The bulk of marine skeletal remains are composed of the mineral calcite. Some marine organisms also have shells of aragonite or silica.
Calcium carbonate, or CaCO3 is the compound that is found in shells of marine animals and that makes up limestone.
Shells and skeletons of sea animals
Shelly limestone
CaCO3
Limestone is made by the accumulation of shells and marine organisms.
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.
Chalk
limestone
A lot of shells of marine organisms wind up on the ocean floor. Bones do not last on the ocean floor, they get eaten. But shells can last.
Coquina is an organic sedimentary rock composed primarily of cemented shells of marine organisms.
Limestone is made by the accumulation of shells and marine organisms.
Two types of biogenous sediments are calcareous ooze and siliceous ooze.
Limestone
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.
Chalk
Bioclastic sedimentary rock--coquina.
limestone
Chalk is a form of limestone composed of the skeletons and secretions of small marine organisms.
They can become sedimentary rock, most likely limestone.
They can, and do. Chalk and coquina are examples of limestone formed from skeletal or shell remains of marine organisms.
Chalk is a form of limestone composed of the skeletons and secretions of small marine organisms.