The bulk of marine skeletal remains are composed of the mineral calcite. Some marine organisms also have shells of aragonite or silica.
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Shells of marine organisms are primarily composed of calcium carbonate, which is derived from minerals in seawater. The calcium carbonate can form various crystalline structures, such as calcite or aragonite, leading to different types of shells with varying levels of hardness and resilience. Additionally, shells may also contain proteins and other organic compounds that contribute to their strength and flexibility.
Calcium carbonate, or CaCO3 is the compound that is found in shells of marine animals and that makes up limestone.
Limestone is made by the accumulation of shells and marine organisms.
Shells are usually composed of calcium carbonate formed by marine organisms like mollusks. The calcium carbonate is secreted by the organism and hardens over time to create the structure of the shell.
Diatomaceous earth and limestone are both sedimentary rocks composed of the remains of ancient organisms. However, they are chemically different. Diatomaceous earth is mainly composed of the silica cell walls of diatoms, while limestone is mainly composed of calcium carbonate from the shells and skeletons of marine organisms.
Amoebic organisms with calcareous shells are called Foraminifera. These single-celled organisms have a shell made of calcium carbonate and are found in marine environments. Their shells accumulate on the ocean floor and provide valuable information for studying past climates and environments.
Shells are considered natural resources as they are derived from marine organisms. They have various uses such as in jewelry, decoration, and traditional crafts. Shells are also important in marine ecosystems for providing protection to certain species and contributing to the overall biodiversity of oceans.