Fossils
Types of fossils
- Entire organism preserved
- Original hard parts of invertebrates preserved
- Skeleton preserved
- Altered hard parts of organisms preserved
- Traces of organisms preserved
- Petrification
Entire organism preserved
- In a continuous dry or cold region
- All organic remains, even softer body parts, may remain unchanged for a long time under favourable conditions
- Preserved from bacterial decay
Original hard parts preserved
- Harder parts such as shells and spicules get fossilised
Skeleton preserved
- Skeletons of vertebrates become preserved in their original shape and structure
Altered hard parts preserved
- Original hard parts get altered
- Due to carbonisation
- Soft parts of a body leave behind a film of carbon, so the exact body outline obtained
Petrification
- When the mineral-rich water penetrates through the pores made by decomposition of the organic matter gets deposited in these pores
Specific fossil types
- Mineralisation
- Internal mould
- External mould
- Cast
- Tracks
- Trails
- Burrows
- Borings
- Coprolites
- Gastroliths
Mineralisation
- Certain structures of the fossil remains are replaced by specific minerals
Internal mould
- The cavity is filled with mud or sediments or minerals before the shell is dissolved by percolating water
External mould
- The shells of an organism are buried in sediment or mud which becomes hardened. Organic material is removed by percolating acidified water and a cavity is formed
Cast
- When an animal or other organism dies, its flesh decays and its bones deteriorate. Minerals enter the cavity gradually
Tracks
- Impression of feet passing animal on mud and wet sand covered by sediment before disturbed
Trails
- Irregular markings of moving animals on sedimentary rocks
Burrows
- Presence of burrows in sedimentary rocks
Borings
- Holes made by animals for the sake of food or shelter in wood and rocks
Coprolites
- Fossilised faeces of ancient animals
- Provide information about food and feeding habits of fossil animals
Gastroliths
- Hard, stony pieces found in the stomachs of ancient reptiles and fish.
Uses of fossils
- Chronostratigraphy
- Biostratigraphy
- Index fossils and correlation of rocks
- Paleogeography
- Relative dating
Chronostratigraphy
- Concerned with the age of strata (rock) and the time they represent in relation to other layers
Biostratigraphy
- Fossil contents of beds are used in interpreting the historical sequence of their occurrence