Past Research 1996-2002
P-IIC: Linkages Among
Spatial Variation in Plant Quality, Herbivore Population Dynamics, and Soil
Processes
Summary:
We are investigating a cascading pattern of effects concerning plants,
bugs, and soil.
Specifically, we are interested in how patterns of
environmental heterogeneity
with plants (level one) influence the spatial distribution of
herbivorous insect species and how that influences environmental
heterogeneity patterns in soil processes through leaf fall (level two).
We hypothesize
that heterogeneity in leaf quality for herbivores determines the
spatial
distribution of herbivores. The heterogeneous patterns of
defoliation that
result may influence soil processes by modifying inputs to the forest floor
(ie. decomposing leaves).
Herbivory levels on canopy trees at Coweeta
vary with elevation (Reynolds, 1995), therefore we are interested in to what extent does
spatial variation in the quality and availability of foliage explain
patterns of herbivory along the elevation gradient? and 2) what are the
effects of these patterns of defoliation on the densities and
activities of
soil microarthropods?
Our research has been broken into two
projects, one for each level.
P-IIC1. Herbivory and plant quality
P-IIC2.
Herbivory and soil processes
To learn more about insects and their roles in the ecosystem, please see US
Department of Agriculture's
Agriculture Research Service web site on the
chemical ecology of insects.
P-IIC1. Herbivory and plant quality
Summary: Two factors determine the densities of defoliating insects on
oak trees worldwide: the timing of budburst and leaf-fall and foliar
phenolics.
The
phenology of oak
budburst and leaf-fall influence
herbivore densities among individual trees. Trees that leaf out early and
drop foliage late often support the highest densities of defoliating insects
(Hunter 1992). Second, concentrations of
foliar phenolics influence
herbivore densities among trees. High
tannin
amounts result in low
densities of leaf-chewing insects (Hunter 1996). Tree phenology and tannin
concentrations for oak insects are unstudied along
elevational gradients.
Coweeta Basin is ideal for this
because:
1) Oak foliage remains for four weeks longer at lower elevations than at
higher elevations at Coweeta.
2) Nutrient
availability (which affects foliar phenolic concentrations) is known at five
elevation gradient plots, and varies among plots (Griffith 1993).
3)
Canopy walkways facilitate estimating herbivore population densities, herbivory levels, and foliage chemistry (Reynolds and Crossley 1995).
Using a
photographic method (Hunter, Reynolds), to estimate
budburst dates from individual trees of each important canopy tree species (Quercus rubra
(red oak), Q. prinus ( Oak) and Acer rubrum (red maple). Photographs
of expanding buds were taken weekly and scanned from slides onto a computer to measure bud and leaf expansion and to estimate the date of 50%
leaf expansion. Budburst estimates are made at each of the
five gradient plots. Measures of phenolic chemistry
are made from the same trees once each month from full leaf
expansion to leaf-fall. Branches are collected by a combination
of
shotgun sampling and
collection from canopy walkways. Small disks are
punched from leaves and placed in methanol for
high performance liquid chromatography (HPLC) analysis. HPLC analysis is used for simple
phenolics (for tannins),
depsides, and
flavonoids. Sequential extraction provides an
estimate of total phenolics, including tannins (Waterman and Mole 1994).
Herbivore densities and herbivory are estimated monthly that are accessible
from canopy walkways (methods in Hunter 1992, 1994).
P-IIC2. Herbivory and soil processes
Summary: Although herbivory
may have a dramatic effect on nutrient availability and decomposition in
soils, the relationships between canopy herbivory and soil processes are
poorly known in forest systems.
Canopy defoliation results in a variety of inputs into soils via
insect frass, modified
stem- and
through-fall, and green-fall (portions
of leaves dropped during defoliation by herbivores). For example, Crossley et al. (1988) reported large inputs of ammonium and phosphate to
forest floors, and nitrates to a stream following an insect outbreak (Alsophila
pometaria) at Coweeta. Litter arthropod diversity and abundance may increase
following defoliation events (Schowalter and Sabin 1991). The elevation gradient at Coweeta provides
an opportunity to study the effects of spatial heterogeneity in defoliation
levels on soil microarthropod abundance and decomposition. We will collect
frass in
funnel traps by opening 12 traps at each gradient plot for 4 hours
of daylight and 4 hours of darkness once each month from leaf expansion
through leaf-fall (12 traps x 5 plots = 60 samples per month). These will be
used for estimates of frass fall, and related to herbivore densities
(above). An additional 12
through-fall traps, adjacent to the frass traps,
will be used to assess the effects of herbivory on ammonium and phosphate
concentrations in through-fall (again, correlated with herbivore densities
and defoliation). The abundance and diversity of
oribatid mites will be
measured monthly in 12 individual 1m2 quadrats directly adjacent to the
frass and through-fall traps in each gradient plot. Litter-fall traps
already established at each site will be used to estimate green-fall. From
1996-1998, we gathered estimates of frass-fall, green-fall, and
through-fall for each plot, as described. From 1999-2001, frass-fall,
green-fall, and throughfall are manipulated experimentally into quadrats (using data from
1996-98
to establish appropriate quantities for manipulation). Quadrats receive
either half or double the average input of frass (group 1), green-fall
(group 2), or through-fall (group 3) and compared with controls (group 4).
Each treatment (and controls) are replicated 6 times per plot. The
response of oribatid mite density and diversity to experimental manipulation
of herbivore-derived inputs are measured monthly in each experimental quadrat
from 1999-2001 of the project. Overall, we will use
correlation and analysis of variance techniques to establish the effects of
natural (sampling) and experimental (manipulated) additions of
herbivore-derived inputs for soil arthropod abundance and diversity.
Investigators and Collaborators:
Mark Hunter
D.A. Crossley
Previous
(P-IIB) |
Next (P-IID) |