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Diatoms / Diatomaceous Earth by Almicanna

Diatomaceous earth, also known as diatoms or kieselguhr, is a fossil mineral that has formed from the microscopic shells of deceased diatoms. Diatoms are an important component of the plant plankton in the world's oceans, accounting for over one-fifth of the biomass produced through photosynthesis.

Since the Cretaceous period, thick sedimentary layers composed of fossilized diatom shells have formed in lakes and marine bays, reaching several hundred meters in height in some cases.

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