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The shortgrass steppe (SGS) occupies the middle of the productivity gradient along
which the LTER grassland sites lie. It is unique among North American grasslands for its
long evolutionary history of intense selection by both drought and herbivory, leading to
an ecosystem that is very well adapted to withstand grazing by domestic livestock. The
distinctive features of the SGS are both its vegetation and the concentration of
biological activity and organic matter belowground. The vegetation of the SGS is
characterized by lowgrowing plants that are either tolerant or resistant to grazing and
drought. The large concentration of biological activity belowground reflects the
distribution of plant production (Milchunas and Lauenroth 1992) and the enhanced rates of
energy flow through heterotrophs belowground (Lauenroth and Milchunas 1992). It is also
explained in part by the fact that most biologically active elements in grasslands are
protected from natural disturbances by being stored in soil organic matter (SOM).
The SGS LTER project has been in operation since 1982, and currently supports 46
longterm experiments, numerous shortterm experiments, and has a large emphasis in
integrative simulation analysis. SGS LTER work is divided into 5 major areas: populations
and processes, biogeochemical dynamics, paleoecology and paleopedology, water and energy
dynamics, and disturbances.
Populations and
Processes:
Work in this area is organized by the idea that two kinds of populations are most
important in the longterm dynamics and sustainability of the SGS. The first are dominant
species, such as the shortgrass blue grama (Bouteloua gracilis), which
overwhelmingly dominates the SGS. The second kind of important population is those that
have a large effect on the ecosystem because of their unique traits; these are keystone
species and we propose that prairie dogs (Cynomys ludovicianus) and prickly pear cactus
(Opuntia polyacantha) are keystone
species in the SGS. SGSLTER past and continuing work has focused a great deal on
population dynamics of blue grama and the factors that influence its role in the system.
In addition, population dynamics of other species across the trophic structures are also
studied. New work is proposed for the next 6 years to focus on two aspects: 1.) the
biology of prairie dogs and prickly pear cactus as keystone species, and 2.) population
genetics of blue grama as they influence its resistance to grazing.
Biogeochemical Dynamics:
Our research in this area focuses on elucidating the key abiotic and
biotic variables that control biogeochemical dynamics. Continuing longterm experiments
are designed to assess how precipitation, temperature, topography, and soil texture
interact to control spatial and temporal patterns of primary productivity, nutrient
cycling, and trace gas loss. Proposed new work will address the importance of atmospheric
inputs to ecosystem processes.
Paleoecology and
Paleopedology:
Over evolutionary time scales, climatic variation has been the major force
influencing the structure and function of SGS ecosystems. Our work in this area involves
sampling the extensive paleosols across the SGS site, and evaluating their longterm
vegetative and physiographic history by analyzing the stable C isotope signatures of soil
organic matter, phytoliths, and CaCO3. These studies provide information on the
distribution of C3 and C4 plants during the Holocene soilforming
intervals.
Water and Energy
Dynamics:
The SGSLTER project identifies this area as important because water availability is the
key variable driving SGS ecosystem structure and function. Measurements of precipitation,
temperature, microclimate, and soil water are part of the longterm program. A weighing
lysimeter measures daily evapotranspiration. We propose to initiate a new study to
quantify the potential impact of current land use on the SGS by coupling a mesoscale
atmospheric model with an ecosystem dynamics model.
Disturbance:
Two key hypotheses organize SGS LTER work in the area of disturbance. The first is
that smallscale disturbances are the most important source of mortality for the dominant
plant, blue grama, and as such, these disturbances represent a major influence on the
sustainability of the shortgrass steppe. The second is that the distribution of biotic
components with a large bias towards the below- ground portion of the system leads to a
high degree of resistance of the ecosystem to aboveground disturbances such as grazing or
fire, but a high vulnerability to disturbances such as cultivation that disturb the soil
system. In addition, the evolutionary adaptations of organisms in the SGS provide
additional resistance to grazing. Continuing SGSLTER experiments evaluate the long and
shortterm effects of smallscale disturbances, grazing, and recovery from cultivation
on plant communities, primary productivity, nutrient cycling, and belowground foodweb
dynamics.
In addition, investigators involved in the SGSLTER program continue to be involved in
many synthesis activities. The SGSLTER project will produce a synthesis book this coming
year. One of the areas that has made the SGSLTER unique is our emphasis on integrating
our knowledge about SGS ecosystems into simulation models. Our models are some of the most
widely used worldwide. We plan to continue to use them to encapsulate and test our
knowledge about SGS ecosystems.

03/21/02 |