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Science Grade 6 – Grade Level Expectations
Science Grade 6 – Grade Level Expectations

... Describe the interactions among the parts of the Earth's systems (hydrosphere, lithosphere). CHANGES Processes and Interactions in the Earth System Differentiate between changes that happened quickly and those that have occurred over a long period of time. Identify and describe how rocks chang ...
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Unit B: Interdependence and Relationships Among Organisms
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... Most of the specific research on the relationships between biodiversity and ecosystem functioning has been carried out at a small spatial scale, such as the microcosm or mesocosm, but also over a short time scale (a few generations) (Bengtsson et al., 2002; Naeem and Wright, 2003). Happily, there a ...
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... Scavenger communities play vital roles in nutrient cycling and redistribution as well as disease dynamics via the removal of carrion from the environment, providing a crucial ecosystem service and are therefore ecologically integral for healthy ecosystem functioning. The disruption of intact scaveng ...
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... resource would decrease with nitrogen deposition (perennial C4 grasses, legumes; Tilman 1984). Finally, we hypothesized that seed production responses to declining diversity would be similar to reproductive responses to nitrogen deposition, because declining diversity increases the availability of n ...
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... such as farming. For example, a forest fire might kill all the trees and other plants in a forest, leaving behind only charred wood and soil. Does a changing ecosystem ever stop changing? Does its community of organisms ever reach some final, stable state? Scientists used to think that ecological su ...
Joanna Kolasinski resume - USF College of Marine Science
Joanna Kolasinski resume - USF College of Marine Science

... Linking ramped pyrolysis isotope data to oil content through PAH analysis. Environmental Research Letters 8 044038 doi:10.1088/1748-9326/8/4/044038 ...
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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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