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  2. Iron cycle - Wikipedia

    en.wikipedia.org/wiki/Iron_cycle

    The ocean is a critical component of the Earth's climate system, and the iron cycle plays a key role in ocean primary productivity and marine ecosystem function. Iron limitation has been known to limit the efficiency of the biological carbon pump.

  3. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Iron is a key micronutrient in primary productivity, [49] 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. [50] Iron in the ocean cycles between plankton, aggregated particulates (non-bioavailable iron), and dissolved ...

  4. Iron fertilization - Wikipedia

    en.wikipedia.org/wiki/Iron_fertilization

    Ocean iron fertilization is an example of a geoengineering technique that involves intentional introduction of iron-rich deposits into oceans, and is aimed to enhance biological productivity of organisms in ocean waters in order to increase carbon dioxide (CO 2) uptake from the atmosphere, possibly resulting in mitigating its global warming effects.

  5. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    Ocean stratification is the natural separation of an ocean's ... which can be linked with the strong variations in the thermocline depth in ... iron and magnesium, de ...

  6. High-nutrient, low-chlorophyll regions - Wikipedia

    en.wikipedia.org/wiki/High-nutrient,_low...

    Iron is a critical phytoplankton micronutrient necessary for enzyme catalysis and electron transport. [3] [4] Between the 1930s and '80s, it was hypothesized that iron is a limiting ocean micronutrient, but there were not sufficient methods reliably to detect iron in seawater to confirm this hypothesis. [5]

  7. Iron in biology - Wikipedia

    en.wikipedia.org/wiki/Iron_in_biology

    Iron can also be oxidized by marine microbes under conditions that are high in iron and low in oxygen. [53] Iron can enter marine systems through adjoining rivers and directly from the atmosphere. Once iron enters the ocean, it can be distributed throughout the water column through ocean mixing and through recycling on the cellular level. [54]

  8. Great Oxidation Event - Wikipedia

    en.wikipedia.org/wiki/Great_Oxidation_Event

    The iron in banded iron formations is partially oxidized, with roughly equal amounts of ferrous and ferric iron. [32] Deposition of a banded iron formation requires both an anoxic deep ocean capable of transporting iron in soluble ferrous form, and an oxidized shallow ocean where the ferrous iron is oxidized to insoluble ferric iron and ...

  9. Ocean fertilization - Wikipedia

    en.wikipedia.org/wiki/Ocean_fertilization

    Large algal blooms can be created by supplying iron to iron-deficient ocean waters. These blooms can nourish other organisms. Ocean iron fertilization is an example of a geoengineering technique. [12] Iron fertilization [13] attempts to encourage phytoplankton growth, which removes carbon from the atmosphere for at least a period of time.