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Most calcium carbonate deposits are made up of the skeletal remains of marine plants and animals that have fallen to sediment on the bottom of shallow seas after their death. If the conditions are right, these sediments can build up over geological time to form extremely thick layers.
Calcareous Ooze: Fine-grained deep-ocean biogenous sediment containing at least 30% calcareous tests, or the remains of small marine organisms. Calcite: A common crystalline form of natural calcium carbonate, CaCO3, that is the basic constituent of limestone, marble, and chalk.Also called calcspar.oze: Fine-grained deep-ocean sediment composed of at least 30% calcareous or sililceous remains of small marine organisms, the remainder being clay minerals. pelagic deposit. Phosphate: A sedimentary rock composed largely of calcium phosphate and largely in the form of concretions and nodules.