Limestones are mostly made of calcium carbonate. It is originally made by small photosynthetic protists like certain bacteria, coccolithophores, and algae. Then the carbonate gets used by various animals, like bivalves and the polyps which make coral reefs. They build their shells or framework out of CaCO3 crystals.
- "[Coccolithophores] were the first organisms to bring about a steady rain of calcium carbonate from the upper, illuminated zone of the ocean towards the deep sea".p144
Carbonates are rocks formed from these sources, plus any CaCO3 which is precipitated out of solution. Some carbonate dissolves in the water. It gets precipitated when the physical condition of the water changes. For example, if the concentration of CaCO3 is high, then a temperature drop, or a pH (acidity) change, can cause precipitation.
Florida Bay [change]
Florida Bay, the shallow lagoon behind the Florida Keys, is a model for the conditions which produced limestones on the continental shelf. Of course, all the species were somewhat different then but, as an ecosystem, it is similar.
In the Florida Bay a type of flowering plant called sea grass is in abundance. Also in abundance is white, milky water full of calcium carbonate. This is mainly formed by Melobesia, a small red alga which lives on the sea grass.p151 Finally, the organisms produce huge amounts of slime, which is a polysaccharide. There is good reason to think the slime is produced by microorganisms to control the way their carbonate skeletons are formed.p139 As a side-effect the slime limits the amount of carbonate which goes into solution.p155
Florida Bay is a flat platform which has laid down a huge amount of carbonate rock.
- "You have to drill for more than 3000 feet before you reach a different rock type, and that is of Cretaceous age—some 70 million years ago".p158
Fossiliferous limestones [change]
Many limestones contain fossils, and some are made up almost entirely of skeletal material. Chalk is ~99% coccoliths; Solnhofen limestone is famous for its animal fossils; and there are many shelly limestones from different periods. Limestone is not found much before the Cambrian period, because shelled animals had not yet evolved.
When limestone is heated to a high temperature, and squeezed at the base of a mountain, it becomes the metamorphic rock marble. Marbles are fairly dense, relatively easy to cut, or be shaped into blocks, and some forms are white in colour.
Limestone is hard enough to resist weathering but usually soft enough to be worked (cut and carved) by stonemasons. It is used for building material. Limestone, particularly Portland limestone, became popular in the 19th and 20th centuries for building things such as churches, banks and houses.
Related pages [change]
- "Limestone". www.watersheds.org. http://www.watersheds.org/earth/limestone.htm. Retrieved 2009-07-28.
- "Calcite". mine-engineer.com. http://www.mine-engineer.com/mining/mineral/calcite.htm. Retrieved 2008-02-13.
- "Limestone (mineral)".. Retrieved on 13 February 2008.
- Lapo 1986. Traces of bygone biospheres. Synergetic Press: Oracle, AZ.
- Westbroek, Peter 1991. Life as a geological force: dynamics of the Earth. Norton, New York. ISBN 0-393-30817-0
- Small shelly fossils occur in the latest Ediacaran for the first time.
- Learn Science intermediate, grades 5 to 6, by Mike Evans and Linda Ellis
- West, Ian 2012. Ian West's website on the Jurassic Coast and more. Includes the Isle of Portland and its surrounds. Soton.ac.uk
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