Southwestern Ecological Restoration Project
Mt
Trumbull, Arizona
Summary of 1996 annual report
(complete
text available at http://www.for.nau.edu/-pzf)
Research Design
The adaptive ecological restoration experiment will test the general hypothesis
that ecosystem restoration in ponderosa pine can restore ecosystem health, reduce
crown fire risk, and enhance indigenous biodiversity, while improving human
habitats.
Hierarchical
scaling in space, time, and trophic levels
· Hierarchical ecological structures have often been ignored in research
and management but must be addressed in landscape-scale restoration.
· Spatial scale: Ponderosa and related long-needled pines range
from southwestern Canada to northern Mexico. The ponderosa pine landscape at
Mt Trumbull covers about 17,000 acres. Inside the overall boundaries of the
ponderosa pine-dominated area are meadows, sagebrush communities, "stringers"
of pinyon and juniper woodland, and stands of Gambel oak and New Mexican locust.
Forest stands are clumpy with varying species, densities, and sizes of trees.
Individual plants may range in size from 90feet-tall dominants to seedlings.
Sub-plant scales include leaves, stems, and roots, with the finest definable
spatial scales probably occurring at the level of sod biochemistry. Disturbance
patterns vary in scale from fires that may cover the entire forest, to small
patchy fires or clumps of bark beetle mortality, down to individual mortality
of plants or plant parts (defoliation).
· Temporal scale: The evolutionary context is set within the Holocene
period (past 10,000 years), characterized by glacial retreat and northward and
upward colonization of long-needled pines. Human presence on the Arizona Strip
is documented beginning approximately 6,000 years before present. Time periods
associated with biological activities range from several thousand years (soil
development), to 600+ years (tree lifespans), to 20-40 year pulses of tree establishment,
to one to several year lifespans of understory plants and dominant animals.
Organisms are affected by seasonal and daily change, with the finest definable
scales ranging down to the rates of chemical processes (photosynthesis, combustion).
Disturbance patterns also have varying cycles in a hierarchy of time, ranging
from daily and seasonal changes (fire behavior, fire season), to annual or multi-year
occurrence (fire frequency), extending to long-term changes
wish
climatic fluctuation.
· Trophic hierarchies: A broad general view (autotroph-herbivore-predator-detritivore)
can be split into an extremely fine separation of subspecies and races. At the
finest level of detail there are likely to be organisms which have never been
identified (fungi, microorganisms). An intermediate trophic categorization may
be based on functional attributes, for example aggregating insects into guilds
based on their feeding behavior.
Key variables
· How can appropriate studies be designed given the tremendous diversity
and huge changes of scale inherent in nature?
· Keystone hypothesis: Certain scales and ecological thresholds
are controlled by a small group of keystone organisms and abiotic processes.
This structuring set, in turn, strongly affects its own environment and that
of the other members of the community. Dominant species and predominant contagious
disturbance regimes maintain this self-reinforcing hierarchical pattern of ecosystem
structure and function across the landscape (Holling 1992, Perry 1995).
· Key structuring organisms in the ponderosa pine ecosystem include the
trees, herbaceous plants, and animals (mammals, birds, insects) which range
within the spatial extent of the forest. Key disturbance forces include fire
and human activity. Scales of study should be related to the relevant spatial
scales of the key variables (e.g., ponderosa pine distribution, presettlement
fire size) as well as the temporal scales (slowest living variable in the system,
e.g., 600+ year age of oldest trees).
Landscape-scale research design
· Success
in determining the effects of the Mt Trumbull restoration treatments and ability
to apply knowledge to other settings depends on our ability to evaluate the
treatments. However, traditional experimental methodologies based on small-plot
studies and 'agricultural' experimental models are not well suited to landscape-level
research.
oak clumps
that have not been thinned, a relationship between oak thinning and growth
rate may be established. Old-growth Gambel oak trees are also found in a range
of densities: growing in isolation or surrounded by numerous sprouts. Evaluating
the growth rate for oaks found in isolation versus those surrounded by sprouts
will indicate whether sprouting has an effect on growth rate and survival. In
each case growth rates will be measured with dendroecological (tree-ring) methods.
Status: sampling complete at Mt Trumbull.
Year 2: sampling at other sites and analysis.
Completion: 1997.
Wilderness restoration methods
Ecological restoration is especially important in wilderness areas and parks,
places which have been deliberately set aside to preserve natural ecosystems.
Simple reintroduction of prescribed fire into altered ponderosa ecosystems is
not sufficient to restore the functioning natural ecosystem. However, application
of restoration methods such as removal of dense trees, propagation of native
understory plants, and treatment of accumulated fuels to protect old trees,
may conflict at times with traditional perceptions of appropriate management
techniques for these protected areas. The objective of this study is twofold:
first, to develop and test 'minimal impact' restoration techniques. Examples
may include hand felling of trees, the use of animal power to remove debris,
and firing techniques designed to thin trees and consume fuels. The second objective
is to explore the social and political context of wilderness and park management
in order to seek a consensus on suitable ecological restoration goals and methods
in these areas.
Status: initial study design and literature review.
Year 2: complete design and initiate small-scale (I acre) test treatments.
Completion: 1998.
Dendroclimatic reconstruction
Climate history over the past several hundred years is recorded in the varying
widths of tree rings. Climate has an important influence both on vegetation
(species composition, establishment, growth, and mortality) and on the patterns
of disturbances such as fire. Increment cores were collected in 1996 from old
ponderosa. pine trees growing on sites highly sensitive to climatic fluctuations,
such as high, rocky ridges. After these cores are crossdated and measured to
develop a long tree-ring width chronology for the Mt Trumbull area, the chronology
will be correlated with weather data. 'Me model will reconstruct past climatic
trends and will be compared with tree age data and fire history results to search
for past climateplant-disturbance connections and to suggest potential future
changes.
Status: sampling complete.
Year 2: dendrochronological analysis and climatic reconstruction.
Completion: 1997.
Fire history
Frequent, low-intensity fire regimes are characteristic of ponderosa pine throughout
its range, but specific knowledge of the characteristics of presettlement fire
patterns at Mt Trumbull is important to guide the re-introduction of fire and
to permit future evaluation of the restored fire disturbance regime. Fire history
reconstruction based on dendrochronological measurement of fire-scarred trees,
stumps, and logs is being undertaken at Mt Trumbull to estimate the frequency
and seasonality of presettlement fire as wen as determining the date
of fire exclusion and developing a record of any postsettlement fires. A key
feature of the project is the landscape scale of sampling across the entire
ponderosa pine forest, allowing us to explore questions of fire size, intensity,
and variability within the ecosystem, issues which have exceeded the scope of
many previous studies. Preliminary results are presented on pages 35-36.
other factors
of soil formation relatively similar (climate, topography, parent material and
time), soils that develop underneath ponderosa pine trees can be quite different
than soils that develop underneath grass. Phytolith and soil characteristics
are presently being examined at 6 study sites in the Gus Pearson Natural Area
near Flagstaff and sampling will be extended to Mt Trumbull and other sites
in 1997.
Status: testing of method.
Year 2: sampling at Mt Trumbull.
Completion: multi-year.
With increased funding available at the end of year 1, the following selected
studies will be designed to complement the ecosystem restoration research in
year 2:
Physiological response of presettlement trees: to be developed in year 2.
Changes in soil chemistry and nutrient cycling: to be developed in year 2.
Small mammal habitat changes: to be developed in year 2.
Native American ecosystem management practices: to be developed in year 2.