Increasing atmospheric CO₂ will likely affect both the hydrologic cycle and ecosystem productivity. Current assumptions that increasing CO₂ will lead to increased ecosystem productivity and plant water use efficiency (WUE) are driving optimistic predictions of higher crop yields as well as greater availability of freshwater resources due to a decrease in evapotranspiration.

Malawi is a land of farmers and facing rampant environmental problems whose capability for restoration is made dimmer by the looming shadow of climate change and variability. The Malawi Environmental Observatory Network is a small candle flickering with light for identification of prioritized environmental problems and setting of the road map of how such monumental problems could efficiently be tackled with the available meager resources.

The McMurdo Dry Valleys in Antarctica (MCM) forms one of the most extreme deserts on Earth. It consists of a mosaic of permanently ice-covered lakes, ephemeral streams, exposed soils, and glaciers. Microorganisms are the only life forms occupying these landscape units. Given the relatively low and seasonal growth rates of these organisms, we contend that the distribution of microorganisms within this environment is controlled by physical factors.

Denitrification is a key step returning nitrogen from soils to the atmosphere. The primary denitrifiers in most ecosystems are heterotrophic bacteria. Although, fungi are also known to transform nitrogen compounds, such as the production of N2O, but few studies have explored this process in soils. Aridland systems experience high temperatutres and low moisture conditions, favoring fungi in these environments. Thus, we explored the role of fungi and bacteria in denitrification of Sonoran Desert soils.

Japan Long Term Ecological Research (JaLTER) Network was established in 2006, currently consisting of 18 core sites and 38 associated sites that represent forest, grassland, lake, and marine ecosystems.
JaLTER is an official member of International LTER (ILTER) Network since 2007.

Soil respiration is a major pathway of flux in the terrestrial ecosystem carbon cycle and has received a great deal of attention recently. This is largely because even a small change in soil respiration can exacerbate the annual input of CO2 into the atmosphere. Soil respiration represents the combined respiration of roots and soil micro- and macro-organisms, and a number of studies on soil respiration have been undertaken in a variety of ecosystems.

A key climatic feature of the Shortgrass Steppe is the summertime pattern of moderate to large precipitation events, separated by weeks of hot, dry conditions. These precipitation events have potential to revive plants, microbes and soil fauna that became less active in the intervening dry period, and thus structure ecosystem-scale patterns including net carbon exchange.

Ecosystem processes in northern systems depend heavily on inputs of biologically fixed nitrogen (N) from A. tenuifolia, which contributes the majority of N accumulated during boreal forest succession. However because of the high phosphorus (P) demands of this plant, we hypothesize that N-fixation inputs are controlled by the ability of alder to assimilate P through associations with ectomycorrhizal fungi (EMF), which produce enzymes that mobilize organic and recalcitrant P forms.

A forest die-back caused by a beetle outbreak on lodgepole and limber pine was used to assess the relative importance of root inputs to the soil food web and chemistry of soils in the Colorado Front Range. We measured a suite of biological and chemical parameters at six sites containing both live and dead trees. We found an increase in amounts of soil inorganic N, decreased soil lable C, and thus a decreased soil labile C:N ratio.

The Sevilleta LTER is located at the intersection of several aridland ecosystem types. Although it is axiomatic that water is the key limiting resource in aridland ecosystems, most arid land soils are also chronically low in nutrients and organic matter. Resource availability is a function of the frequency and size of precipitation events as well as the time between events. As a consequence, NPP and organic matter decomposition are often decoupled in space and time, and soil nutrient supply rates may limit NPP during periods when soil moisture is sufficient for plant growth.