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Shark history is known mainly from the preservation ability of their hard
resilient calcium phosphate teeth.
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It is unusual to find shark skeletons or impressions in the fossil record
since this would require a low energy, anoxic environment with an extremely
rapid burial rate; otherwise the cartilaginous skeleton would decompose
and the individual apatite (calcium phosphate) minerals which overlay the
cartilaginous skeleton would be transported to another location.
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Since some sharks lose teeth at a rate of one every four hours, the number
of recovered fossilized teeth is extremely high.
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Shark teeth are the most common vertebrate fossil.
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