- Library Home /
- Search Collections /
- Open Collections /
- Browse Collections /
- UBC Theses and Dissertations /
- Aspen, elk, and fire in the Canadian Rocky Mountains
Open Collections
UBC Theses and Dissertations
UBC Theses and Dissertations
Aspen, elk, and fire in the Canadian Rocky Mountains White, Cliff
Abstract
Trembling aspen (Populus tremuloides) is failing to survive through the sapling stage (2 to 4 m) to tree size in many national parks in western North America. Hypotheses for aspen decline include reduced burning, climate change, high herbivory by native ungulates (mainly elk (Cervus elaphus)), or interactions between these factors. Historic and current aspen condition was investigated in several watersheds, inside and outside of national parks, in the Rocky Mountains of Alberta, Canada to determine the causes of aspen decline. Methods included repeats of historical photographs, fire history by dendrochronology, time-series analysis (of climate, burned area, elk density, and aspen regeneration), wildlife exclosure measurements, analysis of elk functional herbivory response to aspen density, and effects of predation risk on elk-aspen foraging patterns. Aspen regeneration was abundant in historic photographs, is currently abundant in areas with low elk density (<2 elk/ km ), but has declined precipitously in national park areas with high elk density. Historic anthropogenic burning appeared to be important along valley-bottom corridors occupied by aspen, but declined c. 1900 due to changes in cultural land uses. Yearly fluctuations in climatic conditions or burned area did not appear to be factors in aspen decline. Aspen is regenerating in wildlife exclosures on a range of site moisture conditions. Thus, climate or disturbance, either individually, or interactively with herbivory, do not appear to be major factors in aspen decline. However, elk herbivory was a highly significant factor. Elk-aspen herbivory followed a Type 2 functional response (decreased rates of browsing at higher densities of aspen regeneration) that may have occurred because predation sensitive elk avoided dense aspen stands. Historically, valley-bottom aspen habitats were heavily used by predators (humans and wolves) which reduced elk herbivory, and were frequently human-burned which stimulated regeneration of dense stems. Current land uses in national parks (with control of hunting and fire, and high human use that displaces wary predators but habituates elk) are the opposite of these long-term processes. Successful aspen regeneration will likely require a period of very low densities of elk that are wary of predators and humans, followed by restoration of anthropogenic burning.
Item Metadata
Title |
Aspen, elk, and fire in the Canadian Rocky Mountains
|
Creator | |
Publisher |
University of British Columbia
|
Date Issued |
2001
|
Description |
Trembling aspen (Populus tremuloides) is failing to survive through the sapling
stage (2 to 4 m) to tree size in many national parks in western North America.
Hypotheses for aspen decline include reduced burning, climate change, high herbivory by
native ungulates (mainly elk (Cervus elaphus)), or interactions between these factors.
Historic and current aspen condition was investigated in several watersheds, inside and
outside of national parks, in the Rocky Mountains of Alberta, Canada to determine the
causes of aspen decline. Methods included repeats of historical photographs, fire history
by dendrochronology, time-series analysis (of climate, burned area, elk density, and
aspen regeneration), wildlife exclosure measurements, analysis of elk functional
herbivory response to aspen density, and effects of predation risk on elk-aspen foraging
patterns. Aspen regeneration was abundant in historic photographs, is currently abundant
in areas with low elk density (<2 elk/ km ), but has declined precipitously in national
park areas with high elk density. Historic anthropogenic burning appeared to be
important along valley-bottom corridors occupied by aspen, but declined c. 1900 due to
changes in cultural land uses. Yearly fluctuations in climatic conditions or burned area
did not appear to be factors in aspen decline. Aspen is regenerating in wildlife exclosures
on a range of site moisture conditions. Thus, climate or disturbance, either individually,
or interactively with herbivory, do not appear to be major factors in aspen decline.
However, elk herbivory was a highly significant factor. Elk-aspen herbivory followed a
Type 2 functional response (decreased rates of browsing at higher densities of aspen
regeneration) that may have occurred because predation sensitive elk avoided dense
aspen stands. Historically, valley-bottom aspen habitats were heavily used by predators
(humans and wolves) which reduced elk herbivory, and were frequently human-burned
which stimulated regeneration of dense stems. Current land uses in national parks (with
control of hunting and fire, and high human use that displaces wary predators but
habituates elk) are the opposite of these long-term processes. Successful aspen
regeneration will likely require a period of very low densities of elk that are wary of
predators and humans, followed by restoration of anthropogenic burning.
|
Extent |
13653301 bytes
|
Genre | |
Type | |
File Format |
application/pdf
|
Language |
eng
|
Date Available |
2009-10-09
|
Provider |
Vancouver : University of British Columbia Library
|
Rights |
For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use.
|
DOI |
10.14288/1.0090793
|
URI | |
Degree | |
Program | |
Affiliation | |
Degree Grantor |
University of British Columbia
|
Graduation Date |
2001-11
|
Campus | |
Scholarly Level |
Graduate
|
Aggregated Source Repository |
DSpace
|
Item Media
Item Citations and Data
Rights
For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use.