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