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They discovered that the higher the rock/water ratio within the container, and the faster the container spun, the more silica dissolved into solution. After analyzing and upscaling their results, they estimated that anywhere from 3.2 ± 1.0 – 5.0 ± 2.0 Tmol Si yr −1 of lithogenic DSi could enter the ocean from sandy beaches, a massive ...
Silicon enters the ocean in a dissolved form such as silicic acid or silicate. [103] Since diatoms are one of the main users of these forms of silicon, they contribute greatly to the concentration of silicon throughout the ocean. Silicon forms a nutrient-like profile in the ocean due to the diatom productivity in shallow depths. [103]
Since liquid water flows, ocean waters cycle and flow in currents around the world. Since water easily changes phase, it can be carried into the atmosphere as water vapour or frozen as an iceberg. It can then precipitate or melt to become liquid water again. All marine life is immersed in water, the matrix and womb of life itself. [7]
The remaining opal silica is exported to the deep ocean in sinking particles. [11] In the deep ocean, another 26.2 Tmol Si Year −1 is dissolved before being deposited to the sediments as opal silica. [11] At the sediment water interface, over 90% of the silica is recycled and upwelled for use again in the photic zone. [11]
The shells of dead diatoms can reach as much as a half-mile (800 m) deep on the ocean floor, and the entire Amazon basin is fertilized annually by 27 million tons of diatom shell dust transported by transatlantic winds from the African Sahara, much of it from the Bodélé Depression, which was once made up of a system of fresh-water lakes. [14 ...
Silicon forms a nutrient-like profile in the ocean due to the diatom productivity in shallow depths, which means there is less concentration of silicon in the upper ocean and more concentration of silicon in the deep ocean. [19] Diatom productivity in the upper ocean contribute to the amount of silicon exported to the lower ocean. [20]
For example, microscopic particles of silica called phytoliths can be found in grasses and other plants. Silica is an amorphous metalloid oxide formed by complex inorganic polymerization processes. This is opposed to the other major biogenic minerals, comprising carbonate and phosphate , which occur in nature as crystalline iono-covalent solids ...
Siliceous sponges are usually found in the marine ecosystem but they are occasionally found in freshwater. During the Triassic, siliceous sponges grew reefs similar to calcarea of the modern era. During the Cretaceous period, diatoms became so successful that they significantly decreased the amount of silica present in sea water, after which ...