Just as ocean beaches display a variety of sediment types, the ocean floor may be made of sand, rock, remains of living organisms, or other material. The grains and particles that make up the seafloor sediments are classified by their size and their point of origin. Sediments can come from land (terrigenous), from living organisms (biogenous), from chemical reactions in the water column (hydrogenous), and even from outer space (cosmogenous).
Terrigenous sediments dominate the edges of the ocean basins, close to land where they originated. As you move deeper into the ocean basins, biogenous sediments begin to dominate. Biogenous sediments can consist of waste products or remains of organisms, including those of microscopic phytoplankton and zooplankton. When skeletal remains of microscopic organisms make up more than 30% of the sediment, it is called "ooze."
There are two types of oozes, calcareous ooze and siliceous ooze. Calcareous ooze, the most abundant of all biogenous sediments, comes from organisms whose shells (also called tests) are calcium-based, such as those of foraminifera, a type of zooplankton. Foraminifera are one of the most abundant types of zooplankton and are widely distributed throughout the surface of the world's oceans.
Siliceous oozes are made up of the remains of diatoms, a microscopic phytoplankton, and radiolaria, a microscopic zooplankton. Diatoms are one of the most important primary producers in the ocean. Because they are primary producers, diatoms are found in nutrient-rich areas of the ocean especially in areas of upwelling like the polar seas. As you move from continental shelf to open ocean areas, the number of diatoms present decreases. Radiolarians, the other source of siliceous ooze, feed on phytoplankton and thus are also more abundant in nutrient-rich water. However, radiolaria favor the equatorial upwelling zones as opposed to the polar upwelling zones.
Another factor that affects where biogenous sediments will occur is the depth of the ocean floor. Calcium carbonate dissolves readily under pressure and in cold water, therefore deeper ocean floors will have less calcareous ooze. At a depth of about 5 km, the rate of dissolution (how quickly calcium carbonate dissolves) is faster than the rate at which calcium shells are raining down from above. This depth is called the carbonate compensation depth or CCD.
Using what you've learned about the distribution of diatoms, radiolaria and foraminifera and about the carbonate compensation depth, predict where you think you would find calcareous and siliceous oozes. Print a global map, and mark your predictions on it.
Next, print the IUPUI's Introduction to Oceanography: Marine Sediment Map. This map shows the general location of
Lisa Ayers Lawrence, Virginia Sea Grant, Virginia Institute of Marine Science
Terrigenous, Biogenous, Hydrogenous, Cosmogenous, Calcareous ooze, Siliceous ooze, Foraminifera, Diatoms, adiolaria, Carbonate compensation depth
Natl. Science Standards
IK-1 IK-2 L5-4 L9-5 ES5-1 ES9-2
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