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  2. Shelly limestone - Wikipedia

    en.wikipedia.org/wiki/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.

  3. Fossiliferous limestone - Wikipedia

    en.wikipedia.org/wiki/Fossiliferous_limestone

    If a particular type of fossil dominates, a more specialized term can be used as in "Crinoidal", "Coralline", "Conchoidal" limestone. If seashells, shell fragments, and shell sand form a significant part of the rock, a term "shell limestone" is used. [1] The fossils in these rocks may be of macroscopic or microscopic size.

  4. Marine biogenic calcification - Wikipedia

    en.wikipedia.org/wiki/Marine_biogenic_calcification

    The shell of a Patella piperatamollusc seen from the dorsal, lateral (left side), ventral, back, ... Limestone rock, which consists mostly of calcite, is a prime ...

  5. Limestone - Wikipedia

    en.wikipedia.org/wiki/Limestone

    Limestone (calcium carbonate CaCO 3) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of CaCO 3. Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place ...

  6. Coquina - Wikipedia

    en.wikipedia.org/wiki/Coquina

    Coquina strata from Caleta Hornos (Coquimbo Formation). Coquina (/ k oʊ ˈ k iː n ə /) is a sedimentary rock that is composed either wholly or almost entirely of the transported, abraded, and mechanically sorted fragments of mollusks, trilobites, brachiopods, or other invertebrates.

  7. Geiseltal (fossil deposit) - Wikipedia

    en.wikipedia.org/wiki/Geiseltal_(fossil_deposit)

    The area was bordered to the south by a shell limestone plateau with steep slopes sloping down to the north. The plateau itself was partly karstified. The chemical weathering created limestone water which penetrated the moorland and ensured the excellent preservation of the fossils. [141] Thick layer of leaves of Dryophyllum from the Geiseltal