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Climate Change

Icehouse and greenhouse Earth, from Cenozoic cooling to the Holocene

  • 2 things to know
  • Component 03

Overview

Recall questions on greenhouse and icehouse Earth, cooling over the last 100 million years and its causes, silicate weathering, the glaciation of Antarctica and ocean gateways, the Quaternary glacial cycles and their changing rhythm, the Last Glacial Maximum and its ice sheets, the Holocene, the Medieval Warm Period and the Little Ice Age.

What you need to know

Answer each one before you reveal it.

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Key term

Give two reasons for the long-term cooling of the last 100 million years.

Key term

Define a greenhouse Earth state.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    Define a greenhouse Earth state.

    Model answer

    A greenhouse Earth is a prolonged interval with no permanent ice at either pole, high atmospheric CO₂ and a weak temperature gradient between equator and poles.

  2. 2

    Define an icehouse Earth state.

    Model answer

    An icehouse Earth is a prolonged interval in which permanent ice exists at one or both poles, with that ice repeatedly expanding and contracting.

  3. 3

    Is Earth currently in a greenhouse or an icehouse state, and how can you tell?

    Model answer

    Earth is in an icehouse state, because permanent ice sheets survive on Greenland and Antarctica even through warm interglacials.

  4. 4

    Describe the overall direction of global climate over the past 100 million years.

    Model answer

    Climate has cooled substantially, from a Cretaceous world with no polar ice to the glaciated icehouse of the present.

  5. 5

    Give two reasons for the long-term cooling of the last 100 million years.

    Model answer

    Rates of sea-floor spreading and volcanic outgassing of CO₂ declined, and mountain uplift such as the rise of the Himalaya increased chemical weathering, which draws CO₂ out of the atmosphere.

  6. 6

    How does chemical weathering of silicate rock cool the planet over geological time?

    Model answer

    Weathering consumes atmospheric CO₂ and converts it to dissolved bicarbonate, which is carried to the sea and buried as carbonate sediment, weakening the greenhouse effect.

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AThe lower quartile is the 2nd value, 11 cm.
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