Lakeshore residential development is associated with decreases in riparian zone vegetation and littoral zone structure, and increased angling effort. Depending upon the species and their associated body size, fishes may respond differently to these changes. Responses may be particularly difficult to predict for species that undergo marked changes in habitat use and diet over ontogeny, such as the popular sportfish largemouth bass (Micropterus salmoides).

The KBS LTER site is in a diverse, rural-to-semirural landscape typical of the U.S. Great Lakes and upper Midwest regions. Research at KBS asks how diverse plants, animals, and microbes in agricultural landscapes can contribute to farm productivity, environmental performance, and profitability. We study annual and perennial crops including corn, soybean, and wheat rotations, forage crops such as alfalfa, and biofuel crops such as poplars, switchgrass, and native successional communities.

The PAL study area encompasses a 200 x 500 km region extending from the nearshore coastal zone heavily influenced by seasonal sea ice cover to the open Southern Ocean, and from a northern area where sea ice cover is now limited to only the colder winters, to the south where perennial sea ice cover persists into summer months. In this region, primary production is dominated by unicellular phytoplankton and limited by light availability to the October-April period. The region is characterized by spring phytoplankton blooms that have declined by up to 90% in the northern region since 1978.

The National Ecological Observatory Network (NEON) is a national-scale research platform for assessing the impacts of climate change, land-use change, and invasive species on ecosystem structure and function. NEON partitions the United States into 20 ecoclimate domains. Each domain hosts fully instrumented aquatic sites in permanent (wildland area) and relocatable sites (36 sites in current definition). Relocatable sites aims to capture ecologically significant contrasts within and between domains.

 The National Ecological Observatory Network (NEON) is a national-scale research platform for analyzing and understanding the impacts of climate change, land-use change, and invasive species on ecology. NEON features sensor networks and experiments, linked by advanced cyberinfrastructure to record and archive ecological data for at least 30 years. Using standardized protocols and an open data policy, NEON will gather essential data for developing the scientific understanding and theory required to manage ecological challenges.

Urban ecosystems present ecologists with the unique opportunity to study ecological communities in the context of drastic structural and environmental change unprecedented in pristine environments. Metacommunity theory organizes a suite of predictions of how species assemble locally from the regional species pool. Understanding assemblage structure in urban ecosystems requires a revised perspective embracing human behavior and decision-making.

Post-fire nutrient enrichment is known to affect benthic macroinvertebrate assemblages and stream food webs in forested regions, but little is known about the impact of tundra fires. The 2007 Anaktuvuk River fire (North Slope, Alaska), the largest recorded tundra fire (≈1,000 km²), provided an opportunity to study the first-year effects of a tundra fire on stream communities. We predicted that a tundra fire would increase inorganic nutrient inputs to streams, thereby increasing primary production and in turn, increasing abundance and biomass of benthic macroinvertebrates.

Rusty crayfish (Orconectes rusticus) are invasive in the upper Midwest United States. They often reach high densities and negatively affect native crayfish species, aquatic macrophytes, benthic invertebrates, and some fish populations. However, in some lakes rusty crayfish do not achieve high densities and do not negatively affect native biota. We conducted a whole-lake experiment designed to remove rusty crayfish from Sparkling Lake, a part of the North Temperate Lakes LTER site in Vilas County, Wisconsin.

The McMurdo Dry Valleys have no rainfall and most snowfall sublimates before wetting the soils significantly. Glacial melt streams are also seasonal, flowing for only 4 to 6 weeks per year. Consequently, hydrology does not provide significant connections among ecosystem components. Conversely, wind is a persistent daily feature of the McMurdo Dry Valleys environment throughout the year. In summer, cool air from the ice-covered oceans flows into the relatively warm valleys creating a strong thermal gradient in the valleys.