Science // Dinosaurs & Paleontology

How Fossils Form

Explain in simple terms how fossils form: an organism dies and is quickly buried in sediment; over millions of years minerals replace the remains and the sediment turns to rock, preserving the shape

Ages
7 to 9
Type
Concept
Builds on
3 topics
Leads to
3 topics

Quick check

If the learner made a salt-dough fossil at school, could they explain how real fossils form underground over millions of years?

Ask this to see whether the topic is secure.

Topic // Mastery

What mastery looks like

What a learner can do once this topic is secure.
  • Describe the basic sequence: organism dies, buried in sediment, minerals replace remains over time
  • Explain why fossilisation is rare — most organisms decompose before being buried
  • Use the words 'sediment', 'minerals', and 'rock' correctly when explaining

Topic // Map

Where this fits

What to learn first and what this topic opens up, with the reason for each link. Required links come first.
  • RequiredMust come first
  • HelpfulHelps, but not essential

Before this

3 topics
  • Dinosaurs & Paleontology // Ages 5 to 7

    Must understand what fossils are before learning how they form in detail

  • Dinosaurs & Paleontology // Ages 5 to 7

    Understanding how fossils form (and that fossil evidence is the basis of dinosaur science) is enriched by the prior understanding that dinosaurs are real animals distinct from fictional or commonly-confused creatures — scientific reasoning starts from accurate categorisation

  • Earth's Systems // Ages 7 to 8

    Curriculum fossil formation topic (GB Y3) directly underpins detailed dinosaur fossil formation understanding

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How Fossils Form

Ages 7 to 9 // Concept

Leads to

3 topics
  • Dinosaurs & Paleontology // Ages 9 to 11

    Must understand fossil formation in sediment before understanding rock layer sequencing

  • Dinosaurs & Paleontology // Ages 9 to 11

    Must understand fossil formation before learning field excavation methods

  • Dinosaurs & Paleontology // Ages 7 to 9

    Understanding formation helps contextualise different fossil types

Topic // Research-informed

Teaching notes

From the Marble Skill Taxonomy. These notes have not been validated in classrooms, so treat them as a starting point for your own judgement.

The approach

For ages 7–9, teach fossilisation as an ordered CAUSAL chain with conditions: (1) an organism dies; (2) it is RAPIDLY BURIED in sediment (mud/sand) — the make-or-break step, because exposed remains rot or are scavenged; (3) soft parts decay while hard parts (bone, teeth, shell) remain; (4) over millions of years minerals carried by groundwater seep into the hard remains, filling tiny spaces and often gradually replacing the original material, while the sediment compacts and hardens into rock, preserving the shape; (5) later uplift and erosion expose it. Burial is necessary but does not guarantee a fossil. Make RARITY explicit so children reason that most living things leave no fossil, seeding the big idea that the fossil record is an incomplete, lucky sample. Use correct vocabulary (sediment, minerals, rock, buried) in context. The strongest proposed activity is intended to let children choose settings, with quick burial decided by setting-dependent chance, and run time forward so that rarity may become an observed outcome rather than a stated fact; staged diagrams and ordering/check tasks support the sequence and vocabulary.

Common misconceptions

  • 'Fossils are the original bone, unchanged' — minerals usually replace the remains; a fossil is rock in the shape of the original.
  • 'Any dead animal becomes a fossil' — fossilisation is rare; most decay or are eaten before burial.
  • 'Fossils form quickly' — mineral replacement and rock formation take (typically) millions of years.
  • 'Soft parts fossilise as easily as bones' — usually only hard parts (bone, teeth, shell) survive; soft tissue rarely preserves.
  • 'Fossils form on the surface where the animal died' — burial in sediment (often water-laid) is essential; surface remains are lost.

Useful representations

  • A staged cross-section: dead animal on a riverbed → layers of sediment pile on → minerals replace bone → rock with fossil → erosion exposes it.
  • A timeline slider showing 'millions of years' compressing the mineralisation step.
  • A 'fossil or lost?' branching diagram: buried quickly → fossil; left exposed → rots/scavenged → no fossil.
  • Soft-parts-vs-hard-parts labelling on an organism.

Teaching practices

  • Teach it as a conditional CAUSAL chain (each step enables the next), foregrounding rapid burial as the make-or-break step.
  • Make rarity explicit — have children reason that most animals rot or are eaten, so only a tiny fraction fossilise; this seeds 'the fossil record is incomplete'.
  • Distinguish soft parts (usually lost) from hard parts (bone, teeth, shell) that typically fossilise, explaining why we mostly find skeletons.
  • Insist on correct vocabulary (sediment, minerals, rock, buried) used in context, per Y3 'Rocks'.
  • Use a compare-conditions approach (buried fast vs left exposed) so the necessity of burial is discovered, not asserted.

Activities to try

  1. 1

    Play fate for a dead animal: vary conditions and run time forward

    Why it works: Fossilisation is a conditional sequence in which rapid burial before decay is the crux. Burial is needed but not a guarantee, and because most animals are never buried fast enough, only a tiny lucky fraction fossilise, so the fossil record is incomplete.

    1. For each of about 20 animals, choose where the body falls (e.g. muddy river delta, dry plain, open ground); the model then decides by chance whether sediment covers it quickly or it is left exposed. The odds depend on the setting: quick burial is more likely in a muddy delta and unlikely on dry open ground.
    2. Advance a time dial forward through 'millions of years' and watch what happens for each choice.
    3. For buried-quickly cases, observe the sequence: soft parts fade, hard parts (bone/teeth/shell) remain, minerals seep in and the bone colour-shifts to 'stone', sediment layers compact and harden into rock, then uplift and erosion reveal the fossil. Notice that some buried cases still end with no fossil (for example, the bone dissolves or the rock is later worn away), and some fossils are never exposed.
    4. For left-exposed cases, observe scavengers and decay strip the body to nothing — 'no fossil'.
    5. Keep a running tally of how many of the 20 animals became fossils, then state in your own words why fossils are rare.
  2. 2

    Compare buried vs exposed: the 'fossil or lost?' branch

    Why it works: Burial before decay is the pivotal condition that determines whether anything is preserved at all.

    1. Look at two identical animals that die in the same place; one is buried quickly by sediment, the other is left on the surface.
    2. Predict what will happen to each after a very long time, and say why.
    3. Trace a branching diagram: buried quickly → hard parts remain → minerals replace them → rock → fossil; left exposed → rots/scavenged → no fossil.
    4. Explain in one sentence why quick burial is the step that makes the difference.
  3. 3

    Read the staged cross-section and label soft vs hard parts

    Why it works: The ordered sequence of fossilisation, and why hard parts are usually what we find because soft tissue rarely preserves.

    1. Study a staged cross-section: dead animal on a riverbed → layers of sediment pile on → minerals replace the bone → rock holding a fossil → erosion exposes it.
    2. Reveal each stage's caption in order and retell the sequence aloud using the words sediment, minerals, and rock.
    3. On a picture of an organism, label which parts are soft (usually lost) and which are hard — bone, teeth, shell — and typically survive.
    4. Explain why we mostly find skeletons rather than whole animals.

Science // Dinosaurs & Paleontology