Fossils: evidence of past life
- Types of fossils
- Petrified cavities and pores are filled with
precipitated mineral matter
- Formed by replacement cell material is removed
and replaced with mineral matter
- Mold shell or other structure is buried and
then dissolved by underground water
- Cast hollow space of a mold is filled with
mineral matter
- Natural casts of shelled invertebrates
- Carbonization organic matter becomes a thin
residue of carbon
- Impression replica of the fossil's surface
preserved in fine-grained sediment
- Preservation in amber hardened resin of ancient
trees surrounds an organism
- Indirect evidence includes
- Tracks
- Burrows
- Coprolites fossil dung and stomach contents
- Gastroliths stomach stones used to grind
food by some extinct reptiles
- A dinosaur footprint
- Conditions favoring preservation
- Rapid burial
- Possession of hard parts
- Fossils and correlation
- Principle of fossil succession
- Fossils succeed one another in a definite and
determinable order
- Proposed by William Smith late 1700s and
early 1800s
- Correlation of rock layers
- Matching rocks of similar age in different regions
- Often relies upon fossils
- Index fossils
- Widespread geographically
- Existed for a short range of geologic time
Relative dating | Fossils:
evidence of past life | Radioactivity and radiometric dating
| Geologic time scale | Links
| top | Classes
Home
|