Most corals can only live in warm, fairly shallow waters of about 40 ft. deep. Any deeper and the water would be too cold and the corals would die off.
Limestone is made up out of fossils of corals and shells from the water.
Usually 72 - 76 degrees F, but most corals prefer different temps, when answering this question it depends on if it is soft corals or hard corals, but this is the average temp
Yes, soft corals can be food for certain organisms such as certain shrimp, snails, and nudibranchs. Some fish species may also feed on soft corals as part of their diet.
Although corals first appeared in the Cambrian period, some 542 million years ago, fossils are extremely rare until the Ordovician period, 100 million years later, when rugose and tabulate corals became widespread.
The presence of marine fossils within the limestone is the best observation that shows it was formed from ocean sediments. Marine fossils like shells, corals, or sea creatures preserved within the rock provide direct evidence of its marine origin. Additionally, the presence of ripple marks or cross-bedding in the limestone can also indicate its formation in a marine environment.
Like most fish, corals do not have a certain size that they stop growing there for, they will continue to grow. Most corals do slow down when they get huge sizes but never stop.
about 75 degrees Fahrenheit
Aragonite, a carbonate mineral.
A coral reef.
Corals cannot flourish with opaque water. With this, they need clear water for them to get sunlight to do well. They also need warm temperature specially the reef-building corals.
it occurs between the tropic where the temperature is at least 21 degrees centigrade. the waters should not be deep because the corals need sunlight to grow. in deep waters sun light doesnt penetrate. so temperature and shallow water are ideal conditions for the corals to grow. this mainly happens between the tropic i.e tropic of cancer and tropic of capricon.
Limestone is a biochemical rock that can contain fossils. It is formed from the accumulation of calcite or aragonite shells or skeletal fragments of organisms such as corals, foraminifera, and mollusks. Over time, these remains can be compressed and preserved in the rock.