Shelly limestone
Shelly limestone is a highly fossiliferous limestone, composed of a number of fossilized organisms such as brachiopods, bryozoans, crinoids, sponges, corals and mollusks. It varies in color, texture and hardness. Coquina is a poorly indurated form of shelly limestone.
Shelly limestone is a sedimentary rock because it is made up of fragments. To be shelly, it is full of broken shells which are "glued" together with calcite. Calcium carbonate often makes up around 10% of the volume, whilst many varied sized shells from granular to very large pebbles. Its color is gray.
Formation
Each shelly limestone is unique in its own way, where every stone of this type is composed of different fossilized organism and shell fragments. Shelly limestones are mainly found near where marine life live or where marine life once occupied.The unique qualities of a shelly limestone are formed with the help of calcite, acting as a sticking agent for small shell fragments, dead marine organism and other minerals. Typically, the rock is composed of approximately 10 percent calcium carbonate. The appearance of shelly limestones can differ in color, composition, hardness and texture depending on where the stone is formed. Generally, however, shelly limestones have noticeable shell fragments in various sizes. Shelly limestone is considered a carbonate rock because the stone is mainly composed primarily of carbonate minerals. In detail, shelly limestones are formed when rocks containing different minerals get weathered down then get transported to a standing body of water. From here organisms that precipitate carbon, phosphate, and silicate materials combine with the minerals and go through a process called deposition, where the minerals and organic components sort by size and density. Once sorted, the fragments go through diagenesis, where the fragments compress and cement together, and over time will form a shelly limestone.
Shelly limestone can be found dating back to Precambrian and Cambrian times.