Carbon dating live snail

If this hole is later filled with other minerals, it is a cast.

An endocast or internal mold is formed when sediments or minerals fill the internal cavity of an organism, such as the inside of a bivalve or snail or the hollow of a skull. If the chemistry is right, the organism (or fragment of organism) can act as a nucleus for the precipitation of minerals such as siderite, resulting in a nodule forming around it.

Some fossils consist only of skeletal remains or teeth; other fossils contain traces of skin, feathers or even soft tissues. In some cases the original remains of the organism completely dissolve or are otherwise destroyed.

The remaining organism-shaped hole in the rock is called an external mold.

In many cases, however, compressions and impressions occur together.

There are many processes that lead to fossilization, including permineralization, casts and molds, authigenic mineralization, replacement and recrystalization, adpression, carbonization, and bioimmuration.If this happens rapidly before significant decay to the organic tissue, very fine three-dimensional morphological detail can be preserved.Nodules from the Carboniferous Mazon Creek fossil beds of Illinois, USA, are among the best documented examples of such mineralization.In this case the fossil consists of original material, albeit in a geochemically altered state.This chemical change is an expression of diagenesis.

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For this reason, one term covers the two modes of preservation: adpression.

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