The distribution of Adélie penguins along the West Antarctic Peninsula (WAP) is spatially heterogeneous. Large Adélie colonies occur spatially in regions characterized by deep seafloor canyons. Often associated with these regions is persistent upwelling of warm, nutrient-rich UCDW, which is hypothesized to provide a predictable food resource close to the colonies such that they can be accessed by the penguins given their limited foraging range.

Relatively little attention has been given to the processes that control the production and subsequent availability of amino acids in temperate forest soils. We examined how differences in soil organic matter chemistry and mycorrhizal association between temperate forest tree species of the Northeastern US lead to variation in amino acid cycling. We measured amino acid cycling throughout the growing season in soils from single tree species plots located in both the Harvard Forest, MA and the Pisgah State Forest, NH.

The southern California Current System (CCS) is a moderate upwelling system comprised of water masses with differing nutrient loadings and consequently community structure. The mesozooplankton community of the CCS is dominated by copepods and euphausiids; the copepod species Calanus pacificus is one of the two dominant copepod species in this region, and the dominant euphausiid species is Euphausia pacifica. The abundances of both of these species vary significantly with El Niño Southern Oscillation conditions.

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.

Although temperate forests have long been thought to be primarily nitrogen limited, resource optimization theory suggests that ecosystem productivity should be co-limited by multiple nutrients. In northeastern North America, air pollution and forest harvesting disturbance elevate N availability and contribute to the likelihood of P limitation.

 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.

In arid ecosystems, current year precipitation explains a low proportion of the annual aboveground net primary production (ANPP). There is evidence that precipitation that occurred in previous years is responsible for the observed difference between actual and expected ANPP, a concept called legacy. Here, we study the mechanisms that generate these legacies, thus we will able to better understand the controls of the global carbon cycle, and to forecast changes in ANPP with a changing climate.

Barrier islands may represent an underestimated sink for atmospheric carbon because they combine potential for high above-ground primary productivity (ANPP) with young, infertile soils capable of sequestering significant amounts of carbon. Ecosystem ANPP on many barrier islands of the Virginia Coast Reserve (VCR) has been further enhanced by the rapid expansion of woody shrubs. Compared to adjacent grasslands, shrubs in coastal systems combine high leaf area index with high photosynthetic rates.

Primary production in arid and semiarid systems is predominantly limited by water availability. Precipitation is a strong predictor of primary production at broad scales in these systems. However, due to local variability in soil-water availability associated with landscape position, soil characteristics, and species composition, precipitation can be a pore predictor of production at finer scales. Thus, measured soil moisture content should provide a better predictor of primary production at fine scales.