_unstemmed A Postglacial Pollen Record from Western Kodiak Island, Alaska
title_sort postglacial pollen record from western kodiak island, alaska
publisher The Arctic Institute of North America
publishDate 1988
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747
genre Arctic
Kodiak
Alaska
genre_facet Arctic
Kodiak
Alaska
op_source ARCTIC; Vol. 41 No. 1 (1988): March: 1–90; 59-63
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747/48661
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64747
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