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Structure and Function of Chihuahuan Desert
Structure and Function of Chihuahuan Desert

... Desert Rangeland Research Center (CDRRC) during the twentieth century. Early studies dealt with animal species that were thought to reduce the amount of primary production that was available to support livestock. With the establishment of the International Biological Programme (IBP) in the late 1960 ...
Ward et al. - Massachusetts Institute of Technology
Ward et al. - Massachusetts Institute of Technology

... importance of both nutrient and grazer controls. The model suggests that zooplankton : phytoplankton (Z : P) biomass ratios may vary from an order of 0.1 in the oligotrophic gyres to an order of 10 in upwelling and highlatitude regions. Global estimates of the strength of bottom-up and top-down cont ...
Soil Invertebrates and Abiotic Factors
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... The Ecology of Soil Invertebrates The soil is a radically different environment for life than the ones on and above the ground; yet the essential requirements do not differ. Like organisms that live outside the soil, life in the soil requires living space, oxygen, food, and water. Without the prese ...
Marine Ecology Progress Series 282:87
Marine Ecology Progress Series 282:87

... merged aquatic vegetation because it stimulates overnecessary for reversing seagrass declines, given that growth of epiphytic algae and macroalgae from the the eutrophication and overfishing hypotheses predi‘bottom-up’ (Walker & McComb 1992, Duarte 1995, cate very different management responses. How ...
DECOMPOSER INSECTS
DECOMPOSER INSECTS

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UV radiation changes algal stoichiometry but does not have
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... found either in the atmosphere or dissolved in ocean waters. • Plants and other producers convert carbon dioxide to glucose during photosynthesis. • Carbon is returned to the environment by living organisms as carbon dioxide, a product of cellular respiration. • Because atmospheric carbon dioxide tr ...
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soil structure stability and distribution of carbon in water

... on the critical level of organic matter. These effects were more positive in MT than in CT as well as in CR+NPK compared to NPK and Co. However, in the long term this effect was observed in CT, as illustrated by the results of 13 years (Šimanský et al., 2008), because in intensive cultivated soils the ...
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Full text in pdf format
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rain forests: floristics

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... Wu & Sun 2010), the community includes a diverse detritivore assemblage, including beetles, flies, ants, earthworms and their associated predators (e.g. spiders, centipedes and predatory beetles; Wu & Sun 2010). At our study site, there are two earthworm species, Aporrectodea nocturna and Pheretima ...
Bioaugmentation-A Strategy For Cleaning Up Soil
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... Augmentation approaches appears to have a great potential for cleaning of aromatic compounds. The most important step in bioaugmentation is selection of microbial strains. The principle of bioaugmentation can be achieved by using microbial inoculants isolated from environments where contamination ha ...
Wildlife Management - Midlands State University
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Biodiversity Conservation
Biodiversity Conservation

... Students will obtain knowledge about the actual management rules regarding the protection of biological diversity (including genes, species and habitats); with this information, relevant research questions should be formulated taking into account actual socio-economic problems. Fundamental biologica ...
Accounting for soil biotic effects on soil health and crop productivity
Accounting for soil biotic effects on soil health and crop productivity

... a Algoma University, Sault Ste Marie, Ontario, P6A 2G4, Canada b Sault Ste Marie Innovation Centre, Sault Ste Marie, Ontario, P6A 2G4, Canada ...
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Human impact on the nitrogen cycle



Human impact on the nitrogen cycle is diverse. Agricultural and industrial nitrogen (N) inputs to the environment currently exceed inputs from natural N fixation. As a consequence of anthropogenic inputs, the global nitrogen cycle (Fig. 1) has been significantly altered over the past century. Global atmospheric nitrous oxide (N2O) mole fractions have increased from a pre-industrial value of ~270 nmol/mol to ~319 nmol/mol in 2005. Human activities account for over one-third of N2O emissions, most of which are due to the agricultural sector. This article is intended to give a brief review of the history of anthropogenic N inputs, and reported impacts of nitrogen inputs on selected terrestrial and aquatic ecosystems.
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