Fossilization (Unit 3) - Types of Fossilization at Florissant
When fluids supersaturated with silica and other minerals penetrate the remains of organisms with abundant pore systems such as trees, the mineral precipitates within the pores and the original material (at least most of it) eventually rots or dissolves away. This leaves behind a mineralized version of the original organism.
The best-known example of permineralization is petrified wood, which is abundant at Florissant. About 34 million years ago, a volcanic mudflow called a lahar killed and buried a forest of redwoods and other trees. Eventually the portion of the trees above the mudflow rotted away, leaving the encased trunks buried. The wood was slowly replaced with silica from supersaturated ground water. Detailed study has shown what possibly could be original plant material left behind in some of the stumps, but for the most part they are completely replaced with silica. The wood is preserved so well that scientists can study the structure under a microscope, down to the individual cells.
Fossil bones and teeth of mammals, birds, and fish are also preserved by permineralization in many cases.
Some organisms, particularly fragile insects and plants, can be preserved in shale as a carbon film "image" of the original organism. The paper wasp Palaeovespa and many of the other fossil plants and insects at Florissant, are preserved as carbon films. Some carbon films are so detailed that patterns on butterfly and other insect wings can still be seen.
Impression fossils are another common form of preservation at Florissant. These are usually formed from sturdy leaves or molluscs such as snails and clams, which left three-dimensional impressions of their surfaces in the rock.
Did You Know?
The modern Tsetse fly lives in Africa, but examples like the fossil pictured here have been found in the Florissant fossil beds. This fossil is 34.07 million years old. This image is protected by copyright. All rights reserved. To learn More...