Unveiling the Secrets of Ammonitic Fossils: A Journey into the Past
Ammonitic refers to a type of fossilized cephalopod (such as an ammonite) that has been replaced by calcite or other minerals. This process, known as replacement mineralization, can occur over time as the original organic material of the fossil is broken down and replaced by minerals from the surrounding environment. The result is a fossil with a detailed internal structure that is preserved in three dimensions, providing valuable information for paleontologists studying the evolution and diversity of ancient life forms.
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