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Compare the nitrogen, carbon, and oxygen cycles. short paragraph
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The nitrogen, carbon, and oxygen cycles all circulate essential elements between the atmosphere, biosphere, hydrosphere, and lithosphere, but they differ in key processes and reservoirs. Carbon cycles rapidly through photosynthesis, respiration, decomposition and more slowly through sedimentation and fossil-fuel formation, with large reservoirs in rocks, soils, oceans, and the atmosphere (CO2); human fossil-fuel burning and land-use change have driven a rapid increase in atmospheric CO2. Nitrogen requires specialized biological and microbial transformations—nitrogen fixation, nitrification, denitrification and ammonification—because most organisms cannot use atmospheric N2 directly; human fertilizer use and fossil-fuel combustion have greatly altered the nitrogen balance, causing eutrophication and atmospheric pollution. Oxygen cycling is tightly coupled to the carbon cycle—produced by photosynthesis and consumed by respiration, decay, and combustion—with its atmospheric abundance buffered by large reservoirs and geological processes. Together these cycles interact (e.g., CO2 uptake affects O2 levels; nitrogen availability limits carbon uptake) and are all being disrupted by human activities.
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