Silisiumdiatomfrustuler
Silisiumdiatomfrustuler refers to the intricate, ornate cell walls of diatoms, which are single-celled algae. These frustules are primarily composed of amorphous silica, or hydrated silicon dioxide. Diatoms are a major group of algae and are among the most common types of phytoplankton in the world's oceans. The frustule is a key characteristic used in diatom taxonomy and identification due to its diversity in shape, size, and ornamentation.
Each frustule consists of two overlapping halves, called valves, that fit together like a lid on a
Accumulations of fossilized diatom frustules form a sedimentary rock known as diatomaceous earth, or diatomite. This