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26 Αυγ 2019 · The biogeochemical cycle of silicon (Si) interacts with relevant marine chemical and ecological processes, which include modulation of the primary production 1 and removal of atmospheric CO 2...
18 Φεβ 2021 · The element silicon (Si) is required for the growth of silicified organisms in marine environments, such as diatoms. These organisms consume vast amounts of Si together with N, P, and C, connecting the biogeochemical cycles of these elements.
In the marine silicon cycle, silicon travels from the land into the oceans via rivers and groundwater. Near the ocean’s surface, silicon is taken up by phytoplankton like diatoms and incorporated into their skeletons. When these organisms die, they sink to the bottom of the ocean.
25 Ιαν 2024 · In this article, we discuss why we need to understand the marine silicon cycle, explain the steps that happen in the ocean, and demonstrate how the marine silicon cycle affects humans.
15 Δεκ 2000 · A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy. Author links open overlay panel. O Ragueneau a. , P Tréguer a. , A Leynaert a. , R.F Anderson b. , M.A Brzezinski c. , D.J DeMaster d. , R.C Dugdale e. , J Dymond f. , G Fischer g. , R François h. ,
The element silicon (Si) is required for the growth of silicified organisms in marine environments, such as di-atoms. These organisms consume vast amounts of Si to-gether with N, P, and C, connecting the biogeochemical cy-cles of these elements.
1 Ιαν 2005 · Variations in the marine silica cycle may influence atmospheric CO 2 levels and thus global climate. Atmospheric CO 2 is dissolved in the surface ocean, where it is taken up by phytoplankton via photosynthesis. This process requires nutrients such as dissolved silicate that are available in surface waters only in limited amounts.
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