polymorphism
See also restriction fragment length polymorphism; single nucleotide polymorphism.
Polymorph
Polymorph
A polymorph is a chemical composition that can crystallize into more than one type of structure. This results in different minerals with identical compositions and distinguished by their crystallography.
Some common examples of polymorphs are calcite and aragonite. The composition of these two minerals is CaCO3, but calcite is rhombohedral while aragonite is orthorhombic. Diamond and graphite , both of which are pure carbon , are also polymorphs. Diamond, however, is cubic while graphite is hexagonal. Pyrite is the cubic form of FeS2, marcasite, the orthorhombic version.
A single chemical composition that can form polymorphs does so as a response to varying conditions of formation. The temperature , pressure, and chemical environment all affect the crystallization process and can determine the resulting polymorph. For example, diamond requires very high pressure to crystallize, while graphite forms at lower pressures. For the composition CaCO3, calcite is the high temperature-low pressure polymorph while aragonite forms at higher pressures and lower temperatures.
Many polymorphs are only stable within a certain range of conditions and solid-state transitions from one polymorph to another are possible. When low-quartz, which is rhombohedral, is heated to above 1063°F (573°C), it instantaneously goes through an internal structural displacement, or shift, to form hexagonal high-quartz. This type of polymorphic transition is reversible if the temperature is lowered. Other polymorphic transitions involve extensive internal rearrangement and reconstruction of the crystal and subsequently require significantly more energy. The examples of diamond-graphite, pyrite-marcasite, and calcite-aragonite are all known as reconstructive transitions. The large amounts of energy required to effect these polymorphic changes makes the resulting mineral more stable and the process less reversible than with a displacive transition.
See also Crystals and crystallography; Mineralogy
polymorphism
1. In genetics, the existence of two or more forms that are genetically distinct from one another but contained within the same interbreeding population. The polymorphism may be transient or it may persist over many generations, when it is said to be balanced. Classical examples of polymorphisms are the presence or absence of banding in Cepaea snails, the number of spots on the wings of ladybirds, and eye colour in humans. All these are visible polymorphisms that can readily be seen in nature. Some polymorphisms, however, are cryptic and require biochemical techniques to identify phenotypic differences. Such techniques include gel electrophoresis of enzymes and other proteins, and the fragmentation of the DNA molecule by restriction enzymes (which allows the sequencing of nucleotides), both of which operate nearer to the level of the genotype.
2. In social insects, the presence of different castes within the same sex. See POLYTYPISM.
polymorphism
polymorphism
polymorphism
polymorphism
1. In genetics, the existence of two or more forms that are genetically distinct from one another but contained within the same interbreeding population. The polymorphism may be transient or it may persist over many generations, when it is said to be balanced. Classical examples of polymorphisms are the presence or absence of banding in Cepaea snails, the number of spots on the wings of ladybirds, and eye colour in humans. All these are visible polymorphism that can readily be seen in nature. Some polymorphism, however, is cryptic and requires biochemical techniques to identify phenotypic differences.
2. In social insects, the presence of different castes within the same sex. See also polytypism.