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16 The Biosphere and Ecological Relationships
16 The Biosphere and Ecological Relationships

... The largest store of nitrogen is in the atmosphere in the form gaseous N2. Approximately 78% of the Earth’s atmosphere is N2 gas. Nitrogen combines with oxygen to form nitrates (NO3- ) and with hydrogen to form ammonia (NH3) and the ammonium ion (NH4+). It is made into proteins, DNA and RNA by plant ...
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... example, many fish species consume squid. Most of these species eat other fish too. A consumer may prey on both primary and secondary consumers as well as on decomposers. Robins, for example, consume both plant-eating insects and decomposers, such as earthworms. Omnivores, such as humans, eat a vari ...
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... • Melting of permafrost releases large amounts of carbon into the atmosphere increasing • “Greenhouse Affect” as organic matter decays and released carbon dioxide. • Erosion is emerging due to permafrost thaw and overgrazing • Poaching – hunting and fishing out of season, on protected land, or to en ...
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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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