AQA · GCSE · Biology

    Course version: 8461 · Version from Sept 2018

    What traces there were have been mainly destroyed by geological activity.

    Full specification wording

    Fossils: What traces there were have been mainly destroyed by geological activity.

    Even when a soft-bodied organism did leave a trace, that trace is unlikely to survive to the present day.

    Checked against the AQA 8461 specification (opens in a new tab) on .

    • Point 4 of 7
    • 2 key terms

    Study notes

    From the checked teaching notes for this specification point.

    The idea

    Even when a soft-bodied organism did leave a trace, that trace is unlikely to survive to the present day. Geological activity such as plate movement, mountain building, volcanic eruptions, erosion and metamorphism can crush, melt, heat or wear away fossil-bearing rock. Fossils are mostly found in sedimentary rock because sedimentary layers are less likely to be destroyed than rocks subjected to intense heat and pressure. Over millions of years, repeated cycles of erosion and rock recycling remove most ancient traces. This helps explain why the fossil record is incomplete, especially for the earliest and most fragile organisms.

    What earns the marks

    • States that geological activity has destroyed many traces of early life.
    • Names processes such as plate movement, volcanic activity, erosion or metamorphism.
    • Explains that heat and pressure can destroy fossils or the rocks containing them.
    • Links destruction of fossils to the incompleteness of the fossil record.
    • Recognises that sedimentary rock is more likely to preserve fossils than rock altered by geological activity.

    Common mistakes and how to put them right

    • Thinking fossils survive forever once formed.

      Put it right by explaining that rock recycling and geological processes destroy them.

    • Confusing geological destruction with decay.

      Put it right by separating biological decay from physical and chemical rock processes.

    • Assuming all rock types preserve fossils equally.

      Put it right by noting that heat and pressure in metamorphic rock destroy fossils.

    Exam tips

    • Name at least one specific geological process when explaining destruction.
    • Connect destroyed traces to gaps in the fossil record.
    • Use the idea of rock recycling over millions of years.

    Try the lesson

    The start of the Fossils: What traces there were have been mainly destroyed by geological activity. lesson, made from checked teaching notes for this specification point.

    Have a go first

    What has mainly destroyed the traces left by early soft-bodied life?

    Listen

    Even when a soft-bodied organism did leave a trace, that trace is unlikely to survive to the present day. Geological activity such as plate movement, mountain building, volcanic eruptions, erosion and metamorphism can crush, melt, heat or wear away fossil-bearing rock. Fossils are mostly found in sedimentary rock because sedimentary layers are less likely to be destroyed than rocks subjected to intense heat and pressure. Over millions of years, repeated cycles of erosion and rock recycling remove most ancient traces. This helps explain why the fossil record is incomplete, especially for the earliest and most fragile organisms. A strong answer earns marks for these points. States that geological activity has destroyed many traces of early life. Names processes such as plate movement, volcanic activity, erosion or metamorphism. Explains that heat and pressure can destroy fossils or the rocks containing them. Links destruction of fossils to the incompleteness of the fossil record. A common slip: Thinking fossils survive forever once formed. Instead, explaining that rock recycling and geological processes destroy them. Exam tip: Name at least one specific geological process when explaining destruction.

    See it

    A top-down flowchart. A single node labelled "Geological activity" branches into five process nodes: "Plate movement", "Mountain building", "Volcanic eruptions", "Erosion" and "Metamorphism". All five arrows lead into one node labelled "Fossil-bearing rock crushed, melted, heated or worn away". An arrow from that node leads to "Most ancient traces removed over millions of years", and a final arrow leads to "Fossil record incomplete".
    Shows how geological processes destroy fossil-bearing rock and leave the fossil record incomplete.

    Key words

    Say what each word means before you turn the card.

    Geological processes

    Try answering aloud or in your head before turning the card.

    Incomplete fossil record

    Try answering aloud or in your head before turning the card.

    See every definition
    Geological processes
    Processes such as plate movement, mountain building, volcanic eruptions, erosion and metamorphism that can crush, melt, heat or wear away fossil-bearing rock.
    Incomplete fossil record
    The gaps in the record of past life that result from geological activity destroying many traces, especially of the earliest and most fragile organisms.

    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. A single node labelled "Geological activity" branches into five process nodes: "Plate movement", "Mountain building", "Volcanic eruptions", "Erosion" and "Metamorphism". All five arrows lead into one node labelled "Fossil-bearing rock crushed, melted, heated or worn away". An arrow from that node leads to "Most ancient traces removed over millions of years", and a final arrow leads to "Fossil record incomplete".
    • 1Box 1

    • 2Box 2

    • 3Box 3

    0 of 3 labelled

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