Alot of sea creatures do not need the strong skeleton to support their weight. But we have barely explored any of the actual deep sea, so who knows what might be found.
Its when a sea animal forms a skeleton from calcium carbonate (CaCO3). Calcium carbonate is dissolved in seawater, but less soluable at higher temperatures. The majority of animals with calcareous skeletons, such as corals, are found in the tropics where it takes less energy to get it out of the seawater
Calcareous oozes form when the calcium carbonate shells and skeletons of marine organisms, such as foraminifera and coccolithophores, accumulate on the ocean floor. Over time, these calcareous remains compact and cement together to form a sediment known as calcareous ooze.
Calcareous ooze is an example of a type of biogenic sediment made up of the skeletal remains of marine organisms like foraminifera, coccolithophores, and pteropods. It is a common component of deep-sea sediments in regions where these organisms are abundant.
Internal skeletons are characteristic of vertebrates, which include animals such as mammals, birds, reptiles, amphibians, and fish. There are about 68,000 known species of vertebrates. Additionally, some invertebrates, like certain species of echinoderms (e.g., sea stars and sea urchins), also possess internal skeletons made of calcareous materials. Overall, the total number of species with internal skeletons is in the range of tens of thousands, primarily dominated by vertebrate species.
Limestone is a rock that is formed from the skeletal remains of sea animals and plants. It is primarily composed of calcium carbonate, which is derived from the shells and skeletons of marine organisms such as coral, mollusks, and foraminifera. Over time, these remains accumulate and become compacted and cemented to form limestone rock.
Deep-sea muds are primarily composed of fine-grained terrestrial material and are transported to the ocean floor by rivers or wind. Deep-sea oozes, on the other hand, are composed mainly of the calcareous or siliceous remains of microscopic marine organisms, such as foraminifera and diatoms, that accumulate on the ocean floor over time.
the best known phyla are Mollusca, Porifera.Cnidaria, Platyhelminthes, Nematoda, Annelida, Anthropoda, Echinodemata, and Chordada to which human beings belong. However no satisfactory definition exists
Limestone is a boigenic rock. It is formed as a byproduct of living things, frequently it is made from the calcareous skeletons of living creatures. If we take the Chalk as a limestone, this was made in a warm shallow sea from the shells of microscopic plankton as they died and sank to the sea floor. However along with the calcareous shells, there were also shells of diatomic plankton which are made out of silicon dioxide (quartz). After deposition as the chalk was compacted by the overlying sediments that were laid down on top of it and it became buried, the water it contained became heated and the skeletons of the silicious diatoms dissolved in the water and then were redeposited as layers of "Chert" or "Flint" in the Chalk.
The phylum Echinodermata has an internal calcareous skeleton made up of plates or ossicles. This skeleton provides support and protection for organisms in this phylum, such as sea stars and sea urchins.
the galopagos islands
On the ocean floor
the mindanao deep found in the souther part of the Philippines. its deep is enough to sink the mt. Everest