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#iron_cycle

Iron cycle

The iron cycle (Fe) is the biogeochemical cycle of iron through the atmosphere, hydrosphere, biosphere and lithosphere. While Fe is highly abundant in the Earth's crust, it is less common in oxygenated surface waters. Iron is a key micronutrient in primary productivity, and a limiting nutrient in the Southern ocean, eastern equatorial Pacific, and the subarctic Pacific referred to as High-Nutrient, Low-Chlorophyll (HNLC) regions of the ocean.

Mon 19th

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Iron cycle Sponge iron reaction Iron Phosphorus cycle Iron oxide cycle Iron oxide Iron-oxidizing bacteria Biogeochemical cycle Nitrogen cycle Marine biogeochemical cycles
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