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The silica cycle is the biogeochemical cycle in which biogenic silica is transported between the Earth's systems. Silicon is considered a bioessential element and is one of the most abundant elements on Earth. The silica cycle has significant overlap with the carbon cycle (see carbonate–silicate cycle) and plays an important role in the sequestration of carbon through continental weathering, biogenic export and burial as oozes on geologic timescales.

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  • Ciclo del silicio (es)
  • Cycle du dioxyde de silicium (fr)
  • Silica cycle (en)
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  • El ciclo del silicio es un ciclo biogeoquímico durante el cual los minerales de silicio se intercambian entre diferentes organismos y la corteza terrestre. El silicio es un bioelemento esencial para algunos seres vivos y uno los elementos más abundantes en la tierra, especialmente en forma de dióxido de silicio o sílice (SiO2). El ciclo del silicio tiene lugar mediante la meteorización de las rocas, la exportación biogénica y el entierro como sedimentos marinos en escalas de tiempo geológicas. Presenta un alto grado de solapamiento con el ciclo del carbono y tiene una función importante en el secuestro de carbono.​​​ (es)
  • Le cycle du dioxyde de silicium est le cycle biogéochimique dans lequel le dioxyde de silicium SiO2 (ou silice) est transféré entre les différents systèmes terrestres. Le silicium est un élément bioessentiel et c'est aussi l'un des éléments les plus abondants sur Terre. Le cycle du dioxyde de silicium a un chevauchement significatif avec le cycle du carbone (cycle carbonate-silicate) et joue un rôle important dans l'enfermement du carbone par le biais de l'altération continentale, de l'exportation biogénique et de l'enfouissement sous forme de limons à l'échelle des temps géologiques. (fr)
  • The silica cycle is the biogeochemical cycle in which biogenic silica is transported between the Earth's systems. Silicon is considered a bioessential element and is one of the most abundant elements on Earth. The silica cycle has significant overlap with the carbon cycle (see carbonate–silicate cycle) and plays an important role in the sequestration of carbon through continental weathering, biogenic export and burial as oozes on geologic timescales. (en)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/SiO_H2O.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Calocycloma_sp._-_Radiolarian_(32163186535).jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Stephanopyxis_grunowii.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/WOA09_sea-surf_H4SIO4_AYool.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Low-temperature_processes_controlling_silicon_dissolution_in_seawater.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Silica_cycle.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Silicon_cycle_and_balance_in_the_modern_world_ocean.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/Marine_Silica_Cycle.png
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