Diatoms plays a large role in oceanography. Due to the shell they have, Diatoms, once they die, become part of the sediment, leaving their silicate shell(Si02) behind. This is appropriately named diatomic earth. Over time, the sediment will weather out, providing more silica to the ocean. They are omnipresent, as they are marine floaters. They also provide how the condition of the water is and is used as a gauging tool for environments in the past, determining if there was any sort of pollution. They usually set a good record as they started to appear in the Cretaceous period. There are three types of diatoms, for three different types of diatoms based on nutrient limit toleration and water speed, the categories being low profile guild, medium profile guild and high profile guild. The diatoms in the low profile guild tend to be in nutrient-poor and live in high speed habitats. High profile guilds tend to live in
nutrient high areas along with places with slow running water. This could be called their ideal spot. Last but not least, the medium profile guild would live in areas of moderate nutrients and moderate water speed.

Passy, Sophia I. "Diatom ecological guilds display distinct and predictable behavior along nutrient and disturbance gradients in running waters."
Aquatic Botany 86.2 (2007): 171-178.
Academic Search Premier. EBSCO. Web. 29 Apr. 2011.
D. B. Lazarus, B. Kotrc, G. Wulf, and D. N. Schmidt. Radiolarians decreased silicification as an evolutionary response to reduced Cenozoic ocean silica availability. PNAS, June 9, 2009; 106(23): 9333 - 9338.