2.5.10

The Formation of Fossils

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Fossils

Fossils are the remains or traces of ancient life. Fossils are found in rocks and have been preserved by natural processes. There are 3 different ways of forming fossils:

Hardening soft materials

Hardening soft materials

  • The hardening of soft materials can produce casts or impressions, such as footprints.
    • For example, clay hardens around an organism that is buried within it. This organism then decays, leaving behind a cast of itself.
Preservation when decay is not possible

Preservation when decay is not possible

  • Where decomposers cannot act, preservation is possible.
  • Decomposers cannot operate in glaciers (extreme, low temperatures) and peat bogs (extreme acidity).
Mineral replacement

Mineral replacement

  • Hard parts of organisms are gradually replaced by minerals as they decay slowly, creating a rock-like substance.
  • When the surrounding sediment turns to rock, the teeth-shaped mineral structure remains distinct (different).
Jump to other topics
1

Biology

1.1

Cells, Tissues & Organs

1.2

Reproduction & Variation

1.3

Ecological Relationships & Classification

1.4

Digestion & Nutrition

1.5

Plants & Photosynthesis

1.6

Biological Systems & Processes

2

Chemistry

2.1

Particles

2.2

Chemical Reactions

2.3

Atoms, Elements, Compounds

2.4

The Periodic Table

2.5

Materials & the Earth

2.6

Reactivity

2.7

Energetics

2.8

Properties of Materials

3

Physics

3.1

Energy

3.2

Forces & Motion

3.3

Waves

3.4

Electricity & Magnetism

3.5

Matter

3.6

Space Physics

4

Disciplinary Knowledge

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