AQA · GCSE · Combined Science

    Course version: 8464 · Version from Sept 2018

    We can learn from fossils how much or how little different organisms have…

    Full specification wording

    Fossils: We can learn from fossils how much or how little different organisms have changed as life developed on Earth.

    Fossils are preserved remains or traces of organisms from the past, and comparing them with living species reveals the extent of change over geological time.

    Checked against the AQA 8464 specification (opens in a new tab) on .

    • Point 7 of 8
    • 4 key terms

    Study notes

    From the checked teaching notes for this specification point.

    The idea

    Fossils are preserved remains or traces of organisms from the past, and comparing them with living species reveals the extent of change over geological time. Some lineages show little change: horsehoe crabs in rocks hundreds of millions of years old closely resemble modern forms, so they are often called living fossils. Others show major change: comparing ancient whale fossils with modern whales reveals the gradual loss of hind limbs and the shift to flippers. Fossils also document extinction, showing that many organisms no longer exist. By arranging fossils by rock age, we can see whether a body plan stayed stable or was modified, and how life on Earth developed.

    What earns the marks

    • Fossils are remains or traces of organisms preserved in rocks, ice or amber, and their age can be estimated from the rock layer in which they are found.
    • Comparing the structure of a fossil with a living organism shows whether the body plan has changed a lot or only a little over time.
    • Organisms such as horseshoe crabs have changed very little over hundreds of millions of years, whereas whale ancestors show major changes in limb structure.
    • Fossils provide evidence that some species became extinct, because their fossils appear in older rocks but no living examples exist.
    • Sequencing fossils from oldest to youngest allows trends in body structure to be identified as life developed on Earth.

    Common mistakes and how to put them right

    • Thinking every fossil is a complete skeleton.

      Put it right: Most fossils are fragments, impressions or traces, so conclusions are based on the features preserved.

    • Assuming all organisms change at the same rate.

      Put it right: Some lineages remain similar for long periods while others change substantially.

    • Believing fossils show the exact age of an organism without evidence.

      Put it right: Age is inferred from the rock layer or dating methods, not from the fossil alone.

    Exam tips

    • When describing change, name the specific feature compared, such as limb bones or shell shape, rather than saying the organism 'changed'.
    • Use the command word: 'describe' needs features and trends, while 'explain' needs a reason linking the fossil evidence to change over time.
    • Quote data from any chart or table, such as 'the fossil is 300 million years old', to support your comparison.

    Try the lesson

    The start of the Fossils: We can learn from fossils how much or how little different organisms have changed as life developed on Earth. lesson, made from checked teaching notes for this specification point.

    Have a go first

    The fossil record of horses shows a sequence of species over 50 million years. Older fossils show small animals with four toes, while more recent fossils show larger animals with a single hoof. What does this fossil evidence demonstrate about the evolution of horses?

    Listen

    Fossils are preserved remains or traces of organisms from the past, and comparing them with living species reveals the extent of change over geological time. Some lineages show little change: horsehoe crabs in rocks hundreds of millions of years old closely resemble modern forms, so they are often called living fossils. Others show major change: comparing ancient whale fossils with modern whales reveals the gradual loss of hind limbs and the shift to flippers. Fossils also document extinction, showing that many organisms no longer exist. By arranging fossils by rock age, we can see whether a body plan stayed stable or was modified, and how life on Earth developed. A strong answer earns marks for these points. Fossils are remains or traces of organisms preserved in rocks, ice or amber, and their age can be estimated from the rock layer in which they are found. Comparing the structure of a fossil with a living organism shows whether the body plan has changed a lot or only a little over time. Organisms such as horseshoe crabs have changed very little over hundreds of millions of years, whereas whale ancestors show major changes in limb structure. Fossils provide evidence that some species became extinct, because their fossils appear in older rocks but no living examples exist. Exam tip: When describing change, name the specific feature compared, such as limb bones or shell shape, rather than saying the organism 'changed'.

    See it

    A top-down flowchart. The first box reads 'Fossils preserved in rocks, ice or amber' and points to 'Age estimated from rock layer'. From there one arrow leads to 'Compare fossil structure with living organism', which branches into three outcomes: 'Little change: horseshoe crabs resemble modern forms', 'Major change: whale ancestors lost hind limbs and shifted to flippers', and 'Fossils in older rocks with no living examples: extinction'. A second arrow from 'Age estimated from rock layer' leads to 'Sequence fossils oldest to youngest', which points to 'Identify trends in body structure as life developed'.
    It shows how fossils are aged, compared with living organisms to judge how much or little change occurred, and sequenced to reveal trends and extinction.

    Key words

    Say what each word means before you turn the card.

    Fossils

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    Extinction

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    Change over geological time

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    Comparing fossil and living structures

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    See every definition
    Fossils
    Remains or traces of organisms preserved in rocks, ice or amber, whose age can be estimated from the rock layer in which they are found.
    Extinction
    When species no longer exist, shown by fossils appearing in older rocks but no living examples existing.
    Change over geological time
    Whether a body plan stayed stable or was modified, seen by arranging fossils by rock age as life developed on Earth.
    Comparing fossil and living structures
    Showing whether the body plan has changed a lot or only a little over time by comparing the structure of a fossil with a living organism.

    Label the diagram

    Some boxes have lost their names. Pick the right name for each number.

    The diagram again, with 3 boxes numbered instead of named. A top-down flowchart. The first box reads 'Fossils preserved in rocks, ice or amber' and points to 'Age estimated from rock layer'. From there one arrow leads to 'Compare fossil structure with living organism', which branches into three outcomes: 'Little change: horseshoe crabs resemble modern forms', 'Major change: whale ancestors lost hind limbs and shifted to flippers', and 'Fossils in older rocks with no living examples: extinction'. A second arrow from 'Age estimated from rock layer' leads to 'Sequence fossils oldest to youngest', which points to 'Identify trends in body structure as life developed'.
    • 1Box 1

    • 2Box 2

    • 3Box 3

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