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Criteria for a Good Index Fossil

An index fossil is a fossil that can be used to assign a relative age to a layer or layers of rock, thus placing the layer and any other fossils in it at the proper place on the geologic time scale.
  1. Good Index Fossils are Common

    • To be useful as an index fossil, the fossil must be common. The more common a fossil, the more likely a paleontologist will find it in a layer of rock. Rare forms are not useful, because their absence does not necessarily mean that the rocks are of a different age--it may simply mean that the rare animal wasn't nearby.

    Good Index Fossils are Widespread

    • The best index fossils are animals that are present in rocks all over the world, and present in a wide variety of rock types. Swimming or floating animals tend to make better index fossils because their remains can be found almost anywhere, while plants and most bottom-dwellers live only within a narrow range of conditions.

    Good Index Fossils Represent a Limited Time Span

    • The presence of a fossil animal that flourished for several geologic time periods does little to narrow down the age of a rock layer. Fossil animals that were around for a relatively short time allow more precise definition of a layer's relative age.


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