A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska

Thesis (M.S.) University of Alaska Fairbanks, 2001 Macrofossil remains and pollen from an 18,000 year old buried surface from the northern Seward Peninsula enable a reconstruction of the full-glacial environment of an upland portion of the Bering Land Bridge. The buried surface represents a dry mead...

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Main Author: Wolf, Victoria Goetcheus
Format: Thesis
Language:English
Published: 2001
Subjects:
Online Access:http://hdl.handle.net/11122/6715
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/6715 2023-05-15T15:42:39+02:00 A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska Wolf, Victoria Goetcheus 2001-12 http://hdl.handle.net/11122/6715 en_US eng http://hdl.handle.net/11122/6715 Thesis 2001 ftunivalaska 2023-02-23T21:36:42Z Thesis (M.S.) University of Alaska Fairbanks, 2001 Macrofossil remains and pollen from an 18,000 year old buried surface from the northern Seward Peninsula enable a reconstruction of the full-glacial environment of an upland portion of the Bering Land Bridge. The buried surface represents a dry meadow and herb-rich tundra. Prostrate shrubs were rare on the landscape, but abundant locally. A large and diverse insect fauna populated the surface, preying on the plants and each other. Small mammals and their predators lived on the surface. Large mammals, such as caribou and bison, were present as well. The productivity of the surface was maintained by a continual influx of loess, which replenished the nutrients of the soil. Study of the buried surface provides an important addition to knowledge about the vegetation mosaic of full-glacial Beringia. Thesis Bering Land Bridge Seward Peninsula Tundra Alaska Beringia University of Alaska: ScholarWorks@UA Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Thesis (M.S.) University of Alaska Fairbanks, 2001 Macrofossil remains and pollen from an 18,000 year old buried surface from the northern Seward Peninsula enable a reconstruction of the full-glacial environment of an upland portion of the Bering Land Bridge. The buried surface represents a dry meadow and herb-rich tundra. Prostrate shrubs were rare on the landscape, but abundant locally. A large and diverse insect fauna populated the surface, preying on the plants and each other. Small mammals and their predators lived on the surface. Large mammals, such as caribou and bison, were present as well. The productivity of the surface was maintained by a continual influx of loess, which replenished the nutrients of the soil. Study of the buried surface provides an important addition to knowledge about the vegetation mosaic of full-glacial Beringia.
format Thesis
author Wolf, Victoria Goetcheus
spellingShingle Wolf, Victoria Goetcheus
A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
author_facet Wolf, Victoria Goetcheus
author_sort Wolf, Victoria Goetcheus
title A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
title_short A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
title_full A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
title_fullStr A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
title_full_unstemmed A window to the past: macrofossil remains from an 18,000 year-old buried surface, Seward Peninsula, Alaska
title_sort window to the past: macrofossil remains from an 18,000 year-old buried surface, seward peninsula, alaska
publishDate 2001
url http://hdl.handle.net/11122/6715
geographic Fairbanks
geographic_facet Fairbanks
genre Bering Land Bridge
Seward Peninsula
Tundra
Alaska
Beringia
genre_facet Bering Land Bridge
Seward Peninsula
Tundra
Alaska
Beringia
op_relation http://hdl.handle.net/11122/6715
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