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  2. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    The surface ocean engages in air-sea interactions and absorbs carbon dioxide (CO 2) from the atmosphere, making the ocean the Earth's largest sink for atmospheric CO 2. Carbon dioxide dissolves in and reacts with seawater to form carbonic acid. Subsequent reactions then produce carbonate (CO 3 2−), bicarbonate (HCO 3 −), and hydrogen (H ...

  3. Marine biogeochemical cycles - Wikipedia

    en.wikipedia.org/wiki/Marine_biogeochemical_cycles

    Winds drive ocean currents in the upper 100 meters of the ocean's surface. However, ocean currents also flow thousands of meters below the surface. These deep-ocean currents are driven by differences in the water's density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation.

  4. Mesopelagic zone - Wikipedia

    en.wikipedia.org/wiki/Mesopelagic_zone

    The mesopelagic zone plays a key role in the ocean's biological pump, which contributes to the oceanic carbon cycle. In the biological pump, organic carbon is produced in the surface euphotic zone where light promotes photosynthesis. A fraction of this production is exported out of the surface mixed layer and into the mesopelagic zone.

  5. Ocean stratification - Wikipedia

    en.wikipedia.org/wiki/Ocean_stratification

    The microbial pump is likely to play a larger role in nutrient cycling in the stratified surface ocean with less biological activity occurring to move dissolved organic carbon to the deep ocean [18]. As water stratification increases, the amount of dissolved oxygen made available to organisms further from the surface decreases [21].

  6. Marine chemistry - Wikipedia

    en.wikipedia.org/wiki/Marine_chemistry

    Warmer ocean water holds less oxygen and is more buoyant than cooler water. This leads to reduced mixing of oxygenated water near the surface with deeper water, which naturally contains less oxygen. Warmer water also raises oxygen demand from living organisms; as a result, less oxygen is available for marine life. [40]

  7. A new volcano-like structure has been found in the Arctic ...

    www.aol.com/news/volcano-structure-found-arctic...

    Then, they found a new volcano-like formation deep in the ocean waters. The new volcano-like structure sits more than 1,600 meters from the water's surface. So, it's far too deep to pose a danger ...

  8. Marine primary production - Wikipedia

    en.wikipedia.org/wiki/Marine_primary_production

    Some of these processes take place in deep water so that where there is an upwelling of cold waters, and also near estuaries where land-sourced nutrients are present, plant growth is higher. This means that the most productive areas, rich in plankton and therefore also in fish, are mainly coastal. [79]: 160–163

  9. A New Study Says Microplastics Are Widespread in Seafood ...

    www.aol.com/study-says-microplastics-widespread...

    It's important to note that researchers are "not advocating for people to stay away from seafood," as microplastics are already contaminating just about everything, including "bottled water, beer ...