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Department of Geography,
UTK
Laboratory of
Tree-Ring Science
Great Smoky Mountains National
Park
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Funded by the JFSP,
Project 01-3-3-32
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ABSTRACT
Table
Mountain pine is a tree species endemic to the southern
Appalachians that is heavily dependent on repeated surface
fires for successful regeneration. Since the implementation of fire suppression as a forest management
tool in the early 1900s, the fire frequency in Great Smoky
Mountains National Park and surrounding National Forests has
been dramatically altered. Without
fire, Table Mountain pine will not persist in the southern
Appalachian Mountains. We
used dendrochronology to analyze the fire history and current
age structure of Table Mountain pine populations.
This approach provided baseline information on the
current successional status of Table Mountain pine stands and
their relationships with past fire.
Cores were collected from a minimum of 75 trees at each
of five study sites in Great Smoky Mountains National Park.
Additionally, samples were taken from fire-scarred
snags, stumps, and downed logs.
Results indicated that the age structure of Table
Mountain pine populations in the park exhibits a generally
J-shaped distribution with the last major recruitment event
occurring around 70 years ago.
Fire history analysis indicated that the pre-park
Weibull Median Fire Interval was 6.8 years, while the Maximum
Hazard Interval, the longest fire-free period that can occur
before burning is highly probable, was 80.6 years.
These results indicate that the pre-park fire regime
was characterized by frequent fires. Because the post-park fire interval has been dramatically increased
by approximately 70 years of fire suppression, Table Mountain
pine is being slowly extirpated from the southern Appalachian
landscape. Data
provided by the dendrochronological techniques used in this
study are essential for the successful reintroduction of fire
to regenerate Table Mountain pine in the region.
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